Tectonic Boundary Objects in Europe
hierarchy root: true
hierarchy root type: ConceptScheme
description: Named tectonic boundary objects as they appear on the HIKE European fault database. The determing factors for the hierarchical ranking of the tectonic boundaries are primarily their present-day spatial relation and secondly their kinematic linkage during at least deformation phase. All named tectonic boundary objects are identified by an ID representing a two-letter country-specific prefix. Fault systems and/or fault domains crossing political borders are shared by several countries. Therefore, they can contain faults from different countries, indicated by the country-specific prefixes to the respective ID.
type: ConceptScheme
created: 2020-04-30T14:26:58.648Z
has top concept: Tectonic Boundary in Belgium
has top concept: Tectonic Boundary in Albania
has top concept: Tectonic Boundary in the Pannonian Basin
has top concept: Tectonic Boundary in Denmark
has top concept: Tectonic Boundary in France
has top concept: Tectonic boundary in Lithuania
has top concept: Tectonic Boundary in Saxony-Anhalt
has top concept: Falha em Portugal
has top concept: Tectonic Boundary in Slovenia
has top concept: Tectonic Boundary in Austria
has top concept: Tectonic Boundary in Germany
has top concept: Tectonic Boundary in Ukraine
has top concept: Tectonic Boundaries in Bavaria
has top concept: Tectonic Boundary in Iceland
has top concept: Tectonic Boundary in Italy
has top concept: Tectonic Boundary in Poland
has top concept: Tectonic Boundary in Brandenburg
has top concept: Tectonic Boundary in the Netherlands

Tectonic Boundary in Belgium
type: Concept
top concept of: Tectonic Boundary Objects in Europe
created: 2021-03-23T14:34:26.952Z
narrower: Aguesses-Asse Fault
narrower: Monty Fault
narrower: Mouhy Fault
narrower: Ostende Fault
narrower: Verviers Fault
narrower: Bouhouille Fault
narrower: Malmedy fault system
narrower: Ardenne basal detachment
narrower: Borzée Fault
narrower: José Fault
narrower: Jupille Fault
narrower: Landenne Fault
narrower: Theux Fault
narrower: Walhorn Fault
narrower: Xhoris Fault
notation: BE-0
scope note: All named tectonic boundary objects that are located (at least partly) in Belgium, are identified by an ID with the prefix „BE“ listed in the notation. Fault systems and/or fault domains can cross political borders and are therefore shared by several countries. Therefore, they can contain faults from different countries, indicated by country-specific prefixes to the respective ID.
definition: Fault in Belgium, displayed in the HIKE European fault database.
in scheme: Tectonic Boundary Objects in Europe

Jupille Fault
type: Concept
created: 2021-03-23T14:34:27.021Z
notation: BE-2167
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Belgium

Aguesses-Asse Fault
type: Concept
created: 2021-03-23T14:34:26.955Z
scope note: There is still ongoing discussion about the connection between the two faults. Either they are two individual faults or they form a continuation of each other, separated by a sinistral transverse fault. Furthermore there is a discussion of the importance of the Aguesses-Asse Fault. Either it is a minor thrust separating the Herve and Liège units, both located north of the Variscan front thrust or it is a major thrust constituting an eastern segment of the Variscan front thrust and continuation of the Eifelian Fault (Cambier G. & Dejonghe L., 2010).
definition: The Aguesses and Asse Faults are both thrust faults of Variscan age (Cambier G. & Dejonghe L., 2010).
narrower: Aguesse Fault
narrower: Asse Fault
references: https://data.geoscience.earth/ncl/geoera/ref/8570
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Belgium

Aguesse Fault
type: Concept
created: 2021-03-23T14:34:26.957Z
notation: BE-2150
in scheme: Tectonic Boundary Objects in Europe
broader: Aguesses-Asse Fault

Asse Fault
type: Concept
created: 2021-03-23T14:34:26.960Z
notation: BE-2151
in scheme: Tectonic Boundary Objects in Europe
broader: Aguesses-Asse Fault

José Fault
type: Concept
created: 2021-03-23T14:34:27.018Z
notation: BE-2166
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Belgium

Borzée Fault
type: Concept
created: 2021-03-23T14:34:27.016Z
notation: BE-2162
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Belgium

Ardenne basal detachment
type: Concept
created: 2021-03-23T14:34:26.982Z
alternative label: Ardenne thrust
narrower: Haine-Sambre-Meuse fault system
narrower: Northern Variscan thrust faults
narrower: Midi Fault
narrower: Eupen Fault
narrower: Aachen Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Belgium

Haine-Sambre-Meuse fault system
type: Concept
created: 2021-03-23T14:34:26.985Z
notation: BE-2173
definition: System of major Varsican thrust faults in Belgium with an east-west direction. The system is located directly north of the Midi fault (Delmer A., 2000; Belanger I. et al., 2012).
narrower: Malonne Fault
narrower: Masse Fault
narrower: Chamborgneau Fault
narrower: Tombe Fault
narrower: Ormont Fault
narrower: Saint-Pierre Fault
references: https://data.geoscience.earth/ncl/geoera/ref/8572
references: https://data.geoscience.earth/ncl/geoera/ref/8573
in scheme: Tectonic Boundary Objects in Europe
broader: Ardenne basal detachment

Masse Fault
type: Concept
created: 2021-03-23T14:34:26.991Z
notation: BE-2170
in scheme: Tectonic Boundary Objects in Europe
broader: Haine-Sambre-Meuse fault system

Malonne Fault
type: Concept
created: 2021-03-23T14:34:26.988Z
notation: BE-2169
in scheme: Tectonic Boundary Objects in Europe
broader: Haine-Sambre-Meuse fault system

Saint-Pierre Fault
type: Concept
created: 2021-03-23T14:34:27.002Z
notation: BE-2175
in scheme: Tectonic Boundary Objects in Europe
broader: Haine-Sambre-Meuse fault system

Ormont Fault
type: Concept
created: 2021-03-23T14:34:26.999Z
notation: BE-2174
in scheme: Tectonic Boundary Objects in Europe
broader: Haine-Sambre-Meuse fault system

Tombe Fault
type: Concept
created: 2021-03-23T14:34:26.996Z
notation: BE-2177
definition: The Tombe Fault was first described by Smeysters (1880). The fault dips gently to the south and is connected to other fractures related to the Midi Fault (Cambier G. & Dejonghe L., 2012).
references: https://data.geoscience.earth/ncl/geoera/ref/8574
in scheme: Tectonic Boundary Objects in Europe
broader: Haine-Sambre-Meuse fault system

Chamborgneau Fault
type: Concept
created: 2021-03-23T14:34:26.993Z
notation: BE-2163
notation: BE-2164
in scheme: Tectonic Boundary Objects in Europe
broader: Haine-Sambre-Meuse fault system

Aachen Fault
type: Concept
created: 2021-03-23T14:34:27.013Z
scope note: Discussion is ongoing about the connectivity of the Midi-Eifelian Fault and the Aachen Fault. Either the Aguesse-Asse Fault or the Tunnel Fault connects these two major Variscan thrust faults (Cambier G. & Dejonghe L., 2012).
notation: BE-2161
definition: The Aachen fault is a thrust fault of Variscan age and is the continuation of the Variscan thrust front in the east of Belgium towards Germany, where it is crosscut by the Feldbiss Fault Zone of the Roer Valley Graben (Cambier G. & Dejonghe L., 2012).
references: https://data.geoscience.earth/ncl/geoera/ref/8577
in scheme: Tectonic Boundary Objects in Europe
broader: Ardenne basal detachment

Eupen Fault
type: Concept
created: 2021-03-23T14:34:27.010Z
scope note: The out-of-sequence Eupen Fault is thought to crosscut, merge with and postdate the Theux Fault in the southern part of the Theux Window. Therefore the Eupen Fault forms the south/southwestern boundary of the Theux Window (Cambier G. & Dejonghe L., 2010).
notation: BE-2165
definition: The Eupen Fault is a thrust fault of Variscan age. It branches off the Theux–Tunnel Fault and locally forms the southern boundary between the Vesdre Nappe and the Stavelot Massif (Hance et al., 1999).
references: https://data.geoscience.earth/ncl/geoera/ref/8576
references: https://data.geoscience.earth/ncl/geoera/ref/8570
in scheme: Tectonic Boundary Objects in Europe
broader: Ardenne basal detachment

Midi Fault
type: Concept
created: 2021-03-23T14:34:27.008Z
scope note: The Eifel and Tunnel Faults are assumed to be the eastern continuation of the Midi Fault, yet there is still a lot of uncertainty in this area (see ScopeNote of Aguesses-Asse Fault and Aachen Fault) (Cambier G. & Dejonghe L., 2010).
notation: BE-2171
notation: BE-2172
definition: The Midi Fault is a major thrust which extends laterally from Germany to England of Variscan age. The fault has a low angle dip which flattens at depth and roots into a detachment underlying the thick terrigenous sequence of the Variscan frontal units. The eastern continuation of the Midi Fault from Belgium to Germany is the Aachen Fault (Keppie J.D. 1994).
references: https://data.geoscience.earth/ncl/geoera/ref/8575
references: https://data.geoscience.earth/ncl/geoera/ref/8570
in scheme: Tectonic Boundary Objects in Europe
broader: Ardenne basal detachment

Northern Variscan thrust faults
type: Concept
created: 2021-03-23T14:34:27.005Z
scope note: The known northern limit of the Varsican deformation corresponds to these thrust faults (the Northern Varsican thrust faults). These are therefore used at GIS level for this purpose, rather than being a conceptual SF limit.
in scheme: Tectonic Boundary Objects in Europe
broader: Ardenne basal detachment

Malmedy fault system
type: Concept
created: 2021-03-23T14:34:26.979Z
notation: BE-2157
notation: BE-2158
notation: BE-2159
notation: BE-2160
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Belgium

Bouhouille Fault
type: Concept
created: 2021-03-23T14:34:26.976Z
scope note: The importance of the Bouhouille Fault depends on the relevance of the Aguesses-Asse Fault (see ScopeNote of Aguesse-Asse Fault). If the Asse Fault is interpreted as the eastward continuation of the Aguesse Fault and not as an individual fault, than the Bouhouille Fault plays an important role in explaining the transverse movement between the Aguesses and Asse faults (GeoConnect³d).
notation: BE-2156
definition: The Bouhouille Fault is a NNW-SSE oriented sinistral transverse fault of post-Variscan age. Towards the south it continues as the Evegnée Fault (Cambier G. & Dejonghe L. 2010; Barchy L. & Marion J. (2000).
alternative label: Evegnée Fault
references: https://data.geoscience.earth/ncl/geoera/ref/8570
references: https://data.geoscience.earth/ncl/geoera/ref/8571
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Belgium

Verviers Fault
type: Concept
created: 2021-03-23T14:34:26.973Z
notation: BE-2155
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Belgium

Ostende Fault
type: Concept
created: 2021-03-23T14:34:26.970Z
notation: BE-2154
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Belgium

Xhoris Fault
type: Concept
created: 2021-03-23T14:34:27.032Z
notation: BE-2179
definition: The Xhoris Fault is a thrust-type fracture of Variscan age that affects two major units of Belgian regional geology. The western segment disrupts the Eifelian-Frasnian formations of the eastern border of the Dinant Synclinorium. While the eastern segment displaces the Cambrian-Ordovician rocks of the Stavelot Massif (Cambier G. & Dejonghe L., 2010).
references: https://data.geoscience.earth/ncl/geoera/ref/8570
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Belgium

Mouhy Fault
type: Concept
created: 2021-03-23T14:34:26.966Z
notation: BE-2153
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Belgium

Walhorn Fault
type: Concept
created: 2021-03-23T14:34:27.029Z
notation: BE-2178
definition: The Walhorn Fault is a thrust fracture of Variscan age that comprises of different fault segments, each named differently depending on their geography, from east to west: the Walhorn, Renoupré, Haute-Folie and Pépinster Faults. The fault bounds the northern part of the Goé Unit, a small inner thrust sheet of the Vesdre Nappe (Cambier G. & Dejonghe L., 2010).
alternative label: Pepinster Fault
references: https://data.geoscience.earth/ncl/geoera/ref/8570
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Belgium

Monty Fault
type: Concept
created: 2021-03-23T14:34:26.963Z
notation: BE-2152
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Belgium

Theux Fault
type: Concept
created: 2021-03-23T14:34:27.027Z
scope note: It marks the boundary between the autochthonous area of the Theux Window and the surrounding allochthonous thrust nappe. In the north, the north-dipping Theux Fault is indicated to connect with the south-dipping Tunnel Fault, making the Theux-Tunnel Thrust to be considered as a junction between the Midi Fault in the west and the Aachen Fault in the east (Cambier G. & Dejonghe L., 2010).
notation: BE-2176
definition: The Theux Fault is a circle-shaped thrust fracture (window) which bounds the west, north and east sides of the Theux Window (Cambier G. & Dejonghe L., 2010).
references: https://data.geoscience.earth/ncl/geoera/ref/8570
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Belgium

Landenne Fault
type: Concept
created: 2021-03-23T14:34:27.024Z
notation: BE-2168
definition: The Landenne Fault is a steeply dipping reverse fracture with northward plunge. It marks the boundary between Silurian rocks of the Brabant Massif to the north and Lower Carboniferous rocks of the Namur Synclinorium to the south (Cambier G. & Dejonghe L., 2010).
references: https://data.geoscience.earth/ncl/geoera/ref/8570
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Belgium

Tectonic Boundary in Albania
preferred label: Tektonikat e Shqiperise @sq
definition: Kontakt tektonik midis zonës tektonike Jonike dhe zonës tektonike Sazani @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
top concept of: Tectonic Boundary Objects in Europe
created: 2021-05-03T08:51:31.086Z
type: Concept
notation: AL-0
scope note: All named tectonic boundary objects that are located in Albania, are identified by an ID with the prefix „AL“ listed in the notation.
definition: Fault in Albania, displayed in the HIKE European fault database.
in scheme: Tectonic Boundary Objects in Europe
narrower: Qafe Llogara Fault System
narrower: Leskovik-Poliçan-Liqeni i Banjes Large-Scale Fault System
narrower: Kuc-Ramice Large-Scale Fault System
narrower: Leskovik-Kukur-Elbasan-Milot-Oblik Nappe boundary
narrower: Mali I Vashes-Rohmisht-Strelce-Mali I Firtit-Guri I Bardhe-Rubik-Hajmel Nappe boundary
narrower: Vau I Dejes-Selimaj Nappe boundary
narrower: Shkoder-Selimaj nappe boundary
narrower: Zerqan-Surroj-Morine Nappe boundary

Shkoder-Selimaj nappe boundary
type: Concept
created: 2021-08-19T10:13:09.264Z
creator: schmar
notation: AL-032
preferred label: Shkoder-Selimaj @sq
definition: Tektonike mbihypëse- Kontakt tektonik midis zonës tektonike të Alpeve dhe zonës tektonike Cukali @sq
narrower: Bena-Ura e Shenjte Fault 1
narrower: Bena-Ura e Shenjte Fault 2
narrower: Shllaku Fault
narrower: Vila Fault
narrower: Kiri Fault
narrower: Toplana Fault 1
narrower: Toplana Fault 2
narrower: Shkembi I Merturit Fault
narrower: Liraj-Biga e Shales Fault System
narrower: Curraj I Eperm Fault System 2
narrower: Kastrati-Maja e Surtes Fault System
narrower: Razem Fault System
narrower: Vucim-Cerem-Mali I Brovines Fault System
narrower: Nikolic-Gjergovic Fault System
narrower: Dardha Fault System
narrower: Shkoza Fault System
narrower: Mançurisht Fault System
narrower: Mali I Thate Fault System
narrower: Guri I Topit Fault System
narrower: Fush Bualli Fault System
narrower: Qarishta Fault System
narrower: Rrajc-Sterblev Fault System
narrower: Kostenje-Çerenec Fault System
narrower: Ostreni Fault System
narrower: Bulqize-Selishte Fault System
narrower: Qafshtame-Rubik Fault System
narrower: Ulez Fault System
narrower: Rubik-Rrenja e Zeze Fault System
narrower: Levrushk-Kalimash Fault System
narrower: Qeleza Fault System
narrower: Fushe-Arrezi Fault System
narrower: Kashnjeti Fault System
narrower: Kurbnesh Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Albania

Kostenje-Çerenec Fault System
type: Concept
created: 2021-08-19T10:13:09.697Z
creator: schmar
notation: AL-1836
preferred label: Kostenje-Çerenec @sq
definition: Mbulesore @sq
narrower: Sebisht Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Sebisht Fault
type: Concept
created: 2021-08-19T10:13:09.702Z
creator: schmar
notation: AL-1837
preferred label: Sebisht @sq
definition: Tektonike afrovertikale, tektonike shariazhuese (mbulesore) @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kostenje-Çerenec Fault System

Kurbnesh Fault System
type: Concept
created: 2021-08-19T10:13:09.801Z
creator: schmar
notation: AL-1857
preferred label: Kurbnesh @sq
definition: Mbihypese @sq
narrower: Perlat I Eperm Fault
narrower: Malaj Fault
narrower: Merkurth Fault
narrower: Thirre Fault
narrower: Sakati (Blerim) Fault
narrower: Kulumri (Blerim) Fault
narrower: Mziu Fault
narrower: Karme Fault
narrower: Zogaj Fault
narrower: Cahani Fault
narrower: Kruma Fault
narrower: Arreni Fault
narrower: Kunora e Lures Fault
narrower: Zall Gjoçaj Fault
narrower: Macukulli Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Kruma Fault
type: Concept
created: 2021-08-19T10:13:09.850Z
creator: schmar
notation: AL-1868
preferred label: Kruma @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kurbnesh Fault System

Arreni Fault
type: Concept
created: 2021-08-19T10:13:09.854Z
creator: schmar
notation: AL-1869
preferred label: Arreni @sq
definition: Tektonike afrovertikale, tektonike paralele formacionale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kurbnesh Fault System

Zogaj Fault
type: Concept
created: 2021-08-19T10:13:09.840Z
creator: schmar
notation: AL-1866
preferred label: Zogaj @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kurbnesh Fault System

Cahani Fault
type: Concept
created: 2021-08-19T10:13:09.845Z
creator: schmar
notation: AL-1867
preferred label: Cahani @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kurbnesh Fault System

Macukulli Fault
type: Concept
created: 2021-08-19T10:13:09.868Z
creator: schmar
notation: AL-1872
preferred label: Macukulli @sq
definition: Tektonike afrovertikale, tektonike parakretake me karakter mbihypes @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kurbnesh Fault System

Kunora e Lures Fault
type: Concept
created: 2021-08-19T10:13:09.859Z
creator: schmar
notation: AL-1870
preferred label: Kunora e Lures @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kurbnesh Fault System

Zall Gjoçaj Fault
type: Concept
created: 2021-08-19T10:13:09.863Z
creator: schmar
notation: AL-1871
preferred label: Zall Gjoçaj @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kurbnesh Fault System

Merkurth Fault
type: Concept
created: 2021-08-19T10:13:09.813Z
creator: schmar
notation: AL-1860
preferred label: Merkurth @sq
definition: Tektonike afrovertikale, tektonike strike-slip @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kurbnesh Fault System

Thirre Fault
type: Concept
created: 2021-08-19T10:13:09.817Z
creator: schmar
notation: AL-1861
preferred label: Thirre @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kurbnesh Fault System

Perlat I Eperm Fault
type: Concept
created: 2021-08-19T10:13:09.805Z
creator: schmar
notation: AL-1858
preferred label: Perlat I Eperm @sq
definition: Tektonike afrovertikale, tektonike parakretake me karakter mbihypes @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kurbnesh Fault System

Malaj Fault
type: Concept
created: 2021-08-19T10:13:09.809Z
creator: schmar
notation: AL-1859
preferred label: Malaj @sq
definition: Mbihypese @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kurbnesh Fault System

Mziu Fault
type: Concept
created: 2021-08-19T10:13:09.831Z
creator: schmar
notation: AL-1864
preferred label: Mziu @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kurbnesh Fault System

Karme Fault
type: Concept
created: 2021-08-19T10:13:09.835Z
creator: schmar
notation: AL-1865
preferred label: Karme @sq
definition: Tektonike afrovertikale, tektonike paralele formacionale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kurbnesh Fault System

Sakati (Blerim) Fault
type: Concept
created: 2021-08-19T10:13:09.822Z
creator: schmar
notation: AL-1862
preferred label: Sakati (Blerim) @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kurbnesh Fault System

Kulumri (Blerim) Fault
type: Concept
created: 2021-08-19T10:13:09.827Z
creator: schmar
notation: AL-1863
preferred label: Kulumri (Blerim) @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kurbnesh Fault System

Kashnjeti Fault System
type: Concept
created: 2021-08-19T10:13:09.791Z
creator: schmar
notation: AL-1855
preferred label: Kashnjeti @sq
definition: Tektonike afrovertikale @sq
narrower: Bukmire Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Bukmire Fault
type: Concept
created: 2021-08-19T10:13:09.796Z
creator: schmar
notation: AL-1856
preferred label: Bukmire @sq
definition: Tektonike afrovertikale , tektonike parakretake me karakter mbihypes @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kashnjeti Fault System

Vucim-Cerem-Mali I Brovines Fault System
type: Concept
created: 2021-08-19T10:13:09.514Z
creator: schmar
notation: AL-100
preferred label: Vucim-Cerem-Mali I Brovines @sq
definition: Tektonike shariazhuese- Kontakt tektonik midis zones tektonike Gashi dhe zones tektonike Alpine @sq
narrower: Mali I Marlules Fault
narrower: Seferece Fault
narrower: Vrepcke Fault
narrower: Radanj Fault
narrower: Germenj Fault
narrower: Borova Fault
narrower: Gjonçi Fault
narrower: Vithkuq Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Seferece Fault
type: Concept
created: 2021-08-19T10:13:09.523Z
creator: schmar
notation: AL-102
preferred label: Seferece @sq
definition: Tektonike afrovertikale @sq
narrower: Sulbica Subfault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Vucim-Cerem-Mali I Brovines Fault System

Sulbica Subfault
type: Concept
created: 2021-08-19T10:13:09.528Z
creator: schmar
notation: AL-103
preferred label: Sulbica @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Seferece Fault

Vrepcke Fault
type: Concept
created: 2021-08-19T10:13:09.532Z
creator: schmar
notation: AL-181
preferred label: Vrepcke @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Vucim-Cerem-Mali I Brovines Fault System

Borova Fault
type: Concept
created: 2021-08-19T10:13:09.548Z
creator: schmar
notation: AL-184
preferred label: Borova @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Vucim-Cerem-Mali I Brovines Fault System

Radanj Fault
type: Concept
created: 2021-08-19T10:13:09.536Z
creator: schmar
notation: AL-182
preferred label: Radanj @sq
definition: Tektonike afrovertikale formacionale, tektonike shariazhuese @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Vucim-Cerem-Mali I Brovines Fault System

Germenj Fault
type: Concept
created: 2021-08-19T10:13:09.540Z
creator: schmar
notation: AL-183
preferred label: Germenj @sq
definition: Tektonike mbulesore @sq
narrower: Germenj Subfault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Vucim-Cerem-Mali I Brovines Fault System

Germenj Subfault
type: Concept
created: 2021-08-19T10:13:09.544Z
creator: schmar
notation: AL-18311
preferred label: Germenj (1) @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Germenj Fault

Mali I Marlules Fault
type: Concept
created: 2021-08-19T10:13:09.518Z
creator: schmar
notation: AL-101
preferred label: Mali I Marlules @sq
definition: Tektonike afrovertikale formacionale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Vucim-Cerem-Mali I Brovines Fault System

Gjonçi Fault
type: Concept
created: 2021-08-19T10:13:09.552Z
creator: schmar
notation: AL-185
preferred label: Gjonçi @sq
definition: Tektonike afrovertikale formacionale, tektonike parakretake @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Vucim-Cerem-Mali I Brovines Fault System

Vithkuq Fault
type: Concept
created: 2021-08-19T10:13:09.556Z
creator: schmar
notation: AL-186
preferred label: Vithkuq @sq
definition: Tektonike afrovertikale, tektonike me karakter mbulesor @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Vucim-Cerem-Mali I Brovines Fault System

Shkoza Fault System
type: Concept
created: 2021-08-19T10:13:09.604Z
creator: schmar
notation: AL-1816
preferred label: Shkoza @sq
definition: Tektonike afrovertikale @sq
narrower: Kloça Fault
narrower: Pirgu Fault
narrower: Kapshtica Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Kapshtica Fault
type: Concept
created: 2021-08-19T10:13:09.617Z
creator: schmar
notation: AL-1819
preferred label: Kapshtica @sq
definition: Tektonike afrovertikale, tektonike paralele @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoza Fault System

Pirgu Fault
type: Concept
created: 2021-08-19T10:13:09.612Z
creator: schmar
notation: AL-1818
preferred label: Pirgu @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoza Fault System

Kloça Fault
type: Concept
created: 2021-08-19T10:13:09.608Z
creator: schmar
notation: AL-1817
preferred label: Kloça @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoza Fault System

Ostreni Fault System
type: Concept
created: 2021-08-19T10:13:09.707Z
creator: schmar
notation: AL-1838
preferred label: Ostreni @sq
definition: Mbulesore, tektonike paralele dhe nderprerese @sq
narrower: Trebisht Fault
narrower: Mali me Gropa Fault
narrower: Guri I Bardhe Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Trebisht Fault
type: Concept
created: 2021-08-19T10:13:09.711Z
creator: schmar
notation: AL-1839
preferred label: Trebisht @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Ostreni Fault System

Mali me Gropa Fault
type: Concept
created: 2021-08-19T10:13:09.716Z
creator: schmar
notation: AL-1840
preferred label: Mali me Gropa @sq
definition: Tektonike afrovertikale, Bllok gravitativ @sq
narrower: Burimas Subfault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Ostreni Fault System

Burimas Subfault
type: Concept
created: 2021-08-19T10:13:09.720Z
creator: schmar
notation: AL-1841
preferred label: Burimas @sq
definition: Bllok gravitativ @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Mali me Gropa Fault

Guri I Bardhe Fault
type: Concept
created: 2021-08-19T10:13:09.724Z
creator: schmar
notation: AL-1842
preferred label: Guri I Bardhe @sq
definition: Tektonike afrovertikale, tektonike parakretake me karakter mbihypes @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Ostreni Fault System

Bena-Ura e Shenjte Fault 1
type: Concept
created: 2021-08-19T10:13:09.268Z
creator: schmar
notation: AL-033
preferred label: Bena-Ura e Shenjte @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Bena-Ura e Shenjte Fault 2
type: Concept
created: 2021-08-19T10:13:09.272Z
creator: schmar
notation: AL-0331
preferred label: Bena-Ura e Shenjte @sq
definition: Tektonike afrovertikale @sq
narrower: Ukbibaj Subfault
narrower: Mazreku Subfault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Ukbibaj Subfault
type: Concept
created: 2021-08-19T10:13:09.277Z
creator: schmar
notation: AL-034
preferred label: Ukbibaj @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Bena-Ura e Shenjte Fault 2

Mazreku Subfault
type: Concept
created: 2021-08-19T10:13:09.281Z
creator: schmar
notation: AL-035
preferred label: Mazreku @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Bena-Ura e Shenjte Fault 2

Curraj I Eperm Fault System 2
type: Concept
created: 2021-08-19T10:13:09.364Z
creator: schmar
notation: AL-0111
preferred label: Curraj I Eperm (2) @sq
definition: Mbihypese @sq
narrower: Raba e Ducajve Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Raba e Ducajve Fault
type: Concept
created: 2021-08-19T10:13:09.368Z
creator: schmar
notation: AL-0112
preferred label: Raba e Ducajve @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Curraj I Eperm Fault System 2

Shllaku Fault
type: Concept
created: 2021-08-19T10:13:09.285Z
creator: schmar
notation: AL-036
preferred label: Shllaku @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Mali I Thate Fault System
type: Concept
created: 2021-08-19T10:13:09.626Z
creator: schmar
notation: AL-1821
preferred label: Mali I Thate @sq
definition: Tektonike afrovertikale @sq
narrower: Velçani I Gores Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Velçani I Gores Fault
type: Concept
created: 2021-08-19T10:13:09.631Z
creator: schmar
notation: AL-1822
preferred label: Velçani I Gores @sq
definition: Tektonike afrovertikale, tektonike parakretake me karakter mbihypes @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Mali I Thate Fault System

Bulqize-Selishte Fault System
type: Concept
created: 2021-08-19T10:13:09.729Z
creator: schmar
notation: AL-1843
preferred label: Bulqize-Selishte @sq
definition: Mbihypese, tektonike parakretake me karakter mbihypes @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Vila Fault
type: Concept
created: 2021-08-19T10:13:09.289Z
creator: schmar
notation: AL-037
preferred label: Vila @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Razem Fault System
type: Concept
created: 2021-08-19T10:13:09.380Z
creator: schmar
notation: AL-0115
preferred label: Razem @sq
definition: Tektonike afrovertikale @sq
narrower: Repshaj Fault
narrower: Boge Fault
narrower: Mali I Bukoviqit Fault
narrower: Nikshi Fault
narrower: Mali I Radomires Fault
narrower: Mali I Shenikut Fault
narrower: Mali I Vajushes Fault
narrower: Lepusha Fault
narrower: Mali I Golishtit Fault 1
narrower: Mali I Golishtit Fault 2
narrower: Mali I Kashticit Fault
narrower: Mali I Zarzit Fault
narrower: Mali I Jezerces Fault 2
narrower: Mali I Cet Harushes Fault
narrower: Dragobia Fault
narrower: Brodoshnica Fault
narrower: Mali I Brodoshnices Fault
narrower: Mali I Shkelzenit Fault
narrower: Mali I Gjarprit Fault
narrower: Qafa e Barit Fault 1
narrower: Qafa e Barit Fault 2
narrower: Vucim Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Lepusha Fault
type: Concept
created: 2021-08-19T10:13:09.429Z
creator: schmar
notation: AL-0124
preferred label: Lepusha @sq
definition: Tektonike afrovertikale @sq
narrower: Mali I Grebenit Subfault
narrower: Vermosh Subfault
narrower: Gropat e Selces Subfault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Razem Fault System

Vermosh Subfault
type: Concept
created: 2021-08-19T10:13:09.439Z
creator: schmar
notation: AL-0126
preferred label: Vermosh @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Lepusha Fault

Mali I Grebenit Subfault
type: Concept
created: 2021-08-19T10:13:09.434Z
creator: schmar
notation: AL-0125
preferred label: Mali I Grebenit @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Lepusha Fault

Gropat e Selces Subfault
type: Concept
created: 2021-08-19T10:13:09.444Z
creator: schmar
notation: AL-0127
preferred label: Gropat e Selces @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Lepusha Fault

Mali I Cet Harushes Fault
type: Concept
created: 2021-08-19T10:13:09.477Z
creator: schmar
notation: AL-0135
preferred label: Mali I Cet Harushes @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Razem Fault System

Dragobia Fault
type: Concept
created: 2021-08-19T10:13:09.480Z
creator: schmar
notation: AL-0136
preferred label: Dragobia @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Razem Fault System

Mali I Bukoviqit Fault
type: Concept
created: 2021-08-19T10:13:09.397Z
creator: schmar
notation: AL-0118
preferred label: Mali I Bukoviqit @sq
definition: Tektonike afrovertikale @sq
narrower: Tamare Subfault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Razem Fault System

Tamare Subfault
type: Concept
created: 2021-08-19T10:13:09.402Z
creator: schmar
notation: AL-0119
preferred label: Tamare @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Mali I Bukoviqit Fault

Mali I Golishtit Fault 2
type: Concept
created: 2021-08-19T10:13:09.453Z
creator: schmar
notation: AL-0129
preferred label: Mali I Golishtit (2) @sq
definition: Mbihypese, tektonikeme karakter mbihypese @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Razem Fault System

Mali I Gjarprit Fault
type: Concept
created: 2021-08-19T10:13:09.497Z
creator: schmar
notation: AL-0140
preferred label: Mali I Gjarprit @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Razem Fault System

Mali I Kashticit Fault
type: Concept
created: 2021-08-19T10:13:09.457Z
creator: schmar
notation: AL-0130
preferred label: Mali I Kashticit @sq
definition: Mbihypese, tektonikeme karakter mbihypes @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Razem Fault System

Qafa e Barit Fault 1
type: Concept
created: 2021-08-19T10:13:09.501Z
creator: schmar
notation: AL-0141
preferred label: Qafa e Barit @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Razem Fault System

Repshaj Fault
type: Concept
created: 2021-08-19T10:13:09.386Z
creator: schmar
notation: AL-0116
preferred label: Repshaj @sq
definition: Tektonike afrovertikale, tektonike qe nderpret formacionin kryq @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Razem Fault System

Mali I Brodoshnices Fault
type: Concept
created: 2021-08-19T10:13:09.489Z
creator: schmar
notation: AL-0138
preferred label: Mali I Brodoshnices @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Razem Fault System

Boge Fault
type: Concept
created: 2021-08-19T10:13:09.391Z
creator: schmar
notation: AL-0117
preferred label: Boge @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Razem Fault System

Mali I Golishtit Fault 1
type: Concept
created: 2021-08-19T10:13:09.448Z
creator: schmar
notation: AL-0128
preferred label: Mali I Golishtit (1) @sq
definition: Tektonike afrovertikale, tektonikeme karakter mbihypese @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Razem Fault System

Mali I Shkelzenit Fault
type: Concept
created: 2021-08-19T10:13:09.493Z
creator: schmar
notation: AL-0139
preferred label: Mali I Shkelzenit @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Razem Fault System

Mali I Shenikut Fault
type: Concept
created: 2021-08-19T10:13:09.419Z
creator: schmar
notation: AL-0122
preferred label: Mali I Shenikut @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Razem Fault System

Mali I Vajushes Fault
type: Concept
created: 2021-08-19T10:13:09.424Z
creator: schmar
notation: AL-0123
preferred label: Mali I Vajushes @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Razem Fault System

Mali I Jezerces Fault 2
type: Concept
created: 2021-08-19T10:13:09.473Z
creator: schmar
notation: AL-0134
preferred label: Mali I Jezerces (2) @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Razem Fault System

Nikshi Fault
type: Concept
created: 2021-08-19T10:13:09.408Z
creator: schmar
notation: AL-0120
preferred label: Nikshi @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Razem Fault System

Mali I Zarzit Fault
type: Concept
created: 2021-08-19T10:13:09.461Z
creator: schmar
notation: AL-0131
preferred label: Mali I Zarzit @sq
definition: Mbihypese @sq
narrower: Qafa e Kloshit-Rogam Subfault
narrower: Mali I Jezerces Fault 1 Subfault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Razem Fault System

Mali I Jezerces Fault 1 Subfault
type: Concept
created: 2021-08-19T10:13:09.469Z
creator: schmar
notation: AL-0133
preferred label: Mali I Jezerces (1) @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Mali I Zarzit Fault

Qafa e Kloshit-Rogam Subfault
type: Concept
created: 2021-08-19T10:13:09.465Z
creator: schmar
notation: AL-0132
preferred label: Qafa e Kloshit-Rogam @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Mali I Zarzit Fault

Qafa e Barit Fault 2
type: Concept
created: 2021-08-19T10:13:09.505Z
creator: schmar
notation: AL-01412
preferred label: Qafa e Barit @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Razem Fault System

Mali I Radomires Fault
type: Concept
created: 2021-08-19T10:13:09.413Z
creator: schmar
notation: AL-0121
preferred label: Mali I Radomires @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Razem Fault System

Vucim Fault
type: Concept
created: 2021-08-19T10:13:09.510Z
creator: schmar
notation: AL-0142
preferred label: Vucim @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Razem Fault System

Brodoshnica Fault
type: Concept
created: 2021-08-19T10:13:09.484Z
creator: schmar
notation: AL-0137
preferred label: Brodoshnica @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Razem Fault System

Qafshtame-Rubik Fault System
type: Concept
created: 2021-08-19T10:13:09.735Z
creator: schmar
notation: AL-1844
preferred label: Qafshtame-Rubik @sq
definition: Mbihypese @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Kastrati-Maja e Surtes Fault System
type: Concept
created: 2021-08-19T10:13:09.372Z
creator: schmar
notation: AL-0113
preferred label: Kastrati-Maja e Surtes @sq
definition: Tektonike afrovertikale @sq
narrower: Hoti Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Hoti Fault
type: Concept
created: 2021-08-19T10:13:09.376Z
creator: schmar
notation: AL-0114
preferred label: Hoti @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kastrati-Maja e Surtes Fault System

Mançurisht Fault System
type: Concept
created: 2021-08-19T10:13:09.621Z
creator: schmar
notation: AL-1820
preferred label: Mançurisht @sq
definition: Tektonike afrovertikale, tektonike paralele @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Toplana Fault 2
type: Concept
created: 2021-08-19T10:13:09.302Z
creator: schmar
notation: AL-0310
preferred label: Toplana (2) @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Fush Bualli Fault System
type: Concept
created: 2021-08-19T10:13:09.652Z
creator: schmar
notation: AL-1826
preferred label: Fush Bualli @sq
definition: Tektonike afrovertikale, tektonike paralele @sq
narrower: Spathar Fault
narrower: Gurshpat Fault
narrower: Berzeshta Fault
narrower: Xhyra Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Berzeshta Fault
type: Concept
created: 2021-08-19T10:13:09.666Z
creator: schmar
notation: AL-1829
preferred label: Berzeshta @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Fush Bualli Fault System

Xhyra Fault
type: Concept
created: 2021-08-19T10:13:09.670Z
creator: schmar
notation: AL-1830
preferred label: Xhyra @sq
definition: Tektonike afrovertikale, tektonike parakretake me karakter mbihypes @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Fush Bualli Fault System

Spathar Fault
type: Concept
created: 2021-08-19T10:13:09.656Z
creator: schmar
notation: AL-1827
preferred label: Spathar @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Fush Bualli Fault System

Gurshpat Fault
type: Concept
created: 2021-08-19T10:13:09.661Z
creator: schmar
notation: AL-1828
preferred label: Gurshpat @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Fush Bualli Fault System

Kiri Fault
type: Concept
created: 2021-08-19T10:13:09.294Z
creator: schmar
notation: AL-038
preferred label: Kiri @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Guri I Topit Fault System
type: Concept
created: 2021-08-19T10:13:09.636Z
creator: schmar
notation: AL-1823
preferred label: Guri I Topit @sq
definition: Mbihypese @sq
narrower: Verdova Fault
narrower: Stravaj Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Stravaj Fault
type: Concept
created: 2021-08-19T10:13:09.647Z
creator: schmar
notation: AL-1825
preferred label: Stravaj @sq
definition: Tektonike afrovertikale, tektonike paralele formacionale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Guri I Topit Fault System

Verdova Fault
type: Concept
created: 2021-08-19T10:13:09.641Z
creator: schmar
notation: AL-1824
preferred label: Verdova @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Guri I Topit Fault System

Ulez Fault System
type: Concept
created: 2021-08-19T10:13:09.741Z
creator: schmar
notation: AL-1845
preferred label: Ulez @sq
definition: Tektonike afrovertikale, tektonike parakretake me karakter mbihypes @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Toplana Fault 1
type: Concept
created: 2021-08-19T10:13:09.298Z
creator: schmar
notation: AL-039
preferred label: Toplana (1) @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Rubik-Rrenja e Zeze Fault System
type: Concept
created: 2021-08-19T10:13:09.745Z
creator: schmar
notation: AL-1846
preferred label: Rubik-Rrenja e Zeze @sq
definition: Mbihypese, tektonike parakretake me karakter mbihypes @sq
narrower: Iballe Fault
narrower: Berishe e Vogel-Bugjon Fault
narrower: Geraj Fault
narrower: Dushaj Fault
narrower: Kurora e Dardhes Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Dushaj Fault
type: Concept
created: 2021-08-19T10:13:09.763Z
creator: schmar
notation: AL-1849
preferred label: Dushaj @sq
definition: Mbihypese, tektonike parakretake formacionale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Rubik-Rrenja e Zeze Fault System

Kurora e Dardhes Fault
type: Concept
created: 2021-08-19T10:13:09.767Z
creator: schmar
notation: AL-1850
preferred label: Kurora e Dardhes @sq
definition: Mbihypese @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Rubik-Rrenja e Zeze Fault System

Geraj Fault
type: Concept
created: 2021-08-19T10:13:09.758Z
creator: schmar
notation: Al-G.M48_1
preferred label: Geraj @sq
definition: tektonike parakretake me karakter mbihypes @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Rubik-Rrenja e Zeze Fault System

Iballe Fault
type: Concept
created: 2021-08-19T10:13:09.750Z
creator: schmar
notation: AL-1847
preferred label: Iballe @sq
definition: Mbihypese @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Rubik-Rrenja e Zeze Fault System

Berishe e Vogel-Bugjon Fault
type: Concept
created: 2021-08-19T10:13:09.754Z
creator: schmar
notation: AL-1848
preferred label: Berishe e Vogel-Bugjon @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Rubik-Rrenja e Zeze Fault System

Nikolic-Gjergovic Fault System
type: Concept
created: 2021-08-19T10:13:09.565Z
creator: schmar
notation: AL-187
preferred label: Nikolic-Gjergovic @sq
definition: Mbihypese, tektonike me karakter srtike-slip @sq
narrower: Arrza Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Arrza Fault
type: Concept
created: 2021-08-19T10:13:09.570Z
creator: schmar
notation: AL-188
preferred label: Arrza @sq
definition: Tektonike afrovertikale, tektonika paralele @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Nikolic-Gjergovic Fault System

Liraj-Biga e Shales Fault System
type: Concept
created: 2021-08-19T10:13:09.319Z
creator: schmar
notation: AL-011
preferred label: Liraj-Biga e Shales @sq
definition: Tektonike afrovertikale @sq
narrower: Mali I Kurriles Fault 1
narrower: Mali I Kurriles Fault 2
narrower: Mali I Mardomit Fault
narrower: Ducaj Fault
narrower: Vajushi Fault 1
narrower: Vajushi Fault 2
narrower: Troshani Fault
narrower: Curraj I Eperm Fault 1
narrower: Mali I Hekurave Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Mali I Hekurave Fault
type: Concept
created: 2021-08-19T10:13:09.360Z
creator: schmar
notation: AL-0110
preferred label: Mali I Hekurave @sq
definition: Tektonike afrovertikale, tektonike me karakter mbihypës @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Liraj-Biga e Shales Fault System

Troshani Fault
type: Concept
created: 2021-08-19T10:13:09.352Z
creator: schmar
notation: AL-018
preferred label: Troshani @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Liraj-Biga e Shales Fault System

Curraj I Eperm Fault 1
type: Concept
created: 2021-08-19T10:13:09.356Z
creator: schmar
notation: AL-019
preferred label: Curraj I Eperm (1) @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Liraj-Biga e Shales Fault System

Mali I Mardomit Fault
type: Concept
created: 2021-08-19T10:13:09.332Z
creator: schmar
notation: AL-013
preferred label: Mali I Mardomit @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Liraj-Biga e Shales Fault System

Ducaj Fault
type: Concept
created: 2021-08-19T10:13:09.336Z
creator: schmar
notation: AL-014
preferred label: Ducaj @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Liraj-Biga e Shales Fault System

Mali I Kurriles Fault 1
type: Concept
created: 2021-08-19T10:13:09.323Z
creator: schmar
notation: AL-012
preferred label: Mali I Kurriles (1) @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Liraj-Biga e Shales Fault System

Mali I Kurriles Fault 2
type: Concept
created: 2021-08-19T10:13:09.328Z
creator: schmar
notation: AL-01211
preferred label: Mali I Kurriles (2) @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Liraj-Biga e Shales Fault System

Vajushi Fault 1
type: Concept
created: 2021-08-19T10:13:09.340Z
creator: schmar
notation: AL-016
preferred label: Vajushi (1) @sq
definition: Tektonike afrovertikale @sq
narrower: Perroi I Rrjollit Subfault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Liraj-Biga e Shales Fault System

Perroi I Rrjollit Subfault
type: Concept
created: 2021-08-19T10:13:09.344Z
creator: schmar
notation: AL-017
preferred label: Perroi I Rrjollit @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Vajushi Fault 1

Vajushi Fault 2
type: Concept
created: 2021-08-19T10:13:09.348Z
creator: schmar
notation: AL-0171
preferred label: Vajushi (2) @sq
definition: Tektonike afrovertikale, tektonike paralele @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Liraj-Biga e Shales Fault System

Shkembi I Merturit Fault
type: Concept
created: 2021-08-19T10:13:09.307Z
creator: schmar
notation: AL-0311
preferred label: Shkembi I Merturit @sq
definition: Tektonike afrovertikale @sq
narrower: Brozhta Subfault
narrower: Palaj Subfault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Palaj Subfault
type: Concept
created: 2021-08-19T10:13:09.315Z
creator: schmar
notation: AL-0313
preferred label: Palaj @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkembi I Merturit Fault

Brozhta Subfault
type: Concept
created: 2021-08-19T10:13:09.311Z
creator: schmar
notation: AL-0312
preferred label: Brozhta @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkembi I Merturit Fault

Rrajc-Sterblev Fault System
type: Concept
created: 2021-08-19T10:13:09.680Z
creator: schmar
notation: AL-1832
preferred label: Rrajc-Sterblev @sq
definition: Tektonike afrovertikale @sq
narrower: Miraka Fault
narrower: Kuturman Fault
narrower: Gurakuq Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Miraka Fault
type: Concept
created: 2021-08-19T10:13:09.684Z
creator: schmar
notation: AL-1833
preferred label: Miraka @sq
definition: Tektonike afrovertikale, tektonike parakretake me karakter mbihypes @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Rrajc-Sterblev Fault System

Kuturman Fault
type: Concept
created: 2021-08-19T10:13:09.689Z
creator: schmar
notation: AL-1834
preferred label: Kuturman @sq
definition: Mbihypese, tektonike shariazhuese @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Rrajc-Sterblev Fault System

Gurakuq Fault
type: Concept
created: 2021-08-19T10:13:09.693Z
creator: schmar
notation: AL-1835
preferred label: Gurakuq @sq
definition: Mbulesore, tektonike shariazhuese (mbulesore) @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Rrajc-Sterblev Fault System

Fushe-Arrezi Fault System
type: Concept
created: 2021-08-19T10:13:09.787Z
creator: schmar
notation: AL-1854
preferred label: Fushe-Arrezi @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Levrushk-Kalimash Fault System
type: Concept
created: 2021-08-19T10:13:09.773Z
creator: schmar
notation: AL-1851
preferred label: Levrushk-Kalimash @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Dardha Fault System
type: Concept
created: 2021-08-19T10:13:09.574Z
creator: schmar
notation: AL-189
preferred label: Dardha @sq
definition: Tektonike afrovertikale @sq
narrower: Voskopoja Fault
narrower: Lavdari I Korçes Fault
narrower: Gjylasi-Qerecke Fault
narrower: Kurshove Fault
narrower: Lozhani Fault
narrower: Limanit Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Voskopoja Fault
type: Concept
created: 2021-08-19T10:13:09.578Z
creator: schmar
notation: AL-1810
preferred label: Voskopoja @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Dardha Fault System

Lavdari I Korçes Fault
type: Concept
created: 2021-08-19T10:13:09.583Z
creator: schmar
notation: AL-1811
preferred label: Lavdari I Korçes @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Dardha Fault System

Lozhani Fault
type: Concept
created: 2021-08-19T10:13:09.596Z
creator: schmar
notation: AL-1814
preferred label: Lozhani @sq
definition: Tektonike afrovertikale formacionale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Dardha Fault System

Limanit Fault
type: Concept
created: 2021-08-19T10:13:09.600Z
creator: schmar
notation: AL-1815
preferred label: Limanit @sq
definition: Tektonike afrovertikale formacionale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Dardha Fault System

Gjylasi-Qerecke Fault
type: Concept
created: 2021-08-19T10:13:09.587Z
creator: schmar
notation: AL-1812
preferred label: Gjylasi-Qerecke @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Dardha Fault System

Kurshove Fault
type: Concept
created: 2021-08-19T10:13:09.591Z
creator: schmar
notation: AL-1813
preferred label: Kurshove @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Dardha Fault System

Qarishta Fault System
type: Concept
created: 2021-08-19T10:13:09.675Z
creator: schmar
notation: AL-1831
preferred label: Qarishta @sq
definition: Mbihypese @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Qeleza Fault System
type: Concept
created: 2021-08-19T10:13:09.778Z
creator: schmar
notation: AL-1852
preferred label: Qeleza @sq
definition: Tektonike afrovertikale formacionale @sq
narrower: Kushneni Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Shkoder-Selimaj nappe boundary

Kushneni Fault
type: Concept
created: 2021-08-19T10:13:09.782Z
creator: schmar
notation: AL-1853
preferred label: Kushneni @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Qeleza Fault System

Leskovik-Kukur-Elbasan-Milot-Oblik Nappe boundary
type: Concept
created: 2021-08-19T10:13:09.027Z
creator: schmar
notation: AL-151
preferred label: Leskovik-Kukur-Elbasan-Milot-Oblik @sq
definition: Tektonike mbulesore (shariazhuese)- Kontakt tektonik midis zonës tektonike Kruja dhe zonës tektonike Krasta @sq
narrower: Cercka Fault
narrower: Postenan Fault
narrower: Leshnja Fault
narrower: Brashtan Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Albania

Cercka Fault
type: Concept
created: 2021-08-19T10:13:09.032Z
creator: schmar
notation: AL-152
preferred label: Cercka @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Leskovik-Kukur-Elbasan-Milot-Oblik Nappe boundary

Postenan Fault
type: Concept
created: 2021-08-19T10:13:09.035Z
creator: schmar
notation: AL-153
preferred label: Postenan @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Leskovik-Kukur-Elbasan-Milot-Oblik Nappe boundary

Leshnja Fault
type: Concept
created: 2021-08-19T10:13:09.039Z
creator: schmar
notation: AL-154
preferred label: Leshnja @sq
definition: Tektonike afrovertikale, tektonike paralele dhe terthore @sq
narrower: Ulove Fault
narrower: Gurezeza Subfault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Leskovik-Kukur-Elbasan-Milot-Oblik Nappe boundary

Ulove Fault
type: Concept
created: 2021-08-19T10:13:09.044Z
creator: schmar
notation: AL-155
preferred label: Ulove @sq
definition: Tektonike afrovertikale @sq
narrower: Ulove Subfault 1
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Leshnja Fault

Ulove Subfault 1
type: Concept
created: 2021-08-19T10:13:09.048Z
creator: schmar
notation: AL-1551
preferred label: Ulove (1) @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Ulove Fault

Gurezeza Subfault
type: Concept
created: 2021-08-19T10:13:09.052Z
creator: schmar
notation: AL-156
preferred label: Gurezeza @sq
definition: Bllok gravitativ @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Leshnja Fault

Brashtan Fault System
type: Concept
created: 2021-08-19T10:13:09.056Z
creator: schmar
notation: AL-157
preferred label: Brashtan @sq
definition: Tektonike afrovertikale @sq
narrower: Nezhan Fault
narrower: Selita e Malit Fault
narrower: Mener I Siperm Fault
narrower: Sanxhak Fault
narrower: Mali I Kakariqit Fault
narrower: Mali I Rencit Fault 1
narrower: Mali I Rencit Fault 2
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Leskovik-Kukur-Elbasan-Milot-Oblik Nappe boundary

Selita e Malit Fault
type: Concept
created: 2021-08-19T10:13:09.074Z
creator: schmar
notation: AL-1511
preferred label: Selita e Malit @sq
definition: Tektonike afrovertikale, tektonike paralele @sq
narrower: Zall-Bastar Subfault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Brashtan Fault System

Zall-Bastar Subfault
type: Concept
created: 2021-08-19T10:13:09.078Z
creator: schmar
notation: AL-1512
preferred label: Zall-Bastar @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Selita e Malit Fault

Mali I Kakariqit Fault
type: Concept
created: 2021-08-19T10:13:09.090Z
creator: schmar
notation: AL-1515
preferred label: Mali I Kakariqit @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Brashtan Fault System

Mali I Rencit Fault 1
type: Concept
created: 2021-08-19T10:13:09.095Z
creator: schmar
notation: AL-1516
preferred label: Mali I Rencit (1) @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Brashtan Fault System

Mener I Siperm Fault
type: Concept
created: 2021-08-19T10:13:09.082Z
creator: schmar
notation: AL-1513
preferred label: Mener I Siperm @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Brashtan Fault System

Sanxhak Fault
type: Concept
created: 2021-08-19T10:13:09.086Z
creator: schmar
notation: AL-1514
preferred label: Sanxhak @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Brashtan Fault System

Nezhan Fault
type: Concept
created: 2021-08-19T10:13:09.061Z
creator: schmar
notation: AL-158
preferred label: Nezhan @sq
definition: Tektonike afrovertikale, tektonike mbulesore @sq
narrower: Trepsenisht Subfault
narrower: Letan Subfault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Brashtan Fault System

Letan Subfault
type: Concept
created: 2021-08-19T10:13:09.070Z
creator: schmar
notation: AL-1510
preferred label: Letan @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Nezhan Fault

Trepsenisht Subfault
type: Concept
created: 2021-08-19T10:13:09.065Z
creator: schmar
notation: AL-159
preferred label: Trepsenisht @sq
definition: Bllok gravitativ, tektonike paralele @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Nezhan Fault

Mali I Rencit Fault 2
type: Concept
created: 2021-08-19T10:13:09.099Z
creator: schmar
notation: AL-1517
preferred label: Mali I Rencit (2) @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Brashtan Fault System

Leskovik-Poliçan-Liqeni i Banjes Large-Scale Fault System
type: Concept
created: 2021-08-19T10:13:08.779Z
creator: schmar
notation: AL-141
preferred label: Leskovik-Poliçan-Liqeni i Banjes @sq
definition: Tektonike afrovertikale @sq
narrower: Çarçove-Bodar-Poliçan-Turje Fault System
narrower: Dumre Fault System
narrower: Toske-Mbjeshtove Fault System
narrower: Velçan Fault System
narrower: Krahesi i Siperm Fault System
narrower: Zhulat-Picari Fault System
narrower: Caush-Janjar Fault System
narrower: Borsh-Bolene Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Albania

Dumre Fault System
type: Concept
created: 2021-08-19T10:13:08.819Z
creator: schmar
notation: AL-149
preferred label: Dumre @sq
definition: Mbihypje @sq
narrower: Xhafaj-Mbolan Fault
narrower: Xhafaj-Mbolan Fault 1
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Leskovik-Poliçan-Liqeni i Banjes Large-Scale Fault System

Xhafaj-Mbolan Fault
type: Concept
created: 2021-08-19T10:13:08.823Z
creator: schmar
notation: AL-1410
preferred label: Xhafaj-Mbolan @sq
definition: Mbihypje @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Dumre Fault System

Xhafaj-Mbolan Fault 1
type: Concept
created: 2021-08-19T10:13:08.827Z
creator: schmar
notation: AL-1411
preferred label: Xhafaj-Mbolan (1) @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Dumre Fault System

Zhulat-Picari Fault System
type: Concept
created: 2021-08-19T10:13:08.901Z
creator: schmar
notation: AL-1428
preferred label: Zhulat-Picari @sq
definition: Mbihypje @sq
narrower: Çepune-Senice Fault
narrower: Vergo-Rusan Fault
narrower: Delvina Fault
narrower: Krongj-Leshnice Fault
narrower: Janicat-Qafe Leshnice Fault
narrower: Zminec Fault
narrower: Cerkovice Fault
narrower: Dermish-Karroq Fault
narrower: Kodra Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Leskovik-Poliçan-Liqeni i Banjes Large-Scale Fault System

Vergo-Rusan Fault
type: Concept
created: 2021-08-19T10:13:08.910Z
creator: schmar
notation: AL-1430
preferred label: Vergo-Rusan @sq
definition: Tektonike Diapirike @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Zhulat-Picari Fault System

Delvina Fault
type: Concept
created: 2021-08-19T10:13:08.914Z
creator: schmar
notation: AL-1431
preferred label: Delvina @sq
definition: Mbihypje @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Zhulat-Picari Fault System

Çepune-Senice Fault
type: Concept
created: 2021-08-19T10:13:08.906Z
creator: schmar
notation: AL-1429
preferred label: Çepune-Senice @sq
definition: Mbihypje @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Zhulat-Picari Fault System

Zminec Fault
type: Concept
created: 2021-08-19T10:13:08.928Z
creator: schmar
notation: AL-1434
preferred label: Zminec @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Zhulat-Picari Fault System

Cerkovice Fault
type: Concept
created: 2021-08-19T10:13:08.933Z
creator: schmar
notation: AL-1435
preferred label: Cerkovice @sq
definition: Mbihypje @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Zhulat-Picari Fault System

Krongj-Leshnice Fault
type: Concept
created: 2021-08-19T10:13:08.919Z
creator: schmar
notation: AL-1432
preferred label: Krongj-Leshnice @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Zhulat-Picari Fault System

Janicat-Qafe Leshnice Fault
type: Concept
created: 2021-08-19T10:13:08.923Z
creator: schmar
notation: AL-1433
preferred label: Janicat-Qafe Leshnice @sq
definition: Bllok gravitativ @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Zhulat-Picari Fault System

Dermish-Karroq Fault
type: Concept
created: 2021-08-19T10:13:08.937Z
creator: schmar
notation: AL-1436
preferred label: Dermish-Karroq @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Zhulat-Picari Fault System

Kodra Fault
type: Concept
created: 2021-08-19T10:13:08.941Z
creator: schmar
notation: AL-1437
preferred label: Kodra @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Zhulat-Picari Fault System

Toske-Mbjeshtove Fault System
type: Concept
created: 2021-08-19T10:13:08.831Z
creator: schmar
notation: AL-1412
preferred label: Toske-Mbjeshtove @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Leskovik-Poliçan-Liqeni i Banjes Large-Scale Fault System

Velçan Fault System
type: Concept
created: 2021-08-19T10:13:08.835Z
creator: schmar
notation: AL-1413
preferred label: Velçan @sq
definition: Bllok gravitativ @sq
narrower: Vokopole Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Leskovik-Poliçan-Liqeni i Banjes Large-Scale Fault System

Vokopole Fault
type: Concept
created: 2021-08-19T10:13:08.840Z
creator: schmar
notation: AL-1414
preferred label: Vokopole @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Velçan Fault System

Çarçove-Bodar-Poliçan-Turje Fault System
type: Concept
created: 2021-08-19T10:13:08.784Z
creator: schmar
notation: AL-142
preferred label: Çarçove-Bodar-Poliçan-Turje @sq
definition: Tektonike afrovertikale @sq
narrower: Petran-Kukuçova Fault
narrower: Peshtan-Mezhgoran Fault
narrower: Golemaj-Bubsi Fault
narrower: Topojan-Klos Fault
narrower: Dragot-Sulove Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Leskovik-Poliçan-Liqeni i Banjes Large-Scale Fault System

Dragot-Sulove Fault
type: Concept
created: 2021-08-19T10:13:08.815Z
creator: schmar
notation: AL-148
preferred label: Dragot-Sulove @sq
definition: Tektonike Diapirike @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Çarçove-Bodar-Poliçan-Turje Fault System

Topojan-Klos Fault
type: Concept
created: 2021-08-19T10:13:08.807Z
creator: schmar
notation: AL-147
preferred label: Topojan-Klos @sq
definition: Tektonike afrovertikale @sq
narrower: Topojan-Klos Subfault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Çarçove-Bodar-Poliçan-Turje Fault System

Topojan-Klos Subfault
type: Concept
created: 2021-08-19T10:13:08.811Z
creator: schmar
notation: AL-1471
preferred label: Topojan-Klos @sq
definition: Tektonike afrovertikale-nderfaciale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Topojan-Klos Fault

Petran-Kukuçova Fault
type: Concept
created: 2021-08-19T10:13:08.788Z
creator: schmar
notation: AL-143
preferred label: Petran-Kukuçova @sq
definition: Tektonike afrovertikale @sq
narrower: Selcka-Maja e Laducit Subfault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Çarçove-Bodar-Poliçan-Turje Fault System

Selcka-Maja e Laducit Subfault
type: Concept
created: 2021-08-19T10:13:08.792Z
creator: schmar
notation: AL-144
preferred label: Selcka-Maja e Laducit @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Petran-Kukuçova Fault

Golemaj-Bubsi Fault
type: Concept
created: 2021-08-19T10:13:08.803Z
creator: schmar
notation: AL-146
preferred label: Golemaj-Bubsi @sq
definition: Tektonike afrovertikale-nderfaciale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Çarçove-Bodar-Poliçan-Turje Fault System

Peshtan-Mezhgoran Fault
type: Concept
created: 2021-08-19T10:13:08.795Z
creator: schmar
notation: AL-145
preferred label: Peshtan-Mezhgoran @sq
definition: Bllok gravitativ @sq
narrower: Beçisht Subfault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Çarçove-Bodar-Poliçan-Turje Fault System

Beçisht Subfault
type: Concept
created: 2021-08-19T10:13:08.799Z
creator: schmar
notation: AL-145111
preferred label: Beçisht @sq
definition: Tektonike afrovertikale-nderfaciale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Peshtan-Mezhgoran Fault

Caush-Janjar Fault System
type: Concept
created: 2021-08-19T10:13:08.945Z
creator: schmar
notation: AL-1438
preferred label: Caush-Janjar @sq
definition: Tektonike afrovertikale @sq
narrower: Janjar Subfault
narrower: Markat-Verva Fault
narrower: Sopiku Fault
narrower: Bregas-Nivice Fault
narrower: Vana-Lukova Fault
narrower: Vergo-Tatzat Fault
narrower: Tatzat Fault
narrower: Fushebardhe Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Leskovik-Poliçan-Liqeni i Banjes Large-Scale Fault System

Vana-Lukova Fault
type: Concept
created: 2021-08-19T10:13:08.970Z
creator: schmar
notation: AL-1444
preferred label: Vana-Lukova @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Caush-Janjar Fault System

Vergo-Tatzat Fault
type: Concept
created: 2021-08-19T10:13:08.974Z
creator: schmar
notation: AL-1445
preferred label: Vergo-Tatzat @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Caush-Janjar Fault System

Tatzat Fault
type: Concept
created: 2021-08-19T10:13:08.978Z
creator: schmar
notation: AL-1446
preferred label: Tatzat @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Caush-Janjar Fault System

Janjar Subfault
type: Concept
created: 2021-08-19T10:13:08.949Z
creator: schmar
notation: AL-1439
preferred label: Janjar @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Caush-Janjar Fault System

Fushebardhe Fault
type: Concept
created: 2021-08-19T10:13:08.982Z
creator: schmar
notation: AL-1447
preferred label: Fushebardhe @sq
definition: Tektonike Diapirike @sq
narrower: Çiflik Subfault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Caush-Janjar Fault System

Çiflik Subfault
type: Concept
created: 2021-08-19T10:13:08.986Z
creator: schmar
notation: AL-1448
preferred label: Çiflik @sq
definition: Mbihypje @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Fushebardhe Fault

Bregas-Nivice Fault
type: Concept
created: 2021-08-19T10:13:08.965Z
creator: schmar
notation: AL-1443
preferred label: Bregas-Nivice @sq
definition: Mbihypje @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Caush-Janjar Fault System

Markat-Verva Fault
type: Concept
created: 2021-08-19T10:13:08.953Z
creator: schmar
notation: AL-1440
preferred label: Markat-Verva @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Caush-Janjar Fault System

Sopiku Fault
type: Concept
created: 2021-08-19T10:13:08.957Z
creator: schmar
notation: AL-1441
preferred label: Sopiku @sq
definition: Tektonike afrovertikale @sq
narrower: Ksamil Subfault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Caush-Janjar Fault System

Ksamil Subfault
type: Concept
created: 2021-08-19T10:13:08.961Z
creator: schmar
notation: AL-1442
preferred label: Ksamil @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Sopiku Fault

Borsh-Bolene Fault System
type: Concept
created: 2021-08-19T10:13:08.990Z
creator: schmar
notation: AL-1449
preferred label: Borsh-Bolene @sq
definition: Tektonike afrovertikale @sq
narrower: Qeparo Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Leskovik-Poliçan-Liqeni i Banjes Large-Scale Fault System

Qeparo Fault
type: Concept
created: 2021-08-19T10:13:08.995Z
creator: schmar
notation: AL-1450
preferred label: Qeparo @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Borsh-Bolene Fault System

Krahesi i Siperm Fault System
type: Concept
created: 2021-08-19T10:13:08.844Z
creator: schmar
notation: AL-1415
preferred label: Krahesi i Siperm @sq
definition: Tektonike afrovertikale @sq
narrower: Greshice Fault
narrower: Ballsh Fault
narrower: Libohove Fault 1
narrower: Glina Fault
narrower: Libohove Fault 2
narrower: Nivan Fault
narrower: Maja e Strokavecit Fault
narrower: Maja e Kendrevices Fault
narrower: Bençe Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Leskovik-Poliçan-Liqeni i Banjes Large-Scale Fault System

Ballsh Fault
type: Concept
created: 2021-08-19T10:13:08.852Z
creator: schmar
notation: AL-1417
preferred label: Ballsh @sq
definition: Bllok gravitativ @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Krahesi i Siperm Fault System

Libohove Fault 1
type: Concept
created: 2021-08-19T10:13:08.857Z
creator: schmar
notation: AL-1418
preferred label: Libohove (1) @sq
definition: Tektonike Diapirike @sq
narrower: Radat Subfault
narrower: Vllaho-Goranxi Subfault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Krahesi i Siperm Fault System

Radat Subfault
type: Concept
created: 2021-08-19T10:13:08.861Z
creator: schmar
notation: AL-1419
preferred label: Radat @sq
definition: Tektonike Diapirike @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Libohove Fault 1

Vllaho-Goranxi Subfault
type: Concept
created: 2021-08-19T10:13:08.865Z
creator: schmar
notation: AL-1420
preferred label: Vllaho-Goranxi @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Libohove Fault 1

Nivan Fault
type: Concept
created: 2021-08-19T10:13:08.878Z
creator: schmar
notation: AL-1423
preferred label: Nivan @sq
definition: Tektonike afrovertikale @sq
narrower: Asim Zeneli Subfault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Krahesi i Siperm Fault System

Asim Zeneli Subfault
type: Concept
created: 2021-08-19T10:13:08.882Z
creator: schmar
notation: AL-1424
preferred label: Asim Zeneli @sq
definition: Mbihypje @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Nivan Fault

Glina Fault
type: Concept
created: 2021-08-19T10:13:08.869Z
creator: schmar
notation: AL-1421
preferred label: Glina @sq
definition: Bllok gravitativ @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Krahesi i Siperm Fault System

Libohove Fault 2
type: Concept
created: 2021-08-19T10:13:08.874Z
creator: schmar
notation: AL-1422
preferred label: Libohove (2) @sq
definition: Bllok gravitativ @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Krahesi i Siperm Fault System

Maja e Strokavecit Fault
type: Concept
created: 2021-08-19T10:13:08.886Z
creator: schmar
notation: AL-1425
preferred label: Maja e Strokavecit @sq
definition: Bllok gravitativ @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Krahesi i Siperm Fault System

Maja e Kendrevices Fault
type: Concept
created: 2021-08-19T10:13:08.891Z
creator: schmar
notation: AL-1426
preferred label: Maja e Kendrevices @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Krahesi i Siperm Fault System

Greshice Fault
type: Concept
created: 2021-08-19T10:13:08.848Z
creator: schmar
notation: AL-1416
preferred label: Greshice @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Krahesi i Siperm Fault System

Bençe Fault
type: Concept
created: 2021-08-19T10:13:08.897Z
creator: schmar
notation: AL-1427
preferred label: Bençe @sq
definition: Tektonike Diapirike @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Krahesi i Siperm Fault System

Vau I Dejes-Selimaj Nappe boundary
type: Concept
created: 2021-08-19T10:13:09.256Z
creator: schmar
notation: AL-031
preferred label: Vau I Dejes-Selimaj @sq
definition: Tektonike shariazhuese- Kontakt tektonik midis zonave tektonike @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Albania

Qafe Llogara Fault System
type: Concept
created: 2021-08-19T10:13:08.748Z
creator: schmar
notation: AL-261
preferred label: Qafe Llogara @sq
definition: Kontakt Tektonik Horst-Graben @sq
narrower: Qafa e Brisarit Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Albania

Qafa e Brisarit Fault
type: Concept
created: 2021-08-19T10:13:08.753Z
creator: schmar
notation: AL-262
preferred label: Qafa e Brisarit @sq
narrower: Dhermi Subfault
narrower: Mali i Flamurit Subfault
narrower: Kepi i Gjuhezes Subfault 1
narrower: Kepi i Gjuhezes Subfault 2
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Qafe Llogara Fault System

Kepi i Gjuhezes Subfault 1
type: Concept
created: 2021-08-19T10:13:08.767Z
creator: schmar
notation: AL-265
preferred label: Kepi i Gjuhezes (1) @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Qafa e Brisarit Fault

Kepi i Gjuhezes Subfault 2
type: Concept
created: 2021-08-19T10:13:08.771Z
creator: schmar
notation: AL-266
preferred label: Kepi i Gjuhezes (2) @sq
definition: Kontakt tektonik midis zonës tektonike Jonike dhe zonës tektonike Kruja @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Qafa e Brisarit Fault

Mali i Flamurit Subfault
type: Concept
created: 2021-08-19T10:13:08.762Z
creator: schmar
notation: AL-264
preferred label: Mali i Flamurit @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Qafa e Brisarit Fault

Dhermi Subfault
type: Concept
created: 2021-08-19T10:13:08.758Z
creator: schmar
notation: AL-263
preferred label: Dhermi @sq
definition: Tektonike afrovertikale Horst-Graben @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Qafa e Brisarit Fault

Zerqan-Surroj-Morine Nappe boundary
type: Concept
created: 2021-08-19T10:13:09.876Z
creator: schmar
notation: AL-15211
preferred label: Zerqan-Surroj-Morine @sq
definition: Mbihypese, Tektonika paralele @sq
narrower: Gryke Noka Fault System
narrower: Sopoti Fault System
narrower: Kulla e Zyberit Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Albania

Kulla e Zyberit Fault System
type: Concept
created: 2021-08-19T10:13:09.938Z
creator: schmar
notation: AL-152115
preferred label: Kulla e Zyberit @sq
definition: Mbihypese @sq
narrower: Turaj Fault
narrower: Lume-Xhaferaj Fault
narrower: Tershana Fault
narrower: Kolesjan Fault
narrower: Tejdrini Fault
narrower: Shtiqen Fault
narrower: Gjallica Fault
narrower: Pobreg Fault
narrower: Nimce Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Zerqan-Surroj-Morine Nappe boundary

Nimce Fault
type: Concept
created: 2021-08-19T10:13:09.979Z
creator: schmar
notation: AL-152124
preferred label: Nimce @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kulla e Zyberit Fault System

Tershana Fault
type: Concept
created: 2021-08-19T10:13:09.954Z
creator: schmar
notation: AL-152118
preferred label: Tershana @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kulla e Zyberit Fault System

Kolesjan Fault
type: Concept
created: 2021-08-19T10:13:09.958Z
creator: schmar
notation: AL-152119
preferred label: Kolesjan @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kulla e Zyberit Fault System

Turaj Fault
type: Concept
created: 2021-08-19T10:13:09.943Z
creator: schmar
notation: AL-152116
preferred label: Turaj @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kulla e Zyberit Fault System

Lume-Xhaferaj Fault
type: Concept
created: 2021-08-19T10:13:09.947Z
creator: schmar
notation: AL-152117
preferred label: Lume-Xhaferaj @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kulla e Zyberit Fault System

Gjallica Fault
type: Concept
created: 2021-08-19T10:13:09.970Z
creator: schmar
notation: AL-152122
preferred label: Gjallica @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kulla e Zyberit Fault System

Pobreg Fault
type: Concept
created: 2021-08-19T10:13:09.974Z
creator: schmar
notation: AL-152123
preferred label: Pobreg @sq
definition: Tektonike afrovertikale formacionale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kulla e Zyberit Fault System

Tejdrini Fault
type: Concept
created: 2021-08-19T10:13:09.962Z
creator: schmar
notation: AL-152120
preferred label: Tejdrini @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kulla e Zyberit Fault System

Shtiqen Fault
type: Concept
created: 2021-08-19T10:13:09.966Z
creator: schmar
notation: AL-152121
preferred label: Shtiqen @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kulla e Zyberit Fault System

Gryke Noka Fault System
type: Concept
created: 2021-08-19T10:13:09.880Z
creator: schmar
notation: AL-15212
preferred label: Gryke Noka @sq
definition: Tektonike afrovertikale, tektonika paralele @sq
narrower: Lukani Fault
narrower: Selishta Fault
narrower: Homesh Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Zerqan-Surroj-Morine Nappe boundary

Selishta Fault
type: Concept
created: 2021-08-19T10:13:09.889Z
creator: schmar
notation: AL-15214
preferred label: Selishta @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Gryke Noka Fault System

Homesh Fault
type: Concept
created: 2021-08-19T10:13:09.893Z
creator: schmar
notation: AL-15215
preferred label: Homesh @sq
definition: Tektonike afrovertikale, tektonike me karakter shariazhues (mbulesor) @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Gryke Noka Fault System

Lukani Fault
type: Concept
created: 2021-08-19T10:13:09.884Z
creator: schmar
notation: AL-15213
preferred label: Lukani @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Gryke Noka Fault System

Sopoti Fault System
type: Concept
created: 2021-08-19T10:13:09.897Z
creator: schmar
notation: AL-15216
preferred label: Sopoti @sq
definition: Mbulesore @sq
narrower: Fushe Bulqize Fault
narrower: Zimur Fault
narrower: Poçest Fault
narrower: Peshkopia Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Zerqan-Surroj-Morine Nappe boundary

Poçest Fault
type: Concept
created: 2021-08-19T10:13:09.930Z
creator: schmar
notation: AL-152113
preferred label: Poçest @sq
definition: Shariazh, tektonike shariazhuese me karakter mbulesor @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Sopoti Fault System

Peshkopia Fault
type: Concept
created: 2021-08-19T10:13:09.934Z
creator: schmar
notation: AL-152114
preferred label: Peshkopia @sq
definition: Shariazh, tektonike me karakter mbihypes @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Sopoti Fault System

Fushe Bulqize Fault
type: Concept
created: 2021-08-19T10:13:09.901Z
creator: schmar
notation: AL-15217
preferred label: Fushe Bulqize @sq
definition: Tektonike afrovertikale @sq
narrower: Gjurasi Subfault
narrower: Arapaj I Poshtem Subfault
narrower: Shqathi Subfault
narrower: Fushe Muhur Subfault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Sopoti Fault System

Gjurasi Subfault
type: Concept
created: 2021-08-19T10:13:09.905Z
creator: schmar
notation: AL-15218
preferred label: Gjurasi @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Fushe Bulqize Fault

Fushe Muhur Subfault
type: Concept
created: 2021-08-19T10:13:09.919Z
creator: schmar
notation: AL-152111
preferred label: Fushe Muhur @sq
definition: Tektonike afrovertikale, tektonike shariazhuese me karakter mbulesor @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Fushe Bulqize Fault

Arapaj I Poshtem Subfault
type: Concept
created: 2021-08-19T10:13:09.910Z
creator: schmar
notation: AL-15219
preferred label: Arapaj I Poshtem @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Fushe Bulqize Fault

Shqathi Subfault
type: Concept
created: 2021-08-19T10:13:09.914Z
creator: schmar
notation: AL-152110
preferred label: Shqathi @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Fushe Bulqize Fault

Zimur Fault
type: Concept
created: 2021-08-19T10:13:09.924Z
creator: schmar
notation: AL-152112
preferred label: Zimur @sq
definition: Shariazh, tektonike shariazhuese me karakter mbulesor @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Sopoti Fault System

Kuc-Ramice Large-Scale Fault System
type: Concept
created: 2021-08-19T10:13:09.003Z
creator: schmar
notation: AL-1451
preferred label: Kuc-Ramice @sq
definition: Tektonike afrovertikale @sq
narrower: Llakatund Fault
narrower: Ilias - Pilur Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Albania

Ilias - Pilur Fault
type: Concept
created: 2021-08-19T10:13:09.011Z
creator: schmar
notation: AL-1452
preferred label: Ilias - Pilur @sq
definition: Tektonike afrovertikale, ektonike paralele @sq
narrower: Sinje Subfault
narrower: Arianitasi Subfault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kuc-Ramice Large-Scale Fault System

Arianitasi Subfault
type: Concept
created: 2021-08-19T10:13:09.019Z
creator: schmar
notation: AL-1454
preferred label: Arianitasi @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Ilias - Pilur Fault

Sinje Subfault
type: Concept
created: 2021-08-19T10:13:09.015Z
creator: schmar
notation: AL-1453
preferred label: Sinje @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Ilias - Pilur Fault

Llakatund Fault
type: Concept
created: 2021-08-19T10:13:09.007Z
creator: schmar
notation: AL-14511
preferred label: Llakatund @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kuc-Ramice Large-Scale Fault System

Mali I Vashes-Rohmisht-Strelce-Mali I Firtit-Guri I Bardhe-Rubik-Hajmel Nappe boundary
type: Concept
created: 2021-08-19T10:13:09.108Z
creator: schmar
notation: AL-1524
preferred label: Mali I Vashes-Rohmisht-Strelce-Mali I Firtit-Guri I Bardhe-Rubik-Hajmel @sq
definition: Tektonike mbulesore (shariazhuese)- Kontakt tektonik midis zonës tektonike Krasta dhe zonës tektonike Mirdita @sq
narrower: Nenishat
narrower: Kamniku Fault 1
narrower: Kamniku Fault 2
narrower: Lencka Fault
narrower: Kurtes Fault System
narrower: Ostrovica Fault System
narrower: Propanik Fault System
narrower: Qafa e Selites Fault System
narrower: Bostani Fault System
narrower: Cudhi-Kami Fault System
narrower: Manati Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Albania

Bostani Fault System
type: Concept
created: 2021-08-19T10:13:09.212Z
creator: schmar
notation: AL-152418
preferred label: Bostani @sq
definition: Tektonike afrovertikale, tektonike paralele @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Mali I Vashes-Rohmisht-Strelce-Mali I Firtit-Guri I Bardhe-Rubik-Hajmel Nappe boundary

Cudhi-Kami Fault System
type: Concept
created: 2021-08-19T10:13:09.217Z
creator: schmar
notation: AL-152419
preferred label: Cudhi-Kami @sq
definition: Tektonike afrovertikale @sq
narrower: Selita Fault
narrower: Spiten Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Mali I Vashes-Rohmisht-Strelce-Mali I Firtit-Guri I Bardhe-Rubik-Hajmel Nappe boundary

Selita Fault
type: Concept
created: 2021-08-19T10:13:09.222Z
creator: schmar
notation: AL-152420
preferred label: Selita @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Cudhi-Kami Fault System

Spiten Fault
type: Concept
created: 2021-08-19T10:13:09.226Z
creator: schmar
notation: AL-152421
preferred label: Spiten @sq
definition: Tektonike afrovertikale, tektonike paralele dhe terthore @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Cudhi-Kami Fault System

Manati Fault System
type: Concept
created: 2021-08-19T10:13:09.231Z
creator: schmar
notation: AL-152422
preferred label: Manati @sq
definition: Tektonike afrovertikale @sq
narrower: Manati Fault
narrower: Mali i Merqies Fault
narrower: Mërqi Fault
narrower: Nenshati Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Mali I Vashes-Rohmisht-Strelce-Mali I Firtit-Guri I Bardhe-Rubik-Hajmel Nappe boundary

Manati Fault
type: Concept
created: 2021-08-19T10:13:09.235Z
creator: schmar
notation: AL-1524221
preferred label: Manati (1) @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Manati Fault System

Nenshati Fault
type: Concept
created: 2021-08-19T10:13:09.247Z
creator: schmar
notation: AL-152425
preferred label: Nenshati @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Manati Fault System

Mali i Merqies Fault
type: Concept
created: 2021-08-19T10:13:09.239Z
creator: schmar
notation: AL-152423
preferred label: Mali i Merqies @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Manati Fault System

Mërqi Fault
type: Concept
created: 2021-08-19T10:13:09.243Z
creator: schmar
notation: AL-152424
preferred label: Mërqi @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Manati Fault System

Lencka Fault
type: Concept
created: 2021-08-19T10:13:09.129Z
creator: schmar
notation: AL-15244
preferred label: Lencka @sq
definition: Tektonike afrovertikale formacionale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Mali I Vashes-Rohmisht-Strelce-Mali I Firtit-Guri I Bardhe-Rubik-Hajmel Nappe boundary

Kamniku Fault 1
type: Concept
created: 2021-08-19T10:13:09.117Z
creator: schmar
notation: AL-15241
preferred label: Kamniku (1) @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Mali I Vashes-Rohmisht-Strelce-Mali I Firtit-Guri I Bardhe-Rubik-Hajmel Nappe boundary

Kamniku Fault 2
type: Concept
created: 2021-08-19T10:13:09.121Z
creator: schmar
notation: AL-15242
preferred label: Kamniku (2) @sq
definition: Tektonike afrovertikale, bllok brenda formacionit @sq
narrower: Benjeza Subfault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Mali I Vashes-Rohmisht-Strelce-Mali I Firtit-Guri I Bardhe-Rubik-Hajmel Nappe boundary

Benjeza Subfault
type: Concept
created: 2021-08-19T10:13:09.125Z
creator: schmar
notation: AL-15243
preferred label: Benjeza @sq
definition: Bllok gravitativ @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kamniku Fault 2

Ostrovica Fault System
type: Concept
created: 2021-08-19T10:13:09.142Z
creator: schmar
notation: AL-15247
preferred label: Ostrovica @sq
definition: Tektonike afrovertikale @sq
narrower: Ostrovica Fault
narrower: Gurekuq Fault
narrower: Alloktoni I Devollit Fault 1
narrower: Alloktoni I Devollit Fault 2
narrower: Mali I Oparit Fault
narrower: Mali I Lenies Fault
narrower: Lenie Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Mali I Vashes-Rohmisht-Strelce-Mali I Firtit-Guri I Bardhe-Rubik-Hajmel Nappe boundary

Alloktoni I Devollit Fault 1
type: Concept
created: 2021-08-19T10:13:09.161Z
creator: schmar
notation: AL-15249
preferred label: Alloktoni I Devollit (1) @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Ostrovica Fault System

Mali I Lenies Fault
type: Concept
created: 2021-08-19T10:13:09.176Z
creator: schmar
notation: AL-152411
preferred label: Mali I Lenies @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Ostrovica Fault System

Lenie Fault
type: Concept
created: 2021-08-19T10:13:09.182Z
creator: schmar
notation: AL-152412
preferred label: Lenie @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Ostrovica Fault System

Alloktoni I Devollit Fault 2
type: Concept
created: 2021-08-19T10:13:09.165Z
creator: schmar
notation: AL-152491
preferred label: Alloktoni I Devollit (2) @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Ostrovica Fault System

Mali I Oparit Fault
type: Concept
created: 2021-08-19T10:13:09.170Z
creator: schmar
notation: AL-152410
preferred label: Mali I Oparit @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Ostrovica Fault System

Ostrovica Fault
type: Concept
created: 2021-08-19T10:13:09.147Z
creator: schmar
notation: AL-152471
preferred label: Ostrovica @sq
definition: tektonike paralele dhe terthore @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Ostrovica Fault System

Gurekuq Fault
type: Concept
created: 2021-08-19T10:13:09.151Z
creator: schmar
notation: AL-15248
preferred label: Gurekuq @sq
definition: Tektonike afrovertikale @sq
narrower: Gurakuqi Subfault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Ostrovica Fault System

Gurakuqi Subfault
type: Concept
created: 2021-08-19T10:13:09.156Z
creator: schmar
notation: AL-152481
preferred label: Gurakuqi (1) @sq
definition: tektonike nderprerese @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Gurekuq Fault

Kurtes Fault System
type: Concept
created: 2021-08-19T10:13:09.133Z
creator: schmar
notation: AL-15245
preferred label: Kurtes @sq
definition: Tektonike afrovertikale @sq
narrower: Trebicka Fault
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Mali I Vashes-Rohmisht-Strelce-Mali I Firtit-Guri I Bardhe-Rubik-Hajmel Nappe boundary

Trebicka Fault
type: Concept
created: 2021-08-19T10:13:09.138Z
creator: schmar
notation: AL-15246
preferred label: Trebicka @sq
definition: Tektonike afrovertikale, tektonike paralele dhe terthore @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Kurtes Fault System

Propanik Fault System
type: Concept
created: 2021-08-19T10:13:09.187Z
creator: schmar
notation: AL-152413
preferred label: Propanik @sq
definition: Tektonike afrovertikale @sq
narrower: Labinot Mal Fault
narrower: Bena Fault
narrower: Shengjin I Madh
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Mali I Vashes-Rohmisht-Strelce-Mali I Firtit-Guri I Bardhe-Rubik-Hajmel Nappe boundary

Bena Fault
type: Concept
created: 2021-08-19T10:13:09.198Z
creator: schmar
notation: AL-152415
preferred label: Bena @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Propanik Fault System

Shengjin I Madh
type: Concept
created: 2021-08-19T10:13:09.203Z
creator: schmar
notation: AL-152416
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Propanik Fault System

Labinot Mal Fault
type: Concept
created: 2021-08-19T10:13:09.193Z
creator: schmar
notation: AL-152414
preferred label: Labinot Mal @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Propanik Fault System

Nenishat
type: Concept
created: 2021-08-19T10:13:09.113Z
creator: schmar
notation: AL-1524111
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Mali I Vashes-Rohmisht-Strelce-Mali I Firtit-Guri I Bardhe-Rubik-Hajmel Nappe boundary

Qafa e Selites Fault System
type: Concept
created: 2021-08-19T10:13:09.208Z
creator: schmar
notation: AL-152417
preferred label: Qafa e Selites @sq
definition: Tektonike afrovertikale @sq
references: https://data.geoscience.earth/ncl/geoera/ref/10712
in scheme: Tectonic Boundary Objects in Europe
broader: Mali I Vashes-Rohmisht-Strelce-Mali I Firtit-Guri I Bardhe-Rubik-Hajmel Nappe boundary

Tectonic Boundary in the Pannonian Basin
created: 2021-05-03T08:57:16.045Z
top concept of: Tectonic Boundary Objects in Europe
type: Concept
notation: HGI
notation: MBFSZ
notation: GeoInform
in scheme: Tectonic Boundary Objects in Europe

Tectonic Boundary in Denmark
created: 2021-05-03T08:53:05.430Z
type: Concept
top concept of: Tectonic Boundary Objects in Europe
notation: DK-0
scope note: All named tectonic boundary objects that are located (at least partly) in Denmark, are identified by an ID with the prefix „DK“ listed in the notation. Fault systems and/or fault domains can cross political borders and are therefore shared by several countries. Therefore, they can contain faults from different countries, indicated by country-specific prefixes to the respective ID.
definition: Fault in Denmark, displayed in the HIKE European fault database.
in scheme: Tectonic Boundary Objects in Europe

Tectonic Boundary in France
type: Concept
top concept of: Tectonic Boundary Objects in Europe
created: 2021-05-03T08:54:10.603Z
notation: FR-0
scope note: All named tectonic boundary objects that are located (at least partly) in France, are identified by an ID with the prefix „FR“ listed in the notation. Fault systems and/or fault domains can cross political borders and are therefore shared by several countries. Therefore, they can contain faults from different countries, indicated by country-specific prefixes to the respective ID.
definition: Fault in France, displayed in the HIKE European fault database.
in scheme: Tectonic Boundary Objects in Europe

Tectonic boundary in Lithuania
scope note: All named tectonic boundary objects that are located (at least partly) in Lithuania, are identified by an ID with the prefix „LT“ listed in the notation. Fault systems and/or fault domains can cross political borders and are therefore shared by several countries. Therefore, they can contain faults from different countries, indicated by country-specific prefixes to the respective ID.
definition: Fault in Lithuania displayed in the HIKE European fault database.
type: Concept
top concept of: Tectonic Boundary Objects in Europe
created: 2020-05-25T08:59:45.777Z
notation: LT-000
preferred label: Tektoninės ribos Lietuvoje @lt
narrower: West Lithuanian Fault Domain
narrower: East Lithuanian Fault Domain
narrower: Mid-Lithuanian Share Zone
in scheme: Tectonic Boundary Objects in Europe

West Lithuanian Fault Domain
type: Concept
created: 2020-05-25T08:59:45.804Z
definition: Faults were identified by 2D (predominantly) and 3D seismic, well data, supported by potential fields data. West Lithuanian fault domain is situated in the west part of Lithuania, from the Baltic sea to Pasvalys town, Nevezis river, Kaunas city and Lazdijai town. Faults of the Domain are identified in crystalline basement and penetrate the Lower Paleozoic sedimentary cover. The faults could be traced up to Lower Devonian Gragzdai Group (Early Pragian).
definition: Lūžiai nustatyti 2D (daugiausiai) ir 3D seisminės žvalgybos, gręžinių ir potencialių laukų duomenimis. Vakarų Lietuvos lūžių domeinas apima vakarinę Lietuvos dalį, nuo Baltijos jūros iki Pasvalio miesto, Nevėžio upės, Kauno miesto ir Lazdijų miesto. Lūžių domeiną sudarantys lūžiai išskiriami kristaliniame pamate ir nuosėdinėje dangoje iki apatinio devono Gargždų Serijos (ankstyvaisis Pragis). @lt
notation: LT-001
preferred label: Vakarų Lietuvos lūžių Domeinas @lt
narrower: Mazeikiai-Telsiai Fault Set
narrower: Gargzdai Fault Chain
narrower: Rietavas Fault SubDomain
narrower: Gubriai Fault Chain
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic boundary in Lithuania

Gubriai Fault Chain
type: Concept
created: 2020-05-25T08:59:46.084Z
definition: Gubriai fault chain comprises N-S and W-E oriented faults. They extend from the river Jura to Griniai village. Faults are of reverse type, they have been identified by 2D seismic and well data.
definition: Grandinę sudaro lūžiai orentuoti Š-P ir V-R kryptimis besitęsiantys nuo Jūros upės iki Grinių gyvenvietės. Lūžiai yra antsprūdžio tipo, išskirti 2D seisminės žvalgybos ir gręžinių duomenimis. @lt
notation: LT-014
preferred label: Gūbrių lūžių grandinė @lt
references: https://data.geoscience.earth/ncl/geoera/ref/899
references: https://data.geoscience.earth/ncl/geoera/ref/900
in scheme: Tectonic Boundary Objects in Europe
broader: West Lithuanian Fault Domain

Mazeikiai-Telsiai Fault Set
type: Concept
created: 2020-05-25T08:59:45.832Z
definition: The fault set comprises predominantly rerverse type faults, identified by 2D and 3D seismic and well data. Fault set is located in the North west part of Lithuania, in the North the faults strike from Skuodas town to Mazeikiai town, in the South - from the coast of Baltic sea, crosses Kretinga town and Siauliai city, and continues to Pakruojis town. Faults of the fault set are identified in crystalline basement and penetrate Lower Paleozoic sedimentary cover. The faults could be traced up to Lower Devonian Gragzdai Group (Early Pragian).
definition: Lūžių grupę sudaro ansprūdžio tipo lūžiai, išskirti seisminės 2D ir 3D žvalgybos ir gręžinių duomenimis. Mažeikių-Telšių lūžių grupė yra šiaurės vakarinėje Lietuvos dalyje, šiaurėje lūžiai transuojami nuo Skuodo miesto iki Mažeikių miesto, pietuose nuo Baltijos jūros kranto, kerta Kretingos ir Šiaulių miestus ir tęsiasi link Pakruojo miesto. Lūžiai išskiriami kristaliniame pamate ir nuosėdinėje dangoje iki apatinio devono Gargždų Serijos (ankstyvaisis Pragis). @lt
notation: LT-011
preferred label: Mažeikių - Telšių lūžių grupė @lt
narrower: Telsiai Fault Zone
narrower: Klaipeda Fault
narrower: Akmene Fault
narrower: Mazeikiai Fault
narrower: Tryskiai Fault
narrower: Gruzdziai Fault
references: https://data.geoscience.earth/ncl/geoera/ref/907
in scheme: Tectonic Boundary Objects in Europe
broader: West Lithuanian Fault Domain

Telsiai Fault Zone
type: Concept
created: 2020-05-25T08:59:45.861Z
definition: Telsiai fault zone is oriented in W-E direction and is asigned to reverse fault type. The amplitude exceeds 300 m; the total length of onshore Telsiai fault zone is up to 270 km.The NE-SW faults are dipping at the angles 60-80o. The fault zone was identified in crystalline basement and penetrate Lower Paleozoic sedimentary cover. The faults could be traced up to Lower Devonian Gragzdai Group (Early Pragian). The fault zone extends from the Baltic sea, through Palanga town, Plunge town, Telsiai town, crosses Siauliai city and continues to Birzai town.
definition: Telšių lūžių zona yra orientuota V-R kryptimi, ji tęsiasi nuo Baltijos jūros pakrantės, pro Palangos miestą, Plungės miestą ir Telšių miestą, kerta Šiaulių miestą ir tęsiasi link Biržų miesto. Lūžių zonos lūžiai yra antstūmio tipo. Telšių lūžių zonos amplitudė viršija 300 m, o jos žemyninės dalies ilgis siekia 270 km. Lūžiai išskiriami kristaliniame pamate ir nuosėdinėje dangoje iki apatinio devono Gargždų Serijos (ankstyvaisis Pragis). @lt
notation: LT-111
preferred label: Telšių lūžių zona @lt
references: https://data.geoscience.earth/ncl/geoera/ref/907
references: https://data.geoscience.earth/ncl/geoera/ref/904
references: https://data.geoscience.earth/ncl/geoera/ref/906
references: https://data.geoscience.earth/ncl/geoera/ref/901
in scheme: Tectonic Boundary Objects in Europe
broader: Mazeikiai-Telsiai Fault Set

Gruzdziai Fault
type: Concept
created: 2020-05-25T08:59:46.001Z
definition: Gruzdziai fault is oriented in SW - NE direction. The fault strikes from the Gruzdziai village and continues towards direction of Latvia, it croses Musa river along the way. The type of the fault is assigned to reverse faults type. It has been identified by 2D seismic survey data and by interpretation of the magnetic and gravity anomalies.
definition: Gruzdžių lūžis yra orentuotas PV-ŠR kryptimi. Jis tęsiasi nuo Gruzdžių gyvenvietės link Latvijos teritorijos, pakeliui kertant Mūšos upę. Gruzdžių ansprūdžio tipo lūžis yra nustatytas 2D seisminės žvalgybos duomenimis ir interpretuojant gravitacinės ir magnetinės žvalgybos duomenis. @lt
notation: LT-116
preferred label: Gruzdžių lūžis @lt
references: https://data.geoscience.earth/ncl/geoera/ref/899
references: https://data.geoscience.earth/ncl/geoera/ref/900
in scheme: Tectonic Boundary Objects in Europe
broader: Mazeikiai-Telsiai Fault Set

Tryskiai Fault
type: Concept
created: 2020-05-25T08:59:45.971Z
definition: Tryskiai fault is oriented in S - N direction. Tryskiai fault strikes from the Virvyte river and continues towards direction of Venta town. The type of the fault is reverse fault. It has been identified by 2D seismic survey data. The fault was identified in crystalline basement and penetrate Lower Paleozoic sedimentary cover. The faults could be traced up to Lower Devonian Gragzdai Group (Early Pragian).
definition: Tryškių lūžis yra orentuotas P-Š kryptimi ir tęsiasi nuo Virvytės upės link Ventos miesto. Šis lūžia yra priskiriamas antsprūdžio tipo lūžiams. Lūžis nustatytas naudojant 2D seisminės žvalgybos duomenis. Tryškių lūžis yra išskiriamas kristaliniame pamate ir nuosėdinėje dangoje iki apatinio devono Gargždų Serijos (ankstyvaisis Pragis). @lt
notation: LT-115
preferred label: Tryškių lūžis @lt
references: https://data.geoscience.earth/ncl/geoera/ref/899
references: https://data.geoscience.earth/ncl/geoera/ref/900
in scheme: Tectonic Boundary Objects in Europe
broader: Mazeikiai-Telsiai Fault Set

Klaipeda Fault
type: Concept
created: 2020-05-25T08:59:45.888Z
definition: Klaipeda fault is oriented in SW - NE direction. The fault strikes from coast of Baltic sea to Palanga town and continues to direction of Salantai village. Fault is asigned to reverse faults type. It has been identified by 2D seismic survey and well data. The fault was identified in crystalline basement and penetrate Lower Paleozoic sedimentary cover. The faults could be traced up to Lower Devonian Gragzdai Group (Early Pragian).
definition: Klaipėdos lūžis - orentuotas PV - ŠR kryptimi, jis tęsiasi nuo Baltijos jūros pakrantės, pro Palangos miestą link Salantų gyvenvietės. Lūžis yra priskiriamas prie ansprūdžio tipo lūžių. Lūžis nustatytas 2D seisminės žvalgybos ir gręžinių duomenimis. Klaipėdos lūžis yra išskiriamas kristaliniame pamate ir nuosėdinėje dangoje iki apatinio devono Gargždų Serijos (ankstyvaisis Pragis). @lt
notation: LT-112
preferred label: Klaipėdos lūžis @lt
references: https://data.geoscience.earth/ncl/geoera/ref/907
references: https://data.geoscience.earth/ncl/geoera/ref/904
references: https://data.geoscience.earth/ncl/geoera/ref/906
references: https://data.geoscience.earth/ncl/geoera/ref/901
in scheme: Tectonic Boundary Objects in Europe
broader: Mazeikiai-Telsiai Fault Set

Mazeikiai Fault
type: Concept
created: 2020-05-25T08:59:45.944Z
definition: Mazeikiai fault is oriented in SW - NE direction. Mazeikiai fault strikes from Tryksiai village, through Mazeikiai town and continues to Venta river. The amplitudes ranges from 25 to 50 meters. The fault inclines to the north, it is assigend to reverse faults type. It has been identified by 2D seismic and well data. The fault was identified in crystalline basement and penetrate Lower Paleozoic sedimentary cover. The faults could be traced up to Lower Devonian Gragzdai Group (Early Pragian).
definition: Mažeikių lūžis orentuotas V-ŠR kryptimi tęsiasi nuo Trikšlių gyvenvietės, pro Mažeikių miestą link Ventos upės. Lūžio amplitudė kaiti - vidutiniškai yra apie 25 m, vietomis padidėja iki 50 m. Lūžis yra antspūdžio tipo palinkęs šiaurės kryptimi. Lūžis nustatytas 2D seisminės žvalgybos ir gręžinių duomenimis. Mažeikių lūžis yra išskiriamas kristaliniame pamate ir nuosėdinėje dangoje iki apatinio devono Gargždų Serijos (ankstyvaisis Pragis). @lt
notation: LT-114
preferred label: Mažeikių lūžis @lt
references: https://data.geoscience.earth/ncl/geoera/ref/901
references: https://data.geoscience.earth/ncl/geoera/ref/908
references: https://data.geoscience.earth/ncl/geoera/ref/904
references: https://data.geoscience.earth/ncl/geoera/ref/906
in scheme: Tectonic Boundary Objects in Europe
broader: Mazeikiai-Telsiai Fault Set

Akmene Fault
type: Concept
created: 2020-05-25T08:59:45.916Z
definition: Akmene fault is oriented in NW - SE - NE direction. Fault strikes from Skuodas town, to Seda village and continues to Naujoji Akmene town. The fault continues as Pape fault zone to the Latvian teritory. This fault is asighn to reverse faults type. It has been identifiedby 2D seismic survey and well data.The fault was identified in crystalline basement and penetrate Lower Paleozoic sedimentary cover. The fault could be traced up to the Carboniferouse.
definition: Akmenės lūžis yra orentuotas ŠV-PR-ŠR kryptimi. Lūžis tęsiasi nuo Skuodo miesto, pro Sedos miestelį link Naujosios Akmenės miesto. Lūžis vakarų Latvijoje susijungia su Papės lūžių zona. Jis yra antsprudžio tipo. Lūžis nustatytas 2D seisminės žvalgybos ir gręžinių duomenimis. Akmenės lūžis yra išskiriamas kristaliniame pamate ir nuosėdinėje dangoje iki karbono. @lt
notation: LT-113
preferred label: Akmenės lūžis @lt
references: https://data.geoscience.earth/ncl/geoera/ref/901
references: https://data.geoscience.earth/ncl/geoera/ref/908
references: https://data.geoscience.earth/ncl/geoera/ref/904
references: https://data.geoscience.earth/ncl/geoera/ref/906
in scheme: Tectonic Boundary Objects in Europe
broader: Mazeikiai-Telsiai Fault Set

Rietavas Fault SubDomain
type: Concept
created: 2020-05-25T08:59:46.057Z
definition: Reverse faults are oriented in SW-NE direction. Faults are situated between Kliete river and Rietavas town. Faults are identified in crystalline basement and penetrate the Lower Paleozoic sedimentary cover up to Lower Devonian Gragzdai Group (Early Pragian). They have been identified by 2D seismic and well data.
definition: Lūžiai yra orentuoti PV-ŠR kryptimi. Lūžiai yra išsidėstę tarp Klietės upės ir Rietavo miesto. Lūžiai išskiriami kristaliniame pamate ir nuosėdinėje dangoje iki apatinio devono Gargždų Serijos (ankstyvaisis Pragis). Lūžiai išskirti 2D seisminės žvalgybos ir gręžinių duomenimis. @lt
notation: LT-013
preferred label: Rietavo lūžių Sub-Domeinas @lt
references: https://data.geoscience.earth/ncl/geoera/ref/899
references: https://data.geoscience.earth/ncl/geoera/ref/900
in scheme: Tectonic Boundary Objects in Europe
broader: West Lithuanian Fault Domain

Gargzdai Fault Chain
type: Concept
created: 2020-05-25T08:59:46.029Z
definition: NNE-SSW striking Fault Chain consists of a set of reverse faults. The fault chain extend from Agluonenai village to Gargzdai town. It consists of major Gargzdai fault zone and related sattelite faults. The amplitudes range from a few dozen to 100 m. The NE-SW faults set shows rather simple compresional geometries dipping to the west at the angles 70-80o. Faults were identified by 2D and 3D seismic and well data. Faults are identified in crystalline basement and penetrate Lower Paleozoic sedimentary cover up to Lower Devonian Gragzdai Group (Early Pragian ).
definition: Lūžių grandinę sudaro antsprūdžio tipo lūžiai, orientuoti ŠŠR - PPV ir ŠR-PV kryptimis. Lūžiai yra išsidėstę nuo Agluonėnų gyvenvietės link Gargždų miesto. Lūžių grandinė vakaruose ribojasi su Baltijos jūra ir rytuose ribojasi su Veiviržo upe. Gargždų lūžių grandinę sudaro pagrindinė Gargždų lūžių zona ir kiti susiję lūžiai. Gargždų lūžių grandinę sudarančių lūžių amplitudė kinta nuo kelių dešimčių iki 100 metrų. Gargždų lūžių grandinės lūžiai nustatyti 2D ir 3D seisminės žvalgybos ir gręžinių duomenimis. Lūžiai išskiriami kristaliniame pamate ir nuosėdinėje dangoje iki apatinio devono Gargždų Serijos (ankstyvaisis Pragis). @lt
notation: LT-012
preferred label: Gargždų lūžių grandinė @lt
references: https://data.geoscience.earth/ncl/geoera/ref/901
references: https://data.geoscience.earth/ncl/geoera/ref/908
references: https://data.geoscience.earth/ncl/geoera/ref/904
references: https://data.geoscience.earth/ncl/geoera/ref/906
in scheme: Tectonic Boundary Objects in Europe
broader: West Lithuanian Fault Domain

East Lithuanian Fault Domain
type: Concept
created: 2020-05-25T08:59:46.112Z
definition: The East Lithuanian fault domain is dominated by alternation of distinct NNE-SSW and W-E trending faults' chains, coinciding with magnetic and gravity anomalies implying lenticular tectonic fabric of the basement rocks. The internal structure of the ELD is composed by a system of thrust-folds dipping to the west at low angles. East Lithuanian Fault Domain is located in eastern part of Lithuania. In the west from the fault domain there are Pasvalys town, Nevezis river, Kaunas city and Lazdijai town, in the east - Latvia and Belarus boundaries.
definition: Rytų Lietuvos lūžių domeiną sudaro ŠŠR-PPV ir V-R kryptimis besitęsiančios lūžių grandinės, išskirtos pagal gravitacines ir magnetines anomalijas, gerai atspindinčias kristalinio pamato lentikuliarinę tektoninę sandarą. Domeino vidinei sandarai būdinga antstūmių-raukšlių sistema, nedideliu kampu palinkusi vakarų kryptimi. Rytų Lietuvos lūžių domeinas yra rytinėje Lietuvos dalyje, jis vakaruose ribojasi su Pasvalio miestu, Nevėžio upe, Kauno miestu ir Lazdijų miestu, ir rytuose tęsiasi link Latvijos ir Baltarusijos sienų. @lt
notation: LT-002
preferred label: Rytų Lietuvos lūžių domeinas @lt
narrower: South-East Lithuanian Fault Chain
narrower: Zarasai-Polockas Fault system
narrower: Ignalina Fault Chain
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic boundary in Lithuania

South-East Lithuanian Fault Chain
type: Concept
created: 2020-05-25T08:59:46.140Z
definition: The fault chain consist of W-E and NNE-SSW oriented faults of the crystalline basement, identified by interpretation of the magnetic and gravity anomalies. The North-Western part of chain is located in vicinity of Kaunas city, the Eastern part - in vicinity of Vilnius city, and the Southern part - in vicinity of Druskininkai town.
definition: Pietryčių Lietuvos lūžių grandinę sudaro V- R ir ŠŠR- PPV tįsos kristalinio pamato lūžiai. Šiaurės vakaruose lūžių grandinės dalis ribojasi su Kauno miestu, rytuose - su Vilniaus miestu, o pietuose su Druskininkų miestu. Lūžiai išskirti gravitacinės ir magnetinės žvalgybos duomenimis. @lt
notation: LT-021
preferred label: Pietryčių Lietuvos lūžių grandinė @lt
narrower: W-E trending SubFaults
narrower: NNE-SSW trending SubFaults
references: https://data.geoscience.earth/ncl/geoera/ref/899
references: https://data.geoscience.earth/ncl/geoera/ref/900
in scheme: Tectonic Boundary Objects in Europe
broader: East Lithuanian Fault Domain

NNE-SSW trending SubFaults
type: Concept
created: 2020-05-25T08:59:46.195Z
definition: These NNE-SSW oriented faults of the crystalline basement are identified by interpretation of gravity and magnetic anomalies. In the North-West fault chain there is Kaunas city, in the East - Vilnius city and in the South - Druskininkai town.
definition: Lūžiai yra antsprūdžio tipo, orientuoti ŠŠR - PPV kryptimi, nustatyti gręžinių, gravitacinės ir magnetinės žvalgybos duomenimis. Šiaurės vakaruose lūžių grandinė ribojasi su Kauno miestu, rytuose su Vilniaus miestu ir pietuose su Druskininkų miestu. @lt
notation: LT-212
preferred label: ŠŠR - PPV krypties tįsos sub-lūžiai @lt
references: https://data.geoscience.earth/ncl/geoera/ref/899
references: https://data.geoscience.earth/ncl/geoera/ref/900
in scheme: Tectonic Boundary Objects in Europe
broader: South-East Lithuanian Fault Chain

W-E trending SubFaults
type: Concept
created: 2020-05-25T08:59:46.167Z
definition: These W-E oriented faults of the crystalline basement are identified by interpretation of the magnetic and gravity anomalies. The North-Western part of chain is located in vicinity of Kaunas city, the Eastern part - in vicinity of Vilnius city, and the Southern part - in vicinity of Druskininkai town.
definition: Lūžiai orientuoti V-R kryptimi, išskirti kritaliniame pamate gravitacinės ir magnetinės žvalgybos duomenimis. Šiaurės vakaruose lūžių grandinė ribojasi su Kauno miestu, rytuose su Vilniaus miestu ir pietuose su Druskininkų miestu. @lt
notation: LT-211
preferred label: V-R krypties tįsos sub-lūžiai @lt
references: https://data.geoscience.earth/ncl/geoera/ref/899
references: https://data.geoscience.earth/ncl/geoera/ref/900
in scheme: Tectonic Boundary Objects in Europe
broader: South-East Lithuanian Fault Chain

Ignalina Fault Chain
type: Concept
created: 2020-05-25T08:59:46.306Z
definition: Faults are oriented in SW-NE direction. They are reverse type faults, located around the Visaginas town. They have been identified with seismic survey data and by interpretation of gravity and magnetic anomalies and well data. The faults were identified in crystalline basement and penetrate Lower Paleozoic sedimentary cover.
definition: Ignalinos lūžių grandinės lūžiai yra PV- ŠR krypties, nustatyti aplink Visagino miestą. Šie lūžiai nustatyti seisminės žvalgybos, gravitacinės ir magnetinės žvalgybos ir gręžinių duomenimis. Lūžiai išskiriami kristaliniame pamate ir nuosėdinėje dangoje. @lt
notation: LT-023
preferred label: Ignalinos lūžių grandinė @lt
references: https://data.geoscience.earth/ncl/geoera/ref/902
in scheme: Tectonic Boundary Objects in Europe
broader: East Lithuanian Fault Domain

Zarasai-Polockas Fault system
type: Concept
created: 2020-05-25T08:59:46.223Z
definition: W-E trending fault system of the crystalline basement is identified by interpretation of the magnetic and gravity anomalies. Fault system is in the Northeast Lithuania, between Zarasai, Panevezys, Ramygala and Ignalina towns.
definition: V-R kryptimi orientuoti kristalinio pamato lūžiai, nustatyti gravitacinės ir magnetinės žvalgybos duomenimis. Lūžių sistema yra šiaurės rytinėje Lietuvos dalyje, tarp Zarasų, Panevėžio, Ramygalos ir Ignalinos miestų. @lt
notation: LT-022
preferred label: Zarasų-Polocko lūžių sistema @lt
narrower: Zarasai Fault
narrower: Polockas Fault
references: https://data.geoscience.earth/ncl/geoera/ref/905
references: https://data.geoscience.earth/ncl/geoera/ref/903
references: https://data.geoscience.earth/ncl/geoera/ref/902
in scheme: Tectonic Boundary Objects in Europe
broader: East Lithuanian Fault Domain

Polockas Fault
type: Concept
created: 2020-05-25T08:59:46.279Z
definition: Polockas fault is oriented in W-E direction and identified as share zone, inclined to the north at the angle 25o. The dislocation amplitude at crystaline basement is up to 50 m. Polockas fault strikes from Ramygala town to the Ignalina town and continues to Belarus. The fault has been identified by interpretation of the magnetic and gravity anomalies.
definition: Polocko lūžis yra V-R krypties, antsprūdžio tipo, pasviręs į šiaurę 25o laipsnių kampu. Kristaliniame pamate dislokacijų amplitudė siekia 50 metrų. Šis lūžis trasuojamas nuo Ramygalos miesto, pro Ignalinos miestą link Baltarusijos teritorijos. Lūžis nustatytas gravitacinės ir magnetinės žvalgybos ir gręžinių duomenimis. @lt
notation: LT-222
preferred label: Polocko lūžis @lt
references: https://data.geoscience.earth/ncl/geoera/ref/903
in scheme: Tectonic Boundary Objects in Europe
broader: Zarasai-Polockas Fault system

Zarasai Fault
type: Concept
created: 2020-05-25T08:59:46.251Z
definition: Fault in the crystalline basement is oriented in W-E direction. It is nearly vertical. The strike-slip movements are preferred along the fault. It strikes from the city of Panevezys to the Zarasai town and continues to Latvia. The fault has been identified by interpretation of gravity and magnetic anomalies.
definition: Lūžiai orientuoti V-R kryptimi, išskirti kritaliniame pamate. Jis tęsiasi nuo Panevėžio miesto pro Zarasų miestą link Latvijos teritorijos. Lūžis nustatytas gravitacinės ir magnetinės žvalgybos duomenimis. @lt
notation: LT-221
preferred label: Zarasų lūžis @lt
references: https://data.geoscience.earth/ncl/geoera/ref/905
references: https://data.geoscience.earth/ncl/geoera/ref/902
in scheme: Tectonic Boundary Objects in Europe
broader: Zarasai-Polockas Fault system

Mid-Lithuanian Share Zone
type: Concept
created: 2020-05-25T08:59:46.334Z
definition: The first-order tectonic element of the crystalline basement is the N-S trending Middle Lithuanian share zone separating Western Lithuanian domain and East Lithuanian Domain, it also marks a considerable offset of the Moho (amplitude ~10 km). Middle Lithuanian share zone extends from Lazdijai town, through Kaunas and Panevezys cities to Joniskis town.
definition: Tai stambiausio rango kristalinio pamato tektoninių šlyties deformacijų zona, skirianti Rytų ir Vakarų Lietuvos domeinus. Zona stebima ir Moho paviršiaus deformacijomis (iki 10 km amplitudės). Ši zona yra vidurio Lietuvoje ir tęsiasi šiaurės-pietų kryptimi. Vidurio Lietuvos šlyties zona tęsiasi nuo Lazdijų miesto, per Kauno ir Panevėžio miestus link Joniškio miesto. @lt
notation: LT-003
preferred label: Vidurio Lietuvos šlyties deformacijų zona @lt
narrower: Vaskai Fault
narrower: Zaltiniai Fault Chain
references: https://data.geoscience.earth/ncl/geoera/ref/903
references: https://data.geoscience.earth/ncl/geoera/ref/905
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic boundary in Lithuania

Zaltiniai Fault Chain
type: Concept
created: 2020-05-25T08:59:46.389Z
definition: Faults are oriented in E-W and NW-SE directions. Faults strike to the South and South-East from Sakiai town. They have been identified by 2D siesmic data and by interpretation of the magnetic and gravity anomalies and well data. These faults are reverse type.
definition: Lūžiai orentuoti R-V ir ŠV-PR kryptimis. Žaltinių lūžių grandinę sudarantys lūžiai trasuojami pietuose - pietryčiuose nuo Šakių miesto. Jie nustatyti 2D seisminės žvalgybos, gravitacinės ir magnetinės žvalgybos ir gręžinių duomenimis. Šie lūžiai yra antsprūdžio tipo. @lt
notation: LT-032
preferred label: Žaltinių lūžių grandinė @lt
references: https://data.geoscience.earth/ncl/geoera/ref/899
references: https://data.geoscience.earth/ncl/geoera/ref/900
in scheme: Tectonic Boundary Objects in Europe
broader: Mid-Lithuanian Share Zone

Vaskai Fault
type: Concept
created: 2020-05-25T08:59:46.361Z
definition: Vaskai fault is oriented in SW-NE direction, it is identified in the crystalline basement and penetrates the entire Devonian strata with an amplitude up to 25 m. Some segments of fault were identified by 2D seismic survey data, some - by gravity and magnetic survey and well data. Fault strikes from Pakruojis town, through Birzai town and continues to Latvia teritory.
definition: Vaškų lūžis yra PV-ŠR krypties ir transuoja nuo Pakruojo miesto, pro Biržų miestą link Latvijos teritorijos . Šie lūžiai yra antsprūdžio tipo. Dalis šių lūžių yra nustatyta seisminės žvalgybos duomenimis, kita dalis - gręžinių, gravitacinės ir magnetinės žvalgybos duomenimis. @lt
notation: LT-031
preferred label: Vaškų lūžis @lt
references: https://data.geoscience.earth/ncl/geoera/ref/907
in scheme: Tectonic Boundary Objects in Europe
broader: Mid-Lithuanian Share Zone

Tectonic Boundary in Saxony-Anhalt
scope note: All named tectonic boundary objects that are located (at least partly) in Saxony-Anhalt, are identified by an ID with the prefix „DE-ST“ listed in the notation. Fault systems and/or fault domains can cross political borders and are therefore shared by several countries. Therefore, they can contain faults from different countries, indicated by country-specific prefixes to the respective ID. In addition, as the concepts are also located in Germany, they may have an additional ID in form of „DE“ referring to a national Germany-wide dataset.
definition: Representation of an interpreted tectonic boundary in Saxony-Anhalt as displayed in the HIKE European fault database
type: Concept
top concept of: Tectonic Boundary Objects in Europe
created: 2021-03-03T16:08:14.944Z
notation: DE-ST-0
definition: Repräsentation einer interpretierten tektonischen Grenzfläche in Sachsen-Anhalt. @de
preferred label: Tektonische Grenzfläche in Sachsen-Anhalt @de
narrower: Fault zone of the Altmark area
narrower: Fault zones of the Calvörde Block
narrower: Fault zones of the Flechtingen High
narrower: Fault zones of the Subhercynian Basin
narrower: Fault zones of the Thuringian Basin
in scheme: Tectonic Boundary Objects in Europe

Fault zones of the Calvörde Block
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
type: Concept
created: 2021-03-03T16:08:15.148Z
notation: DE-ST-2000
definition: The Calvörde Block in the south and southwest of the Altmark area forms a basement uplift of Late Cretaceous age. It is covered by older Mesozoic rocks (Triassic), which were uplifted and folded in a flexure above a large basement fault, the Gardelegen Fault, respectively. To the south the Haldensleben and Wittenberg Fault zones separate the Calvörde Block against the Flechtingen High.
definition: Die Scholle von Calvörde im Süden und Südwesten der Altmark bildet eine Sockelerhebung, die sich in der späten Kreidezeit heraushob. Sie ist von älteren mesozoischen Gesteinen (Trias) bedeckt, die in einer Flexur über einer großen Sockelstörung, der Gardelegen-Überschiebung, emporgehoben und gefaltet wurden. Im Süden trennen die Haldensleben und Wittenberg Überschiebungen den Calvörde-Block vom Flechtinger Höhenzug. @de
preferred label: Störungszonen der Scholle von Calvörde @de
narrower: Gardelegen Fault Zone
narrower: Dannefeld Fault Zone
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Saxony-Anhalt

Dannefeld Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
type: Concept
created: 2021-03-03T16:08:15.157Z
notation: DE-ST-35
definition: The Dannefeld fault zone forms a reverse reactivated normal fault in Permian to Mesozoic strata of the western Calvörde Block. Activity along the Dannefeld fault zone was strongly associated with halokinetic movements in the Zechstein salt thus resulting in the formation of the Dannefeld diapir.
definition: Die Dannefeld-Verwerfungszone bildet eine revers-reaktivierte Abschiebung in der permischen bis mesozoischen Schichtenfolge der Scholle von Calvörde. Die Aktivität entlang der Dannefeld Störungszone war stark mit halokinetischen Bewegungen im Zechstein-Salz verbunden, was zur Bildung des Dannefeld Diapirs führte. @de
preferred label: Dannefeld-Störungszone @de
alternative label: Dannefeld Fault
narrower: Crestal Graben of the Dannefeld salt structure
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Calvörde Block

Crestal Graben of the Dannefeld salt structure
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-03-03T16:08:15.161Z
notation: DE-ST-73
definition: The Scheitelgraben Dannefeld forms a collaps structure on top of the Dannefeld diapir.
definition: Der Scheitelgraben Dannefeld bildet eine Einbruchstruktur im Dachbereich des Salzstocks Dannefeld. @de
preferred label: Scheitelgraben der Salzstruktur Dannefeld @de
broader: Dannefeld Fault Zone

Gardelegen Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8105
references: https://data.geoscience.earth/ncl/geoera/ref/8068
references: https://data.geoscience.earth/ncl/geoera/ref/7994
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:15.152Z
notation: DE-ST-22
definition: The NW-SE-striking and SW-dipping, 50 km long Gardelegen fault is one of the most important basement thrusts (‘Central German Main Escarpments’). While a maximum vertical displacement of 3.5 km (corresponding to 5 km fault offset) is detectable at the Base Zechstein horizon, fault offsets in the sedimentary cover (Top Zechstein) are low (< 200 m) and deformation is substituted by flexural folding. These huge offset variations furthermore coincide with thickness variations of the Zechstein salt across the Gardelegen fault. That observation indicates that salt migrated from the hanging wall to the footwall, which may was associated with thrusting and folding equivalent to ‘trishear’ fault-propagation folding (Erslev, 1991; Hardy and Ford, 1997). In the west, the fault zone abruptly starts with large offsets. A 10 km wide, long-wavelength foreland syncline comprises a uniform basin fill of Early Triassic-Late Jurassic strata overlain by a thick Late Cretaceous (Coniacian to Santonian) succession. Farther east, Late Jurassic-Early Cretaceous strata is absent and the foreland syncline became narrower. Fault offsets slightly decrease, where the fault trace converges towards the Haldensleben fault in a complex ‘en echelon’ pattern of fault zones (Brehm fault and Burg-Reuden-fault).
definition: Die NW-SE-streichende und SW-einfallende, 50 km lange Gardelegen-Überschiebung ist eine der wichtigsten Sockel-Überschiebungen („Mitteldeutsche Hauptabbrüche“) Mitteldeutschlands. Während die Basis Zechstein bis zu 3,5 km relativ zum nördlichen Vorland gehoben ist (entspricht ca. 5 km Störungsversatz), sind Versätze in den mesozoischen Einheiten relativ gering (<200 m) und durch eine großräumige Flexur vertreten. Diese enormen Versatzvariationen gehen mit Mächtigkeitsschwankungen der Zechstein-Salze über die Gardelegen-Überschiebung einher. Diese Beobachtung deutet darauf hin, dass Salz vom Hangenden zum Liegenden migrierte. Im Westen beginnt die Verwerfungszone abrupt mit großen Versatzbeträgen. Eine 10 km breite, langwellige Mulde im Vorland zeigt einheitliche Beckensedimente der frühen Trias bis zum späten Jura. Diese werden einer mächtigen Abfolge der spätkretazischer Sedimente (Coniacian bis Santonian) überlagert. Weiter östlich fehlen Schichten des späten Jura und der frühen Kreide und die Vorland-Mulde wird deutlich kurzwelliger. Die Störungsversätze nehmen leicht ab, wobei die Störungsspur in einem komplexen „en echelon“-Muster von Einzelstörungen (Brehm Störungszone und Burg-Reuden Störungszone) gegen die Haldensleben Überschiebung konvergiert. @de
preferred label: Gardelegen-Überschiebung @de
alternative label: Gardelegen Thrust
alternative label: Abbruch von Gardelegen @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Calvörde Block

Fault zones of the Subhercynian Basin
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:15.183Z
notation: DE-ST-4000
definition: The Subhercynian Depression is that area of Saxony-Anhalt, which is located between the basement uplifts of the Flechtingen High and the Harz Mountains. To the north (Flechtingen High) its border forms the mostly continuous transition from Mesozoic and Late Palaeozoic (Zechstein) strata to Palaeozoic crystalline and sedimentary rocks of the Flechtingen High. To the south the northern border fault of the Harz Mountains and steep-dipping Zechstein strata associated with basement faulting form the structural border of the Subhercynian Depression. The internal structure of the Subhercynian Depression is mostly characterized by NW-SE-trending fault zones, which are in parts accompanied with the intrusion of mechanically weak (Zechstein) salt (e.g. salt structure ‘Oberes Allertal’, ‘Offleben-Oschersleben-Staßfurter Salzsattel’), local thin-skinned anticlines (e.g., ‘Quedlinburger Sattel’, long-wavelength fault-related folds and deep synclines. Although the entire Subhercynian Depression underwent uplift in Late Mesozoic to Cenozoic times, relicts of older (Mesozoic) strata indicate a similar structural evolution like in the Altmark area further north. The Subhercynian Depression can be subdivided into several smaller blocks [Martiklos et al., 2001.]
definition: Das Subherzyne Becken ist eine geologische Großstruktur im Gebiet von Sachsen-Anhalt, das sich zwischen den Sockelaufbrüchen des Flechtinger Höhenzugs im Norden und des Harzes im Süden befindet. Im Norden ist seine Grenze meist durch den gering versetzten, kontinuierlichen Übergang von Schichten des Mesozoikums und des späten Paläozoikums (Zechstein) zu kristallinen und sedimentären Gesteinen des Paläozoikums des Flechtinger Höhenzugs definiert. Im Süden bildet die Harznordrandstörung und die mit ihr assoziierten steil einfallenden Permotriassischen Schichten die strukturelle Grenze des Subherzynen Beckens. Die innere Struktur des Subherzynen Beckens ist hauptsächlich durch NW-SE-streichende Störungszonen charakterisiert, die teilweise mit dem Aufstieg von mechanisch weichen Einheiten, den Zechstein-Salzen einhergehen (z. B. Salzstruktur 'Oberes Allertal', 'Offleben-Oschersleben-Staßfurter Salzsattel'). Lokal existieren enge Detachment Faulten (z. B.' Quedlinburger Sattel ', langwellige störungsbedingte Falten und tiefe Synklinalen). Obwohl das gesamte Subherzyne Becken im späten Mesozoikum bis ins Känozoikum emporgehoben wurde, weisen Relikte älterer (mesozoischer) Schichten auf eine ähnliche strukturelle Entwicklung wie im weiter nördlich gelegenen Altmark-Gebiet hin. @de
preferred label: Störungszonen des Subherzynen Beckens @de
narrower: Allertal Fault Zone
narrower: Schönebeck Graben
narrower: Bernburg Graben
narrower: Paschleben Fault Zone
narrower: Oschersleben-Staßfurt Fault Zone
narrower: Large Graben Fault
narrower: Fallstein-Huy-Hakel Structure
narrower: Halberstadt Fault Zone
narrower: Aschersleben Fault Zone
narrower: Westerhausen Fault Zone
narrower: Harz Northern Border Fault
narrower: Gröbzig Fault Zone
narrower: Athensleben Fault Zone
narrower: Hohenerxleben Fault Zone
narrower: Grimschleben-Roschwitz Fault Zone
narrower: Köthen-Bitterfeld Fault Zone
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Saxony-Anhalt

Westerhausen Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:15.266Z
notation: DE-ST-200
definition: The Westerhausen fault zone forms an major basement fault in the western Subhercynian Basin, which is associated with strong halokinetic movements.
definition: Die Westerhausen Störung bildet eine bedeutende Sockelstruktur im westlichen Subherzynen Becken, die mit bedeutenden halokinetischen Bewegungen einherging. @de
preferred label: Westerhausen-Störungszone @de
alternative label: Westerhausen Fault
narrower: Vienenburg-Schauen Fault Zone
narrower: Quedlinburg Fault Zone
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Subhercynian Basin

Quedlinburg Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:15.275Z
notation: DE-ST-55
definition: The Quedlinburg Fault Zone forms a NW-SE-striking anticline in the eastern part of the Subhercynian Basin. It separates the Halberstadt and Blankenburg Synclines against each other.
definition: Der Quedlinburger Störungszone bildet eine NW-SE-streichende Antiklinalstruktur im östlichen Subherzynen Becken. Die abgescherte Antiklinalstrukture separiert die Halberstädter und Blankenburger Mulde gegeneinander. @de
preferred label: Quedlinburger Störungszone @de
alternative label: Quedlinburg Fault
alternative label: Quedlinburger Sattel @de
in scheme: Tectonic Boundary Objects in Europe
broader: Westerhausen Fault Zone

Vienenburg-Schauen Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:15.270Z
notation: DE-ST-54
definition: The Vienenburg-Schauen fault zone is a thin-skinned thrust fault and forms the western part of the Westerhausen fault zone.
definition: Die Vienenburg-Schauen Störungszone ist eine abgescherte Überschiebungsstruktur und bildet den westlichen Abschnitt der Westerhausen Störungszone. @de
preferred label: Vienenburg-Schauen-Störungszone @de
alternative label: Harli-Störungszone @de
in scheme: Tectonic Boundary Objects in Europe
broader: Westerhausen Fault Zone

Aschersleben Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/7989
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:15.261Z
notation: DE-ST-53
definition: The Aschersleben fault forms a NW-SE trending basement fault accompanied by halokinesis. The northern basement block is raised approx. 1 km compared to the southern one. In the uppermost crest of the structure halokinetic structures (Aschersleben salt structure) occur, which are accompanied with subrosion sinks, some of which filled with thick tertiary sediments.
definition: Die Ascherslebener Störung bildet eine markante NW-SE streichende, durch Halokinese begleitete Sockelstörung. Der nördliche Sockelblock ist gegenüber dem südlichen markant um ca. 1 km angeboben. Im Dachbereich der Struktur treten vermehrt halokinetische Strukturen (Ascherslebener Salzsattel) und Subrosionssenken auf, die zum Teil mit mächtigen tertiären Sedimenten gefüllt sind. @de
preferred label: Ascherslebener-Störungszone @de
alternative label: Aschersleben Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Subhercynian Basin

Schönebeck Graben
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:15.206Z
notation: DE-ST-44
definition: The Schönebeck Graben forms an extensional fault zone on the Weferlingen Block.
definition: Der Schönebecker Graben bildet eine extensionale Störungszone im Bereich der Weferlinger Scholle. @de
preferred label: Schönebecker Graben @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Subhercynian Basin

Halberstadt Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8114
references: https://data.geoscience.earth/ncl/geoera/ref/8103
references: https://data.geoscience.earth/ncl/geoera/ref/8052
references: https://data.geoscience.earth/ncl/geoera/ref/8040
type: Concept
created: 2021-03-03T16:08:15.256Z
notation: DE-ST-52
definition: The Halberstadt fault zone forms a NW-SE trending fault zone in the Subhercynian Basin, which separates the central basin area from the deep synkinematic Cretaceous synclines of the Harz foreland.
definition: Die Halberstadt Störungszone bildet eine NW-SE streichende Störungszone im Subherzynen Becken, die den zentralen Beckenbereich von den tiefen synkinematischen Kreidemulden des direkten Harzvorlandes trennt. @de
preferred label: Halberstadt-Störung @de
alternative label: Halberstadt Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Subhercynian Basin

Köthen-Bitterfeld Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:15.307Z
notation: DE-ST-300
definition: The Köthen-Bitterfeld fault zone forms a NW-SE trending fault zone in the central area of the Halle-Wittenberg Block.
definition: Die Köthen-Bitterfeld Störungszone bildet eine NW-SE streichende Störungszone im Zentralbereich der Halle-Wittenberg Scholle. @de
preferred label: Köthen-Bitterfeld-Störungszone @de
alternative label: Köthen-Bitterfeld Fault
narrower: Bitterfeld Fault Zone
narrower: Zörbig Fault Zone
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Subhercynian Basin

Zörbig Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:15.316Z
notation: DE-ST-88
definition: The Zörbig fault zone forms a NW-SE trending fault zone in the border area of the Halle-Wittenberg Block.
definition: Die Zörbiger Störungszone bildet eine NW-SE streichende Störungszone im Grenzbereich der Halle-Wittenberg-Scholle. @de
preferred label: Zörbiger Störungszone @de
alternative label: Zörbig Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Köthen-Bitterfeld Fault Zone

Bitterfeld Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:15.312Z
notation: DE-ST-87
definition: The Bitterfeld fault zone forms a NW-SE trending fault zone in the border area of the Halle-Wittenberg Block. It forms the southeastern part of the Köthen-Bitterfeld fault zone.
definition: Die Bitterfeld Störungszone bildet eine NW-SE streichende Störungszone im Grenzbereich der Halle-Wittenberg-Scholle. Sie bildet das südöstliche Teilglied der Köthen-Bitterfelder Störungszone. @de
preferred label: Bitterfelder Störungszone @de
alternative label: Bitterfeld Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Köthen-Bitterfeld Fault Zone

Grimschleben-Roschwitz Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:15.301Z
notation: DE-ST-81
definition: The Grimschleben-Roschwitz fault zone is a NE-SW to north-south trending fault zone in the southeastern Subhercynian Basin.
definition: Die Grimschleben-Roschwitz Störungszone ist eine NE-SW bis nahezu Nord-Süd streichende Störungszone im südöstlichen Subherzynen Becken. @de
preferred label: Grimschleben-Roschwitz-Störungszone @de
alternative label: Grimschleben-Roschwitz Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Subhercynian Basin

Allertal Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/7995
references: https://data.geoscience.earth/ncl/geoera/ref/8107
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:15.188Z
notation: DE-ST-42
definition: The Allertal Fault separates the Weferlingen Block in the north to the Lappwald Block in the south. Although fault kinematics of the Allertal Fault are still matter of debate [Best and Zirngast, 2000; Stottmeister et al., 1998], it can be summarized to form a Late Triassic/Late Jurassic-Early Cretaceous high-offset (> 2.5 km) normal fault, which probably formed as an extensional detachment fault and later underwent mild contraction and inversion.
definition: Die Allertalstörung trennt den Weferlingen Block im Norden vom Lappwald Block im Süden. Obwohl die Störungskinematik der Allertalstörungszone immer noch umstritten ist [Best und Zirngast, 2000; Stottmeister et al., 1998], kann zusammengefasst werden, dass diese als flache Abschiebung mit hohem Versatz (> 2,5 km) während der späten Trias und der späten Jura-frühen Kreidezeit ausgebildet wurde. Während der späten Kreide erfuhr sie eine schwache Einengung und Reaktivierung als Aufschiebung. @de
preferred label: Allertal-Störungszone @de
alternative label: Allertal Fault
alternative label: Störungszone Oberes Allertal @de
narrower: Crestal Graben of the Allertal salt structure
narrower: Ummendorf Graben
narrower: Ummendorf-Allertal Fault Zone
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Subhercynian Basin

Ummendorf-Allertal Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
references: https://data.geoscience.earth/ncl/geoera/ref/8071
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-03-03T16:08:15.201Z
notation: DE-ST-43
definition: The Ummendorf-Allertal fault zone forms a E-W-trending extensional fault zone on the Weferlingen Block.
definition: Die Ummendorf-Allertal Störungszone bildet eine Ost-West-streichende Grabenstruktur im Bereich der Weferlinger Scholle. @de
preferred label: Ummendorf-Allertal-Störungszone @de
broader: Allertal Fault Zone

Ummendorf Graben
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
references: https://data.geoscience.earth/ncl/geoera/ref/8071
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-03-03T16:08:15.197Z
notation: DE-ST-76
definition: The Ummendorf Graben forms a collaps structure on the top of the Allertal salt structure.
definition: Der Ummendorfer Graben bildet eine Einbruchstruktur über der Salzstruktur Allertal. @de
preferred label: Ummendorfer Graben @de
broader: Allertal Fault Zone

Crestal Graben of the Allertal salt structure
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
references: https://data.geoscience.earth/ncl/geoera/ref/8071
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-03-03T16:08:15.193Z
notation: DE-ST-75
definition: The Scheitelgraben Allertal forms a collaps structure on top of the Allertal salt structure.
definition: Der Scheitelgraben Allertal bildet eine Einbruchstruktur im Dachbereich der Allertal Salzstruktur. @de
preferred label: Scheitelgraben der Allertal Salzstruktur @de
broader: Allertal Fault Zone

Fallstein-Huy-Hakel Structure
references: https://data.geoscience.earth/ncl/geoera/ref/7989
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:15.237Z
notation: DE-ST-100
definition: The Fallstein-Huy-Hakel structure is an anticline in the Mesozoic strata of the Subhercynian Basin. It is associated with major reverse basement faults and associated flexures in the Mesozoic cover.
definition: Der Fallstein-Huy-Hakel-Strukturzug bildet eine markante Antiklinale in der mesozoischen Schichtenfolge des Subherzynen Beckens. Diese ist an bedeutende Sockelstörungen gebunden, während in der mesozoischen Abfolge überwiegend flexurelle Falten auftreten. @de
preferred label: Fallstein-Huy-Hakel Störungszone @de
narrower: Fallstein Northern Border Fault
narrower: Fallstein Southern Border Fault
narrower: Huy Fault Zone
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Subhercynian Basin

Huy Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
references: https://data.geoscience.earth/ncl/geoera/ref/7989
type: Concept
created: 2021-03-03T16:08:15.251Z
notation: DE-ST-51
definition: The Huy Fault Zone forms an important basement fault of the Fallstein-Huy-Hakel structure in the Subhercynian Basin.
definition: Die Huy Störung bildet eine markante Störungszone des des Fallstein-Huy-Hakel-Strukturzugs. @de
preferred label: Huy-Störungszone @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fallstein-Huy-Hakel Structure

Fallstein Southern Border Fault
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
references: https://data.geoscience.earth/ncl/geoera/ref/7989
type: Concept
created: 2021-03-03T16:08:15.247Z
notation: DE-ST-50
definition: The Fallstein Soutehrn Boundary Fault forms the soutern boundary fault of the Fallstein structure.
definition: Die Fallstein-Südrand-Störung bildet die südliche Sockelstörung des Fallstein-Huy-Hakel-Strukturzugs. @de
preferred label: Fallstein-Südrandstörung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fallstein-Huy-Hakel Structure

Fallstein Northern Border Fault
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
references: https://data.geoscience.earth/ncl/geoera/ref/7989
type: Concept
created: 2021-03-03T16:08:15.242Z
notation: DE-ST-49
definition: The Fallstein Northern Boundary Fault forms the northern boundary fault of the Fallstein structure.
definition: Die Fallstein-Nordrand-Störung bildet die nördliche Sockelstörung des Fallstein-Huy-Hakel-Strukturzugs. @de
preferred label: Fallstein-Nordrandstörung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fallstein-Huy-Hakel Structure

Large Graben Fault
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
type: Concept
created: 2021-03-03T16:08:15.232Z
notation: DE-ST-48
definition: The Großer Graben fault zone is a E-W-trending fault zone at the state borders between Lower Saxony and Saxony-Anhalt. Although only poorly explored, the fault zone might be associated with major tectonic movements during Triassic times as proved by strongly variating thicknesses of Triassic strata.
definition: Die Großer Graben Störungszone ist eine E-W-streichende Verwerfungszone an der Landesgrenze zwischen Niedersachsen und Sachsen-Anhalt. Obwohl nur gering untersucht, steht die Verwerfungszone möglicherweise mit bedeutenden tektonischen Bewegungen während der Trias in Verbindung, die entlang des Westrandes des Subherzynen Beckens stattfanden. @de
preferred label: Großer Graben Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Subhercynian Basin

Oschersleben-Staßfurt Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/7989
references: https://data.geoscience.earth/ncl/geoera/ref/8071
references: https://data.geoscience.earth/ncl/geoera/ref/8052
type: Concept
created: 2021-03-03T16:08:15.220Z
notation: DE-ST-47
definition: The Oschersleben-Staßfurt fault zone forms is a basement fault associated with the Offleben-Oschersleben-Staßfurt Salzsattel. It forms the border between the Lappwald Block in the north and the Central Subhercynian Depression.
definition: Die Oschersleben-Staßfurt Störungszone ist eine Sockelstörung, die im Zusammenhang mit dem Offleben-Oschersleben-Staßfurt-Salzsattel steht. Sie bildet die Grenze zwischen dem Lappwaldblock im Norden und dem zentralen Subherzynen Becken. @de
preferred label: Oschersleben-Staßfurter-Störungszone @de
narrower: Offleben Fault
narrower: Güsten Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Subhercynian Basin

Güsten Fault
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
type: Concept
created: 2021-03-03T16:08:15.228Z
notation: DE-ST-78
definition: The Güsten fault zone is one part of the Oschersleben-Staßfurt Fault zone in the central part of the Subhercynian Basin. It is associated with strong halokinetic movements und huge subsidence during Cenozoic times.
definition: Die Güsten Störungszone bildet einen Teil der Oschersleben-Staßfurter Störungszone im zentralen Subherzynen Becken. Ihre Aktivität ist von ausgeprägten halokinetischen Bewegungen und starker Subsidenz während des Känozoikums begleitet. @de
preferred label: Güstener Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Oschersleben-Staßfurt Fault Zone

Offleben Fault
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
type: Concept
created: 2021-03-03T16:08:15.224Z
notation: DE-ST-77
definition: The Offleben Fault Zone is one part of the Oschersleben-Staßfurt Fault zone in the westernmost Subhercynian Basin.
definition: Die Offleben Störungszone bildet einen Teilabschnitt der Oschersleben-Staßfurter Störungszone im westlichen Subherzynen Becken. @de
preferred label: Offlebener Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Oschersleben-Staßfurt Fault Zone

Paschleben Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/7989
references: https://data.geoscience.earth/ncl/geoera/ref/8071
references: https://data.geoscience.earth/ncl/geoera/ref/8052
type: Concept
created: 2021-03-03T16:08:15.215Z
notation: DE-ST-46
definition: The Paschleben fault zone is a NW-SE-trending fault zone, which separates the Paleozoic strata of the Paschleben anticline against the Mesozoic strata of the Subhercynian Basin.
definition: Die Paschlebener Vorsprung Störungszone ist eine NW-SE-streichende Störungszone, die die Paläozoischen Einheiten des Paschlebener Vorsprungs gegen die mesozoischen Einheiten des Subherzynen Beckens abgrenzt. @de
preferred label: Paschlebener Störungszone @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Subhercynian Basin

Bernburg Graben
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:15.210Z
notation: DE-ST-45
definition: The Bernburg Graben forms an extensional fault zone in the east of the Offleben-Oschersleben-Staßfurter Salzsattel.
definition: Der Bernburg Graben bildet eine extensionale Störungszone im Osten des Offleben-Oschersleben-Staßfurter Salzsattels. @de
preferred label: Bernburger Graben @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Subhercynian Basin

Hohenerxleben Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:15.297Z
notation: DE-ST-80
definition: The Hohenerxleben fault zone is a NNE-SSW trending fault zone in the eastern Subhercynian Basin. It limits the Egelner salt structure in the southeast.
definition: Die Hohenerxlebener Störungszone ist eine NNE-SSW streichende, Störungszone im östlichen Subherzynen Becken. Sie begrenzt den Egelner Sattel im Südosten. @de
preferred label: Hohenerxleben-Störungszone @de
alternative label: Hohenerxleben Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Subhercynian Basin

Athensleben Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:15.292Z
notation: DE-ST-79
definition: The Athensleben fault zone is a NNE-SSW trending fault zone that crosses the NW-SE trending main faults of the Subhercynian Basin.
definition: Die Athenslebener Störungszone ist eine NNE-SSW streichende Störungszone, die die NW-SE-streichenden Hauptstörungen des Subherzynen Beckens quert. @de
preferred label: Athensleben-Störung @de
alternative label: Athensleben Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Subhercynian Basin

Gröbzig Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:15.284Z
notation: DE-ST-57
definition: The Gröbzig fault zone is a SW-NE trending fault in the northwestern part of the Halle-Wittenberg Block postulated in particular on the basis of gravity measurements.
definition: Die Gröbziger Störung ist eine insbesondere auf der Grundlage gravimetrischer Messungen postulierte SW-NE streichende Störung im nordwestlichen Randbereich der Halle-Wittenberg-Scholle. @de
preferred label: Gröbziger Störungszone @de
alternative label: Gröbzig Fault
narrower: Alsleben-Gröbziger Fault Zone
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Subhercynian Basin

Alsleben-Gröbziger Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:15.288Z
notation: DE-ST-85
definition: The Alsleben-Gröbziger Fault Zone is part of the Gröbzig Fault Zone.
definition: Die Alsleben-Gröbziger Störungszone bildet eine Teilstruktur der Gröbziger Störungszone. @de
preferred label: Alsleben-Gröbzig-Störungszone @de
in scheme: Tectonic Boundary Objects in Europe
broader: Gröbzig Fault Zone

Harz Northern Border Fault
references: https://data.geoscience.earth/ncl/geoera/ref/8103
references: https://data.geoscience.earth/ncl/geoera/ref/8119
references: https://data.geoscience.earth/ncl/geoera/ref/8120
references: https://data.geoscience.earth/ncl/geoera/ref/8104
type: Concept
created: 2021-03-03T16:08:15.279Z
notation: DE-ST-56
definition: The Harz Northern Boundary Fault forms a NW-SE-trending fault zone structure that plunges to a depth of approx. 1000 m at an average dip of 60 degrees. Different offset values between 3000 m and up to 7000 m are given. The depth range is estimated to be 10-12 km, according to gravimetric indications even up to 30 km. Their first activity was probably Variscan, perhaps even pre-Variscan. Today's structur is mainly the result of multiphase post-variscan activities. During the Latest Cretaceous, the Harz Mountains were raised and their frontal thrust on their foreland was at least 2-3 km in a north-north-east direction.
definition: Die Harz-Nordrandstörung bildet eine NW-SE-streichende und bis zu einer Teufe von ca. 1000 m mit durchschnittlich 60° oder steiler nach Süden einfallende, im Wesentlichen aus drei jeweils in das Harzpaläozoikum hineinlaufenden Teilstörungen zusammengesetzte Bruchstruktur. Als Versetzungsbetrag werden unterschiedliche Werte zwischen 3000 m und bis zu 7000 m angegeben, die Tiefenreichweite soll schätzungsweise 10-12 km, nach gravimetrischen Indikationen sogar bis 30 km betragen. Ihre Anlage erfolgte wahrscheinlich variszisch, vielleicht auch schon prävariszisch. Das heutige Strukturbild ist hauptsächlich Ergebnis mehrphasiger postvariszischer Aktivierungen. Während der späten Kreide erfolgte die Heraushebung des Harzes sowie deren Nordnordost gerichtete, mindestens 2-3 km betragende frontale Überschiebung auf ihr Vorland. @de
preferred label: Harznordrandstörung @de
alternative label: Harz Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Subhercynian Basin

Fault zones of the Flechtingen High
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
references: https://data.geoscience.earth/ncl/geoera/ref/8105
definition: The Flechtingen High, often referred to as the Flechtingen-Rosslau Block, forms the approx. 100 km long and 20 km wide, NW-SE trending surface outcrop of Palaeozoic rocks in central Saxony-Anhalt. In wide areas Cenozoic strata cover that basement block. The outcropping rocks were low-grade metamorphic, moderately deformed foreland sediments of the Rhenohercynian Zone as well as high-grade metamorphic and intrusive rocks in the Mid-German-Crystalline Rise. They are widely covered by Late Carboniferous to Early Permian sedimentary rocks. After the Variscan orogeny, the border faults of the Flechtingen High evolved as large dextral strike-slip faults forming the southern Elbe Zone, a crustal-scale wrench system ranging from the Bohemian Massif in the southeast to the North Sea in the northwest. It is supposed that sedimentary rocks of the Central European Basin System covered the Flechtingen High during Mesozoic times. The border faults, i.e. parts of the Elbe Zone, were probably reactivated under extension during the Jurassic to Early Cretaceous. Late Cretaceous contraction lead to the uplift of the Flechtingen High and probably affected later large-scale crustal movements as revealed by the distribution of Cenozoic strata [Stackebrandt, 1986].
type: Concept
created: 2021-03-03T16:08:15.165Z
notation: DE-ST-3000
definition: Der Flechtingen Höhenzug, oft als Flechtingen-Rosslau-Scholle bezeichnet, bildet einen rd. 100 km lange und 20 km breiten, NW-SE-streichenden-Oberflächenaufschluss paläozoischer Gesteine. In weiten Gebieten bedecken känozoische Schichten diesen Sockelaufbruch. Die aufgeschlossenen Gesteine ​​sind niedriggradige metamorphe Gesteine sowie mäßig deformierte Vorland-Sedimente des Rhenoherzynikums sowie hochgradige metamorphe und intrusive Gesteine ​​der Mitteldeutschen Kristallinzone. Sie sind weitgehend von Sedimentgesteinen aus spätem Karbon bis frühem Perm bedeckt. Nach der Varizischen Orogenese entwickelten sich die Randstörungen des Flechtinger Höhenzugs zu großen dextralen Scherzonen, die zusammen als südliche Elbzone beschrieben werden und ein Wrench-System im Krustenmaßstab bilden, das vom Böhmischen Massiv im Südosten bis zur Nordsee im Nordwesten reicht. Es wird vermutet, dass Sedimentgesteine ​​des mitteleuropäischen Beckensystems den Flechtinger Höhenzug während des Mesozoikums bedeckten. Die Randstörungen, d. h. Teile der Elbzone, wurden wahrscheinlich während der Jura- bis frühen Kreidezeit unter einem extensionalen Spannungsfeld als Abschiebungen reaktiviert. Einengung während der späten Kreide führte zur Anhebung des Flechtinger Höhenzugs und beeinflusste als existierende Hochlage auch spätere großräumige Krustenbewegungen, wie die Verteilung der känozoischen Sedimente zeigt [Stackebrandt, 1986]. @de
preferred label: Störungszonen des Flechtinger Höhenzugs @de
alternative label: Störungszonen der Flechtingen-Rosslau-Scholle @de
narrower: Haldensleben Fault Zone
narrower: Wittenberg Fault Zone
narrower: Flechtingen High Southern Border Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Saxony-Anhalt

Flechtingen High Southern Border Fault
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:15.179Z
notation: DE-ST-41
definition: The Flechtingen-Südrand fault zone delimits the Flechtingen-Rosslau Block in the north against the Subhercynian Basin in the south with comparatively small offsets.
definition: Die Flechtingen-Südrand Störungszone begrenzt mit vergleichsweise geringen Versätzen die Flechtingen-Rosslau Scholle im Norden gegen das Subherzyne Becken im Süden. @de
preferred label: Flechtingen-Suedrand-Störungszone @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Flechtingen High

Wittenberg Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8105
references: https://data.geoscience.earth/ncl/geoera/ref/8068
references: https://data.geoscience.earth/ncl/geoera/ref/7994
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:15.174Z
notation: DE-ST-38
definition: The Wittenberg fault zone forms the eastern section of the Haldensleben fault and is thus one of the "Central German main escarpments". It borders the Flechtingen-Rosslau-Block in the south against the North German Basin in the north.
definition: Der Wittenberg-Abbruch bildet den östlichen Abschnitt der Haldensleben Überschiebung und ist damit einer der "Mitteldeutschen Hauptabbrüche". Er begrenzt die Flechtingen-Rosslau-Scholle im Süden gegen das Norddeutsche Becken im Norden. @de
preferred label: Wittenberg-Störungszone @de
alternative label: Wittenberg Thrust
alternative label: Abburch von Wittenberg @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Flechtingen High

Haldensleben Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8105
references: https://data.geoscience.earth/ncl/geoera/ref/8068
references: https://data.geoscience.earth/ncl/geoera/ref/7994
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:15.169Z
notation: DE-ST-36
definition: The Haldensleben fault delimits the Central European Basin succession of the Calvörde Block in the north against the outcrop of Palaeozoic strata of the Flechtingen High in the south. It forms a large SW-dipping reverse fault. Uniform fault offsets only exceed 3 km in the east, where the Gardelegen fault converges with the Haldensleben fault. In its northern foreland subordinated basement faults with minor normal and reverse offsets separate Triassic to Early Jurassic strata in narrow (5 km wide) sub-basins and grabens indicating a complex pre-thrusting history. In the outer east several basement reverse faults border smaller uplifts of Palaeozoic rocks.
definition: Die Haldensleben Überschiebung begrenzt die Scholle von Calvörde als Teil des Zentraleuropäischen Beckens im Norden gegen die paläozoischer Schichten der Flechtingen-Rosslau-Scholle im Süden. Als einer der "Mitteldeutschen Hauptabbrüche" bildet sie eine bedeutende Überschiebung mit einem Einfallen nach Südwesten. Die vergleichsweise einheitlichen Störungsversätze überschreiten im Osten selten 3 km. Hier konvergiert die Gardelegen Überschiebung mit der Haldensleben Überschiebung. Im nördlichen Vorland trennen untergeordnete Sockelstörungen mit geringfügigen Abschiebungs- und Aufschiebungsversätzen mesozoische Schichten in enge (5 km breiten) Teilbecken und Gräben, was auf eine komplexe Vorgeschichte hinweist. Im äußeren Osten grenzen mehrere Sockelstörungen an kleinere Erhebungen paläozoischer Einheiten. @de
preferred label: Haldensleben-Störungszone @de
alternative label: Haldensleben Thrust
alternative label: Abbruch von Haldensleben @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Flechtingen High

Fault zone of the Altmark area
references: https://data.geoscience.earth/ncl/geoera/ref/8117
references: https://data.geoscience.earth/ncl/geoera/ref/8052
references: https://data.geoscience.earth/ncl/geoera/ref/8068
references: https://data.geoscience.earth/ncl/geoera/ref/8092
definition: The northern part of Saxony-Anhalt (Altmark area) forms the southern rim of the Central European Basin System. It underwent continuous subsidence since Permian times. The major tectonic blocks trend either NNE-SSW or NW-SE. Hence, in earlier classifications [e.g., Katzung and Ehmke, 1993] the entire area was named ‘Altmark-Fläming Depression’. Based on more recent investigations based on extensive reflection seismic data and several hundreds of boreholes, which were combined in a homogeneous 3D geological model [Malz et al., 2020], the Altmark area can be subdivided into six major tectonic units: (1) The eastern part of the Gifhorn Trough is located in the outer northwest and forms a NNE-SSW-trending Mesozoic (trans-)tensional graben. (2) The (Eichsfeld-) Altmark Swell to the east of the Gifhorn Trough is an approximately 50 km wide NNE-SSW to NE-SW-striking structural high [Wienholz, 1964] initially emerged during the latest Permian to Triassic [Paul, 1993]. It is interpreted as the former graben shoulder of the western adjacent Gifhorn Trough [Malz et al., 2020] and is bordered by a deep crustal shear zone (Arendsee Lineament) to the east [Franke, 1990]. (3) In the northeast of the Altmark structures of similar trending direction (NNE-SSW) are associated with the Rheinsberg Trough located at the eastern border of Saxony-Anhalt. In these areas (Gifhorn Trough, Altmark Swell and Rheinsberg Trough) associated fault zones are difficult to detect due to the complex interplay of synkinematic erosion and deposition, extensive diapirism as well as crosscutting NW-SE-striking normal and reverse faults. (4) The inverted Altmark-Fläming Basin s. str. is located between the Altmark Swell and the Rheinsberg Trough. Narrow NW-SE-striking, in parts reverse reactivated normal faults and long wavelength folds, salt pillows and diapirs characterize this area. (5) The ‘Late Jurassic Altmark Swell’ borders the Altmark-Fläming Basin s. str. to the south. It forms the southern graben s…
type: Concept
created: 2021-03-03T16:08:14.947Z
notation: DE-ST-1000
preferred label: Störungszone des Norddeutschen Beckens @de
alternative label: Fault Zone of the North German Basin
alternative label: Störungszone der Altmark @de
narrower: Arendsee Fault Zone
narrower: Schrampe Fault Zone
narrower: Seehausen Fault Zone
narrower: Meseberg Fault Zone
narrower: Unterelbe Fault Zone
narrower: Salzwedel Fault Zone
narrower: Kleinau Fault Zone
narrower: Schorstedt Fault Zone
narrower: Schollene Fault Zone
narrower: Kerkau Fault Zone
narrower: Gerstedt Fault Zone
narrower: Rockenthin-Peckensen-Gladdenstedt Fault Zone
narrower: Altmersleben-Demker Fault Zone
narrower: Uelzen Fault Zone
narrower: Ahlum Fault Zone
narrower: Kakerbeck-Mahlpfuhl Fault Zone
narrower: Jahrstedt-Ristedt-Poppau-Apenburg Fault Zone
narrower: Gifhorn Trough Eastern Border Fault Zone
narrower: Jübar Fault Zone
narrower: Parsau Fault Zone
narrower: Crestal Graben of the Peckensen diapir
narrower: Groß Schwechten Fault Zone
narrower: Hassel-Schwarzholz Fault Zone
narrower: Mahlitz Fault Zone
narrower: Fleetmark Fault Zone
narrower: Kuhfelde Fault Zone
narrower: Schieben Fault Zone
narrower: Zerben Fault Zone
narrower: Brehm Fault Zone
narrower: Crestal Graben of the Lüge-Liesten and Meßdorf diapirs
narrower: Crestal Graben of the Ristedt diapir
narrower: Crestal Graben of the Apenburg and Poppau diapirs
narrower: Crestal Graben of the Jahrstedt diapir
narrower: Burg-Reuden Fault Zone
narrower: Schweinitz Fault Zone
narrower: Schönewalde Fault Zone
narrower: Zahna Fault Zone
narrower: Elster Fault Zone
narrower: Neuferchau Graben
narrower: Tarnefitz Fault Zone
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Saxony-Anhalt

Salzwedel Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8068
references: https://data.geoscience.earth/ncl/geoera/ref/7994
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:14.982Z
notation: DE-ST-6
definition: The regional, NW-SE-striking Salzwedel fault system crosses nearly the whole north of Saxony-Anhalt. All faults in the ‘supra-salt’ succession can be clearly correlated with corresponding basement faults. The fault zone comprises several individual fault strands (from west to east): (1) The Wustrow-Lüge-Liesten fault segment, a north-dipping major fault and with steeply south-dipping antithetic faults arranged in an anticline, shows minor normal and reverse offsets indicating a poly-phase activity. Towards the east, it becomes replaced by the (2) Lüge-Liesten-Meßdorf fault segment, which forms a steeply dipping reverse reactivated normal fault with a ‘harpoon structure’ (cf. McClay and Buchanan, 1992) in its hanging wall. Preserved syn-extensional Upper Jurassic to Lower Cretaceous strata became later uplifted and thrusted against Upper Cretaceous rocks in the footwall. In the (3) Meßdorf-Groß Schwechten fault segment the structural style changes to a south-dipping steep normal fault with relatively low offsets.
definition: Die regionale, NW-SE-streichende Salzwedel Störungszone quert nahezu den gesamten Nordteil Sachsen-Anhalts. Ihre einzelnen Segmente werden auch nach den gequerten Salzstrukturen benannt, weshalb sich eine Unterteilung der Störungszone in einzelne Abschnitte ergibt. So werden innerhalb der Störungszone Wustrow-Lüge Liesten die Dehnungsstrukturen in der Umrahmung des Salzstockes Wustrow nach Südosten durch Einengungsstrukturen abgelöst. Die in sich gestörte NE-Flanke ist gegenüber dem SW-Flügel angehoben. Diese enthält zum Teil mächtige synkinematische Oberkreide-Sedimente. Lokal sind auf der NE-Flanke grabenbruchartige Strukturen mit Unterkreide nachgewiesen. Teilweise Salzintrusionen in die Störungszone nachgewiesen. Jüngste Bewegungen sind lokal bis ins Tertiär nachgewiesen. In Richtung Osten setzt sich die Störungszone Lüge Liesten-Meßdorf mit einem ähnlichen Strukturinventar der NE- und SW-Flanken fort. Beiderseits der Störungszone sind Senken mit kretazischen Sedimenten ausgebildet (Unterkreide im NE, Oberkreide im SW), die eine polyphase tektonische Entwicklung belegen. Die Störungszone Meßdorf-Groß Schwechten weißt eine deutliche Abweichung vom strukturellen Baustil auf. Salzintrusionen in die Störungszone sind nicht nachgewiesen. Stattdessen ist das suprasalinare Deckgebirge entlang der Störungszone deutlich in einer weitgespannten Mulde eingesunken. @de
preferred label: Salzwedel-Störungszone @de
alternative label: Salzwedel Fault
alternative label: Wustrow-Lüge-Liesten-Meßdorf-Groß Schwechten Störungszone @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Unterelbe Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8032
references: https://data.geoscience.earth/ncl/geoera/ref/7996
type: Concept
created: 2021-03-03T16:08:14.978Z
notation: DE-ST-5
definition: The Unterelbe fault zone as a part of the Elbe Lineament is a crustal discontinuity at the northern border of the Altmark area. In the Permian to Mesozoic cover it is represented by mild normal faulting during Jurassic-Early Cretaceous times and became reverse reactivated during Late Cretaceous basin inversion.
preferred label: Unterelbe-Störungszone @de
alternative label: Elbe Lineament
alternative label: Unterelbe-Barenthin-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Meseberg Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8068
references: https://data.geoscience.earth/ncl/geoera/ref/8028
type: Concept
created: 2021-03-03T16:08:14.974Z
notation: DE-ST-4
definition: The Meseberg fault zone is a NW-SE-trending fault zone associated with the Meseberg diapir. The activity of the fault zone is strongly associated with halokinetic movements and the formation of the Meseberg salt pillow in Late Cretaceous times.
preferred label: Meseberg-Störungszone @de
alternative label: Meseberg Fault
alternative label: Meseberg-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Hassel-Schwarzholz Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8068
references: https://data.geoscience.earth/ncl/geoera/ref/8028
definition: Die ungefähr 22 km lange und bis zu 5 km breite Hassel-Schwarzholz-Störungszone (Emmerlich 2017) befindet sich nördlich von Stendal in der östlichen Altmark und stellt ein NNE-SSW bis N-S streichendes Störungssystem dar, das zwischen den Salzstöcken Mahlitz im Osten und Groß Schwechten im Westen die Salzwedel-Störungszone quert. Für dieses bereits von Lapschin et al. 1972 beschriebene Störungssystem wurde im Rahmen der Modellerstellung erstmals eine Trassierung durchgeführt, um eine in sich konsistente dreidimensionale Vorstellung zum Störungsverlauf und dessen Entstehung zu entwickeln. In früheren Arbeiten (Lapschin et al. 1972) konnte diese Trassierung aufgrund der zu geringen Profildichte und einem spitzwinkligen Verlauf der Profile zu den Störungen noch nicht durchgeführt werden. Ihre Existenz wurde aber bereits in diesen Arbeiten schon auf Basis von Änderungen der Sprungtendenz und dem plötzlichen Ausklingen der die Struktur querenden und NW-SE streichenden Salzwedel-Störungszone postuliert. Bei allen Einzelbrüchen der Hassel-Schwarzholz-Störungszone handelt es sich um Abschiebungen und Grabenbrüche (Lapschin et al. 1972). Die Störungszone besteht im Modell aus zwei mehr oder weniger getrennten Systemen, einem südwestlichen Störungsabschnitt, der aus zwei Einzelbrüchen mit gegenläufigem Einfallen aufgebaut ist, und einem nordöstlichen Abschnitt mit drei Einzelbrüchen. Die Hauptstörungen beider Abschnitte bilden im Zentrum der Salzwedel-Störungszone eine Schnittlinie, an der der nordöstliche Abschnitt endet. Der südwestliche Abschnitt hingegen verläuft über nahezu die gesamte Länge der Störungszone. Die Hauptstörungen der beiden Störungsabschnitte zeigen deutlich eine Fortsetzung innerhalb der subsalinaren Einheiten, während die von ihnen begleiteten Zweigstörungen nur die Basis des Buntsandsteins versetzen. Die stratigraphisch höchsten von bruchhafter Deformation beeinflussten Einheiten sind die Horizonte der Unterkreide, deren Verbreitung sich stark an der Has… @de
type: Concept
created: 2021-03-03T16:08:15.067Z
notation: DE-ST-27
definition: The approximately 30 km long and 1.5 km wide Hassel-Schwarzholz fault consists out of five individual normal faults with respectively low (< 50 m) fault offsets. The fault zone retraces the axis of a NNE-SSW trending sub-basin located directly between the Groß Schwechten and Mahlitz diapirs. Due to its spatial relation to the Late Jurassic-Early Cretaceous sub-basin we interpret that transtensional/extensional faulting started synchronously. Furthermore, the fault zone's location coinciding with the eastern outline of Late Cretaceous strata probably suggests a Late Cretaceous transpressional/compressional overprint.
preferred label: Hassel-Schwarzholz-Störungszone @de
alternative label: Hassel-Schwarzholz Fault
alternative label: Hassel-Schwarzholz-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Seehausen Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
type: Concept
created: 2021-03-03T16:08:14.969Z
notation: DE-ST-3
definition: The Seehausen fault zone is a NW-SE-trending extensional fault zone in the Permian to Mesozoic strata of the northeastern Altmark area.
preferred label: Seehausen-Störungszone @de
alternative label: Seehausen Fault
alternative label: Seehausen-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Groß Schwechten Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8068
references: https://data.geoscience.earth/ncl/geoera/ref/8028
type: Concept
created: 2021-03-03T16:08:15.063Z
notation: DE-ST-26
definition: The Groß Schwechten fault zone consists of three normal faults located on the outer limbs of the associated Groß Schwechten salt pillow. All faults dip towards the centre of the diapir. A relatively uniform layering of Triassic to lower Middle Jurassic strata suggests that deformation and vertical movements started in Late Jurassic-Early Cretaceous times at the earliest. The regional Late Cretaceous unconformity sealing the entire fault zone marks the end of deformation.
definition: Die Störungszone Groß Schwechten bildet eine NNE-SSW streichende Grabenstruktur in der östlichen Altmark. Ihre Namensgebung beruht auf dem sich in ihrem Grabeninneren befindenden Salzstock Groß Schwechten (Emmerlich 2017). Die ungefähr 2,5 km breite und bis zu 17 km lange Störungszone besteht aus einer östlichen Hauptstörung und einer westlichen antithetischen Zweigstörung. Bei beiden Störungen handelt es sich um Abschiebungen, die durch die Transgression der Oberkreide nach oben hin begrenzt sind. Eine Fortsetzung der Störungen im Subsalinar deutet sich auf vielen reflexionsseismischen Profilen an und ist als wahrscheinlich anzunehmen. Die Ausbildung der Störungszone wird für den Zeitraum Oberjura/Unterkreide angenommen, und steht in engem Zusammenhang mit der Ausbildung eines Salzkissens unter dem heutigen Salzstock Groß Schwechten. Aus regionalgeologischen Betrachtungen zur Hauptspannungsrichtung während des Zeitraums Oberjura/Unterkreide (Franzke et al. 2007; Navabpour et al. 2017; Sippel et al. 2009) handelt es sich bei der Störungszone, wie auch bei den anderen Randelementen des Rheinsberg-Trogs, um transtensionale Strukturen, die einen deutlichen Blattverschiebungsversatz aufweisen sollten. @de
preferred label: Groß Schwechten-Störungszone @de
alternative label: Groß Schwechten Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Schrampe Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
type: Concept
created: 2021-03-03T16:08:14.965Z
notation: DE-ST-2
definition: The Schrampe fault zone is a NW-SE-trending fault zone in the Mesozoic cover in the NW of the Arendsee diapir. It is elongated from the state border between Lower Saxony in the west to the Arendsee diapir in the east.
preferred label: Schrampe-Störungszone @de
alternative label: Schrampe Fault
alternative label: Schrampe-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Crestal Graben of the Peckensen diapir
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
type: Concept
created: 2021-03-03T16:08:15.059Z
notation: DE-ST-25
definition: The Scheitelgraben Peckensen forms a collaps structure on top of the Peckensen diapir.
definition: Der Scheitelgraben Peckensen bildet eine Einbruchstruktur im Dachbereich Salzstocks Peckensen. @de
preferred label: Scheitelgraben des Salzstocks Peckensen @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Parsau Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
type: Concept
created: 2021-03-03T16:08:15.055Z
notation: DE-ST-23
definition: The Parsau fault zone forms a complex, small-scale fault zone in the western Altmark. Due to the intersection of several strike directions, this fault zone is characterized by steeply dipping layers and small-scale changing offsets.
definition: Die Parsau Störungszone bildet eine komplexe, kleinräumige Störungszone in der westlichen Altmark. Aufgrund der Kreuzung mehrerer Streichrichtungen ist diese Störungszone durch steil einfallende Schichten und kleinräumig wechselnde Versätze charakterisiert. @de
preferred label: Parsau-Störungszone @de
alternative label: Parsau Fault
alternative label: Parsau-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Tarnefitz Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
type: Concept
created: 2021-03-03T16:08:15.143Z
notation: DE-ST-74
definition: The Tarnefitz fault zone forms a Cenozoic fault zone in the southern Altmark. It is only found in the Cenozoic sediments.
definition: Die Tarnefitz Störungszone bildet eine känozoische Störungszone in der südlichen Altmark. Sie ist ausschließlich in den känozoischen Sedimenten nachgewiesen. @de
preferred label: Tarnefitz-Störungszone @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Arendsee Fault Zone
related: Arendsee Lineament
references: https://data.geoscience.earth/ncl/geoera/ref/8033
references: https://data.geoscience.earth/ncl/geoera/ref/8068
references: https://data.geoscience.earth/ncl/geoera/ref/7994
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:14.955Z
notation: DE-ST-1
definition: The Arendsee fault zone, locally named Arendsee-Lüge-Liesten or Wittenberge-Arendsee fault, is located above an 80 km long crustal structure, the Arendsee Lineament respectively (Franke, 1990). Major faults steeply (c. 70°) dip towards the west and form narrow grabens. Generally fault throws are low, locally cease and rarely exceed 200 m. The Arendsee-Lüge-Liesten and the Wittenberge-Arendsee faults form narrow northeast-dipping grabens in ‘supra-salt’ strata located above a southeast-dipping ‘sub-salt’ crustal fault zone, the Arendsee Lineament respectively.
definition: Die Arendsee Störungszone, die lokal entsprechend ihrer Einzelsegmente auch als Arendsee-Lüge Liesten oder Wittenberge-Arendsee Störung bezeichnet wird, befindet sich über einer 80 km langen tiefreichenden, krustalen Bruchstruktur, dem Arendsee-Lineament (Franke, 1990). Die Hauptstörungen fallen steil (ca. 70°) nach Westen ein und bilden zusammen mit ihren antithetischen Störungen schmale Gräben. Im Allgemeinen sind die Versatzbeträge gering, nehmen stellenweise aber auf kurze Distanz stark ab und überschreiten selten 200 m. Die Arendsee-Lüge Liesten und Wittenberge-Arendsee Störungen bilden schmale, nach Nordosten abgesenkte Gräben innerhalb der suprasalinaren Einheiten, die sich über einer nach Südosten einfallenden subsalinaren Sockelabschiebung, dem Arendsee-Lineament, befinden. @de
preferred label: Arendsee-Störungszone @de
alternative label: Arendsee Lineament
narrower: Crestal Graben of the Arendsee diapir
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Crestal Graben of the Arendsee diapir
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8034
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-03-03T16:08:14.960Z
notation: DE-ST-68
definition: The Scheitelgraben Arendsee forms a collaps structure on top of the Arendsee diapir.
definition: Der Scheitelgraben Arendsee bildet eine Einbruchstruktur im Dachbereich des Arendsee Salzstocks. @de
preferred label: Scheitelgraben des Salzstocks Arendsee @de
alternative label: Scheitelgraben Arendsee @de
broader: Arendsee Fault Zone

Jübar Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
type: Concept
created: 2021-03-03T16:08:15.051Z
notation: DE-ST-21
definition: The Jübar fault zone forms a complex, small-scale fault zone in the western Altmark. Due to the intersection of several strike directions, this fault zone is characterized by steeply dipping layers and small-scale changing offsets.
definition: Die Jübar Störungszone bildet eine komplexe, kleinräumige Störungszone in der westlichen Altmark. Aufgrund der Kreuzung mehrerer Streichrichtungen ist diese Störungszone durch steil einfallende Schichten und kleinräumig wechselnde Versätze charakterisiert. @de
preferred label: Jübar-Störungszone @de
alternative label: Jübar Fault
alternative label: Jübar-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Neuferchau Graben
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
type: Concept
created: 2021-03-03T16:08:15.138Z
notation: DE-ST-72
definition: The Neuferchau fault zone forms a Cenozoic fault zone in the southwestern Altmark. It is only found in the Cenozoic sediments.
definition: Die Neuferchauer Störungszone bildet eine känozoische Störungszone in der südwestlichen Altmark. Sie ist ausschließlich in den känozoischen Sedimenten nachgewiesen. @de
preferred label: Neuferchauer Graben @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Elster Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8078
type: Concept
created: 2021-03-03T16:08:15.134Z
notation: DE-ST-90
definition: The Elster fault zone forms a subordinate fault zone in the direct foreland of the Gardelegen thrust.
definition: Die Elster Störungszone bildet eine untergeordnete Störungszone im direkten Vorland der Gardelegen Überschiebung. @de
preferred label: Elster-Störungszone @de
alternative label: Elster Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Zahna Fault Zone
related: Zahna Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8078
type: Concept
created: 2021-03-03T16:08:15.129Z
notation: DE-ST-89
definition: The Zahna fault zone forms a subordinate fault zone in the direct foreland of the Gardelegen thrust.
definition: Die Zahna Störungszone bildet eine untergeordnete Störungszone im direkten Vorland der Gardelegen Überschiebung. @de
preferred label: Zahna-Störungszone @de
alternative label: Zahna Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Schönewalde Fault Zone
related: Schönewalde Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8078
type: Concept
created: 2021-03-03T16:08:15.125Z
notation: DE-ST-40
definition: The Schönewalde fault zone forms a subordinate fault zone in the direct foreland of the Gardelegen thrust.
definition: Die Schönewalde Störungszone bildet eine untergeordnete Störungszone im direkten Vorland der Gardelegen Überschiebung. @de
preferred label: Schönewalde-Störungszone @de
alternative label: Schönewalde Fault
alternative label: Schönewalde-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Schweinitz Fault Zone
related: Schweinitz Fault
references: https://data.geoscience.earth/ncl/geoera/ref/8078
type: Concept
created: 2021-03-03T16:08:15.121Z
notation: DE-ST-39
definition: The Schweinitz fault zone forms a subordinate fault zone in the direct foreland of the Gardelegen thrust.
definition: Die Schweinitz Störungszone bildet eine untergeordnete Störungszone im direkten Vorland der Gardelegen Überschiebung. @de
preferred label: Schweinitz-Störungszone @de
alternative label: Schweinitz Fault
alternative label: Schweinitz-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Schollene Fault Zone
related: Schollene Fault
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
type: Concept
created: 2021-03-03T16:08:14.994Z
notation: DE-ST-9
definition: The Schollene fault zone is a major basement fault in the northestern Altmark area.
definition: Die Schollene Störungszone bildet eine bedeutende Sockelstörung in der nordöstlichen Altmark. @de
preferred label: Schollene-Störungszone @de
alternative label: Schollene Fault
alternative label: Schollene-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Schorstedt Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
type: Concept
created: 2021-03-03T16:08:14.991Z
notation: DE-ST-8
definition: The Schorstedt fault zone is a subordinated basement fault in the northern Altmark area, which is probably associated with Permian and Triassic extension relating to the formation of the Rheinsberg Trough.
definition: Die Schorstedt Störungszone bildet eine untergeordnete Störungszone in der nördlichen Altmark. Als extensionale Störungszone in den Permo-Triassischen Einheiten ausgebildet, steht ihre Bildung mit der Entstehung des Rheinsberg Troges in Zusammenhang. @de
preferred label: Schorstedt-Störungszone @de
alternative label: Schorstedt Fault
alternative label: Schorstedt-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Kleinau Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
type: Concept
created: 2021-03-03T16:08:14.987Z
notation: DE-ST-7
definition: The Kleinau fault zone is a subordinated basement fault south of the Arendsee diapir.
definition: Die Kleinau Störungszone bildet eine untergeordnete Sockelstörung im Süden des Salzstocks Arendsee. @de
preferred label: Kleinau-Störungszone @de
alternative label: Kleinau Fault
alternative label: Kleinau-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Mahlitz Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8068
references: https://data.geoscience.earth/ncl/geoera/ref/8028
type: Concept
created: 2021-03-03T16:08:15.077Z
notation: DE-ST-28
definition: The Mahlitz fault, which crosses the Mahlitz diapir, forms a single east-dipping normal fault with vertical offsets not exceeding 100 m. Indications for the onset of fault activity are scarce due to a Late Jurassic to Late Cretaceous hiatus. Nevertheless, from adjacent structures a synchronous onset of transtensional/extensional faulting and salt migration into the Mahlitz salt pillow during Late Jurassic/Early Cretaceous times must be supposed.
definition: Die Mahlitz-Störung, eine den Salzstock Mahlitz in NNE-SSW-Richtung querende und nach diesem benannte Störung (Emmerlich 2017), befindet sich in der östlichen Altmark und versetzt entlang ihrer nach Osten einfallenden Störungsfläche die Modellhorizonte des Zechsteins bis zur Oberkreide. Basierend auf den Ergebnissen der reflexionsseismischen Messungen (Muraschew et al. 1972) ist von einer Sprunghöhe zwischen 50 und 100 m bei einem abschiebenden bis transtensionalen Versatzsinn auszugehen. Diese vergleichsweise geringe Sprunghöhe erschwert die Einschätzung der Begrenzung der Störung im Hangenden. Diese kann sowohl durch ein allmähliches Abklingen der Sprunghöhe aber auch als abruptes Ende der Deformation in prätertiärer Zeit angesehen werden (Küstermann 1972). Im Modell wurde deshalb davon ausgegangen, dass die Störung ausschließlich prätertiäres Alter aufweist und die Transgression des Oberpaläozäns die Störung im Hangenden begrenzt. @de
preferred label: Mahlitz-Störungszone @de
alternative label: Mahlitz Fault
alternative label: Mahlitz-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Kakerbeck-Mahlpfuhl Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8068
references: https://data.geoscience.earth/ncl/geoera/ref/7994
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:15.030Z
notation: DE-ST-16
definition: The Kakerbeck-Mahlpfuhl fault zone is a narrow, NW-SE-striking structure. It forms a large, faulted NE-vergent anticline in the west. Fault offsets do not exceed 500 m, but a huge structural heave of the hanging wall is associated with an up to one kilometre thick salt core. Thickness variations of Early Jurassic strata infer that contractional deformation overprinted a complex pre-thrusting configuration with inherited normal faults and differentially subsided blocks. Towards the east offsets decrease over short distances. Here, the fault zone is replaced by a narrow salt-cored anticline (detachment fold) with Late Cretaceous synkinematic strata in the north and south.
definition: Die Kakerbek-Mahlpfuhl Störungszone ist eine kurzwellige, NW-SE-streichende Struktur. Im Westen bildet sie eine NE-vergente Antiklinale. Störungsversätze sind vergleichsweise gering und übersteigen nur selten 500 m. Dennoch ist die SW-Flanke der Struktur hier aufgrund von deutlicher Salzakkumulation im Kern der Antiklinale bedeutend gegenüber der NE-Flanke gehoben. Mächtigkeitsvariationen innerhalb des Jura deuten darauf hin, dass die deutliche einengende Deformation während der späten Kreide eine sehr komplexe Konfiguration mit vererbten Abschiebungen und unterschiedlich stark abgesenkten Blöcken überprägte. In Richtung Osten nehmen die Versatzbeträge der Einzelstörungen kontinuierlich ab und die Störungszone wird durch eine enge Antiklinale mit mächtigem Salzkern (Detachment-Falte) vertreten, die durch mächtige spätkretazische Sedimente im Norden und Süden begleitet wird. @de
preferred label: Kakerbeck-Mahlpfuhl-Störungszone @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Burg-Reuden Fault Zone
related: Burg-Reuden Fault
references: https://data.geoscience.earth/ncl/geoera/ref/8068
type: Concept
created: 2021-03-03T16:08:15.118Z
notation: DE-ST-37
definition: The Burg-Reuden fault consists of the western (‘Burg’) part, where a single reverse fault exists in the outer crest of a salt-cored anticline in its hanging wall. Here, similar fault offsets (300 m) in the cover and the basement exist. In the eastern (‘Reuden’) part relatively high fault offsets (1 km) exist at the intersection with the Brehm fault indicating a significant amount of displacement transfer from that structure.
definition: Die Burg-Reuden Störungszone besteht aus dem westlichen Teil („Burg“), in dem eine einzige Aufschiebung im äußeren Bogen einer Detachment Falte vorliegt. Hier bestehen ähnliche Versatzbeträge (300 m) im Sockel wie auch im Deckgebirge. Im östlichen Teil („Reuden“) sind im Kreuzungsbereich mit der Brehm Störungszone relativ hohe Versätze (1 km) auszumachen, was auf einen erheblichen Versatztransfer zwischen diesen Strukturen hinweist. @de
preferred label: Burg-Reuden-Störungszone @de
alternative label: Burg-Reuden Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Ahlum Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8068
references: https://data.geoscience.earth/ncl/geoera/ref/7994
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:15.026Z
notation: DE-ST-15
definition: The Ahlum fault zone forms the western elongation of the Gardelegen fault in map view. It is bounded by up to 2.5 km thick Late Cretaceous strata in the north and south. The fault zone is <1.5 km wide and reverse offsets (up to 1.5 km) are restricted to the Mesozoic cover. Hence, we interpret the Ahlum fault to represent a thin-skinned reverse fault, which thus must be kinematically linked to thick-skinned thrusting farther south; i.e., at the western Gardelegen fault.
definition: Die Ahlum Störungszone erstreckt sich zwischen dem Salzstock Ristedt und dem Südende des Salzstocks Peckensen. Sie bildet die westliche Verlängerung der Gardelegen Störung im Kartenbild. Sie ist asymmetrisch aufgebaut und sehr deutlich kompressiv überprägt. Sie weißt eine intensive bruchtektonische Zerlegung der Südflanke und des Strukturtops auf. Teilweise überkippte Lagerung der Schichtenfolge belegt zusätzlich die kompressive Überprägung. Charakteristisch für die Ahlum Störungszone ist ihre vergleichsweise enge Ausbildung im Vergleich zu ihren beiderseits vorhandenen bis zu 1,5 km mächtigen Randsenken mit spätkretazischen Sedimenten. @de
preferred label: Ahlum-Störungszone @de
alternative label: Ahlum Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Crestal Graben of the Jahrstedt diapir
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
references: https://data.geoscience.earth/ncl/geoera/ref/8034
type: Concept
created: 2021-03-03T16:08:15.113Z
notation: DE-ST-71
definition: The Scheitelgraben Jahrstedt forms a collaps structure on top of the Jahrstedt diapir.
definition: Der Scheitelgraben Jahrstedt bildet eine Einbruchstruktur im Dachbereich des Jahrstedt Salzstocks. @de
preferred label: Scheitelgraben des Salzstocks Jahrstedt @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Crestal Graben of the Apenburg and Poppau diapirs
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
references: https://data.geoscience.earth/ncl/geoera/ref/8034
type: Concept
created: 2021-03-03T16:08:15.108Z
notation: DE-ST-70
definition: The Scheitelgraben Apenburg-Poppau forms a collaps structure on top of the Apenburg and Poppau diapirs.
definition: Der Scheitelgraben Apenburg-Poppau bildet eine Einbruchstruktur im Dachbereich der Salzstöcke Apendburg und Poppau. @de
preferred label: Scheitelgraben der Salzstöcke Apenburg und Poppau @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Uelzen Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/7992
references: https://data.geoscience.earth/ncl/geoera/ref/8068
references: https://data.geoscience.earth/ncl/geoera/ref/7994
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:15.017Z
notation: DE-ST-14
definition: The Uelzen Lineament forms an inverted halfgraben with a listric, north-dipping normal fault flattening in the mechanically weak strata of the Zechstein group and the Upper Buntsandstein subgroup. Due to prior intense E-W extension along bedding parallel normal faults these weak strata are super-imposed. Hence, flattening of the listric Uelzen normal fault may was associated with the reactivation of a pre-existing shear zone within the basal detachment. Antithetic normal faults of the Uelzen Lineament lead to subordinate syntectonic basins with steeply dipping (up to 45°) Late Jurassic strata. Late Cretaceous syn-contractional deposits in the footwall and in the farther hanging wall prove a contractional overprint and retrace the typical distribution of synkinematic strata adjacent to inverted halfgrabens with reactivated listric normal faults (Buchanan and McClay, 1991).
definition: Das Uelzen-Linieament bildet einen invertierten Halbgraben mit einer listrischen, nach Norden einfallenden Hauptstörung. Diese zeigt eine Verflachung in den Salinaren des Zechsteins und Oberen Buntsandsteins. Aufgrund der vorherigen intensiven E-W-Ausdehnung entlang schichtparalleler Abschiebungen liegen diese mechanisch weichen Schichten in störungsbedingt direkt übereinander. Daher kann eine Abflachung der listrischen Uelzen-Hauptabschiebung während der spätjurassischen Extension mit der Reaktivierung einer bereits vorhandenen, triassischen Scherzone innerhalb des Zechsteins verbunden sein. Antithetische Abschiebungen des Uelzen-Linieaments führen zu untergeordneten syntektonischen Sedimentbecken mit steil abfallenden (bis zu 45 °) spätjurassischen Sedimenten. Spätkretazische syn-kontraktionale Ablagerungen im Liegenden und Hangenden der Hauptstörung belegen die spätkretazische Inversion und zeichnen die typische Verteilung von synkinematischen Schichten neben invertierten Halbgrabenen mit reaktivierten listrischen Hauptabschiebungen nach. @de
preferred label: Uelzen-Lineament @de
alternative label: Uelzen Lineament
narrower: Bierstedt Fault Zone
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Bierstedt Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-03-03T16:08:15.022Z
notation: DE-ST-24
definition: The Bierstedt fault forms a normal fault in the east of the Peckensen diapir on top of the Altmark Swell. It forms the easternmost expression of the Uelzen Lineament, where it crosses the Peckensen diapir.
definition: Die Bierstedt Störung bildet eine Abschiebungszone im Osten des Salzstocks Peckensen im Top-Bereich der Altmark Schwelle. Sie bildet das östliche Ende des Uelzen-Lineaments, wo dieses den Salzstock Peckensen kreuzt. @de
preferred label: Bierstedt-Störungszone @de
alternative label: Bierstedt Fault
alternative label: Bierstedt-Störung @de
broader: Uelzen Fault Zone

Crestal Graben of the Ristedt diapir
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
references: https://data.geoscience.earth/ncl/geoera/ref/8034
type: Concept
created: 2021-03-03T16:08:15.104Z
notation: DE-ST-69
definition: The Scheitelgraben Ristedt forms a collaps structure on top of the Ristedt diapir.
definition: Der Scheitelgraben Ristedt bildet eine Einbruchstruktur im Dachbereich des Ristedt Salzstocks. @de
preferred label: Scheitelgraben des Salzstocks Ristedt @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Altmersleben-Demker Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8068
references: https://data.geoscience.earth/ncl/geoera/ref/7994
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:15.013Z
notation: DE-ST-13
definition: The Altmersleben-Demker fault zone forms an 80 km long structure, which roughly coincides with the southern distribution outline of Late Jurassic and Lower Cretaceous strata. The north-dipping steep major fault and several antithetic faults form a narrow graben structure located in the crest of an anticline. In the west, the fault zone abruptly starts with a vertical displacement of 500 m, large fault offsets and a south-vergent anticline. To the east, fault offsets decrease over a short distance and the entire structure is only mildly folded and faulted. Farther east, large normal offsets in Triassic strata are detectable, while the Late Jurassic-Early Cretaceous basin fill was uplifted, folded and faulted with reverse sense.
definition: Die Störungszone Altmersleben-Demker bildet eine NW-SE-streichende Störungszone im Norden Sachsen-Anhalts. In ihrem Nordwesten ist sie als weitgespannte, störungsgebundene, in Richtung Südwesten überschobene Antiklinale mit Scheitelstörungen ausgebildet. In Richtung Osten wird der Bau der Störungszone komplizierter. Entlang der Störungszone ist das Salz unterschiedlich hoch aufgedrungen und bildet stellenweise diapirartige Körper (Altmersleben, Berkau) aus. In Richtung Osten zeigt die Störungsfläche innerhalb der post-salinaren Einheiten ein deutlich steileres Einfallen. Die deutlich in Richtung Nordosten einfallenden Hauptstörung zeigt anhand der sie begrenzenden Schichtenfolge und deren Mächtigkeit deutliche Anzeichen für eine spätjurassisch/frühkretazische extensionale Aktivität und daran anschließende spätkretazische Phase der Einengung (Inversion des nördlich angrenzenden Grabens). @de
preferred label: Altmersleben-Demker-Störungszone @de
alternative label: Genthin-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Crestal Graben of the Lüge-Liesten and Meßdorf diapirs
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
references: https://data.geoscience.earth/ncl/geoera/ref/8034
type: Concept
created: 2021-03-03T16:08:15.100Z
notation: DE-ST-67
definition: The Scheitelgraben Lüge-Liesten-Meßdorf forms a collaps structure on top of the Lüge-Liesten and Meßdorf diapirs and the salt-related faults of the Salzwedel fault zone.
definition: Der Scheitelgraben Lüge-Liesten-Meßdorf bildet eine Einbruchstruktur im Dachbereich der Salzstöcke Lüge-Liesten und Meßdorf sowie der diese verbindenden Salzwedel Störungszone. @de
preferred label: Scheitelgraben der Salzstöcke Lüge-Liesten und Meßdorf @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Rockenthin-Peckensen-Gladdenstedt Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8068
references: https://data.geoscience.earth/ncl/geoera/ref/7994
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:15.009Z
notation: DE-ST-12
definition: The Rockenthin-Peckensen-Gladdenstedt fault zone striking NNE-SSW is a major fault zone associated with a highly complex fault system at the outer eastern border of the Gifhorn Trough. The major fault of this system forms a mildly westward-dipping, bedding-parallel normal fault with associated antithetic normal faults in its hanging wall. In parts subordinated extensional detachments and duplexes occur between the Triassic salt horizons (Upper Buntsandstein and Middle Muschelkalk detachments) and the Zechstein evaporites. Thickness distribution and a local hiatus between Buntsandstein and Upper Keuper (Arnstadt and Exter Fm.) strata suggest that major faulting occurred due to E-W-directed extension during Late Triassic (Karnian) times. During Late Jurassic to Early Cretaceous times the fault zone became reactivated under extension/transtension as inferred by the onset of diapirism at the Peckensen salt dome. In parts subsequent contraction during Late Cretaceous times is inferred.
definition: Bei der NE-SW-streichenden Störungszone Rockenthin-Peckensen-Gladdenstedt handelt es sich um eine komplexe Störungszone, die im Zusammenhang mit dem Störungssystem am Ostrand des Gifhorn-Trogs steht. Über einem Salzkern angelegt, ist der südöstliche Bereich deutlich gegenüber dem Nordwesten gehoben. Dies veranlasste Benox et al. (1997) zu der Deutung, dass es sich um eine nach Nordwesten gerichtete Aufschiebung handelt. Neuere Interpretationen im Bereich der Rockenthin-Peckensen-Gladdenstedt Störungszone (Malz et al., 2020) weise dagegen darauf hin, dass die Störungszone ein komplexes System aus ursprünglich altkimmerisch (Karnium) angelegten, flachen Abschiebungen bildet, welches sowohl während der spätjurassisch-frühkretazischen Dehnung transpressiv als auch während der spätkretazischen Einengung transpressiv überprägt wurde. Dies ist sowohl durch unterschiedlich tiefreichende Diskordanzen innerhalb des Mesozoikums, die Verbreitung und Mächtigkeit der Sedimente als auch durch das Einsetzen des Diapirsmus am Salzstock Peckensen belegt. Die Versatzbeträge der Störungszone klingen sowohl von Norden als auch von Süden zum Salzstock Peckensen hin aus. Dennoch lässt sich die Existenz der Störungszone unter dessen Salzüberhängen aufgrund von unterschiedlichen strukturellen Niveaus im Osten und Westen des Salzstocks als gesichert annehmen. @de
preferred label: Rockenthin-Peckensen-Gladdenstedt Störungszone @de
alternative label: Peckensen-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Brehm Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8068
type: Concept
created: 2021-03-03T16:08:15.096Z
notation: DE-ST-34
definition: The Brehm fault forms the 30 km long, along-strike continuation of the Gardelegen fault in the Mesozoic cover. Single reverse faults are arranged in a 4 km wide anticline bordered by synclines filled with Late Cretaceous strata. To the east the Brehm fault converges towards the Burg-Reuden fault farther south.
definition: Die Brehm Störungszone bildet die 30 km lange, östliche Fortsetzung der Gardelegen-Verwerfung in den mesozoischen Sedimenten. Lokal sind Aufschiebungen in einer bis zu 4 km breiten Antiklinale angeordnet, die von Synklinalen im Norden und Süden begrenzt wird. Diese sind mit Sedimenten spätkretazischen Alters gefüllt. Im Osten konvergiert die Brehm Störungszone mit der Burg-Reuden Störungszone. @de
preferred label: Brehm-Störungszone @de
alternative label: Brehm Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Gerstedt Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8068
references: https://data.geoscience.earth/ncl/geoera/ref/7994
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:15.004Z
notation: DE-ST-11
definition: The Gerstedt fault forms an E-W-striking fault zone, with a northdipping major reverse fault and minor antithetic back thrusts or reverse reactivated normal faults. Syn-extensional strata in the hanging wall indicate Early Cretaceous halfgraben formation and (Late Cretaceous) inversion. Fault offsets are relatively high (up to 1.5 km), which can be seen by Middle to Late Triassic strata located next to Upper Cretaceous rocks. Further subhorizontal thrusts in the footwall range some hundred meters far to the south (i.e., below the Peckensen diapir) and indicate a distinct amount of yet unrecognized thin-skinned thrusting.
definition: Die Störungszone Gerstedt bildet eine E-W-streichende Störungszone, die im Westen zwischen den Salzstöcken Wustrow und Peckensen beginnt und sich in Richtung Osten hin zum Salzstock Lüge-Liesten erstreckt. Die zum Teil stark gestörte Nordflanke ist gegenüber der Südflanke deutlich überschoben. Zum Teil setzen sich diese Überschiebungen bis in den Fußbereich des Salzstocks Peckensen als flache Überschiebungen in Form von zum Teil mehreren Hundertermeter langen Schuppen fort. Vielfache Bohrungen, die in geringen Teufen zum Teil mächtiges Salz antrafen, deuten auf einen deutlichen Salzeinschub in die Störungszone hin, weshalb diese oftmals als Salzstock gedeutet wurde. Aufgrund der erbohrten stratigraphischen Abfolge und widersprechender geophysikalischer, hauptsächlich reflexionsseismischer Belege sind diese zum Teil mächtigen Salzvorkommen allerdings als lokale Verdickungen triassischer Salinare (Röt und Muschelkalk) zu deuten. Das Vorkommen mächtiger Unterkreidesedimente auf der Nordflanke, die auf der Südflanke fehlen und durch spätkretazische Sedimente vertreten werden, deuten auf eine deutliche Vorprägung der spätkretazischen Einungsstruktur durch frühkretazische Abschiebungen hin. @de
preferred label: Gerstedt-Störungszone @de
alternative label: Gerstedt Fault
alternative label: Strukturzug Groß Gerstedt @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Zerben Fault Zone
related: Zerben-Belzig Structural Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8068
type: Concept
created: 2021-03-03T16:08:15.092Z
notation: DE-ST-33
definition: The Zerben fault (the eastern elongation of the Kakerbek-Mahlpfuhl fault zone) forms a large, faulted NE-vergent anticline in the west. Fault offsets do not exceed 500 m, but a huge structural heave of the hanging wall is associated with an up to one kilometre thick salt-cored anticline (detachment fold) with Late Cretaceous synkinematic strata in the north and south.
definition: Die Zerben Störungszone (östliche Verlängerung der Kakerbek-Mahlpfuhl Störungszone) bildet eine große, gestörte nordost-vergente Antiklinale im Westen. Störungsversätze übersteigen nirgendwo 500 m, aber die Hebungsbeträge der Schichtenfolge im Hangenden deuten auf eine bedeutend größere Einengung hin, die mit einer deutlichen Akkumulation von Zechstein Salzen im Kern einer bis zu einem Kilometer mächtigen Detachment Falte und mächtigen spätkretazischen Sedimenten im Norden und Süden einhergehen. @de
preferred label: Zerben-Störungszone @de
alternative label: Zerben Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Kerkau Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
type: Concept
created: 2021-03-03T16:08:14.998Z
notation: DE-ST-10
definition: The Kerkau fault zone is a subordinated basement fault south of the Arendsee diapir.
definition: Die Kerkau Störungszone bildet eine untergeordnete Sockelstörung im Süden des Salzstocks Arendsee. @de
preferred label: Kerkau-Störungszone @de
alternative label: Kerkau Fault
alternative label: Kerkau-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Schieben Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
type: Concept
created: 2021-03-03T16:08:15.088Z
notation: DE-ST-31
definition: The Schieben fault zone forms a small-scale and subordinate fault zone in the border area of the Altmark threshold and the Altmark-Fläming basin.
definition: Die Schieben Störungszone bildet eine kleinräumige und untergeordnete Störungszone im Grenzbereich der Altmark Schwelle und des Altmark-Fläming-Beckens. @de
preferred label: Schieben-Störungszone @de
alternative label: Schieben Fault
alternative label: Schieben-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Kuhfelde Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
type: Concept
created: 2021-03-03T16:08:15.084Z
notation: DE-ST-30
definition: The Kuhfelde fault zone forms a small-scale and subordinate fault zone in the border area of the Altmark threshold and the Altmark-Fläming basin.
definition: Die Kuhfelde Störungszone bildet eine kleinräumige und untergeordnete Störungszone im Grenzbereich der Altmark Schwelle und des Altmark-Fläming-Beckens. @de
preferred label: Kuhfelde-Störungszone @de
alternative label: Kuhfelde Fault
alternative label: Kuhfelde-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Fleetmark Fault Zone
type: Concept
created: 2021-03-03T16:08:15.081Z
notation: DE-ST-29
definition: The Fleetmark Fault Zone is a minor fault zone in northern Saxony-Anhalt.
definition: Die Fleetmark-Verwerfungszone ist eine kleinere Verwerfungszone in Nordsachsen-Anhalt. @de
preferred label: Fleetmark Störungszone @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Gifhorn Trough Eastern Border Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8097
type: Concept
created: 2021-03-03T16:08:15.039Z
notation: DE-ST-18
definition: The Gifhorn Trough Eastern Border Fault is a flat, detachment-related normal fault in the westernmost Altmark area. With large normal offsets of up to 7 km this NNE-SSW-trending fault system separates the Altmark Swell in the east towards the Gifhorn Trough in the west.
definition: Die Ostrandstörung des Gifhorn Trogs ist charakterisiert durch eine Vielzahl flacher, abgescherter Abschiebungen mit großen Versätzen von bis zu 7 km. Diese NNE-SSW-streichende Störungszone trennt die Altmark Schwelle im Osten gegen den Gifhorn Trog im Westen. @de
preferred label: Gifhorn Trog-Ostrand-Störungssystem @de
narrower: Diesdorf Fault Zone
narrower: Crestal Graben of Bonese and Waddekath diapirs
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Crestal Graben of Bonese and Waddekath diapirs
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8041
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-03-03T16:08:15.047Z
notation: DE-ST-20
definition: The Scheitelgraben Bonese-Waddekath forms a collaps structure on top of the Bonese and Waddekath diapirs.
definition: Der Scheitelgraben Bonese-Waddekath bildet eine Einbruchstruktur im Dachbereich der Salzstöcke Bonese und Waddekath. @de
preferred label: Scheitelgraben der Salzstöcke Bonese und Waddekath @de
broader: Gifhorn Trough Eastern Border Fault Zone

Diesdorf Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8068
references: https://data.geoscience.earth/ncl/geoera/ref/7994
references: https://data.geoscience.earth/ncl/geoera/ref/8071
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-03-03T16:08:15.043Z
notation: DE-ST-19
definition: The Diesdorf fault as well as minor faults near the Bonese and Waddekath diapirs are NNE-SSW-striking structures associated with a highly complex fault system at the outer eastern border of the Gifhorn Trough. The major fault of this system forms a mildly westward-dipping, bedding-parallel normal fault with associated antithetic normal faults in its hanging wall. In parts subordinated extensional detachments and duplexes occur between the Triassic salt horizons (Upper Buntsandstein and Middle Muschelkalk detachments) and the Zechstein evaporites. Thickness distribution (e.g., up to 1.5 km Middle Keuper strata in the vicinity of the Bonese/Waddekath diapirs) and a local hiatus between Buntsandstein and Upper Keuper (Arnstadt and Exter Fm.) strata suggest that major faulting occurred due to E-W-directed extension during Late Triassic (Karnian) times. During the Late Jurassic in parts this system became reactivated under extension/transtension as inferred by corresponding strata only preserved west of the Diesdorf fault.
definition: Die Diesdorfer Störungszone (Benox et al. 1997) bildet eine N-S streichende Störungszone, die sich in etwa in der Mitte zwischen den Salzstöcken Peckensen und Bonese auf einer Länge von ca. 7 km bis zur Landesgrenze zu Niedersachen erstreckt. Diese Störungszone, auf die bereits durch Arndt et al. (1978) hingewiesen wurde und die dort als zur Randsenke des Salzstocks Peckensen hin einfallende Störung gedeutet wurde, stellt auf Basis neuerer reflexionsseismischer Messungen (Hesche et al. 1985) einen im Intervall des Jura bis zu 1,5 km breiten Grabenbruch dar, dessen Grabeninneres durch mehrere Einzelbrüche gegliedert ist. Diese Einzelbrüche weisen allesamt ein Einfallen nach Osten hin auf. Im hier beschriebenen 3D-Modell ist die Störungszone durch zwei Einzelstörungen abgebildet, eine östliche und nach Westen einfallende Hauptabschiebung sowie deren antithetische Zweigstörung. Die Schnittlinie beider Störungen befindet sich innerhalb des Keuper-Intervalls, so dass die tieferen triassischen Einheiten einzig durch die Hauptabschiebung beeinflusst sind. In Richtung Norden verliert die Störungszone allmählich an Versatz und endet sie ungefähr 1 km südlich der Landesgrenze zu Niedersachsen. Ihre Südbegrenzung bilden die Störungen des Uelzener Lineaments zwischen den Salzstöcken Bonese und Peckensen. Auffällig an dieser Störungszone ist ihre Position relativ zu den sie umgebenden Störungszonen. So bildet sie im Bereich der westlichen Altmark ein relativ selten beobachtetes Lineament, das nur eng begrenzt auftritt und weder im Norden noch im Süden eine Fortsetzung oder Entsprechung findet. Hierbei weist die Störung relativ zur für diese Region strukturprägenden „Pauline-Störung“ eine prominente Position auf. Die Diesdorfer Störungszone befindet sich exakt über der Position der für die „Pauline-Störung“ beschriebenen Rampe im unteren und mittleren Buntsandstein. Diese Position liefert Hinweise auf ihre mögliche Entstehung und eventuelle genetische Zusammenhänge, weshalb die D… @de
preferred label: Diesdorf-Störungszone @de
alternative label: Diesdorf Fault
broader: Gifhorn Trough Eastern Border Fault Zone

Jahrstedt-Ristedt-Poppau-Apenburg Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8068
references: https://data.geoscience.earth/ncl/geoera/ref/7994
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:15.035Z
notation: DE-ST-17
definition: The Jahrstedt-Ristedt-Poppau-Apenburg fault zone forms a regional fault zone of the Arendsee lineament. It extends from the Lüge-Liesten diapir in the north to the Jahrstedt diapir in the south. In general, the fault zone forms a westward dipping normal fault that can be traced through the entire Mesozoic and large parts of the Cenozoic strata.
definition: Die Jahrstedt-Ristedt-Poppau-Apenburg Störungszone bildet eine regionale Störungszone des Arendsee-Lineaments. Sie erstreckt sich vom Salzstock Lüge-Liesten im Norden bis südlich des Salzstocks Jahrstedt. Generell bildet die Störungszone eine nach Westen einfallende Abschiebung, die sich durch die gesamte mesozoische und weite Teile känozoische Schichtenfolge hindurch verfolgen lässt. @de
preferred label: Jahrstedt-Ristedt-Poppau-Apenburg-Störungszone @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zone of the Altmark area

Fault zones of the Thuringian Basin
references: https://data.geoscience.earth/ncl/geoera/ref/8066
references: https://data.geoscience.earth/ncl/geoera/ref/8098
references: https://data.geoscience.earth/ncl/geoera/ref/8052
references: https://data.geoscience.earth/ncl/geoera/ref/8054
type: Concept
created: 2021-03-03T16:08:15.320Z
notation: DE-ST-5000
definition: NW-SE- and subordinated NNE-SSW-striking fault zones, long-wavelength folds and local Cenozoic depressions characterize the southern part of Saxony-Anhalt, which belong to larger structure referred to the Thuringian Basin. The deep Palaeozoic structure comprises NE-SW-trending faults and folds of the Rhenohercynian Zone in the west and the Saxothuringian Zone in the southeast of the former Rheic Suture Zone (Mid-German Crystalline Rise). This crystalline to low-grade metamorphic basement is segmented by the NE-SW-striking, Permocarboniferous ‘Saale Depression’ [Kuhnert, 1995; Schneider et al., 2005]. Faults and structures of Mesozoic age dominantly strike NW-SE and subdivide the northeastern Thuringian Syncline. In parts these faults border small basement uplifts (e.g., the Kyffhäuser Mountains, the Bottendorf High and the Hornburg Anticline) or separate local depressions in the Mesozoic cover against each other [Katzung and Ehmke, 1993]. Thereby, faults of the Thuringian Syncline typically show low normal or reverse offsets, which is probably due to reverse reactivation of former normal faults [cf. Kley, 2013; Malz, 2014 and references therein].
definition: NW-SE- und untergeordnete NNE-SSW-streichende Störungszonen, langwellige Falten und lokale känozoische Senken charakterisieren den südlichen Teil von Sachsen-Anhalt, der zu einer größeren Struktur gehört, dem Thüringer Becken. Die tiefe paläozoische Struktur umfasst NE-SW-streichende Störungen und Falten der Rhenoherzynischen Zone im Westen und der Saxothuringischen Zone im Südosten der ehemaligen Rheischen Sutur (repräsentiert durch die Mitteldeutsche Kristallinzone). Dieser kristalline bis niedriggradig metamorphe Sockel wird durch die NE-SW-streichende, permokarbone „Saale-Senke“ segmentiert [Kuhnert, 1995; Schneider et al., 2005]. Störungen und Strukturen des Mesozoikums streichen vorwiegend NW-SE und unterteilen die nordöstliche Thüringer Mulde in schmale "Leistenschollen". Teilweise grenzen diese Verwerfungen an kleine Sockelhebungen (z. B. das Kyffhäuser-Gebirge, der Bottendorfer Höhenzug und der Hornburger Sattel) oder an einzelne lokale Senken im Mesozoikum [Katzung und Ehmke, 1993]. Dabei zeigen Störungen in der Thüringer Mulde typischerweise niedrige Abschiebungs- und/oder Aufschiebungsversätze, die mit einer kompressiven Reaktivierung mesozoischer Abschiebungen während der späten Kreide zurückzuführen sind [vgl. Kley, 2013; Malz, 2014 und Referenzen darin]. @de
preferred label: Störungszonen des Thüringer Beckens @de
alternative label: Faults of the Thuringian Syncline
narrower: Halle Fault Zone
narrower: Blankenheim-Geiseltal Fault Zone
narrower: Hornburg Deep Fault System
narrower: Nienstedt-Eindorf Fault Zone
narrower: Kyffhäuser-Crimmitschau Fault Zone
narrower: Finne Fault Zone
narrower: Lützen-Zwenkau Fault Zone
narrower: Lauchstädt-Teutschenthal Fault Zone
narrower: Rosslau Fault Zone
narrower: Naumburg Fault Zone
narrower: Hettstedt Fault Zone
narrower: Zwochau-Elstertal Fault Zone
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Saxony-Anhalt

Lauchstädt-Teutschenthal Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/7989
references: https://data.geoscience.earth/ncl/geoera/ref/8071
references: https://data.geoscience.earth/ncl/geoera/ref/8067
type: Concept
created: 2021-03-03T16:08:15.369Z
notation: DE-ST-500
definition: The Lauchstädt-Teutschenthal fault zone forms a NW-SE trending fault system in southern Saxony-Anhalt.
definition: Die Lauchstädt-Teutschenthaler Störungszone bildet eine NW-SE streichende Störungszone im Süden Sachsen-Anhalts. @de
preferred label: Lauchstädt-Teutschenthaler Störungszone @de
narrower: Lauchstädt Fault Zone
narrower: Höhnstedt Fault Zone
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Thuringian Basin

Höhnstedt Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/7989
references: https://data.geoscience.earth/ncl/geoera/ref/8071
references: https://data.geoscience.earth/ncl/geoera/ref/8067
type: Concept
created: 2021-03-03T16:08:15.379Z
notation: DE-ST-84
definition: The Höhnstedt fault zone forms a NW-SE-trending fault strand of the Lauchstädt-Teutschenthal fault zone.
definition: Die Höhnstedt Störungszone bildet eine NW-SE-streichende Störungsspur der Lauchstädt-Teutschenthal Störungszone. @de
preferred label: Höhnstedter-Störungszone @de
alternative label: Höhnstedter Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Lauchstädt-Teutschenthal Fault Zone

Lauchstädt Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/7989
references: https://data.geoscience.earth/ncl/geoera/ref/8071
references: https://data.geoscience.earth/ncl/geoera/ref/8067
type: Concept
created: 2021-03-03T16:08:15.374Z
notation: DE-ST-66
definition: The Lauchstädt-Teutschenthal fault zone forms a NW-SE trending fault in the south of Saxony-Anhalt with offsets of up to 500 m.
definition: Die Lauchstädt-Teutschenthaler Störungszone bildet eine NW-SE streichende, etwa 500 m Sprunghöhe aufweisende Störung im Süden Sachsen-Anhalts. @de
preferred label: Lauchstädt-Störungszone @de
alternative label: Lauchstädt-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Lauchstädt-Teutschenthal Fault Zone

Lützen-Zwenkau Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8071
references: https://data.geoscience.earth/ncl/geoera/ref/8067
type: Concept
created: 2021-03-03T16:08:15.363Z
notation: DE-ST-65
definition: The Lützen-Zwenkau fault zone forms a geophysically proven SW-NE trending fault in the southeast of Saxony-Anhalt in the border area to Saxony.
definition: Die Lützen-Zwenkau Störungszone bildet eine geophysikalisch nachgewiesene SW-NE streichende Störung im Südosten Sachsen-Anhalts im Grenzbereich zu Sachsen. @de
preferred label: Lützen-Zwenkauer StörungSzone @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Thuringian Basin

Finne Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8103
references: https://data.geoscience.earth/ncl/geoera/ref/8018
references: https://data.geoscience.earth/ncl/geoera/ref/8019
references: https://data.geoscience.earth/ncl/geoera/ref/8065
type: Concept
created: 2021-03-03T16:08:15.358Z
notation: DE-ST-63
definition: The Finne Fault Zone forms a NW-SE trending fault zone crossing the Thuringian Basin over a distance of 150 km. It forms the southwestern border of the Hermundurian Block and is interpreted as part of the seismically active Gera-Jáchymov zone.
definition: Die Finne Störungszone bildet eine NW-SE-streichende, über 150 km verlaufende Störungszone im Norden des Thüringer Beckens. Sie bildet die südwestliche Grenze der Hermundurischen Scholle und wird als Teil der seismisch aktiven Gera-Jáchymov-Zone interpretiert. @de
preferred label: Finne-Störungszone @de
alternative label: Finne Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Thuringian Basin

Kyffhäuser-Crimmitschau Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8044
references: https://data.geoscience.earth/ncl/geoera/ref/8101
references: https://data.geoscience.earth/ncl/geoera/ref/8103
references: https://data.geoscience.earth/ncl/geoera/ref/8071
type: Concept
created: 2021-03-03T16:08:15.353Z
notation: DE-ST-62
definition: The Kyffhäuser-Crimmitschau fault zone forms a significant NW-SE trending fault zone that separates the Hermundurian Block in the southwest from the Merseburg Block in the northeast. The offset is largest in the area of the Kyffhauser mountains. Interpreted as part of the Gera-Jáchymov zone, it still shows seismic activity today.
definition: Die Kyffhäuser-Crimmitschau Störungszone bildet eine bedeutende NW-SE-streichende Störungszone, die die Hermundurische Scholle im Südwesten von der Merseburger Scholle im Nordosten trennt. Ihre größte Sprunghöhe zeigt die Störung im Bereich des Kyffhäusers. Als Teil der Gera-Jáchymov-Zone interpretiert zeigt sie immer noch seismische Aktivität in heutiger Zeit. @de
preferred label: Kyffhäuser-Crimmitschau-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Thuringian Basin

Nienstedt-Eindorf Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8071
references: https://data.geoscience.earth/ncl/geoera/ref/8044
references: https://data.geoscience.earth/ncl/geoera/ref/8067
type: Concept
created: 2021-03-03T16:08:15.349Z
notation: DE-ST-61
definition: The Nienstedt-Eindorfer fault zone forms a NW-SE trending, SW-dipping fault in the central section of the Sangerhäuser Syncline. It reaches maximum offsets of up to 300 m.
definition: Die Nienstedt-Eindorfer Störungszone bildet eine NW-SE streichende, nach Südwesten einfallende Störung im Zentralabschnitt der Sangerhäuser Mulde. Sie erreicht maximale Versätze von bis zu 300 m. @de
preferred label: Nienstedt-Eindorfer Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Thuringian Basin

Zwochau-Elstertal Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/7989
references: https://data.geoscience.earth/ncl/geoera/ref/8071
references: https://data.geoscience.earth/ncl/geoera/ref/8067
type: Concept
created: 2021-03-03T16:08:15.396Z
notation: DE-ST-600
definition: The Zwochau-Elstertal Fault describes a system of fault zones that strikes almost north-south and separates the Halle Block from the Northwest Saxony Block.
definition: Die Zwochau-Elstertal Störung beschreibt ein System von Störungszonen, die annähernd Nord-Süd streichen und die Halle Scholle von der Nordwestsächsischen Scholle trennen. @de
preferred label: Zwochau-Elstertal-Störungszone @de
narrower: Zwochau Fault Zone
narrower: Elstertal Fault Zone
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Thuringian Basin

Elstertal Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/7989
references: https://data.geoscience.earth/ncl/geoera/ref/8071
references: https://data.geoscience.earth/ncl/geoera/ref/8067
type: Concept
created: 2021-03-03T16:08:15.405Z
notation: DE-ST-92
definition: The Elstertal fault zone forms a fault branch of the Zwochau-Elstertal fault zone.
definition: Die Elstertal Störungszone bildet einen Störungsast der Zwochaus-Elstertal Störungszone. @de
preferred label: Elstertal-Störungszone @de
in scheme: Tectonic Boundary Objects in Europe
broader: Zwochau-Elstertal Fault Zone

Zwochau Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/7989
references: https://data.geoscience.earth/ncl/geoera/ref/8071
references: https://data.geoscience.earth/ncl/geoera/ref/8067
type: Concept
created: 2021-03-03T16:08:15.400Z
notation: DE-ST-91
definition: The Zwochau Fault Zone forms one fault strand of the Zwochau-Elstertal Fault.
definition: Die Zwochau Störungszone bildet einen Störungsast der Zwochau-Elstertal Störungszone. @de
preferred label: Zwochau-Störungszone @de
in scheme: Tectonic Boundary Objects in Europe
broader: Zwochau-Elstertal Fault Zone

Hornburg Deep Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/8099
references: https://data.geoscience.earth/ncl/geoera/ref/8042
references: https://data.geoscience.earth/ncl/geoera/ref/8043
references: https://data.geoscience.earth/ncl/geoera/ref/8044
type: Concept
created: 2021-03-03T16:08:15.344Z
notation: DE-ST-60
definition: The Hornburg Deep Fault System is a WSW-ENE trending fault zone in the north of the Thuringian Basin. It limits the Hornburger Sattel in the east. It shows offsets fluctuating over small distances reaching a maximum of 1500 m.
definition: Die Hornburger Tiefenstörung ist eine WSW-ENE streichende Störungszone im Norden des Thüringer Beckens. Sie begrenzt den Hornburger Sattel im Osten. Sie zeigt kleinräumig schwankende und maximal 1500 m betragende Versätze. @de
preferred label: Hornburger Tiefenstörung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Thuringian Basin

Hettstedt Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/7989
references: https://data.geoscience.earth/ncl/geoera/ref/8071
references: https://data.geoscience.earth/ncl/geoera/ref/8067
type: Concept
created: 2021-03-03T16:08:15.391Z
notation: DE-ST-86
definition: The Hettstedt fault zone describes a fault system in the area of the Halle-Hettstedt Anticline. This fault system separates the Subhercynian Basin from the Thuringian Basin and connects the basement uplifts of the Harz and the Halle-Wittenberg Block.
definition: Die Hettstedt Störungszone beschreibt ein Störungssystem im Bereich der Halle-Hettstedter Gebirgsbrücke. Dieses Störungssystem trennt das Subherzyne Becken vom Thüringer Becken und verbindet die Grundgebirgsaufbrüche des Harzes und der Halle-Wittenberg-Scholle. @de
preferred label: Hettstedt-Störungszone @de
alternative label: Hettstedter Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Thuringian Basin

Naumburg Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/7989
references: https://data.geoscience.earth/ncl/geoera/ref/8071
references: https://data.geoscience.earth/ncl/geoera/ref/8067
type: Concept
created: 2021-03-03T16:08:15.387Z
notation: DE-ST-83
definition: The Naumburg fault zone is a NE-SW trending fault zone in the north-eastern Thuringia basin postulated on the basis of gravity gradient studies.
definition: Die Naumburger Störungszone ist eine auf der Grundlage gravimetrischer Gradientenuntersuchungen postulierte NE-SW streichende Störungszone im nordöstlichen Thüringer Becken. @de
preferred label: Naumburger Störungszone @de
alternative label: Naumburg-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Thuringian Basin

Blankenheim-Geiseltal Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8052
references: https://data.geoscience.earth/ncl/geoera/ref/8071
references: https://data.geoscience.earth/ncl/geoera/ref/8041
type: Concept
created: 2021-03-03T16:08:15.330Z
notation: DE-ST-400
definition: The Blankenheim-Geiseltal fault zone describes the fault zone on the southern edge of the Hornburg anticline and its extension into the Geiseltal area in the southeast. It forms a fault zone that was already active in Permian times, which can be proven on the basis of differentiated sedimentation and magmatic activity.
definition: Die Blankenheim-Geiseltal Störungszone bezeichnet die Störungszone am Südrand des Hornburger Sattels sowie ihre Verlängerung in den Bereich des Geiseltals im Südosten. Sie bildet eine bereits im Perm aktive Störungszone aus, was auf Basis differenzierter Sedimentation und magmatischer Aktivität belegt werden kann. @de
preferred label: Blankenheim-Geiseltal-Störungszone @de
narrower: Hornburg Anticline Southern Border Fault
narrower: Geiseltal Fault Zone
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Thuringian Basin

Geiseltal Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8052
references: https://data.geoscience.earth/ncl/geoera/ref/8071
references: https://data.geoscience.earth/ncl/geoera/ref/8044
references: https://data.geoscience.earth/ncl/geoera/ref/8067
type: Concept
created: 2021-03-03T16:08:15.339Z
notation: DE-ST-64
definition: The Geiseltal Fault forms the eastern section of the Blankenheim-Geiseltal Fault Zone.
definition: Die Geiseltal Störung bezeichnet den östlichen Abschnitt der Blankenheim-Geiseltal Störungszone. @de
preferred label: Geiseltal-Störungszone @de
in scheme: Tectonic Boundary Objects in Europe
broader: Blankenheim-Geiseltal Fault Zone

Hornburg Anticline Southern Border Fault
references: https://data.geoscience.earth/ncl/geoera/ref/8067
references: https://data.geoscience.earth/ncl/geoera/ref/8071
references: https://data.geoscience.earth/ncl/geoera/ref/8043
references: https://data.geoscience.earth/ncl/geoera/ref/8044
type: Concept
created: 2021-03-03T16:08:15.334Z
notation: DE-ST-59
definition: The Hornburg Anticline Southern border fault forms the western section of the Blankenheim-Geiseltal fault zone. It delimits the Paleozoic units of the Hornburg Anticline in the north against the Mesozoic units of the Thuringian Basin in the south.
definition: Die Hornburger Sattel Südrandstörung bildet den westlichen Abschnitt der Blankenheim-Geiseltal Störungszone. Sie begrenzt die paläozoischen Einheiten des Hornburger Sattels im Norden gegen die Mesozoischen Einheites des Thüringer Beckens im Süden. @de
preferred label: Hornburger Sattel Südrand-Störung @de
alternative label: Hornburg Fault
alternative label: Hornburger Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Blankenheim-Geiseltal Fault Zone

Rosslau Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/7989
references: https://data.geoscience.earth/ncl/geoera/ref/8071
references: https://data.geoscience.earth/ncl/geoera/ref/8067
type: Concept
created: 2021-03-03T16:08:15.383Z
notation: DE-ST-82
definition: The Rosslau fault zone is a NE-SW-trending fault that forms the southeastern border of the Flechtingen High against the Halle-Wittenberg Block in the pre-cenozoic subsurface. It forms the border between the Northern Phyllite Zone and the Central German Crystalline Zone.
definition: Die Rosslau Störungszone ist eine NE-SW streichende Störung, die im präkänozoischen Untergrund die Südostgrenze der Flechtingen-Roßlauer Scholle gegen die Halle-Wittenberg Scholle bildet. Hierbei bildet sie die Grenze zwischen der Nördlichen Phyllitzone und der Mitteldeutschen Kristallinzone. @de
preferred label: Rosslauer Störungszone @de
alternative label: Rosslau-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Thuringian Basin

Halle Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8100
type: Concept
created: 2021-03-03T16:08:15.326Z
notation: DE-ST-58
definition: The Halle fault zone forms a W-E to NW-SE trending, slightly curved fault in the south of Saxony-Anhalt. It borders the Halle Porphyry Complex in the north against the Mesozoic strata of the northeastern Thuringian Basin in the south. With an offset of up to 1000 m, it forms one of the most significant fault zones in central Germany.
definition: Die Halle Störungszone bildet eine W-E bis NW-SE streichende, leicht geschwungen verlaufende Störung im Süden Sachsen-Anhalts. Sie begrenzt den Halleschen Porphyrkomplex im Norden gegen die mesozoische Schichtenfolge des nordöstlichen Thüringer Beckens im Süden. Mit einem Versatz von bis zu 1000 m bildet sie eine der bedeutsamsten Störungzonen in Mitteldeutschland. @de
preferred label: Hallesche Störungszone @de
alternative label: Halle Fault
alternative label: Hallesche Marktplatzverwerfung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Fault zones of the Thuringian Basin

Falha em Portugal
scope note: All named tectonic boundary objects that are located (at least partly) in Portugal, are identified by an ID with the prefix „PT“ listed in the notation.
narrower: Gerês-Lobios Fault
narrower: Monte Figo Fault
narrower: Martinhal Fault
narrower: Cercal Anticline Fault
narrower: Lousal-Caveira Anticline Fault
narrower: Vidigueira-Moura Fault
narrower: Amareleja Fault
narrower: Maranhão Fault
narrower: Santo Aleixo da Restauração Thrust
narrower: Juromenha Thrust
narrower: Alter do Chão Fault
narrower: Castelo de Vide Fault
narrower: Terena Thrust
narrower: Estremoz Antiform Fault
narrower: Ferrarias Antiform Fault
narrower: Ponsul Fault
narrower: Seia-Lousã Fault
narrower: Segura Fault
narrower: Alvados-Minde Fault System
narrower: Mendiga-Reguengo do Fetal Fault System
narrower: Rio Maior-Porto de Mós Fault
narrower: Candeeiros Fault
narrower: Cidral Fault
narrower: Caldas da Rainha diapiric structure
narrower: Nazaré Fault
narrower: Abrã Fault
narrower: Turquel Fault
narrower: Ferrel Fault
narrower: Lourinhã Fault
narrower: Torres Vedras Fault
narrower: Cercal-Candeeiros Fault
narrower: Areeiro Fault
narrower: Rocha Forte Fault
narrower: Tojeira Fault
narrower: Runa Fault System
narrower: Sapataria Fault
narrower: Sobral Fault
narrower: Almargem do Bispo Fault System
narrower: Dona Maria Fault
narrower: Sintra Fault System
narrower: Cascais Fault
narrower: São Julião-Barcarena Fault
narrower: Ajuda Fault
narrower: Forte da Baralha Fault
narrower: Cova da Mijona Fault
narrower: Sesimbra-Santana Fault
narrower: Vale do Brejo-Frade-Zambujal Fault
narrower: Galapos Fault
narrower: São Luís Fault
narrower: Palmela Fault
narrower: El Carmen Fault
narrower: Viso Fault
narrower: Ferreira-Ficalho Thrust
narrower: Pulo do Lobo Thrust
narrower: Galé Thrust
narrower: Mértola Thrust
narrower: Castro Verde Thrust
narrower: Neves Corvo Thrust
narrower: Ribeira de Vascão Fault
narrower: Alcoutim Fault
narrower: Ferreira-Pias Fault
narrower: Pedrogão fault
narrower: Campo Maior Fault
narrower: Ouguela Fault
narrower: Mosteiros Fault
narrower: Portalegre-Esperança Fault
narrower: Alegrete Fault
narrower: Ariques Fault
narrower: Alvaiázere Fault
narrower: Condeixa Fault
narrower: Quiaios Fault
narrower: Buçaco-Penedo de Góis Fault
narrower: S. Pedro Dias-Segade Fault
narrower: Portela de Unhais Fault
narrower: Ademoço Fault
narrower: Cebola Fault
narrower: Pé da Serra-Cartamil Fault
narrower: Vilar Barroco-Fajão Fault
narrower: Penacova-Régua-Verín Fault

Seia-Lousã Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7247
references: https://data.geoscience.earth/ncl/geoera/ref/7249
references: https://data.geoscience.earth/ncl/geoera/ref/7252
type: Concept
created: 2020-11-19T13:10:52.941Z
alternative label: Lousã Fault
alternative label: Falha de Lousã @pt
notation: PT-038
preferred label: Falha de Seia-Lousã @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6315
references: https://data.geoscience.earth/ncl/geoera/ref/988
definition: Extending between Lousã and Seia regions, this fault is a major structure limiting the Portuguese Central System in the north. It's interpreted as a late Variscan strike-slip, reactivated with an important reverse component, verging N, during the Mesozoic (Cretaceous) and the several Alpine compression episodes occurred in the Cenozoic. This fault conditions the occurrence of Caldas de S. Paulo water spring - Water temperature: 23º C.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Malpica-Lamego Fault
definition: This structure extend between Malpica (Spain) and Lamego (Portugal) regions and corresponds to an important shear zone with a complex tectonic history since pre‐Variscan to Variscan orogeny times. This structure conditions the occurrence of several water springs/sources - Water temperatures: < 20º C (Dossãos), 33º C (Caldelas), < 20º C (Giestal), 32º C (Caldas das Taipas), 50º C (Caldas de Vizela), 23º C (Caldas das Murtas/Pataratas), < 20º C (Varões).
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
type: Concept
created: 2020-11-19T13:10:56.631Z
notation: PT-148
preferred label: Falha de Malpica-Lamego @pt
references: https://data.geoscience.earth/ncl/geoera/ref/7252
references: https://data.geoscience.earth/ncl/geoera/ref/6335
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Segura Fault
type: Concept
created: 2020-11-19T13:10:52.967Z
notation: PT-039
preferred label: Falha de Segura @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6321
definition: This fault extends between Cegonhas Velhas and the Segura region, limiting, to the north, the Segura basin (Cenozoic), a subbasin located in the middle sector of the Lower Tagus Basin.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Ferrarias Antiform Fault
type: Concept
created: 2020-11-19T13:10:52.872Z
notation: PT-036
preferred label: Falha do Antiforma de Ferrarias @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6308
definition: This NW-SE structure is mapped along almost 3 km, next to Mina do Bugalho. It suffers a sinistral offset of about 2 km related with the Messejana Fault.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Mesão Frio Fault
definition: This fault is interpreted as a late Variscan sinistral strike-slip fault. This fault conditions the occurrence of several water springs - Water temperatures: 67º C (Termas de S. Pedro do Sul), < 20º C (Piar), < 20º C (Miguas/Ponte de Frende), 45º C (Caldas de Moledo) and 23º C (Seromenho).
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
type: Concept
created: 2020-11-19T13:10:56.572Z
notation: PT-146
preferred label: Falha de Mesão Frio @pt
references: https://data.geoscience.earth/ncl/geoera/ref/7252
references: https://data.geoscience.earth/ncl/geoera/ref/998
references: https://data.geoscience.earth/ncl/geoera/ref/7253
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Ponsul Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7247
references: https://data.geoscience.earth/ncl/geoera/ref/7252
type: Concept
created: 2020-11-19T13:10:52.906Z
notation: PT-037
preferred label: Falha do Ponsul @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6318
definition: In Portugal, the fault extends between Arneiro and Termas de Monfortinho areas. It's a late Variscan sinistral strike-slip fault, reactivated as a N verging reverse fault during the Cenozoic. It also coincides with the N limit of the Lower Tagus (Cenozoic) basin middle sector. It is one of the structures that accommodated the upflift of the Central System (Portuguese sector). This fault conditions the occurrence of Fonte das Virtdudes and Fonte Santa de Monfortinho water springs - Water temperatures: 21º C and 28º C, respectively.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Dúrico-Beirão Carboniferous Sulc Fault
definition: This structure extends between Apúlia and Janarde areas, and is an important Variscan structure in the control of the Carboniferous basins, in the region.
type: Concept
created: 2020-11-19T13:10:56.604Z
notation: PT-147
preferred label: Falha do Sulco Carbonífero Sulco-Beirão @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6351
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Morais Fault
definition: This fault causes a sinistral offset on the Morais Complex, probably related with late Variscan deformation, and shows evidence of reverse behaviour in the Quaternary. This fault, in apparently conjunction with Morais Nappe Complex (PT-137), conditions the occurrence of Fonte da Abelheira and Escarledo water springs - Water temperature: < 20º C on both cases.
type: Concept
created: 2020-11-19T13:10:56.515Z
notation: PT-144
preferred label: Falha de Morais @pt
references: https://data.geoscience.earth/ncl/geoera/ref/998
references: https://data.geoscience.earth/ncl/geoera/ref/988
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Estremoz Antiform Fault
type: Concept
created: 2020-11-19T13:10:52.841Z
notation: PT-035
preferred label: Carreamento do Antiforma de Estremoz @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6306
references: https://data.geoscience.earth/ncl/geoera/ref/6350
definition: It extends along aproximately 40 km between Alandroal and Sousel areas. It's an interpreted structure, consisting in a deformed overthrust by the folding event responsible for the Estremoz Antiform formation.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Manteigas-Vilariça-Bragança Fault
definition: This structure is a Variscan sinistral strike slip fault, reactivated along the Cenozoic with the same kinematic behaviour. This extensive structure conditions the occurrence of several water springs/sources - Water temperatures: 37º C (Unhais da Serra), 48º C (Caldas de Manteigas), < 20º C (Santo Amaro), < 20º C (Santo António), 34º C (Longroiva), 21º C (Currais do Leitão/Bem Saúde).
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
type: Concept
created: 2020-11-19T13:10:56.542Z
notation: PT-145
preferred label: Falha de Manteigas-Vilariça-Bragança @pt
references: https://data.geoscience.earth/ncl/geoera/ref/7252
references: https://data.geoscience.earth/ncl/geoera/ref/988
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Deixa-o-Resto Fault
type: Concept
created: 2020-07-20T13:36:23.042Z
preferred label: Falha de Deixa-o-Resto @pt
notation: PT-8
references: https://data.geoscience.earth/ncl/geoera/ref/1001
references: https://data.geoscience.earth/ncl/geoera/ref/1002
definition: Probably extending from Melides to Sines (and further south to the offshore), this fault has strongly influenced the tectonic and stratigraphic evolution of the region. It's also one of the main structures controling the western slope of the Grândola range.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Grândola Fault
type: Concept
created: 2020-07-20T13:36:23.015Z
preferred label: Falha de Grândola @pt
notation: PT-7
references: https://data.geoscience.earth/ncl/geoera/ref/1001
definition: This fault controls the northern face of the Grândola range, interpreted as a fault scarp. The real extension in unknown, however it is identifiable for about 45 km. It probably corresponds to an inherited variscan fault, reactivated with the alpine compression.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Carcavai Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
references: https://data.geoscience.earth/ncl/geoera/ref/7252
type: Concept
created: 2020-07-20T13:36:22.875Z
preferred label: Falha de Carcavai @pt
notation: PT-5
references: https://data.geoscience.earth/ncl/geoera/ref/1003
references: https://data.geoscience.earth/ncl/geoera/ref/1000
definition: Extending from Quarteira to São Brás de Alportel, it had an important role on the Algarve basin structuration during the Mesozoic. It was reactivated during the Cenozoic, related to the Alpine compression. This fault, in conjunction with the São Marcos-Quarteira Fault (PT-004), conditions the occurrence of Fonte Santa (Quarteira) water spring - Water temperature: 21º C.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Lower Tagus Valley Fault System
type: Concept
created: 2020-07-20T13:36:22.903Z
preferred label: Sistema de falhas do Vale Inferior do Tejo @pt
notation: PT-6
narrower: Azambuja Fault
narrower: Vila Franca de Xira Fault
narrower: Santa Iria Fault
references: https://data.geoscience.earth/ncl/geoera/ref/990
references: https://data.geoscience.earth/ncl/geoera/ref/987
definition: Lower Tagus Valley FS is an important structure in the genesis and evolution of the intermediate sector of the Cenozoic Lower Tagus basin. Its extension is uncertain because a major part of its course follows the present Tagus river channel, hidden bellow recent alluvium.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Santa Iria Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
type: Concept
created: 2020-07-20T13:36:22.986Z
preferred label: Falha de Santa Iria @pt
notation: PT-6-3
references: https://data.geoscience.earth/ncl/geoera/ref/994
definition: Mapped between São João da Talha e Vialonga areas, this fault is part of an important fault system in the tectono-stratigraphic evolution of the Cenozoic Lower Tagus basin. Apparently, this fault, in conjuction with Vila Franca de Xira Fault (PT-006-2), conditions the occurrence of Mouchão da Póvoa water spring - Water temperature: < 20º C.
in scheme: Tectonic Boundary Objects in Europe
broader: Lower Tagus Valley Fault System

Vila Franca de Xira Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
type: Concept
created: 2020-07-20T13:36:22.959Z
preferred label: Falha de Vila Franca de Xira @pt
notation: PT_6_2
references: https://data.geoscience.earth/ncl/geoera/ref/990
definition: This fault is mapped between Alverca do Ribatejo and Carregado areas. Part of it extends below the Tagus river alluvium. It was an important fault accomodating the Mesozoic extension, as a normal fault, and was tectonically inverted during the Cenozoic as a reverse fault. Apparently, this fault conditions the occurrence of Mouchão da Póvoa water spring: water temperature < 20º C.
in scheme: Tectonic Boundary Objects in Europe
broader: Lower Tagus Valley Fault System

Azambuja Fault
type: Concept
created: 2020-07-20T13:36:22.931Z
preferred label: Falha da Azambuja @pt
notation: PT-6-1
references: https://data.geoscience.earth/ncl/geoera/ref/991
definition: It enxtends from Azambuja to Almoster area (uncertain extension) and had an important role in the structuration of the Lower Tagus basin during the Cenozoic.
in scheme: Tectonic Boundary Objects in Europe
broader: Lower Tagus Valley Fault System

Ribeira de Telhares Fault System
type: Concept
created: 2020-07-20T13:36:23.098Z
preferred label: Sistema de Falhas da Ribeira de Telhares @pt
notation: PT-10
references: https://data.geoscience.earth/ncl/geoera/ref/996
definition: A fault system that extends between Nave Redonda and Corte de Briques. There are a group of tectonic depressions related to its activity along the Neogene and early Pleistocene, with clear morphological expression.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Mendiga-Reguengo do Fetal Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/7250
type: Concept
created: 2020-11-19T13:10:53.089Z
notation: PT-041
narrower: Reguengo do Fetal Fault
narrower: Mendiga Fault
references: https://data.geoscience.earth/ncl/geoera/ref/6313
references: https://data.geoscience.earth/ncl/geoera/ref/997
definition: Mendiga – Reguengo do Fetal fault system is inherited from late Variscan deformation. After Lower Cretaceous, Reguengo do Fetal fault behaved as a normal fault and Mendiga fault has a strike-slip. Apparently, this system fault conditions the occurrence of Lena and Liz karstic springs on Maciço Calcário Estremenho aquifer system - Water tempertures: < 20º C on both cases.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Mendiga Fault
type: Concept
created: 2020-11-19T13:10:53.158Z
notation: PT-041-2
preferred label: Falha da Mendiga @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6313
in scheme: Tectonic Boundary Objects in Europe
broader: Mendiga-Reguengo do Fetal Fault System

Reguengo do Fetal Fault
type: Concept
created: 2020-11-19T13:10:53.126Z
notation: PT-041-1
preferred label: Falha do Reguengo do Fetal @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6313
in scheme: Tectonic Boundary Objects in Europe
broader: Mendiga-Reguengo do Fetal Fault System

Vale de Fecho Fault
type: Concept
created: 2020-07-20T13:36:23.070Z
preferred label: Falha de Vale de Fecho @pt
notation: PT-9
references: https://data.geoscience.earth/ncl/geoera/ref/1001
definition: This fault extends approximately 14 km to the south, from São Teotónio. Its total extension is unknown. The deformation is directly expressed by one outcrop showing a fault zone affecting Plio-Quaternary continental sediments, and by the existence of a tectonic depression filled with Neogene and early Quaternary sediments.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Alvados-Minde Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/7250
type: Concept
created: 2020-11-19T13:10:52.996Z
notation: PT-040
preferred label: Sistema de falhas de Alvados-Minde @pt
narrower: Minde Fault
narrower: Alvados Fault
references: https://data.geoscience.earth/ncl/geoera/ref/6313
references: https://data.geoscience.earth/ncl/geoera/ref/997
definition: Alvados – Minde fault system separates Santo António plateau from Aire mountain range and São Mamede plateau, creating a deep depression in the Alvados and Minde area. The system functioned as normal fault during the Mesozoic distensive period leading to the roll-over structuring of São Mamede Plateau, being subsequently reactivated as a dextrogira lateral ramp of the Arrife thrust during the miocene inversion period. This fault system conditions the depressions of Alvados and Minde which, due to the various temporary karstic springs and swallow holes that occur there, constitute both recharge zones and discharge zones of the Maciço Calcário Estremenho aquifer system, the bigger and the most important karstic aquifer of Portugal - Water temperatures: < 20º C on all cases.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Alvados Fault
type: Concept
created: 2020-11-19T13:10:53.055Z
notation: PT-040-2
preferred label: Falha de Alvados @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6313
in scheme: Tectonic Boundary Objects in Europe
broader: Alvados-Minde Fault System

Minde Fault
type: Concept
created: 2020-11-19T13:10:53.028Z
notation: PT-040-1
preferred label: Falha de Minde @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6313
in scheme: Tectonic Boundary Objects in Europe
broader: Alvados-Minde Fault System

Torrão Fault
type: Concept
created: 2020-07-20T13:36:23.126Z
preferred label: Falha de Torrão @pt
notation: PT-11
references: https://data.geoscience.earth/ncl/geoera/ref/999
references: https://data.geoscience.earth/ncl/geoera/ref/1001
definition: Extending between Cuba and Vale de Arca areas, it was an important structure in the genesis and evolution of the Cenozoic Alvalade basin.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Vidigueira-Moura Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
references: https://data.geoscience.earth/ncl/geoera/ref/7252
type: Concept
created: 2020-11-19T13:10:52.598Z
notation: PT-027
preferred label: Falha de Vidigueira-Moura @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6310
definition: The fault extends about 65 km between Vidigueira and Moura. It acted as a sinistral strike-slip during the late Variscan fragile regime and was reactivated several times in the Cenozoic in relation with the Alpine orogeny, controling the tectonostratigraphic evolution of the Cenozoic Moura basin. Apparently, this fault not conditions the water sources of Termas de Moura located on the south of it - Water temperature: 22º C.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Morais Nappe Complex
definition: This correspond to a complex of nappes limited by overthrusts, consisting in a series of allocthonous and parautocthonous units emplaced over the Iberian Terrane during the Variscan orogeny.
type: Concept
created: 2020-11-19T13:10:56.298Z
notation: PT-137
preferred label: Complexo de Nappes de Morais @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6339
references: https://data.geoscience.earth/ncl/geoera/ref/6344
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Amareleja Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
type: Concept
created: 2020-11-19T13:10:52.630Z
notation: PT-028
preferred label: Falha de Amareleja @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6342
definition: This fault extends about 9 km between Amareleja and Póvoa. It seems responsible for the existence of a small tectonic scarp and controlled the neogenic sedimentation on the southern footwall block. ic evolution of the Cenozoic Lower Tagus basin. This fault conditions the occurrence of Fonte Santana water spring - Water temperature: < 20º C.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Vila Verde Fault
definition: This fault is a Variscan thrust.
references: https://data.geoscience.earth/ncl/geoera/ref/6338
type: Concept
created: 2020-11-19T13:10:56.333Z
notation: PT-138
preferred label: Falha de Vilaverde @pt
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Cercal Anticline Fault
type: Concept
created: 2020-11-19T13:10:52.532Z
notation: PT-025
preferred label: Falha do Anticlinal do Cercal @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6331
definition: This SW verging reverse fault is located along the western flank of the Cercal Anticline.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Trás-os-Montes Main Thrust
definition: This is a main structure separating the Central Iberian Zone and the Galicia - Trás-os-Montes Zone. This structure conditions the occurrence of Moimenta da Raia, Terronha and Lagoaça water springs - Water temperature: < 20º C, on all cases. It conditions too the Carvalhelhos spring - Water temperature: 22 ºC.
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
type: Concept
created: 2020-11-19T13:10:56.238Z
notation: PT-135
preferred label: Cavalgamento principal de Trás-os-Montes @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6339
references: https://data.geoscience.earth/ncl/geoera/ref/6344
references: https://data.geoscience.earth/ncl/geoera/ref/7252
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Lousal-Caveira Anticline Fault
type: Concept
created: 2020-11-19T13:10:52.566Z
notation: PT-026
preferred label: Falha do Anriclinal de Lousal-Caveira @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6332
definition: This SW verging reverse fault corresponds to a rupture along the SW flank of the Lousal-Caveira Anticline.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Bragança Nappe Complex
definition: This correspond to a complex of nappes limited by overthrusts, consisting in a series of allocthonous and parautocthonous units emplaced over the Iberian Terrane during the Variscan orogeny. This structure conditions the occurrence of Santa Cruz water spring - Water temperature: < 20º C.
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
type: Concept
created: 2020-11-19T13:10:56.271Z
notation: PT-136
preferred label: Complexo de Nappes de Bragança @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6339
references: https://data.geoscience.earth/ncl/geoera/ref/6344
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Vale de Asnes-Faílde Fault
definition: This fault is interpreted as a Variscan strike-slip. This fault conditions the occurrence of Alfaião water spring - Water temperature: < 15º C.
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
type: Concept
created: 2020-11-19T13:10:56.202Z
notation: PT-134
preferred label: Falha de Vale de Asnes-Faílde @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6322
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Castelo de Vide Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
references: https://data.geoscience.earth/ncl/geoera/ref/7252
type: Concept
created: 2020-11-19T13:10:52.782Z
notation: PT-033
preferred label: Falha de Castelo de Vide @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6337
definition: This fault is mapped between Santo Amaro and Meada areas, along 60 km, and is probably a late hercynian or alpine left-lateral strike slip fault, cutting through all the hercynian structure. At Castelo de Vide, a sinistral offset of about 300 m can be seen, affecting Ordovician quartzites. This fault conditions the occurrence of some water springs in Termas de Castelo de Vide (Fonte da Vila, Fonte Mealhada) and Cabeço de Vide (Termas da Sulfúrea) - Water temperatures: < 20º C on all cases.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Aveleda-Gimonde Fault
definition: This fault is interpreted as a oblique dextral late Variscan strike-slip. It conditions the occurrence of Alfaião water spring - Water temperature: < 15º C.
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
type: Concept
created: 2020-11-19T13:10:56.484Z
notation: PT-143
preferred label: Falha de Aveleda-Gimonde @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6327
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Terena Thrust
type: Concept
created: 2020-11-19T13:10:52.814Z
alternative label: Terena Overthrust
alternative label: Carreamento de Terena @pt
notation: PT-034
preferred label: Cavalgamento de Terena @pt
references: https://data.geoscience.earth/ncl/geoera/ref/998
definition: This fault is a Variscan structure located in the Barrancos-Elvas sector of the Ossa Morena Zone.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Juromenha Thrust
type: Concept
created: 2020-11-19T13:10:52.724Z
alternative label: Carreamento da Juromenha @pt
notation: PT-031
preferred label: Cavalgamento da Juromenha @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6307
definition: This fault extends between the Alter do Chão and Juromenha regions. It is considered an important structure in the Ossa Morena Zone, separating the Cambrian units of Alter do Chão-Elvas from Silurian rocks of Estremoz-Barrancos sectors.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Pena Suar Fault
definition: This fault is interpreted as a normal intra-orogenic fault with a sinistral component, during the Variscan orogeny.
type: Concept
created: 2020-11-19T13:10:56.423Z
notation: PT-141
preferred label: Falha de Pena Suar @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6314
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Messejana Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
type: Concept
created: 2020-07-20T13:36:22.791Z
alternative label: Odemira-Ávila Fault
alternative label: Falha de Odemira-Ávila @pt
preferred label: Falha da Messejana @pt
notation: PT-2
references: https://data.geoscience.earth/ncl/geoera/ref/988
definition: Extending about 250 km in Portugal (500 km in total), between São Teotónio and Campo Maior, it is the largest mapped fault in Portugal. Its fault trace frequently coincides with an igneous dyke intruded during the Lower Jurassic. It had an important role on the tectonic genesis and evolution of the Cenozoic Alvalade basin. This fault conditions the occurrence of Fonte da Graça (Ouguela) and S. João do Deserto (Aljustrel) water springs - Water temperatures: < 20º C on both cases.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Alter do Chão Fault
type: Concept
created: 2020-11-19T13:10:52.752Z
notation: PT-032
preferred label: Falha de Alter do Chão @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6333
definition: This fault corresponds to the northern border of the Alter do Chão-Elvas, in the Ossa Morena Zone domain. To the north there's the Tomar-Badajoz-Córdoba Shear Zone. It is recognized along aproximately 25 km, between Monforte and Alter do Chão regions.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Vinhais Fault
definition: This fault extends between the Vinhais and Bragança areas and is a Variscan sinistral strike-slip fault. This fault, in apparently conjunction with Bragança Nappe Complex (PT-136), conditions the occurrence of Castro de Avelãs water spring - Water temperature: < 20º C.
references: https://data.geoscience.earth/ncl/geoera/ref/7247
type: Concept
created: 2020-11-19T13:10:56.451Z
notation: PT-142
preferred label: Falha de Vinhais @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6326
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

São Teotónio-Aljezur-Sinceira Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/7246
type: Concept
created: 2020-07-20T13:36:22.764Z
preferred label: Sistema de falhas de São Teotónio-Aljezur-Sinceira @pt
notation: PT-1
references: https://data.geoscience.earth/ncl/geoera/ref/992
references: https://data.geoscience.earth/ncl/geoera/ref/993
definition: It extends about 45 km between Sagres and São Teotónio, where it connects to the Messejana fault. Along the fault trace there are several tectonic depressions related to its strike-slip kinematics during the Cenozoic. This fault conditions the occurrence of Sinceira (Vila do Bispo) water spring - Water temperature: < 20º C.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Maranhão Fault
type: Concept
created: 2020-11-19T13:10:52.658Z
notation: PT-029
preferred label: Falha do Maranhão @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6342
references: https://data.geoscience.earth/ncl/geoera/ref/6317
definition: This fault is interpreted as a late Hercynian reverse fault that was reactivaded as a right-lateral strike slip during the Alpine compression. Altough related deformation was recognized from Montargil lake to about 30 km to SE, its total lenght is still uncertain.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Vila Flôr-Aguiar da Beira Fault
definition: This fault is interpreted as a Variscan strike-slip. It conditions the occurrence of Fonte Santa do Seixo, Lagarteira and, apparently, Caldas da Cavaca water springs/sources - Water temperatures: 21º C, < 20º C and 29º C, respectively.
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
type: Concept
created: 2020-11-19T13:10:56.360Z
notation: PT-139
preferred label: Falha de Vila Flôr-Aguiar da Beira @pt
references: https://data.geoscience.earth/ncl/geoera/ref/7252
references: https://data.geoscience.earth/ncl/geoera/ref/998
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

São Marcos-Quarteira Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
references: https://data.geoscience.earth/ncl/geoera/ref/7252
type: Concept
created: 2020-07-20T13:36:22.847Z
preferred label: Falha de São Marcos Quarteira @pt
notation: PT-4
references: https://data.geoscience.earth/ncl/geoera/ref/1003
references: https://data.geoscience.earth/ncl/geoera/ref/989
definition: Extending from Quarteira to São Marcos da Serra it had an important role on the Algarve basin structuration during the Mesozoic. It was reactivated during the Cenozoic in relation to the Alpine compression. This fault, in conjunction with the Carcavai Fault (PT-005), conditions the occurrence of Fonte Santa (Quarteira) water spring - Water temperature: 21º C.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Santo Aleixo da Restauração Thrust
type: Concept
created: 2020-11-19T13:10:52.691Z
alternative label: Santo Aleixo da Restauração Overthrust
alternative label: Carreamento de Santo Aleixo da Restauração @pt
notation: PT-030
preferred label: Cavalgamento de Santo Aleixo da Restauração @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6309
definition: It's a major structure in the Ossa Morena Zone, separating the Montemor-Ficalho and Estremoz-Barrancos sectors.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Santa Comba-Covilhã Fault
definition: This fault is interpreted as a late Variscan sinistral strike-slip. It conditions the occurrence of Cótimos and Vilares water springs - Water temperatures: < 20º C on both cases.
references: https://data.geoscience.earth/ncl/geoera/ref/7247
type: Concept
created: 2020-11-19T13:10:56.392Z
notation: PT-140
preferred label: Falha de Santa Comba-Covilhã @pt
references: https://data.geoscience.earth/ncl/geoera/ref/998
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Arrife Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7250
type: Concept
created: 2020-07-20T13:36:22.819Z
preferred label: Falha do Arrife @pt
notation: PT-3
references: https://data.geoscience.earth/ncl/geoera/ref/997
definition: From Casais Monizes to Serra de Baixo, it had an important role in the fracturation of Pangea and the opening of the Atlantic as a normal fault; has been reactived as strike-slip with reverse component during the Alpine orogeny, promoting the Lusitanian basin Inversion. This fault conditions the occurrence of Alviela and Almonda water springs, the two most flowing karstic exsurgencies of Portugal - Water temperatures: < 20º C on both cases.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Quiaios Fault
type: Concept
created: 2020-11-19T13:10:54.965Z
notation: PT-093
preferred label: Falha de Quiaios @pt
references: https://data.geoscience.earth/ncl/geoera/ref/988
definition: This fault extends between Ereira and Murtinheira. It is a local structure that accommodated the shortening promoted by the Alpine compression.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Celorico de Basto Nappe Complex
definition: This correspond to a complex of nappes limited by overthrusts, consisting in a series of allocthonous and parautocthonous units emplaced over the Iberian Terrane during the Variscan orogeny.
type: Concept
created: 2020-11-19T13:10:55.957Z
notation: PT-126
preferred label: Complexo de Nappes de Celorico de Basto @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6339
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Vila Verde fault
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
references: https://data.geoscience.earth/ncl/geoera/ref/998
created: 2020-11-20T09:44:15.568Z
preferred label: Falha de Vila Verde @pt
notation: PT-049
type: Concept
definition: NNW-SSW fault, extending from the coast, near Caldas da Rainha, to SSW until the Tagus river, close to Vila franca de Xira. This fault conditions the occurrence of Convento da Visitação water spring - Water temperature: < 20º C.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Castanheiro do Norte-Nagozelo Fault
definition: This fault is interpreted as a late Variscan sinistral strike-slip. Apparently, this fault conditions the occurrence of Caldas de Carlão, Caldas de S. Lourenço and Ponte do Fumo water springs - Water temperatures: 29ºC (Carlão), 30º C (S. Lourenço) and < 20º C (Ponte de Fumo).
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
type: Concept
created: 2020-11-19T13:10:55.988Z
notation: PT-127
preferred label: Falha de Castanheiro do Norte-Nagozelo @pt
references: https://data.geoscience.earth/ncl/geoera/ref/7252
references: https://data.geoscience.earth/ncl/geoera/ref/6352
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Alvaiázere Fault
definition: N-S Fault that borders the Ariques Mountain range. It is a major listric fault parallel to Porto-Tomar Fault which is the boundary of Lusitanian Mesozoic basin
type: Concept
created: 2020-11-19T13:10:54.901Z
notation: PT-091
preferred label: Falha de Alvaiázere @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6305
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Ortiga-Torrão Fault
definition: This fault corresponds to the Ossa Morena Zone/Central Iberian Zone in the Tomar-Sardoal-Ferreira do Zêzere sector.
type: Concept
created: 2020-11-19T13:10:55.899Z
notation: PT-124
preferred label: Falha de Ortiga-Torrão @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6348
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Condeixa Fault
type: Concept
created: 2020-11-19T13:10:54.936Z
notation: PT-092
preferred label: Falha de Condeixa @pt
references: https://data.geoscience.earth/ncl/geoera/ref/998
definition: This fault extends through Condeixa city until Coimbra city. It is a normal fault that originated in the opening of the Lusitanian Basin.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Casal da Igreja-Sardoal Fault
definition: This structure extends between the Casal da Igreja and Sardoal areas and marks the boundary between the Fontes metagraywacks and phyllites, and the Mouriscas Gnaissic Complex.
type: Concept
created: 2020-11-19T13:10:55.930Z
notation: PT-125
preferred label: Falha de Casal da Igreja-Sardoal @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6348
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Alegrete Fault
definition: This fault crosses Alegrete village. It is a transcurrent fault of the southern border of the Centro Iberica tectonostratigraphic zone.
type: Concept
created: 2020-11-19T13:10:54.840Z
notation: PT-089
preferred label: Cavalgamento de Alegrete @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6340
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Ariques Fault
definition: N-S oriented Fault that borders the Alvaiázere Mountain range. It is a major listric fault parallel to Porto-Tomar Fault, which is the boundary of Lusitanian Mesozoic basin. This fault conditions the occurrence of Agroal water spring - Water temperature: < 20º C.
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
type: Concept
created: 2020-11-19T13:10:54.873Z
notation: PT-090
preferred label: Falha de Ariques @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6305
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Mosteiros Fault
definition: This transcurrent fault extends between Crato and Campo Maior, and is one of the major faults that defines the Coimbra-Cordoba Shear Zone, wich makes the frontier between Ossa Morena and Centro Ibérica tectono stratigraphic zone of tha Iberian Massif.
type: Concept
created: 2020-11-19T13:10:54.775Z
notation: PT-087
preferred label: Falha de Mosteiros @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6340
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Portalegre-Esperança Fault
definition: This fault extends between Portalegre city and Esperança village. It is a transcurrent fault of the southern border of Centro Iberica tectonostratigraphic zone.
type: Concept
created: 2020-11-19T13:10:54.809Z
notation: PT-088
preferred label: Cavalgamento de Portalegre-Esperança @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6340
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Campo Maior Fault
definition: Campo Maior fault is one of the southern faults of the Coimbra-Cordoba shear zone wich makes the frontier between Ossa Morena and Centro Ibérica tectono stratigraphic zones of tha Iberian Massif.
type: Concept
created: 2020-11-19T13:10:54.715Z
notation: PT-085
preferred label: Falha de Campo Maior @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6340
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Ouguela Fault
definition: Ouguela fault is one of the southern faults of Coimbra-Cordoba shear zone wich makes the boundary between Ossa Morena and Centro Ibérica tectono stratigraphic zones of the Iberian Massif. This fault, in conjunction with the Messejana Fault (PT-002), conditions the occurrence of Fonte da Graça (Ouguela) water spring - Water temperature: < 20º C .
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
type: Concept
created: 2020-11-19T13:10:54.748Z
notation: PT-086
preferred label: Falha de Ouguela @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6340
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Pedrogão fault
type: Concept
created: 2020-11-19T13:10:54.680Z
notation: PT-084
preferred label: Falha de Pedrogão @pt
references: https://data.geoscience.earth/ncl/geoera/ref/998
definition: The fault crosses the locality of Pedrogão. It acted as a sinistral strike-slip during the late Variscan fragile regime and was reactivated several times in the Cenozoic in relation with the Alpine orogeny.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Martinhal Fault
type: Concept
created: 2020-11-19T13:10:52.503Z
notation: PT-024
preferred label: Falha de Martinhal @pt
references: https://data.geoscience.earth/ncl/geoera/ref/992
definition: This fault is observed at Martinhal beach, near Sagres, consisting of a reverse fault affecting Upper Jurassic and Pliocene-Pleistocene sands. Measured striae also point to the existence of dextral movement.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Outeiro-Avinhó Fault
definition: This fault is interpreted as a Variscan dextral strike-slip.
type: Concept
created: 2020-11-19T13:10:56.144Z
notation: PT-132
preferred label: Falha de Outeiro-Avinhó @pt
references: https://data.geoscience.earth/ncl/geoera/ref/998
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Monte Figo Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
references: https://data.geoscience.earth/ncl/geoera/ref/7252
type: Concept
created: 2020-11-19T13:10:52.469Z
notation: PT-023
preferred label: Falha de Monte Figo @pt
references: https://data.geoscience.earth/ncl/geoera/ref/1003
definition: The fault extends in about 10 km between Estói and Moncarapacho. It is interpreted as a northwards directed thrust and the existence of sheared and folded Upper Jurassic beds overlain by undeformed Lower Cretaceous indicates a compressive episode on the Jurassic/Cretaceous boundary, intercalated in a distensive regime. Apparently, in conjuction with Silves Benaciate Fault (PT-112), it conditions the occurrence of Olheiros water spring - Water temperature: <20º C.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Alfândega da Fé-Almendra Fault
definition: This fault is interpreted as a Variscan fragile structure.
type: Concept
created: 2020-11-19T13:10:56.174Z
notation: PT-133
preferred label: Falha de Alfândega da Fé-Almendra @pt
references: https://data.geoscience.earth/ncl/geoera/ref/998
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Porto-Tomar-Ferreira do Alentejo Shear Zone
definition: This structure is a main fracture zone in Iberia, establishing the boundary between the Ossa Morena Zone and Central Portuguese Zone, in its northern sector, and the boundary between the Ossa Morena Zone and the South Portuguese Zone, in its southern sector. This structure conditions the occurrence of some water spring/sources - Water temperatures: 23º C (Caldinhas de Vilar), 23º C (Caldas de S. Jorge), < 15º C (Vale da Mó), 27º C (Termas de Luso) and < 20º C (Foz do Sertã).
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
type: Concept
created: 2020-11-19T13:10:56.082Z
notation: PT-130
preferred label: Zona de Cisalhamento Porto-Tomar-Ferreira do Alentejo @pt
references: https://data.geoscience.earth/ncl/geoera/ref/7252
references: https://data.geoscience.earth/ncl/geoera/ref/6319
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Pinhal Novo-Alcochete Fault
definition: This fault presented extensional kinematic during the Mesozoic and was reactivated in the Cenozoic as a left lateral strike-slip fault.
type: Concept
created: 2020-11-19T13:10:56.110Z
notation: PT-131
preferred label: Falha de Pinhal Novo-Alcochete @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6330
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Praia Norte fault
definition: This fault is interpreted as a Variscan sinistral strike-slip.
type: Concept
created: 2020-11-19T13:10:56.018Z
notation: PT-128
preferred label: Falha de Praia Norte @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6334
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Vilarouco-Vale de Janeiro Fault
definition: This fault is interpreted as a Variscan sinistral strike-slip.
type: Concept
created: 2020-11-19T13:10:56.049Z
notation: PT-129
preferred label: Falha de Vilarouco-Vale de Janeiro @pt
references: https://data.geoscience.earth/ncl/geoera/ref/998
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Alcoutim Fault
type: Concept
created: 2020-11-19T13:10:54.620Z
notation: PT-082
preferred label: Falha de Alcoutim @pt
references: https://data.geoscience.earth/ncl/geoera/ref/998
definition: NE-SW cenozoic fault that extends throught Pomarão anticline
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Antas Fault
definition: Occurring next to Antas, this fault is part of a set of structures that delimit fragments of oceanic lithosphere (ophiolite sequences).
type: Concept
created: 2020-11-19T13:10:55.632Z
notation: PT-115
preferred label: Falha de Antas @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6336
references: https://data.geoscience.earth/ncl/geoera/ref/998
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Ferreira-Pias Fault
type: Concept
created: 2020-11-19T13:10:54.647Z
notation: PT-083
preferred label: Falha de Ferreira-Pias @pt
references: https://data.geoscience.earth/ncl/geoera/ref/998
definition: The fault extends between Ferreira do Alentejo and Pias. It acted as a sinistral strike-slip fault during the late Variscan fragile regime and was reactivated several times in the Cenozoic in relation with the Alpine orogeny.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Santana Fault
definition: Occurring near Santana, this fault is part of a set of structures that delimit fragments of oceanic lithosphere (ophiolite sequences).
type: Concept
created: 2020-11-19T13:10:55.666Z
notation: PT-116
preferred label: Falha de Santana @pt
references: https://data.geoscience.earth/ncl/geoera/ref/998
references: https://data.geoscience.earth/ncl/geoera/ref/6336
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Neves Corvo Thrust
type: Concept
created: 2020-11-19T13:10:54.557Z
notation: PT-080
preferred label: Cavalgamento de Neves Corvo @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6345
definition: This thrust limit the southern limb of Rosario anticline where the Neves Corvo mine is located.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Ribeira de Vascão Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7247
type: Concept
created: 2020-11-19T13:10:54.589Z
notation: PT-081
preferred label: Falha da Ribeira do Vascão @pt
references: https://data.geoscience.earth/ncl/geoera/ref/998
definition: NE-SW cenozoic fault of the Pomarão anticline that extends along the Vascão stream. This fault conditions the occurrence of Águas Santas de Besteiros (Vascão) water spring - Water temperature: 21º C.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Vila Ruiva Fault
definition: Occurring next to Vila Ruiva, this fault is part of a set of structures that delimit fragments of oceanic lithosphere (ophiolite sequences).
type: Concept
created: 2020-11-19T13:10:55.599Z
notation: PT-114
preferred label: Falha de Vila Ruiva @pt
references: https://data.geoscience.earth/ncl/geoera/ref/998
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Mértola Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/7247
type: Concept
created: 2020-11-19T13:10:54.497Z
notation: PT-078
preferred label: Cavalgamento de Mértola @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6345
definition: Limits the Mértola nappe at the South Portuguese tectono stratigraphic zone. This thrust conditions the occurrence of Mértola and Água Santa da Morena water springs - Water temperatures: < 20º C on both cases.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Castro Verde Thrust
type: Concept
created: 2020-11-19T13:10:54.530Z
notation: PT-079
preferred label: Cavalgamento de Castro Verde @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6345
definition: The Castro Verde thrust limits a major anticline near Castro Verde village, where Neves-Corvo mine is located.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Pulo do Lobo Thrust
type: Concept
created: 2020-11-19T13:10:54.432Z
notation: PT-076
preferred label: Cavalgamento de Pulo do Lobo @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6345
definition: This thrust makes the south limit of Pulo do Lobo accretionary terrane at the South Portuguese tectono stratigraphic zone
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Galé Thrust
type: Concept
created: 2020-11-19T13:10:54.464Z
notation: PT-077
preferred label: Cavalgamento da Galé @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6345
definition: Limits the Galé-Cela nappe at the South Portuguese tectono stratigraphic zone
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Viso Fault
type: Concept
created: 2020-11-19T13:10:54.369Z
notation: PT-074
preferred label: Falha do Viso @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6322
definition: Major thrust of the Viso assymmetric anticline, northwest of Setúbal.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Ferreira-Ficalho Thrust
type: Concept
created: 2020-11-19T13:10:54.403Z
notation: PT-075
preferred label: Cavalgamento de Ferreira Ficalho @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6345
definition: Major thrust that mark the boundary between Ossa Morena and South Portuguese tectono-stratigraphic zones. This boundary corresponds to a Variscan suture between the Iberian and Avalonia terranes and was first interpreted as corresponding to the Beja-Acebuches Ophiolitic Complex. It extends from the spanish border (Ficalho) to west, near Ferreira do Alentejo.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

São Brás de Alportel fault
type: Concept
created: 2020-07-20T13:36:23.432Z
preferred label: Falha de São Brás de Alportel @pt
notation: PT-22
references: https://data.geoscience.earth/ncl/geoera/ref/992
definition: The fault extends between Alportel and Aceifãos. It has morphological expression represented by a scarp, facing S, and accommodated part of the Caldeirão range uplift, during the Quaternary.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Albufeira Fault
type: Concept
created: 2020-07-20T13:36:23.293Z
preferred label: Falha de Albufeira @pt
notation: PT-17
references: https://data.geoscience.earth/ncl/geoera/ref/1003
references: https://data.geoscience.earth/ncl/geoera/ref/992
definition: This fault extends between Ponta da Baleeira and Mourição. It accommodated the Mesozoic extension as a normal fault and was tectonically inverted during the Cenozoic, as a left lateral strike slip. It's an important structure controlling local diparism (the Albufeira diapir).
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Baleeira Fault
type: Concept
created: 2020-07-20T13:36:23.265Z
preferred label: Falha da Baleeira @pt
notation: PT-16
references: https://data.geoscience.earth/ncl/geoera/ref/992
definition: The fault extends between Albufeira and Pêra, approximately. It accommodated the Mesozoic extension as a normal fault and was tectonically inverted during the Cenozoic, as a reverse dextral fault.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Faro Fault
type: Concept
created: 2020-07-20T13:36:23.348Z
preferred label: Falha de Faro @pt
notation: PT-19
references: https://data.geoscience.earth/ncl/geoera/ref/995
references: https://data.geoscience.earth/ncl/geoera/ref/992
definition: The extension of this fault is unknown. It was inferred from geophysical data and sedimentary facies analysis. It's an important structure in the control of local diapirism.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Loulé fault
type: Concept
created: 2020-07-20T13:36:23.320Z
preferred label: Falha de Loulé @pt
notation: PT-18
references: https://data.geoscience.earth/ncl/geoera/ref/1003
references: https://data.geoscience.earth/ncl/geoera/ref/992
definition: Extending between Loulé and Boliqueime, the Loulé fault behaved as a normal fault during the Mesozoic extensive and as a sinistral normal fault in the Pleistocene.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Lagos Fault
type: Concept
created: 2020-07-20T13:36:23.182Z
alternative label: Porto de Mós Fault
alternative label: Falha de Porto de Mós @pt
preferred label: Falha de Lagos @pt
notation: PT-13
references: https://data.geoscience.earth/ncl/geoera/ref/1003
references: https://data.geoscience.earth/ncl/geoera/ref/992
definition: The fault extends from Canelas to Porto de Mós beach, where a reverse fault affecting Cretaceous and Miocene sediments can be observed. It behaved as a normal fault during the Mesozoic.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Portimão Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
type: Concept
created: 2020-07-20T13:36:23.154Z
preferred label: Falha de Portimão @pt
notation: PT-12
references: https://data.geoscience.earth/ncl/geoera/ref/1003
references: https://data.geoscience.earth/ncl/geoera/ref/992
definition: From Guenos to Praia da Rocha (Portimão) in Portugal mainland, this fault extends further south to the offshore. It is interpreted as a late Variscan structure reactivated during the Mesozoic and Cenozoic. Apparently, thid fault, in conjuction with Silves Benaciate Fault (PT-112), conditions the occurrence of Seixosas/Ferragudo water spring - Water temperature: < 20º C.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Barão de São João Fault
type: Concept
created: 2020-07-20T13:36:23.237Z
preferred label: Falha de Barão de São João @pt
notation: PT-15
references: https://data.geoscience.earth/ncl/geoera/ref/992
definition: It extends between Candeira and Ponte da Torre and one of its main characteristic consists in a well preserved fault scarp.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Espiche-Odiáxere Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
type: Concept
created: 2020-07-20T13:36:23.210Z
preferred label: Falha de Espiche-Odiáxere @pt
notation: PT-14
references: https://data.geoscience.earth/ncl/geoera/ref/1003
references: https://data.geoscience.earth/ncl/geoera/ref/992
definition: The fault extends from Burgau to Monte Judeu. It accommodated the Mesozoic extension as a normal fault and was tectonically inverted during the Cenozoic, as a reverse fault. It conditions the Salema, Valverde and Meia Praia water springs - Water temperatures: < 20º C on all cases.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Olalhas Fault
definition: This structure is located in the Olalhas area and corresponds to a tectonic klippe.
type: Concept
created: 2020-11-19T13:10:55.869Z
alternative label: Olalhas Klippe
alternative label: Klippe de Olalhas @pt
notation: PT-123
preferred label: Falha de Olalhas @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6348
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Rosmaninhal-Casal Novo Fault
definition: This fault extends between the Rosmaninhal and Casal Novo areas.It is related with Variscan deformation in the meridional sector of the Central Iberian Zone.
type: Concept
created: 2020-11-19T13:10:55.812Z
notation: PT-121
preferred label: Falha de Rosmaninhal-Casal Novo @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6346
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

São José das Matas-Gargantada Fault
definition: This fault extends between the São José das Matas and Gargantada areas. It is related with Variscan deformation in the meridional sector of the Central Iberian Zone.
type: Concept
created: 2020-11-19T13:10:55.842Z
notation: PT-122
preferred label: Falha de São José das Matas-Gargantada @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6346
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Casa Branca Shear Zone
definition: This structure is part of a corridor of ductile deformation known as the Montemor-o-Novo Shear Zone.
type: Concept
created: 2020-11-19T13:10:55.753Z
notation: PT-119
preferred label: Zona de Cisalhamento de Casa Branca @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6341
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Eira de Agosto Fault
type: Concept
created: 2020-07-20T13:36:23.404Z
preferred label: Falha de Eira de Agosto @pt
notation: PT-21
references: https://data.geoscience.earth/ncl/geoera/ref/992
definition: The fault extends between Alportel and Carrasqueiro. It has a morphological expression represented by a scarp, facing SW, and accommodated part of the Caldeirão range uplift, during the Quaternary.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Queixopêrra-Louriceira Fault
definition: This fault extends between the Queixopêrra and Louriceira areas.It is related with Variscan deformation in the meridional sector of the Central Iberian Zone.
type: Concept
created: 2020-11-19T13:10:55.780Z
notation: PT-120
preferred label: Falha de Queixopêrra-Louriceira @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6346
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Santo Estevão Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
references: https://data.geoscience.earth/ncl/geoera/ref/7252
type: Concept
created: 2020-07-20T13:36:23.376Z
preferred label: Falha de Santo Estevão @pt
notation: PT-20
references: https://data.geoscience.earth/ncl/geoera/ref/992
definition: The extension of this fault is unknown but it probably extends between the Olhão and Castro Marim areas. This fault conditions the occurrence of Santo António/Atalaia and Fonte Salgada water springs - Water temperature: 25º C and < 20º C, respectively. Apparently, in conjuction with Monte Figo Fault (PT-023), this fault conditions too the Olheiros water spring - Water temperature: < 20º C.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Oriola Fault
definition: Occurring next to Oriola, this fault is part of a set of structures that delimit fragments of oceanic lithosphere (ophiolite sequences).
type: Concept
created: 2020-11-19T13:10:55.694Z
notation: PT-117
preferred label: Falha de Oriola @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6336
references: https://data.geoscience.earth/ncl/geoera/ref/998
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Boa Fé Shear Zone
definition: This structure is the northern limit of a corridor of ductile deformation known as the Montemor-o-Novo Shear Zone.
type: Concept
created: 2020-11-19T13:10:55.723Z
notation: PT-118
preferred label: Zona de Cisalhamento de Boa Fé @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6341
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

São Luís Fault
type: Concept
created: 2020-11-19T13:10:54.278Z
notation: PT-071
preferred label: Cavalgamento de São Luís @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6322
definition: Major thrust of the São Luís assymmetric anticline, northwest of Setúbal.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Chão das Servas-Carregais Fault
definition: This structure is a SW verging thrust that occurs along the NE flank of the Vila Velha de Ródão syncline. It is related with the Variscan orogeny deformation.
type: Concept
created: 2020-11-19T13:10:55.298Z
notation: PT-104
preferred label: Falha de Chão das Servas-Carregais @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6329
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Palmela Fault
type: Concept
created: 2020-11-19T13:10:54.305Z
notation: PT-072
preferred label: Escama de Palmela @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6322
definition: Gravitational Collapse structure near Palmela village.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Sobral Fernando Fault
definition: This fault, with unknown extension, is interpreted as Variscan lateral ramp reactivated as a dextral strike-slip during the late Variscan tectonic episodes.
type: Concept
created: 2020-11-19T13:10:55.325Z
notation: PT-105
preferred label: Falha de Sobral Fernando @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6329
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Vale do Brejo-Frade-Zambujal Fault
type: Concept
created: 2020-11-19T13:10:54.214Z
notation: PT-069
preferred label: Falha de Vale do Brejo-Frade-Zambujal @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6322
definition: NW-SE fault diverging radially from the Sesimbra diapiric structure.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Galapos Fault
type: Concept
created: 2020-11-19T13:10:54.247Z
notation: PT-070
preferred label: Falha de Galapos @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6322
definition: Galapos Fault is a major thrust extending from Galapos beach to Risco, to the west.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Cova da Mijona Fault
type: Concept
created: 2020-11-19T13:10:54.157Z
notation: PT-067
preferred label: Falha da Cova da Mijona @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6322
definition: This fault is one of the Cova da Mijona dome border, west of Sesimbra village.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Sesimbra-Santana Fault
type: Concept
created: 2020-11-19T13:10:54.185Z
notation: PT-068
preferred label: Falha de Sesimbra-Santana @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6322
definition: Major fault bordering the Sesimbra diapiric structure.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Ajuda Fault
type: Concept
created: 2020-11-19T13:10:54.092Z
notation: PT-065
preferred label: Falha da Ajuda @pt
references: https://data.geoscience.earth/ncl/geoera/ref/998
definition: Strike slip fault extending throught the western sector of Lisbon.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Forte da Baralha Fault
type: Concept
created: 2020-11-19T13:10:54.123Z
notation: PT-066
preferred label: Falha do Forte da Baralha @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6322
definition: This fault is the west border of Forte da Baralha horst, near Espichel cape.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

São Julião-Barcarena Fault
type: Concept
created: 2020-11-19T13:10:54.060Z
notation: PT-064
preferred label: Falha de São Julião-Barcarena @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6324
definition: Normal fault crossing the city of Oeiras.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Silves-Benaciate Fault
definition: This fault extends between the Silves and Benaciate areas. Apparently, in conjuction with Porimão Fault (PT-012), it conditions the occurrence of Seixosas/Ferragudo water spring - Water temperature: < 20º C
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
type: Concept
created: 2020-11-19T13:10:55.537Z
notation: PT-112
preferred label: Falha de Silves-Benaciate @pt
references: https://data.geoscience.earth/ncl/geoera/ref/998
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Peroguarda Fault
definition: This fault is mapped between the Trigaches and Monte da Barrada areas, north of Ferreira do Alentejo.
type: Concept
created: 2020-11-19T13:10:55.569Z
notation: PT-113
preferred label: Falha de Peroguarda @pt
references: https://data.geoscience.earth/ncl/geoera/ref/998
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Algibre Fault System
definition: This fault is mapped between the Algibre and Querença areas, in Algarve. It behaved as a normal fault during the Mesozoic and suffered tectonic inversion, as a reverse fault, during the Cenozoic Alpine compression. This fault system conditions the occurrence of Benémola water spring - Water temperature: < 20º C.
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
type: Concept
created: 2020-11-19T13:10:55.481Z
alternative label: Algibre Fault
alternative label: Falha de Algibre @pt
notation: PT-110
preferred label: Sistema de falhas de Algibre @pt
references: https://data.geoscience.earth/ncl/geoera/ref/1003
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Carvalhal-Amendoeira Fault
type: Concept
created: 2020-11-19T13:10:55.508Z
notation: PT-111
preferred label: Falha de Carvalhal-Amendoeira @pt
references: https://data.geoscience.earth/ncl/geoera/ref/998
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Assumadas-Freixo Seco Fault
definition: This fault extends between Assumada and Freixo Seco, Algarve. It's a north verging reverse fault, affecting the Triassic Silves Formation and the Carboniferous Mira Formation.
type: Concept
created: 2020-11-19T13:10:55.418Z
notation: PT-108
preferred label: Falha de Assumadas-Freixo Seco @pt
references: https://data.geoscience.earth/ncl/geoera/ref/998
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

São Brás de Alportel-Julião Fault
definition: This fault extends between São Brás de Alportel and Julião, in Algarve. It is probably related with the basin inversion episodes related with the Alpine orogeny.
type: Concept
created: 2020-11-19T13:10:55.451Z
notation: PT-109
preferred label: Falha de São Brás de Alportel-Julião @pt
references: https://data.geoscience.earth/ncl/geoera/ref/998
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

El Carmen Fault
type: Concept
created: 2020-11-19T13:10:54.335Z
notation: PT-073
preferred label: Falha de El Carmen @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6322
definition: El Carmen Fault is mainly a normal fault, being reactivated as a thrust in the Miocene Alpine orogeny. It extends northwards, from Galapos beach.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Galdins-Rapoula-Chão da Vã Fault
definition: This fault is the northern limit of the Cenozoic Sarzedas basin (subbasin of the Lower Tagus basin) and was active during the Neogene compressive episodes related to the Alpine orogeny. It is one of the structures that accommodated the upflift of the Central System (Portuguese sector). This fault conditions the occurrence of Foz do Cobrão water spring - Water temperature: 20º C.
references: https://data.geoscience.earth/ncl/geoera/ref/7248
type: Concept
created: 2020-11-19T13:10:55.358Z
notation: PT-106
preferred label: Falha de Galdins-Rapoula-Chão da Vã @pt
references: https://data.geoscience.earth/ncl/geoera/ref/988
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Sobreira Formosa-Grade-Sobral do Campo Fault
definition: This fault is one of the main structures that accommodated the upflift of the Portuguese Central System in its southern sector.
type: Concept
created: 2020-11-19T13:10:55.391Z
notation: PT-107
preferred label: Falha de Sobreira Formosa-Grade-Sobral do Campo @pt
references: https://data.geoscience.earth/ncl/geoera/ref/988
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Sintra Fault System
type: Concept
created: 2020-11-19T13:10:53.948Z
notation: PT-062
preferred label: Sistema de Falhas de Sintra @pt
narrower: Sintra/Galamares Thrust
narrower: São João das Lampas Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/6324
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Sintra/Galamares Thrust
type: Concept
created: 2020-11-19T13:10:53.976Z
notation: PT-062-1
preferred label: Cavalgamento de Sintra/Galamares @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6324
definition: Sintra/Galamares thrust is north vergent and was formed during the cenozoic tectonic inversion.
in scheme: Tectonic Boundary Objects in Europe
broader: Sintra Fault System

São João das Lampas Thrust
type: Concept
created: 2020-11-19T13:10:54.004Z
notation: PT-062-2
preferred label: Cavalgamento de São João das Lampas @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6324
definition: São João das Lampas thrust verges to the north and was formed during the cenozoic tectonic inversion.
in scheme: Tectonic Boundary Objects in Europe
broader: Sintra Fault System

Buçaco-Penedo de Góis Fault
type: Concept
created: 2020-11-19T13:10:54.992Z
notation: PT-094
preferred label: Falha de Buçaco-Penedo de Góis @pt
references: https://data.geoscience.earth/ncl/geoera/ref/998
definition: This fault extends along the Buçaco-Penedo de Góis syncline, controlling its SW flank.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Dona Maria Fault
type: Concept
created: 2020-11-19T13:10:53.914Z
notation: PT-061
preferred label: Falha de Dona Maria @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6324
definition: The Dona Maria fault extends from Almargem do Bispo to south of Dona Maria village.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Sobral Fault
type: Concept
created: 2020-11-19T13:10:53.759Z
notation: PT-059
preferred label: Falha do Sobral @pt
references: https://data.geoscience.earth/ncl/geoera/ref/998
definition: Sobral fault is a major normal fault that intersects the Upper Jurassic Arruda sub-basin near Sobral de Monte Agraço village. This fault is in continuity with Santa Iria fault (PT006-3).
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Almargem do Bispo Fault System
type: Concept
created: 2020-11-19T13:10:53.787Z
notation: PT-060
narrower: Pero Pinheiro Fault
narrower: Cortegaça Fault
narrower: Almargem do Bispo Fault
references: https://data.geoscience.earth/ncl/geoera/ref/6324
definition: This N-S fault system is an extensional structure formed during the cenozoic inversion tectonic event.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Almargem do Bispo Fault
type: Concept
created: 2020-11-19T13:10:53.879Z
notation: PT-060-3
preferred label: Falha de Almargem do Bispo @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6324
definition: This structure is, possibly, a conjugate of the Cortegaça fault, and extends from Almargem do Bispo to near Negrais.
in scheme: Tectonic Boundary Objects in Europe
broader: Almargem do Bispo Fault System

Pero Pinheiro Fault
type: Concept
created: 2020-11-19T13:10:53.817Z
notation: PT-060-1
preferred label: Falha de Pero Pinheiro @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6324
definition: This structure extends between the areas of Almargem do Bispo and Sobral da Abelheira.
in scheme: Tectonic Boundary Objects in Europe
broader: Almargem do Bispo Fault System

Cortegaça Fault
type: Concept
created: 2020-11-19T13:10:53.852Z
notation: PT-060-2
preferred label: Falha de Cortegaça @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6324
definition: This structure is paralel to Pero Pinheiro fault and extends between A-dos-Francos and the Enxara do Bispo area.
in scheme: Tectonic Boundary Objects in Europe
broader: Almargem do Bispo Fault System

Vinagra-Foz do Cobrão Fault
definition: This structure is a NE verging thrust that occurs along the SW flank of the Vila Velha de Ródão syncline. It is related with the Variscan orogeny deformation. This fault, in apparently conjunction with Galdins-Rapoula-Chão da Vã Fault (PT-106), conditions the occurrence of Foz do Cobrão water spring - Water temperature: 20º C.
references: https://data.geoscience.earth/ncl/geoera/ref/7248
type: Concept
created: 2020-11-19T13:10:55.270Z
notation: PT-103
preferred label: Falha de Vinagra-Foz do Cobrão @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6329
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Penacova-Régua-Verín Fault
definition: This fault extends between the Penacova (Portugal) and Verín (Spain) regions and is interpreted as a late Variscan sinistral strike-slip fault, reactivated in the Cenozoic during the Alpine compression with the same kinematics. This extensive structure conditions the occurrence of several water springs/sources (Caldas de Penacova, Termas do Carvalhal; Pedras Salgadas, Vila Verde/Areal, Fonte Salus, Termas de Vidago, Caldas de Chaves and Vilarelho da Raia) - Water temperatures: <20º C (Penacova), 41º C (Carvalhal), <20º C (Pedras Salgadas), <15º C (V. Verde/Areal), <20º C (Fonte Salus); <15º C (Termas de Vidago), <77º C (Chaves), <20º C (Vilharelho).
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
references: https://data.geoscience.earth/ncl/geoera/ref/7251
type: Concept
created: 2020-11-19T13:10:55.210Z
notation: PT-101
preferred label: Falha de Penacova-Régua-Verín @pt
references: https://data.geoscience.earth/ncl/geoera/ref/988
references: https://data.geoscience.earth/ncl/geoera/ref/6349
references: https://data.geoscience.earth/ncl/geoera/ref/7252
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Monforte da Beira Fault
definition: This fault extends along the quartzite crest of Monforte da Beira, affecting Cambrian and Ordovician rocks.
type: Concept
created: 2020-11-19T13:10:55.243Z
notation: PT-102
preferred label: Falha de Monforte da Beira @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6347
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Pé da Serra-Cartamil Fault
definition: This structure occurs along the NE flank of the Serra do Moradal-Fajão Variscan syncline.
type: Concept
created: 2020-11-19T13:10:55.147Z
notation: PT-099
preferred label: Falha de Pé da Serra-Cartamil @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6328
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Vilar Barroco-Fajão Fault
definition: This structure extends along the SW flank of the Serra do Moradal-Fajão Variscan syncline.
type: Concept
created: 2020-11-19T13:10:55.178Z
notation: PT-100
preferred label: Falha de Vilar Barroco-Fajão @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6328
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Ademoço Fault
definition: This fault has unkown extension and is interpreted as a Variscan sinistral strike-slip fault.
type: Concept
created: 2020-11-19T13:10:55.084Z
notation: PT-097
preferred label: Falha de Ademoço @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6328
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Cebola Fault
definition: This fault is interpreted as a late Variscan strike-slip fault causing a dextral offset on the Serra do Moradal-Fajão syncline.
type: Concept
created: 2020-11-19T13:10:55.116Z
notation: PT-098
preferred label: Falha de Cebola @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6328
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

S. Pedro Dias-Segade Fault
type: Concept
created: 2020-11-19T13:10:55.025Z
notation: PT-095
preferred label: Falha de S. Pedro Dias-Segade @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6349
definition: Extending between S. Pedro Dias and Segade areas, this structure is related with an important compression episode in the Alpine orogeny context.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Cascais Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
type: Concept
created: 2020-11-19T13:10:54.032Z
notation: PT-063
preferred label: Falha de Cascais @pt
references: https://data.geoscience.earth/ncl/geoera/ref/7252
references: https://data.geoscience.earth/ncl/geoera/ref/6324
definition: This dextral srike slip fault extends from Cascais to NW, near Guincho beach. Apparently, this fault conditions the occurrence of Termas do Estoril water springs/sources - Water temperature: 35º C.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Portela de Unhais Fault
definition: This fault extends between Meãs and Senhora da Peneda, and is related with the Portela de Unhais quartzite ridge.
type: Concept
created: 2020-11-19T13:10:55.056Z
notation: PT-096
preferred label: Falha de Portela de Unhais @pt
references: https://data.geoscience.earth/ncl/geoera/ref/998
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Gerês-Lobios Fault
created: 2021-01-19T13:53:34.870Z
type: Concept
notation: PT-149
definition: This fault is an important fracture, well represented in the morphology by a long straight valley. It conditions the occurrence of Caldas do Gerês water spring - Water temperature: 47º C .
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
references: https://data.geoscience.earth/ncl/geoera/ref/7252
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Tojeira Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
type: Concept
created: 2020-11-19T13:10:53.610Z
notation: PT-056
preferred label: Falha de Tojeira @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6316
definition: Thrust fault located west of the Montejunto anticline. This fault, in conjunction with the Vila Verd Fault (PT-049), conditions the occurrence of Convento da Visitação water spring - Water temperature: < 20º C.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Runa Fault System
type: Concept
created: 2020-11-19T13:10:53.638Z
notation: PT-057
narrower: Runa Fault
narrower: Sizandro Fault
references: https://data.geoscience.earth/ncl/geoera/ref/998
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Runa Fault
type: Concept
created: 2020-11-19T13:10:53.667Z
notation: PT-057-1
preferred label: Falha de Runa @pt
references: https://data.geoscience.earth/ncl/geoera/ref/998
definition: N-S trending fault that establishes the west boundary of the Cretaceous Runa sub-basin. This sub-basin separates the Upper Jurassic sub-basins of Arruda and Turcifal.
in scheme: Tectonic Boundary Objects in Europe
broader: Runa Fault System

Sizandro Fault
type: Concept
created: 2020-11-19T13:10:53.699Z
notation: PT-057-2
preferred label: Falha do Sizandro @pt
references: https://data.geoscience.earth/ncl/geoera/ref/998
definition: N-S trending fault that establishes the west boundary of the Cretaceous Runa sub-basin. This sub-basin separates the Upper Jurassic sub-basins of Arruda and Turcifal.
in scheme: Tectonic Boundary Objects in Europe
broader: Runa Fault System

Areeiro Fault
type: Concept
created: 2020-11-19T13:10:53.549Z
notation: PT-054
preferred label: Falha de Areeiro @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6316
definition: Fault affecting the northern limb of Montejunto anticline.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Rocha Forte Fault
type: Concept
created: 2020-11-19T13:10:53.577Z
notation: PT-055
preferred label: Falha de Rocha Forte @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6316
definition: This thrust fault is located at the northen sector of the Montejunto Structure and has a vergence to the north.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Torres Vedras Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
type: Concept
created: 2020-11-19T13:10:53.493Z
notation: PT-052
preferred label: Falha de Torres Vedras @pt
references: https://data.geoscience.earth/ncl/geoera/ref/7252
references: https://data.geoscience.earth/ncl/geoera/ref/6316
definition: E-W fault near Torres Vedras city, extending to the east until the Montejunto Mountain range. Main movement as normal fault in relation with the Mesozoic Atlantic opening, later reactivated as a reverse fault during the Alpine orogeny. This fault conditions the occurrence of Cucos water spring group - Water temperature: 40º C.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Cercal-Candeeiros Fault
type: Concept
created: 2020-11-19T13:10:53.522Z
notation: PT-053
preferred label: Falha de Cercal-Candeeiros @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6316
definition: This fault extends between the Montejunto and Candeeiros mountain ranges. It behaved as a normal fault during the Mesozoic Atlantic opening, later reactivated as a reverse fault during the Alpine orogeny.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Lourinhã Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
type: Concept
created: 2020-11-19T13:10:53.459Z
notation: PT-051
preferred label: Falha da Lourinhã @pt
references: https://data.geoscience.earth/ncl/geoera/ref/7252
references: https://data.geoscience.earth/ncl/geoera/ref/998
definition: NNE-SSW trending fault, extending from Serra del Rei to near de Vimeiro diapir, to the south. The Lourinhã fault is rooted in the paleozoic basement as showed by seismic profiles. This fault conditions the occurrence of Vimeiro water spring group - Water temperature: 26º C.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Sapataria Fault
type: Concept
created: 2020-11-19T13:10:53.727Z
notation: PT-058
preferred label: Falha da Sapataria @pt
references: https://data.geoscience.earth/ncl/geoera/ref/998
definition: N-S normal fault extending between Sapataria and Lousa villages.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Caldas da Rainha diapiric structure
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
references: https://data.geoscience.earth/ncl/geoera/ref/7252
type: Concept
created: 2020-11-19T13:10:53.277Z
notation: PT-045
preferred label: Estrutura diapirica de Caldas da Rainha @pt
references: https://data.geoscience.earth/ncl/geoera/ref/997
definition: This structure extends from the area of Valado dos Frades until the south of Óbidos. Its eastern sector limits the western border of Estremenho Limestone Massif, in the so-called Bombarral Basin - Alcobaça. The Caldas da Rainha Diapiric structure was active during the Cenozoic. This diapiric structure conditions the occurrence of Caldas da Rainha, Óbidos (Gaeiras), Salir do Porto and Águas Santas water springs - Water temperatures: 36º C (Caldas da Rainha), 29º C (Óbidos), 20º C (Salir do Porto) and < 20º C (Águas Santas).
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Nazaré Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
references: https://data.geoscience.earth/ncl/geoera/ref/7252
type: Concept
created: 2020-11-19T13:10:53.307Z
notation: PT-046
preferred label: Falha da Nazaré @pt
references: https://data.geoscience.earth/ncl/geoera/ref/997
definition: Nazaré Fault is a first order tectonic strtucture wich separates two differente domains of Lusitanian basin. This fault extends from the Nazaré region, on the coast, to Pombal. This fault conditions the occurrence of Piedade, Fonte Quente and Porto Moniz water springs - Water temperatures: 27º C (Piedade), 24º C (Fonte Quente) and < 20º C (Porto Moniz).
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Candeeiros Fault
type: Concept
created: 2020-11-19T13:10:53.217Z
notation: PT-043
preferred label: Falha de Candeeiros @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6313
references: https://data.geoscience.earth/ncl/geoera/ref/997
definition: It behaved as a normal fault at least during the Middle Jurassic. Its southernmost section was reactivated during the Miocene. It extends from the east region of Évora de Alcobaça to near Porto de Mós, to the north.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Cidral Fault
type: Concept
created: 2020-11-19T13:10:53.250Z
notation: PT-044
preferred label: Falha do Cidral @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6313
references: https://data.geoscience.earth/ncl/geoera/ref/997
definition: This structure limits the Pliocene Rio Maior Basin to the East. It is related with diapiric tectonics and behaved as a normal fault during the Pliocene.
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Rio Maior-Porto de Mós Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7246
references: https://data.geoscience.earth/ncl/geoera/ref/7247
type: Concept
created: 2020-11-19T13:10:53.186Z
notation: PT-042
preferred label: Falha de Rio Maior-Porto de Mós @pt
references: https://data.geoscience.earth/ncl/geoera/ref/997
references: https://data.geoscience.earth/ncl/geoera/ref/6313
references: https://data.geoscience.earth/ncl/geoera/ref/7252
definition: The Rio Maior-Porto de Mós fault is a major fault rooted in the paleozoic basement. Its reactivation and the existent diapiric structure are related. This fault conditions the occurrence of Salgadas (Batalha) and Fonte da Pipa (Rio Maior) water springs/sources - Water temperatures: 23º C (Salgadas) and < 20º C (Fonte da Pipa).
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Ferrel Fault
type: Concept
created: 2020-11-19T13:10:53.432Z
notation: PT-050
preferred label: Falha de Ferrel @pt
references: https://data.geoscience.earth/ncl/geoera/ref/6312
definition: This fault extends along the coast line located north of Peniche (near Ferrel).
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Abrã Fault
type: Concept
created: 2020-11-19T13:10:53.340Z
notation: PT-047
preferred label: Falha de Abrã @pt
references: https://data.geoscience.earth/ncl/geoera/ref/998
definition: N-S Fault that intersects the igneous breccia of Abrã
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Turquel Fault
type: Concept
created: 2020-11-19T13:10:53.368Z
notation: PT-048
preferred label: Falha de Turquel @pt
references: https://data.geoscience.earth/ncl/geoera/ref/998
definition: NW-SE fault that crosses the Caldas da Rainha diapiric structure extending from Famalicao (NW) to Turquel and Benedita (SE).
in scheme: Tectonic Boundary Objects in Europe
broader: Falha em Portugal

Tectonic Boundary in Slovenia
preferred label: Prelomi v Sloveniji @sl
type: Concept
top concept of: Tectonic Boundary Objects in Europe
created: 2020-08-19T13:00:01.678Z
notation: SI-000
narrower: Raba Fault System
narrower: Pöls-Lavanttal Fault System
narrower: Periadriatic-Mid-Hungarian Large-scale Fault System
narrower: Dinaric Fault System
narrower: External Dinaric Thrust and Fold Belt
narrower: Adriatic-Apulian Foreland Thrust System
narrower: South Alpine Thrust and Fold Belt
narrower: Idrija Triassic Fault Set
scope note: All named tectonic boundary objects that are located (at least partly) in Slovenia, are identified by an ID with the prefix „SI“ listed in the notation. Fault systems and/or fault domains can cross political borders and are therefore shared by several countries. Therefore, they can contain faults from different countries, indicated by country-specific prefixes to the respective ID.
definition: Fault in Slovenia displayed in the HIKE European fault database. Information on faults in Slovenia are based on the map and database of active faults in Slovenia (MAF.SI) which includes all known active, probably active and potentially active faults with surface fault traces >5 km in length.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8761

Pöls-Lavanttal Fault System
preferred label: Pölsko-Labotski prelomni sistem @sl
references: https://data.geoscience.earth/ncl/geoera/ref/726
references: https://data.geoscience.earth/ncl/geoera/ref/749
references: https://data.geoscience.earth/ncl/geoera/ref/1148
references: https://data.geoscience.earth/ncl/geoera/ref/823
references: https://data.geoscience.earth/ncl/geoera/ref/831
notation: SI-3
notation: AT-137
type: Concept
created: 2020-04-30T14:27:00.849Z
definition: This ca. 150 km long, approximately NW-SE, partly NNW-SSE trending Fault System extends from the Pöls Valley (south of Trieben) to Judenburg and Obdach, following the Lavant Valley to Lavamünd (Labot) and Drauburg (Dravograd) and the Mislinja Valley (SLO) to Slovenske Konjice (south of the Pohorje Mountains). There it is cut by the Sava-Celje-Faultsystem. It includes the Pöls (Decker et al. 1994), Lavanttal Subfault Systems (Linzer et al., 2002; Kurz et al., 2011) and the Labot Fault (Fodor et al., 1998). A continuation into the Drau (Drava) Subfault System is expected. It shows a long-lasting history, with initial shear zones and faults in the Koralpe region during Cretaceous times. It was reactivated as right-lateral strike-slip faults during Miocene to Pliocene times and syn-tectonic basin formation of Fohnsdorf, Obdach and Lavant. Rates of 10-20 km horizontal (Fodor et al., 1998, Linzer et al, 2002 and references therein) and 2-5 km vertical (Kurz et al., 2011) displacement are described. According to Frisch et al., (2000) a displacement of the Periadriatic Fault System by 20 km is suggested.
definition: Dieses etwa NNW-SSE-streichende ca. 150 km lange Störungssystem verläuft vom Pölstal (südlich Trieben) über Judenburg und Obdach ins Lavanttal und über Lavamünd (Labot) nach Drauburg (Dravograd) weiter ins Mislinja-Tal (SLO) und bis Slovenske Konjice (südlich des Pohorje-Gebirge), wo sie ins Sava-Sostanje-Donat-Störungssystem übergeht bzw. von diesem abgeschnitten wird. Sie setzt sich aus der Pöls- (Decker et al. 1994), Lavanttal-Störung (Linzer et al., 2002; Kurz et al., 2011) und Labot-Störung (Fodor et al., 1998) zusammen. Die Bewegungsphasen lassen sich in mehrere Zeitabschnitte untergliedern: So wird eine Initiierung entlang von Scherzonen und Störungen im Gebiet der Koralpe während der Oberkreide bis Paläogen diskutiert. Ihre Hauptprägung erfuhr sie im Miozän bis Pliozän mit dextral-seitenverschiebender Kinematik, Bildung/Einsenkung der miozänen Fohnsdorf-, Obdach-, Lavanttal-Becken und Versatzweiten von 10-18 km horizontal (Fodor et al., 1998, Linzer et al, 2002 und die darin aufgeführten Referenzen) und 2-5 km vertikal (Kurz et al., 2011) sowie ein Versatz des Periadriatische Lienament-Störungssystem von bis zu 20 km wird angenommen (Frisch et al., 2000). @de
preferred label: Pöls-Lavanttal-Störungssystem @de
narrower: Bretstein Fault
narrower: Pöls Fault
narrower: Hirschegg Fault
narrower: Lavanttal Fault
narrower: Obdach Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Slovenia
broader: Tectonic Boundary in Austria

Pöls Fault
references: https://data.geoscience.earth/ncl/geoera/ref/726
notation: AT-10264
type: Concept
created: 2020-04-30T14:27:00.906Z
preferred label: Pöls-Störung @de
definition: The NNW-SSE trending fault along the valley of the Pöls is part of the Pöls-Lavantal Faultsystem and runs from Oberzeiring through St. Joahnn am Tauern to west of Hohentauern. A left-lateral displacement of 12 km is described (Decker et al., 1994).
definition: Die NNW-SSE-streichende Störung entlang des Pölstales ist Teil des Pöls-Lavanttal-Störungssystems und verläuft von Oberzeiring durch St. Johann am Tauern bis westlich von Hohentauern. Ein sinistraler Versatz von 12 km wird angenommen (Decker et al., 1994). @de
in scheme: Tectonic Boundary Objects in Europe
broader: Pöls-Lavanttal Fault System

Bretstein Fault
definition: Die NW-SE-streichende Störung entlang des Bretsteinbaches verläuft von Oberzeiring etwa 20 km in Richtung NW und wird dem Pöls-Lavanttal Störungssystem zugeordnet (Tollmann, 1986). @de
references: https://data.geoscience.earth/ncl/geoera/ref/732
notation: AT-10024
type: Concept
created: 2020-04-30T14:27:00.877Z
preferred label: Bretstein-Störung @de
definition: The NW-SE trending fault running in the valley of the Bretsteinbach extends from Oberzeiring about 20 km in NW direction and belongs to the Pöls-Lavanttal Fault System (Tollmann, 1986).
in scheme: Tectonic Boundary Objects in Europe
broader: Pöls-Lavanttal Fault System

Hirschegg Fault
references: https://data.geoscience.earth/ncl/geoera/ref/732
notation: AT-10111
type: Concept
created: 2020-04-30T14:27:00.934Z
definition: Is a NE-SW trending fault near Hirschegg belonging to the Pöls-Lavanttal Fault System (Tollmann, 1986).
definition: Ist eine NE-SW-streichende Störung bei Hirschegg und wird dem Pöls-Lavanttal Störungssystem zugeordnet (Tollmann, 1986). @de
preferred label: Hirschegg-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Pöls-Lavanttal Fault System

Obdach Fault
references: https://data.geoscience.earth/ncl/geoera/ref/732
notation: AT-10236
type: Concept
created: 2020-04-30T14:27:00.990Z
definition: Is a NNE-SSW trending fault in the area of the village Obdach as part of the Pöls-Lavanttal Fault System (Tollmann, 1986).
definition: Ist eine NNE-SSW-streichende Störung im Bereich von Obdach und Teil des Pöls-Lavanttal-STS (Tollmann, 1968). @de
preferred label: Obdach-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Pöls-Lavanttal Fault System

Lavanttal Fault
preferred label: Labotski prelom @sl
references: https://data.geoscience.earth/ncl/geoera/ref/823
references: https://data.geoscience.earth/ncl/geoera/ref/844
definition: This subvertical NNE-SSW trending dextral strike slip fault runs in Austria parallel to the Lavant valley (Kurz et al., 2011; Linzer et al., 2002; Reischenbacher & Sachsenhoffer, 2013) and continues in NW-SE direction along the Drava and Mislinja valleys W of the Pohorje Mountains and then between Mislinja and Slovenske Konjice to the W of the Boč Mountain (e.g. Fodor et al., 1998; Atanackov et al., 2019). GPS measurements suggest the fault is recently active with an estimated average slip-rate of 0.5-1 mm/yr (Pavlovčič Prešeren et al., 2005). In Austria, seismic activity along the fault has been observed (XX)
notation: SI-3.001
alternative label: Labot Fault
references: https://data.geoscience.earth/ncl/geoera/ref/1127
references: https://data.geoscience.earth/ncl/geoera/ref/831
references: https://data.geoscience.earth/ncl/geoera/ref/1158
notation: AT-10175
type: Concept
created: 2020-04-30T14:27:00.962Z
preferred label: Lavanttal-Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/1148
in scheme: Tectonic Boundary Objects in Europe
broader: Pöls-Lavanttal Fault System

Adriatic-Apulian Foreland Thrust System
preferred label: Jadransko-Apulijski predgorski narivni sistem @sl
type: Concept
created: 2020-08-19T13:00:02.917Z
definition: The Adriatic-Apulian Foreland Thrust System comprises NW-SE striking, SW-vergent low-angle thrusts and reverse faults, extending from the Friuli plain across the northern Adriatic into the Istria peninsula (Placer, 2008; Placer et al., 2010). Also referred to as Istria-Friuli underthrust system (Placer et al., 2010).
notation: SI-6
narrower: Črni Kal Thrust
narrower: Buzet Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/1160
references: https://data.geoscience.earth/ncl/geoera/ref/1164
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Slovenia

Črni Kal Thrust
preferred label: Črnokalski nariv @sl
references: https://data.geoscience.earth/ncl/geoera/ref/1136
references: https://data.geoscience.earth/ncl/geoera/ref/1137
type: Concept
created: 2020-08-19T13:00:02.946Z
definition: The Črni Kal Thrust is a 73 km long NW-SE striking, gently NE-dipping active thrust in extreme SW Slovenia, NW Croatia and the Gulf of Trieste (Atanackov et al., 2019). The surface trace runs from southern Friuli (NE Italy) in the NW to E Istria (NW Croatia). It is defined from geologic mapping and geophysical data (Pleničar et al., 1969; Celarc and Milanič, 2009; HGI, 2009; Placer et al., 2010; Busetti et al., 2010; Carulli, 2011). It is considered active, based on evidence from geophysical data (Romeo, 2009; Busetti et al., 2010).
notation: SI-6.001
alternative label: Palmanova Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/1127
references: https://data.geoscience.earth/ncl/geoera/ref/1165
references: https://data.geoscience.earth/ncl/geoera/ref/1164
references: https://data.geoscience.earth/ncl/geoera/ref/1140
references: https://data.geoscience.earth/ncl/geoera/ref/1143
notation: IT-0220
in scheme: Tectonic Boundary Objects in Europe
broader: Adriatic-Apulian Foreland Thrust System

Buzet Thrust
preferred label: Buzetski nariv @sl
references: https://data.geoscience.earth/ncl/geoera/ref/1171
type: Concept
created: 2020-08-19T13:00:02.973Z
definition: Is a gently NE-dipping, 62 km long NW-SE striking thrust running across the Gulf of Trieste and SW Slovenia into NW Croatia (Atanackov et al., 2019). It runs from the Grado lagoon in the NW, across SW Slovenia into central Istria in NW Croatia (HGI, 2009; Placer et al., 2010; Busetti et al., 2010; Carulli, 2011). It is considered potentially active, based on its geometry with respect to the stress field and limited geodetic data (Rižnar et al., 2007).
notation: SI-6.002
references: https://data.geoscience.earth/ncl/geoera/ref/1127
references: https://data.geoscience.earth/ncl/geoera/ref/1137
references: https://data.geoscience.earth/ncl/geoera/ref/1136
references: https://data.geoscience.earth/ncl/geoera/ref/1143
references: https://data.geoscience.earth/ncl/geoera/ref/1164
in scheme: Tectonic Boundary Objects in Europe
broader: Adriatic-Apulian Foreland Thrust System

Dinaric Fault System
preferred label: Dinarski prelomni sistem @sl
type: Concept
created: 2020-08-19T13:00:02.218Z
definition: This fault system is composed of subparallel NW-SE striking, subvertical strike-slip faults running in the Slovenian part of the Southern Alps and the Northern Dinarides (Poljak et al., 2000; Vrabec in Fodor, 2006; Moulin et al., 2016, and references therein). The faults of this system cut older External Dinaric Thrust Belt and South Alpine Thrust and Fold Belt and have been dextrally active since the beginning of Pliocene. Some of the longest faults from this system are seismically active, e.g. the Ravne, Idrija, Predjama-Avče and Raša faults (e.g. Poljak et al., 2000; Kastelic et al., 2008; Vičič et al., 2019).
notation: SI-4
alternative label: Idrija Fault System
narrower: Idrija-Ampezzo Subfault System
narrower: Ravne Fault
narrower: Čeplez Fault
narrower: Predjama-Avče Fault
narrower: Raša Fault
narrower: Divača Fault
narrower: Dražgoše Fault
narrower: Kranj Fault
narrower: Planina-Podpreska Fault
narrower: Rakitna Fault
narrower: Mišja dolina Fault
narrower: Želimlje-Ortnek Fault
narrower: Dobrepolje Fault
narrower: Žužemberk Fault
narrower: Stična Fault
narrower: Toplice Fault
narrower: Zagorje Fault
narrower: Hrastnik Fault
references: https://data.geoscience.earth/ncl/geoera/ref/1156
references: https://data.geoscience.earth/ncl/geoera/ref/1169
references: https://data.geoscience.earth/ncl/geoera/ref/1147
references: https://data.geoscience.earth/ncl/geoera/ref/1172
references: https://data.geoscience.earth/ncl/geoera/ref/1173
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Slovenia

Kranj Fault
preferred label: Kranjski prelom @sl
type: Concept
created: 2020-08-19T13:00:02.471Z
definition: The fault runs in NW-SE direction along the southern rim of the Ljubljana Basin from Bled to Kranj (Poljak, 2007; Jamšek Rupnik, 2013). This is steeply NE-dipping dextral strike slip fault, which is considered as potentially still active in Quaternary times (Atanackov et al., 2019).
notation: SI-4.008
references: https://data.geoscience.earth/ncl/geoera/ref/1127
references: https://data.geoscience.earth/ncl/geoera/ref/1144
references: https://data.geoscience.earth/ncl/geoera/ref/1168
in scheme: Tectonic Boundary Objects in Europe
broader: Dinaric Fault System

Planina-Podpreska Fault
preferred label: Planinsko-Podpreskin prelom @sl
type: Concept
created: 2020-08-19T13:00:02.499Z
definition: This is a NW-SE striking and steeply SW-dipping dextral transpressive fault running along the Loški potok and Travljanska gora in mountainous terrain between Lož and Kočevje poljes (Atanackov et al., 2019, and references therein).
notation: SI-4.009
references: https://data.geoscience.earth/ncl/geoera/ref/1127
in scheme: Tectonic Boundary Objects in Europe
broader: Dinaric Fault System

Rakitna Fault
preferred label: Rakitniški prelom @sl
type: Concept
created: 2020-08-19T13:00:02.526Z
definition: This is a NW-SE striking and steeply NE-dipping dextral transpressive fault running from Horjul in NW across the Ljubljana Moor and further through the mountainous terrain, through Rakitna and Sodražica to the Ribnica Polje in SE. The fault is considered as potentially still active in Quaternary times (Atanackov et al., 2019; and references therein).
notation: SI-4.010
references: https://data.geoscience.earth/ncl/geoera/ref/1127
in scheme: Tectonic Boundary Objects in Europe
broader: Dinaric Fault System

Idrija-Ampezzo Subfault System
preferred label: Idrija-Ampezzo prelomni podsistem @sl
type: Concept
created: 2020-08-19T13:00:02.245Z
definition: About 200 km long system composed of steeply NE-dipping and approximately NW-SE-striking dextral strike-slip faults running through Friuli region in Italy along the Resia and Tagliamento valleys (Poli and Zanferrari, 2018) and in Slovenia from the Julian Alps through the Northern Dinarides along the Soča valley through Idrija and along several karst poljes in the SE part; Planina, Cerknica and Lož poljes (e.g. Poljak et al., 2000; Moulin et al., 2016). The system has been active in Pliocene and Quaternary.
notation: SI-4.001
narrower: Idrija Fault
references: https://data.geoscience.earth/ncl/geoera/ref/1167
references: https://data.geoscience.earth/ncl/geoera/ref/1169
references: https://data.geoscience.earth/ncl/geoera/ref/1156
in scheme: Tectonic Boundary Objects in Europe
broader: Dinaric Fault System

Idrija Fault
preferred label: Idrijski prelom @sl
type: Concept
created: 2020-08-19T13:00:02.273Z
definition: About 120 km long, NW-SE striking and steeply NE-dipping fault runs along the Soča Valley between Žaga and Most na Soči, then along several smaller valleys towards Idrija, further towards Logatec and then along the Planina, Cerknica and Lož poljes (Poljak, 2007; Atanackov et al., 2019, and references therein). The fault has been active as dextral strike-slip fault in Pliocene and Quaternary and is recently seismically active (Moulin et al., 2016; Atanackov et al., 2019; Vičič et al., 2019).
notation: SI-4.001.01
references: https://data.geoscience.earth/ncl/geoera/ref/1127
references: https://data.geoscience.earth/ncl/geoera/ref/1168
references: https://data.geoscience.earth/ncl/geoera/ref/1156
references: https://data.geoscience.earth/ncl/geoera/ref/1172
notation: IT-0379
in scheme: Tectonic Boundary Objects in Europe
broader: Idrija-Ampezzo Subfault System

Mišja dolina Fault
preferred label: Mišjedolski prelom @sl
type: Concept
created: 2020-08-19T13:00:02.554Z
definition: This is a NNW-SSE striking and subvertical dextral strike-slip fault running along the Gradaščica Valley, through the Ljubljana Moor to the Iška Village and continues through the mountainous terrain along the Mokrec Mountain and Mišja Valley towards Sodražica (Poljak, 2007; Atanackov et al., 2019; and references therein). Quaternary displacements along the fault were documented (Atanackov, 2013).
notation: SI-4.011
references: https://data.geoscience.earth/ncl/geoera/ref/1127
references: https://data.geoscience.earth/ncl/geoera/ref/1129
references: https://data.geoscience.earth/ncl/geoera/ref/1168
in scheme: Tectonic Boundary Objects in Europe
broader: Dinaric Fault System

Raša Fault
preferred label: Raški prelom @sl
references: https://data.geoscience.earth/ncl/geoera/ref/1162
references: https://data.geoscience.earth/ncl/geoera/ref/1172
type: Concept
created: 2020-08-19T13:00:02.385Z
definition: This 87 km long, NW-SE striking subvertical dextral strike slip fault runs from Goriška Brda on NW, across Vipava Valley, along the NE edge of the Kras plateau and through the Raša Valley, through Vremščica and Ilirska Bistrica in SE (Buser, 1968; Janež et al., 1997; Moulin et al., 2016; Jurkovšek, 2013; Placer and Jamšek, 2011; Atanackov et al., 2019). The fault has been active in Pliocene and Quaternary and is recently seismically active (Moulin et al., 2016; Vičič et al., 2019).
notation: SI-4.005
references: https://data.geoscience.earth/ncl/geoera/ref/1127
references: https://data.geoscience.earth/ncl/geoera/ref/1133
references: https://data.geoscience.earth/ncl/geoera/ref/1145
references: https://data.geoscience.earth/ncl/geoera/ref/1146
references: https://data.geoscience.earth/ncl/geoera/ref/1156
notation: IT-0375
in scheme: Tectonic Boundary Objects in Europe
broader: Dinaric Fault System

Divača Fault
preferred label: Divaški prelom @sl
type: Concept
created: 2020-08-19T13:00:02.389Z
definition: The fault runs along the prominent scarp through the Kras plateau in Slovenia. This is NW-SE striking and steeply NE-dipping dextral strike slip fault, which is considered as probably still active in Quaternary times (Jurkovšek, 2013; Atanackov et al., 2019).
notation: SI-4.006
references: https://data.geoscience.earth/ncl/geoera/ref/1127
references: https://data.geoscience.earth/ncl/geoera/ref/1146
notation: IT-0286
in scheme: Tectonic Boundary Objects in Europe
broader: Dinaric Fault System

Dražgoše Fault
preferred label: Dražgoški prelom @sl
type: Concept
created: 2020-08-19T13:00:02.415Z
definition: This is NW-SE striking and steeply NE-dipping dextral strike slip fault running from Pokljuka plateau in Slovenian Julian Alps, along the Jelovica plateau through Dražgoše, further SE along the Selška Sora Valley to the Kranj-Sora Polje (Poljak, 2007; Jamšek Rupnik, 2013; Atanackov et al., 2019). The fault is considered as probably still active in Quaternary times (Atanackov et al., 2019).
notation: SI-4.007
references: https://data.geoscience.earth/ncl/geoera/ref/1127
references: https://data.geoscience.earth/ncl/geoera/ref/1144
references: https://data.geoscience.earth/ncl/geoera/ref/1168
in scheme: Tectonic Boundary Objects in Europe
broader: Dinaric Fault System

Toplice Fault
preferred label: Topliški prelom @sl
type: Concept
created: 2020-08-19T13:00:02.692Z
definition: The Toplice fault is a SE-NW striking vertical dextral strike slip fault. The surface trace is 36 km long, from Senožeti in the NW to Žužemberk in the SE. Its trace is defined based on geologic mapping data (Mlakar, 1987; Buser, 1969, Premru, 1983). It is considered active based on seismicity (Atanackov et al., 2019).
notation: SI-4.016
references: https://data.geoscience.earth/ncl/geoera/ref/1127
references: https://data.geoscience.earth/ncl/geoera/ref/1134
references: https://data.geoscience.earth/ncl/geoera/ref/1154
references: https://data.geoscience.earth/ncl/geoera/ref/1170
in scheme: Tectonic Boundary Objects in Europe
broader: Dinaric Fault System

Zagorje Fault
preferred label: Zagorski prelom @sl
type: Concept
created: 2020-08-19T13:00:02.720Z
definition: This is a SE-NW striking vertical dextral strike slip fault with a 26 km surface trace. It runs from Trojane in the NW to Brunk in the SE (Buser, 1997; Placer, in prep., Celarc et al., 2009). It is considered probably active (Atanackov et al., 2019).
notation: SI-4.017
references: https://data.geoscience.earth/ncl/geoera/ref/1127
references: https://data.geoscience.earth/ncl/geoera/ref/1135
references: https://data.geoscience.earth/ncl/geoera/ref/1161
references: https://data.geoscience.earth/ncl/geoera/ref/1139
in scheme: Tectonic Boundary Objects in Europe
broader: Dinaric Fault System

Hrastnik Fault
preferred label: Hrastniški prelom @sl
type: Concept
created: 2020-08-19T13:00:02.749Z
definition: The Hrastnik fault is a SE-NW striking vertical dextral strike slip fault with a 26 km surface trace. It runs from Vrhe in the NW, to Zabukovje in the SE (Pleničar et al., 1976; Buser, 1977; Celarc et al., 2009; Placer, in prep.). It is considered probably active (Atanackov et al., 2019).
notation: SI-4.018
references: https://data.geoscience.earth/ncl/geoera/ref/1127
references: https://data.geoscience.earth/ncl/geoera/ref/1135
references: https://data.geoscience.earth/ncl/geoera/ref/1139
references: https://data.geoscience.earth/ncl/geoera/ref/1161
references: https://data.geoscience.earth/ncl/geoera/ref/1166
in scheme: Tectonic Boundary Objects in Europe
broader: Dinaric Fault System

Želimlje-Ortnek Fault
preferred label: Želimeljsko-Ortneški prelom @sl
type: Concept
created: 2020-08-19T13:00:02.581Z
definition: The fault runs from Ljubljana in NW, along the eastern rim of the Ljubljana Moor and then along the Želimeljščica Valley, across Velike Lašče, Ortnek and continues along the Ribnica and Kočevje poljes in SE (Poljak, 2007; Atanackov et al., 2019, and references therein). This NNW-SSE striking and steeply ENE dipping dextral strike-slip fault is considered as probably still active in Quaternary times (Atanackov et al., 2019).
notation: SI-4.012
references: https://data.geoscience.earth/ncl/geoera/ref/1127
references: https://data.geoscience.earth/ncl/geoera/ref/1168
in scheme: Tectonic Boundary Objects in Europe
broader: Dinaric Fault System

Ravne Fault
preferred label: Ravenski prelom @sl
type: Concept
created: 2020-08-19T13:00:02.301Z
definition: The Ravne fault is NW-SE striking and steeply NE-dipping dextral strike slip fault running through the mountainous terrain in the Slovenian part of the Julian Alps between Bovec and Cerkno (Atanackov et al., 2019, and references therein). The fault was the source of damaging 1998 Mw 5.6 and 2004 Mw 5.2 earthquakes (Kastelic et al., 2008, and references therein).
notation: SI-4.002
references: https://data.geoscience.earth/ncl/geoera/ref/1127
references: https://data.geoscience.earth/ncl/geoera/ref/1147
notation: IT-0263
in scheme: Tectonic Boundary Objects in Europe
broader: Dinaric Fault System

Dobrepolje Fault
preferred label: Dobrepoljski prelom @sl
type: Concept
created: 2020-08-19T13:00:02.609Z
definition: NW-SE striking and steeply NE-dipping dextral strike slip fault running from the Ljubljana Moor to the SE along the Dobrepolje, Kočevska Mala gora in Poljanska Valley to the Stari trg ob Kolpi (Poljak, 2007; Atanackov et al., 2019, and references therein). The fault is considered as probably still active in Quaternary times (Atanackov et al., 2019).
notation: SI-4.013
references: https://data.geoscience.earth/ncl/geoera/ref/1127
references: https://data.geoscience.earth/ncl/geoera/ref/1168
in scheme: Tectonic Boundary Objects in Europe
broader: Dinaric Fault System

Čeplez Fault
preferred label: Čepleški prelom @sl
type: Concept
created: 2020-08-19T13:00:02.329Z
definition: This is a NW-SE striking, steeply NE-dipping dextral strike-slip fault running through the mountainous terrain between Cerkno and Smrečje near Rovte (Mlakar, 1982; Atanackov et al., 2019). The fault is considered as potentially still active in Quaternary times (Atanackov et al., 2019).
notation: SI-4.003
references: https://data.geoscience.earth/ncl/geoera/ref/1127
references: https://data.geoscience.earth/ncl/geoera/ref/1153
in scheme: Tectonic Boundary Objects in Europe
broader: Dinaric Fault System

Žužemberk Fault
preferred label: Žužemberški prelom @sl
type: Concept
created: 2020-08-19T13:00:02.637Z
definition: This is an active, 70 km long, NW-SE striking and steeply NE-dipping dextral strike-slip fault, running from Gameljne in the NW across the Ljubljana Polje, through Grosuplje and along the Krka Valley through Žužemberk and Dolenjske Toplice in SE (e.g. Poljak, 2007; Atanackov et al., 2019, and references therein).
notation: SI-4.014
references: https://data.geoscience.earth/ncl/geoera/ref/1127
references: https://data.geoscience.earth/ncl/geoera/ref/1168
in scheme: Tectonic Boundary Objects in Europe
broader: Dinaric Fault System

Predjama-Avče Fault
preferred label: Predjamski prelom @sl
type: Concept
created: 2020-08-19T13:00:02.357Z
definition: The fault runs in NW-SE direction from Kambreško, through Avče then across the Banjšice and Trnovski Gozd plateaus further SE through Col and then between Nanos and Hrušica plateaus to Postojna (Janež et al., 1997; Poljak, 2007). This is 75 km long, steeply NE-dipping dextral strike-slip fault, active in Pliocene and Quaternary (Moulin et al., 2016; Atanackov et al., 2019).
notation: SI-4.004
alternative label: Predjama Fault
references: https://data.geoscience.earth/ncl/geoera/ref/1127
references: https://data.geoscience.earth/ncl/geoera/ref/1145
references: https://data.geoscience.earth/ncl/geoera/ref/1168
references: https://data.geoscience.earth/ncl/geoera/ref/1156
notation: IT-0376
in scheme: Tectonic Boundary Objects in Europe
broader: Dinaric Fault System

Stična Fault
preferred label: Stiški prelom @sl
type: Concept
created: 2020-08-19T13:00:02.665Z
definition: The Stična fault is a SE-NW striking vertical dextral strike slip fault. It runs along a 26 km trace from Domžale in the NW to Dol pri Ljubljani in the SE. Its trace is defined based on geologic mapping data (Mlakar, 1987; Buser, 1969, Premru, 1983). It is considered probably active (Atanackov et al., 2019), however, no firm evidence of activity has been found.
notation: SI-4.015
references: https://data.geoscience.earth/ncl/geoera/ref/1127
references: https://data.geoscience.earth/ncl/geoera/ref/1134
references: https://data.geoscience.earth/ncl/geoera/ref/1154
references: https://data.geoscience.earth/ncl/geoera/ref/1170
in scheme: Tectonic Boundary Objects in Europe
broader: Dinaric Fault System

Raba Fault System
preferred label: Rabski prelomni sistem @sl
type: Concept
created: 2020-08-19T13:00:02.103Z
definition: The Raba Fault System is a set of Lower-Neogene WSW-ENE trending normal faults that separate the Burgenland swell in SE Austria from the Murska Sobota extensional block in NE Slovenia (Márton et al., 2002; Fodor et al., 2011). The Raba Fault System definition extends to neighbouring faults with related histories (e.g. formed in the same tectonic phase) and generally similar geometric and kinematic properties. The Raba Fault System is considered inactive.
notation: SI-2
narrower: Lovrenc Fault
references: https://data.geoscience.earth/ncl/geoera/ref/1142
references: https://data.geoscience.earth/ncl/geoera/ref/1150
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Slovenia

Lovrenc Fault
preferred label: Lovrenški prelom @sl
type: Concept
created: 2020-08-19T13:00:02.131Z
definition: The fault is based on geologic data (Mioč and Žnidarčič, 1978; Žnidarčič and Mioč, 1989; Maros et al., 2012) and geomorphic analysis. The 28 km long E-W trace runs from Ribnica na Pohorju in the W to Maribor in the E. The fault originated as a lower-Neogene normal fault, bounding the Ribnica half-graben and is inferred to be recently reactivated as a reverse fault. It is considered a potentially active fault, in favourable orientation with the current stress field and activity along the nearby Labot/Lavanttal fault (Atanackov et al., 2019), however, no evidence of activity has been found so far.
notation: SI-2.001
references: https://data.geoscience.earth/ncl/geoera/ref/1127
references: https://data.geoscience.earth/ncl/geoera/ref/1152
references: https://data.geoscience.earth/ncl/geoera/ref/1149
references: https://data.geoscience.earth/ncl/geoera/ref/1175
in scheme: Tectonic Boundary Objects in Europe
broader: Raba Fault System

South Alpine Thrust and Fold Belt
preferred label: Južnoalpski narivni pas @sl
type: Concept
created: 2020-08-19T13:00:03.001Z
definition: South Alpine Thrust and Fold Belt is part of the Eastern Southern Alps, located to the east of the N Giudicarie Line, originated by polyphase compressional evolution of Tertiary age (Castellarin & Cantelli, 2000). The Neogene shortening in the Adria-Eurasia collision zone produced top-to-the south thrusting of the Alps south of the Periadriatic Fault System. Thrusting began in the Middle Miocene and mostly ended by the Pliocene. W-E striking and south verging thrusts are positioned in the southern part of the Julian Alps (NW Slovenia), in the southern part of the Kamnik-Savinja Alps (central-N Slovenia) (Poljak, 2007; Placer, 2008).
notation: SI-7
narrower: Krn Thrust
narrower: Jelovica Thrust
narrower: Selca Thrust
narrower: Litija Thrust
narrower: Dole Thrust
narrower: Kum Thrust
narrower: Friuli Fault Domain
references: https://data.geoscience.earth/ncl/geoera/ref/1138
references: https://data.geoscience.earth/ncl/geoera/ref/1168
references: https://data.geoscience.earth/ncl/geoera/ref/1160
narrower: Tolmin Thrust
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Slovenia

Litija Thrust
preferred label: Litijski nariv @sl
type: Concept
created: 2020-08-19T13:00:03.114Z
definition: This is a Dinaric thrust, folded in the Alpine direction (Placer, 2008). It is running from Medvode in the west to the Litija in the E (Poljak, 2007).
notation: SI-7.005
alternative label: Litija Overthrust
references: https://data.geoscience.earth/ncl/geoera/ref/1168
references: https://data.geoscience.earth/ncl/geoera/ref/1160
references: https://data.geoscience.earth/ncl/geoera/ref/1132
in scheme: Tectonic Boundary Objects in Europe
broader: South Alpine Thrust and Fold Belt

Dole Thrust
preferred label: Dolski nariv @sl
type: Concept
created: 2020-08-19T13:00:03.142Z
definition: Dole Thrust is positioned below the Litija Thrust and has according to the Placer (2008), the same genesis; it is a Dinaric thrust, folded in the Alpine direction. It is running in the E-W direction in the vicinity of Dolsko (Poljak, 2007).
notation: SI-7.006
alternative label: Dole Nappe
references: https://data.geoscience.earth/ncl/geoera/ref/1168
references: https://data.geoscience.earth/ncl/geoera/ref/1160
references: https://data.geoscience.earth/ncl/geoera/ref/1132
in scheme: Tectonic Boundary Objects in Europe
broader: South Alpine Thrust and Fold Belt

Kum Thrust
preferred label: Kumski nariv @sl
type: Concept
created: 2020-08-19T13:00:03.170Z
definition: Kum Thrust represents eastern continuation of the Dole Thrust (Placer, 2008) and has the same genesis. It is running in the E-W direction east from Kum, north from Sevnica and near Kozje (Poljak, 2007).
notation: SI-7.007
alternative label: Kum Nappe
references: https://data.geoscience.earth/ncl/geoera/ref/1168
references: https://data.geoscience.earth/ncl/geoera/ref/1160
references: https://data.geoscience.earth/ncl/geoera/ref/1132
in scheme: Tectonic Boundary Objects in Europe
broader: South Alpine Thrust and Fold Belt

Friuli Fault Domain
preferred label: Furlanska prelomna domena @sl
type: Concept
created: 2020-08-19T13:00:03.199Z
definition: This is a thrust and fold belt in the Southern Alps, composed of south-verging reverse faults. Seismically active reverse faults have a roughly E-W trend and turn southwest in the western part (e.g. Poli and Zanferrari, 2018).
notation: SI-7.008
narrower: Kobarid Fault
references: https://data.geoscience.earth/ncl/geoera/ref/1167
in scheme: Tectonic Boundary Objects in Europe
broader: South Alpine Thrust and Fold Belt

Kobarid Fault
preferred label: Kobariški prelom @sl
type: Concept
created: 2020-08-19T13:00:03.226Z
definition: Slovenian part of Kobarid Fault runs in approximately W-E direction between Breginj and Kobarid in the Julian Alps (Atanackov et al., 2019, and references therein). This is a N-dipping thrust, related to the Gemona Fault in Italy (Bressan et al., 2016). The fault is considered as potentially active through the Quaternary (Atanackov et al., 2019).
notation: SI-8.001
alternative label: Gemona Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/1127
references: https://data.geoscience.earth/ncl/geoera/ref/1130
in scheme: Tectonic Boundary Objects in Europe
broader: Friuli Fault Domain

Tolmin Thrust
preferred label: Tolminski nariv @sl
type: Concept
created: 2020-10-28T13:09:11.975Z
notation: SI-7.003
notation: IT-0265
alternative label: Podmelec Overthrust
definition: E-W striking and gently N dipping thrust, part of the South Alpine Thrust and Fold Belt (Poljak, 2007; Placer, 2008), running from Breginj in the west under southern foothills of the Julian Alps to the Selce on east, where it continues as Selce Thrust.
references: https://data.geoscience.earth/ncl/geoera/ref/1168
references: https://data.geoscience.earth/ncl/geoera/ref/1160
references: https://data.geoscience.earth/ncl/geoera/ref/1132
in scheme: Tectonic Boundary Objects in Europe
broader: South Alpine Thrust and Fold Belt

Krn Thrust
preferred label: Krnski nariv @sl
type: Concept
created: 2020-08-19T13:00:03.029Z
definition: E-W striking and gently N dipping thrust, part of the South Alpine Thrust and Fold Belt (Poljak, 2007; Placer, 2008), running from Bovec in the west under southern foothills of the Julian Alps.
notation: SI-7.001
alternative label: Krn Overthrust
references: https://data.geoscience.earth/ncl/geoera/ref/1168
references: https://data.geoscience.earth/ncl/geoera/ref/1160
references: https://data.geoscience.earth/ncl/geoera/ref/1132
in scheme: Tectonic Boundary Objects in Europe
broader: South Alpine Thrust and Fold Belt

Jelovica Thrust
preferred label: Jeloviški nariv @sl
type: Concept
created: 2020-08-19T13:00:03.057Z
definition: E-W striking and gently N dipping thrust, part of the South Alpine Thrust and Fold Belt (Poljak, 2007; Placer, 2008). This is probably eastern extension of the Krn Thrust. It is positioned along eastern foothills of the Jelovica Plateu near Kropa.
notation: SI-7.002
alternative label: Jelovica Overthrust
references: https://data.geoscience.earth/ncl/geoera/ref/1168
references: https://data.geoscience.earth/ncl/geoera/ref/1160
references: https://data.geoscience.earth/ncl/geoera/ref/1132
in scheme: Tectonic Boundary Objects in Europe
broader: South Alpine Thrust and Fold Belt

Selca Thrust
preferred label: Selški nariv @sl
type: Concept
created: 2020-08-19T13:00:03.086Z
definition: Part of the South Alpine Thrust and Fold Belt, originally E-W striking and gently N dipping, now it is partially overprinted with younger tectonic phases (Poljak, 2007; Placer, 2008). It is positioned in the vicinity of Škofja Loka.
notation: SI-7.004
alternative label: Selca Overthrust
references: https://data.geoscience.earth/ncl/geoera/ref/1168
references: https://data.geoscience.earth/ncl/geoera/ref/1160
references: https://data.geoscience.earth/ncl/geoera/ref/1132
in scheme: Tectonic Boundary Objects in Europe
broader: South Alpine Thrust and Fold Belt

External Dinaric Thrust and Fold Belt
preferred label: Zunanjedinarski narivni pas @sl
type: Concept
created: 2020-08-19T13:00:02.778Z
definition: The External Dinarides are built of thrust units, striking in the NW-SE direction with southwest vergence (Poljak, 2007; Placer, 2008; Placer et al., 2010). They were formed in the time from Upper Jurassic to Upper Eocene, and even to Lower Oligocene.
notation: SI-5
narrower: Snežnik Thrust
narrower: Hrušica Thrust
narrower: Trnovo Thrust
narrower: Bela Krajina W Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/1168
references: https://data.geoscience.earth/ncl/geoera/ref/1160
references: https://data.geoscience.earth/ncl/geoera/ref/1164
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Slovenia

Snežnik Thrust
preferred label: Snežniški nariv @sl
type: Concept
created: 2020-08-19T13:00:02.806Z
definition: The lowermost thrust of the External Dinaric Thrust Belt (Poljak, 2007; Placer, 2008; Placer et al., 2010) of the Eocene age. NW – SE striking and gently NE dipping, running from Razdrto in the NW, near Ilirska Bistrica and toward Rijeka (Croatia).
notation: SI-5.001
alternative label: Snežnik Overthrust
references: https://data.geoscience.earth/ncl/geoera/ref/1168
references: https://data.geoscience.earth/ncl/geoera/ref/1160
references: https://data.geoscience.earth/ncl/geoera/ref/1164
references: https://data.geoscience.earth/ncl/geoera/ref/1132
in scheme: Tectonic Boundary Objects in Europe
broader: External Dinaric Thrust and Fold Belt

Hrušica Thrust
preferred label: Hrušiški nariv @sl
type: Concept
created: 2020-08-19T13:00:02.834Z
definition: The intermediate thrust of the External Dinaric Thrust Belt (Poljak, 2007; Placer, 2008; Placer et al., 2010) of the Eocene age. NW – SE striking and gently NE dipping, running from vicinity of Ajdovščina in the NW, Vipava, around foothills of the Nanos mountain and toward Postojna.
notation: SI-5.002
alternative label: Hrušica
references: https://data.geoscience.earth/ncl/geoera/ref/1168
references: https://data.geoscience.earth/ncl/geoera/ref/1160
references: https://data.geoscience.earth/ncl/geoera/ref/1164
references: https://data.geoscience.earth/ncl/geoera/ref/1132
in scheme: Tectonic Boundary Objects in Europe
broader: External Dinaric Thrust and Fold Belt

Trnovo Thrust
preferred label: Trnovski nariv @sl
type: Concept
created: 2020-08-19T13:00:02.861Z
definition: The uppermost thrust of the External Dinaric Thrust Belt (Poljak, 2007; Placer, 2008; Placer et al., 2010) of the Eocene age. NW – SE striking and gently NE dipping, running from Nova Gorica, along the SW, S and E slopes of the Trnovo Plateau toward Idrija. It is dextrally displaced by strike-slip Predjama-Avče Fault.
notation: SI-5.003
alternative label: Trnovo Overthrust
references: https://data.geoscience.earth/ncl/geoera/ref/1168
references: https://data.geoscience.earth/ncl/geoera/ref/1160
references: https://data.geoscience.earth/ncl/geoera/ref/1164
references: https://data.geoscience.earth/ncl/geoera/ref/1132
in scheme: Tectonic Boundary Objects in Europe
broader: External Dinaric Thrust and Fold Belt

Bela Krajina W Thrust
preferred label: Zahodni Belokranjski nariv @sl
type: Concept
created: 2020-08-19T13:00:02.889Z
definition: This is thrust of the External Dinaric Thrust Belt (Poljak, 2007; Placer, 2008; Placer et al., 2010) of the Eocene age. It is NW-SE striking and gently NE dipping thrust, running through Bela Krajina from Dobliče near Črnomelj on NW to Vinica on SE.
notation: SI-5.004
references: https://data.geoscience.earth/ncl/geoera/ref/1168
references: https://data.geoscience.earth/ncl/geoera/ref/1160
references: https://data.geoscience.earth/ncl/geoera/ref/1164
in scheme: Tectonic Boundary Objects in Europe
broader: External Dinaric Thrust and Fold Belt

Periadriatic-Mid-Hungarian Large-scale Fault System
preferred label: Periadriatisch-Mittelungarisches-Großstörungssystem @de
preferred label: Periadriatsko-Srednjemadžarski veliki prelomni sistem @sl
alternative label: Insubric-Mid-Hungarian Large-scale Fault System
definition: This ca. 1000 km long, approximately E-W and locally NE-SW trending Large-scale Fault System extends from Ivrea (IT) via the Veltlin Valley (Tonale Fault System) and the Sulztal until Cles. Here, it is displaced left-laterally by the Giudicarie Fault System. The eastern part starts in Sterzing (IT) and extends via the Eisack Valley, Pustertal (Pusteria), Gailtal and the Karawanks mountain range. There it splits into a northern and southern branch until the Lavant(Labot)-Mislinja Valley, where it splits again into several branches. The Lavanttal (Labot) Fault System displaces this Large-scale Fault System right-laterally. Finally, it continues eastward as the Middle Hungarian-Balaton Fault System (Fodor et al., 1998 and references therein). Deformation along this Large-scale Fault System can be subdivided into several phases: The potentially oldest deformation as NE-SW trending horst-and-graben structure from Permian to Lower Jurassic times is still under discussion (Pomella et al., 2012 and references therein). The first observed deformation is represented by Upper Cretaceous transpressive left-lateral shear zones (Müller et al., 2001). The main deformation phase with accompanying plutonic intrusions (Adamello, Bergell) is characterized by both, brittle and ductile, late Eocene-Miocene deformation with right-lateral movement. Recent deformation is reported from the eastern part (Handy et al., 2005 and references therein). Displacement rates are discussed controversially, reaching from at least 100 km of extension parallel to the orogen (Handy et al., 2005 and references therein) up to 500 km (Tari & Pamic, 1998 and discussion therein).
definition: Dieses in etwa E-W (teilweise NE-SW)-streichende ca. 1000 km lange Großstörungssystem zieht sich von Ivrea (nördlich Turin) über das Veltlintal (Tonale-Linie) und das Sulztal bis nach Cles, wo es durch das Judikarien-Störungssystem sinistral versetzt wird. Bei Sterzing wiederbeginnend verläuft es über das Eisacktal, Pustertal, Gailtal und die Karawanken in einen Nord- und Südteil trennend bis zum Lavant-Mislinja-Tal, wo es sich in mehrere Arme auffächert und durch das Lavanttal-Störungssystem dextral versetzt wird. Anschließend setzt es sich nach Osten ins Mittelungarisch-Balaton-Störungssystem (Fodor et al., 1998 und die darin aufgeführten Referenzen) fort. Die Bewegungsphasen entlang dieses Großstörungssystems lassen sich in mehrere Zeitabschnitte untergliedern. Die Anlage als NE-SW-streichende vom Perm bis Lias aktive Horst und Grabenstruktur ist in Diskussion (Pomella et al., 2012 und die darin aufgeführten Referenzen). Die ersten nachgewiesenen Bewegungen werden durch oberkretazische Scherzonen mit sinistral transpressiver Kinematik repräsentiert (Müller et al., 2001). Die Hauptphase mit begleitenden plutonischen Intrusionen (Adamello, Bergell) zeigen duktile und spröde Deformation mit dextraler Kinematik vom späten Eozän bis Miozän. Rezente Bewegungen sind besonders aus den östlichen Anteilen beschrieben (Handy et al. 2005 und die darin aufgeführten Referenzen). Kontrovers sind die ermittelten Versatzweiten von mindestens 100 km orogen paralleler Extension (Handy et al. 2005 und die darin aufgeführten Referenzen) bis 500 km Versatz (Tari & Pamic 1998 und die darin aufgeführten Referenzen). @de
references: https://data.geoscience.earth/ncl/geoera/ref/752
references: https://data.geoscience.earth/ncl/geoera/ref/825
references: https://data.geoscience.earth/ncl/geoera/ref/831
references: https://data.geoscience.earth/ncl/geoera/ref/843
references: https://data.geoscience.earth/ncl/geoera/ref/846
notation: SI-1
type: Concept
created: 2020-04-30T14:26:59.324Z
narrower: Periadriatic Fault System
narrower: Mid-Hungarian-Balaton Fault System
notation: AT-7
narrower: Insubric Fault System
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria
broader: Tectonic Boundary in Slovenia

Mid-Hungarian-Balaton Fault System
preferred label: Srednjemadžarsko-Balatonski prelomni sistem @sl
narrower: Ljutomer Fault
narrower: Donat Fault
notation: SI-1.002
narrower: Orehovec Fault
narrower: Haloze Fault
type: Concept
created: 2020-04-30T14:26:59.550Z
preferred label: Mittelungarisches-Balaton-Störungsystem @de
notation: AT-128
in scheme: Tectonic Boundary Objects in Europe
broader: Periadriatic-Mid-Hungarian Large-scale Fault System

Orehovec Fault
preferred label: Orehovški prelom @sl
type: Concept
created: 2020-08-19T13:00:02.075Z
definition: The Orehovec fault is a sinistral strike-slip fault in the NW part of the Gorjanci Mountains in SE Slovenia. The SW-NE running 28 km long fault trace runs from Semič in the SW to Orehovec in the NE (Bukovac et al., 1984). The fault dips vertically. It is considered probably active, based on geomorphic evidence and geologic mapping (Atanackov et al., 2019).
notation: SI-1.002.04
references: https://data.geoscience.earth/ncl/geoera/ref/1127
references: https://data.geoscience.earth/ncl/geoera/ref/1131
in scheme: Tectonic Boundary Objects in Europe
broader: Mid-Hungarian-Balaton Fault System

Donat Fault
preferred label: Donački prelom @sl
type: Concept
created: 2020-08-19T13:00:01.988Z
definition: This dextral strike-slip fault runs along a 53 km long ENE-WSW trace from south of the Boč Mountain to Miklavž pri Ormožu (Aničić and Juriša, 1985; Maros et al., 2012). It is considered potentially active, being in a favourable geometric relationship with the current stress field and being part of the active Mid-Hungarian zone (Atanackov et al., 2019), however, no firm evidence of activity has been observed.
notation: SI-1.002.01
references: https://data.geoscience.earth/ncl/geoera/ref/1127
references: https://data.geoscience.earth/ncl/geoera/ref/1126
references: https://data.geoscience.earth/ncl/geoera/ref/1149
in scheme: Tectonic Boundary Objects in Europe
broader: Mid-Hungarian-Balaton Fault System

Haloze Fault
preferred label: Haloški prelom @sl
type: Concept
created: 2020-08-19T13:00:02.018Z
definition: The Haloze fault is a 45 km long, steeply dipping N-vergent and E-W striking reverse fault, part of the Mid-Hungarian zone. The surface trace / projection of the fault runs from north of Boč Mountain to Ormož (Aničić and Juriša, 1985; Žnidarčič and Mioč, 1989; Mioč and Marković, 1998; Maros et al., 2012). It is considered potentially active, being in a favourable geometric relationship with the current stress field and being part of the active Mid-Hungarian zone (Atanackov et al., 2019), however, no firm evidence of activity has been observed.
notation: SI-1.002.02
references: https://data.geoscience.earth/ncl/geoera/ref/1127
references: https://data.geoscience.earth/ncl/geoera/ref/1126
references: https://data.geoscience.earth/ncl/geoera/ref/1151
references: https://data.geoscience.earth/ncl/geoera/ref/1175
references: https://data.geoscience.earth/ncl/geoera/ref/1149
in scheme: Tectonic Boundary Objects in Europe
broader: Mid-Hungarian-Balaton Fault System

Ljutomer Fault
preferred label: Ljutomerski prelom @sl
type: Concept
created: 2020-08-19T13:00:02.047Z
definition: This blind reverse fault runs along a 28 km long E-W oriented surface trace projection from Savci in the west to the extreme E tip of Slovenia in the east (Mioč and Marković, 1998; Maros et al., 2012). It is a steeply dipping N-vergent blind fault, defined based on deep seismic reflection data (Atanackov, 2007). It is considered probably active, being in a favourable geometric relationship with the current stress field and being part of the active Mid-Hungarian zone (Atanackov et al., 2019). No conclusive evidence of activity has been found, however, geomorphic evidence in the associated Ormož-Selnica anticline suggests recent activity.
notation: SI-1.002.03
references: https://data.geoscience.earth/ncl/geoera/ref/1127
references: https://data.geoscience.earth/ncl/geoera/ref/1128
references: https://data.geoscience.earth/ncl/geoera/ref/1149
references: https://data.geoscience.earth/ncl/geoera/ref/1151
in scheme: Tectonic Boundary Objects in Europe
broader: Mid-Hungarian-Balaton Fault System

Periadriatic Fault System
preferred label: Periadriatski prelom @sl
references: https://data.geoscience.earth/ncl/geoera/ref/752
references: https://data.geoscience.earth/ncl/geoera/ref/778
references: https://data.geoscience.earth/ncl/geoera/ref/759
references: https://data.geoscience.earth/ncl/geoera/ref/823
references: https://data.geoscience.earth/ncl/geoera/ref/831
narrower: Fella-Sava-Celje Subfault System
notation: SI-1.001
narrower: Periadriatic Fault
narrower: Šoštanj Fault
type: Concept
created: 2020-04-30T14:26:59.352Z
preferred label: Periadriatisches Störungssystem @de
narrower: Pustertal-Gailtal Subfault System
narrower: Karawanks Subfault System
notation: AT-135
narrower: Menina-Vransko Fault
definition: This approximately 700 km long, E-W trending Fault System extends from Ivrea (IT) at its western margin via the Veltlin Valley (Tonale Fault System) and the Sulztal until Cles. Here, it is displaced left-laterally by the Giudicarie Fault System. The eastern part starts in Sterzing (IT) and runs via the Eisack Valley, Pustertal (Pusteria), Gailtal and the Karawanks Mountains towards the E. There it splits into a northern and southern branch until the Lavant (Labot)-Mislinja Valley, where it splits again into several branches. It is cut off by right-lateral movement along the Lavanttal (Labot) Fault System and continues to the East into the Middle-Hungarian-Balaton Fault System (Fodor et al., 1998 and references therein). It shows a long-lasting history with a main activity, accompanied by plutonic Intrusions (e.g. Pohorje), with right-lateral ductile and brittle movement during late Eocene to Miocene times. Recent activity along the fault is observed. Displacement rates of at least 100 km orogeny parallel extension is described (Handy et al. 2005 and references therein; Linzer et al. 2002 and references therein).
definition: Dieses in etwa E-W - streichende ca. 700 km lange Störungssystem verläuft von Ivrea (nördlich Turin) über das Veltlintal (Tonale-Linie) und das Sulztal bis nach Cles, wo es durch das Judikarien-Störungssystem sinistral versetzt wird. Bei Sterzing wiederbeginnend verläuft es über das Eisacktal, Pustertal, Gailtal und die Karawanken in einen Nord- und Südteil trennend bis zum Lavant-Mislinja-Tal, wo sie sich in mehrere Arme auffächert und durch das Lavanttal- Störungssystem dextral versetzt wird. Anschließend setzt es sich nach Osten ins Mittelungarisch-Balaton- Störungssystem (Fodor et al., 1998 und die darin aufgeführten Referenzen) fort. Die Bewegungsphasen entlang dieses Störungssystem lassen sich in mehrere Zeitabschnitte untergliedern. Die Hauptphase mit begleitenden plutonischen Intrusionen (Pohorje) zeigt duktile und spröde Deformation mit dextraler Kinematik vom späten Eozän bis Miozän bis zu rezenten Bewegungen (Sprenger, 1996). Ermittelte Versatzweiten orogen paralleler Extension liegen bei mindestens 100 km (Handy et al. 2005 und die darin aufgeführten Referenzen; Linzer et al. 2002 und die darin aufgeführten Referenzen). @de
narrower: Canavese Fault
narrower: Tonale Fault
narrower: Giudicarie North Line
in scheme: Tectonic Boundary Objects in Europe
broader: Periadriatic-Mid-Hungarian Large-scale Fault System

Periadriatic Fault
type: Concept
created: 2020-08-19T13:00:01.845Z
definition: The Slovenian part of the Periadriatic Fault runs approximately in E-W direction through the northeastern part of the Kamnik-Savinja Alps and is cut by the Šoštanj Fault in the E. This is subvertical dextral transpressive fault, that was probably active also through the Quaternary (Fodor et al., 1998; Atanackov et al., 2019).
notation: SI-1.001.02
alternative label: Periadriatic Line
references: https://data.geoscience.earth/ncl/geoera/ref/1127
references: https://data.geoscience.earth/ncl/geoera/ref/831
in scheme: Tectonic Boundary Objects in Europe
broader: Periadriatic Fault System
broader: Insubric Fault System

Šoštanj Fault
preferred label: Šoštanjski prelom @sl
type: Concept
created: 2020-08-19T13:00:01.877Z
definition: Approximately 90 km long, WNW-ESE striking subvertical dextral strike slip fault that runs through Šoštanj and along the southern rim of the Velenje Basin, through Dobrna towards Rogaška Slatina and further towards the E, where it enters Croatia (e.g. Poljak, 2007; Atanackov et al., 2019). The fault has been active also through Quaternary with an estimated slip-rate of 0.1-0.9 mm/yr (Atanackov et al., 2019, and references therein).
notation: SI-1.001.03
references: https://data.geoscience.earth/ncl/geoera/ref/1168
references: https://data.geoscience.earth/ncl/geoera/ref/1127
in scheme: Tectonic Boundary Objects in Europe
broader: Periadriatic Fault System

Menina-Vransko Fault
preferred label: Meninsko-Vranski prelom @sl
type: Concept
created: 2020-08-19T13:00:01.931Z
definition: The ENE-WSW-striking an N-dipping reverse Menina-Vransko Fault runs along the southern edge of the Menina Mountain and the western rim of the Celje Basin (Fodor et al., 1998; Atanackov et al., 2019). The fault is considered as potentially active through the Quaternary (Atanackov et al., 2019).
notation: SI-1.001.05
references: https://data.geoscience.earth/ncl/geoera/ref/1127
references: https://data.geoscience.earth/ncl/geoera/ref/831
in scheme: Tectonic Boundary Objects in Europe
broader: Periadriatic Fault System

Karawanks Subfault System
preferred label: Karavanški prelomni podsistem @sl
definition: The E-W trending fault is part of the Periadriatic Fault System with dextral-lateral kinematics in the Karavanks Mountains.
definition: Die E-W-streichende Störung ist Teil des Periadriatischen Störungssystem mit dextral-seitenverscheibender Kinematik im Bereich der Karawanken (Polinski & Eisbacher, 1992). @de
alternative label: Karavanke Subfault System
narrower: Northern Karawanks Fault
alternative label: Karawanken Subfault System @de
type: Concept
created: 2020-04-30T14:26:59.466Z
preferred label: Karawanken-Teilstörungssystem @de
narrower: Feistritz Fault
narrower: Karavanks Fault
notation: AT-509
notation: SI-1.001.04
references: https://data.geoscience.earth/ncl/geoera/ref/850
in scheme: Tectonic Boundary Objects in Europe
broader: Periadriatic Fault System

Northern Karawanks Fault
preferred label: Severnokaravanški prelom @sl
definition: Diese hauptsächlich überschiebende Störung im Bereich der Karawanken ist Teil des Karawanken-Substörungssystems, das wiederum zum Periadriatischen Störungssystem gehört (Polinski & Eisbacher, 1992). In Österreich verläuft die E-W streichende, nach S einfallende Störung südlich der Drau vom Rabenberg via Unterloibl bis Zauchen/Suha. Der slovenische Teil der Störung verläuft zwischen Mežica und dem Slovenj-Gradec-Becken. Diese SSE-NNW-streichende, nach SSW einfallende Überschiebung wird als potentiell im Quartär aktiv angesehen (Nemes et al., 1997; Fodor et al., 1998; Atanackov et al., 2019). @de
type: Concept
created: 2020-08-19T13:00:01.904Z
definition: This fault with mainly thrusting character within the Karawanks Mountains is part of the Karawanks Subfault System, which in turn is part of the Periadriatic Fault System (Polinski & Eisbacher, 1992). In Austria, the E-W trending and S-dipping fault runs south of and parallel to the Drau River, from the Rabenberg Mt. via the village of Unterloibl towards Zauchen/Suha. The Slovenian part of the Northern Karawanks Fault runs between Mežica and the Slovenj Gradec Basin. This SSE-NNW-striking and SSW-dipping thrust is considered as potentially active through the Quaternary (Nemes et al., 1997; Fodor et al., 1998; Atanackov et al., 2019).
notation: SI-1.001.04.01
preferred label: Nördliche Karawanken-Störung @de
notation: AT-10139
references: https://data.geoscience.earth/ncl/geoera/ref/1127
references: https://data.geoscience.earth/ncl/geoera/ref/831
references: https://data.geoscience.earth/ncl/geoera/ref/1157
references: https://data.geoscience.earth/ncl/geoera/ref/850
in scheme: Tectonic Boundary Objects in Europe
broader: Karawanks Subfault System

Feistritz Fault
preferred label: Feistritz-Störung @de
type: Concept
created: 2020-04-30T14:26:59.494Z
notation: AT-10465
definition: The ENE-WSW trending fault in the Southern Alps runs from close to the Austrian-Slovenian border 5 km south of Bad Eisenkappel (AT) to Podljubelj (SLO), where it terminates at the Hochstuhl Fault.
definition: Die ENE-WSW-streichende Störung der Südalpen verläuft nahe der österreichisch-slowenischen Grenze von 5 km südlich von Bad Eisenkappel (AT) bis nach Podljubelj (SLO), wo sie von der Hochstuhl-Störung abgeschnitten wird. @de
in scheme: Tectonic Boundary Objects in Europe
broader: Karawanks Subfault System

Karavanks Fault
alternative label: Karavanke Fault
references: https://data.geoscience.earth/ncl/geoera/ref/850
type: Concept
created: 2020-04-30T14:26:59.522Z
definition: This E-W trending fault with right-lateral movement in the area of the Karawanken Mountains is part of the Periadriatic Fault System (Polinski & Eisbacher, 1992).
definition: Diese E-W-streichende Störung mit dextral-seitenverscheibender Kinematik im Bereich der Karawanken ist Teil des Periadriatischen Störungssystem mit (Polinski & Eisbacher, 1992). @de
preferred label: Karawanken-Störung @de
notation: AT-10139
alternative label: Karawanken Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Karawanks Subfault System

Fella-Sava-Celje Subfault System
preferred label: Belsko-Savsko-Celjski prelomni podsistem @sl
type: Concept
created: 2020-08-19T13:00:01.761Z
definition: This is an approximately W-E striking, 250 km long system consisting of the reverse Fella Fault and the dextral transpressive Sava and Celje faults (Placer, 1996; Fodor et al., 1998; Vrabec and Fodor, 2006; Jamšek Rupnik, 2013; Poli and Zanferrari, 2018). It runs from the Carnic Alps in Italy (Fella Fault), through the Upper Sava Valley in Julian Alps in Slovenia and along the northern rim of the Ljubljana Basin (Sava fault) and continues eastwards between the Kamnik-Savinja Alps and Sava Hills and along the southern rim of the Celje Basin (Celje Fault). The system has been active in Quaternary.
notation: SI-1.001.01
narrower: Sava W Fault
narrower: Sava E - Celje Fault
references: https://data.geoscience.earth/ncl/geoera/ref/831
references: https://data.geoscience.earth/ncl/geoera/ref/1159
references: https://data.geoscience.earth/ncl/geoera/ref/1173
references: https://data.geoscience.earth/ncl/geoera/ref/1144
references: https://data.geoscience.earth/ncl/geoera/ref/1167
in scheme: Tectonic Boundary Objects in Europe
broader: Periadriatic Fault System

Sava E - Celje Fault
preferred label: Savsko-Celjski prelom @sl
type: Concept
created: 2020-08-19T13:00:01.817Z
definition: The fault runs between the Kamnik-Savinja Alps and the Sava Hills in Slovenia and along the southern rim of the Celje Basin. This E-W striking steeply N-dipping dextral transpressive fault is considered active also through the Quaternary (Vrabec in Fodor, 2006; Atanackov et al., 2019).
notation: SI-1.001.01.02
references: https://data.geoscience.earth/ncl/geoera/ref/1127
references: https://data.geoscience.earth/ncl/geoera/ref/1173
in scheme: Tectonic Boundary Objects in Europe
broader: Fella-Sava-Celje Subfault System

Sava W Fault
preferred label: Savski prelom @sl
type: Concept
created: 2020-08-19T13:00:01.789Z
definition: The fault runs through the Upper Sava Valley in the Julian Alps in Slovenia and along the northern rim of the Ljubljana Basin, where it separates the Kamnik-Savinja Alps from the Ljubljana Basin (Jamšek Rupnik, 2013; Atanackov et al., 2019). This is a WNW-ESE striking steeply NNE-dipping dextral transpressive fault, with documented Quaternary displacements (Jamšek Rupnik, 2013).
notation: SI-1.001.01.01
alternative label: Sava Fault
references: https://data.geoscience.earth/ncl/geoera/ref/1127
references: https://data.geoscience.earth/ncl/geoera/ref/1144
in scheme: Tectonic Boundary Objects in Europe
broader: Fella-Sava-Celje Subfault System

Pustertal-Gailtal Subfault System
references: https://data.geoscience.earth/ncl/geoera/ref/752
references: https://data.geoscience.earth/ncl/geoera/ref/778
references: https://data.geoscience.earth/ncl/geoera/ref/838
type: Concept
created: 2020-04-30T14:26:59.381Z
definition: This approximately E-W trending Subfault System extends along the Puster and Gail Valleys (Pustertal and Gailtal, respectively) and are part of the Periadriatic Fault System. It shows a long-lasting history with right-lateral ductile and brittle movement during late Eocene to Miocene times. Recent activity along the fault is observed. (Handy et al, 2005; Mancktelow et al, 2001; Sprenger, 1996)
preferred label: Pustertal-Gailtal-Teilstörungssystem @de
narrower: Pustertal Fault
narrower: Gailtal Fault
notation: AT-512
definition: Dieses ca. E-W-streichende Teilstörungssystem verläuft entlang des Pustertals und Gailtals und ist Teil des Periadriatischen Störungssystem. Es zeigt eine duktile und spröde Deformation mit dextral-seitenverschiebender Kinematik vom Eozän bis ins Miozän. Rezente seismische Aktivität ist beschrieben. (Handy et al, 2005; Mancktelow et al, 2001; Sprenger, 1996) @de
in scheme: Tectonic Boundary Objects in Europe
broader: Insubric Fault System
broader: Tectonic Boundary in Italy
broader: Periadriatic Fault System

Gailtal Fault
type: Concept
created: 2020-04-30T14:26:59.437Z
preferred label: Gailtal-Stoerung @de
notation: AT-10072
definition: This approximately E-W trending fault along the valleys of the River Gail is part of the Pustertal-Gailtal Subfault System of the large-scale Periadriatic Fault System. It shows a long-lasting history with right-lateral ductile and brittle movement during late Eocene to Miocene times. Recent activity along the fault is observed. (Handy et al, 2005; Mancktelow et al, 2001; Sprenger, 1996)
definition: Die in etwa E-W-streichende Störung entlang des Gailtals zählt zum Pustertal-Gailtal-Teilstörungssystem des Periadriatischen Störungssystems. Es zeigt eine duktile und spröde Deformation mit dextral-seitenverschiebender Kinematik vom Eozän bis ins Miozän. Rezente seismische Aktivität ist beschrieben. (Handy et al, 2005; Mancktelow et al, 2001; Sprenger, 1996) @de
references: https://data.geoscience.earth/ncl/geoera/ref/778
references: https://data.geoscience.earth/ncl/geoera/ref/838
references: https://data.geoscience.earth/ncl/geoera/ref/752
in scheme: Tectonic Boundary Objects in Europe
broader: Pustertal-Gailtal Subfault System

Pustertal Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4781
notation: IT-4190
hidden label: Pusteria Fault
preferred label: Pustertal-Störung @de
preferred label: Linea della Pusteria @it
definition: This approximately E-W trending Fault along the valley of the River Puster is part of the Pustertal-Gailtal Subfault System of the large-scale Periadriatic Fault System. It shows a long-lasting history with right-lateral ductile and brittle movement during late Eocene to Miocene times. Recent activity along the fault is observed. (Handy et al, 2005; Mancktelow et al, 2001; Sprenger, 1996)
definition: Die in etwa E-W-streichende Störung entlang des Pustertals zählt zum Pustertal-Gailtal-Teilstörungssystem des Periadriatischen Störungssystems. Es zeigt eine duktile und spröde Deformation mit dextral-seitenverschiebender Kinematik vom Eozän bis ins Miozän. Rezente seismische Aktivität ist beschrieben. (Handy et al, 2005; Mancktelow et al, 2001; Sprenger, 1996) @de
definition: Linea ad andamento SSE-NNO con cimenatica transpressiva destra. @it
references: https://data.geoscience.earth/ncl/geoera/ref/778
type: Concept
created: 2020-04-30T14:26:59.409Z
references: https://data.geoscience.earth/ncl/geoera/ref/838
notation: AT-10278
references: https://data.geoscience.earth/ncl/geoera/ref/752
in scheme: Tectonic Boundary Objects in Europe
broader: Pustertal-Gailtal Subfault System

Giudicarie North Line
references: https://data.geoscience.earth/ncl/geoera/ref/4773
references: https://data.geoscience.earth/ncl/geoera/ref/4791
preferred label: Nördliche Judikarien-Störung @de
type: Concept
created: 2020-10-16T07:56:52.632Z
notation: IT-4195
preferred label: Linea delle Giudicarie nord @it
definition: NE-SW transfer zone acting first with a sinistral strike-slip displacement of some tens kms, then inverted as thrust with a western domain overthrusting the eastern one.
definition: Linea di traferimento NE-SO che ha agito prima con un movimento trascorrente sinsitro di alcune decine di mk, quindi invertita a sovrascorrimento con il settore occidentale a sovrascorrere quello orientale. Https://doi.org/10.1016/j.tecto.2005.10.019 @it
in scheme: Tectonic Boundary Objects in Europe
broader: Periadriatic Fault System
broader: Giudicarie-Brenner-Silltal Large-scale Fault System
broader: Insubric Fault System

Canavese Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4782
references: https://data.geoscience.earth/ncl/geoera/ref/4793
preferred label: Canavese-Störung @de
type: Concept
created: 2020-10-16T07:56:52.576Z
notation: IT-4248
preferred label: Linea del Canavese @it
definition: SW-NE trending lineament with dextral strike slip movement.
definition: Linea ad andamento SO-NE con movimento trascorrente destro. @it
in scheme: Tectonic Boundary Objects in Europe
broader: Insubric Fault System
broader: Periadriatic Fault System

Tonale Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4785
preferred label: Tonale-Störung @de
type: Concept
created: 2020-10-16T07:56:52.604Z
notation: IT-4254
preferred label: Linea del Tonale @it
definition: W-E trending lineament with dextral strike slip movement, up to 100 km.
definition: Linea ad andamento O-E con movimento trascorrente destro fino a 100 km. @it
in scheme: Tectonic Boundary Objects in Europe
broader: Insubric Fault System
broader: Periadriatic Fault System

Insubric Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/4793
preferred label: Insubrische Linie @de
definition: This fault system demarcates the boundary between Africa and Europe plates. It is the original suture, potentially dating back to the Hercynian orogeny, which separates the S-verging Southalpine from the N-verging Penninic and Austroalpine domains. It is constituted, from west to east, by the SW-NE Canavese Line and the W-E Tonale Line (with important dextral strike slip movements (60-100 km along the Tonale Fault). The displacement continues along its eastern prolongation, the SW-NE N-Giudicarie Line, the NNW-SSE Pusteria and Gailtal Lines.
narrower: Giudicarie North Line
narrower: Pustertal-Gailtal Subfault System
narrower: Periadriatic Fault
type: Concept
created: 2020-10-16T07:56:52.549Z
notation: IT-9904
preferred label: Linea Insubrica @it
definition: Questo sistema di faglie marca il limite tra le placche europea e africana; è una zona di sutura, potenzialmente riferibile già all'orogenesi ercinica, che separa il Sudalpino, vergente a sud, dai domini Pennidico e Austroalpino, con vergenza verso nord. Esso è costituito, da ovest verso est: dalla linea del Canavese, ad andamento SO-NE, e da quella del Tonale, ad andamento O-E, caratterizzate da una rilevante componente trascorrente destra del movimento (60-100 km lungo la linea del Tonale), dalla linea delle Giudicarie, ad andamento SO-NE, dalla linea della Pusteria e Gailtal, ad andamento NNO-SSE. Questo sistema di faglie è parte del lineamento regionale denominato Periadriatico. @it
narrower: Canavese Fault
narrower: Tonale Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Periadriatic-Mid-Hungarian Large-scale Fault System
broader: Tectonic Boundary in Italy

Idrija Triassic Fault Set
preferred label: Idrijski triasni prelomni snop @sl
type: Concept
created: 2020-08-19T13:00:03.254Z
definition: Idrija Triassic Fault Set is a system of predominately E-W striking Triassic (Ladinian) normal faults, related to the aborted continental rifting at the edge of the expanding Meliata Ocean (Mlakar & Čar, 2009, and references therein). Faulting led to formation of half-grabens, filled with thick succession of the clastic rocks, connected with volcanic activity and Hg mineralization of the famous Idrija mercury mine. Normal faults are cut by younger thrusts of the External Dinaric Thrust Belt or faults of the Dinaric Fault System.
notation: SI-9
narrower: Rudišče Fault
narrower: Zavratec Fault
narrower: Ledine Fault
narrower: Ravenovo Fault
references: https://data.geoscience.earth/ncl/geoera/ref/1155
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Slovenia

Zavratec Fault
preferred label: Zavraški prelom @sl
references: https://data.geoscience.earth/ncl/geoera/ref/1155
type: Concept
created: 2020-08-19T13:00:03.309Z
definition: E-W striking Triassic (Ladinian) normal – (aborted) rifting related – fault, E from the Idrija town (central-west Slovenia) (Mlakar & Čar, 2009, and references therein).
notation: SI-9.002
in scheme: Tectonic Boundary Objects in Europe
broader: Idrija Triassic Fault Set

Ledine Fault
preferred label: Ledinski prelom @sl
type: Concept
created: 2020-08-19T13:00:03.337Z
definition: E-W striking Triassic (Ladinian) normal – (aborted) rifting related – fault, N from the Idrija town (central-west Slovenia) (Mlakar & Čar, 2009, and references therein).
notation: SI-9.003
references: https://data.geoscience.earth/ncl/geoera/ref/1155
in scheme: Tectonic Boundary Objects in Europe
broader: Idrija Triassic Fault Set

Ravenovo Fault
preferred label: Ravenovški prelom @sl
type: Concept
created: 2020-08-19T13:00:03.365Z
definition: SSE-NNW striking Triassic (Ladinian) normal – (aborted) rifting related – fault, W from the Idrija town (central-west Slovenia) (Mlakar & Čar, 2009, and references therein).
notation: SI-9.004
references: https://data.geoscience.earth/ncl/geoera/ref/1155
in scheme: Tectonic Boundary Objects in Europe
broader: Idrija Triassic Fault Set

Rudišče Fault
preferred label: Rudiščni prelom @sl
references: https://data.geoscience.earth/ncl/geoera/ref/1155
type: Concept
created: 2020-08-19T13:00:03.281Z
definition: E-W striking Triassic (Ladinian) normal – (aborted) rifting related – fault, SE from the Idrija town (central-west Slovenia) (Mlakar & Čar, 2009, and references therein).
notation: SI-9.001
in scheme: Tectonic Boundary Objects in Europe
broader: Idrija Triassic Fault Set

Tectonic Boundary in Austria
scope note: All named tectonic boundary objects that are located (at least partly) in Austria, are identified by an ID with the prefix „AT“ listed in the notation. Fault systems and/or fault domains can cross political borders and are therefore shared by several countries. Therefore, they can contain faults from different countries, indicated by country-specific prefixes to the respective ID.
definition: Instance of a tectonic boundary, as as they appear on the HIKE European fault database. They were published on the Geological Map of Austria at the scale of 1:1.000.000 of the Geological Survey of Austria.
narrower: Styrian Fault Set
narrower: Eisenstadt Fault
narrower: Emsrütti Fault
narrower: Formarin Fault
narrower: Gallneukirchen Fault
narrower: Inntal Thrust
narrower: Male Karpaty Fault
narrower: Mattersburg Fault
narrower: Moldanubian Thrust
narrower: Pöll Fault
narrower: Pregarten Fault
narrower: Vils Fault
narrower: Stollkogel-Schrankeck Fault
narrower: Mödring Fault
narrower: Katschbachtal Fault
narrower: Korneuburg Fault System
narrower: Anger-Piregg Fault
narrower: Csapod Fault
top concept of: Tectonic Boundary Objects in Europe
narrower: Klostertal Fault
narrower: Leogang Fault
has map: https://gis.geologie.ac.at/geoserver/ge_tectlines/wms
narrower: Vorau Fault
narrower: Wiesmath Fault
type: Concept
created: 2020-04-30T14:26:58.675Z
definition: Instanz einer Tektonischer Grenzfläche, wie sie in Datensätzen und Karten der Geologischen Bundesanstalt publiziert ist. @de
preferred label: Tektonische Grenzfläche in Österreich @de
narrower: Engadin-Inntal-Innsbruck-Salzburg-Amstetten Large-scale Fault System
narrower: Diendorf-Boskovice-Cebin Large-scale Fault System
narrower: Giudicarie-Brenner-Silltal Large-scale Fault System
narrower: Periadriatic-Mid-Hungarian Large-scale Fault System
narrower: Mur-Mürz-Vienna Basin-Vah Large-scale Fault System
notation: AT-0
narrower: Kourim-Blanice-Rodl-Kaplice Large-scale Fault System
narrower: Vitis-Pribyslav Fault System
narrower: Salzach-Ennstal-Mariazell-Puchberg Fault System
narrower: Nappe Boundary in Austria
narrower: Rust Fault System
narrower: Niedere Tauern Southern Margin Fault System
narrower: Ostergunten Fault System
narrower: Palten-Liesing Fault System
narrower: Pfahl Fault System
narrower: Pöls-Lavanttal Fault System
narrower: Drautal-Zwischenbergen-Wöllatratten Fault System
narrower: Iseltal Fault System
narrower: Ragga-Teuchl Fault System
narrower: Görtschitztal Fault System
narrower: Hochstuhl-Gegendtal Fault System
narrower: Defereggen-Antholz-Vals Fault System
narrower: Danube Fault System
narrower: Jachymov Fault System
narrower: Karlstift Fault System
narrower: Mölltal Fault System
narrower: Kalkstein-Vallarga Fault System
narrower: NCA ENE-WSW Fault Set
narrower: NCA NW-SE Fault Set
narrower: NCA NE-SW Fault Set
narrower: NCA E-W Fault Set
narrower: NCA NNE-SSW Fault Set
narrower: Gurktal Alps Subfault System
narrower: Tauern Window Subfault System
narrower: Königsee-Lammertal-Traunsee Subfault System
narrower: Telfs Subfault System
narrower: Trojeralm Fault Set
narrower: Freyenstein Fault System
narrower: West Molasse Fault Set
narrower: NE Molasse Fault Set
narrower: Iller Valley Fault
in scheme: Tectonic Boundary Objects in Europe

Görtschitztal Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/748
references: https://data.geoscience.earth/ncl/geoera/ref/757
references: https://data.geoscience.earth/ncl/geoera/ref/780
notation: AT-114
type: Concept
created: 2020-04-30T14:27:01.218Z
definition: This ca. 50 km long, approximately NNW-SSE trending Fault System between the Gurktal and Sau Alps extends from the Neumarkt Sattel, following the Görtschitz Valley via Hüttenberg and Brückl to the Drau Valley. Its terminology and subdivision was in detail described by Fritsch (1963). It shows a significant vertical displacement with uplift of the E block during Eocene and Oligocene times indicated by deposits of the Gosau sediments in the Krappfeld. Proofs for right-lateral movement in the Miocene are described. (Frisch et al, 1998, 2003)
definition: Dieses in etwa NNW-SSE-streichende ca. 50 km lange Störungssystem verläuft vom Neumarkter Sattel über Hüttenberg, das Görtschitztal zwischen Gurktaler Alpen und Saualpe über Brückl bis ins Drautal. Zur Nomenklatur und die Aufsplitterung in verschiedene Teiläste wurde von Fritsch (1963) beschrieben. Die Bewegungsphasen lassen sich in mehrere Zeitabschnitte untergliedern: Ein signifikanter vertikaler Versatz und Hebung des Ostteils, was mit einem eozänen bis oligozänen Einsenken der Gosauvorkommen des Krappfeldes in Verbindung stehen wird angenommen, welcher sich im Miozän als dextrale Seitenverschiebung fortsetzt. (Frisch et al, 1998, 2003) @de
preferred label: Görtschitztal-Störungssystem @de
narrower: Görtschitztal Fault
narrower: Griffen Fault
narrower: Zollfeld Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Görtschitztal Fault
definition: The NNE-SSW trending brittle fault with right-lateral movement in the Görtschitz Valley is part of the Görtschitztal Fault System (Fritsch, 1963).
definition: Die NNW-SSE-streichende dextral-seitenverschiebende spröde Störung ist Teil des Görtschitztal-Störungssystem (Fritsch, 1963). @de
references: https://data.geoscience.earth/ncl/geoera/ref/780
notation: AT-10090
type: Concept
created: 2020-04-30T14:27:01.247Z
preferred label: Görtschitztal-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Görtschitztal Fault System

Zollfeld Fault
definition: The NNE-SSW trending fault from Glanegg to Althofen in the area of the Zollfeld (Carinthia) at the border to the Klagenfurt basin is part of the Görtschitztal Faultsystem (Kahler, 1953).
definition: Die NNE-SSW-streichende Störung im Zollfeld (Kärnten) von Glanegg bis Althofen ist Teil des Görtschitztal-Störungssystems am Rand des Klagenfurter Beckens (Kahler, 1953). @de
references: https://data.geoscience.earth/ncl/geoera/ref/758
notation: AT-10419
type: Concept
created: 2020-04-30T14:27:01.304Z
preferred label: Zollfeld-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Görtschitztal Fault System

Griffen Fault
definition: The NNE-SSW trending fault with right-lateral movement in the area of the town Griffen is part of the Görtschitztal Faultsystem and runs from about 4 km north of St. Oswald to Bleiburg (Kleinschmidt & Wurm, 1966; Seeger & Thiedig, 1983).
definition: Die NNE-SSW-streichende Störung mit dextral-seitenverschiebender Kinematik ist Teil des Görtschitztal-Störungssystem und verläuft von 5 km nördlich von St. Oswald bis Bleiburg (Kleinschmidt & Wurm, 1966; Seeger & Thiedig, 1983). @de
references: https://data.geoscience.earth/ncl/geoera/ref/735
references: https://data.geoscience.earth/ncl/geoera/ref/836
notation: AT-10096
type: Concept
created: 2020-04-30T14:27:01.276Z
preferred label: Griffen-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Görtschitztal Fault System

Male Karpaty Fault
type: Concept
created: 2020-04-30T14:27:03.470Z
definition: This NE-SW trending fault is a part of the Vienna Basin Fault System (FS) at the eastern border of the Vienna Basin in the area of the Little Carpathian Mountains (Male Karpaty). It has normal faulting character. (Lenhardt et al., 2007; Nemcok et al., 1989)
definition: Ist eine NE-SW-streichende Störung als Teil des Wien-Beckens Störungssystem (STS) am Ostrand des Wiener Beckens im Bereich der Kleinen Karpathen (Male Karpaty) mit initial abschiebender Kinematik. (Lenhardt et al., 2007; Nemcok et al., 1989) @de
preferred label: Kleine Karpathen-Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/738
references: https://data.geoscience.earth/ncl/geoera/ref/785
notation: AT-10152
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Giudicarie-Brenner-Silltal Large-scale Fault System
narrower: Giudicarie North Line
definition: Dieses grob N-S (teilweise NNE-SSW)-streichende ca. 250 km Großstörungssystem zieht vom Etschtal im Süden über Bozen bis Meran, wo es sich in mehrere Äste, über das Passeiertal bis Sterzing und die Sarntaler Alpen bis Mauls verzweigt, dann weiter nach Norden über den Brenner und das Silltal bis nach Innsbruck zum Inntal. Es setzt sich aus dem S und N-Judikarien- und Brenner-Silltal-Störungssystem zusammen und beinhaltet auch mehrere etwa parallel streichende (Teil)-Störungssysteme, wie das Jaufen-Passeier-Störungssystem (Viola et al., 2001), Meran-Mauls-Störungssystem (Viola et. al., 2001; Schmid et al., 2013), Fartleis-Pejo-Teilstörungssystem und das Naif-Völlan-Trento-Cles-Teilstörungssystem. Ihr signifikantes Erscheinungsbild ist der sinistrale Versatz des Canavese-Tonale-Periadriatisch-Mittelungarisches Großstörungssystem um 80 km (Pomella et al., 2011 und die darin angegebenen Referenzen). Eine Anlage bzw. Erhaltung von präexistierenden überschiebenden kretazischen und eozänen Scherzonen und dextralen Seitenverschiebungen ist beschrieben (Fügenschuh et al., 1997, Pomella et al., 2015). Ihre Hauptprägung dieses Großstörungssystem erfolgte bei der oligozänen-miozänen Intendierung der Adriatischen Mikroplatte nach Norden mit einer sinistral seitenverschiebenden Komponente und teilweise überschiebende Strukturen im südlichen Abschnitt. Aktivität bis in rezente Zeiten ist beobachtbar. @de
references: https://data.geoscience.earth/ncl/geoera/ref/740
references: https://data.geoscience.earth/ncl/geoera/ref/763
references: https://data.geoscience.earth/ncl/geoera/ref/769
references: https://data.geoscience.earth/ncl/geoera/ref/828
references: https://data.geoscience.earth/ncl/geoera/ref/833
type: Concept
created: 2020-04-30T14:26:59.128Z
definition: This ca. 250 km long, approximately N-S (and partly NNE-SSW) trending large-scale fault system extends from the Adige (Etsch) Valley at its southern end via Trento, Bolzano to Merano (IT) where it splits into several branches, along the Passeier Valley until Sterzing (IT) and along the Sarntal Mountains until Mauls. It continues towards the north via the Brenner and Sill Valleys until Innsbruck (AT). It includes several parallel trending (sub-)fault systems, like the Orobic Subfault System, the S-and N-Giudicarie Fault System, the Meran-Mauls Fault System (Viola et. al., 2001; Schmid et al., 2013), the Jaufen–Passeier Fault System, the Fartleis-Pejo Subfault System (Viola et al., 2001), the Naif-Völlan-Trento–Cles Subfault System and the Brenner-Silltal Fault System. The major characteristic of this large-scale fault system is the left-lateral displacement of the Canavese-Tonale-Periadraric-Midhungarian Large-scale Fault System for about 80 km (Pomella et al., 2011 and reference therein). Proofs of pre-existing thrusting and right-lateral strike-slip faulting during Cretaceous and Eocene times are observed. (Fügenschuh et al., 1997; Pomella et al, 2015). The main deformation phase of this large-scale fault system occurred during the Oligocene-Miocene northward movement of the Adriatic microplate. This is combined with left-lateral strike-slip and thrusting components at its southern part. Recent activity along the fault is observed.
narrower: Brenner-Silltal Fault System
notation: AT-6
narrower: fault (IT-0030)
narrower: fault (IT-0048)
narrower: fault (IT-0051)
narrower: fault (IT-4189)
in scheme: Tectonic Boundary Objects in Europe
preferred label: Giudicarie-Brenner-Silltal-Großstörungssystem @de
broader: Tectonic Boundary in Austria
broader: Tectonic Boundary in Italy

fault (IT-0051)
type: Concept
created: 2020-10-16T07:56:52.493Z
notation: IT-0051
in scheme: Tectonic Boundary Objects in Europe
broader: Austroalpine Domain
broader: Giudicarie-Brenner-Silltal Large-scale Fault System

fault (IT-4189)
type: Concept
created: 2020-10-16T07:56:52.521Z
notation: IT-4189
in scheme: Tectonic Boundary Objects in Europe
broader: Giudicarie-Brenner-Silltal Large-scale Fault System
broader: Austroalpine Domain

fault (IT-0048)
type: Concept
created: 2020-10-16T07:56:52.436Z
notation: IT-0048
in scheme: Tectonic Boundary Objects in Europe
broader: Giudicarie-Brenner-Silltal Large-scale Fault System
broader: Austroalpine Domain

Brenner-Silltal Fault System
definition: This ca. 45 km long, approximately N-S-trending Fault System extends from Sterzing (IT) to the Brenner Pass following the Sill Valley to the Inn Valley, where it is cut by the Engadin-Inntal Fault System. It includes the Brenner and Silltal subfault systems and parallel trending faults and shear zones. Proofs of pre-existing nappe boundaries with top E and W kinematics during Cretaceous, reactivated from the late Oligocene to Miocene as W-dipping normal fault with top W sense of shear and left-lateral strike-slip faults are observed (Fügenschuh et al., 1997). Displacement rates are discussed controversially, depending on the vertical displacement reaching from 10 up to 27,5 km and the dip-angles of the normal fault, indicating a total displacement of 14 to 70 km respectively. (Fügenschuh et al., 1997 and references therein; Rosenberg & Garcia, 2011)
definition: Dieses grob N-S-streichende ca. 45 km lange Störungssystem zieht von Sterzing über den Brennerpass und das Silltal bis ins Inntal, wo es vom Engadin-Inntal-Störungssystem abgeschnitten wird. Es beinhaltet das Brenner- und das Silltal-Teilstörungssystem mit parallel verlaufenden Störungen und Scherzonen. Seine Anlage als kreidezeitliche Deckengrenze mit EW-Kinematik und eine spät-Oligozäne bis Miozäne Reaktivierung als W-einfallende Abschiebung mit top W-gerichteter Kinematik sowie sinistral seitenverschiebender Kinematik wurden beschrieben. Ein Vertikalversatz von 10-27,5 km und dip-slip Versatzweiten von 14-70 km werden diskutiert. (Fügenschuh et al., 1997 und die darin aufgeführten Referenzen; Rosenberg & Garcia, 2011) @de
references: https://data.geoscience.earth/ncl/geoera/ref/833
type: Concept
created: 2020-04-30T14:26:59.156Z
preferred label: Brenner-Silltal-Störungssystem @de
narrower: Brenner Subfault System
narrower: Silltal Fault
narrower: Portjoch Fault
notation: AT-104
in scheme: Tectonic Boundary Objects in Europe
broader: Giudicarie-Brenner-Silltal Large-scale Fault System

Brenner Subfault System
definition: This N-S trending fault system in the area of the Brenner Pass is part of the Brenner-Silltal Fault System. Normal faulting is described (Fügenschuh et al., 2000).
definition: Diese N-S-streichende Störung im Bereich des Brennerpasses ist Teil des Brenner-Silltal-Störungssystem. Abschiebende Kinematik ist beschrieben (Fügenschuh et al., 2000). @de
references: https://data.geoscience.earth/ncl/geoera/ref/853
type: Concept
created: 2020-04-30T14:26:59.184Z
preferred label: Brenner-Teilstoerungssystem @de
narrower: Brenner Fault
narrower: Brenner Shearzone
notation: AT-578
in scheme: Tectonic Boundary Objects in Europe
broader: Brenner-Silltal Fault System

Brenner Fault
definition: This N-S trending fault in the area of the Brenner Pass is part of the Brenner-Silltal Fault System. Steep brittle normal faulting is described (Fügenschuh et al., 2000).
definition: Diese N-S-streichende Störung im Silltal (W des Brennerpasses) ist Teil des Brenner-Silltal-Störungssystem. Steilstehende spröde abschiebende Kinematik ist beschrieben (Fügenschuh et al., 2000). @de
references: https://data.geoscience.earth/ncl/geoera/ref/853
type: Concept
created: 2020-04-30T14:26:59.212Z
preferred label: Brenner-Stoerung @de
notation: AT-10022
in scheme: Tectonic Boundary Objects in Europe
broader: Brenner Subfault System

Brenner Shearzone
definition: The N-S trending ductile shear zone in the area of the Brenner Pass is part of the Brenner-Silltal Fault System. Gently dipping ductile normal faulting is described (Fügenschuh et al., 2000).
definition: Diese N-S-streichende Störung im Silltal (W des Brennerpasses) ist Teil des Brenner-Silltal-Störungssystem. Flach einfallende duktile abschiebende Kinematik ist beschrieben (Fügenschuh et al., 2000). @de
references: https://data.geoscience.earth/ncl/geoera/ref/853
type: Concept
created: 2020-04-30T14:26:59.240Z
preferred label: Brenner-Scherzone @de
notation: AT-1006
in scheme: Tectonic Boundary Objects in Europe
broader: Brenner Subfault System

Silltal Fault
definition: This N-S trending fault in the area of the Brenner Pass is part of the Brenner-Silltal Fault System. Normal faulting is described (Fügenschuh et al., 2000).
definition: Diese N-S-streichende Störung im Silltal (W des Brennerpasses) ist Teil des Brenner-Silltal-Störungssystem. Abschiebende Kinematik ist beschrieben (Fügenschuh et al., 2000). @de
references: https://data.geoscience.earth/ncl/geoera/ref/853
type: Concept
created: 2020-04-30T14:26:59.268Z
preferred label: Silltal-Stoerung @de
notation: AT-10330
in scheme: Tectonic Boundary Objects in Europe
broader: Brenner-Silltal Fault System

Portjoch Fault
definition: This N-S trending fault in the area of Mt. Portjoch (W of the Brenner Pass) is part of the Brenner-Silltal Fault System. Normal faulting is described (Fügenschuh et al., 2000).
definition: Die N-S-streichende Störung im Bereich des Portjoch (W des Brennerpasses) ist Teil des Brenner-Silltal-Störungssystem. Abschiebende Kinematik ist beschrieben (Fügenschuh et al., 2000). @de
references: https://data.geoscience.earth/ncl/geoera/ref/853
type: Concept
created: 2020-04-30T14:26:59.296Z
preferred label: Portjoch-Störung @de
notation: AT-10266
in scheme: Tectonic Boundary Objects in Europe
broader: Brenner-Silltal Fault System

fault (IT-0030)
type: Concept
created: 2020-10-16T07:56:52.380Z
notation: IT-0030
in scheme: Tectonic Boundary Objects in Europe
broader: Austroalpine Domain
broader: Giudicarie-Brenner-Silltal Large-scale Fault System

Diendorf-Boskovice-Cebin Large-scale Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/738
references: https://data.geoscience.earth/ncl/geoera/ref/845
type: Concept
created: 2020-04-30T14:26:58.987Z
definition: This ca. 230 km long, approximately NNE-SSW (and partly NE-SW) trending Large-scale Fault System extends from Cebin (CZ), following the Boskovice furrow and the graben of Zöbing to Diendorf in the south. It includes the Diendorf-Boskovice Fault System and Cebin Fault, showing a long-lasting and multiphase history. Parallel trending structures and conjugated shear zones and faults are correlated with this Large-scale Fault System. Proofs of NE-SW-trending left-lateral strike-slip partly ductile, mylonitic shear zones during upper Carboniferous and Permian times are observed in the Diendorf Subfault System. To the north it continues to horst-graben structures filled with upper Carboniferous to Permian sediments (Rostinsky et al., 2001). The deformation continuous left-lateral strike-slip faulting during Miocene and recent times. (Lenhardt et al., 2007; Rostinsky et al., 2013)
definition: Dieses in etwa NNE-SSW – streichende (teilweise NE-SW), ca. 230 km lange Großstörungssystem zieht sich von Cebin (CZ), entlang dem Boskovice-Graben, dann von Miozänen Sedimenten bedeckt bis zum Graben von Zöbing und weiter bis Diendorf. Es setzt sich aus dem Diendorf-Boskovice-Störungssystem und der Cebin-Störung zusammen und zeigt eine langandauernde und multiphase Entwicklung. Parallel streichende Strukturen und konjugierte Scherzonen und Störungen werden mit diesem Großstörungssystem assoziiert. Duktile mylonitische Scherzonen mit sinistral seitenverschiebender Kinematik des oberen Karbons bis Perms (Rostinsky et al., 2013) sind vorwiegend entlang des Diendorf-Teilstörungssystem beschrieben und setzt sich nach Norden in von oberkarbonen-permischen Sedimenten verfüllte Horst und Grabenstruktur fort (Rostinsky et al., 2001). Diese wird durch spröde Störungen mit sinistral seitenverschiebender Kinematik überprägt, welche bis in rezente Zeit beobachtbar sind. (Lenhardt et al., 2007; Rostinsky et al., 2013) @de
preferred label: Diendorf-Boskovice-Cebin-Großstörungssystem @de
narrower: Diendorf-Boskovice Fault System
notation: AT-2
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Diendorf-Boskovice Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/738
references: https://data.geoscience.earth/ncl/geoera/ref/845
narrower: Diendorf Subfault System
type: Concept
created: 2020-04-30T14:26:59.015Z
definition: This ca. 200 km long, approximately NNE-SSW (and partly NE-SW) trending Fault System extends from the Boskovice furrow and the graben of Zöbing to Diendorf in the south. It includes the Diendorf and Boskovice Subfault System, showing a long-lasting and multiphase history. Proofs of NE-SW-trending left-lateral strike-slip partly ductile, mylonitic shear zones during upper Carboniferous and Permian times are observed in the Diendorf Subfault System. To the north it continues to horst-graben structures filled with upper Carboniferous to Permian sediments (Rostinsky et al., 2001). The deformation continuous left-lateral strike-slip faulting during Miocene and recent times. (Lenhardt et al., 2007; Rostinsky et al., 2013)
definition: Dieses in etwa NNE-SSW - streichende (teilweise NE-SW) ca. 200 km lange Großstörungssystem zieht vom Boskovice-Graben bis zum Graben von Zöbing und weiter bis Diendorf. Es setzt sich aus dem Diendorf- und Boskovice-Teilstörungssystemen zusammen und zeigt eine langandauernde und multiphase Entwicklung. Duktile mylonitische Scherzonen mit sinistral seitenverschiebender Kinematik des oberen Karbons bis Perms (Rostinsky et al., 2013) sind vorwiegend entlang des Diendorf-Teilstörungssystem beschrieben und setzt sich nach Norden in von oberkarbonen-permischen Sedimenten verfüllte Horst und Grabenstruktur fort (Rostinsky et al., 2001). Diese wird durch spröde Störungen mit sinistral seitenverschiebender Kinematik überprägt, welche bis in rezente Zeit beobachtbar sind. (Lenhardt et al., 2007; Rostinsky et al., 2013) @de
preferred label: Diendorf-Boskovice-Störungssystem @de
notation: AT-108
in scheme: Tectonic Boundary Objects in Europe
broader: Diendorf-Boskovice-Cebin Large-scale Fault System

Diendorf Subfault System
type: Concept
created: 2020-04-30T14:26:59.043Z
definition: This subfault system contains the Austrian part of the Diendorf-Boskovice fault system and consists of several parallel NNE-SSW trending faults.
definition: Dieses Substörungssystem umfasst den österreichischen Teil des Diendorf-Boskovice-Störungssystems und setzt sich aus verschiedenen parallel zueinander laufenden, haupsächlich NNE-SSE streichenden Störungen zusammen. @de
preferred label: Diendorf-Teilstörungssystem @de
narrower: Mörtersdorf Fault
narrower: Waitzendorf Fault
notation: AT-505
in scheme: Tectonic Boundary Objects in Europe
broader: Diendorf-Boskovice Fault System

Mörtersdorf Fault
definition: The N-S striking normal fault runs in the valley of the River Kamp from Fernitz to Kammern, where it terminates at a subfault of the Diendorf-Boskovice Fault System. Top to the west faulting was active during the Eggenburgian.
definition: Die N-S-streichende Abschiebung verläuft im Kamptal von Fernitz bis Kammern, wo sie an einer Teilstörung des Diendorf-Boskovice-Störunggssystems endet. Die Bewegungsrichtung des Hangendblocks ging im Eggenburgium gegen Westen. @de
type: Concept
created: 2020-04-30T14:26:59.071Z
preferred label: Mörtersdorf-Störung @de
notation: AT-10449
in scheme: Tectonic Boundary Objects in Europe
broader: Diendorf Subfault System

Waitzendorf Fault
definition: This NE-SW trending fault extends from Waitzendorf towards Retz and Znojmo (CZ). It runs parallel to and northwest of the Diendorf Fault. The Waitzendorf Fault delimits the Thaya Batolith towards the East. Cataclastic fault rocks indicate mainly brittle deformation along the fault.
definition: Diese NE-SW-streichende Störung verläuft zwischen Waitzendorf, Retz und Znojmo (CZ, Znaim), nordwestlich und parallel zur Diendorf-Störung. Diese Störung begrenzt den Thaya-Batholith nach Osten hin. Kataklase Störungsgesteine weisen auf eine hauptsächlich spröde Deformation hin. @de
type: Concept
created: 2020-04-30T14:26:59.099Z
preferred label: Waitzendorf-Störung @de
notation: AT-10478
in scheme: Tectonic Boundary Objects in Europe
broader: Diendorf Subfault System

Emsrütti Fault
type: Concept
created: 2020-04-30T14:27:03.327Z
definition: NE-SW striking normal fault between the towns of Götzis, Hohenems and Dornbirn that offsets the eastern margin of the Rhine Valley. (Oberhauser, 1991, Zerlauth, 2014)
definition: NE-SW streichende Abschiebung, die zwischen Götzis, Hohenems und Dornbirn den Ostrand des Rheintales abschiebend versetzt. (Oberhauser, 1991; Zerlauth, 2014) @de
preferred label: Emsrütti-Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/774
references: https://data.geoscience.earth/ncl/geoera/ref/745
notation: AT-10434
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Ragga-Teuchl Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/790
references: https://data.geoscience.earth/ncl/geoera/ref/786
notation: AT-139
type: Concept
created: 2020-04-30T14:27:01.161Z
definition: This ca. 35 km long, approximately NW-SE, partly NNE-SSW trending Fault System extends from Baldramsdorf in the Möll Valley to Teuchl and the Ragga-Alm. Here, it is displaced left-laterally by the Wöllatratten Fault. Then it extends from Stall up to Sagritz. It includes parallel trending shear zones and faults (Hoke, 1990). Proofs of pre-existing nappe boundaries during Cretaceous times which were reactivated as ductile shear zones and faults with right-lateral strike-slip movement during Oligocene times are observed (Ilickovic & Schuster, 2014).
definition: Dieses etwa WNW-ESE-streichende ca. 35 km lange Störungssystem zieht sich von Baldramsdorf im Mölltal über Teuchl und die Ragga-Alm. Im oberen Mölltal wird sie sinistral von der Wöllatratten-Störung versetzt und verläuft von Stall weiter bis Sagritz. Es beinhaltet parallel verlaufenden Störungen und Scherzonen (Hoke, 1990). Es wurde als Deckengrenze in der Oberkreide angelegt und als duktile Scherzonen und spröde Störungen mit dextral seitenverschiebender Kinematik im Oligozän reaktiviert (Ilickovic, 2014). @de
preferred label: Ragga-Teuchl-Störungssystem @de
narrower: Ragga-Teuchl Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Ragga-Teuchl Fault
references: https://data.geoscience.earth/ncl/geoera/ref/790
references: https://data.geoscience.earth/ncl/geoera/ref/786
notation: AT-10284
type: Concept
created: 2020-04-30T14:27:01.190Z
definition: The Ragga-Teuchl fault represents the brittle part of the Ragga-Teuchl Fault System and shows right-lateral movement. (Hoke, 1990; Ilickovic & Schuster, 2014)
definition: Die Ragga-Teuchl-Störung repräsentiert den spröden Anteil des Ragga-Teuchl-Störungssystems mit spröder dextral seitenverschiebender Kinematik. (Hoke, 1990; Ilickovic & Schuster, 2014) @de
preferred label: Ragga-Teuchl-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Ragga-Teuchl Fault System

Eisenstadt Fault
created: 2020-04-30T14:27:03.299Z
definition: The NE-SW striking and SE-dipping fault runs from Grosshöflein via Eisenstadt along the southeastern side of the Leitha Mountains towards Parndorf. The main deformation phase shows normal faulting character. (Tollmann, 1986)
definition: Die NE-SW streichende, nach SE einfallende Störung verläuft von Großhöflein über Eisenstadt südöstlich vom Leithagebirge bis nach Parndorf. Die Hauptdeformation hat abschiebenden Charakter. (Tollmann, 1986) @de
preferred label: Eisenstadt-Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/732
type: Concept
notation: AT-10051
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Gallneukirchen Fault
type: Concept
created: 2020-04-30T14:27:03.384Z
definition: The NW-SE striking fault runs from Gallneukirchen via Mauthausen to Strengberg into the Molasse subsurface. It forms the SW margin of the Gallneukirchen Basin with top-to-the-NE normal movement. (Kröll et al., 2001; Seiberl et al., 1996)
definition: Die NW-SE streichende Störung verläuft von Gallneukirchen über Mauthausen nach Strengberg in den Molasseuntergrund. Sie formt die SW-Grenze des Gallneukirchen-Beckens, wobei das Hangende gegen NE abgeschoben wurde. (Kröll et al., 2001; Seiberl et al., 1996) @de
preferred label: Gallneukirchen-Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/728
references: https://data.geoscience.earth/ncl/geoera/ref/743
notation: AT-10075
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Formarin Fault
type: Concept
created: 2020-04-30T14:27:03.356Z
definition: This NW-SE striking fault runs SW of the Rote Wand mountain from the Laguzbach Valley to Lake Formarin. (Tollmann, 1986).
definition: Diese NW-SE streichende Störung verläuft südwestlich der Roten Wand vom Laguzbachtal zum Formarinsee. (Tollmann, 1986) @de
preferred label: Formarin-Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/732
notation: AT-10452
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

NCA E-W Fault Set
references: https://data.geoscience.earth/ncl/geoera/ref/840
references: https://data.geoscience.earth/ncl/geoera/ref/841
notation: AT-528
type: Concept
created: 2020-04-30T14:27:02.285Z
definition: This fault set of E-W trending faults within the Northern Calcareous Alps includes the Ebner Fault, Königsberg Fault, and Spullersee Fault amongst other similar orientated faults with same kinematics. These faults were probably generated during Oligocene-Early Miocene times as reverse faults. During Late Miocene N-S extension compression, they might have been reactivated as normal faults. (Peresson & Decker, 1997a, b)
definition: Dieses Störungsset von E-W-streichenden Störungen in den Nördlichen Kalkalpen (NKA) beinhaltet die Ebner-, Königsberg-, Spullersee- und weitere ähnlich orientierte Störungen mir derselben Kinematik. Diese Störungen entwickelten sich seit dem Oligozän bis frühem Miozän als Überschiebungen und wurden während des späten Miozän als Abschiebungen reaktiviert. (Peresson & Decker, 1997a, b) @de
preferred label: NKA-Störungsset (E-W) @de
narrower: Ebner Fault
narrower: Grünalmkogel Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Grünalmkogel Fault
references: https://data.geoscience.earth/ncl/geoera/ref/732
notation: AT-10453
type: Concept
created: 2020-04-30T14:27:02.341Z
definition: The NE-SW striking fault runs from the Outer Weissenbach Valley at the Grünalmkogel moutain (Höllengebirge moutains) to the Langbathseen. (Tollmann, 1986)
definition: Die NE-SW streichende Störung verläuft vom Tal des Äußeren Weißenbach am Grünalmkogel (Höllengebirge) vorbei zu den Langbathseen. (Tollmann, 1986) @de
preferred label: Grünalmkogel-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: NCA E-W Fault Set

Ebner Fault
references: https://data.geoscience.earth/ncl/geoera/ref/737
references: https://data.geoscience.earth/ncl/geoera/ref/782
notation: AT-10049
type: Concept
created: 2020-04-30T14:27:02.313Z
definition: Is an E-W-trending brittle thrust fault in the western Northern Calcareous Alps (NCA). (Eisbacher & Brandtner, 1995, 1996)
definition: Ist eine E-W-streichende spröde Störung mit überschiebender Kinematik in den westlichen Nördlichen Kalkalpen (NKA). (Eisbacher & Brandtner, 1995, 1996) @de
preferred label: Ebner-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: NCA E-W Fault Set

Korneuburg Fault System
type: Concept
created: 2020-04-30T14:27:03.186Z
preferred label: Korneuburg-Teilstörungssystem @de
narrower: Schliefberg Fault
definition: This subfault system consists all faults related to the subsidence of the Korneuburg Basin NW of Vienna. It includes the Schliefberg and the Helfens Fault.
definition: Dieses Teilstörungssystem beinhaltet alle Störungen, die im Zusammenhang mit der Einsenkung des Korneuburger Beckens im NW von Wien im Zusammenhang stehen, z.B. die Schliefberg- und Helfens-Störung. @de
notation: AT-571
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Schliefberg Fault
type: Concept
created: 2020-04-30T14:27:03.214Z
definition: The normal fault dips with more than 60° to ESE and limits the Korneuburg basin towards the WNW. The hanging wall in the E is offset by 800 m. (Wessely, 2006)
definition: Die mit über 60° nach ESE einfallende Abschiebung begrenzt das Korneuburger Becken nach WNW hin ab. Das Hangende im E wird um 800 m versetzt. (Wessely, 2006) @de
preferred label: Schliefberg-Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/849
notation: AT-10428
in scheme: Tectonic Boundary Objects in Europe
broader: Korneuburg Fault System

Drautal-Zwischenbergen-Wöllatratten Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/786
references: https://data.geoscience.earth/ncl/geoera/ref/783
notation: AT-110
type: Concept
created: 2020-04-30T14:27:01.019Z
definition: This ca. 60 long, NE-SW trending Fault System extends from Sillian, following the Drau Valley to Lienz. Here, it is displaced dextral-laterally by the Iseltal Fault System. The eastern part starts in Zwischenbergen, following the upper Möll Valley to Wöllatratten and Flattach. Itself it displaces the Ragga-Teuchl Fault System and includes parallel trending faults and shear zones. Proofs of pre-existing nappe boundaries during Cretaceous times, reactivated as left-lateral strike-slip faults during Miocene times are observed. (Ilickovic & Schuster, 2014; Probst et al, 2003)
definition: Dieses NE-SW -streichende ca. 60 km lange Störungssystem zieht sich von Sillian, das Drautal entlang bis Lienz wo es durch das Iseltal-Störungssystem dextral versetzt wird und dann über Zwischenbergen das obere Mölltal bis Wöllatratten und Flattach folgt. Es versetzt das Ragga-Teuchl- Störungssystem und beinhaltet parallel verlaufende Störungen und Scherzonen, welche als kreidezeitliche Deckengrenze angelegt und als sinistral seitenverschiebende Scherzonen und Störungen im Oligozän und Miozän reaktiviert wurden. (Ilickovic & Schuster, 2014; Probst et al, 2003) @de
preferred label: Drautal-Zwischenbergen-Wöllatratten-Störungssystem @de
narrower: Drautal Fault
narrower: Zwischenbergen-Wöllatratten Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Drautal Fault
definition: The ENE-WSW trending brittle fault along the Drau Valley, from Sillian to Lienz, with left-lateral movement was active during the Miocene (Probst et al., 2003).
definition: Die NE-SW-streichende spröde Störung entlang des Drautales, von Sillian nach Lienz, mit sinistral-seitenverschiebender Kinematik war im Miozän aktiv (Probst et al., 2003). @de
references: https://data.geoscience.earth/ncl/geoera/ref/783
notation: AT-10040
type: Concept
created: 2020-04-30T14:27:01.047Z
preferred label: Drautal-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Drautal-Zwischenbergen-Wöllatratten Fault System

Zwischenbergen-Wöllatratten Fault
definition: The ENE-WSW trending brittle fault of the Drautal-Zwischenbergen-Wöllatratten Fault System was reactivated as left-lateral strike-slip fault during the Oligocene and Miocene (Probst et al, 2003).
definition: Die NE-SW-streichende spröde Störung des Drautal-Zwischenbergen-Wöllatratten-Störungssystemes wurde als sinistral seitenverschiebende Scherzonen und Störungen im Oligozän und Miozän reaktiviert wurden (Probst et al, 2003). @de
references: https://data.geoscience.earth/ncl/geoera/ref/783
notation: AT-10422
type: Concept
created: 2020-04-30T14:27:01.076Z
preferred label: Zwischenbergen-Wöllatratten-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Drautal-Zwischenbergen-Wöllatratten Fault System

Csapod Fault
references: https://data.geoscience.earth/ncl/geoera/ref/760
type: Concept
created: 2020-04-30T14:27:03.271Z
definition: The NNE-SSW trending fault runs from Tadten and Parnhagen via Fertöszentmiklós (HUN) east of Csapod to Bö (HUN). It dips steeply towards the ESE and has been deformed as a normal fault. The main deformation phase occurred presumably during Eggenburgian and Sarmatian. (Csaszar, G., 2000)
definition: Die NNE-SSW streichende Störung verläuft von Tadten und Parnhagen über Fertöszentmiklós (HUN) östlich von Csapod bis nach Bö (HUN). Sie fällt steil nach ESE ein und hat abschiebenden Bewegungscharakter. Die Hauptbewegungsphase war vermutlich zwischen Eggenburgium und Sarmatium. (Csaszar, G., 2000) @de
preferred label: Csapod-Störung @de
notation: AT-10471
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Iseltal Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/823
notation: AT-153
type: Concept
created: 2020-04-30T14:27:01.104Z
definition: This ca. 90 km long, approximately NW-SE trending Fault System extends from Matrei in Osttirol, following the Isel Valley to Oberdrauburg, continuing to St. Georgen im Gitschtal and Görtschach. It displaces the Drautal-Zwischenbergen-Wöllatratten Fault System and includes structures trending parallel to the Isel Valley. Proofs for right-lateral ductile (northern parts) and brittle movement during Miocene times with displacement rates of approximately 15-20 km are described. (Linzer et al., 2002)
definition: Dieses in etwa NW-SE-streichende ca. 90 km lange Störungssystem zieht von Matrei im Osttirol über das Iseltal entlang bis Oberdrauburg, weiter über St. Georgen im Gitschtal bis Görtschach. Es versetzt das Drautal-Zwischenbergen-Wöllatratten- Störungssystem und beinhaltet parallel zum Iseltal verlaufenden Störungen, welche während des Miozän als Störungen und Scherzonen (nördliche Anteile) mit dextral seitenverschiebender Kinematik aktiv waren. Versatzweiten von 15-20 km werden beschrieben. (Linzer et al., 2002) @de
preferred label: Iseltal-Störungssystem @de
narrower: Iseltal Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Iseltal Fault
definition: This approximately NW-SE trending fault is the part of the Iseltal Fault System and runs extends from Matrei in Osttirol, following the Isel Valley to Lienz and continues parallel to the Drau Valley until Görtschach. Proofs for right-lateral ductile (northern parts) and brittle movement during Miocene times with displacement rates of approximately 15-20 km are described. (Linzer et al., 2002)
definition: Diese NW-SE-streichende Störung ist Teil des Iseltal-Störungssystem und zieht sich von Matrei im Osttirol über das Iseltal entlang bis Lienz, und weiter im Drautal bis Görtschach. Dextral seitenverschiebender Kinematik und Versatzweiten von 15-20 km werden für das Miozän beschrieben. (Linzer et al., 2002) @de
notation: AT-10125
type: Concept
created: 2020-04-30T14:27:01.133Z
preferred label: Iseltal-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Iseltal Fault System

Anger-Piregg Fault
references: https://data.geoscience.earth/ncl/geoera/ref/779
type: Concept
created: 2020-04-30T14:27:03.242Z
definition: The steeply inclined Arlui Fault extends from Reith via Birkfeld and Anger towards Gleisdorf in an arch-shape. Most probably, the fault has a polyphase deformation history, where the eastern block has been moved downwards. (Schuster & Ilickovic, 2015)
definition: Die steilstehende Störung verläuft bogenförmig von Reith über Birkfeld und Anger bis Gleisdorf. Vermutlich wurde die Störung polyphas bewegt, wobei auf jeden Fall der Ostblock abgesenkt wurde. (Schuster & Ilickovic, 2015) @de
preferred label: Anger-Piregg-Störung @de
notation: AT-10437
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Inntal Thrust
type: Concept
created: 2020-04-30T14:27:03.441Z
definition: This fault is a roughly E-W trending thrust fault. It was active during middle to late Cretaceous times and was reactivated as right-lateral strike-slip fault during Miocene. (Eisbacher & Brandtner, 1996; Ortner et al., 2006)
definition: Diese Überschiebung is eine ungefähr E-W-streichende spröde Überschiebung mit top-to-the-WNW/NW-gerichteter Kinematik, welche während der mittleren bis oberen Kreide angelegt wurde und während des Miozäns als dextrale Seitenverschiebung reaktiviert wurde. (Eisbacher & Brandtner, 1996; Ortner et al., 2006) @de
preferred label: Inntal-Überschiebung @de
notation: AT-1019
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Engadin-Inntal-Innsbruck-Salzburg-Amstetten Large-scale Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/771
references: https://data.geoscience.earth/ncl/geoera/ref/823
type: Concept
created: 2020-04-30T14:26:58.703Z
definition: This ca. 400 km long, approximately WSW-ENE (and partly SW-NE) trending Large-scale Fault System extends from Bregaglia Valley(north of the Bergell massive), following the Inn Valley to Nauders, Pfunds, Imst and Telfs. At Telfs, it is dextrally offset by the Telfs Subfault System. The eastern part strikes from Innsbruck to Wörgl and Kufstein continuing over Salzburg to Amstetten. It includes the Engadin-Inntal and Innsbruck-Salzburg-Amstetten fault systems and shows a long-lasting deformation history with significant displacement. Proofs of thrusting and normal faulting during Cretaceous and Paleogene times are observed (Froitzheim et al., 1997), continuing with left-lateral strike-slip faulting during upper Oligocene to recent times. Displacement reaches up to around 17 km of normal faulting and 74-135 km of left-lateral displacement. (Egger, 1997; Froitzheim et al., 1997; Linzer et al., 2002 and references therein)
definition: Dieses ca. WSW-ESE - streichende ca. 400 km lange Großstörungssystem zieht vom Bregaglia-Tal (nördlich des Bergell-Massivs) über das Inntal bis Nauders, Pfunds, Imst und Telfs. Am Telfs-Teilstörungssystem wird das Großstörungssystem dextral versetzt und verläuft dann von Innsbruck über Wörgl bis Kufstein und dann über Salzburg nach Amstetten. Es beinhaltet das Engadin-Inntal- sowie Innsbruck-Salzburg-Amstetten-Störungssystem und zeigt eine lang andauernde Bewegungsgeschichte mit beträchtlichen Versatzweiten. So wird eine frühe kreidezeitliche bis paläogene Initiierung im Ostteil mit über- und abschiebender Kinematik beschrieben, welche sich vom obersten Oligozän bis rezent mit sinistral seitenverschiebender Kinematik fortsetzt. Eine horizontale Gesamtversatzweite von 74-135 km kann angenommen werden. (Egger, 1997; Froitzheim et al., 1997; Linzer et al., 2002 und die darin aufgeführten Referenzen) @de
preferred label: Engadin-Inntal-Innsbruck-Salzburg-Amstetten-Großstörungssystem @de
narrower: Innsbruck-Salzburg-Amstetten Fault System
narrower: Engadin-Inntal Fault System
notation: AT-3
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Engadin-Inntal Fault System
narrower: Inntal Subfault System
references: https://data.geoscience.earth/ncl/geoera/ref/771
references: https://data.geoscience.earth/ncl/geoera/ref/764
references: https://data.geoscience.earth/ncl/geoera/ref/823
type: Concept
created: 2020-04-30T14:26:58.844Z
definition: This ca. 225 km long, approximately SW-NE trending Fault System extends from Bregaglia Valley (north of the Bergell massive), following the Inn Valley to Nauders, Pfunds, Imst and Telfs. Here, it is displaced right-laterally by the Telfs Subfault System. The eastern part starts in Innsbruck to Wörgl and Kufstein. It includes subfault systems along the Engadin and Inn valleys and parallel trending structures such as the Schlinig, Gallo and Arlui shear zones. It shows a long-lasting history and was initiated as ductile nappe boundaries and shear zones with E-dipping, top-to-the-W-directed thrusting and top-to-the-ESE-directed normal faults during Cretaceous and Paleogene times. During the Oligocene it was reactivated along shear zones with top WNW kinematics (e.g. Engadin and Schlinig shear zones). Left-lateral brittle strike-slip faults are active from the upper Oligocene to the Miocene, indicated by sediment deposits in the Inn Valley (Froitzheim et al, 1997; Ortner et al., 2006). Displacement rates can be summarized, reaching around 17 km of normal faulting and 31-75 km of left-lateral displacement. (Froitzheim et al., 1997; Linzer et al., 2002 and references therein)
definition: Dieses in etwa NE-SW - streichende ca. 225 km Störungssystem zieht vom Bregaglia-Tal (nördlich des Bergell-Massivs) über das Inntal bis Nauders, Pfunds, Imst und Tels. Es wird am Telfs-Teilstörungssystem dextral versetzt und verläuft dann von Innsbruck das Inntal weiter über Wörgl bis Kufstein. Es beinhaltet die Engadin- und Inntal-Teilstörungssysteme sowie parallel verlaufende Strukturen, wie die Schlinig-, Gallo- und Arlui-Scherzonen. Die Bewegungsphasen lassen sich in mehrere Zeitabschnitte untergliedern: So wird eine Initiierung als duktile Deckengrenzen und Scherzonen mit W-gerichteten Überschiebungen und nach E-einfallende, top-to-the-ESE-Abschiebungen während der Oberkreide bis Paläogen, mit einer überschiebenden Reaktivierung im Oligozän entlang der Engadin-Scherzone beschrieben. Ihre spröde Hauptprägung erfuhr sie im späten Oligozän bis Miozän mit sinistral seitenverschiebender Kinematik und Sedimentation im Inntal. Auch rezente seismische Aktivität ist bekannt (Froitzheim et al, 1997; Ortner et al., 2006). Ermittelte Versatzweiten zeigen ca. 17 km abschiebende Werte, sinistral seitenverschiebende Versatzweiten für das Engadin-Teilstörungssystem von 3-20 km und für das Inntal-Teilstörungssystem von 31-75 km. (Linzer et al., 2002 und die darin aufgeführten Referenzen) @de
preferred label: Engadin-Inntal-Störungssystem @de
narrower: Engadin Subfault System
narrower: Schlinig Subfault System
notation: AT-111
in scheme: Tectonic Boundary Objects in Europe
broader: Engadin-Inntal-Innsbruck-Salzburg-Amstetten Large-scale Fault System

Schlinig Subfault System
references: https://data.geoscience.earth/ncl/geoera/ref/771
type: Concept
created: 2020-04-30T14:26:58.929Z
definition: This approximately 20 km long N-S striking subfault system runs between the Reschen Pass (Passo die Resia) and the area of the Vinschgau (Venosta Valley). The subfault system displaces the Ötztal nappe base by approximately 17 km (Froizheim et al., 1997).
definition: Diese ca. 20 km lange N-S streichende Teiltörungssystem verläuft zwischen dem Reschenpass und dem Vinschgau und ist Teil des Engadin-Innsbruck-Störungssystemes. Das Substörungssystem versetzt die Ötztalbasisüberschiebung um ca. 17 km (Froizheim et al. 1997). @de
preferred label: Schlinig-Teilstörungssystem @de
narrower: Schlinig Fault
notation: AT-548
in scheme: Tectonic Boundary Objects in Europe
broader: Engadin-Inntal Fault System

Schlinig Fault
references: https://data.geoscience.earth/ncl/geoera/ref/771
references: https://data.geoscience.earth/ncl/geoera/ref/827
type: Concept
created: 2020-04-30T14:26:58.958Z
definition: The fault trace on the map describes a concave line towards the W (Trümpy, 1980) that extends from the Reschen Pass (Passo di Resia) to the Vinschgau (Venosta Valley). Froizheim et al. (1997) postulates that the Schlinig Fault, together with its southern continuation, the Gallo Fault, was generated as Late Cretaceous fault with top-to-the-SE shear sense.
definition: Der Ausbiss der Schlining-Störung in der Karte beschreibt eine nach W hin konkave Linie (Trümpy, 1980), die sich vom Reschenpass bis zum Vinschgau hinzieht. Froizheim et al. (1997) postuliert die Schlinig-Störung zusammen mit ihrer südlichen Fortsetzung, der Gallo-Störung, als spätkretazische Abschiebung mit top-to-the-SE Schersinn. @de
preferred label: Schlinig-Störung @de
notation: AT-10317
in scheme: Tectonic Boundary Objects in Europe
broader: Schlinig Subfault System

Engadin Subfault System
references: https://data.geoscience.earth/ncl/geoera/ref/771
references: https://data.geoscience.earth/ncl/geoera/ref/823
type: Concept
created: 2020-04-30T14:26:58.901Z
definition: This ca. 155 km long, approximately NE-SW trending fault system extends from Bregaglia Valley (North of the Bergell Massive), following the Inn Valley to Nauders, Pfunds, Imst and Tels. It includes faults along the Engadin Valley and parallel trending structures such as the Schlinig, Gallo, and Arlui shear zones. It shows a long-lasting deformation history and was initiated as ductile nappe boundaries and shear zones with E-dipping, top-to-the-W-directed thrusting and top-to-the-ESE-directed normal faults during Cretaceous and Paleogene times. During the Oligocene, it was reactivated along shear zones with top-to-the-WNW kinematics (e.g. Engadin and Schlinig shear zones). Left-lateral brittle strike-slip faults were active from the Upper Oligocene to the Miocene (Froitzheim et al, 1997). Total displacement amounts up to around 17 km normal faulting and 3-20 km left-lateral displacement. (Froitzheim et al., 1997; Linzer et al., 2002 and references therein)
definition: Dieses in etwa NE-SW - streichende ca. 155 km lange Teilstörungssystem zieht vom Bregaglia-Tal (nördlich des Bergell-Massivs) über das Inntal bis Nauders – Pfunds –Imst bis Telfs. Es beinhaltet entlang und parallel des Engadin- Gebietes verlaufende Scherzonen und Störungen, wie die Schlinig-, Gallo und Arlui-Scherzonen. Eine Initiierung als duktile Deckengrenzen und Scherzone mit W-gerichteten Überschiebungen und Richtung E-einfallende top-ESE-Abschiebungen während der Oberkreide bis Paläogen, mit einer überschiebenden Reaktivierung im Oligozän ist beschrieben (Froitzheim et al., 1997). Ihre spröde Hauptprägung erfuhr sie im späten Oligozän bis Miozän mit sinistral seitenverschiebender Kinematik. Versatzweiten von ca. 17 km abschiebender Komponente und von 3-20 km sinistral seitenverschiebender Versatzweiten werden angenommen. (Froitzheim et al., 1997; Linzer et al., 2002 und die darin aufgeführten Referenzen) @de
preferred label: Engadin-Teilstörungssystem @de
notation: AT-506
narrower: Gallo Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Engadin-Inntal Fault System

Gallo Fault
type: Concept
created: 2020-10-16T07:56:52.409Z
notation: IT-0040
in scheme: Tectonic Boundary Objects in Europe
broader: Austroalpine Domain
broader: Engadin Subfault System

Inntal Subfault System
references: https://data.geoscience.earth/ncl/geoera/ref/823
references: https://data.geoscience.earth/ncl/geoera/ref/771
type: Concept
created: 2020-04-30T14:26:58.759Z
definition: This ca. 170 km long, approximately SW-NE trending subfault system extends from Innsbruck, following the Inn Valley to Wörgl and Kufstein and then to Salzburg and Thalgau. It includes faults and shearzones along the Inn Valley and parallel trending structures. Left-lateral brittle strike-slip faults are active from the Upper Oligocene to the Miocene, indicated by sediment deposits described in the Inn Valley (Froitzheim et al, 1997; Ortner et al., 2006). Seismic activity has been observed along the Inn Valley. Total displacement reaches up to around 17 km normal faulting and 31-75 km left-lateral displacement. (Froitzheim et al., 1997; Linzer et al., 2002 and references therein)
definition: Dieses in etwa NE-SW - streichende ca. 170 km lange Teilstörungssystem läuft das Inntal entlang von Innsbruck-Wörgl bis Kufstein und weiter über Salzburg bis Thalgau. Es beinhaltet entlang und parallel des Inntals verlaufende Störungen und Scherzonen. Ihre spröde Hauptprägung erfuhr sie im späten Oligozän bis Miozän mit sinistral seitenverschiebender Kinematik und Sedimentation im Inntal. Auch rezente seismische Aktivität ist bekannt. Es wurden Versatzweiten von 31-75 km ermittelt. (Froitzheim et al., 1997; Linzer et al., 2002 und die darin aufgeführten Referenzen) @de
preferred label: Inntal-Teilstörungssystem @de
narrower: Inntal Shear zone
narrower: Inntal Fault
notation: AT-507
in scheme: Tectonic Boundary Objects in Europe
broader: Engadin-Inntal Fault System
broader: Innsbruck-Salzburg-Amstetten Fault System

Inntal Fault
definition: Die WSW-ENE-streichende spröde Störung ist Teil des Inntal-Teilstörungssystems. (Froitzheim et al., 1997; Linzer et al., 2002 und die darin aufgeführten Referenzen) @de
definition: The WSW-ENE trending brittle fault is part of the of the Inntal Subfault System. (Froitzheim et al., 1997; Linzer et al., 2002 and references therein)
references: https://data.geoscience.earth/ncl/geoera/ref/771
references: https://data.geoscience.earth/ncl/geoera/ref/823
type: Concept
created: 2020-04-30T14:26:58.816Z
preferred label: Inntal-Stoerung @de
notation: AT-10121
in scheme: Tectonic Boundary Objects in Europe
broader: Inntal Subfault System

Inntal Shear zone
definition: The WSW-ENE trending shearzone containing the ductile part of the Inntal Subfault System, extends north of the Inn Valley over more than 80 km from south of Obergilben to north of Innsbruck and Hall/Tirol. (Froitzheim et al., 1997; Linzer et al., 2002 and references therein)
definition: Die WSW-ENE-streichende und 10-20 km breite duktile Scherzone, die Teil des Inntal-Teilstörungssystems ist, erstreckt sich nördlich des Inntales über mehr als 80 km von südlich von Obergilben bis nördlich von Innsbruck und Hall in Tirol. (Froitzheim et al., 1997; Linzer et al., 2002 und die darin aufgeführten Referenzen) @de
references: https://data.geoscience.earth/ncl/geoera/ref/771
references: https://data.geoscience.earth/ncl/geoera/ref/823
type: Concept
created: 2020-04-30T14:26:58.787Z
preferred label: Inntal-Scherzone @de
notation: AT-1019
in scheme: Tectonic Boundary Objects in Europe
broader: Inntal Subfault System

Innsbruck-Salzburg-Amstetten Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/851
type: Concept
created: 2020-04-30T14:26:58.731Z
definition: The term Innsbruck-Salzburg-Amstetten Fault System (ISAM) was first mentioned by Egger (1997). He describes a mainly sinistral strike-slip fault system between Innsbruck, Salzburg and Amstetten which has offset the southern edge of the Northern Calcareous Alps by at least 40 km. The fault system runs parallel to the Inntal Shear Zone between Innsbruck and Kufstein. Between Salzburg and the Lake Mondsee, the fault runs along the northern rim of the Northern Calcareous Alps and runs between the lakes Mondsee and Attersee within the Flysch zone north of Hochplett. East of Lake Attersee, Egger (1997) describes two fault branches belonging to the ISAM. The Pettenbach Fault and a related fault in the south running from northern rim of the Ultrahelvetic Units from Gschliefgraben (Lake Traunsee) via the village of Untergrünburg (Steyrtal) towards Amstetten. In addition, all sinistral fault branches are kinematically linked to ISAM, which emerge from the ISAM and thereby offset the Rhenodanubian Flyschzone. (Egger, 1997)
definition: Der Begriff Innsbruck-Salzburg-Amstetten-Störungssystem (ISAM) wurde von Egger (1997) zum ersten Mal erwähnt. Er beschreibt damit ein hauptsächlich sinistrales Blattverschiebungssystem zwischen Innsbruck, Salzburg und Amstetten, das den Kalkalpensüdrand um mindestens 40 km versetzt hat. Zwischen Innsbruck und Kufstein verläuft das Störungssystem parallel zur Inntalscherzone (bzw. entspricht der Inntalstörung). Zwischen Salzburg und dem Mondsee entspricht der Verlauf der Nordbegrenzung der Kalkalpen und verläuft zwischen Mond- und Attersee innerhalb der Flyschzone nördlich von Hochplett. Östlich vom Attersee werden von Egger (1997) zwei zur Innsbruck-Salzburg-Amstetten-Störungssystem gehörige Störungsäste beschrieben, die Pettenbach-Störung sowie ein südlich davon verlaufender Störungsast, der am Nordrand des Ultrahelvetikums von Gschliefgraben (Traunsee) über Untergrünburg (Steyrtal) nach Amstetten verläuft. Kinematisch verlinkt zur Innsbruck-Salzburg-Amstetten-Störungssystem sind zusätzlich alle sinistralen Störungsäste, die aus dieser abbiegen und dabei die Rhenodanubische Flyschzone versetzen. (Egger, 1997) @de
preferred label: Innsbruck-Salzburg-Amstetten-Störungssystem @de
narrower: Inntal Subfault System
notation: AT-152
in scheme: Tectonic Boundary Objects in Europe
broader: Engadin-Inntal-Innsbruck-Salzburg-Amstetten Large-scale Fault System

Mur-Mürz-Vienna Basin-Vah Large-scale Fault System
preferred label: Mur-Mürz-Wiener-Becken-Vah-Großstörungssystem @de
definition: Dieses ca. 400 km lange Großstörungssystem beinhaltet von S nach N das Mur-Mürz-Störungssystem, das Wiener Becken-Störungssystem sowie das Vah-Störungssystem (Decker et al., 2005) und ist kinematisch mit Überschiebungen in den äußeren Karpaten in Galizien (POL) verbunden. Es besteht hauptsächlich aus ENE-WSW-streichenden sinistralen Seitenverschiebungen und NNE-SSW-streichenden Abschiebungen. Seine Hauptphase war während des Miozäns als Folge der Ost-Bewegung der Ostalpen (Ratschbacher et al. 1991, Linzer et al., 2002). Versatzweiten von bis zu 40 km entlang des Abschnittes Mur-Mürz-Wiener Becken wurden ermittelt (Linzer et al., 2002). Erste Untersuchungen zu Erdbeben von Gutdeusch & Aric (1988) entlang der sogenannten Mur-Mürz-Wiener Becken-Zilina seismologische Zone deuten auf rezente seismische Aktivität hin. @de
references: https://data.geoscience.earth/ncl/geoera/ref/8691
references: https://data.geoscience.earth/ncl/geoera/ref/777
references: https://data.geoscience.earth/ncl/geoera/ref/765
references: https://data.geoscience.earth/ncl/geoera/ref/823
has map: http://egditest01.geus.dk/egdi/
type: Concept
created: 2020-04-30T14:26:59.578Z
definition: From S to N, this ca. 400 km long Large-scale Fault System includes the Mur-Mürz Fault System, Vienna Basin Fault System, and the Vah Fault System (Decker et al., 2005) and seems to be kinematically linked to thrust faults in the outer Carpathians in Polish Galicia. This large-scale fault system consists mostly of ENE-WSW trending left-lateral strike-slip and NNE-SSW trending normal faulting. Onset of faulting along the entire large-scale fault system started in the Miocene as consequence of eastward extrusion of the Central Eastern Alps (Ratschbacher et al. 1991, Linzer et al., 2002). In total, Miocene offset in the Mur-Mürz-Vienna Basin area has been estimated to up to 40 km (Linzer et al., 2002). Earthquakes have been observed for the first time along the so-called Mur-Mürz-Vienna Basin-Zilina seismogenic zone by Gutdeusch & Aric (1988) proving recent activity of the large-scale fault system.
narrower: Mur-Mürz Fault System
narrower: Vienna Basin Fault System
notation: AT-5
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Mur-Mürz Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/749
references: https://data.geoscience.earth/ncl/geoera/ref/823
type: Concept
created: 2020-04-30T14:26:59.607Z
definition: The ca. 130 km long, approximately ENE-WSW trending fault system extends from Judenburg along the Mur and Mürz Valleys and builds the southern border of the Vienna Basin close to Gloggnitz (Frisch et al., 2002). The fault system consists mostly of left-lateral strike-slip faults, but includes also small pull-apart basins. Based on sedimentary deposits in the pull-apart basins, left-lateral deformation started in the Karpatian (Linzer et al., 2002). Miocene offset reaches up to 40 km. (Linzer et al., 2002)
definition: Dieses ca. 130 km lange, ungefähr ENE-WSW-streichende Störungssystem verläuft von Judenburg, entlang des Mur- und Mürztales und bildet den Südrand des Wiener Beckens nahe Gloggnitz (Frisch et al, 2002). Es zeigt vorwiegend sinistral seitenverschiebende Kinematik mit der Bildung kleinerer Pull-Apart-Becken. Anhand sedimentärer Ablagerungen belegt, startet die Entwicklung im Karpatium, mit Versatzweiten bis zu 40 km. (Linzer et al., 2002) @de
preferred label: Mur-Mürz-Störungssystem @de
narrower: Mürz Fault
narrower: Mur Fault
notation: AT-131
in scheme: Tectonic Boundary Objects in Europe
broader: Mur-Mürz-Vienna Basin-Vah Large-scale Fault System

Mur Fault
preferred label: Mur-Störung @de
definition: This approximately ENE-WSW trending fault is part of the Mur-Mürz Fault System. It extends along the river Mur and shows left-lateral movement (Linzer et al., 2002; Tollmann, 1986). Recent seismic activity has been recorded along the fault (Reinecker & Lenhardt, 1999).
definition: Die ungefähr ENE-WSW-streichende Störung ist teil des Mur-Mürz-Störungssystems. Sie erstreckt sich entlang des Murtales mit sinistral-seitenverschiebender Kinematik. (Linzer et al., 2002; Tollmann, 1986). Rezente seismische Aktivität ist beschrieben (Reinecker & Lenhardt, 1999). @de
references: https://data.geoscience.earth/ncl/geoera/ref/732
references: https://data.geoscience.earth/ncl/geoera/ref/823
references: https://data.geoscience.earth/ncl/geoera/ref/8692
type: Concept
created: 2020-04-30T14:26:59.664Z
notation: AT-10220
in scheme: Tectonic Boundary Objects in Europe
broader: Mur-Mürz Fault System

Mürz Fault
references: https://data.geoscience.earth/ncl/geoera/ref/732
references: https://data.geoscience.earth/ncl/geoera/ref/823
type: Concept
created: 2020-04-30T14:26:59.635Z
definition: This approximately ENE-WSW trending fault extends along the valley of the river Mürz and shows left-lateral movement. (Linzer et al., 2002; Tollmann, 1986)
definition: Es ist eine ungefähr ENE-WSW-streichende Störung entlang des Mürztales mit sinistral-seitenverschiebender Kinematik. (Linzer et al., 2002; Tollmann, 1986) @de
preferred label: Mürz-Störung @de
notation: AT-10221
in scheme: Tectonic Boundary Objects in Europe
broader: Mur-Mürz Fault System

Vienna Basin Fault System
preferred label: Wiener-Becken-Störungssystem @de
references: https://data.geoscience.earth/ncl/geoera/ref/8691
references: https://data.geoscience.earth/ncl/geoera/ref/724
references: https://data.geoscience.earth/ncl/geoera/ref/829
references: https://data.geoscience.earth/ncl/geoera/ref/835
references: https://data.geoscience.earth/ncl/geoera/ref/848
type: Concept
created: 2020-04-30T14:26:59.692Z
definition: The almost 200 km long, NNE-SSW trending, rhombohedral Vienna Basin consists of mostly NE-SW striking oblique left-lateral strike-slip faults at its eastern margin and NNE-SSW trending listric normal faults compensating E-W extension (Decker, 1996). It extends from Gloggnitz at its southern end via the recent flood plain of the River Danube between Vienna and Hainburg at its widest point towards Zilina in the North. Formation of the Vienna Basin Fault System started due to pull-apart subsidence during the Badenian at around 16 Ma and lasted until 9 - 8 Ma (Decker, 1996; Peresson & Decker, 1997; Hölzel et al., 2010). Quaternary reactivation is indicated by dissected Pleistocene terraces and Quaternary basins (Decker et al., 2005, Beidinger & Decker, 2011).
definition: Dieses ca. 200 km lange, NNE-SSW-streichende Störungssystem beinhaltet alle Störungen und Strukturen des rhomboedrischen Wiener Pull-Apart-Beckens mit vorwiegend NE-SW-streichenden sinistralen Seitenverschiebungen an seinem Ostrand und NNE-SSW-streichende listrische Abschiebungen als Folge seiner E-W-Extension (Decker, 1996). Es zieht von Gloggnitz, seinem Südende, über die Donau zwischen Wien und Hainburg bis Zilina, an seinem Nordende. Es entstand als Pull-Apart-Becken während des Badenium (ca. 16 Ma) bis ins obere Miozän (9-8 Ma; Decker, 1996, Peresson & Decker, 1997; Hölzel et al., 2010). Quartäre Reaktivierungen der Störungen werden durch pleistozäne Terassenbildungen und quartäre Beckenbildungen dokumentiert (Decker et al., 2005, Beidinger & Decker, 2011). @de
narrower: Poysbrunn Fault
narrower: Mitterndorf Subfault System
narrower: Schrattenberg Fault
narrower: Steinberg Fault
narrower: Pirawarth-Hochleiten Subfault System
narrower: Leopoldsdorf Fault
narrower: Markgrafneusiedl Fault
narrower: Matzen Subfault System
narrower: Nussdorf Fault
narrower: Aderklaa-Bockfliess Subfault System
narrower: Bisamberg Fault
narrower: Engelhartstetten Fault
narrower: Lassee Subfault System
in scheme: Tectonic Boundary Objects in Europe
notation: AT-154
broader: Mur-Mürz-Vienna Basin-Vah Large-scale Fault System

Markgrafneusiedl Fault
references: https://data.geoscience.earth/ncl/geoera/ref/730
references: https://data.geoscience.earth/ncl/geoera/ref/727
references: https://data.geoscience.earth/ncl/geoera/ref/829
type: Concept
created: 2020-04-30T14:26:59.976Z
definition: The NE-SW, partly N-S trending, steeply E-dipping normal fault in the central part of the Vienna Basin runs from Fischamend via Wittau to Markgrafneusiedl. Between Markgrafneusiedl and Gänserndorf, it forms the eastern margin of the Pleistocene Gänserndorf terrace (Beidinger & Decker, 2011; Schopper, 1992; Wessely, 2000).
definition: Die NE-SW, teilweise N-S-streichende, steil nach E einfallende Störung mit abschiebender Kinematik verläuft im zentralen Wiener Becken von Fischamend via Wittau nach Markgrafneusiedl. Zwischen Markgrafneusiedl und Gänserndorf bildet sie die östliche Begrenzung der pleistozänen Gänserndorfterrasse (Beidinger & Decker, 2011; Schopper, 1992; Wessely, 2000). @de
preferred label: Markgrafneusiedl-Störung @de
notation: AT-10200
in scheme: Tectonic Boundary Objects in Europe
broader: Vienna Basin Fault System

Leopoldsdorf Fault
definition: This NNW-SSE trending, steeply E-dipping normal fault in the western part of the Vienna Basin running from Ebreichsdorf via Leopoldsdorf towards the City of Vienna. The Leopoldsdorf Fault crosses Vienna from Oberlaa via Schwedenplatz towards Strebersdorf (Küpper, 1968; Plachy, 1981; Beidinger & Decker, 2011).
definition: Diese NNW-SSE-streichende, steil nach E einfallende Störung mit abschiebender Kinematik verläuft im westlichen Wiener Becken von Ebreichsdorf via Leopoldsdort nach Wien. Im Wiener Stadtgebiet lässt sie sich von Oberlaa über den Schwedenplatz bis nach Strebersdorf verfolgen (Küpper, 1968; Plachy, 1981; Beidinger & Decker, 2011). @de
references: https://data.geoscience.earth/ncl/geoera/ref/854
references: https://data.geoscience.earth/ncl/geoera/ref/829
type: Concept
created: 2020-04-30T14:26:59.947Z
preferred label: Leopoldsdorf-Störung @de
notation: AT-10179
in scheme: Tectonic Boundary Objects in Europe
broader: Vienna Basin Fault System

Schrattenberg Fault
references: https://data.geoscience.earth/ncl/geoera/ref/741
references: https://data.geoscience.earth/ncl/geoera/ref/730
type: Concept
created: 2020-04-30T14:26:59.804Z
definition: This ENE-WSW trending normal fault splits from the Poysbrunn Fault at Hörersdorf and runs via Poysdorf to Schrattenberg and Valtice at the Austrian-Czech border (Schopper, 1992; Kovac et al., 2004).
definition: Diese ENE-SSW-streichende Störung mit abschiebender Kinematik spaltet sich bei Hörersdorf von der Poysbrunn-Störung nach Osten ab und verläuft via Poysdorf bis nach Schrattenberg bzw. Valtice an der österreichisch-tschechischen Grenze (Schopper, 1992; Kovac et al., 2004). @de
preferred label: Schrattenberg-Störung @de
notation: AT-10320
in scheme: Tectonic Boundary Objects in Europe
broader: Vienna Basin Fault System

Bisamberg Fault
references: https://data.geoscience.earth/ncl/geoera/ref/829
type: Concept
created: 2020-04-30T14:27:00.115Z
notation: AT-10017
definition: It is a NNE-SSW trending brittle normal fault in the northwestern Vienna basin active since the Miocene (Beidinger & Decker, 2011 and references therein).
definition: Es ist eine NNE-SSW-streichende Störung im nordwestlichen Wiener Becken mit abschiebender Kinematik welche seit dem Miozän aktiv ist (Beidinger & Decker, 2011 und die darin aufgeführten Referenzen). @de
preferred label: Bisamberg-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Vienna Basin Fault System

Pirawarth-Hochleiten Subfault System
references: https://data.geoscience.earth/ncl/geoera/ref/849
type: Concept
created: 2020-04-30T14:26:59.861Z
definition: It is a NE-SW trending normal fault in the northern part of the Vienna Basin (Wessely, 2006).
definition: Es ist eine NE-SW-streichende Störung mit abschiebender Kinematik im nördlichen Wiener Becken (Wessely, 2006). @de
preferred label: Pirawarth-Hochleiten-Teilstörungssystem @de
narrower: Putzing Fault
narrower: Kronberg Fault
notation: AT-570
in scheme: Tectonic Boundary Objects in Europe
broader: Vienna Basin Fault System

Kronberg Fault
type: Concept
created: 2020-04-30T14:26:59.918Z
definition: This NE-SW striking and steeply SW dipping fault runs from Münichsthal to the North of Kronberg, parallel to the Putzing Fault (Grill, 1968). The normal offset is between 30 to 70 m.
definition: Diese NE-SW streichende und steil nach SW einfallende Störung verläuft von Münichsthal bis nördlich von Kronberg parallel zur Putzing-Störung (Grill, 1968). Der abschiebende Versatz beträgt zwischen 30 und 70 m. @de
preferred label: Kronberg-Störung @de
notation: AT-10485
in scheme: Tectonic Boundary Objects in Europe
broader: Pirawarth-Hochleiten Subfault System

Putzing Fault
type: Concept
created: 2020-04-30T14:26:59.890Z
definition: This NE-SW striking and steeply SW dipping fault is the southern end of the Pirawarth-Hochleiten Subfault System. It runs from Königsbrunn to Putzing, where it is displaced right-laterally for approximately 900 m by a E-W striking fault. It then continues until Riedenthal and is cut of there by a NW-SE striking fault (Grill, 1968). The normal offset is at least 150 m.
definition: Diese NE-SW streichende und steil nach SW einfallende Störung bildet das südliche Ende des Pirawarth-Hochleiten-Teilstörungssystems. Sie verläuft von Königsbrunn bis Putzing, wo sie durch eine E-W verlaufende Störung um ca. 900 m rechtslateral versetzt wird. Sie verläuft dann weiter nach Norden bis Riedenthal, wo sie durch eine NW-SE streichende Störung abgeschnitten wird (Grill, 1968). Die Sprunghöhe beträgt mindestens 150 m. @de
preferred label: Putzing-Störung @de
notation: AT-10484
in scheme: Tectonic Boundary Objects in Europe
broader: Pirawarth-Hochleiten Subfault System

Lassee Subfault System
references: https://data.geoscience.earth/ncl/geoera/ref/829
definition: Dieses NW-SE streichende Teilstörungssystem erstreckt sich von Wagram an der Donau (AT) im SW via Lassee und Marchegg nach Zohor (SK). Es zeigt die Struktur einer negativen Blumenstruktur und entspricht dem von Beidinger & Decker (2011) beschriebenen Lassee-Segment @de
notation: AT-566
type: Concept
created: 2020-04-30T14:27:00.171Z
definition: This NE-SW trending subfault system extends from Wagram an der Donau (Austria) in the SW via Lassee and Marchegg to Zohor (Slovakia). It has the structure of a negative flower structure and corresponds to the Lassee segment described by Beidinger & Decker (2011)
preferred label: Lassee-Teilstörungssystem @de
narrower: Lassee Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Vienna Basin Fault System

Lassee Fault
definition: This NE-SW trending fault is the main fault of the Lassee subfault system at depth, where all the fault strands reachting at the surface are rooting. It is mainly a strike slipe fault with a normal fault component (Beidinger & Decker, 2011).
notation: AT-10171
type: Concept
created: 2020-04-30T14:27:00.199Z
definition: Diese NE-SW-streichende Störung ist die Hauptstörung des Lassee-Teilstörungssystems, in dem alle an der Oberfläche sichtbaren Störungsäste in der Tiefe zusammenlaufen. Ihre hauptsächliche Kinematik ist sinistral seitenverschiebend mit einer bedeutenden abschiebenden Komponente (Beidinger & Decker, 2011). @de
preferred label: Lassee-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Lassee Subfault System

Steinberg Fault
references: https://data.geoscience.earth/ncl/geoera/ref/741
references: https://data.geoscience.earth/ncl/geoera/ref/829
type: Concept
created: 2020-04-30T14:26:59.833Z
definition: This NNE-SSW striking and steeply ESE dipping fault runs from Gross-Schweinbarth via Zistersdorf and Neusiedl an der Zaya until north of Breclav (CZ; Kovac, 2004). The eastern hanging wall was offest by 5 km of normal faulting during the Miocene. During the Quaternary, this fault was probably reactivated together with other faults in the Vienna Basin. (Decker et al., 2005, Beidinger & Decker, 2011)
definition: Diese NNE-SSW streichende, steil nach ESE einfallende Störung verläuft von Groß-Schweinbarth über Zistersdorf, Neusiedl an der Zaya bis nördlich von Breclav (CZ; Kovac, 2004). Der E-Block wurde während des Miozäns um rund 5 km abgeschoben. Im Quartär wurde die Störung vermutlich zeitgleich mit anderen Störungen im Wiener Becken abschiebend reaktiviert. (Decker et al., 2005; Beidinger & Decker, 2011) @de
preferred label: Steinberg-Störung @de
notation: AT-10340
in scheme: Tectonic Boundary Objects in Europe
broader: Vienna Basin Fault System

Engelhartstetten Fault
references: https://data.geoscience.earth/ncl/geoera/ref/727
notation: AT-10055
type: Concept
created: 2020-04-30T14:27:00.143Z
definition: It is a NE-SW trending fault at the eastern border of the Vienna Basin (Wessely, 2000).
definition: Es ist eine NE-SW-streichende Störung am Ostrand des Wiener Beckens (Wessely, 2000). @de
preferred label: Engelhartstetten-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Vienna Basin Fault System

Poysbrunn Fault
references: https://data.geoscience.earth/ncl/geoera/ref/8693
references: https://data.geoscience.earth/ncl/geoera/ref/849
type: Concept
created: 2020-04-30T14:26:59.720Z
definition: This NNE-SSW trending normal fault is the northwestern margin of the Vienna Basin (Grill, 1968; Wessely, 2006). West of Poysbrunn, the fault runs from Olgersdorf via Falkenstein to Drasenhofen. In Hörersdorf, the Schrattenberg Fault splits from the Poysbrunn Fault.
definition: Diese NNE-SSW-streichende Störung mit abschiebender Kinematik bildet die nordwestliche Begrenzung des Wiener Beckens (Grill, 1968). Sie verläuft westlich von Poysbrunn von Olgersdorf über Falkenstein bis Drasenhofen. Bei Hörersdorf vereint sie sich mit der Schrattenber-Störung (Wessely, 2006). @de
alternative label: Falkenstein Fault
alternative label: Falkensteiner Bruch, Falkenstein-Störung @de
preferred label: Poysbrunn-Störung @de
notation: AT-10430
in scheme: Tectonic Boundary Objects in Europe
broader: Vienna Basin Fault System

Nussdorf Fault
preferred label: Nussdorf-Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/854
type: Concept
created: 2020-04-30T14:27:00.032Z
definition: It is a NNE-SSW trending normal fault in the northwestern part of the Vienna Basin (Küpper, 1968).
definition: Es ist eine NNE-SSW-streichende Störung im nordwestlichen Wiener Becken mit abschiebender Kinematik (Küpper, 1968). @de
notation: AT-10424
in scheme: Tectonic Boundary Objects in Europe
broader: Vienna Basin Fault System

Matzen Subfault System
references: https://data.geoscience.earth/ncl/geoera/ref/730
references: https://data.geoscience.earth/ncl/geoera/ref/727
type: Concept
created: 2020-04-30T14:27:00.004Z
definition: It is a NE-SW trending normal fault in the Vienna Basin. (Schopper, 1992; Wessely, 2000)
definition: Es ist eine NE-SW-streichende Störung im Wiener Becken mit abschiebender Kinematik. (Schopper, 1992; Wessely, 2000) @de
preferred label: Matzen-Teilstörungssystem @de
notation: AT-569
in scheme: Tectonic Boundary Objects in Europe
broader: Vienna Basin Fault System

Mitterndorf Subfault System
definition: This subfault system includes all faults related to the opening of the Mitterndorf Basin, the southernmost subbasin of the Vienna Basin. The Pottendorf Fault is part of this subfault system. Its extent corresponds to the extent of the Mitterndorf-Schwadorf segment described by Beidinger & Decker (2011).
references: https://data.geoscience.earth/ncl/geoera/ref/829
definition: Dieses Teilstörungssystem beinhaltet alle Störungen, die mit der Öffnung des Mitterndorf-Beckens im Süden des Wiener Beckens in Zusammenhang stehen. Die Pottendorf-Störung wird diesem Teilstörungssystem zugerechnet. Das Teilstörungssystem entspricht in der Ausdehnung dem Mitterndorf-Schwadorf-Segment von Beidinger & Decker (2011). @de
type: Concept
created: 2020-04-30T14:26:59.748Z
preferred label: Mitterndorf-Teilstörungssystem @de
narrower: Pottendorf Fault
notation: AT-567
in scheme: Tectonic Boundary Objects in Europe
broader: Vienna Basin Fault System

Pottendorf Fault
references: https://data.geoscience.earth/ncl/geoera/ref/738
references: https://data.geoscience.earth/ncl/geoera/ref/730
references: https://data.geoscience.earth/ncl/geoera/ref/727
references: https://data.geoscience.earth/ncl/geoera/ref/847
type: Concept
created: 2020-04-30T14:26:59.776Z
definition: This NE-SW trending normal fault is located at the southern part of the Vienna Basin. (Lenhardt et al., 2007; Schopper, 1992; Wessely, 1984, 2000)
definition: Es ist eine NE-SW-streichende Störung mit abschiebender Kinematik im südlichen Wiener Becken. (Lenhardt et al., 2007; Schopper, 1992; Wessely, 1984, 2000) @de
preferred label: Pottendorf-Störung @de
notation: AT-10268
in scheme: Tectonic Boundary Objects in Europe
broader: Mitterndorf Subfault System

Aderklaa-Bockfliess Subfault System
references: https://data.geoscience.earth/ncl/geoera/ref/744
references: https://data.geoscience.earth/ncl/geoera/ref/849
preferred label: Aderklaa-Bockfliess-Teilstörungssystem @de
narrower: Aderklaa-Bockfliess Fault
type: Concept
created: 2020-04-30T14:27:00.061Z
definition: This NNE-SSW striking and steeply dipping subfault system consists of several en-echelon faults running from Groß-Enzersdorf via Breitenlee, Aderklaa, Deutsch-Wagram, and Bockfließ to the south of Gross-Schweinbarth (Wessely, 2006). While the northern faults are parallel to the NNE-SSW striking main fault, the southern faults run NW-SE. The western block has been shifted downward during Miocene before it was reactivated in the Quaternary period. (Decker et al., 2005, Weissl et al., 2016)
definition: Dieses NNE-SSW streichende, hauptsächlich steil nach WNW einfallende Teilstörungssystem besteht aus mehreren en-echelon angeordneten Störungen, die von Groß-Enzersdorf über Breitenlee, Aderklaa, Deutsch-Wagram und Bockfließ bis südlich von Groß-Schweinbarth verlaufen (Wessely, 2006) . Während die nördlichen Störungen parallel zur NNE-SSW streichenden Hauptstörung verlaufen, streichen die südlichen Störungen in NW-SE-Richtung. Der W-Block wurde während des Miozäns abgeschoben. Im Quartär wurde die Störung wiederum abschiebend reaktiviert. (Decker et al., 2005, Weissl et al., 2016) @de
notation: AT-568
in scheme: Tectonic Boundary Objects in Europe
broader: Vienna Basin Fault System

Aderklaa-Bockfliess Fault
type: Concept
created: 2020-04-30T14:27:00.088Z
definition: This NNE-SSW striking fault is the main fault of the Aderklaa-Bockfließ subfault system. It is the eastern margin of the Gänserndorf terrace and runs from Aderklaa via Deutsch-Wagram and Bockfließ to the south of Gross-Schweinbarth (Wessely, 2006).
definition: Diese NNE-SSW streichende Störung ist die Hauptstörung des Aderklaa-Bockfliess-Teilstörungssystems. Sie bildet die Ostkante der Gänserndorf-Terrasse und verläuft von Aderklaa über Deutsch-Wagram und Bockfließ bis südlich von Groß-Schweinbarth (Wessely, 2006) @de
preferred label: Aderklaa-Bockfliess-Störung @de
notation: AT-10429
in scheme: Tectonic Boundary Objects in Europe
broader: Aderklaa-Bockfliess Subfault System

Pfahl Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/731
references: https://data.geoscience.earth/ncl/geoera/ref/755
references: https://data.geoscience.earth/ncl/geoera/ref/822
notation: AT-136
type: Concept
created: 2020-04-30T14:27:00.821Z
definition: This NW-SE striking, steep to NE dipping fault system runs from the northeastern edge of the Bavarian Forest (D) through the Czech Republic and runs from Schwarzenberg (A) via Haslach an der Mühl to Rodl, where it is cut off from the Rodl fault system south of Obernaukirchen. The ductile major event, similar to the Rodl fault system, is applied to the late Variscian event, predominantly with a dextral direction of movement. It is considered that during Miocene a brittle reactivation with the same kinematics went on. (Brandmayr et al., 1997; Büttner, 2007; Siebel et al., 2005)
definition: Dieses NW-SE streichende, steil nach NE einfallende Störungssystem zieht sich vom nördöstlichen Rand des Bayrischen Waldes durch die Tschechische Republik und verläuft ab Schwarzenberg (A) über Haslach an der Mühl bis zur Rodl, wo sie südlich von Obernaukirchen vom Rodl-Störungssystem abgeschnitten wird. Die duktile Hauptbewegungsphase wird, analog zum Rodl-Störungssystem, auf das Spätvariszikum gelegt, mit hauptsächlich dextraler Bewegungsrichtung. Von einer spröden miozänen Reaktivierung mit selber Bewegungskinematik wird ebenfalls ausgegangen. (Brandmayr et al., 1997; Büttner, 2007; Siebel et al., 2005) @de
preferred label: Pfahl-Störungssystem @de
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Ostergunten Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/774
notation: AT-149
type: Concept
created: 2020-04-30T14:27:00.736Z
definition: It is a system setting up of several NNE-SSW striking, parallel running sinistral strike-slip faults with normal fault component on the east side of the Kanisfluh-Aniklinale, which extend from Buchboden (Großes Walsertal) via Schönbach-Vorsäße and Sibratsgfäll to Balderschwang (Bavaria, D). All together, the eastern block subsides approximately 600 m. The Ultrahelvetic Unit is offset by about 3 km. (Zerlauth et al., 2014)
definition: Ein System aus mehreren NNE-SSW streichenden, parallel verlaufenden sinistralen Blattverschiebungen mit abschiebenden Komponente an der Ostseite der Kanisfluh-Aniklinale, die sich von Buchboden (Großes Walsertal) über Schönbach-Vorsäße und Sibratsgfäll nach Balderschwang (Bayern, D) hinziehen. Insgesamt kann von ca. 600 m Absenkung des östlichen Blocks ausgegangen werden. Das Ultrahelvetikum wird um ca. 3 km sinistral versetzt. (Zerlauth et al., 2014) @de
preferred label: Ostergunten-Störungssystem @de
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Palten-Liesing Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/1148
references: https://data.geoscience.earth/ncl/geoera/ref/729
references: https://data.geoscience.earth/ncl/geoera/ref/823
notation: AT-134
type: Concept
created: 2020-04-30T14:27:00.764Z
definition: This ca. 65 km long, approximately WNW-ESE trending Fault System extends from Lienz, following the Palten and Liesing Valleys to the village of St. Michael in der Obersteiermark in the Mur Valley. It includes the Palten and Liesing Fault Systems and shows right-lateral strike-slip movement during Miocene times. Total displacement of 8 km is assumed. (Kurz et al., 2011; Linzer et al., 2002; Metz, 1978)
definition: Dieses in etwa WNW-ESE-streichende ca. 65 km lange Störungssystem verläuft von Liezen, über das Paltental und Liesingtal bis ins Murtal (St. Michael in der Obersteiermark). Sie setzt sich aus der Palten- und Liesing-Störung zusammen und zeigt dextral-seitenverschiebende Kinematik im Miozän. Ein Versatz von 8 km wird angenommen. (Kurz et al., 2011; Linzer et al., 2002; Metz, 1978) @de
preferred label: Palten-Liesing-Störungssystem @de
narrower: Trofaiach Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Trofaiach Fault
references: https://data.geoscience.earth/ncl/geoera/ref/784
notation: AT-10380
type: Concept
created: 2020-04-30T14:27:00.792Z
definition: It is an E-W trending fault along the northern part of the basin of Trofaiach and shows left-lateral movement. The belonging to the Mur-Mürz Fault System is discussed as well as its continuation into this Fault System (Nievoll, 1985).
definition: Es ist eine EW-streichende Störung nördlich des Trofaiach-Becken mit sinistral seitenverschiebender Kinematik. Eine Zugehörigkeit bzw. ein Übergang ins Mur-Mürz-Störungssystem wird diskutiert. (Nievoll, 1985) @de
preferred label: Trofaiach-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Palten-Liesing Fault System

NCA NE-SW Fault Set
references: https://data.geoscience.earth/ncl/geoera/ref/840
references: https://data.geoscience.earth/ncl/geoera/ref/841
notation: AT-529
type: Concept
created: 2020-04-30T14:27:02.004Z
definition: This fault set of NE-SW trending faults within the Northern Calcareous Alps (NCA) includes Annaberg Fault, Isar Fault, Leutasch Fault, Loisach Fault, Pernitz Fault, Pyhrn Fault, Saalach Fault, Salzsteig Fault, and Torscharten Fault amongst other similar orientated faults with same shear sense. These faults were generated during Middle Miocene times as left-lateral strike-slip faults. During Pannonian E-W compression, these NE-SW striking faults were reactivated as right-lateral strike-slip faults. (Peresson & Decker, 1997a, b)
definition: Dieses Störungsset von NE-SW-streichenden Störungen in den Nördlichen Kalkalpen (NKA) beinhaltet die Annaberg-, Isar-, Leutasch-, Loisach-, Pernitz-, Pyhrn-, Saalach-, Salzsteig-, Torscharten- und weitere ähnlich orientierte Störungen mit ähnlicher Kinematik. Diese Störungen entwickelten sich während des mittleren Miozäns als sinistrale Seitenverschiebungen und wurde während des Pannonium als dextrale Seitenverschiebungen reaktiviert. (Peresson & Decker, 1997a, b) @de
preferred label: NKA-Störungsset (NE-SW) @de
narrower: Salzsteig Fault
narrower: Saalach Fault
narrower: Torscharten Fault
narrower: Pernitz Fault
narrower: Pyhrn Fault
narrower: Isar Fault
narrower: Leutasch Fault
narrower: Loisach Fault
narrower: Annaberg Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Annaberg Fault
definition: For the NW-SE trending brittle fault running from 5 km north of Mariazell to Lilienfeld left-lateral strike-slip diplacement was decribed for Oligocene-Miocene times due to 2 km offset of the Hochwart Fault. Late Miocene right-lateral movement during E-W-compression is expected. (Linzer et al., 2002)
definition: Für die NW-SE-streichende spröde Störung von 5 km nördlich von Mariazell bis Lilienfeld ist eine sinistral-seitenverschiebende Kinematik im Oligozän-Miozän, wegen eines Versatzes der Hochwart Störung von 2 km, bekannt. Spät-Miozäne dextrale Bewegung während E-W-Kompression wird angenommen. (Linzer et al., 2002) @de
notation: AT-10009
type: Concept
created: 2020-04-30T14:27:02.257Z
preferred label: Annaberg-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: NCA NE-SW Fault Set

Salzsteig Fault
references: https://data.geoscience.earth/ncl/geoera/ref/726
references: https://data.geoscience.earth/ncl/geoera/ref/725
references: https://data.geoscience.earth/ncl/geoera/ref/823
notation: AT-10307
type: Concept
created: 2020-04-30T14:27:02.032Z
definition: This NE-SW trending fault with left-lateral shear sense runs in the area of the Salzsteig. (Decker, 1994; Linzer et al., 2002; Peresson & Decker, 1996)
definition: Diese NE-SW-streichende Störung mit sinistral seitenverschiebender Kinematik verläuft entlang des Salzsteiges. (Decker, 1994; Linzer et al., 2002; Peresson & Decker, 1996) @de
preferred label: Salzsteig-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: NCA NE-SW Fault Set

Isar Fault
references: https://data.geoscience.earth/ncl/geoera/ref/737
references: https://data.geoscience.earth/ncl/geoera/ref/782
notation: AT-10123
type: Concept
created: 2020-04-30T14:27:02.172Z
definition: This NE-SW trending fault with left-lateral shear sense runs parallel to the Isar valley. (Eisbacher & Brandtner, 1995, 1996)
definition: Diese NE-SW-streichende Störung mit sinistral seitenverschiebender Kinematik verläuft parallel zum Isartales. (Eisbacher & Brandtner, 1995, 1996) @de
preferred label: Isar-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: NCA NE-SW Fault Set

Pyhrn Fault
references: https://data.geoscience.earth/ncl/geoera/ref/726
references: https://data.geoscience.earth/ncl/geoera/ref/725
references: https://data.geoscience.earth/ncl/geoera/ref/823
notation: AT-10255
type: Concept
created: 2020-04-30T14:27:02.144Z
definition: This NE-SW trending fault with left-lateral shear sense runs parallel to the Pyhrnbach Valley. (Decker, 1994; Linzer et al., 2002; Peresson & Decker, 1996)
definition: Diese NE-SW-streichende Störung mit sinistral seitenverschiebender Kinematik verläuft parallel zum Verlauf des Pyhrnbaches. (Decker, 1994; Linzer et al., 2002; Peresson & Decker, 1996) @de
preferred label: Pyhrn-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: NCA NE-SW Fault Set

Loisach Fault
references: https://data.geoscience.earth/ncl/geoera/ref/737
references: https://data.geoscience.earth/ncl/geoera/ref/782
references: https://data.geoscience.earth/ncl/geoera/ref/823
notation: AT-10189
type: Concept
created: 2020-04-30T14:27:02.229Z
definition: This NE-SW trending fault with left-lateral movement runs parallel to the Loisach valley. (Eisbacher & Brandtner, 1995, 1996; Linzer et al., 2002)
definition: Diese NE-SW-streichende Störung mit sinistral seitenverschiebender Kinematik verläuft parallel zum Loisachtal. (Eisbacher & Brandtner, 1995, 1996; Linzer et al., 2002) @de
preferred label: Loisach-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: NCA NE-SW Fault Set

Leutasch Fault
references: https://data.geoscience.earth/ncl/geoera/ref/781
notation: AT-10180
type: Concept
created: 2020-04-30T14:27:02.200Z
definition: This NE-SW trending fault with left-lateral shear sense is located in the area of the village of Leutasch. (Mählmann & Morlok, 1992)
definition: Diese NE-SW-streichende Störung mit sinistral seitenverschiebender Kinematik befindet sich bei Leutasch. (Mählmann & Morlok, 1992) @de
preferred label: Leutasch-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: NCA NE-SW Fault Set

Saalach Fault
references: https://data.geoscience.earth/ncl/geoera/ref/732
notation: AT-10301
type: Concept
created: 2020-04-30T14:27:02.060Z
definition: This NE-SW trending fault has assumedly left-lateral shear sense and runs parallel to the Saalach Valley. (Tollmann, 1986)
definition: Diese NE-SW-streichende Störung verläuft parallel zum Verlauf des Saalachtales. Es wird ein sinistral seitenverschiebender Kinematik angenommen. (Tollmann, 1986) @de
preferred label: Saalach-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: NCA NE-SW Fault Set

Pernitz Fault
references: https://data.geoscience.earth/ncl/geoera/ref/724
references: https://data.geoscience.earth/ncl/geoera/ref/823
notation: AT-10252
type: Concept
created: 2020-04-30T14:27:02.116Z
definition: This NE-SW trending fault with left-lateral shear sense runs close to the village of Pernitz. (Decker, 1996; Linzer et al., 2002)
definition: Diese NE-SW-streichende Störung mit sinistral seitenverschiebender Kinematik verläuft in der Nähe von Pernitz. (Decker, 1996; Linzer et al., 2002) @de
preferred label: Pernitz-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: NCA NE-SW Fault Set

Torscharten Fault
references: https://data.geoscience.earth/ncl/geoera/ref/748
notation: AT-10371
type: Concept
created: 2020-04-30T14:27:02.088Z
definition: This NE-SW trending fault with left-lateral shear sense runs in the area of the Hohe Torscharte. (Frisch & Gawlick, 2003)
definition: Diese NE-SW-streichende Störung mit sinistral seitenverschiebender Kinematik verläuft im Bereich der Hohen Torscharte. (Frisch & Gawlick, 2003) @de
preferred label: Torscharten-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: NCA NE-SW Fault Set

NE Molasse Fault Set
notation: AT-563
narrower: Niederhollabrunn Fault
type: Concept
created: 2020-04-30T14:27:02.930Z
preferred label: Nordöstliches Molasse Störungsset @de
narrower: Mailberg Fault
narrower: Stetteldorf Fault
narrower: Tullnerfeld Fault
narrower: Zwentendorf Fault
definition: This fault set consists of faults within in the Molasse Basin between Melk in the southwest and Laa/Thaya in the northeast. It is bound by the outcropping crystalline rock suites of the Bohemian Massif to the northwest, and the Alpine Thrust front to the south and southeast. All faults within the basin are blind faults, active until Badenian of mid-Miocene at the latest, solely evidenced by seismic surveys and drillings. (Kröll et al., 2001; Wagner, 1998)
definition: Dieses Störungset besteht aus Störungen des Mollassebeckens zwischen Melk im Südwesten and Laa a.d. Thaya im Nordosten. Es wird im Nordosten von Kristallingesteinen der Böhmischen Masse begrenzt und von der Alpinen Überschiebungsfront im Süden und Südosten. Alle Brüche innerhalb des Beckens sind blinde Störungen, die längstens bis ins Baden des Mittleren Miozäns aktiv waren, und die nur mittels Seismik und Bohrungen nachgewiesen wurden. (Kröll et al., 2001; Wagner, 1998) @de
references: https://data.geoscience.earth/ncl/geoera/ref/750
references: https://data.geoscience.earth/ncl/geoera/ref/728
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Stetteldorf Fault
definition: This SE dipping and NE-SW striking normal fault delimitates the Moosbierbaum-Horst towards SE. It runs from the west of Langenrohr via Göllersdorf to the castle Schloss Glaswein. To the south, the fault is cut off from the Tullnerfeld Fault. The main deformation event took place during the Karpatian. (Wessely, 2006)
definition: Diese nach SE einfallende, NE-SW streichende Abschiebung begrenzt den Moosbierbaum-Horst nach NE hin. Sie verläuft von westlich von Langenrohr über Göllersdorf bis Schloss Glaswein. Im Süden wird die Störung von der Tullnerfeld-Störung abgeschnitten. Die Hauptbewegungsphase war im Karpatium. (Wessely, 2006) @de
references: https://data.geoscience.earth/ncl/geoera/ref/849
notation: AT-10425
type: Concept
created: 2020-04-30T14:27:03.015Z
preferred label: Stetteldorf-Störung @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: NE Molasse Fault Set

Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
description: Inventory and concepts of major tectonic boundaries (faults) and overarching fault domains (areally distinct regions with similar fault pattern and properties) in European principal carbonate geothermal reservoirs as identified on mapping and modelling HotLime’s case study areas.
created: 2020-04-29T09:07:57.164Z
type: ConceptScheme
applied type: SpatialObject

Zwentendorf Fault
definition: This NW dipping and NE-SW striking normal fault delimitates the Moosbierbaum-Horst towards NW. It runs from west of Absdorf via Zwentendorf to Moosbierbaum, where it terminates at the Tullnerfeld Fault. The main deformation event took place during the Karpatian. Wessely (2006) describes this fault as Moosbierbaumer-Störung.
definition: Die nach NW einfallende, NE-SW streichende Abschiebung, begrenzt den Moosbierbaum-Horst nach NW hin. Sie verläuft von westlich von Absdorf über Zwentendorf nach Moosbierbaum, wo sie von der Tullnerfeld-Störung abgeschnitten wird. Die Hauptbewegungsphase war im Karpatium. Wessely (2006) beschreibt die Störung als Moosbierbaumer-Störung. @de
type: SpatialObject
notation: AT-10426
type: Concept
created: 2020-04-30T14:27:03.072Z
preferred label: Zwentendorf-Störung @de
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: NE Molasse Fault Set

Tullnerfeld Fault
references: https://data.geoscience.earth/ncl/geoera/ref/849
notation: AT-10427
type: Concept
created: 2020-04-30T14:27:03.043Z
definition: This S-dippping, EW-trending normal fault runs from Tulln through the Tullnerfeld south of the river Danube to Oberbierbaum. Wessely (2006) describes this fault as a Moosbierbaumer Südbruch. (Wessely, 2006).
definition: Diese nach S einfallende, grob E-W streichende Abschiebung schneidet den Moosbierbaum-Horst und die ihn nach NW (Zwentendorf-Störung) bzw. SE (Stetteldorf-Störung) begrenzenden Störungen ab. Sie verläuft von Tulln durch das Tullnerfeld südlich der Donau bis Oberbierbaum. Bei Wessely (2006) wird diese Störung als Moosbierbaumer Südbruch beschrieben. (Wessely, 2006) @de
preferred label: Tullnerfeld-Störung @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: NE Molasse Fault Set

Mailberg Fault
references: https://data.geoscience.earth/ncl/geoera/ref/772
references: https://data.geoscience.earth/ncl/geoera/ref/742
references: https://data.geoscience.earth/ncl/geoera/ref/849
notation: AT-10191
type: Concept
created: 2020-04-30T14:27:02.959Z
definition: This NE-SW striking and SE-dipping fault runs in Austria from Hollabrunn over Mailberg to Laa an der Thaya. North of Laa an der Thaya, the fault runs parallel to the CZ-Austrian border and along the River Thaya. The downward movement of the hanging wall is 700 m at its maximum. (Buchroithner, 1984; Janouschek, 1980; Wessely, 2006)
definition: Die NE-SW streichende, nach SE einfallende Störung verläuft in Österreich von Hollabrunn über Mailberg nach Laa an der Thaya. Nördlich von Laa a. d. Thaya verläuft die Störung parallel zum Grenzverlauf bzw. zum Flussverlauf der Thaya. Das Hangende ist um max. 700 m abgeschoben worden. (Buchroithner, 1984; Janouschek, 1980; Wessely, 2006) @de
preferred label: Mailberg-Störung @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: NE Molasse Fault Set

Niederhollabrunn Fault
type: SpatialObject
definition: This NE-SW striking normal fault in Lower Austria runs from Stockerau via Niederhollabrunn to Naglern. The fault is located in the subsurface at about 3000 m below groundlevel, steeply dipping towards SE. There is no topographical expression of this fault at the surface (Rötzel et al., 2009)
definition: Diese NE-SW-streichende Abschiebung in Niederösterreich verläuft von Stockerau via Niederhollabrunn bis Naglern. Die steil nach SE einfallende Störung befindet sich ca. 3000 m unter der Erdoberfläche und zeigt keine geomorphologische Kante an der Oberfläche (Rötzel et al., 2009) @de
references: https://data.geoscience.earth/ncl/geoera/ref/4126
created: 2020-09-09T13:27:07.302Z
type: Concept
preferred label: Niederhollabrunn-Störung @de
notation: AT-10653
alternative label: Niederhollabrunn Störung @de
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: NE Molasse Fault Set

Styrian Fault Set
definition: The fault set comprises mostly N-S striking faults within the Styrian Basin that have no surface expression. They are observed at depth via industrial seismic and borehole data.
definition: Das Störungsset beinhaltet hauptsächlich N-S-streichende Störungen innerhalb des Steirischen Beckens, die keine oberflächliche Morphologie ausbilden. Diese Störungen wurden anhand von Industrieseismik- und Bohrlochdaten im tieferen Untergrund nachgewiesen. @de
created: 2020-04-30T14:27:03.100Z
preferred label: Steirisches Becken Störungsset @de
narrower: Leber Fault
narrower: Weiz Fault
notation: AT-550
type: Concept
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Leber Fault
definition: The NNW-SSE striking light-lateral strike-slip fault runs from east of Frohnleiten via Graz to Spielfeld (Tollmann, 1977; Untersweg, 1982, Flügel, 1988, Kröll et al., 1988).
definition: Die NNW-SSE-streichende dextrale Seitenverschiebung mit teiweiser top nach Osten abschiebender Kinematik verläuft östlich von Frohnleiten über Graz nach Spielfeld und ist deutlich im Bereich zwischen Semriach und Stattegger Graben ausgeprägt (Tollmann, 1977; Untersweg, 1982; Flügel, 1988; Kröll et al., 1988). @de
references: https://data.geoscience.earth/ncl/geoera/ref/8695
references: https://data.geoscience.earth/ncl/geoera/ref/8696
references: https://data.geoscience.earth/ncl/geoera/ref/8697
references: https://data.geoscience.earth/ncl/geoera/ref/8698
type: Concept
created: 2020-04-30T14:27:03.128Z
preferred label: Leber-Störung @de
notation: AT-10436
in scheme: Tectonic Boundary Objects in Europe
broader: Styrian Fault Set

Weiz Fault
definition: The E-W striking fault runs from Garrach-Dorf via Weiz to Stubenberg and is part of the Styrian Basin. (Flügel, 1988)
definition: Die E-W-streichende Störung verläuft von Garrach-Dorf über Weiz bis Stubenberg. (Flügel, 1988) @de
references: https://data.geoscience.earth/ncl/geoera/ref/8695
type: Concept
created: 2020-04-30T14:27:03.157Z
preferred label: Weiz-Störung @de
notation: AT-10440
in scheme: Tectonic Boundary Objects in Europe
broader: Styrian Fault Set

Iller Valley Fault
limit type: strikeSlipFault
type: Limit
type: Fault
references: https://data.geoscience.earth/ncl/geoera/ref/774
alternative label: Illertal-Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/768
alternative label: Iller-Störung @de
notation: AT-10433
alternative label: Iller Fault
definition: N-S trending sinistral strike-slip fault with an oblique normal fault component subparallel to the Iller river valley. Displaces the Alpine Basal Thrust [DE-BY_753] and the Northern Boundary of Subalpine Molasse [DE-BY_789] (Lagally et al. 2009, p 22).
references: https://data.geoscience.earth/ncl/geoera/ref/6363
references: https://data.geoscience.earth/ncl/geoera/ref/6366
references: https://data.geoscience.earth/ncl/geoera/ref/6367
sf touches: Northern Boundary of Subalpine Molasse
definition: Diese N-S verlaufende sinistrale Blattverschiebung mit abschiebender Komponente verläuft von Immenstadt (Bayern, D) subparallel zum N-S orientierten Streichen des Illertales bis zur deutsch-österreichischen Grenze. Dabei versetzt sie den Nordrand der Faltenmolasse [DE-BY_789]. (Pfiffner, 2011, Zerlauth, 2014) @de
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:38.400Z
notation: DE-BY_788
preferred label: Iller Störung @de
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
notation: LfU-BY_788
broader: Foreland Molasse Southern Margin Faults
broader: Tectonic Boundary in Austria

Danube Fault System
type: Fault
type: Limit
type: Concept
type: SpatialObject
notation: AT-109
definition: Südwestliche Begrenzung des variszischen Grundgebirges der Böhmischen Masse zum Niederbayerischen Molassebecken. Großräumig NW-SE streichendes, ca. 70° nach SW einfallendes bis saigeres polyphases Störungssystem subparallel zum Verlauf der Donau zwischen Regensburg und Deggendorf, von wo es sich in Teilästen bis nach Österreich hinzieht. Die duktile Hauptbewegungsphase mit vorwiegend dextraler Bewegungsrichtung im Spätvariszikum und dessen miozäne Reaktivierung bildeten ein komplexes Störungssystem mit ausgedehnten Tektonit-Zonen, Bruchstufen und Staffelbrüchen mit Versätzen von bis zu über 1 km. durch ± senkrecht dazu streichende Bayerwald Meridional Störungen [DE-BY_1350] und deren die Stallwanger Furche begrenzende Pendants. @de
references: https://data.geoscience.earth/ncl/geoera/ref/755
narrower: Danube Fault
definition: Southwestern boundary of the exposed Variscan basement rock suites of the Bohemian Massif towards Lower Bavaria Molasse Basin. Overall NW-SE trending, approx. 70° SW to vertically dipping polyphase large-scale fault system running subparallel to the Danube river from Regensburg to Deggendorf, continuing in various branches further to Austrian territory. The Late Variscan ductile main displacement phase, a principally dextral movement, and the Miocene brittle reactivation resulted in a complex fault system of extensive tectonite zones, fault scarps and step faults with an overall throw up to more than 1 km.
narrower: Danube Shear Zone
alternative label: Donau-Störungssystem @de
references: https://data.geoscience.earth/ncl/geoera/ref/6358
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/4151
references: https://data.geoscience.earth/ncl/geoera/ref/4082
references: https://data.geoscience.earth/ncl/geoera/ref/731
sf touches: Keilberg Fault
sf touches: Schwarzwald-Bayerwald Line
narrower: Haselbach-Patriching Fault
narrower: Ratzing-Kachlet Fault
scope note: Im Donaustörungssystem mit einem Vertikalversatz von bis zu mehr als 1 km, treffen die tiefen, überdeckten Störungen des niederbayerisch-oberösterreichischen Molassebeckens und die gering überdeckten, selten exponierten Störungen der Böhmischen Masse aufeinander. Die Beschreibungen der tiefliegenden Störungen im Molassebecken beziehen sich auf die im 3D-Modell ermittelten Schnittspuren an der Weißjura-Oberfläche bzw. deren Randfazies-Äquivalenten, abgeleitet aus seismischen und Schwere-Messungen sowie vereinzelten Bohrungsbelegen; subseismische Merkmale konnten dabei naturgemäß nicht berücksichtigt werden. Die Beschreibungen der abgeleiteten (gering überdeckten) und kartierten (aufgeschlossenen) Störungen im Kristallin der Böhmischen Masse entsprechen dem im Maßstab von etwa 1:100.000 generalisierten Störungsverlauf an der Geländeoberfläche, wobei flächige Störungszonen aus Tektoniten in den HotLime-Darstellungen als Mittellinie zusammengefasst sind. @de
created: 2020-10-09T11:35:35.168Z
scope note: The Danube Fault System, featuring a throw of up to more than 1 km, represents the borderline where the blind faults of the Lower Bavaria - Upper Austria Molasse Basin and exposed resp. subcropping faults of the Bohemian Massif converge. The basinal faults, as 3D modelled based on evidence in seismic and gravity surveys and scarce deep drillings, are described as traced on the top of Upper Jurassic strata or its marginal facies equivalents. Conditioned by methodology, subseismic features are neglected. The inferred subcropping and mapped rarely outcropping tectonic boundaries of the Bohemian Massif crystalline rock suites are described generalized equivalent to an approximately 1:100,000 scale, in HotLime spatial representations consolidated to the centerlines of wide fault zones made up of mylonites and cataclastites.
notation: DE-BY_697
preferred label: Donaustörungssystem @de
narrower: Donaurand Fault Scarp
narrower: Aicha-Halser Nebenpfahl
narrower: Donauleiten Fault
narrower: Paleo-Donaurand Fault Scarp
narrower: Wolfach Fault
narrower: Kalkberg Fault
narrower: Niederachdorf-Platting Fault
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11686
notation: LfU-BY_697
limit type: normalFault
broader: Tectonic Boundary in Austria
broader: Lower Bavaria - Upper Austria Molasse Basin Eastern Margin Fault Systems

Danube Shear Zone
type: Limit
type: Fault
definition: This NW-SE trending shear zone is the older and ductile part of the Donau fault system with predominantly right-lateral strike-slip movement. (Daurer, 1975; Platzer, 1992; Büttner, 2007; Scheck-Wenderoth et al., 2008).
definition: Diese NW-SE-streichende Scherzone beinhaltet den duktilen Teil des Donau-Störungssystems mit hauptsächlich dextral-seitenverschiebender Bewegungsrichtung. (Daurer, 1975; Platzer, 1992; Büttner, 2007; Scheck-Wenderoth et al., 2008) @de
notation: AT-1010
type: Concept
created: 2020-04-30T14:27:01.471Z
preferred label: Donau-Scherzone @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Danube Fault System

Ratzing-Kachlet Fault
type: Limit
type: Fault
references: https://data.geoscience.earth/ncl/geoera/ref/6358
created: 2021-01-25T14:58:14.735Z
type: Concept
type: SpatialObject
preferred label: Ratzing-Kachlet Störung @de
notation: DE-BY_1488
definition: Inferred southeastern continuation of Paleo-Donaurand Fault Scarp [DE-BY_1237] following the Danube river valley gash.
definition: Dem Donautal-Einschnitt folgende, vermutete südöstliche Fortsetzung des Paläo-Donaurandbruchs [DE-BY_1237]. @de
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
notation: LfU-BY_1489
broader: Danube Fault System

Danube Fault
type: Fault
type: Limit
definition: This NW-SE trending fault is the mostly brittle part of the Donau fault system with predominantly right-lateral strike-slip movement. (Daurer, 1975; Platzer, 1992; Büttner, 2007; Scheck-Wenderoth et al., 2008).
definition: Diese NW-SE-streichende Störung beinhaltet den spröden Teil des Donau-Störungssystems mit hauptsächlich dextral-seitenverschiebender Bewegungsrichtung. (Daurer, 1975; Platzer, 1992; Büttner, 2007; Scheck-Wenderoth et al., 2008) @de
references: https://data.geoscience.earth/ncl/geoera/ref/755
references: https://data.geoscience.earth/ncl/geoera/ref/723
references: https://data.geoscience.earth/ncl/geoera/ref/821
references: https://data.geoscience.earth/ncl/geoera/ref/842
notation: AT-10038
type: SpatialObject
type: Concept
created: 2020-04-30T14:27:01.444Z
preferred label: Donau-Störung @de
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Danube Fault System

Haselbach-Patriching Fault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6358
type: Concept
created: 2021-01-25T14:55:05.669Z
type: SpatialObject
preferred label: Haselbach-Patriching Störung @de
notation: DE-BY_1491
definition: Slightly NE-ward arcuate NNW-SSE trending, vertical to subvertical fault truncating the mylonite zones of Aicha-Halser Nebenpfahl [DE-BY_762] in the east.
definition: Leicht NE-wärts gebogen NNW-SSE verlaufende, saigere to subvertikale Störung, die die Mylonitzonen des Aicha-Halser Nebenpfahls [DE-BY_762]im Osten begrenzen. @de
references: https://data.geoscience.earth/ncl/geoera/ref/7320
sf touches: Aicha-Halser Nebenpfahl
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
notation: LfU-BY_1491
broader: Danube Fault System

Paleo-Donaurand Fault Scarp
limit type: obliqueSlipFault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4082
type: Concept
created: 2020-10-09T11:35:35.283Z
notation: DE-BY_1237
preferred label: Paläo-Donaurandbruch @de
definition: Running from Winzer to Gerading, southwestern intra-basement branch of Donau Fault System southwest of Deggendorf. NW-SE trending ± vertical, moderate throw polyphase fault featuring vein quartz, mylonites and cataclastites. Cutting across a downthrow block of Jurassic carbonates in its northwestern part close to Danube river.
definition: Von Winzer bis Gerading ziehender Südwest-Ast des Donaustörungssystems im Grundgebirge der Böhmischen Masse. NW-SE verlaufende, steilstehende mehrphasige Störung aus Gangquarz, Myloniten und Kataklastiten. Querstörungen im nordwestlichen, Donau-nahen Abschnitt begrenzen eine abgesenkte Scholle jurassischer Karbonate. @de
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
notation: LfU-BY_1237
broader: Danube Fault System

Donauleiten Fault
limit type: https://data.geoscience.earth/ncl/geoera/geoconnect3d/category/57
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/7269
definition: NW-SE to WNW-ESE trending continuation of the Aicha-Halser Nebenpfahl along the Danube river valley downriver of Passau featuring brittle faulting segments as well as mylonite zones. Evolved from two phases of mainly dextral movement direction, a Late Varican ductile main phase and a Miocene brittle reactivation (Brandmayr et al. 1997).
references: https://data.geoscience.earth/ncl/geoera/ref/4079
sf touches: Aicha-Halser Nebenpfahl
narrower: Donauleiten Subsidiary Faults
type: Concept
created: 2020-10-09T11:35:35.251Z
notation: DE-BY_934
preferred label: Donauleiten Störung @de
definition: NW-SE bis WNW-ESE verlaufende Fortsetzung des Aicha-Halser-Nebenpfahles entlang des Donautals unterhalb von Passau mit bruchtektonischen Segmenten sowie Mylonitzonen. Entstanden in zwei Phasen mit vorwiegend dextraler Bewegungsrichtung, einer spätvariszischen duktilen Hauptbewegungsphase und einer miozänen spröden Reaktivierung (Brandmayr et al. 1997). @de
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
notation: LfU-BY_934
broader: Danube Fault System

Donauleiten Subsidiary Faults
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6358
references: https://data.geoscience.earth/ncl/geoera/ref/7255
created: 2021-01-25T14:56:47.797Z
type: Concept
type: SpatialObject
preferred label: Donauleiten Nebenstörungen @de
notation: DE-BY_1540
definition: WNW-ESE trending vertical to subvertical strike slip faults parallel to and kinematically related with Donauleiten Fault.
definition: WNW-ESE verlaufende, saigere bis subvertikale Blattverschiebungen parallel zu und kinematisch verbunden mit der Donauleiten Störung. @de
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
notation: LfU-BY_1540
broader: Donauleiten Fault

Aicha-Halser Nebenpfahl
limit type: https://data.geoscience.earth/ncl/geoera/geoconnect3d/category/57
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/4149
references: https://data.geoscience.earth/ncl/geoera/ref/4082
sf touches: Donauleiten Fault
type: Concept
created: 2020-10-09T11:35:35.223Z
notation: DE-BY_762
alternative label: Halser Pfahl @de
definition: Running from Winzer southwest of Deggendorf to Passau northeastern intra-basement branch of Donau Fault System. Predominantly NW-SE trending vertical to steeply SW dipping, moderate throw polyphase fault mainly manifested in extensive zones of mylonites and cataclastites and quartz veins.
definition: Von Winzer bis Passau ziehender Nordost-Ast des Donaustörungssystems im Grundgebirge der Böhmischen Masse. NW-SE verlaufende, steilstehende bis steil SW fallende, polyphase Störung, die in Form ausgedehnter Mylonit- und Kataklastit-Zonen sowie als Gangquarz in Erscheinung tritt. @de
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11686
notation: LfU-BY_762
broader: Danube Fault System

Donaurand Fault Scarp
type: Fault
type: Limit
definition: Main scarp of the Danube Fault System. W-E to NW-SE trending, approx. 70° S to SW dipping fault scarp, in parts step fault, with polyphase kinematics (Late Varican ductile main phase, manifested in tectonite zones of various scale, and Miocene brittle reactivation) establishing the distinctive NE border of the Molasse Basin towards the crystalline rock suites of the Bohemian Massif in an up to more than 1 km throw. Rarely disclosed as mostly covered by Tertiary and Quaternary sediments. In sections, the Danube Fault Scarp is intensely compartmentalised by ± perpendicularly striking Bayerwald Meridional Faults [DE-BY_1350] and the resembling boundary faults of Stallwang Trench (Stallwanger Furche) resulting from late to post-Variscan brittle deformation, reactivated during Late Cretaceous and Paleogene.
narrower: Münster Graben Fault
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4128
references: https://data.geoscience.earth/ncl/geoera/ref/4151
references: https://data.geoscience.earth/ncl/geoera/ref/4082
sf touches: Keilberg Fault
sf touches: Deuerling Fault
narrower: Keilberg-Burgberg Faults
narrower: Steinach-Deggendorf Fault
narrower: Münster Fault
narrower: Natternberg Faults
narrower: Hengersberger Bucht Faults
type: Concept
created: 2020-10-09T11:35:35.195Z
notation: DE-BY_698
hidden label: Großer Donau Abbruch @de
alternative label: Bayerwald Abbruch @de
preferred label: Donaurandbruch @de
definition: Hauptabbruch des Donaustörungssystems. W-E bis NW-SE verlaufende, ca. 70° nach S bis SW einfallende Bruchstufe, bzw. Staffelbruch, geprägt durch eine mehrphasige Kinematik (spätvariszische duktile Hauptbewegungsphase, unter Bildung von Tektoniten unterschiedlicher Erstreckung, und miozäne spröde Reaktivierung). Mit Sprunghöhen bis zu über 1 km bildet der Donaurandbruch die markante NE Begrenzung des Molassebeckens zu den Kristallingesteinen der Böhmischen Masse. Meist von tertiären und quartären Sedimenten überdeckt, nur in wenigen kurzen Abschnitten aufgeschlossen. Der Donaurandbruch wird durch ± senkrecht dazu streichende Bayerwald Meridional Störungen [DE-BY_1350] und deren die Stallwanger Furche begrenzende Pendants bereichsweise stark zergliedert. Diese Querstörungen sind das Ergebnis einer spät- bis postvariszischen bruchhaft-spröden Deformation und deren Reaktivierung während der Unterkreide und im Alttertiär. @de
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11682
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11684
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11690
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11855
notation: LfU-BY_698
limit type: normalFault
broader: Danube Fault System

Hengersberger Bucht Faults
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6358
created: 2021-01-25T14:53:52.853Z
type: Concept
type: SpatialObject
preferred label: Hengersberger Bucht Störungen @de
notation: DE-BY_1487
definition: Blind faults of the Varican basement burried under Tertiary unconsolidated deposits of Hengersberger Bucht (embayment), inferred from on strike elongation of subcropping faults and basin margins. Roughly paralleling the Donaurand Fault Scarp [DE-BY_698] resp. the northern tail of Deggendorf-Ried Faultsystem [DE-BY_929] and offset by ± W-E trending lateral faults.
definition: Überdeckte Störungen des variszischen Grundgebirges unter den tertiären Lockergesteins- Ablagerungen der Hengersberger Bucht, abgeleitet aus der Verlängerung "aufgeschlossener" Störungen und vermuteter Störungen an den Beckenrändern. In etwa parallel zum Donaurandbruch [DE-BY_698] bzw. dem Nordende des Deggendorf-Ried Störungssystems [DE-BY_929] und von ± W-E verlaufenden Querstörungen versetzt. @de
references: https://data.geoscience.earth/ncl/geoera/ref/7676
references: https://data.geoscience.earth/ncl/geoera/ref/4107
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
notation: LfU-BY_1487
broader: Donaurand Fault Scarp

Natternberg Faults
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6358
created: 2021-01-25T14:52:41.750Z
type: Concept
type: SpatialObject
preferred label: Natternberg Störungen @de
notation: DE-BY_1488
definition: Pair of parallel NW-SE trending inversely arranged subvertical subsidiary faults of Donaurand Fault Scarp, truncated by ± perpendicularly striking Bayerwald Meridional Faults [DE-BY_1350], exposing tectonites of the pediment in an uplifted rhomb horst or push-up, aka positive flower structure. Such structures in between upward convex splay faults imply a reverse vertical component of the strike-slip movement.
definition: Paar NW-SE verlaufender, durch ± senkrecht dazu streichende Bayerwald Meridional Störungen [DE-BY_1350] begrenzter, gegensinnig subvertikaler Nebenstörungen des Donaurandbruchs, zwischen denen die Tektonite der Gebirgsfußfläche in einem aufgepressten rhombenförmigen Horst („positive Blumenstruktur“) zu Tage treten. Solche Strukturen zwischen nach oben konvexen Nebenbrüchen implizieren eine aufschiebende Komponente der Blattverschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/7326
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
notation: LfU-BY_1488
broader: Donaurand Fault Scarp

Münster Fault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6358
references: https://data.geoscience.earth/ncl/geoera/ref/7257
type: Concept
created: 2021-01-25T14:51:39.587Z
type: SpatialObject
preferred label: Münster Störung @de
notation: DE-BY_1485
definition: WNW-ESE striking, vertical to steeply SSW dipping normal fault of a Donaurand Scarp [DE-BY_698] step fault segment. Northern boundary of a hanging wall block exposing Mesozoic deposits. In the east offset truncated by Ascha-Furth Fault [DE-BY_1537].
definition: WNW-ESE streichende, vertikal bis steil nach SSW einfallende Abschiebung eines Staffelbruch-Segments des Donaurandbruchs [DE-BY_698]. Nördliche Begrenzung einer abgesenkten Scholle mit mesozoischen Ablagerungen. Im Osten von der Ascha-Furth Störung [DE-BY_1537] abgeschnitten. @de
references: https://data.geoscience.earth/ncl/geoera/ref/7352
sf touches: Bayerwald Meridional Faults
sf touches: Ascha-Furth Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7255
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
notation: LfU-BY_1485
limit type: normalFault
broader: Donaurand Fault Scarp

Münster Graben Fault
type: Fault
type: Limit
definition: WNW-ESE striking, vertical to steeply NNE dipping blind normal fault featuring a throw of about 100 m, southward parallel to the Donaurand Fault Scarp [DE-BY_698] and northward subparallel to Straubing Fault [DE-BY_924], in the west truncated by a Bayerwald Meridional Fault [DE-BY_1350], in the east by Ascha-Furth Fault [DE-BY_1537]. Southern boundary of Münster Graben, formed by the hanging wall in between Münster Graben Fault and Donaurand Fault Scarp, and northern boundary of Parkstetten Step, the footwall of Münster Graben Fault and hanging wall of Straubing Fault [DE-BY_1535].
definition: WNW-ESE streichende, vertikal bis steil nach NNE einfallende überdeckte Abschiebung mit einer Sprunghöhe von ca. 100 m, südlich parallel zum Donaurandbruch [DE-BY_698] und nördlich subparallel zur Straubing Störung [DE-BY_924], im Westen von einer Bayerwald Meridional Störung [DE-BY_1350], im Osten von der Ascha-Furth Störung [DE-BY_1537] abgeschnitten. Südgrenze des Münster Grabens, der von der Liegendscholle zwischen Münster Störung und Donaurandbruch gebildet wird, und Nordgrenze der Parkstetten Stufe, der Hangendscholle der Münster Graben Störung und Liegendscholle der Straubing Störung [DE-BY_1535]. @de
type: Concept
created: 2021-01-21T08:38:14.901Z
type: SpatialObject
preferred label: Münster Graben Störung @de
notation: DE-BY_1539
references: https://data.geoscience.earth/ncl/geoera/ref/6358
references: https://data.geoscience.earth/ncl/geoera/ref/7257
references: https://data.geoscience.earth/ncl/geoera/ref/7255
references: https://data.geoscience.earth/ncl/geoera/ref/7352
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
notation: LfU-BY_1539
limit type: normalFault
broader: Donaurand Fault Scarp

Steinach-Deggendorf Fault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6358
type: Concept
created: 2021-01-25T14:50:22.645Z
type: SpatialObject
preferred label: Steinach-Deggendorf Störung @de
notation: DE-BY_1538
definition: Northward parallel to the main scarp, WNW-ESE trending, steeply SSW dipping subsidiary fault of Donaurand Fault Scarp [DE-BY_698] as the northern boundary of tectonite occurrances.Multiple dextral displacements by Bayerwald Meridional Faults [DE-BY_1350], Ascha-Furth Fault [DE-BY_1537] and Mitterfels-Bogen Fault [DE-BY_1486].
definition: Nördlich parallel zum Hauptabbruch, WNW-ESE verlaufende, steil nach SSW einfallende Nebenstörung des Donaurandbruchs [DE-BY_698] als nördliche Grenze vom Tektonit Vorkommen. Mehrfach von Bayerwald Meridional Störungen [DE-BY_1350] und den Ascha-Furth [DE-BY_1537] und Mitterfels-Bogen [DE-BY_1486] Störungen dextral versetzt. @de
references: https://data.geoscience.earth/ncl/geoera/ref/7326
references: https://data.geoscience.earth/ncl/geoera/ref/7352
references: https://data.geoscience.earth/ncl/geoera/ref/7257
references: https://data.geoscience.earth/ncl/geoera/ref/7255
sf touches: Bayerwald Meridional Faults
sf touches: Teisnach-Deggendorf Fault
sf touches: Hunderdorf Fault
sf touches: Ascha-Furth Fault
sf touches: Mitterfels-Bogen Fault
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
notation: LfU-BY_1538
limit type: normalFault
broader: Donaurand Fault Scarp

Keilberg-Burgberg Faults
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6358
type: Concept
created: 2021-01-25T14:49:05.765Z
type: SpatialObject
preferred label: Keilberg-Burgberg Störungen @de
notation: DE-BY_1483
definition: W-E trending subsidiary faults of Donaurand Fault Scarp confining blocks of brecciated Rotliegend deposits in a graben-like structure or on top of an intermediate hanging wall block of a step fault segment of Donaurand Fault Scarp, truncated by Keilberg Fault [DE-BY_761] in the west and Kittenrain Faults [DE-BY_1482] in the east.
definition: W-E verlaufende Nebenstörungen des Donaurandbruchs als Begrenzungen von Schollen brekziierter Rotliegend-Ablagerungen, in Form grabenartiger Vertiefungen oder auf höheren Treppenstufen eines Staffelbruch-Abschnitts des Donaurandbruchs; im Westen von der Keilberg Störung [DE-BY_761], im Osten von den Kittenrain Störungen [DE-BY_1482] begrenzt. @de
references: https://data.geoscience.earth/ncl/geoera/ref/7300
references: https://data.geoscience.earth/ncl/geoera/ref/7320
sf touches: Kittenrain Faults
sf touches: Keilberg Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4073
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
notation: LfU-BY_1483
broader: Donaurand Fault Scarp

Niederachdorf-Platting Fault
type: Fault
type: Limit
definition: NW-SE striking, approx. 70° NE dipping train of blind normal faults. Antithetic, probably conjugate fault system to the Donaurand Fault Scarp [DE-BY_698]. Part of northeastern fringe of Regensburg-Straubing Trough.
definition: NW-SE streichender Störungszug ca. 70° nach NE einfallender Abschiebungen. Antithetisches, wahrscheinlich konjugiertes Störungssystem zum Donaurandbruch [DE-BY_698]. Teil des Nordost-Rands der Regensburg Straubinger Senke. @de
references: https://data.geoscience.earth/ncl/geoera/ref/7255
references: https://data.geoscience.earth/ncl/geoera/ref/7257
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4151
references: https://data.geoscience.earth/ncl/geoera/ref/4082
type: Concept
created: 2020-10-09T11:35:35.451Z
notation: DE-BY_765
hidden label: Sünching-Plattling Störung @de
preferred label: Niederachdorf-Plattling Störung @de
narrower: Straubing Fault
narrower: Plattling Fault
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11684
notation: LfU-BY_765
limit type: normalFault
broader: Danube Fault System

Plattling Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4082
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:35.507Z
notation: DE-BY_925
preferred label: Plattling Störung @de
definition: NW-SE striking, approx. 70° NE dipping blind antithetic normal fault.
definition: NW-SE streichende, ca. 70° nach NE einfallende antithetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
notation: LfU-BY_925
limit type: normalFault
broader: Niederachdorf-Platting Fault

Straubing Fault
type: Fault
type: Limit
definition: NW-SE striking, approx. 70° NE dipping blind antithetic normal fault with a throw of about 80 m. In its southeastern segment southwestern boundary of Parkstetten Step, the hanging wall of Münster Graben Fault [LfU-BY_1539] and footwall of Straubing Fault.
definition: NW-SE streichende, ca. 70° nach NE einfallende antithetische Abschiebung mit einem Verwurf von ca. 80 m. In ihrem südöstlichen Abschnitt Südwestgrenze der Parkstetten Stufe, der Hangendscholle der Münster Graben Störung [LfU-BY_1539] und Liegendscholle der Straubing Störung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/7255
references: https://data.geoscience.earth/ncl/geoera/ref/8578
references: https://data.geoscience.earth/ncl/geoera/ref/7257
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4082
type: Concept
created: 2020-10-09T11:35:35.479Z
notation: DE-BY_924
preferred label: Straubing Störung @de
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
notation: LfU-BY_924
limit type: normalFault
broader: Niederachdorf-Platting Fault

Kalkberg Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4082
references: https://data.geoscience.earth/ncl/geoera/ref/4150
references: https://data.geoscience.earth/ncl/geoera/ref/789
sf touches: Wolfach Fault
type: Concept
created: 2020-10-09T11:35:35.423Z
notation: DE-BY_760
alternative label: Kalkberger Aufschiebung @de
alternative label: Kalkberger Bruch @de
preferred label: Kalkberg Störung @de
definition: NW-SE trending, approx. 80° SW dipping reverse fault running from Vilshofen to Neuburger Wald. Regime and kinematics is proved by observation / measuremet in few outcrops. Northeastern limit of Ortenburg Depression featuring a throw of up to 400 m.
definition: NW-SE verlaufende, ca. 80° nach SW einfallende Störung mit aufschiebendem Bewegungssinn zwischen Vilshofen und Neuburger Wald. Verlauf und Kinematik ist durch Beobachtungen in einigen Aufschüssen gesichert. Nordöstliche Begrenzung des Ortenburger Senkungsfelds mit einer Sprunghöhe bis zu 400 m. @de
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11685
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11889
notation: LfU-BY_760
limit type: reverseFault
broader: Danube Fault System

Wolfach Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4082
references: https://data.geoscience.earth/ncl/geoera/ref/4150
references: https://data.geoscience.earth/ncl/geoera/ref/789
sf touches: Kalkberg Fault
type: Concept
created: 2020-10-09T11:35:35.395Z
notation: DE-BY_751
preferred label: Wolfach Störung @de
definition: NNW-SSE striking, approx. 80° NNE dipping normal fault running from Vilshofen to Dorfbach. Western limit of Ortenburg Depression featuring a throw up to 170 m.
definition: NNW-SSE streichende, ca. 80° nach NNE einfallende Abschiebung zwischen Vilshofen und Dorfbach. Westliche Begrenzung des Ortenburger Senkungsfelds mit einer Sprunghöhe bis zu 170 m. @de
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11685
notation: LfU-BY_751
limit type: normalFault
broader: Danube Fault System

Königsee-Lammertal-Traunsee Subfault System
definition: The 110 km long sub fault system branches off from the Salzach fault north of the Tauern window near Zell and strikes with 70° in the south and 30° in the north (Decker et al., 1994). The main deformation of sinistral transpressive character leads to a vertical displacement of 700-2000 m. It offsets the southern margin of the Northern Calcareous Alps by 10-15 km (Linzer et al., 2002).
definition: Das 110 km lange Teilstörungssystem, das nördlich des Tauernfensters bei Zell aus der Salzach-Störung abzweigt, streicht mit 70° im Süden bzw. 30° im Norden (Decker et al., 1994). Die Hauptbewegungsphase hat sinistral transpressiven Charakter und führt zu 700-2000 m vertikalem Versatz. Sie versetzt den Kalkalpensüdrand um 10-15 km (Linzer et al., 2002). @de
references: https://data.geoscience.earth/ncl/geoera/ref/726
references: https://data.geoscience.earth/ncl/geoera/ref/823
notation: AT-524
type: Concept
created: 2020-04-30T14:27:02.706Z
preferred label: Königsee-Lammertal-Traunsee-Teilstörungssystem @de
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Rust Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/736
references: https://data.geoscience.earth/ncl/geoera/ref/776
notation: AT-150
type: Concept
created: 2020-04-30T14:27:00.593Z
definition: This fault system consists of several N-S striking faults towards E and W, which runs from Schützen am Gebirge over St. Margarethen and Rust to the Austro-Hungarian border and supposable to Sopron. These presumably post-Miocene faults limit the so-called Ruster Höhenzug and were possibly originally developed as lateral dislocation. (Kröll et al., 1993; Häusler et al., 2010)
definition: Dieses Störungssystem besteht aus mehreren N-S streichenden, nach E und W einfallenden Abschiebungen, die sich von Schützen am Gebirge über St. Margarethen und Rust bis zur österreichisch-ungarischen Grenze und vermutlich bis Sopron hinziehen. Diese vermutlich postmiozänen Abschiebungen begrenzen den sogenannten Ruster Höhenzug und wurden möglicherweise ursprünglich als Seitenverschiebungen angelegt. (Kröll et al., 1993; Häusler et al., 2010) @de
preferred label: Rust-Störungssystem @de
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Telfs Subfault System
references: https://data.geoscience.earth/ncl/geoera/ref/737
references: https://data.geoscience.earth/ncl/geoera/ref/782
notation: AT-554
type: Concept
created: 2020-04-30T14:27:02.734Z
definition: This ca. 35 km long, approximately WNW-ESE trending Subfault System extends from Fernpass to Imst and Zirl, including the Telfs shear zone and Telfs fault. A Cretaceous system is described with an offset between 10-20 km which were caused during the displacement of the Inntal nappe and the dextral lateral kinematics during Miocene. (Eisbacher, 1995, 1996)
definition: Dieses WNW-ESE-streichende, ca. 35 km lange Teilstörungssystem verläuft vom Fernpass über Imst bis Zirl und beinhaltet die Telfs-Scherzone und Telfs-Störung. Es wird eine kreidezeitliche Anlage beschrieben mit Versatzweiten zwischen 10-20 km die während der Überschiebung der Inntal-Decke und durch Miozäne dextral seitenverschiebende Kinematik zustande gekommen sind. (Eisbacher, 1995, 1996) @de
preferred label: Telfs-Teilstörungssystem @de
narrower: Telfs Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Telfs Fault
definition: The WNW-ESE striking dextral strike-slip fault runs from the Fern Pass south of Biberwier via Telfs to Kematen/Tirol (Eisbacher and Brandner, 1995, 1996).
definition: Die WNW-ESE-streichende dextrale Seitenverschiebung verläuft vom Fernpass südlich von Biberwier über Telfs nach Kematen in Tirol (Eisbacher and Brandner, 1995, 1996). @de
preferred label: Telfs-Störung @de
notation: AT-10362
type: Concept
created: 2020-04-30T14:27:02.762Z
in scheme: Tectonic Boundary Objects in Europe
broader: Telfs Subfault System

Vitis-Pribyslav Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/731
references: https://data.geoscience.earth/ncl/geoera/ref/755
references: https://data.geoscience.earth/ncl/geoera/ref/738
notation: AT-144
type: Concept
created: 2020-04-30T14:27:00.424Z
definition: This NNE-SSW striking, steeply WNW dipping fault system runs from Perg via Zwettl and Vitis to Slavonice (CZ), where it continues in the Czech Republic. The ductile main movement phase, similar to the Rodl fault system, is applied to the Late Variscan, with mainly sinistral direction of motion. It is assumed, that a brittle Miocene reactivation holds the same motion kinematic. (Brandmayr, 1997, Büttner, 2007, Lehnhard, 2007)
definition: Dieses NNE-SSW streichende, steil nach WNW einfallende Störungssystem zieht sich von Perg über Zwettl und Vitis bis Slavonice (CZ), wo es sich in der Tschechischen Republik weiter fortsetzt. Die duktile Hauptbewegungsphase wird, analog zum Rodl-Störungssystem, auf das Spätvariszikum gelegt, mit hauptsächlich sinistraler Bewegungsrichtung. Von einer spröden miozänen Reaktivierung mit selber Bewegungskinematik wird ebenfalls ausgegangen. (Brandmayr, 1997, Büttner, 2007, Lehnhard, 2007) @de
preferred label: Vitis-Pribyslav-Störungssystem @de
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Wiesmath Fault
preferred label: Wiesmath-Störung @de
type: Concept
notation: AT-10441
definition: The approximately E-W striking fault runs from Stickelberg to Schwarzenbach.
definition: Die in etwa E-W-streichende Störung verläuft von Stickelberg bis Schwarzenbach. @de
created: 2020-04-30T14:27:03.808Z
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

NCA ENE-WSW Fault Set
definition: Dieses Störungsset besteht aus ENE-WSW-streichenden Störungen in den Nördlichen Kalkalpen (NKA). Diese Störungen entwickelten sich wahrscheinlich im mittleren Miozän als sinistrale Seitenverschiebungen und wurden während E-W-Kompression im Pannon als dextrale Seitenverschiebungen reaktiviert. (Peresson & Decker, 1997a, b). @de
definition: The fault set contains ENE-WSW trending faults within the Northern Calcareous Alps (NCA). These faults were probably generated during Middle Miocene times as left-lateral strike-slip faults. During Pannonian E-W compression, they might have been reactivated as right-lateral strike-slip faults (Peresson and Decker, 1997a, b).
references: https://data.geoscience.earth/ncl/geoera/ref/840
references: https://data.geoscience.earth/ncl/geoera/ref/841
notation: AT-527
type: Concept
created: 2020-04-30T14:27:01.638Z
preferred label: NKA-Störungsset (ENE-WSW) @de
narrower: Königsberg Fault
narrower: Toplitz Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Königsberg Fault
definition: The E-W trending brittle thrust fault of in the Northern Calcareous Alps runs from Altenmarkt/St. Gallen to 6 km east Kienberg and is juxtaposed by the left-lateral Göstling fault. (Decker et al., 1994)
definition: Die E-W-streichende spröde Überschiebung in den nördlichen Kalkalpen verläuft von Altenmarkt/St. Gallen bis 6 km östlich von Kienberg und wird von der Göstling-Störung sinistral versetzt. (Decker et al., 1994) @de
references: https://data.geoscience.earth/ncl/geoera/ref/726
notation: AT-10156
type: Concept
created: 2020-04-30T14:27:01.666Z
preferred label: Königsberg-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: NCA ENE-WSW Fault Set

Toplitz Fault
references: https://data.geoscience.earth/ncl/geoera/ref/732
notation: AT-10451
type: Concept
created: 2020-04-30T14:27:01.694Z
definition: The ENE-WSW striking fault runs from the east bank of the lake Hallstatt via Bad Aussee across the lakes Grundlsee and Toplitzseee to the west of the Hebenkas-Spitze. (Tollmann, 1986)
definition: Die ENE-WSW streichende Störung verläuft vom Ostufer des Hallstätter Sees über Bad Aussee durch den Grundlsee und Toplitzseee bis westlich der Hebenkas-Spitze. (Tollmann, 1986) @de
preferred label: Toplitz-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: NCA ENE-WSW Fault Set

NCA NW-SE Fault Set
definition: This fault set consists of NW-SE striking faults within the Northern Calcareous Alps (NCA) including Gosaukamm Fault, Gosausee Fault, Hochwart Fault, Lofer Fault, Scharnitzsattel Fault, Windischgarsten Fault, and Wolfgangsee Fault and other similar orientated faults with same kinematics. These faults were generated in the Late Eocene-Oligocene as right-lateral strike-slip faults. During Pannonian E-W compression, these NW-SE striking faults were reactivated as left-lateral strike-slip faults. (Peresson & Decker, 1997a, b)
definition: Dieses Störungsset besteht aus NW-SE-streichenden Störungen in den nördlichen Kalkalpen (NKA) und beinhaltet die Gosaukamm-, Gosausee, Hochwart-, Lofer, Scharnitzsattel-, Windischgarsten-, Wolfgangsee- und weitere ähnlich orientierte Störungen mit derselben Kinematik. Diese Störungen entstanden im späten Eozän bis Oligozän als dextrale Seitenverschiebungen und wurden während E-W-Kompression im Pannonium als sinistrale Seitenverschiebungen reaktiviert. (Peresson & Decker, 1997a,b) @de
references: https://data.geoscience.earth/ncl/geoera/ref/840
references: https://data.geoscience.earth/ncl/geoera/ref/841
notation: AT-531
type: Concept
created: 2020-04-30T14:27:01.722Z
preferred label: NKA-Störungsset (NW-SE) @de
narrower: Hochwart Fault
narrower: Gosausee Fault
narrower: Gosaukamm Fault
narrower: Scharnitzsattel Fault
narrower: Windischgarsten Fault
narrower: Wolfgangsee Fault
narrower: Lofer Fault
narrower: Wendelstein Fault
narrower: Spullersee Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Hochwart Fault
references: https://data.geoscience.earth/ncl/geoera/ref/766
references: https://data.geoscience.earth/ncl/geoera/ref/823
references: https://data.geoscience.earth/ncl/geoera/ref/840
notation: AT-10114
type: Concept
created: 2020-04-30T14:27:01.750Z
definition: This NW-SE trending fault with right-lateral shear sense runs through the area of the mountain Hochwart. (Linzer et al., 1997, 2002; Peresson & Decker, 1997)
definition: Diese NW-SE-streichende Störung mit dextral-seitenverschiebender Kinematik verläuft im Bereich des Hochwart. (Linzer et al., 1997, 2002; Peresson & Decker, 1997) @de
preferred label: Hochwart-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: NCA NW-SE Fault Set

Spullersee Fault
definition: This E-W trending fault is located in the area of the lake Spullersee. (Tollmann, 1986)
definition: Diese E-SW-streichende Störung befindet sich im Bereich des Spullersees. (Tollmann, 1986) @de
references: https://data.geoscience.earth/ncl/geoera/ref/732
notation: AT-10335
type: Concept
created: 2020-04-30T14:27:01.975Z
preferred label: Spullersee-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: NCA NW-SE Fault Set

Wendelstein Fault
definition: This NW-SE trending fault consists of two fault strands running parallel to each other SW and NE of Mt. Wendelstein (DE) from Fischbachau to Oberaudorf. (Frisch & Gawlick, 2003)
definition: Diese NW-SE-streichende Störung verläuft mit zwei Störungsästen von Fischbachau bis Oberaudorf SW und NE vom Wendelstein (DE). (Frisch & Gawlick, 2003) @de
notation: AT-10466
type: Concept
created: 2020-04-30T14:27:01.947Z
preferred label: Wendelstein-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: NCA NW-SE Fault Set

Windischgarsten Fault
references: https://data.geoscience.earth/ncl/geoera/ref/726
references: https://data.geoscience.earth/ncl/geoera/ref/823
references: https://data.geoscience.earth/ncl/geoera/ref/840
notation: AT-10408
type: Concept
created: 2020-04-30T14:27:01.862Z
definition: This NW-SE trending fault with a right-lateral shear sense is located in the area of the town of Windischgarsten. (Decker et al., 1994; Peresson & Decker, 1997; Linzer et al., 2002)
definition: Diese NW-SE-streichen Störung in den nördlichen Kalkalpen befindet sich im Bereich Windischgarsten mit dextral-seitenverschiebender Kinematik. (Decker et al., 1994; Peresson & Decker, 1997; Linzer et al., 2002) @de
preferred label: Windischgarsten-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: NCA NW-SE Fault Set

Scharnitzsattel Fault
references: https://data.geoscience.earth/ncl/geoera/ref/775
notation: AT-10314
type: Concept
created: 2020-04-30T14:27:01.834Z
definition: The NW-SE trending fault with right-lateral shear sense is located in the area of the Scharnitzsattel. (Ortner, 2001)
definition: Diese NW-SE-streichen Störung in den nördlichen Kalkalpen verläuft im Bereich des Scharnitzsattel mit dextral-seitenverschiebender Kinematik. (Ortner, 2001) @de
preferred label: Scharnitzsattel-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: NCA NW-SE Fault Set

Lofer Fault
references: https://data.geoscience.earth/ncl/geoera/ref/748
notation: AT-10188
type: Concept
created: 2020-04-30T14:27:01.918Z
definition: This NW-SE trending fault with right-lateral shear sense is located within the Northern Calcercous Alps close to the town of Lofer. (Frisch & Gawlick, 2003)
definition: Diese NW-SE-streichen Störung verläuft in den nördlichen Kalkalpen bei Lofer mit dextral-seitenverschiebender Kinematik. (Frisch & Gawlick, 2003) @de
preferred label: Lofer-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: NCA NW-SE Fault Set

Wolfgangsee Fault
references: https://data.geoscience.earth/ncl/geoera/ref/726
references: https://data.geoscience.earth/ncl/geoera/ref/748
references: https://data.geoscience.earth/ncl/geoera/ref/830
references: https://data.geoscience.earth/ncl/geoera/ref/840
references: https://data.geoscience.earth/ncl/geoera/ref/841
notation: AT-10411
type: Concept
created: 2020-04-30T14:27:01.890Z
definition: This NW-SE trending fault with right-lateral shear sense is located in the area of the Lake Wolfgang. (Decker et al., 1993, 1994; Peresson & Decker, 1997a, b; Frisch & Gawlick, 2003)
definition: Diese NW-SE-streichen Störung befindet sich in den nördlichen Kalkalpen im Bereich des Wolfgangsees mit dextral-seitenverschiebender Kinematik. (Decker et al., 1993, 1994; Peresson & Decker, 1997a, b; Frisch & Gawlick, 2003) @de
preferred label: Wolfgangsee-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: NCA NW-SE Fault Set

Gosaukamm Fault
references: https://data.geoscience.earth/ncl/geoera/ref/748
notation: AT-10091
type: Concept
created: 2020-04-30T14:27:01.806Z
definition: The NW-SE trending fault with right-lateral shear sense runs through the area of the Gosaukamm. (Frisch & Gawlick, 2003)
definition: Diese NW-SE streichende Störung mit dextral-seitenverschiebender Kinematik verläuft im Bereich des Gosaukammes. (Frisch & Gawlick, 2003) @de
preferred label: Gosaukamm-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: NCA NW-SE Fault Set

Gosausee Fault
references: https://data.geoscience.earth/ncl/geoera/ref/748
references: https://data.geoscience.earth/ncl/geoera/ref/767
notation: AT-10092
type: Concept
created: 2020-04-30T14:27:01.778Z
definition: This NW-SE trending fault with right-lateral shear sense runs in the area of the Gosau lakes. (Frisch & Gawlick, 2003; Wagreich & Decker, 2001)
definition: Diese NW-SE streichende Störung mit dextral-seitenverschiebender Kinematik verläuft im Bereich der Gosauseen. (Frisch & Gawlick, 2003; Wagreich & Decker, 2001) @de
preferred label: Gosausee-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: NCA NW-SE Fault Set

Salzach-Ennstal-Mariazell-Puchberg Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/823
notation: AT-140
type: Concept
created: 2020-04-30T14:27:00.451Z
definition: A WSW-ENE striking fault system of approximately 400 km in length, running from the western Tauern Window to the Vienna basin and up to 70 km of sinistral offset. The deformation holds a gradient from ductile (W) to brittle ductile (central region) to brittle (E). The Salzach-Ennstal-Mariazell-Puchberg Fault System is composed of W to E from the Salzach fault (brittle northern edge of the Tauern window), the Ennstal fault (southern edge of the northern Kalkalpen) and the Mariazell-Puchberg fault. (Linzer, 2002)
definition: Ein WSW-ENE streichendes Störungssystem von ca. 400 km Länge, das sich vom westlichen Tauernfenster bis zum Wiener Becken hinzieht und bis zu 70 km sinistralen Versatz aufweist. Die Deformation weist einen Gradienten von duktil (W) über spröd-duktil (Zentralbereich) bis spröd (E) auf. Das Salzach-Ennstal-Mariazell-Puchberg-Störungssystem setzt sich von W nach E aus dem Salzach-Störung (spröder Nordrand des Tauernfensters), der Ennstal-Störung (südlicher Rand der nördlichen Kalkalpen) und der Mariazell-Puchberg-Störung zusammen. (Linzer, 2002) @de
preferred label: Salzach-Ennstal-Mariazell-Puchberg-Störungssystem @de
narrower: Salzach Subfault System
narrower: Ennstal Subfault System
narrower: Mariazell-Puchberg Subfault System
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Ennstal Subfault System
preferred label: Ennstal-Teilstörungssystem @de
definition: The WSW-ENE trending fault system is part of the Salzach-Ennstal-Mariazell-Puchberg Faultsystem. Left-lateral movement is described (Linzer et al., 2002).
notation: AT-539
definition: Diese WSW-ENE-streichende Störung verläuft parallel zum Salzachtal und ist Teil des Salzach-Ennstal-Mariazell-Puchberg-Störungssystem. Sinistral-seitenverschiebende Kinematik ist beschrieben (Linzer et al., 2002). @de
type: Concept
created: 2020-04-30T14:27:00.536Z
in scheme: Tectonic Boundary Objects in Europe
broader: Salzach-Ennstal-Mariazell-Puchberg Fault System

Mariazell-Puchberg Subfault System
preferred label: Mariazell-Puchberg-Teilstörungssystem @de
notation: AT-511
definition: The WSW-ENE trending fault system is part of the Salzach-Ennstal-Mariazell-Puchberg Faultsystem. Left-lateral movement is described (Linzer et al., 2002).
type: Concept
created: 2020-04-30T14:27:00.564Z
definition: Diese WSW-ENE-streichende Störung verläuft parallel zum Salzachtal und ist Teil des Salzach-Ennstal-Mariazell-Puchberg-Störungssystem. Sinistral-seitenverschiebende Kinematik ist beschrieben (Linzer et al., 2002). @de
in scheme: Tectonic Boundary Objects in Europe
broader: Salzach-Ennstal-Mariazell-Puchberg Fault System

Salzach Subfault System
definition: The WSW-ENE trending fault system runs parallel to the valley of the river Salzach and is part of the Salzach-Ennstal-Mariazell-Puchberg Faultsystem. Left-lateral movement is described (Linzer et al., 2002).
definition: Diese WSW-ENE-streichende Störung verläuft parallel zum Salzachtal und ist Teil des Salzach-Ennstal-Mariazell-Puchberg-Störungssystem. Sinistral-seitenverschiebende Kinematik ist beschrieben (Linzer et al., 2002). @de
notation: AT-514
type: Concept
created: 2020-04-30T14:27:00.479Z
preferred label: Salzach-Teilstörungssystem @de
narrower: Salzach Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Salzach-Ennstal-Mariazell-Puchberg Fault System

Salzach Fault
references: https://data.geoscience.earth/ncl/geoera/ref/823
definition: This WSW-ENE trending fault runs parallel to the valley of the river Salzach and is part of the Salzach-Ennstal-Mariazell-Puchberg Faultsystem. Left -lateral movement is described (Linzer et al., 2002).
definition: Diese WSW-ENE-streichende Störung verläuft parallel zum Salzachtal und ist Teil des Salzach-Ennstal-Mariazell-Puchberg-Störungssystem. Sinistral-seitenverschiebende Kinematik ist beschrieben (Linzer et al., 2002). @de
notation: AT-10306
type: Concept
created: 2020-04-30T14:27:00.508Z
preferred label: Salzachtal-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Salzach Subfault System

Freyenstein Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/746
notation: AT-540
type: Concept
preferred label: Freyenstein-Störungssystem @de
created: 2020-04-30T14:27:02.818Z
definition: This ca. 45 km long NE-SW, partly NNE-SSW trending Subfault System extends from Windpassing to Freyenstein, Ysper and Klein-Nondorf (SW of Grafenschlag). It is part of the Vitis-Pribyslav Fault System at the eastern end of the South Bohemian Batholith. It includes an approximately 500 m thick ductile, SE-dipping mylonitic normal shear zone with top S/SE sense of shear dated to the Late Variscian. Late Miocene reactivation, with left-lateral movement, is assumed (Griesmeier et al., 2016).
definition: Dieses ca. 45 km lange, NE-SW-, teilweise NNE-SSW-streichende Teilstörungssystem verläuft von Windpassing nach Freyenstein und nördlich der Donau weiter nach Ysper und Klein-Nondorf (SW Grafenschlag). Es ist Teil des Vitis-Prybislav-Störungssystems am Ostrand des Südböhmischen Batholithen. Es beinhaltet eine ca. 500 m mächtige duktile SE-einfallende mylonitische Scherzone mit top nach S/SE abschiebender Kinematik aktiv während des spät-Variszikums. Eine Miozäne Reaktivierung mit sinistral-seitenverschiebender Bewegung ist beschrieben (Griesmeier et al., 2016). @de
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Niedere Tauern Southern Margin Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/762
references: https://data.geoscience.earth/ncl/geoera/ref/826
notation: AT-132
type: Concept
created: 2020-04-30T14:27:00.621Z
definition: This ca. 70 km long, approximately ESE-WNW trending Fault System extends from St. Michael im Lungau, following the basins of Tamsweg and Seetal to Oberwölz and Oberzeiring (east of the Pöls Valley) including parallel trending faults (Reinecker, 2000; Eder & Neubauer, 2000). It was initiated as ductile nappe boundaries during Cretaceous times and as S-dipping normal fault with top NE sense of shear active in the Paleogene. Reactivation with left-lateral strike-slip movement and the formation of pull-apart basins during Miocene times is described (Eder & Neubauer, 2000).
definition: Dieses etwa ESE-WNW streichende ca. 70 km lange Störungssystem zieht von St.Michael im Lungau über das Tamsweg- und Seetal-Becken bis Oberwölz und weiter nach Oberzeiring (östlich des Pölstals) und fasst parallel streichende Störungen in diesem Bereich zusammen (Reinecker, 2000; Eder & Neubauer, 2000). Es wurde als Deckengrenzen der Oberkreide angelegt und war vermutlich im Paläogen als dextral seitenverschiebende und top NE abschiebende Störungen aktiv. Diese wurden als sinistrale Seitenverschiebungen mit der Bildung von pull-apart-Becken im Miozän reaktiviert (Eder & Neubauer, 2000). @de
preferred label: Niedere Tauern Südrand Störungssystem @de
narrower: Niedere Tauern Fault
narrower: Tamsweg Basin Subfault System
alternative label: Lower Tauern Southern Margin Fault System
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Tamsweg Basin Subfault System
preferred label: Tamsweg-Becken-Teilstörungssystem @de
type: Concept
created: 2020-04-30T14:27:00.679Z
notation: AT-579
narrower: Seetal Fault
definition: This fault is part of the Niedere Tauern Südrand Fault System and borders respectively divided the Tamsweg basin in a western and eastern part. The strike-slip faults were reactivated contemporaneously with the formation of pull-apart basins during the Miocene (Eder & Neubauer, 2000; Wölfler et al., 2011).
definition: Dieses Teilstörungssystem ist Teil des Niedere Tauern Südrand-Störungssystems und begrenzt bzw. teilt das Tamsweg-Becken in einen östlichen und westlichen Teil. Die Seitenverschiebungen wurden mit der Bildung von pull-apart-Becken im Miozän angelegt (Eder & Neubauer, 2000; Wölfler et al., 2011). @de
references: https://data.geoscience.earth/ncl/geoera/ref/762
references: https://data.geoscience.earth/ncl/geoera/ref/8694
in scheme: Tectonic Boundary Objects in Europe
broader: Niedere Tauern Southern Margin Fault System

Seetal Fault
references: https://data.geoscience.earth/ncl/geoera/ref/762
notation: AT-10328
type: Concept
created: 2020-04-30T14:27:00.707Z
preferred label: Seetal-Störung @de
definition: The approximately E-W trending fault is part of the Niedere Tauern Südrand Fault System and runs from St. Margarethen/Lungau to Murau. Left-lateral strike-slip faults were reactivated contemporaneously with the formation of pull-apart basins during the Miocene (Eder & Neubauer, 2000).
definition: Die in etwa EW-streichende Störung ist Teil des Niedere Tauern Südrand-Störungssystems und verläuft von St. Margarethen im Lungau bis Murau. Die sinistralen Seitenverschiebungen wurden mit der Bildung von pull-apart-Becken im Miozän reaktiviert (Eder & Neubauer, 2000). @de
in scheme: Tectonic Boundary Objects in Europe
broader: Tamsweg Basin Subfault System

Niedere Tauern Fault
preferred label: Niedere-Tauern-Störung @de
notation: AT-10442
type: Concept
created: 2020-04-30T14:27:00.650Z
definition: The approximately E-W trending fault is part of the Niedere Tauern Südrand Fault System and runs from Weißpriach to Teufenbach. Left-lateral strike-slip faults were reactivated contemporaneously with the formation of pull-apart basins during the Miocene (Eder & Neubauer, 2000).
definition: Die in etwa EW-streichende Störung ist Teil des Niedere Tauern Südrand-Störungssystems und verläuft von Weißpriach bis Teufenbach. Die sinistralen Seitenverschiebungen wurden mit der Bildung von pull-apart-Becken im Miozän reaktiviert (Eder & Neubauer, 2000). @de
alternative label: Lower Tauern Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Niedere Tauern Southern Margin Fault System

Trojeralm Fault Set
references: https://data.geoscience.earth/ncl/geoera/ref/734
notation: AT-557
type: Concept
created: 2020-04-30T14:27:02.790Z
definition: This subfault system consists of NW-SE trending parallel mylonitic and brittle strike-slip faults including the Trojeralm-, Fleischbachkees-, and Kalsertal Fault. (Senarclens-Grancy, 1959)
definition: Ist ein Störungsset von NW-SE-streichenden parallelen mylonitischen und spröden Seitenverschiebungen, welche die Trojeralm-, Fleischbachkees- und Kalsertal-Störung beinhaltet. (Senarclens-Grancy, 1959) @de
preferred label: Trojeralm-Störungsset @de
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Nappe Boundary in Austria
definition: Eine Deckengrenze beschreibt in Österreich einen diskreten, spröden oder duktilen Scherhorizont zwischen tektonischen Einheiten (z.B. Decken, Deckensysteme). „Diskret“ bezieht sich hier auf den Kartenmaßstab, denn im Gelände kann eine Deckengrenze einer diffusen tektonischen Melangezone, mit Elementen beider Einheiten die sie trennt, entsprechen (Hintersberger et al. 2017) @de
preferred label: Deckengrenze in Österreich @de
created: 2020-09-09T13:35:18.993Z
definition: In Austria, a nappe boundary describes a discrete, brittle or ductile, shearing horizon between tectonic units (e.g. nappes, nappe systems). In this definition, „discrete“ refers to map scale, since in the field a nappe boundary can correspond to a diffuse tectonic mélange zone with elements of both units that it separates (Hintersberger et al. 2017)
notation: AT-50000
type: Concept
narrower: Base of the Ackerl Nappe
narrower: Base of the Bajuvaric Nappe System
narrower: Base of the Berchtesgaden Nappe
narrower: Base of the Dachstein Nappe
narrower: Base of the Drauzug-Gurktal Nappe System
narrower: Base of the Drosendorf Nappe System
narrower: Base of the Exenberg Nappe
narrower: Base of the Frankenfels Nappe
narrower: Base of the Gföhl Nappe System
narrower: Base of the Glockner Nappe System
narrower: Base of the Göller Nappe
narrower: Base of the Greifenstein Nappe
narrower: Base of the Greywacke Zone Nappe System
narrower: Base of the Sieggraben Nappe
narrower: Base of the Silvretta-Seckau Nappe System
narrower: Base of the Stolzalpe Nappe
narrower: Base of the Stuhleck-Kirchberg Nappe
narrower: Base of the Tirolic Noric Nappe System
narrower: Base of the Totes Gebirge Nappe
narrower: Base of the Ultrahelvetic Units
narrower: Base of the Unterberg Nappe
narrower: Base of the Upper Penninic Nappes
narrower: Base of the Veitsch-Silbersberg Nappe System
narrower: Base of the Gstoder Nappe
narrower: Base of the Hallstatt Nappe
references: https://data.geoscience.earth/ncl/geoera/ref/88
narrower: Base of the Rhenodanubian Nappe System
narrower: Base of the Saualpe-Koralpe Nappe
narrower: Base of the Schneeberg Nappe
narrower: Base of the Schöckel Nappe
narrower: Base of the Semmering-Wechsel Nappe System
narrower: Base of the Juvavic Nappe System
narrower: Base of the Königstuhl Nappe
narrower: Base of the Koralpe-Wölz Nappe System
narrower: Base of the Krabachjoch Nappe
narrower: Base of the Laab Nappe
narrower: Base of the Laufnitzdorf Nappe
narrower: Base of the Lechtal Nappe
narrower: Base of the Lunz Nappe
narrower: Base of the Matrei Nordrahmen Zone Nappe System
narrower: Base of the Middle Penninic Nappes
narrower: Base of the Modereck Nappe System
narrower: Base of the Murau Nappe
narrower: Base of the Ostrong Nappe System
narrower: Base of the Ötztal-Bundschuh Nappe System
narrower: Base of the Pusterwald Nappe
narrower: Base of the Radstadt Nappe System
narrower: Base of the Reichraming Nappe
narrower: Base of the Reisalpe Nappe
narrower: Base of the Helvetic Nappes
narrower: Base of the Hochlantsch Nappe
in scheme: Tectonic Boundary Objects in Europe
propagate type: Limit
type: Limit
broader: Tectonic Boundary in Austria

Base of the Semmering-Wechsel Nappe System
references: https://data.geoscience.earth/ncl/geoera/ref/8714
definition: This nappe system is the lowermost Austroalpine element above the Penninic Nappes on the eastern edge of the Alps, which overlies the Penninic nappes in the Rechnitz Window Group. The base of the Semmering-Wechsel Nappe System can be found between St. Michael/Obersteiermark and Gloggnitz, a small segment also crops out at Hohentauern.
definition: Dieses Deckensystem stellt das tiefste ostalpine Element über den Penninischen Decken am Alpenostrand dar, das die Penninischen Decken im Bereich der Rechnitzer Fenstergruppe überlagert. Die Basis des Semmering-Wechsel Deckensystem kann zwischen St. Michael in der Obersteiermark und Gloggnitz beobachtet werden, ein sehr kleiner Abschnitt auch bei Hohentauern. @de
type: Concept
notation: AT-50564
preferred label: Basis des Semmering-Wechsel-Deckensystems @de
created: 2020-09-09T13:35:19.554Z
in scheme: Tectonic Boundary Objects in Europe
limit to: http://resource.geolba.ac.at/tectonicunit/231
type: Limit
broader: Nappe Boundary in Austria

Base of the Greywacke Zone Nappe System
definition: The base of these nappes lies, for the most part, in Styria in the area between St. Michael/Obersteiermark and Gloggnitz (Lower AustrIa) and crops out as well southwest of Trieben. The Grauwackenzone nappes overlie the Silvretta-Seckau Nappe System and are overlain by the Tirolic-Noric Nappe System. During the Eoalpine event in the Cretaceous (85-135 Ma),they were sheared off from their basement and overthrusted towards northwest (adapted from Froitzheim et al., 2008).
definition: Die Basis dieser Decken liegt großteils in der Steiermark zwischen St.Michael in der Obersteiermark und Gloggnitz (Niederösterreich) und ist auch südwestlich von Trieben aufgeschlossen. Die Decken der Grauwackenzone liegen über dem Silvretta-Seckau-Deckensystem und werden vom Tirolisch-Norischen Deckensystem überlagert. Während des eoalpidischen Ereignisses wurden sie in der Kreide (zwischen 85 und 135 Ma) von ihrem Untergrund abgeschert und gegen Nordwesten überschoben (verändert nach Froitzheim et al., 2008). @de
created: 2020-09-09T13:35:19.582Z
notation: AT-50565
type: Concept
preferred label: Basis des Grauwackenzone-Deckensystems @de
references: https://data.geoscience.earth/ncl/geoera/ref/1243
in scheme: Tectonic Boundary Objects in Europe
limit to: http://resource.geolba.ac.at/tectonicunit/144
type: Limit
broader: Nappe Boundary in Austria

Base of the Modereck Nappe System
references: https://data.geoscience.earth/ncl/geoera/ref/1244
definition: The Modereck Nappe system overlies the Venediger Nappe System in the Tauern Window, therefore its base separates the Subpenninic units throughout the Tauern Window (Pestal et al., 2009).
definition: Die Basis des Modereck-Deckensystems ist im Tauernfenster zu finden und trennt die Modereck Decken vom ebenfalls subpenninischen Venediger-Deckensystem (Pestal et al., 2009). @de
references: https://data.geoscience.earth/ncl/geoera/ref/1246
type: Concept
created: 2020-09-09T13:35:19.440Z
notation: AT-50557
preferred label: Basis des Modereck-Deckensystems @de
in scheme: Tectonic Boundary Objects in Europe
limit to: http://resource.geolba.ac.at/tectonicunit/320
type: Limit
broader: Nappe Boundary in Austria

Base of the Glockner Nappe System
definition: The base of the Glockner Nappe system is an important, mainly S-dipping thrust fault in the Tauern window which was mainly active during Cretaceous times. It thrusts the Penninic Glockner Nappe system onto the underlying Subpenninic Venediger and Modereck Nappe systems. It can be observed throughout the Tauern Window between east of the Brenner pass in the west and Gmünd and Katschberg in the east (Staub, 1924).
definition: Die Basis des Glockner-Deckensystems ist eine wichtige, hauptsächlich nach S einfallende Überschiebung im Tauernfenster, die hauptsächlich in der Kreide aktiv war. Diese Deckengrenze kann im gesamten Tauernfenster zwischen dem Brennerpass im Westen und Gmünd und Katschberg im Osten beobachtet werden. Sie überschiebt das penninische Glockner-Deckensystem über die liegenden subpenninischen Venediger- bzw. Modereck-Deckensysteme (Staub, 1924). @de
created: 2020-09-09T13:35:19.468Z
preferred label: Basis des Glockner-Deckensystems @de
type: Concept
notation: AT-50559
notation: AT-50558
references: https://data.geoscience.earth/ncl/geoera/ref/1247
notation: IT-4390
in scheme: Tectonic Boundary Objects in Europe
limit to: http://resource.geolba.ac.at/tectonicunit/269
type: Limit
broader: Penninic Domain
broader: Nappe Boundary in Austria

Base of the Matrei Nordrahmen Zone Nappe System
definition: This tectonically highest Penninic nappe system in the north and south of the Tauern Window overthrusts the Glockner Nappe System at its base (Schuster et al. 2006).
definition: Dieses tektonisch höchste penninisches Deckensystem im Norden und Süden des Tauernfensters überschiebt an seiner Basis das Glockner-Deckensystem (Schuster et al.. 2006). @de
references: https://data.geoscience.earth/ncl/geoera/ref/1248
notation: IT-4391
notation: AT-50560
notation: AT-50571
type: Concept
preferred label: Basis des Matrei-Nordrahmen-Zone-Deckensystems @de
created: 2020-09-09T13:35:19.498Z
in scheme: Tectonic Boundary Objects in Europe
limit to: http://resource.geolba.ac.at/tectonicunit/357
type: Limit
broader: Austroalpine Domain
broader: Nappe Boundary in Austria

Base of the Radstadt Nappe System
references: https://data.geoscience.earth/ncl/geoera/ref/8709
definition: The Radstadt Nappe System is the northern Lower Austroalpine part of the Tauern Window above the Penninicum and has been integrated in the Alpine orogenic wedge during Upper Cretaceous (Pestal et al., 2009).
definition: Das Radstadt-Deckensystem stellt den Unterostalpinen nördlichen Rahmen des Tauernfensters über dem Penninikum dar und wurde in der Oberkreide in den Alpinen Orogenkeil eingebaut (Pestal et al., 2009). @de
references: https://data.geoscience.earth/ncl/geoera/ref/1246
notation: AT-50561
type: Concept
preferred label: Basis des Radstadt-Deckensystems @de
notation: AT-50569
created: 2020-09-09T13:35:19.525Z
in scheme: Tectonic Boundary Objects in Europe
type: Limit
limit to: http://resource.geolba.ac.at/tectonicunit/220
broader: Nappe Boundary in Austria

Base of the Drosendorf Nappe System
definition: The base of this nappe system of the Moldanubian Nappes seperates the Drosendorf nappe system from the Ostrong Nappe System, which it overthrusts. The base of the Drosendorf Nappe System crops out between Ybbs/Donau and Brand and in smaller parts around Goschenreith and Drosendorf.
definition: Die Basis des Drosendorf-Deckensystems des Moldanubikums trennt dieses vom überschobenen Ostrong-Deckensystem. Sie ist zwischen Ybbs and der Donau und Brand aufgeschlossen, sowie in kleinern Teilen um Goschenreith und Drosendorf. @de
notation: AT-50534
created: 2020-09-09T13:35:19.327Z
notation: AT-50524
preferred label: Basis des Drosendorf-Deckensystems @de
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/1245
in scheme: Tectonic Boundary Objects in Europe
limit to: http://resource.geolba.ac.at/tectonicunit/102
type: Limit
broader: Nappe Boundary in Austria

Base of the Ostrong Nappe System
definition: The Ostrong Nappe System, the lowermost system of the Moldanubian Nappes, is overthrusted by the Drosendorf and Gföhl Nappe Systems. The intrusion of the Southern Bohemian Batholith (300-340 Ma) makes up a great part of the nappe system and caused a high-temperature and low-pressure metamorphism. Its base can only be observed around Nöstling.
definition: Das Ostrong-Deckensystem, das unterste Deckenystem der Moldanubischen Decken, wird von den Drosendorf- und Gföhl-Deckensystemen überlagert. Die Intrusion des Südböhmischen Batholiths (300-340 Ma) hat eine Hochtemperatur-Niederdruck-Metamorphose zur Folge. Die Basis des Ostrong-Deckensystems ist nur bei Nöstlig aufgeschlossen. @de
references: https://data.geoscience.earth/ncl/geoera/ref/1245
notation: AT-50533
type: Concept
created: 2020-09-09T13:35:19.356Z
preferred label: Basis des Ostrong-Deckensystems @de
in scheme: Tectonic Boundary Objects in Europe
limit to: http://resource.geolba.ac.at/tectonicunit/105
type: Limit
broader: Nappe Boundary in Austria

Base of the Drauzug-Gurktal Nappe System
definition: Apart from a small part west of the Brenner Pass in Tirol, the base of this nappe system can be observed in Carynthia and Styria between Bad Kleinkirchheim and Gasen. The Drauzug-Gurktal-Nappes overthrust the Ötztal-Bundschuh and Koralpe Wölz Nappe Systems in shallow reverse faults (Froitzheim et al., 2008).
definition: Abgesehen von einem kleinen Teil westlich des Brennerpasses ist die Basis dieses Deckensystems in Kärnten und der Steiermark zwischen Bad Kleinkirchheim und Gasen aufgeschlossen. Das Drauzug-Gurktal-Deckensystems überfährt in flachen Überschiebungen das Ötztal-Bundschuh- und das Koralpe-Wölz-Deckensystem (Froitzheim et al., 2008). @de
notation: AT-50546
notation: AT-50545
notation: AT-50581
type: Concept
created: 2020-09-09T13:35:19.385Z
preferred label: Basis des Drauzug-Gurktal-Deckensystems @de
references: https://data.geoscience.earth/ncl/geoera/ref/1243
in scheme: Tectonic Boundary Objects in Europe
limit to: http://resource.geolba.ac.at/tectonicunit/126
type: Limit
broader: Nappe Boundary in Austria

Base of the Ötztal-Bundschuh Nappe System
definition: This nappe system includes the Ötztal Nappe to the west and the Bundschuh Nappe to the east of the Tauern Window. The base of these nappes seperates the Ötztal-Bundschuh Nappe System from the overthrusted Koralpe-Wölz Nappe system (Froitzheim et al., 2008).
definition: Dieses Deckensystem umfasst die Ötztal-Decke westlich und die Bundschuh-Decke östlich des Tauernfensters. Die Basis dieser Decken trennt das Ötztal-Bundschuh-Deckensystem vom überschobenen Koralpe-Wölz-Deckensystem. (Froitzheim et al., 2008). @de
references: https://data.geoscience.earth/ncl/geoera/ref/1243
references: https://data.geoscience.earth/ncl/geoera/ref/1244
notation: IT-0034
notation: AT-50572
notation: AT-50562
notation: AT-50573
preferred label: Basis des Ötztal-Bundschuh-Deckensystems @de
created: 2020-09-09T13:35:19.412Z
type: Concept
notation: AT-50549
notation: AT-50547
type: Limit
in scheme: Tectonic Boundary Objects in Europe
limit to: http://resource.geolba.ac.at/tectonicunit/182
broader: Austroalpine Domain
broader: Nappe Boundary in Austria

Base of the Juvavic Nappe System
definition: The base of the Juvavic Nappe System extends from southwest of Salzburg in ENE direction to west of Wiener Neustadt. The Juvavic Nappes were detached from their basement and thrust onto the future Tirolic-Noric Nappe System as early as the Early Upper Jurassic (about 160 Ma). This probably occurred, in part, during the obduction of units from the Neotethys Ocean (Meliaticum), but also partly during a transpressive regime in the Late Upper Jurassic and Early Lower Cretaceous (adapted from Schmid et al., 2004).
definition: Die Basis des Juvavischen Deckensystem erstreckt sich von südwestlich von Salzburg in Richtung ENE bis westlich von Wiener Neustadt. Die Decken wurden bereits ab dem frühen Oberjura (ca. 160 Ma) von ihrem Untergrund abgelöst und auf das zukünftige Tirolisch-Norische Deckensystem aufgeschoben. Dies geschah wahrscheinlich zum Teil im Zuge der Obduktion von Einheiten aus dem Neotethys-Ozean (Meliatikum), zum Teil aber auch in einem transpressiven Regime im späten Oberjura und in der frühen Unterkreide (verändert nach Schmid et al., 2004). @de
references: https://data.geoscience.earth/ncl/geoera/ref/1244
notation: AT-50566
notation: AT-50502
type: Concept
preferred label: Basis des Juvavischen Deckensystems @de
created: 2020-09-09T13:35:19.104Z
in scheme: Tectonic Boundary Objects in Europe
limit to: http://resource.geolba.ac.at/tectonicunit/149
type: Limit
broader: Nappe Boundary in Austria

Base of the Tirolic Noric Nappe System
references: https://data.geoscience.earth/ncl/geoera/ref/1244
definition: Parts of the base of the Tirolic Noric Nappe System can be traced throughout Austria, from southwest of Vorarlberg in ENE direction to west of Wiener Neustadt. The system contains nappes, sheared off in early Lower Cretaceous times (135 Ma), overthrusting the Bajuvaric Nappe System.
definition: Teile der Basis des Tirolisch-Norischen Deckensystems können quer durch Österreich vom Südwesten Vorarlbergs in Richtung ENE bis westlich von Wiener Neustadt verfolgt werden. Das Tirolisch-Norische Deckensystem besteht aus Decken, die ab der frühen Unterkreide (ca. 135 Ma) abgeschert und über das Bajuvarische Deckensystem geschoben wurden. @de
notation: AT-50541
notation: AT-50563
notation: AT-50553
notation: AT-50503
notation: AT-50504
notation: AT-50526
notation: AT-50505
notation: AT-50527
type: Concept
preferred label: Basis des Tirolisch-Norischen Deckensystems @de
created: 2020-09-09T13:35:19.132Z
notation: AT-50582
references: https://data.geoscience.earth/ncl/geoera/ref/1250
in scheme: Tectonic Boundary Objects in Europe
limit to: http://resource.geolba.ac.at/tectonicunit/19
type: Limit
broader: Nappe Boundary in Austria

Base of the Bajuvaric Nappe System
references: https://data.geoscience.earth/ncl/geoera/ref/1244
definition: The base of the Bajuvaric Nappe System crops out in Vorarlberg and can be traced from south of Gmunden (Upper Austria) in ENE direction to southwest of Vienna. The system contains nappes, sheared off in the middle Lower Cretaceous (120 Ma) and forms the lowermost nappe system of the Northern Calcareous Alps (Schmid et al, 2004).
definition: Die Basis des Bajuvarischen Deckensystems ist in Vorarlberg aufgeschlossen und kann von südlich von Gmunden (Oberösterreich) nach ENE bis südwestlich von Wien verfolgt werden. Die Decken wurden in der frühen Unterkreide (ca. 120 Ma) abgeschert und bilden das unterste Deckensystem der nördlichen Kalkalpen (Schmid et al, 2004). @de
notation: AT-50578
type: Concept
preferred label: Basis des Bajuvarischen Deckensystems @de
notation: AT-50506
notation: AT-50507
notation: AT-50508
notation: AT-50509
created: 2020-09-09T13:35:19.161Z
notation: AT-50583
in scheme: Tectonic Boundary Objects in Europe
type: Limit
limit to: http://resource.geolba.ac.at/tectonicunit/116
broader: Nappe Boundary in Austria

Base of the Koralpe-Wölz Nappe System
definition: The base of the nappe system can be observed between east of the Brenner Pass and southwest of Mattersburg. The exhumation of the units took place in the Upper Cretaceous (from 92 Ma) by thrust faults in the underlying parts and normal faults in the overlying parts of the nappe stack. Therefore, the Koralpe Wölz Nappe System represents a metamorphic extrusion wedge which originated during the Eoalpine event. (Froitzheim et al., 2008).
definition: Die Basis dieses Deckensystem kann zwischen dem Brennerpass (E) und südwestlich von Mattersburg beobachtet werden. Die Exhumation der Einheiten erfolgte in der Oberkreide (ab 92 Ma) durch Überschiebungen im liegenden und Abschiebungen im hangenden Teil des Deckenstapels. Demnach stellt das Koralpe-Wölz-Deckensystem einen metamorphen Extrusionskeil dar, der während des eoalpidischen Ereignisses entstand (Froitzheim et al., 2008). @de
references: https://data.geoscience.earth/ncl/geoera/ref/1243
references: https://data.geoscience.earth/ncl/geoera/ref/1244
notation: AT-50570
type: Concept
created: 2020-09-09T13:35:19.189Z
notation: AT-50529
preferred label: Basis des Koralpe-Wölz-Deckensystems @de
notation: AT-50568
notation: AT-50510
notation: AT-50587
notation: AT-50551
notation: AT-50550
in scheme: Tectonic Boundary Objects in Europe
limit to: http://resource.geolba.ac.at/tectonicunit/156
type: Limit
broader: Nappe Boundary in Austria

Base of the Upper Penninic Nappes
definition: The base of the Upper Penninic Nappes can in Austria be found in Vorarlberg, the southwest border of Tirol to Switzerland and from north of Ybbsitz in ENE direction to west of Vienna. They were formed during the closure of the Piemont-Ligurian Ocean, which began in the middle Upper Cretaceous and lasted until the Eocene. The greater part of the oceanic crust was subducted during this process, whereby the Upper Penninic nappes were overthrust by the Austroalpine nappes (Froitzheim et al., 2008).
definition: Die Basis der Oberen Penninischen Decken ist in Österreich in Vorarlberg und der südwestlichen Grenze von Tirol zu finden, sowie von Ybbsitz in Richtung ENE bis in den Westen von Wien. Diese Decken entstanden bei der Schließung des Piemont-Ligurischen Ozeans, die in der mittleren Oberkreide einsetzte und bis ins Eozän andauerte. Bei diesem Prozess wurde der größte Teil der ozeanischen Kruste subduziert. Dabei wurden die Oberen Penninischen Decken von den Ostalpinen Decken überschoben (Froitzheim et al., 2008). @de
notation: AT-50129
notation: AT-50517
type: Concept
created: 2020-09-09T13:35:19.048Z
notation: AT-50516
preferred label: Basis der Oberen Penninischen Decken @de
references: https://data.geoscience.earth/ncl/geoera/ref/1243
in scheme: Tectonic Boundary Objects in Europe
limit to: http://resource.geolba.ac.at/tectonicunit/246
type: Limit
broader: Nappe Boundary in Austria

Base of the Middle Penninic Nappes
definition: The Middle Penninic Nappes and their base can in Austria only be found in the Engadin Window. For the most part, they contain rocks of the Iberia-Briançonnais microcontinent and show no pressure-enhanced metamorphism like the Lower Penninic nappes (Froitzheim et al., 2008).
definition: Die Basis der Mittleren Penninischen Decken ist in Österreich ausschließlich im Unterengadiner Fenster zu finden. Zum größten Teil bestehen sie aus Gesteinen des Ibera-Briançonnais-Mikrokontinent und zeigen keine druckbetonte Metamorphose wie die Unteren Penninischen Decken (Froitzheim et al., 2008). @de
references: https://data.geoscience.earth/ncl/geoera/ref/1243
created: 2020-09-09T13:35:19.076Z
notation: AT-50130
preferred label: Basis der Mittleren Penninischen Decken @de
type: Concept
in scheme: Tectonic Boundary Objects in Europe
limit to: http://resource.geolba.ac.at/tectonicunit/236
type: Limit
broader: Nappe Boundary in Austria

Base of the Lechtal Nappe
references: https://data.geoscience.earth/ncl/geoera/ref/8705
definition: The base of the Lechtal Nappe of the Bajuvaric Nappe System overthrusting the Allgäu Nappe can be observed north of the Lech Valley in Vorarlberg northwest of Lech and in Tirol between Hinterhornbach and Musau. It manifests strikingly in mainly shallow S- to SW-dipping thrusts.
definition: Die Basis der Lechtal Decke des Bajuvarischen Deckensystems überschiebt die Allgäu Decke und kann nördlich des Lechtales in Vorarlberg nordwestlich von Lech und in Tirol zwischen Hinterhornbach und Musau beobachtet werden. Die Überschiebung ist unterhalb der Höllhörner, an der Jochspitze am Hornbachjoch sowie nördlich des Großen Wilden bis südöstlich der Schönberghütte und westlich des Kreuzkopfes aufgeschlossen. Sie ist messerscharf ausgebildet und fällt überwiegend flach nach Süd bis Südsüdost ein. Direkt unter der Deckengrenze treten obertriassische Hauptdolomit-Schürflinge der Lechtal-Decke in der überfahrenen, völlig zerscherten, unterjurassischen Allgäu-Formation der Allgäu-Decke auf, wobei Hartbänke vielfach intensiv in Phacoide zerlegt sind. Die Allgäu-Formation ist aber nicht überall deckenparallel, sondern kann durchaus auch von unten stumpfwinkelig bis nahezu senkrecht gegen die Deckengrenze stossen. Die flachen Deckenüberschiebungen nehmen aber nur im wenigsten der Fälle einen geradlinigen, sondern zeigen meist einen gezackten Verlauf. Ein gutes Beispiel ist die Überfahrung der Lechtal-Decke nördlich des Litnisschrofens, die starke Richtungsänderungen und auch sehr veränderliche Einfallswerte aufweist. Dies ist sowohl durch den strukturgeologischen Aufbau der unterlagernden Algäu-Decke als auch durch Blattverschiebungen quer zur Überschiebungsrichtung zu erklären. Die Überschiebungen können aber auch sehr steil erfolgen, wie dies im Süden der Luitpoldzone zu sehen ist und generell entlang des gesamten Nordrandes der Allgäu-Decke @de
type: Concept
alternative label: Base of the Lech Valley Nappe
preferred label: Basis der Lechtal-Decke @de
created: 2020-09-09T13:35:20.365Z
notation: AT-51069
in scheme: Tectonic Boundary Objects in Europe
type: Limit
broader: Nappe Boundary in Austria

Base of the Krabachjoch Nappe
references: https://data.geoscience.earth/ncl/geoera/ref/1244
definition: The base of the Krabachjoch Nappe of the Tirolic-Noric Nappe System lies north of St.Anton/Arlberg and west of Imst.
definition: Die Basis der Krabachjoch-Decke des Tirolisch-Norischen Deckensystems ist nördlich von St. Anton am Arlberg, sowie westlich von Imst zu finden. (May & Eisbacher, 1999) @de
notation: AT-51070
created: 2020-09-09T13:35:20.393Z
preferred label: Basis der Krabachjoch-Decke @de
type: Concept
in scheme: Tectonic Boundary Objects in Europe
type: Limit
broader: Nappe Boundary in Austria

Base of the Totes Gebirge Nappe
references: https://data.geoscience.earth/ncl/geoera/ref/1244
definition: The base of the Totes Gebirge Nappe of the Tirolic-Noric Nappe System lies between north of Altaussee and west of Steyrling.
definition: Die Basis der Totes Gebirge-Decke des Tirolisch-Norischen Deckensystems kann von nördlich von Altaussee bis welstlich vom Steyrling verfolgt werden. @de
preferred label: Basis der Totes Gebirge-Decke @de
type: Concept
notation: AT-51065
created: 2020-09-09T13:35:20.252Z
in scheme: Tectonic Boundary Objects in Europe
type: Limit
broader: Nappe Boundary in Austria

Base of the Berchtesgaden Nappe
references: https://data.geoscience.earth/ncl/geoera/ref/1244
definition: The base of the Berchtesgarden Nappe of the Juvavic Nappe System can be followed in Austria along the German-Austrian border from east of Wildental via the Saalach Valley to east of Unken.
created: 2020-09-09T13:35:20.280Z
notation: AT-51066
type: Concept
preferred label: Basis der Berchtesgaden-Decke @de
definition: Die Basis der Berchtesgaden-Decke des Juvavischen Deckensystem kann in Österreich entlang der Grenze zu Deutschland von östlich von Wildental, über das Saalachtal bis östlich von Unken verfolgt werden. @de
in scheme: Tectonic Boundary Objects in Europe
type: Limit
broader: Nappe Boundary in Austria

Base of the Saualpe-Koralpe Nappe
references: https://data.geoscience.earth/ncl/geoera/ref/8699
references: https://data.geoscience.earth/ncl/geoera/ref/8707
references: https://data.geoscience.earth/ncl/geoera/ref/8703
references: https://data.geoscience.earth/ncl/geoera/ref/8713
definition: The base of the Pusterwald Nappe, a lower nappe of the Koralpe-Wölz Nappe System is represented at map sheets of the Geological Survey of Austria (Moser, 2015; Ebner et al., 2017; Iglseder, 2019). The emplacement took place during the Eoalpine orogenesis.
definition: Die Basis der Saualpe-Koralpe-Decke, einer liegenden Einheit des Koralpe-Wölz-Deckensystems ist teilweise auf Karten der Geologischen Bundesanstalt dargestellt (Moser, 2015; Ebner et al., 2017; Iglseder, 2019). Ihre Platznahme erfolgte während der eoalpidischen Gebirgsbildung (Schuster, 2015). @de
type: Concept
preferred label: Basis der Saualpe-Koralpe-Decke @de
notation: AT-51067
created: 2020-09-09T13:35:20.308Z
in scheme: Tectonic Boundary Objects in Europe
type: Limit
broader: Nappe Boundary in Austria

Base of the Reichraming Nappe
references: https://data.geoscience.earth/ncl/geoera/ref/1244
definition: The base of the Reichraming Nappe of the Bajuvaric Nappe System can be followed from north of Molln in the west to north of Reichraming in the east.
definition: Die Basis der Reichraming-Decke des Bajuvarischen Deckensystems kann von nörldich von Molln im Westen bis nördlich von Reichraming im Osten verfolgt werden. @de
preferred label: Basis der Reichraming-Decke @de
type: Concept
notation: AT-51068
created: 2020-09-09T13:35:20.336Z
in scheme: Tectonic Boundary Objects in Europe
type: Limit
broader: Nappe Boundary in Austria

Base of the Silvretta-Seckau Nappe System
definition: The base of the Silvretta-Seckau Nappe System seperates the Upper Austroalpine from the Lower Austroalpine. It can be observed in Austria in the south of Vorarlberg and Tirol (?), in the Tauern Window in the area between Flachau and Mauterndorf, and between the Mürz Valley and St. Lorenzen/Wechsel. The Nappe Stystem is overlain by the Greywacke Zone and Koralpe-Wölz Nappe Systems (Froitzheim et al., 2008).
definition: Die Basis des Silvretta-Seckau-Deckensystems trennt das Oberostalpin vom Unterostalpin. Sie ist im Süden von Tirol und Vorarlberg zu finden, im Tauernfenster zwischen Flachau und Mauerndorf, sowie zwischen Mürztal und St. Lorenzen am Wechsel. Das Deckensystem wird vom Grauwackenzone-Deckensystem und vom Koralpe-Wölz-Deckensystem überlagert (Froitzheim et al., 2008). @de
created: 2020-09-09T13:35:19.216Z
type: Concept
notation: AT-50513
notation: AT-50567
preferred label: Basis des Silvretta-Seckau-Deckensystems @de
notation: AT-50575
notation: AT-50552
notation: AT-50574
notation: AT-50585
references: https://data.geoscience.earth/ncl/geoera/ref/1243
in scheme: Tectonic Boundary Objects in Europe
limit to: http://resource.geolba.ac.at/tectonicunit/116
type: Limit
broader: Nappe Boundary in Austria

Base of the Rhenodanubian Nappe System
definition: The base of the Rhenodanubian Nappe System can be observed in Austria and Germany along the north of the Eastern Alps - from the norhern part of Vorarlberg via north of Salzburg to northwest of Vienna. The cretaceous to eocene sediments were stacked in several nappes beneath the Austroalpine through N–NW oriented overthrusting (Froitzheim et al., 2008).
definition: Die Basis des Rhenodanubischen Deckensystems kann im Norden der Ostalpen in Österreich und Deutschland von Vorarlberg über nördlich von Salzburg bis nordwestlich von Wien beobachtet werden. Die kreidezeitlichen bis eozänen Sedimente wurden durch N–NW-gerichtete Überschiebungen in mehreren Decken in einem Akkretionskeil unter dem Ostalpin gestapelt (Froitzheim et al., 2008). @de
references: https://data.geoscience.earth/ncl/geoera/ref/1243
created: 2020-09-09T13:35:19.244Z
type: Concept
notation: AT-50518
notation: AT-50519
preferred label: Basis des Rhenodanubisches Deckensystems @de
notation: AT-50554
in scheme: Tectonic Boundary Objects in Europe
limit to: http://resource.geolba.ac.at/tectonicunit/273
type: Limit
broader: Nappe Boundary in Austria

Base of the Laufnitzdorf Nappe
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/1244
definition: The base of the Laufnitzdorf Nappe can be observed between west of Großstübing and south of Schrems.
definition: Die Basis der Laufnitzdorf-Decke kann zwischen westlich von Großstübing und südlich von Schrems beobachtet werden. @de
created: 2020-09-09T13:35:20.167Z
type: Concept
preferred label: Basis der Laufnitzdorf-Decke @de
notation: AT-51061
in scheme: Tectonic Boundary Objects in Europe
broader: Nappe Boundary in Austria

Base of the Exenberg Nappe
definition: The NW-SE striking and SW-dipping base of the Exenberg Nappe extends from Stanz im Mürztal to just west of Rossegg. For most its extend, it corresponds also to the base of the Koralpe-Wölz Nappe System, except for short part west of the Lindkogel, where it is thrusted over the Radegund Nappe
definition: Die NW-SE streichende und nach SW eintauchende Basis der Exenberg-Decke ist zwischen Stanz im Mürztal und Rossegg aufgeschlossen. Größtenteils entspricht diese Deckenbasis der Basis des Koralpe-Wölz-Deckensystems, außer für einen kurzen Bereich westlich des Lindkogels, wo die Exenberg-Decke über die Radegund-Decke geschoben wurde. @de
type: Concept
notation: AT-51062
created: 2020-09-09T13:35:20.195Z
preferred label: Basis der Exenberg-Decke @de
references: https://data.geoscience.earth/ncl/geoera/ref/779
in scheme: Tectonic Boundary Objects in Europe
limit to: http://resource.geolba.ac.at/tectonicunit/392
type: Limit
broader: Nappe Boundary in Austria

Base of the Ultrahelvetic Units
definition: The base of the Ultrahelveticum can in Austria mainly be found in Vorarlberg between Feldkirch and Hirschegg, but also between Gresten and Texingtal in Lower Austria. The Ultrahelveticum was overthrust onto the Helveticum sensu stricto during the Oligocene and was itself integrated into the nappe structure by the later principal overthrust (out-of-sequence) of the Helvetic nappes (Froitzheim et al., 2008).
definition: Die Basis des Ultrahelvetikums ist in Österreich hauptsächlich in Vorarlberg zwischen Feldkirch und Hirschegg aufgeschlossen, aber auch zwischen Gresten und Texingtal in Niederösterreich. Das Ultrahelvetikum wird im Oligozän auf das Helvetikum s.str. überschoben und wird durch die spätere Hauptüberschiebung (out-of-sequence) der Helvetischen Decken selbst in den Deckenbau einbezogen (Froitzheim et al., 2008). @de
type: Concept
notation: AT-50555
preferred label: Basis des Ultrahelvetikums @de
notation: AT-50520
created: 2020-09-09T13:35:19.272Z
references: https://data.geoscience.earth/ncl/geoera/ref/1243
in scheme: Tectonic Boundary Objects in Europe
type: Limit
limit to: http://resource.geolba.ac.at/tectonicunit/84
broader: Nappe Boundary in Austria

Base of the Dachstein Nappe
references: https://data.geoscience.earth/ncl/geoera/ref/1244
definition: The base of the Dachstein Nappe of the Juvavic Nappe System crops out in the Ramsau area between Sulzbach and Untersee, and from east of Archkogel at the Lake Grundlsee to the Tauplitzalm.
created: 2020-09-09T13:35:20.223Z
preferred label: Basis der Dachstein-Decke @de
notation: AT-51063
type: Concept
definition: Die Basis der Dachstein-Decke des Juvavischen Deckensystem ist in der Ramsau zwischen Sulzbach und Untersee aufgeschlossen, sowie östlich von Archkogel am Grundlsee bis zur Tauplitzalm. @de
in scheme: Tectonic Boundary Objects in Europe
type: Limit
broader: Nappe Boundary in Austria

Base of the Gföhl Nappe System
definition: The base of the uppermost nappe system of the Moldanubian Nappes can in Austria be observed in Lower Austria, between Ybbs/Donau and Raabs/Thaya. The Gföhl Nappe System overthrusts the Drosendorf Nappe System and the Ostrong Nappe System.
definition: Die Basis des obersten Deckensystems des Moldanubikums ist in Österreich nur in Niederösterreich, zwischen Ybbs and der Donau und Raabs an der Thaya zu finden. Das Gföhl-Deckensystem überfährt an seiner Basis das Drosendorf-Deckensystem bzw. das Ostrong Deckensystem. @de
type: Concept
created: 2020-09-09T13:35:19.300Z
notation: AT-50532
notation: AT-50523
preferred label: Basis des Gföhl-Deckensystems @de
references: https://data.geoscience.earth/ncl/geoera/ref/1245
in scheme: Tectonic Boundary Objects in Europe
limit to: http://resource.geolba.ac.at/tectonicunit/103
type: Limit
broader: Nappe Boundary in Austria

Base of the Gstoder Nappe
references: https://data.geoscience.earth/ncl/geoera/ref/8704
references: https://data.geoscience.earth/ncl/geoera/ref/8703
references: https://data.geoscience.earth/ncl/geoera/ref/8710
definition: The emplacement the Gstoder Nappe, an upper nappe of the Koralpe-Wölz Nappe System, took place during the Eoalpine ogogenesis. Earlier shear zones are overprinted by later top-E-directed structures (Iglseder, 2019; Iglseder & Huet, 2019 and references therein; Rantitsch et al., 2020).
definition: Die Platznahme der Gstoder-Decke, eine der hangenden Decken des Koralpe-Wölz-Deckensystems, erfolgte während der eoalpidischen Gebirgsbildung. Dabei wurden frühere Scherzonen von späteren top-E-gerichteten Strukturen überprägt (Iglseder, 2019; Iglseder & Huet, 2019 und die darin aufgeführten Referenzen; Rantitsch et al., 2020). @de
type: Concept
notation: AT-51051
preferred label: Basis der Gstoder-Decke @de
created: 2020-09-09T13:35:20.054Z
in scheme: Tectonic Boundary Objects in Europe
type: Limit
broader: Nappe Boundary in Austria

Base of the Pusterwald Nappe
references: https://data.geoscience.earth/ncl/geoera/ref/8699
references: https://data.geoscience.earth/ncl/geoera/ref/8706
references: https://data.geoscience.earth/ncl/geoera/ref/8707
references: https://data.geoscience.earth/ncl/geoera/ref/8703
references: https://data.geoscience.earth/ncl/geoera/ref/8713
definition: The base of the Pusterwald Nappe, a lower nappe of the Koralpe-Wölz Nappe System is represented at map sheets of the Geological Survey of Austria (Metz, 1979; Moser, 2015; Ebner et al., 2017; Iglseder, 2019). The emplacement took place during the Eoalpine orogenesis.
definition: Die Basis der Pusterwald-Decke, einer liegenden Einheit des Koralpe-Wölz-Deckensystems ist teilweise auf Karten der Geologischen Bundesanstalt dargestellt (Metz, 1979; Moser, 2015; Ebner et al., 2017; Iglseder, 2019). Ihre Platznahme erfolgte während der eoalpidischen Gebirgsbildung (Schuster, 2015). @de
type: Concept
preferred label: Basis der Pusterwald-Decke @de
notation: AT-51054
created: 2020-09-09T13:35:20.082Z
in scheme: Tectonic Boundary Objects in Europe
type: Limit
broader: Nappe Boundary in Austria

Base of the Hochlantsch Nappe
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/8699
references: https://data.geoscience.earth/ncl/geoera/ref/8700
references: https://data.geoscience.earth/ncl/geoera/ref/8702
definition: The base of the Hochlantsch Nappe, an upper nappe of the Drauzug-Gurktal Nappe System is represented at map sheets of the Geological Survey of Austria (Flügel et al., 1990; Ebner et al., 2017). The emplacement took place during the Eoalpine orogenesis.
definition: Die Basis der Hochlantsch-Decke, einer hangenden Decke des Drauzug-Gurktal-Deckensystems ist teilweise auf Karten der Geologischen Bundesanstalt dargestellt (Flügel et al., 1990; Ebner et al., 2017). Ihre Platznahme erfolgte während der eoalpidischen Gebirgsbildung (Fritz, 1988). @de
notation: AT-51059
created: 2020-09-09T13:35:20.110Z
preferred label: Basis der Hochlantsch-Decke @de
in scheme: Tectonic Boundary Objects in Europe
type: Limit
limit to: http://resource.geolba.ac.at/tectonicunit/133
broader: Nappe Boundary in Austria

Base of the Schöckel Nappe
references: https://data.geoscience.earth/ncl/geoera/ref/8699
references: https://data.geoscience.earth/ncl/geoera/ref/8700
references: https://data.geoscience.earth/ncl/geoera/ref/8701
references: https://data.geoscience.earth/ncl/geoera/ref/8702
definition: The base of the Schöckel Nappe, an upper nappe of the Drauzug-Gurktal Nappe System is represented at map sheets of the Geological Survey of Austria (Flügel et al., 1990, 2011; Ebner et al., 2017). The emplacement took place during the Eoalpine orogenesis.
definition: Die Basis der Schöckel-Decke, einer hangenden Decke des Drauzug-Gurktal-Deckensystems ist teilweise auf Karten der Geologischen Bundesanstalt dargestellt (Flügel et al., 1990; Ebner et al., 2017). Ihre Platznahme erfolgte während der eoalpidischen Gebirgsbildung (Fritz, 1988). @de
type: Concept
created: 2020-09-09T13:35:20.140Z
notation: AT-51060
preferred label: Basis der Schöckel-Decke @de
in scheme: Tectonic Boundary Objects in Europe
limit to: http://resource.geolba.ac.at/tectonicunit/140
type: Limit
broader: Nappe Boundary in Austria

Base of the Stolzalpe Nappe
references: https://data.geoscience.earth/ncl/geoera/ref/8704
references: https://data.geoscience.earth/ncl/geoera/ref/8703
references: https://data.geoscience.earth/ncl/geoera/ref/8710
definition: The emplacement of the Stolzalpe Nappe of the Drauzug-Gurktal Nappe System took place during Cretaceous Eoalpine nappe stacking and shows WNW-directed kinematics. This was reactivated at ESE-directed normal faults, localized at the underlying Königstuhl- and Bundschuh nappes (Iglseder, 2019; Iglseder & Huet, 2019 and references therein; Rantitsch et al., 2020).
definition: Die Platznahme der Stolzalpe-Decke des Drauzug-Gurktal-Deckensystem erfolgte während der Eoalpidischen (kretazischen) Deckenstapelung als Überschiebungen mit WNW-gerichteter Bewegung. Diese wurde von ESE-gerichteten Abschiebungen, lokalisiert an der Deckengrenze zur Königstuhl- und Bundschuh-Decke, reaktiviert (Iglseder, 2019; Iglseder & Huet, 2019 und die darin aufgeführten Referenzen; Rantitsch et al., 2020). @de
created: 2020-09-09T13:35:19.944Z
preferred label: Basis der Stolzalpe-Decke @de
type: Concept
notation: AT-51044
in scheme: Tectonic Boundary Objects in Europe
limit to: http://resource.geolba.ac.at/tectonicunit/143
type: Limit
broader: Nappe Boundary in Austria

Base of the Helvetic Nappes
definition: In the Eastern Alps, the Helveticum sensu stricto (and its base) only occurs west of Salzburg. At about 30 Ma, the 'out-of-sequence' overthrusting of the Helvetic Nappes formed through the emplacement on the Infra-Helveticum and the Sub-Alpine Molasse, which continued into the Miocene (Pfiffner, 2009).
definition: In den Ostalpen kommt das Helvetikum sensu stricto, und damit auch dessen Basis, nur westlich von Salzburg vor. Um ca. 30 Ma bildeten sich die 'out-of-sequence'-Überschiebungen der Helvetischen Decken mit der Platznahme auf dem Infrahelvetikum und der Subalpinen Molasse, die bis ins Miozän andauerten (Pfiffner, 2009). @de
references: https://data.geoscience.earth/ncl/geoera/ref/1242
references: https://data.geoscience.earth/ncl/geoera/ref/1243
notation: AT-50556
type: Concept
created: 2020-09-09T13:35:19.020Z
preferred label: Basis des Helvetikums sensu stricto @de
notation: AT-50018
in scheme: Tectonic Boundary Objects in Europe
limit to: http://resource.geolba.ac.at/tectonicunit/63
type: Limit
broader: Nappe Boundary in Austria

Base of the Königstuhl Nappe
references: https://data.geoscience.earth/ncl/geoera/ref/8704
references: https://data.geoscience.earth/ncl/geoera/ref/8703
references: https://data.geoscience.earth/ncl/geoera/ref/8710
definition: The emplacement of the Königstuhl Nappe of the Drauzug-Gurktal Nappe System overthrusting the Ackerl, Murau, Pfannock and Bundschuh Nappes took place during Cretaceous Eoalpine nappe stacking with WNW-directed movement. Later normal-faulting with top ESE-directed kinematics overprinted these nappe boundaries (Iglseder, 2019; Iglseder & Huet, 2019 and references therein; Rantitsch et al., 2020).
definition: Die Platznahme der Königstuhl-Decke des Drauzug-Gurktal-Deckensystem, welche die Pfannock-, Ackerl-, Murau- sowie die Bundschuh-Decke überlagert, erfolgte während der eoalpidischen Gebirgsbildung. Die Deckengrenzen zeigen Überschiebungen mit top-WNW-gerichteter Kinematik, welche durch spätere ESE-gerichtete Abschiebungen überprägt werden (Iglseder, 2019; Iglseder & Huet, 2019 und die darin aufgeführten Referenzen; Rantitsch et al., 2020). @de
preferred label: Basis der Königstuhl-Decke @de
notation: AT-51045
type: Concept
created: 2020-09-09T13:35:19.971Z
in scheme: Tectonic Boundary Objects in Europe
type: Limit
broader: Nappe Boundary in Austria

Base of the Ackerl Nappe
references: https://data.geoscience.earth/ncl/geoera/ref/8704
references: https://data.geoscience.earth/ncl/geoera/ref/8703
references: https://data.geoscience.earth/ncl/geoera/ref/8710
definition: The base of the Ackerl Nappe of the Drauzug-Gurktal Nappe System overthrusting the Murau and Stolzalpe Nappes can be observed south of St. Lorenzen ob Murau and took place during Eoalpine orgenesis. Earlier NW-directed structures are overprinted by later top (E)SE-directed ones (Iglseder, 2019; Iglseder & Huet, 2019 and references therein; Rantitsch et al., 2020).
definition: Die Basis der Überschiebung der Ackerl-Decke des Drauzug-Gurktal-Deckensystem auf die Murau- und Stolzalpe Decken ist südlich St. Lorenzen ob Murau aufgeschlossen und wurde während der eoalpidischen Gebirgsbildung angelegt. Diese zeigen frühere NW-gerichtete Strukturen welche von späteren top-(E)SE-gerichteten überprägt werden (Iglseder, 2019; Iglseder & Huet, 2019 und die darin aufgeführten Referenzen; Rantitsch et al., 2020). @de
type: Concept
notation: AT-51046
created: 2020-09-09T13:35:19.999Z
preferred label: Basis der Ackerl-Decke @de
in scheme: Tectonic Boundary Objects in Europe
type: Limit
broader: Nappe Boundary in Austria

Base of the Murau Nappe
references: https://data.geoscience.earth/ncl/geoera/ref/8704
references: https://data.geoscience.earth/ncl/geoera/ref/8703
references: https://data.geoscience.earth/ncl/geoera/ref/8710
definition: The base of the Murau Nappe of the Drauzug-Gurktal Nappe System overthrusting basal nappes of the Drauzug-Gurktal Nappe System as well as nappes of the Koralpe-Wölz and Ötztal-Bundschuh Nappe Systems was activated during Eoalpine nappe stacking with partly top-W-directed kinematics. Later structures with top-E-directed shearing overprint this boundary (Iglseder, 2019; Iglseder & Huet, 2019 and references therein; Rantitsch et al., 2020).
definition: Die Basis der Überschiebung der Murau-Decke des Drauzug-Gurktal-Deckensystem auf basale Decken des Drauzug-Gurktal-Deckensystems, sowie das Koralpe-Wölz- und Ötztal-Bundschuh-Deckensystem wurde während der eoalpidischen Deckenstapelung angelegt und zeigt teilweise top-W-gerichtete Kinematik. Dies wurden von späteren Strukturen mit top-E-gerichteter Scherung überprägt (Iglseder, 2019; Iglseder & Huet, 2019 und die darin aufgeführten Referenzen; Rantitsch et al., 2020). @de
type: Concept
created: 2020-09-09T13:35:20.027Z
notation: AT-51048
preferred label: Basis der Murau-Decke @de
in scheme: Tectonic Boundary Objects in Europe
type: Limit
broader: Nappe Boundary in Austria

Base of the Stuhleck-Kirchberg Nappe
references: https://data.geoscience.earth/ncl/geoera/ref/779
definition: On the western side of the Wechselfenster, the Stuhleck-Kirchberg Nappe features a Cretaceous contact dipping gently towards west on top of the Vorau Nappe (Silvretta-Seckau Nappe System) and Wechsel Nappe (Lower Austroalpine Nappes). Similar situation can be spotted on the western side of the Wiesmath Fenster where the contact zone inclines WSW. The formation of the base of the Stuhleck-Kirchberg Nappe next to the Rechnitzer Fenster group (part of the Penninic Nappe) was originated during Miocene by steeply ENE dipping normal faults.
definition: An der Westseite des Wechselfensters zeigt die Stuhleck-Kirchberg-Decke einen flach gegen Westen fallenden kretazischen Kontakt zur unterlagernden Vorau-Decke des Silvretta-Seckau-Deckensystems und zur Wechsel-Decke des Unterostalpins. Auch an der Westseite des Wiesmather Fensters ist eine flach, WSW fallende kretazische Deckengrenze erhalten. Die Deckengrenzen gegenüber den Penninischen Decken im Bereich der Rechnitzer Fenstergruppe und Begrenzungen, die durch steilstehende, oft gegen ENE einfallende Abschiebungen gebildet werden, entstanden im Miozän. @de
created: 2020-09-09T13:35:19.888Z
notation: AT-51038
type: Concept
preferred label: Basis der Stuhleck-Kirchberg-Decke @de
in scheme: Tectonic Boundary Objects in Europe
limit to: http://resource.geolba.ac.at/tectonicunit/162
type: Limit
broader: Nappe Boundary in Austria

Base of the Sieggraben Nappe
definition: The emplacement of the Sieggraben Nappe took place in the Upper Cretaceous and is caused by a NE-dipping thrust fault. The remnants of the thrust fault are exposed between Pinkafeld and Mattersburg, east of the area of the Hochwechsel and at the eastern margin of the Bucklige Welt. The primary contact has been reworked by younger faults.
definition: Die Platznahme der Sieggraben-Decke erfolgte an einer NE gerichteten Überschiebung in der Oberkreide. Die heute noch erhaltenen Teile der Überschiebung finden sich zwischen Pinkafeld und Mattersburg östlich des Hochwechsels bzw. am östlichen Rand der Buckligen Welt. Die primären Kontakte sind lokal durch steilstehende jüngere Störungen überprägt. @de
preferred label: Basis der Sieggraben-Decke @de
type: Concept
notation: AT-51039
created: 2020-09-09T13:35:19.916Z
references: https://data.geoscience.earth/ncl/geoera/ref/779
in scheme: Tectonic Boundary Objects in Europe
limit to: http://resource.geolba.ac.at/tectonicunit/173
type: Limit
broader: Nappe Boundary in Austria

Base of the Frankenfels Nappe
references: https://data.geoscience.earth/ncl/geoera/ref/1244
definition: The base of the Frankenfels Nappe of the Bajuvaric Nappe System can be observed between Maria Neustift in the north and St. Gallen in the south.
definition: Die Basis der Frankenfels-Decke des Bajuvarischen Deckensystems ist zwischen Maria Neustift und St. Gallen im Süden beobachten. @de
notation: AT-51035
type: Concept
created: 2020-09-09T13:35:19.860Z
preferred label: Basis der Frankenfels-Decke @de
in scheme: Tectonic Boundary Objects in Europe
type: Limit
broader: Nappe Boundary in Austria

Base of the Laab Nappe
references: https://data.geoscience.earth/ncl/geoera/ref/8711
definition: The base of this unit of the Rhenodanubic Nappe System in the Wienerwald can be observed in the area of Wöllersdorf.
definition: Diese tektonische Einheit des Rhenodanubikums kann bei Wöllersdorf beobachtet werden. @de
preferred label: Basis der Laab-Decke @de
notation: AT-51016
type: Concept
created: 2020-09-09T13:35:19.749Z
in scheme: Tectonic Boundary Objects in Europe
type: Limit
broader: Nappe Boundary in Austria

Base of the Hallstatt Nappe
references: https://data.geoscience.earth/ncl/geoera/ref/1244
definition: The base of the Hallstatt Nappe of the Juvavic Nappe System can be observed west of Lake Hallstatt and east of Johnsbach.
definition: Die Basis der Hallstatt-Decke des Juvavischen Deckensystems kann westlich vom Hallstätter See und östlich von Johnsbach beobachtet werden. @de
type: Concept
notation: AT-51064
preferred label: Basis der Hallstatt-Decke @de
created: 2020-09-09T13:35:19.777Z
notation: AT-51018
in scheme: Tectonic Boundary Objects in Europe
type: Limit
broader: Nappe Boundary in Austria

Base of the Greifenstein Nappe
references: https://data.geoscience.earth/ncl/geoera/ref/8711
definition: This nappe of the Rhenodanubian Nappe System is the dominating tectonic unit of the Flysch Zone in Lower Austria and the Wienerwald. The base of the Greifenstein Nappe can be observed between Kettenreith in the southwest and St. Andrä-Wördern in the northeast.
definition: Diese Decke des Rhenodanubikums ist die dominierende tektonische Einheit in der Flyschzone Niederösterreichs bzw. des Wienerwaldes. Die Basis der Greifenstein-Decke kann zwischen Kettenreith im Südwesten und St. Andrä-Wördern im Nordosten beobachtet werden. @de
preferred label: Basis der Greifenstein-Decke @de
notation: AT-51023
type: Concept
created: 2020-09-09T13:35:19.804Z
in scheme: Tectonic Boundary Objects in Europe
type: Limit
broader: Nappe Boundary in Austria

Base of the Göller Nappe
references: https://data.geoscience.earth/ncl/geoera/ref/1244
definition: The base of the Göller Nappe is a subhorizontal S-dipping thrust fault that stretches from the Salza Valley in the SW via Lake Erlauf (north of Mariazell) across the Vienna Basin in the NE. Just West of the Vienna Basin, it conincides with the nappe boundary between the hanging Tirolic-Noric Nappe System and its footwall, the Bajuvaric Nappe System
definition: Die Basis der Göllerdecke ist eine subhorizontale, nach S einfallende Überschiebung, die vom Salzatal im SW über den Erlaufsee (N von Mariazell) bis zum Untergrund des Wiener Beckens verläuft. Westlich des Wiener Beckens entspricht die Basis der Göller-Decke auch der Deckengrenze zwischen dem hangenden Tirolisch-Norischen und dem liegenden Bajuvarischen Deckensystem. @de
notation: AT-51032
created: 2020-09-09T13:35:19.832Z
type: Concept
preferred label: Basis der Göller-Decke @de
references: https://data.geoscience.earth/ncl/geoera/ref/779
in scheme: Tectonic Boundary Objects in Europe
type: Limit
limit to: http://resource.geolba.ac.at/tectonicunit/201
broader: Nappe Boundary in Austria

Base of the Unterberg Nappe
definition: The base of the Unterberg Nappe is a subhorizontal, S-dipping thrust fault that stretches from the village of Mooslandl in the Enns River Valley in the SW to Altenmark an der Triesting in the NE.
definition: Die Basis der Unterberg-Decke ist eine subhorizontale, nach S einfallende Überschiebung, die von Mooslandl im Ennstal im SW bis Altenmark an der Triesting im NE verfolgbar ist. @de
type: Concept
created: 2020-09-09T13:35:19.637Z
notation: AT-51003
preferred label: Basis der Unterberg-Decke @de
references: https://data.geoscience.earth/ncl/geoera/ref/1249
in scheme: Tectonic Boundary Objects in Europe
limit to: http://resource.geolba.ac.at/tectonicunit/208
type: Limit
broader: Nappe Boundary in Austria

Base of the Schneeberg Nappe
definition: This Juvavic nappe and its base can be observed in the area of the Schneeberg between Gußwerk and Naßwald.
definition: Diese Juvavische Decke, sowie ihre Basis sind im Schneeberggebiet zwischen Gußwerk und Naßwald zu finden. @de
type: Concept
preferred label: Basis der Schneeberg-Decke @de
notation: AT-51008
created: 2020-09-09T13:35:19.665Z
in scheme: Tectonic Boundary Objects in Europe
limit to: http://resource.geolba.ac.at/tectonicunit/155
type: Limit
broader: Nappe Boundary in Austria

Base of the Reisalpe Nappe
definition: The base of the Reisalpe Nappe of the Tirolic-Noric Nappe System is a subhorizontal S-dipping thrust fault that stretches from Lake Lunz in the SW to Pankraziberg in the NE. In large parts, it conincides with the nappe boundary between the hanging Tirolic-Noric Nappe System and its footwall, the Bajuvaric Nappe System
definition: Die Basis der Reisalpe-Decke des Tirolisch-Norischen Deckensystems ist eine subhorizontal nach S einfallende Überschiebung, die vom Lunzer See im SW bis Pankraziberg im NE verfolgbar ist. In großen Teilen entspricht sie der Deckengrenze zwischen dem hangenden Tirolisch-Norischen und dem liegenden Bajuvarischen Deckensystem. @de
preferred label: Basis der Reisalpe-Decke @de
created: 2020-09-09T13:35:19.694Z
notation: AT-51010
type: Concept
in scheme: Tectonic Boundary Objects in Europe
limit to: http://resource.geolba.ac.at/tectonicunit/204
type: Limit
broader: Nappe Boundary in Austria

Base of the Lunz Nappe
references: https://data.geoscience.earth/ncl/geoera/ref/1244
definition: This Bajuvaric nappe and its base can be observed southwest of Vienna in the area the Föhrenberge nature park south of Kaltenleutgeben.
definition: Diese Bajuvarische Decke und ihre Basis ist im Südwesten von Wien Naturpark Föhrenberge südlich von Kaltenleutgeben zu beobachten. @de
type: Concept
preferred label: Basis der Lunz-Decke @de
created: 2020-09-09T13:35:19.721Z
notation: AT-51015
in scheme: Tectonic Boundary Objects in Europe
type: Limit
broader: Nappe Boundary in Austria

Base of the Veitsch-Silbersberg Nappe System
references: https://data.geoscience.earth/ncl/geoera/ref/8712
references: https://data.geoscience.earth/ncl/geoera/ref/8708
definition: This nappe system comprises the lowermost nappes of the Greywacke Zone Nappe System, overthrusting the Silvretta-Seckau Nappe System at its base, which only crops out in the area of Großstübing and Deutschfeistritz. (Neubauer, 1994).
definition: Dieses Deckensystem umfasst die untersten Decken der Grauwackenzone, es überschiebt an seiner Basis, welche nur um Großstübing und Deutschfeistritz aufgeschlossen ist, das Silvretta-Seckau-Deckensystem (Neubauer, 1994; Schuster, 2015). @de
type: Concept
preferred label: Basis des Veitsch-Silbersberg-Deckensystems @de
notation: AT-50584
created: 2020-09-09T13:35:19.610Z
in scheme: Tectonic Boundary Objects in Europe
type: Limit
broader: Nappe Boundary in Austria

West Molasse Fault Set
definition: This fault set consists of faults within the Austrian part of the Lower Bavarian - Upper Austria Molasse Basin between Salzburg in the west and Melk in the east. It is bound by the outcropping crystalline rock suites of the Bohemian Massif to the north and northeast, and the Alpine Thrust front to the south. All faults within the basin are blind faults, active until Badenian of mid-Miocene at the latest, solely evidenced by seismic surveys and drillings. (Kröll et al., 2001; Wagner, 1998)
definition: Dieses Störungset besteht aus Störungen des österreichischen Teils des Unterbayrisch-oberösterreichischen Mollassebeckens zwischen Salzburg im Westen und Melk im Osten. Es wird im Norden und Nordosten von Kristallingesteinen der Böhmischen Masse begrenzt und von der Alpinen Überschiebungsfront im Süden. Alle Brüche innerhalb des Beckens sind blinde Störungen, die längstens bis ins Baden des Mittleren Miozäns aktiv waren, und die nur mittels Seismik und Bohrungen nachgewiesen wurden. (Kröll et al., 2001; Wagner, 1998) @de
references: https://data.geoscience.earth/ncl/geoera/ref/728
references: https://data.geoscience.earth/ncl/geoera/ref/750
narrower: Deggendorf-Ried Faultsystem
notation: AT-564
narrower: Altheim Fault
narrower: Aspach Fault
narrower: Fornach Fault
narrower: Geinberg-Simbach Fault
narrower: Mauerkirchen Fault
narrower: Nonsbach Fault
narrower: Roith Fault
narrower: Steindlberg Fault
type: Concept
created: 2020-04-30T14:27:02.847Z
preferred label: Westliche Molasse Störungsset @de
narrower: Landshut-Neuötting Fault System
narrower: Aselkam Fault
narrower: Pfarrkirchen Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Roith Fault
type: Fault
type: Limit
type: SpatialObject
sf touches: Aspach Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4082
definition: Überdeckte, E-W streichende, steil N-fallende Störung an der Basis des Molassebeckens, Zweig der Aspach Störung [AT_10662], der sich im Osten bis nach Pudexing (AT) zieht. @de
sf touches: Fornach Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4098
created: 2020-09-09T13:25:50.721Z
notation: AT-10659
definition: This E-W striking, steeply N-dipping blind fault at the bottom of the Molasse Basin represents a branch of the Aspach Fault [AT-10662] and terminates to the east near Pudexing (AT).
preferred label: Roith-Störung @de
type: Concept
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Aspach Fault
broader: West Molasse Fault Set

Aselkam Fault
type: Limit
type: Fault
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4082
definition: Überdeckte E-W streichende, steil nach N einfallende Störung an der Basis des Molassebeckens als Zweig der Altheim Störung [AT-10661] der sich bis östlich von Braunau (AT) zieht @de
sf touches: Altheim Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4098
created: 2020-09-09T13:25:50.749Z
notation: AT-10660
preferred label: Aselkam-Störung @de
definition: This E-W striking, steeply N-dipping blind fault at the bottom of the Molasse Basin represents a branch of the Altheim Fault [AT-10661] and terminates to the east in the city of Braunau (AT).
type: Concept
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Altheim Fault
broader: West Molasse Fault Set

Altheim Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4082
definition: W-E striking, vertical to steeply S-dipping blind normal fault at the bottom of the Molasse Basin representing the northern branch of the Nonsbach Fault [AT-10657] and terminating to the east of the city of Braunau (AT). Target of Simbach-Braunau geothermal development
definition: Überdeckte, W-E streichende, vertikale bis steil S-fallende Abschiebung an der Basis des Molassebeckens als Nord-Ast der Nonsbach Störung [AT_10657] der sich bis östlich von Braunau (AT) zieht. Ziel des Simbach-Braunau Geothermie-Vorhabens. @de
narrower: Aselkam Fault
sf touches: Aselkam Fault
sf touches: Nonsbach Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4098
preferred label: Altheim-Störung @de
type: Concept
created: 2020-09-09T13:25:50.778Z
notation: AT-10661
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: West Molasse Fault Set
broader: Lower Bavaria - Upper Austria Molasse Basin fault domain

Aspach Fault
type: Limit
type: Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4082
type: SpatialObject
sf touches: Fornach Fault
definition: Überdeckte ENE-WSW streichende, N-fallende Störung an der Basis des Molassebeckens die sich im Osten bis zum Deggendorf-Ried Störungssystem [DE-BY_929] bei Mehrnbach (AT), im Westen bis zum Landshut-Neuötting Abbruch zieht. @de
sf touches: Ried Fault
sf touches: Handenberg Fault
sf touches: Mauerkirchen Fault
sf touches: Roith Fault
alternative label: Aspach Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/4098
definition: This ENE-WSW striking, N-dipping blind fault at the bottom of the Molasse Basin terminates in the east at the Deggendorf-Ried Fault close to Mehrnbach (AT) and in the west at the Landshut-Neuötting Fault System.
preferred label: Aspach-Störung @de
created: 2020-09-09T13:25:50.808Z
type: Concept
notation: AT-10662
narrower: Roith Fault
definition: This ENE-WSW striking, N-dipping blind fault at the bottom of the Molasse Basin terminates in the east at the Deggendorf-Ried Fault System [DE-BY_929] close to Mehrnbach (AT) and in the west at the Landshut-Neuötting Step Fault.
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Lower Bavaria - Upper Austria Molasse Basin fault domain
broader: West Molasse Fault Set

Landshut-Neuötting Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/772
references: https://data.geoscience.earth/ncl/geoera/ref/789
references: https://data.geoscience.earth/ncl/geoera/ref/821
narrower: Mehring-Seeham Fault
notation: AT-125
narrower: Eggelsbach Fault
narrower: Handenberg Fault
narrower: Grasset-Wechselberg Fault
type: Concept
created: 2020-04-30T14:27:02.902Z
definition: This fault system comprises the NW-SE striking faults, which limit the Landshut-Neuöttinger Hoch. They can be traced from Landshut (D) via Neuötting (D) and Burghausen to the northern rim of the Alps near Michaelbeuren, Perwang and Berndorf north of Salzburg. (Buchroithner, 1984; Unger & Schwarzmeier, 1982; Scheck-Wenderoth et al., 2008)
definition: Dieses Störungssystem umfasst die NW-SE streichenden Störungen, die das Landshut-Neuöttinger Hoch begrenzen und lassen sich von Landshut (D) über Neuötting (D) und Burghausen bis zum Alpennordrand bei Michaelbeuren, Perwang und Berndorf nördlich von Salzburg verfolgen. (Buchroithner, 1984; Unger & Schwarzmeier, 1982; Scheck-Wenderoth et al., 2008) @de
preferred label: Landshut-Neuötting-Störungssystem @de
in scheme: Tectonic Boundary Objects in Europe
related: Landshut-Neuötting Step Fault
broader: West Molasse Fault Set

Mehring-Seeham Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:34.245Z
notation: DE-BY_1225
preferred label: Mehring-Seeham Störung @de
definition: Southwestern branch of the continuation of Landshut-Neuötting Fault Scarp 2 [DE-BY_702], branching off Eggelsbach Fault [AT_10663] just north of the Austrian border. NW-SE trending, on average approx. 75° SW dipping normal fault forming an intermediate step SW of Fault Scarp 2 along the Central Swell Zone in Austria.
definition: Als Abzweig der Landshut-Neuötting Abbruchstufe 2 [DE-BY_702] wenig nördlich der österreichischen Grenze, zieht sich diese NW-SE verlaufende, im Mittel ca. 75° nach SW einfallende Abschiebung, unter Bildung einer Zwischenstufe SW vor der Abbruchstufe 2, entlang der Zentralen Schwellenzone bis zum Obertrumer See. @de
sf touches: Eggelsbach Fault
type: SpatialObject
notation: AT-10666
references: https://data.geoscience.earth/ncl/geoera/ref/4082
sf touches: Landshut-Neuötting Fault Scarp 2
sf touches: Grasset-Wechselberg Fault
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
notation: LfU-BY_1225
limit type: normalFault
broader: Landshut-Neuötting Step Fault
broader: Landshut-Neuötting Fault System

Grasset-Wechselberg Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:34.217Z
notation: DE-BY_1224
alternative label: Landshut-Neuötting Abbruchstufe 4 @de
preferred label: Grasset-Wechselberg Störung @de
definition: Running from south of Altötting into Austrian territory, southwestward arcuate, NW-SE trending, approx. 75° NE dipping reverse fault featuring a cumulative throw of up to 450 m. Southwestern boundary of the protrusion of the lower step of Landshut-Neuötting Rise overthrusting the southern part of Gifthal Trough.
definition: Südwestwärts gebogene, NW-SE verlaufende, ca. 75° nach NE einfallende Haupt-Aufschiebung (begleitet von kleineren Aufschiebungen) mit einem kumulativen Versatz von bis zu 450 m, die sich von südlich Altötting bis nach Franking in Österreich zieht. Südwestgrenze des Vorsprungs der unteren Stufe des Landshut-Neuötting Abbruchs, der die südlichen Ausläufer des Gifthal Trogs überfahren hat. @de
type: SpatialObject
notation: AT-10667
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4082
sf touches: Mehring-Seeham Fault
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11681
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11689
notation: LfU-BY_1224
limit type: reverseFault
broader: Landshut-Neuötting Fault System
broader: Landshut-Neuötting Step Fault

Handenberg Fault
type: Fault
type: Limit
sf touches: Ried Fault
sf touches: Fornach Fault
sf touches: Steindlberg Fault
sf touches: Landshut-Neuötting Main Scarp
definition: Südöstliche Fortsetzung des Landshut-Neuötting Hauptabbruchs [DE-BY_701]. Steil nach SW einfallende Abschiebung die als überdeckte Störung an der Basis des Molassebeckens von nördlich Burghausen (DE) südost- bis ostwärts bis zur Ried Störung [AT_10665] westlich von Neukirchen an der Vöckla (AT) verläuft. @de
type: SpatialObject
sf touches: Aspach Fault
sf touches: Mauerkirchen Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4098
scope note: This SW-dipping blind fault at the bottom of the Molasse Basin marks the northeastern border of the Landshut-Neuötting Fault System and can be traced from north of Burghausen (D) towards SE until the west of Neukirchen an der Vöckla (AT), where it terminates at the Deggendorf-Ried Fault
scope note: Diese nach SW einfallende blinde Störung an der Molassebasis markiert die nordöstliche Grenze des Landshut-Neuötting Störungsystems, und kann von nördich von Burghausen (D) nach SE hin bis westlich von Neukirchen and er Vöckla (AT) verfolgt werden, wo es von der Deggendorf-Ried-Störung abgeschnitten wird. @de
type: Concept
created: 2020-09-09T13:24:10.389Z
preferred label: Handenberg Störung @de
definition: Southeastern continuation of Landshut-Neuötting Main Scarp [DE-BY_701] this steeply SW-dipping blind fault at the bottom of the Molasse Basin can be traced from north of Burghausen (DE) towards SE until the west of Neukirchen an der Vöckla (AT), where it terminates at the Ried Fault [AT_10665].
notation: AT-10655
references: https://data.geoscience.earth/ncl/geoera/ref/4082
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Landshut-Neuötting Fault System
broader: Landshut-Neuötting Step Fault

Eggelsbach Fault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/4082
sf touches: Mehring-Seeham Fault
definition: Northeastern branch of the continuation of Landshut-Neuötting Fault Scarp 2 [DE-BY_702], this SW-dipping blind fault at the bottom of the Molasse Basin runs through Burghausen (DE) towards SE via Perwang am Grabensee (AT) and Neumarkt am Wallersee (AT) and terminates at lake Irrsee.
sf touches: Landshut-Neuötting Fault Scarp 2
definition: Als nordöstlicher Ast der Fortsetzung der Landshut-Neuötting Abbruchstufe 2 [DE-BY_702], verläuft diese überdeckte, im Mittel ca. 75° nach SW einfallende synthetische Abschiebung an der Basis des Molassebeckens von Mehring NW Burghausen (DE) südostwärts via Perwang am Grabensee (AT) und Neumarkt am Wallersee (AT) bis zum Irrsee. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4098
scope note: This SW-dipping blind fault at the bottom of the Molasse Basin runs through Burghausen (D) towards SE via Perwang am Grabensee (AT) and Neumarkt am Wallersee (AT) and terminates at lake Irrsee.
scope note: Die nach SW einfallende blinde Störung an der Basis des Molassebeckens verläuft durch Burghausen (D) in Richtung SE über Perwang am Grabensee (AT) und Neumarkt am Wallersee (AT) und endet am Irrsee. @de
type: Concept
preferred label: Eggelsbach Störung @de
created: 2020-09-09T13:24:10.417Z
notation: AT-10663
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Landshut-Neuötting Step Fault
broader: Landshut-Neuötting Fault System

Geinberg-Simbach Fault
type: Fault
type: Limit
type: SpatialObject
alternative label: Geinberg-Simbach Störung @de
definition: Überdeckte, E-W streichende, ca. 70° nach N einfallende Abschiebung an der Basis des Molassebeckens zwischen N von Geinberg (AT) und Bertenöd NE Simbach (DE); quert den Inn (Deutsch-Österreichische Grenze) bei Mining (AT). Ziel des Geothermie-Vorhabens Geinberg @de
references: https://data.geoscience.earth/ncl/geoera/ref/4082
definition: W-E striking, approx. 70° N dipping blind normal fault at the bottom of the Molasse Basin is located to the north of Geinberg (AT) and northeast of Simbach (DE) and crossing the Inn River (Austria-German border) at Mining (AT). Target of Geinberg geothermal development.
references: https://data.geoscience.earth/ncl/geoera/ref/4098
notation: AT-10658
preferred label: Geinberg-Simbach-Störung @de
type: Concept
created: 2020-09-09T13:25:50.693Z
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
notation: LfU-BY_10658
limit type: normalFault
broader: West Molasse Fault Set
broader: Lower Bavaria - Upper Austria Molasse Basin fault domain

Fornach Fault
type: Fault
type: Limit
type: SpatialObject
sf touches: Aspach Fault
sf touches: Roith Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4082
sf touches: Steindlberg Fault
sf touches: Ried Fault
alternative label: Fornach Störung @de
type: Concept
notation: AT-10656
preferred label: Fornach-Störung @de
created: 2020-09-09T13:25:50.636Z
definition: This SE-NW striking, steeply NE dipping blind fault at the bottom of the Molasse Basin terminates in the SE at the Landshut-Neuötting fault System close to Fornach (AT) and towards the NE near the town of Wagham (AT)
definition: Diese SE-NW-streichende, steil nach NE einfallende blinde Störung an der Basis des Molassebeckens verläuft von SE, wo sie vom Landshut-Neuötting-Störungssystem nahe Fornach (AT) abgeschnitten wird, Richtung NE nahe Wagham (AT) @de
references: https://data.geoscience.earth/ncl/geoera/ref/4099
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: West Molasse Fault Set
broader: Lower Bavaria - Upper Austria Molasse Basin fault domain

Deggendorf-Ried Faultsystem
type: Limit
type: Fault
references: https://data.geoscience.earth/ncl/geoera/ref/753
notation: AT-10444
references: https://data.geoscience.earth/ncl/geoera/ref/4151
references: https://data.geoscience.earth/ncl/geoera/ref/824
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4099
references: https://data.geoscience.earth/ncl/geoera/ref/7269
definition: Branching off southwardly from Danube Fault Scarp [DE-BY_698], a N-S to NW-SE trending fault system of approx. 70° to 80° W to SW dipping normal faults runs from Deggendorf to Ried in Upper Austria the subsurface of the Alpine Molasse Eastern boundary of the Molasse Basin towards the Aidenbach-Griesbach Rise (resp. the Osterhofen pre-rise) featuring a thin sequence of fluviatile Molasse sediments only. The NNE-SSW striking fault runs at subsurface from Deggendorf (D) via Ried im Innkreis towards the Attersee. It is only confirmed by seismic and borehole data. (Freudenberger & Schwerd, 1996; Kröll et al., 2006)
references: https://data.geoscience.earth/ncl/geoera/ref/4082
definition: Südlicher Abzweig vom Donaurandbruch [DE-BY_698], N-S bis NW-SE verlaufendes System, ca. 70° bis 80° nach W bis SW einfallender Abschiebungen zwischen Deggendorf und Ried in Oberösterreich. Östliche Grenze des Molassebeckens zum Aidenbach-Griesbach Hoch hin (bzw. zur Osterhofen Vorstufe), das nur geringermächtige fluviatile Molassesedimente aufweist. Dieses NNE-SSW streichende, im Molasseuntergrund von Deggendorf (D) über Ried im Innkreis bis zum Attersee verlaufende Störungssystem ist nur durch Seismik- und Bohrlochdaten belegt. (Freudenberger & Schwerd, 1996; Kröll et al. 2006) @de
type: Concept
created: 2020-10-09T11:35:35.535Z
scope note: The tectonic boundaries of the Deggendorf-Ried Faultsystem largely are blind faults 3D modelled based on evidence of seismic and gravity surveys and deep drillings. The concepts refer to the fault traces at the top surface of Upper Jurassic carbonate sequence (restricted to the hanging wall in large areas), one of the principal reflectors in seismic surveys. Tectonic boundaries featuring throws of less than approximately 10 m, likewise soft links between faults, like relay ramps or horsetail splays, commonly are subseismic in legacy surveys and detectable only in novel 3D-seismics, so far not carried out in the area. The inventory, thus, cannot be complete with respect to these features, reflects the state of knowledge as of 2020 and is subject to future amendments.
scope note: Die tektonischen Grenzflächen des Deggendorf-Ried Störungssystem sind größtenteils überdeckte Störungen, die im 3D-Modell aus seismischen und Schwere-Messungen sowie Bohrungsbelegen abgeleitet wurden. Die Konzepte der tiefliegenden Störungen beziehen sich auf die im 3D-Modell ermittelten Schnittspuren an der Oberfläche der Liegendscholle, d.h. der Weißjura Karbonat-Abfolge, wobei dessen Vorkommen oft auf die Tiefscholle beschränkt ist. Tektonische Grenzflächen mit Sprunghöhen von weniger als ca. 10 m, oder Übergänge zwischen Störungen wie Akkomodationszonen (relay ramps) oder Auffiederungen (horsetail splays), sind in älteren seismischen Erkundungen gemeinhin nicht erkennbar (subseismisch) und nur in moderner, im Gebiet bisher nicht durchgeführter 3D-Seismik identifizierbar. Dementsprechend bleibt die Zusammenstellung, Stand 2020, im Hinblick auf solche Phänomene unvollständig und ist Gegenstand künftiger Fortschreibungen. @de
notation: DE-BY_929
preferred label: Deggendorf-Ried Störungssystem @de
narrower: Aidenbach-Griesbach Step Fault
narrower: Osterhofen Frontal Scarp
narrower: Pocking Step Fault
narrower: Birnbach-Füssing Step Fault
narrower: Ried Fault
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11682
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11749
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11855
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11889
notation: LfU-BY_929
limit type: normalFault
broader: Lower Bavaria - Upper Austria Molasse Basin Eastern Margin Fault Systems
broader: West Molasse Fault Set

Pocking Step Fault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/789
references: https://data.geoscience.earth/ncl/geoera/ref/4082
references: https://data.geoscience.earth/ncl/geoera/ref/4119
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:35.645Z
notation: DE-BY_699
preferred label: Pockinger Abbruch @de
definition: Northeastern branch of southern continuation of the Aidenbach-Griesbach Step Fault. Blind, undulate NW-SE trending, approx. 80° SW dipping multiphase normal fault featuring a throw of up to 1 km.
definition: Nordöstlicher Zweig der südlichen Fortsetzung des Aidenbach-Griesbach Abbruchs. NW-SO verlaufende, ca. 80° nach SW einfallende mehrphasige Abschiebung mit einer Sprunghöhe von bis zu 1 km. @de
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
notation: LfU-BY_699
limit type: normalFault
broader: Deggendorf-Ried Faultsystem

Osterhofen Frontal Scarp
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4082
sf touches: Aidenbach-Griesbach Step Fault
sf touches: Winklarn-Pörndorf Subfault
type: Concept
created: 2020-10-09T11:35:35.590Z
notation: DE-BY_1241
preferred label: Osterhofener Abbruch @de
definition: N-S to NNW-SSE trending, approx. 70° ± W dipping normal fault, side branch of Aidenbach-Griesbach Step Fault representing the western boundary of the Osterhofen prestage of the Aidenbach-Griesbach Rise.
definition: N-S to NNW-SSE verlaufende, ca. 70° nach ± W einfallende Abschiebung. Seitenast des Aidenbach-Griesbach Abbruchs und westliche Begrenzung der Osterhofen Vorstufe zum Aidenbach-Griesbach Hoch. @de
narrower: Winklarn-Pörndorf Subfault
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11684
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11749
notation: LfU-BY_1241
limit type: normalFault
broader: Deggendorf-Ried Faultsystem

Winklarn-Pörndorf Subfault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4082
type: Concept
created: 2020-10-09T11:35:35.618Z
notation: DE-BY_1242
preferred label: Winklarn-Pörndorf Nebenstörung @de
definition: NNW-SSE trending, approx. 80° WSW dipping synthetic normal fault; branch of Osterhofen Frontal Scarp [DE-BY_1241].
definition: NNW-SSO verlaufende, ca. 80° nach WSW einfallende synthetische Abschiebung, Zweig des Osterhofen Abbruchs [DE-BY_1241]. @de
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11684
notation: LfU-BY_1242
limit type: normalFault
broader: Osterhofen Frontal Scarp

Aidenbach-Griesbach Step Fault
type: Fault
type: Limit
sf touches: Birnbach-Füssing Step Fault
sf touches: Flintsbach Fault
sf touches: Flintsbach-Pleinting Fault
sf touches: Osterhofen Frontal Scarp
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4151
references: https://data.geoscience.earth/ncl/geoera/ref/4082
references: https://data.geoscience.earth/ncl/geoera/ref/4074
narrower: Brand-Dobelwiese Fault
narrower: Flintsbach Fault
narrower: Flintsbach-Pleinting Fault
type: Concept
created: 2020-10-09T11:35:35.562Z
notation: DE-BY_764
alternative label: Schwaimer Abbruch @de
preferred label: Aidenbach-Griesbach Abbruch @de
definition: Northern section of Deggendorf-Ried Fault System, linked by a relay structure to the Pocking Step Fault [DE-BY_669] in the south. Blind N-S to NNW-SSE trending, on average approx. 80° W to WSW dipping, multiphase normal fault, in large parts step fault, featuring a cumulative throw of up to more than 1 km.
definition: Nördlicher Abschnitt des Deggendorf-Ried Störungssystems, im Süden durch eine Relay-Struktur mit dem Pockinger Abbruch [DE-BY_669] verbunden. Nicht aufgeschlossene N-S bis NNW-SSO verlaufende, im Durchschnitt ca. 80° nach W bis WSW einfallende, großteils gestaffelte, mehrphasige Abschiebung mit einer kumulativen Sprunghöhe bis über 1 km. @de
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
notation: LfU-BY_764
limit type: normalFault
broader: Deggendorf-Ried Faultsystem

Brand-Dobelwiese Fault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/4107
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
definition: Displacing Paleo-Donaurand Fault Scarp [DE-BY_1237], SW-NE striking, steeply NW dipping double normal fault, southeastern border of the Flintsbach Jurassic carbonates trough-like embayment into the marginal Bohemian Massif crystalline rock suites.
created: 2020-10-09T11:35:35.339Z
notation: DE-BY_1239
preferred label: Brand-Dobelwiese Störung @de
definition: SW-NE streichende, steil nach NW einfallende Doppel-Abschiebung als südöstliche Grenze der Flintsbacher Jurakalk-Bucht in den Kristallingesteinen am Rand der Böhmischen Masse und versetzt den Paläo-Donaurandbruch [DE-BY_1237]. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
notation: LfU-BY_1239
limit type: normalFault
broader: Aidenbach-Griesbach Step Fault

Flintsbach Fault
type: Fault
type: Limit
sf touches: Aidenbach-Griesbach Step Fault
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4152
references: https://data.geoscience.earth/ncl/geoera/ref/4107
type: Concept
created: 2020-10-09T11:35:35.311Z
notation: DE-BY_1238
preferred label: Flintsbach Störung @de
definition: Slight westward arcuate SW-NE trending, approx. 80° NW dipping normal fault, northwestern border of the Flintsbach Jurassic carbonates trough-like embayment into the marginal Bohemian Massif crystalline rock suites, offsetting Paleo-Donaurand Fault Scarp [DE-BY_1237]. Merges into Aidenbach-Griesbach Step Fault [DE-BY_764] forming the western boundary of a downthrow block featuring Jurassic carbonates at shallow depth.
definition: Leicht nach Westen gebogen, SW-NE verlaufende, ca. 80° nach NW einfallende Abschiebung als nordwestliche Grenze der Flintsbacher Jurakalk-Bucht in den Kristallingesteinen am Rand der Böhmischen Masse und versetzt den Paläo-Donaurandbruch [DE-BY_1237]. Geht im Süden in den Aidenbach-Griesbach Abbruch [DE-BY_764] über und begrenzt eine Scholle mit Jurakalk in geringer Tiefe (Fortsetzung der Flintsbacher Bucht) nach Nordwesten hin. @de
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
notation: LfU-BY_1238
limit type: normalFault
broader: Aidenbach-Griesbach Step Fault

Flintsbach-Pleinting Fault
type: Fault
type: Limit
sf touches: Aidenbach-Griesbach Step Fault
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
definition: Eastward arcuate N-S trending, approx. 80° W dipping normal fault forming a moderate-throw pre-step of Aidenbach-Griesbach Step Fault [DE-BY_764]. Continues in Brand-Doblwiese Fault [DE-BY_1239] in the north and represents the eastern boundary of a downthrow block featuring Jurassic carbonates at shallow depth (continuation of Flintsbach embayment).
created: 2020-10-09T11:35:35.367Z
notation: DE-BY_1240
preferred label: Flintsbach-Pleinting Störung @de
definition: Ostwärts gebogen N-S verlaufende, rund 80° nach W einfallende Abschiebung, Vorbruch mäßiger Sprunghöhe zum Aidenbach-Griesbach Abbruch [DE-BY_764]. Nimmt im Norden die Brand-Doblwiese Störung [DE-BY_1239] auf und begrenzt eine Scholle mit Jurakalk in geringer Tiefe (Fortsetzung der Flintsbacher Bucht) nach Osten hin. @de
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
notation: LfU-BY_1240
limit type: normalFault
broader: Aidenbach-Griesbach Step Fault

Ried Fault
type: Fault
type: Limit
sf touches: Aspach Fault
sf touches: Steindlberg Fault
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/4099
references: https://data.geoscience.earth/ncl/geoera/ref/4082
sf touches: Handenberg Fault
sf touches: Pocking Step Fault
sf touches: Nonsbach Fault
type: Concept
created: 2020-10-09T11:35:35.701Z
notation: AT_10665
alternative label: Rieder Abbruch @de
preferred label: Ried Störung @de
definition: This undulate N-S trending, approx. 80° W dipping multiphase normal fault featuring a throw of up to 600 m runs in the subsurface of the Alpine Molasse from Bad Füssing (DE) via Ried im Innkreis (AT) towards the Attersee (AT). It is the southern continuation of Pocking Step Fault [DE-BY_699] on Austrian territory and is part of the Deggendorf-Ried Fault System [DE-BY_929, AT_1044]. It is confirmed by seismic and borehole data (Freudenberger & Schwerd 1996, Kröll et al. 2006). Its damage zone in the hanging wall is targeted by Ried-Mehrnbach geothermal development.
definition: Diese gewellt N-S verlaufende, ca. 80° nach W einfallende mehrphasige Abschiebung mit einen Vertikalversatz von bis zu 600 m, im Molasseuntergrund von Bad Füssing (DE) über Ried im Innkreis (AT) bis zum Attersee verlaufende Störung ist durch Seismik- und Bohrlochdaten belegt (Freudenberger & Schwerd 1996, Kröll et al. 2006). Sie bildet die südliche Fortsetzung des Pockinger Abbruchs [DE-BY_699] und ist Teil der Deggendorf-Ried Störungssystems [DE-BY_929, AT_1044]. Die störungsbegleitende Zerrüttungszone der Tiefscholle ist der Zielbereich der geothermalen Erschließung Ried-Mehrnbach. @de
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
notation: LfU-BY_10665
limit type: normalFault
broader: Deggendorf-Ried Faultsystem

Birnbach-Füssing Step Fault
type: Fault
type: Limit
sf touches: Aidenbach-Griesbach Step Fault
references: https://data.geoscience.earth/ncl/geoera/ref/789
sf touches: Nonsbach Fault
notation: AT-10669
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4096
references: https://data.geoscience.earth/ncl/geoera/ref/4095
type: Concept
created: 2020-10-09T11:35:35.673Z
notation: DE-BY_930
alternative label: Weihmörting Fault Scarp
alternative label: Weihmörtinger Abbruch @de
preferred label: Birnbach-Füssing Abbruch @de
definition: Southwestern branch of southern continuation of the Aidenbach-Griesbach Step Fault. Blind, undulate NNW-SSE trending, approx. 80° WSW dipping normal fault, featuring a cumulative throw of up to 1 km.
definition: Südwestlicher Zweig der südlichen Fortsetzung des Aidenbach-Griesbach Abbruchs. Gewellt NNW-SSO verlaufende, ca. 80° nach WSW einfallende, überdeckte Abschiebung mit einer kumulativen Sprunghöhe bis zu 1 km. @de
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11683
notation: LfU-BY_930
limit type: normalFault
broader: Deggendorf-Ried Faultsystem

Nonsbach Fault
type: Fault
type: Limit
type: SpatialObject
sf touches: Ried Fault
definition: Überdeckte E-W streichende, steil nach N einfallende Störung an der Basis des Molassebeckens die sich im Osten bis zur Ried Störung [AT-10654] als Teil des Deggendorf-Ried Störungssystems [DE-BY_929], im Westen bis Ranshofen (AT) zieht. @de
sf touches: Mauerkirchen Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4098
notation: AT-10657
definition: This E-W striking, steeply N-dipping blind fault at the bottom of the Molasse Basin terminates in the east at the Ried Fault [AT-10654], a branch of the Deggendorf-Ried Fault System [DE-BY_929], and in the west at Ranshofen (AT).
type: Concept
created: 2020-09-09T13:25:50.665Z
preferred label: Nonsbach-Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/4082
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: West Molasse Fault Set
broader: Lower Bavaria - Upper Austria Molasse Basin fault domain

Pfarrkirchen Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:34.580Z
notation: DE-BY_763
preferred label: Pfarrkirchen Störung @de
definition: NW-SE to NNW-SSE trending, approx. 70° ± NE dipping normal fault with a throw up to 800 m, running from Oberschneiding to Pfarrkirchen as an antithetic conjugated fault to Aidenbach-Griesbach Step Fault [DE-BY_764], and on to Simbach/Inn at the Austrian Border (kinematics uncertain) .
definition: NW-SE bis NNW-SSE streichende, ca. 70° nach ± NE einfallende Abschiebung mit einem Versatz bis zu 800 m. Bildet von Oberschneiding bis Pfarrkirchen eine antithetische, konjugierte Störung zum Aidenbach-Griesbach Abbruch [DE-BY_764], die Fortsetzung bis zum Inn bei Simbach ist kinematisch unsicher. @de
sf touches: Stubenberg-Malching Fault
sf touches: Oberschneiding Transverse Fault
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4082
references: https://data.geoscience.earth/ncl/geoera/ref/4078
sf touches: Holzhamm-Lanzing Fault
sf touches: Haunersdorf-Perbing Fault
sf touches: Hirschbach Fault
sf touches: Gumpersdorf-Schellenberg Fault
narrower: Altenbuch-Oberpöring Subfault
notation: AT-10668
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11684
notation: LfU-BY_763
limit type: normalFault
broader: West Molasse Fault Set
broader: Regensburg-Straubing Trough SW Fringe

Altenbuch-Oberpöring Subfault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:34.609Z
notation: DE-BY_1227
preferred label: Altenbuch-Oberpöring Nebenstörung @de
definition: NNW-SSE striking, approx. 75° ENE dipping antithetic normal fault southwest of Plattling; branch of Pfarrkirchen Fault [DE-BY_ 763].
definition: NNW-SSE streichende, ca. 75° nach ENE einfallende antithetische Abschiebung südwestlich von Plattling; Zweig der Pfarrkirchen Störung [DE-BY_ 763]. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4082
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
notation: LfU-BY_1227
limit type: normalFault
broader: Pfarrkirchen Fault

Steindlberg Fault
type: Fault
type: Limit
type: SpatialObject
definition: Überdeckte, ENE-WSW streichende, N-fallende Störung an der Basis des Molassebeckens, die sich vom Landshut-Neuötting Abbruch im Westen über Mattighofen (AT) bis zur Ried Störung [AT-10654] zieht. Diese Störung ist in der Bohrung Steindlberg 1 nachgewiesen. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4082
notation: AT-10664
preferred label: Steindlberg-Störung @de
definition: This ENE-WSW striking, N-dipping blind fault at the bottom of the Molasse Basin runs via the town of Mattighofen (AT) terminates in the west at the Landshut-Neuötting Fault System and in the east at the Deggendorf-Ried Fault. The Fault is observed at Well Steindlberg 1.
type: Concept
created: 2020-09-09T13:25:50.837Z
references: https://data.geoscience.earth/ncl/geoera/ref/4098
sf touches: Fornach Fault
sf touches: Ried Fault
sf touches: Handenberg Fault
sf touches: Mauerkirchen Fault
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: West Molasse Fault Set
broader: Lower Bavaria - Upper Austria Molasse Basin fault domain

Mauerkirchen Fault
type: Fault
type: Limit
definition: This SE-NW striking, NE-dipping blind fault at the bottom of the Molasse Basin starts east of Braunau (AT) and runs via Mauerkirchen (AT) towards SE and terminates at the Handenberg Fault [AT-10655].
type: SpatialObject
sf touches: Aspach Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4078
definition: Überdeckte, SE-NW streichende, NE-fallende Störung an der Basis des Molassebeckens, die sich von Braunau (AT) im Westen über Mauerkirchen (AT) bis zur Handenberg Sörung [AT-10655] zieht. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4082
references: https://data.geoscience.earth/ncl/geoera/ref/4097
notation: AT-10654
created: 2020-09-09T13:25:50.865Z
type: Concept
preferred label: Mauerkirchen-Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/4099
sf touches: Nonsbach Fault
sf touches: Handenberg Fault
sf touches: Steindlberg Fault
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: West Molasse Fault Set
broader: Lower Bavaria - Upper Austria Molasse Basin fault domain

Karlstift Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/731
references: https://data.geoscience.earth/ncl/geoera/ref/755
notation: AT-121
type: Concept
created: 2020-04-30T14:27:01.555Z
definition: The Karlstift fault system consists of several parallel NNE-SSW trending faults from Nove Hrady (CZ) at the northern end via Höhenberg (AT) towards Lasber or Erdleiten at the southern end. In analogy to the Rodl fault system, the main ductile deformation phase is dated to the Late Variscian, showing mainly right-lateral movement. Late Miocene reactivation, again with right-lateral movement, is assumed. (Brandmayr et al., 1997; Büttner, 2007)
definition: Das Störungssystem besteht aus mehreren parallel, NNE-SSW streichenden Störungen, die sich von Nove Hrady (CZ) und Höhenberg (AT) nach Süden bis Lasber bzw. Erdleiten verfolgen lassen. Die duktile Hauptbewegungsphase wird, analog zum Rodl-Störungssystem, auf das Spätvariszikum gelegt, mit hauptsächlich sinistraler Bewegungsrichtung. Von einer spröden miozänen Reaktivierung mit derselben Bewegungskinematik wird ebenfalls ausgegangen. (Brandmayr, 1997; Büttner, 2007) @de
preferred label: Karlstift-Störungssystem @de
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Vorau Fault
definition: The approximately SW-NE striking fault runs from Prätis to east of Vorau.
type: Concept
created: 2020-04-30T14:27:03.780Z
preferred label: Vorau-Störung @de
notation: AT-10469
definition: Die in etwa SW-NE-streichende Störung verläuft von Prätis bis östlich von Vorau. @de
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Kalkstein-Vallarga Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/752
references: https://data.geoscience.earth/ncl/geoera/ref/834
notation: AT-120
type: Concept
created: 2020-04-30T14:27:01.610Z
definition: This ca. 50 km long, approximately NNE-SSW trending Fault System south of the Tauern window extends from the Weiten (Vallarga) Valley to Kalkstein (southwest of Innervillgraten). In analogy to the Defereggen-Antholz-Vals Fault System, it shows ductile movement during Cretaceous and Paleogene times with brittle left-lateral movement during Oligocene and early Miocene times (Handy et al., 2005).
definition: Ist ein in etwa WNW-ESE-streichendes ca. 50 km langes Störungssystem südlich des Tauern-Fensters, welches von Weitental (Vallarga) bis Kalkstein (südwestlich von Innervillgraten) reicht. Vergleichbar zum Defreggen-Antholz-Vals-Störungssystem wird eine duktile Anlage in der Oberkreide-Paläogen angenommen mit einer deutlichen sinistral seitenverschiebenden spröden Überprägung im Oligozän bis unterstem Miozän (Handy et al., 2005). @de
preferred label: Kalkstein-Vallarga-Störungssystem @de
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Leogang Fault
definition: The E-W striking fault runs from 4 km south of Fieberbrunn via Leogang to Bachwinkl Pabing.
definition: Die E-W striking Störung verläuft vom 4 km südlich von Fieberbrunn über Leogang nach Bachwinkl Pabing. @de
type: Concept
created: 2020-04-30T14:27:03.752Z
preferred label: Leogang-Störung @de
notation: AT-10463
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Mölltal Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/754
references: https://data.geoscience.earth/ncl/geoera/ref/823
notation: AT-130
type: Concept
created: 2020-04-30T14:27:01.582Z
definition: This ca. 65 km long, NE-SW trending Fault System extends from Obervellach, following the Möll Valley to Villach and the Drau Valley, where it is cut by the Periadriatic Fault System. It shows ductile and brittle right-lateral movement with a main activity during Miocene times. An initiation in the Oligocene and continuation to the Tauern window is discussed (Scharf et al., 2013 and references therein). Displacement rates from 20 to 45 km are described (Linzer et al, 2002).
definition: Dieses NW-SE-streichende ca. 65 km lange Störungssystem verläuft von Obervellach, entlang des Mölltals über Villach bis zum Drautal. Dort geht es ins Periadriatisches-Störungssystem über bzw. wird von diesem abgeschnitten. Es zeigt duktile, vorwiegend dextral seitenverschiebende Kinematik mit einer Hauptaktivität im Miozän. Eine Anlage im Oligozän mit Übergängen ins Tauern-Fenster wird diskutiert (Scharf et al., 2013 und die darin aufgeführten Referenzen) und ein Versatz von 20-45 km wird angenommen (Linzer et al, 2002). @de
preferred label: Mölltal-Störungssystem @de
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Jachymov Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/731
references: https://data.geoscience.earth/ncl/geoera/ref/747
notation: AT-118
type: Concept
created: 2020-04-30T14:27:01.499Z
definition: The NW-SE trending Fault System extends from Strakonice (CZ) via České Budějovice and Trebon to Gmünd (AT). The associated faults show evidences for dextral and normal movement between the late Variscan and Miocene. (Brandmayr et al., 1997; Porparczy, 2011)
definition: Das NW-SE streichende Störungssystem, auch unter dem Namen Joachimsthal-Störungssystem bekannt, zieht sich von Strakonice (CZ) über die Budweis- und Trebon-Becken bis nach Gmünd (AT) hin. Die Störungen zeigen Hinweise sowohl auf dextrale wie auch abschiebende Deformation zwischen dem späten Variszikum und post-Miozän. (Brandmayr et al., 1997; Porparczy, 2011) @de
preferred label: Jachymov-Störungssystem @de
narrower: Dubno Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Dubno Fault
definition: This NW-SE striking fault is the SE-bounding fault of the České Budějovice (Budweis) basin and runs from Dehtare to Borsov nad Vlatavou (CZ).
definition: Diese NW-SE-streichende Störung ist die SE-Begrenzung des Budweiser Beckens und verläuft von Dehtare nach Borsov nad Vlatavou (CZ). @de
notation: AT-10435
type: Concept
created: 2020-04-30T14:27:01.527Z
preferred label: Dubno-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Jachymov Fault System

Stollkogel-Schrankeck Fault
definition: This slightly curved, NNE-SSW trending fault runs from Mittersill via the summit of M. Schrankeck to east of M. Stollkogel in the south.
definition: Diese leicht gebogene, NNE-SSW-streichende Störung verläuft von Mittersill über die Erhebung des Schrankecks bis östlich des Stollkogels im Süden. @de
type: Concept
created: 2020-04-30T14:27:03.640Z
preferred label: Stollkogel-Schrankeck-Störung @de
notation: AT-10462
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Kourim-Blanice-Rodl-Kaplice Large-scale Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/756
references: https://data.geoscience.earth/ncl/geoera/ref/731
references: https://data.geoscience.earth/ncl/geoera/ref/755
references: https://data.geoscience.earth/ncl/geoera/ref/773
references: https://data.geoscience.earth/ncl/geoera/ref/733
references: https://data.geoscience.earth/ncl/geoera/ref/750
references: https://data.geoscience.earth/ncl/geoera/ref/837
references: https://data.geoscience.earth/ncl/geoera/ref/839
notation: AT-4
type: Concept
created: 2020-04-30T14:27:00.228Z
definition: This ca. 250 km long, approximately NNE-SSW (and partly NNE-SSW) trending large-scale fault system extends from the Kourim Furrow in the North, following the Blanice Furrow, crossing the basins of Trebon and České Budějovice via Kaplice (CZ) and the valley of the Große Rodl to Gramastetten and the basin of Eferding, where it is partly covered by Miocene sediments, but continues into the basin subsurface (Brandmayr et al., 1997, Wagner, 1998, Zacharias & Hübst, 2012). It includes the Kourim-Blanice and Rodl-Kaplice Fault Systems and shows a long-lasting and multiphase deformation history. Parallel trending structures and conjugated shear zones and faults are correlated with this large-scale fault system (e.g. Haselgraben Subfault System). Proofs of NE-SW-trending left-lateral strike-slip ductile, mylonitic shear zones during Upper Carboniferous and Permian times are predominantly observed in the southern parts (Brandmayr, et al., 1995; Büttner, 2007, Iglseder, 2013). To the North, it continues to build horst-and-graben structures filled with Upper Carboniferous to Permian sediments (Martinek et al., 2001) and associated Permian dykes (Kosler et al., 2001). The deformation continued as left-lateral strike-slip faulting during Cretaceous and Miocene times, indicated by sediment deposits (Iglseder, 2013).
definition: Dieses in etwa NNE-SSW - (teilweise NNE-SSW-) streichende ca. 250 km lange Großstörungssystem zieht vom Kourim-Becken, entlang dem Blanice-Graben, dem Becken von Trebon und dem Becken von Budweis über Kaplice, das Große Rodl-Tal entlang bis Gramastetten und wird im Eferding-Becken von Miozänen Sedimenten überdeckt, setzt sich jedoch in den kristallinen Beckenuntergrund fort (Brandmayr et al., 1997, Wagner, 1998, Zacharias & Hübst, 2012). Es setzt sich aus dem Kourim-Blanice- und Rodl-Kaplice-Störungssystem zusammen und zeigt eine langandauernde und multiphase Entwicklung. Parallel streichende Strukturen und konjugierte Scherzonen und Störungen orientiert als Riedel und Antiriedel werden diesem Großstörungssystem zugeordnet (z.B. Haselgraben-Teilstörungssystem). Die Anlage als NE-SW-streichende duktile mylonitische Scherzonen mit sinistral seitenverschiebender Kinematik des oberen Karbons bis Perms (Brandmayr, et al., 1995; Büttner, 2007) sind vorwiegend in den südlichen Abschnitten beschrieben und setzt sich nach Norden in von oberkarbonen-permischen Sedimenten verfüllte (Martinek et al., 2001) mit permischen Gängen assoziierte Horst und Grabenstruktur fort (Kosler et al., 2001). Diese wird durch spröde Störungen mit sinistral seitenverschiebender Kinematik überprägt (Iglseder, 2013), welche sich anhand von Beckenfüllungen über die Oberkreide bis ins Miozän beobachten lassen. @de
preferred label: Kourim-Blanice-Kaplice-Rodl-Großstörungssystem @de
narrower: Rodl-Kaplice Fault System
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Rodl-Kaplice Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/755
references: https://data.geoscience.earth/ncl/geoera/ref/773
references: https://data.geoscience.earth/ncl/geoera/ref/733
references: https://data.geoscience.earth/ncl/geoera/ref/750
notation: AT-103
type: Concept
created: 2020-04-30T14:27:00.256Z
definition: This ca. 90 km long, approximately NNE-SSW trending fault system extends from Kaplice (CZ), following the valley of the Große Rodl to Gramastetten and the basin of Eferding, where it is partly covered by Miocene sediments, but continues into the basin subsurface (Brandmayr et al., 1997, Wagner, 1998). It includes the Rodl and Haselgraben Subfault Systems and shows a long-lasting and multiphase history. Proofs of NE-SW-trending left-lateral strike-slip ductile mylonitic shear zones during Upper Carboniferous and Permian times are observed (Brandmayr, et al., 1995; Büttner, 2007, Iglseder, 2013). The deformation continuous with left-lateral strike-slip faulting during Cretaceous and Miocene times, indicated by sediment deposits (Iglseder, 2013). Displacement up to 35 km is suggested (Iglseder, 2013).
definition: Dieses etwa NNE-SSW - streichende ca. 90 km lange Störungssystem zieht von Kaplice, das Große Rodl-Tal entlang bis Gramastetten und wird im Eferding-Becken von Miozänen Sedimenten überdeckt, setzt sich jedoch in den kristallinen Beckenuntergrund fort (Brandmayr et al., 1997, Wagner, 1998). Es beinhaltet das Rodl- und Haselgraben-Teilstörungssystem sowie parallel orientierte und konjugierte Strukturen. Eine erste Prägung erfuhren diese NE-SW-streichenden duktilen mylonitischen Scherzonen mit sinistral seitenverschiebender Kinematik im oberen Karbon – Perm (Brandmayr et al., 1995, Büttner, 2007). Diese wird durch spröde Störungen mit sinistral seitenverschiebender Kinematik überprägt (Iglseder, 2013), welche sich anhand von Beckenfüllungen über die Oberkreide bis ins Miozän, sowie Versatz von Miozänen Sedimenten verfolgen lässt. Sinistrale Versatzweiten von bis 35 km werden angenommen (Iglseder, 2013). @de
preferred label: Rodl-Kaplice-Störungssystem @de
narrower: Haselgraben Subfault System
narrower: Rodl Subfault System
in scheme: Tectonic Boundary Objects in Europe
broader: Kourim-Blanice-Rodl-Kaplice Large-scale Fault System

Haselgraben Subfault System
references: https://data.geoscience.earth/ncl/geoera/ref/733
references: https://data.geoscience.earth/ncl/geoera/ref/787
references: https://data.geoscience.earth/ncl/geoera/ref/788
notation: AT-541
type: Concept
created: 2020-04-30T14:27:00.284Z
definition: This ca. 15 km long N-S trending subfault system extends from Hellmondsödt, following the Haselgraben Valley to Linz. It is part of the Rodl-Kaplice Fault System and includes ductile parallel trending shear zones with left-lateral kinematics active during the Late Variscian. In analogy to the Rodl Subfault System, a continuation of brittle left-lateral movement during Cretaceous and Miocene times is suggested. (Iglseder, 2013, 2014a, b)
definition: Dieses ca. 15 km lange N-S-streichende Teilstörungssystem verläuft von Hellmondsödt, den Haselgraben entlang bis Linz und ist Teil des Rodl-Kaplice-Störungssystems. Es beinhaltet duktile parallel verlaufende Scherzonen mit sinistral seitenverschiebender Kinematik aktiv während des Spätvariszikums. Analog zum Rodl-Teilstörungssystem wird eine spröde Reaktivierung mit sinistral-seitenverschiebender Bewegung während der Kreide bis Miozän angenommen. (Iglseder, 2013, 2014a, b) @de
preferred label: Haselgraben-Teilstörungssystem @de
narrower: Haselgraben Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Rodl-Kaplice Fault System

Haselgraben Fault
definition: The N-S trending fault is part of Haselgraben Subfault System and extends from Hellmannsödt in the north along the Haselgraben Valley via Linz to the south of Hofkirchen im Traunkreis (Iglseder, 2013, 2014a, b).
definition: Die N-S streichende Störung ist Teil des Haselgraben-Teilstörungssystems. Sie erstreckt sich von Hellmannsödt im Norden entlang des Haselgrabens via Linz bis nach Hofkirchen im Traunkreis im Süden (Iglseder, 2013, 2014a, b). @de
notation: AT-10105
type: Concept
created: 2020-04-30T14:27:00.312Z
preferred label: Haselgraben-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Haselgraben Subfault System

Rodl Subfault System
references: https://data.geoscience.earth/ncl/geoera/ref/755
references: https://data.geoscience.earth/ncl/geoera/ref/773
references: https://data.geoscience.earth/ncl/geoera/ref/733
references: https://data.geoscience.earth/ncl/geoera/ref/750
definition: This ca. 55 km long, approximately NNE-SSW trending Subfault System extends from Rybnik (CZE), following the Valley of the Große Rodl to Gramastetten and the basin of Eferding, where it is partly covered by Miocene sediments, but continues in the basin subsurface (Brandmayr et al., 1997, Wagner, 1998). It includes partly parallel trending shear zones and faults and shows a long-lasting and multiphase history. Proofs of NE-SW-trending left-lateral strike-slip ductile, mylonitic shear zones during upper Carboniferous and Permian times are observed (Brandmayr, et al., 1995; Büttner, 2007, Iglseder, 2013). The deformation continuous with left-lateral strike-slip faulting during Cretaceous and Miocene times, indicated by sediment deposits. Displacement up to 35 km is suggested. (Iglseder, 2013)
notation: AT-513
type: Concept
created: 2020-04-30T14:27:00.340Z
definition: Dieses NNE-SSW - streichende ca. 55 km lange Teilstörungssystem zieht von Kaplice, das Große Rodl-Tal entlang bis Gramastetten und wird im Eferding-Becken von Miozänen Sedimenten überdeckt, setzt sich jedoch in den kristallinen Beckenuntergrund fort (Brandmayr et al., 1997, Wagner, 1998). Eine erste Prägung erfuhren diese NE-SW-streichenden duktilen mylonitischen Scherzonen mit sinistral seitenverschiebender Kinematik im oberen Karbon – Perm (Brandmayr et al., 1995, Büttner, 2007). Diese wird durch spröde Störungen mit sinistral seitenverschiebender Kinematik überprägt (Iglseder, 2013), welche sich anhand von Beckenfüllungen über die Oberkreide bis ins Miozän, sowie durch den Versatz von Miozänen Sedimenten verfolgen lässt. Sinistrale Versatzweiten von bis 35 km werden angenommen. (Iglseder, 2013) @de
preferred label: Rodl-Teilstörungssystem @de
narrower: Rodl Fault
narrower: Rodl Shearzone
in scheme: Tectonic Boundary Objects in Europe
broader: Rodl-Kaplice Fault System

Rodl Shearzone
definition: The mylonitic part of the NNE-SSW trending Rodl Subfault System is referred to as Rodl Shearzone.
definition: Die in etwa NNE-SSW-streichende Scherzone umfasst den duktilen Teil des Rodl-Teilstörungssystem. @de
references: https://data.geoscience.earth/ncl/geoera/ref/733
notation: AT-1041
type: Concept
created: 2020-04-30T14:27:00.396Z
preferred label: Rodl-Scherzone @de
in scheme: Tectonic Boundary Objects in Europe
broader: Rodl Subfault System

Rodl Fault
definition: The approximately NNE-SSW trending fault contains the brittle part of the Rodl Subfault System.
definition: Die in etwa NNE-SSW-streichende Störung umfasst den spröden Teil des Rodl-Teilstörungssystems. @de
references: https://data.geoscience.earth/ncl/geoera/ref/733
preferred label: Rodl-Störung @de
notation: AT-10295
type: Concept
created: 2020-04-30T14:27:00.368Z
in scheme: Tectonic Boundary Objects in Europe
broader: Rodl Subfault System

Vils Fault
type: Concept
created: 2020-04-30T14:27:03.612Z
definition: The NW-SE striking fault runs from Steinach (Ger) via Vils and Reutte to the lake Plansee. The map view suggests left-lateral offset. (Tollmann, 1986)
definition: Die NW-SE streichende Störung verläuft von Steinach (D) über Vils und Reutte zum Plansee. Aus dem Kartenbild ergibt sich ein sinistraler Versatz. (Tollmann, 1986) @de
preferred label: Vils-Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/732
notation: AT-10395
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

NCA NNE-SSW Fault Set
references: https://data.geoscience.earth/ncl/geoera/ref/840
references: https://data.geoscience.earth/ncl/geoera/ref/841
notation: AT-532
type: Concept
created: 2020-04-30T14:27:02.369Z
definition: This fault set of NNE-SSW trending faults within the Northern Calcareous Alps (NCA) includes the Göstling Fault, the Leonsberg Fault, the Untersalzachtal Fault, the Weyer Fault and other similar orientated faults with same kinematics. Even though they may have been active during Oligocene and Miocene times as sinistral or dextral strike-slip faults, respectively, the main deformation phase of this conjugated fault set occurred during Middle Miocene E-W extension, where the faults had normal fault kinematics. (Peresson & Decker, 1997a, b)
definition: Dieses Störungsset beinhaltet NNE-SSW-streichenden Störungen in den Nördlichen Kalkalpen (NKA), welche die Göstling-, Leonsberg-, Untersalzachtal-, Weyer- und weitere ähnlich orientierte Störungen mir derselben Kinematik beinhaltet. Diese Störungen waren während des Oligozäns-Miozäns als sinistrale und dextrale Seitenverschiebungen aktiv. In ihrer Hauptphase während des mittleren Miozäns zeigen sie abschiebende Kinematik. (Peresson & Decker, 1997a, b) @de
preferred label: NKA-Störungsset (NNE-SSW) @de
narrower: Untersalzachtal Fault
narrower: Leonsberg Fault
narrower: Göstling Fault
narrower: Weyer Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Untersalzachtal Fault
definition: The NNW-SSE trending fault with left-lateral movement runs along valley of the River Salzach between Golling/Salzach and Salzburg. (Frisch & Gawlick, 2003)
definition: Die NNW-SSE-streichende Störung mit sinistral seitenverschiebender Kinematik verläuft im Bereich des unteren Salzachtales etwa zwischen Golling a.d. Salzach bis Salzburg. (Frisch & Gawlick, 2003) @de
references: https://data.geoscience.earth/ncl/geoera/ref/748
notation: AT-10384
type: Concept
created: 2020-04-30T14:27:02.396Z
preferred label: Untersalzachtal-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: NCA NNE-SSW Fault Set

Göstling Fault
definition: The NNE-SSW trending fault with left-lateral movement runs from Hieflau through Göstling to 3 km west of Ybbsbachamt. (Decker et al., 1993, 1994; Linzer et al., 2002)
definition: Die NNE-SSW-streichende Störung mit sinistral seitenverschiebender Kinematik verläuft von Hieflau über Göstling bis 3 km westlich von Ybbsbachamt. (Decker et al., 1993, 1994; Linzer et al., 2002) @de
references: https://data.geoscience.earth/ncl/geoera/ref/726
references: https://data.geoscience.earth/ncl/geoera/ref/823
references: https://data.geoscience.earth/ncl/geoera/ref/830
notation: AT-10093
type: Concept
created: 2020-04-30T14:27:02.453Z
preferred label: Göstling-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: NCA NNE-SSW Fault Set

Leonsberg Fault
definition: The NNE-SSW trending fault runs east of the lake Attersee. (Tollmann, 1986)
definition: Die NNE-SSW-streichende Störung verläuft östlich des Attersees. (Tollmann, 1986) @de
references: https://data.geoscience.earth/ncl/geoera/ref/732
notation: AT-10178
type: Concept
created: 2020-04-30T14:27:02.424Z
preferred label: Leonsberg-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: NCA NNE-SSW Fault Set

Weyer Fault
definition: The NNE-SSW trending fault with left-lateral movement runs from Admont to Neudorf, north of Weyer. (Decker, et al., 1994; Linzer et al., 2002)
definition: Die NNE-SSW-streichende Störung mit sinistral seitenverschiebender Kinematik verläuft von Admont nach Neudorf, nörlich von Weyer. (Decker, et al., 1994; Linzer et al., 2002) @de
references: https://data.geoscience.earth/ncl/geoera/ref/726
references: https://data.geoscience.earth/ncl/geoera/ref/823
notation: AT-10404
type: Concept
created: 2020-04-30T14:27:02.481Z
preferred label: Weyer-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: NCA NNE-SSW Fault Set

Katschbachtal Fault
definition: The approximately NW-SE trending fault runs from 3 km SW of St. Nikolai/Sölktal to Baierdorf.
definition: Die etwa NW-SE-streichende Störung verläuft von 3km südwestlich von St. Nikolai im Sölktal bis Baierdorf. @de
type: Concept
created: 2020-04-30T14:27:03.696Z
preferred label: Katschbachtal-Störung @de
notation: AT-10443
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Mödring Fault
definition: The E-W striking normal fault runs from Scheidersdorf to Sitzendorf. Top to the south faulting was active during the Eggenburgium.
definition: Die E-W-streichende Abschiebung verläuft von Scheidersdorf bis Sitzendorf, die Bewegungsrichtung des Hangendblocks ging im Eggenburgium gegen Süden. @de
type: Concept
created: 2020-04-30T14:27:03.668Z
preferred label: Mödring-Störung @de
notation: AT-10448
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Moldanubian Thrust
type: Concept
created: 2020-04-30T14:27:03.527Z
definition: Along this Variscian E-dipping shear zone, the Moldanubian Superunit moves NNE-vergent over the Moravo-Silesian Superunit. The fault strikes N-S from Langenlois to Horn, where it extends in WNW-ESE direction towards Messern. There, the fault strikes NE-SW via Geras and Vranov (CZ) to Moravský Krumlov (CZ). (Fritz & Neubauer, 1994; Stipska et al., 1999)
definition: Jungvariszische E-einfallende Scherzone, an der das Moldanubikum NNE-vergent über das Moravikum geschoben wurde. Sie verläuft N-S streichend von Langenlois bis östlich von Horn, wo sie dann WNW-ESE streichend bis Messern verläuft. Dort ändert sie wiederum ihre Streichrichtung und verläuft NE-SW streichend über Geras und Vranov (CZ) bis nach Moravský Krumlov (CZ). (Fritz & Neubauer, 1994; Stipska et al., 1999) @de
preferred label: Moldanubische Scherzone @de
references: https://data.geoscience.earth/ncl/geoera/ref/751
references: https://data.geoscience.earth/ncl/geoera/ref/832
notation: AT-1070
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Mattersburg Fault
type: Concept
created: 2020-04-30T14:27:03.498Z
definition: The Mattersburg fault consists of two NW-SE striking and steeply NE-dipping subfaults that extend from Wiener Neustadt via Mattersburg to the Austrian-Hungarian border. Based on the Molasse subsurface map, it has a normal fault character with an offset of up to 1000 m. (Wessely et al., 1993)
definition: Die Mattersburg-Störung besteht aus zwei NW-SE streichenden, steil nach NE einfallenden Teilstörungen, die sich von Wiener Neustadt über Mattersburg bis zur ungarischen Grenze hinziehen. Aus der Molasseuntergrundkarte ist ein abschiebender Charakter mit Versatzweiten bis zu 1000 m ablesbar. (Wessely et al., 1993) @de
preferred label: Mattersburg-Störung @de
notation: AT-10474
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Hochstuhl-Gegendtal Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/850
notation: AT-115
type: Concept
created: 2020-04-30T14:27:01.332Z
definition: This ca. 55 km long, approximately NNW-SSE trending Fault System extends from the Hochstuhl mountain (at the AUT-SLO border), following the Gegendtal (Afritz) Valley to Radenthein. Proofs for right-lateral movement from the Miocene with thrusting along the Rosegg shear zone with displacement rates up to 20 km as well as displacement of the Periadriatic Fault System of 3,5 km are described. (Polinski & Eisbacher, 1992)
definition: Dieses in etwa NNW-SSE - streichende ca. 55 km lange Störungssystem zieht vom Hochstuhl (an der AUT-SLO Grenze), bis Rosegg und weiter über das Gegendtal (Afritzbach) nach Radenthein. Es zeigt dextral seitenverschiebende Kinematik ab dem Miozän mit überschiebender Kinematik entlang der Rosegg-Scherzone. Versatzweiten von bis zu 20 km mit einem Versatz des Periadriatischen Störungssystem von 3,5 km ist beschrieben. (Polinski & Eisbacher, 1992) @de
preferred label: Hochstuhl-Gegendtal-Störungssystem @de
narrower: Hochstuhl Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Hochstuhl Fault
definition: The NW-SE trending fault in the area of the Hochstuhl Mountain from north of Millstatt to Zauchen shows right-lateral displacement and is part of the Hochstuhl-Gegendtal Fault System (Polinski & Eisbacher, 1992).
definition: Die NW-SE-streichende Störung des Hochstuhl-Gegendtal-Störungssystem von Millstatt nach Zauchen zeigt dextral-seitenverschiebende Kinematik (Polinski & Eisbacher, 1992). @de
references: https://data.geoscience.earth/ncl/geoera/ref/850
notation: AT-10113
type: Concept
created: 2020-04-30T14:27:01.360Z
preferred label: Hochstuhl-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Hochstuhl-Gegendtal Fault System

Pregarten Fault
type: Concept
created: 2020-04-30T14:27:03.583Z
definition: The NW-SE striking fault runs from Pregarten via Kriechbaum to Oberlebing. It forms the NE margin of the Gallneukirchen Basin. (Kröll et al., 2001; Seiberl et al., 1996)
definition: Die NW-SE streichende Störung verläuft von Pregarten über Kriechbaum nach Oberlebing. Sie formt die NE-Grenze des Gallneukirchen-Beckens. (Kröll et al., 2001; Seiberl, et al., 1996) @de
preferred label: Pregarten-Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/728
references: https://data.geoscience.earth/ncl/geoera/ref/743
notation: AT-10272
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Pöll Fault
type: Concept
created: 2020-04-30T14:27:03.555Z
definition: The WSW-ENE striking fault runs from the Ochsenkogel mountain south of Leoben via the Hochalpe mountain and the village of Kirchdorf to Stanz im Mürztal. (Tollmann, 1986)
definition: Die WSW-ENE streichende Störung verläuft vom Ochsenkogel südlich von Leoben über die Hochalpe und Kirchdorf nach Stanz in Mürztal. (Tollmann, 1986) @de
preferred label: Pöll-Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/732
notation: AT-10262
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Defereggen-Antholz-Vals Fault System
definition: This is a ca. 70 km long, roughly WE-trending fault system (FS) south of the Tauern window, which runs from Vals (north of Brixen) via the Valleys of Antholz and Defereggen to Huben in the Valley of the Isel, where it is cut by the Iseltal Fault. Proofs of pre-existing nappe boundaries, ductile, mylonitic shear zones with low angle normal faulting and top E sense of shear and partly left-lateral transpressive kinematics during Cretaceous and Paleogene times are observed. Followed by dextral strike-slip transtensive kinematics (parallel to the Rieserferner plutonic body) from the upper Oligocene to the Miocene. (Mancktelow et al., 2001)
definition: Das etwa W-E-streichende ca. 70 km lange Störungssystem südlich des Tauern-Fensters verläuft von Vals (nördlich von Brixen) über das Antholz- und Defereggental bis Huben im Iseltal, wo es von der Iseltal-Störung abgeschnitten wird. Eine kreidezeitliche bis Paläogene Anlage mit duktilen Myloniten in niedrigwinkelig abschiebenden Scherzonen mit top E-gerichteten Schersinnen und sinistral transpressiver Kinematik bis ins obere Oligozän (parallel zur Intrusion des Rieserferners) ist beschrieben. Diese wurde von dextral transtensiver Kinematik im Miozän überprägt. (Mancktelow et al., 2001) @de
references: https://data.geoscience.earth/ncl/geoera/ref/838
notation: AT-107
type: Concept
created: 2020-04-30T14:27:01.388Z
preferred label: Defereggen-Antholz-Vals-Störungssystem @de
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Tauern Window Subfault System
references: https://data.geoscience.earth/ncl/geoera/ref/770
notation: AT-552
type: Concept
created: 2020-04-30T14:27:02.593Z
definition: This ENE-WSW, partly NE-SW trending Subfault System is a fault set of parallel and conjugated shear zones and faults in the western part of the Tauern window with ductile left-lateral movement during the Miocene (Schneider et al., 2013). It includes the Ahorn-, Olperer-, Tux-, Greiner-, and Ahrntal Shear zones amongst other similar orientated faults with same kinematics.
definition: Dieses ENE-WSW-, teilweise NE-SW-streichende Teilstörungssystem ist ein Störungsset von parallel verlaufenden und konjugierten Scherzonen und Störungen im westlichen Tauernfenster mit duktiler, sinistral seitenverschiebender Kinematik aktiv während des Miozän (Schneider et al., 2013). Es beinhaltet die Ahorn-, Olperer-, Tux-, Greiner- und Ahrntal-Scherzonen sowie weitere ähnlich orientierte Scherzonen und Störungen. @de
preferred label: Tauernfenster-Teilstörungssystem @de
narrower: Ahrntal Shear Zone
narrower: Greiner Shear Zone
narrower: Unlasseck-Leiterer Shear Zone
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Unlasseck-Leiterer Shear Zone
definition: The ENE-WSW trending ductile shear zone in the western Tauern window with left-lateral movement was active during the Miocene. (Hintersberger & Iglseder, 2017 subm.)
definition: Die ENE-WSW-streichende Scherzone im westlichen Tauernfenster mit duktiler, sinistral seitenverschiebender Kinematik war während des Miozäns aktiv. (Hintersberger & Iglseder, 2017) @de
notation: AT-1076
type: Concept
created: 2020-04-30T14:27:02.677Z
preferred label: Unlasseck-Leitherer-Scherzone @de
in scheme: Tectonic Boundary Objects in Europe
broader: Tauern Window Subfault System

Greiner Shear Zone
definition: The ENE-WSW trending ductile shear zone in the western Tauern window with left-lateral movement was active during the Miocene. (Schneider et al., 2013)
definition: Die ENE-WSW-streichende Scherzone im westlichen Tauernfenster mit duktiler, sinistral seitenverschiebender Kinematik war während des Miozäns aktiv. (Schneider et al., 2013) @de
references: https://data.geoscience.earth/ncl/geoera/ref/770
notation: AT-1016
type: Concept
created: 2020-04-30T14:27:02.650Z
preferred label: Greiner-Scherzone @de
notation: IT-4197
in scheme: Tectonic Boundary Objects in Europe
broader: Penninic Domain
broader: Tauern Window Subfault System

Ahrntal Shear Zone
definition: The ENE-WSW trending ductile shear zone in the western Tauern window with left-lateral kinematics was active during the Miocene. (Schneider et al., 2013)
definition: Die ENE-WSW-streichende Scherzone im westlichen Tauernfenster mit duktiler, sinistral seitenverschiebender Kinematik war während des Miozäns aktiv. (Schneider et al., 2013) @de
references: https://data.geoscience.earth/ncl/geoera/ref/770
notation: AT-1002
type: Concept
created: 2020-04-30T14:27:02.622Z
preferred label: Ahrntal-Scherzone @de
in scheme: Tectonic Boundary Objects in Europe
broader: Tauern Window Subfault System

Gurktal Alps Subfault System
references: https://data.geoscience.earth/ncl/geoera/ref/739
notation: AT-522
type: Concept
created: 2020-04-30T14:27:02.509Z
definition: This WNW-ESE and partly NW-SE trending Subfault System consists of parallel trending conjugated faults in the Gurktal Alps, showing top-to-the-WNW thrusting and right-lateral strike-slip faults since late Eocene times. (Ratschbacher et al., 1989)
definition: Dieses WNW-ESE-, teilweise NW-SE-streichende Teilstörungssystem ist ein Störungsset von parallel verlaufenden und konjugierten Störungen in den Gurktaler Alpen, welche post-Eozäne top WNW-aufschiebende und dextral seitenverschiebende Kinematik zeigen. (Ratschbacher et al., 1989) @de
preferred label: Gurktaler Alpen-Teilstörungssystem @de
narrower: Trogscharten Fault
narrower: Gurk Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Gurk Fault
references: https://data.geoscience.earth/ncl/geoera/ref/852
notation: AT-10100
type: Concept
created: 2020-04-30T14:27:02.565Z
definition: This NW-SE trending fault is part of the Gurktal Alps Subfault System. (Oberhauser & Bauer, 1980)
definition: Ist eine NW-SE-streichende Störung des Gurktaler-Alpen-Teilstörungssystems. (Oberhauser & Bauer, 1980) @de
preferred label: Gurk-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Gurktal Alps Subfault System

Trogscharten Fault
references: https://data.geoscience.earth/ncl/geoera/ref/791
notation: AT-10472
type: Concept
created: 2020-04-30T14:27:02.536Z
definition: The steep NW-SE striking fault runs from St. Lorenzen ob Murau to Grades im Meinitz Tal. Presumably, the eastern block was lowered. (Neubauer, 1980)
definition: Die steilstehende NW-SE streichende Störung verläuft von St. Lorenzen ob Murau bis Grades im Meinitz-Tal. Vermutlich wurde der Ostblock abgesenkt. (Neubauer, 1980) @de
preferred label: Trogscharten-Störung @de
in scheme: Tectonic Boundary Objects in Europe
broader: Gurktal Alps Subfault System

Klostertal Fault
definition: The approximately E-W striking right lateral brittle strike-slip fault runs from Nenzing to Roppen (Buchroithner, 1984; Tollmann, 1986).
references: https://data.geoscience.earth/ncl/geoera/ref/772
references: https://data.geoscience.earth/ncl/geoera/ref/732
type: Concept
created: 2020-04-30T14:27:03.724Z
preferred label: Klostertal-Störung @de
notation: AT-10154
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Austria

Tectonic Boundary in Germany
narrower: transition North German Basin / Anglo Dutch Basin
narrower: Anglo-Dutch Basin
in scheme: Tectonic Boundary Objects in Europe
created: 2021-05-03T08:55:14.394Z
type: Concept
top concept of: Tectonic Boundary Objects in Europe
notation: DE-0
scope note: The fault data considered are characterized by regional variations in density and detail, different degree of generalization and origin. Therefore, different display scales are recommended for the respective data sets: 1.) German onshore (1: 2500000 - 1: 500000), 2.) Baltic Sea (1:1000000 - 1:250000), 3.) Central German North Sea (1:1000000 - 1:100000), 4.) Entenschnabel region - The northwestern German North Sea sector (1:1000000 - 1:50000). The focus of the concepts presented here follows the idea of assigning faults to different structural (sub)domains, each characterized by a specific tectonic-sedimentary development. The fault data of the Central German North Sea consist of generalized fault intersections with 13 Mesozoic to Cenozoic horizons and the Late Paleozoic Base Zechstein (Baldschuhn et al. 2001). For the northwestern part of the German North Sea, the Entenschabel, faults originate on interpretations of 3D-seismic data from the GPDN-Project (https://www.gpdn.de/; Arfai et al. 2014). Fault data of the Baltic Sea are based on the studies of Seidel et al. (2018), Seidel (2019) and fault intersections of 13 Mesozoic to Cenozoic horizons as well as the base Zechstein and base Upper Rotliegend from Doornenbal & Stevenson (2010). For the HIKE-fault data base these fault intersections were assigned, where useful, to individual faults or fault systems. Even if fault intersections spatially overlap, a direct linkage of a Meso-Cenozoic fault with the Pre-Zechstein must be questioned, as salt often acts as a decoupling element between the overburden and basement. Fault data for the onshore area of Germany originate on the data compiled within the Geothermal Atlas (Schulz et al. 2013). These data are made up of an integration and merging from different map series, such as e.g. the Geological surface map of Germany (e.g., Toloczyki et al., 2006), the Geotectonic Atlas of North West Germany and the German North Sea Sector (e.g., Baldschuhn et al. 2001), the Southern P…
definition: Representations of principal and overarching tectonic boundaries displayed in the HIKE Fault data base presented for entire Germany by the BGR are in an overview scale and are named by the notation DE. For some German Federal States, more detailed concepts are available with prefixed DE-ISO 3166-2 code.
narrower: North German Basin - domain II: uplifted and/ or inverted southern regions of the North German Basin
narrower: Bohemian Massif & East German Variscan to Pre-Variscan basement highs
narrower: Münsterland Cretaceous Basin
narrower: Upper Rhine Graben
narrower: Lower Rhine Bight
narrower: SE Central Netherlands Basin domain
narrower: Rhenish Massif domain
narrower: Trier Bight & Gulf of Luxembourg domain
narrower: Saar-Nahe Basin domain
narrower: Merziger Graben & SW Saarland Triassic platform domain
narrower: Pfalz-Pirmasens-Nancy Trough
narrower: Swabian - Franconian - South Thuringian Block
narrower: South German Molasse Basin
narrower: German Alps
narrower: German Cenozoic Volcanic regions
narrower: Cenozoic impact Nördlinger Ries
narrower: German basement highs
narrower: North German Basin - domain I: North German Plain & Central German North Sea
narrower: Rynkøbing-Fyn-Møn-Arkona highs
narrower: Skurup Block
narrower: Teisseyre-Tornquist Zone (TTZ)
references: https://data.geoscience.earth/ncl/geoera/ref/8052
references: https://data.geoscience.earth/ncl/geoera/ref/8097
references: https://data.geoscience.earth/ncl/geoera/ref/8101
references: https://data.geoscience.earth/ncl/geoera/ref/91
source: references germany.pdf
contributor: schmar
modified: 2021-09-07T15:16:51.782Z

Rhenish Massif domain
applied type: Fault
type: Fault
type: Limit
narrower: Taunuskamm thrust
narrower: Sackpfeifen thrust
narrower: Neuwieder Basin subdomain
narrower: Eifel North - South zone subdomain
narrower: Siegen main thrust
narrower: Wittlich Depression subdomain
narrower: Rauendahl fault
type: Concept
created: 2021-07-23T08:59:09.408Z
creator: schmar
notation: DE-958
notation: DE-1018
notation: DE-1019
notation: DE-1020
notation: DE-961
narrower: Bopparder thrust
narrower: Ebbe thrust
narrower: Ennepe fault
in scheme: Tectonic Boundary Objects in Europe
narrower: Oberhausener fault
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11571
references: https://data.geoscience.earth/ncl/geoera/ref/12182
references: https://data.geoscience.earth/ncl/geoera/ref/12187
references: https://data.geoscience.earth/ncl/geoera/ref/12030
references: https://data.geoscience.earth/ncl/geoera/ref/12224
references: https://data.geoscience.earth/ncl/geoera/ref/12123
references: https://data.geoscience.earth/ncl/geoera/ref/12246
definition: The SW-NE striking Rhenish Massif domain represents a long-living Mesozoic to Tertiary basement high. Most of the rocks show a Variscan age deformation. It is bordered to the south by the Hunsrück southern rim fault (DE-29) and Taunuskamm thrust (DE-189) and to the North by the Münsterland Cretaceous basin. [Domain type: Variscan basement block, Basement: Rhenohercynian.]
scope note: We describe the Rhenish Massif as a tectonostratigraphic basement unit, whose boundaries are defined by faults and especially by outcop pattern of the Pre-Zechstein. The extent of this structural unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
broader: Tectonic Boundary in Germany
broader: Rhenohercynian basement domain

Eifel North - South zone subdomain
type: Concept
created: 2021-07-23T08:59:08.919Z
creator: schmar
notation: DE-1020
in scheme: Tectonic Boundary Objects in Europe
alternative label: Eifel North - South zone fault set
references: https://data.geoscience.earth/ncl/geoera/ref/12212
definition: A North-South oriented zone in the transition from the Rhenish Schiefergebirge to the Ardennes. In the south the Triassic of the Trier Bight & Gulf of Luxembourg lies on the Rhenish Massif. The kinematics and history of this structural element have not yet been clarified. [Domain type: Undefined crustal zone, Basement: Rhenohercynian.]
scope note: We describe the Eifel North - South Zone as a diffuse tectonic element, a N-S striking syncline with relicts of Mesozoic strata on top. The unit is roughly defined by the extent of the syncline. The extent of this unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
broader: Rhenish Massif domain

Bopparder thrust
type: Concept
created: 2021-07-23T08:59:09.411Z
creator: schmar
notation: DE-324
notation: DE-331
notation: DE-332
notation: DE-333
notation: DE-334
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12252
broader: Rhenish Massif domain

Ebbe thrust
type: Concept
created: 2021-07-23T08:59:09.415Z
creator: schmar
notation: DE-197
notation: DE-907
notation: DE-216
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12252
broader: Rhenish Massif domain

Ennepe fault
type: Concept
created: 2021-07-23T08:59:09.418Z
creator: schmar
notation: DE-215
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12252
broader: Rhenish Massif domain

Oberhausener fault
type: Concept
created: 2021-07-23T08:59:08.894Z
creator: schmar
notation: DE-249
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12252
broader: Rhenish Massif domain

Rauendahl fault
type: Concept
created: 2021-07-23T08:59:08.779Z
creator: schmar
notation: DE-684
references: https://data.geoscience.earth/ncl/geoera/ref/12252
in scheme: Tectonic Boundary Objects in Europe
alternative label: Rauendahler fault
definition: Undefined fault within the Münsterland Cretaceous Basin
broader: Rhenish Massif domain
broader: Münsterland Cretaceous Basin

Sackpfeifen thrust
type: Concept
created: 2021-07-23T08:59:08.900Z
creator: schmar
notation: DE-222
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12252
broader: Rhenish Massif domain

Siegen main thrust
type: Concept
created: 2021-07-23T08:59:08.904Z
creator: schmar
notation: DE-237
notation: DE-238
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12252
broader: Rhenish Massif domain

Taunuskamm thrust
type: Concept
created: 2021-07-23T08:59:08.907Z
creator: schmar
notation: DE-189
notation: DE-323
notation: DE-325
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12252
broader: Rhenish Massif domain

Wittlich Depression subdomain
type: Concept
created: 2021-07-23T08:59:08.911Z
creator: schmar
notation: DE-1018
in scheme: Tectonic Boundary Objects in Europe
alternative label: Wittlicher depression fault set
alternative label: Wittlicher depression
references: https://data.geoscience.earth/ncl/geoera/ref/12212
definition: Permo-Carboniferous basin relict on top of Rhenohercynian basement. [Domain type: Post-Variscan basement block, Basement: Rhenohercynian.]
references: https://data.geoscience.earth/ncl/geoera/ref/12222
scope note: We describe the Wittlich depression as a tectonostratigraphic Permo-Carboniferous basement unit on top of Rhenohercynian basement whose boundaries are defined by faults and especially by lithological changes. The extent of this structural unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
broader: Tectonostratigraphic Permo-Caboniferous Übergangsstockwerk
broader: Rhenish Massif domain

Neuwieder Basin subdomain
type: Concept
created: 2021-07-23T08:59:08.915Z
creator: schmar
notation: DE-1019
in scheme: Tectonic Boundary Objects in Europe
alternative label: Neuwieder Basin
references: https://data.geoscience.earth/ncl/geoera/ref/12212
definition: Tertiary to Quaternary Basin. [Domain type: Sedimentary overburden, Basement: Rhenohercynian.]
scope note: We describe the Neuwieder Basin as a Quaternary tectonostratigraphic unit on top of Rhenohercynian basement whose boundaries are defined by faults and especially by lithological changes. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
broader: Rhenish Massif domain

German Cenozoic Volcanic regions
type: Concept
created: 2021-07-23T08:59:09.057Z
creator: schmar
notation: DE-994
narrower: Siebengebirge volcanic field
narrower: East Eifel volcanic field
narrower: West Eifel volcanic field
narrower: Vogelsberg volcanic complex
narrower: Hegau Volcanic field
narrower: Heldburg Gangschar
narrower: Hocheifel Volcanic field
narrower: Lausitz Volcanic complex
narrower: North Hessian volcanic complex
narrower: Urach Volcanic field
narrower: Westerwald Volcanic field
narrower: Rhön Volcanic field
scope note: We describe the German Cenozoic Volcanic regions as a compilation of Cenozoic-Quaternary (rather rare Late Cretaceous) volcanic fields/regions, whose boundaries are defined by the todays distribution of effusive rocks and volcanos. The here used outline is only a rough estimate of the volcanic region with regard to a further necessary inclusion of additional indications for volcanic activity (e.g. mofettes, seismicity - earthquake swarm regions, uplift). The outlines of each volcanic field/region was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK1000. For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12216
references: https://data.geoscience.earth/ncl/geoera/ref/12222
references: https://data.geoscience.earth/ncl/geoera/ref/12243
definition: Accompanied with the formation of the ECRIS an up to 1200 km wide intraplate magmatism developed, also known as European Cenozoic Volcanic province (ECVP). Only few centers of volcanism are located directly within the graben formed in the context of ECRIS. Instead, some are located up to 200 km away from the rift structures. In Germany the main centers are the Vogelsberg, Eifel, Westerwald and Rhön (Fig. 19a, country sheet).
broader: Tectonic Boundary in Germany

Urach Volcanic field
type: Concept
created: 2021-07-23T08:59:09.089Z
creator: schmar
notation: DE-1039
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12243
scope note: We describe the Urach volcanic field as a volcanic field, whose boundaries are defined by the todays distribution of effusive rocks and volcanos. The here used outline is only a rough estimate of the volcanic region with regard to a further necessary inclusion of additional indications for volcanic activity (e.g. mofettes, seismicity - earthquake swarm regions, uplift). The outline of the volcanic field was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK1000. For References see also Tectonic boundaries in Germany.
broader: German Cenozoic Volcanic regions

Westerwald Volcanic field
type: Concept
created: 2021-07-23T08:59:09.092Z
creator: schmar
notation: DE-1044
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12243
scope note: We describe the Westerwald volcanic field as a volcanic field, whose boundaries are defined by the todays distribution of effusive rocks and volcanos. The here used outline is only a rough estimate of the volcanic region with regard to a further necessary inclusion of additional indications for volcanic activity (e.g. mofettes, seismicity - earthquake swarm regions, uplift). The outline of the volcanic field was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK1000. For References see also Tectonic boundaries in Germany.
broader: German Cenozoic Volcanic regions

Siebengebirge volcanic field
type: Concept
created: 2021-07-23T08:59:09.060Z
creator: schmar
notation: DE-1023
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12243
definition: The Siebengebirge volcanic field subdomain belongs to the European Cenozoic Volcanic province and is located at the Rhenish Massif domain.
scope note: We describe the Siebengebirge volcanic field as a volcanic field whose boundaries are defined by the todays distribution of effusive rocks and volcanos. The here used outline is only a rough estimate of the volcanic region with regard to a further necessary inclusion of additional indications for volcanic activity (e.g. mofettes, seismicity - earthquake swarm regions, uplift). The outline of the volcanic field was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK1000. For References see also Tectonic boundaries in Germany.
broader: German Cenozoic Volcanic regions

Rhön Volcanic field
type: Concept
created: 2021-07-23T08:59:09.095Z
creator: schmar
notation: DE-1021
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12243
definition: The Rhön Volcanic field subdomain belongs to the European Cenozoic Volcanic complex and is characterized by Saxonthuringian - Mid-German crystalline high basement.
scope note: We describe the Rhön volcanic field as a volcanic field whose boundaries are defined by the todays distribution of effusive rocks and volcanos. The here used outline is only a rough estimate of the volcanic region with regard to a further necessary inclusion of additional indications for volcanic activity (e.g. mofettes, seismicity - earthquake swarm regions, uplift). The outline of the volcanic field was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK1000. For References see also Tectonic boundaries in Germany.
broader: German Cenozoic Volcanic regions

East Eifel volcanic field
type: Concept
created: 2021-07-23T08:59:09.064Z
creator: schmar
notation: DE-979
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12243
definition: The domain of the Eifel volcanic field belongs to the European Cenozoic Volcanic province and is characterized by Pleistocene to recent activity. Volcanic centers are aligned at SE-striking faults.
scope note: We describe the East Eifel volcanic field as a volcanic field, whose boundaries are defined by the todays distribution of effusive rocks and volcanos. The here used outline is only a rough estimate of the volcanic region with regard to a further necessary inclusion of additional indications for volcanic activity (e.g. mofettes, seismicity - earthquake swarm regions, uplift). The outline of the volcanic field was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK1000. For References see also Tectonic boundaries in Germany.
broader: German Cenozoic Volcanic regions

West Eifel volcanic field
type: Concept
created: 2021-07-23T08:59:09.067Z
creator: schmar
notation: DE-1043
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12243
scope note: We describe the West Eifel volcanic field as a volcanic field, whose boundaries are defined by the todays distribution of effusive rocks and volcanos. The here used outline is only a rough estimate of the volcanic region with regard to a further necessary inclusion of additional indications for volcanic activity (e.g. mofettes, seismicity - earthquake swarm regions, uplift). The outline of the volcanic field was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK1000. For References see also Tectonic boundaries in Germany.
broader: German Cenozoic Volcanic regions

Vogelsberg volcanic complex
type: Concept
created: 2021-07-23T08:59:09.070Z
creator: schmar
notation: DE-1040
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12243
scope note: We describe the Vogelsberg volcanic complex as a volcanic complex whose boundaries are defined by the todays distribution of effusive rocks and volcanos. The here used outline is only a rough estimate of the volcanic region with regard to a further necessary inclusion of additional indications for volcanic activity (e.g. mofettes, seismicity - earthquake swarm regions, uplift). The outline of the volcanic field was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK1000. For References see also Tectonic boundaries in Germany.
broader: German Cenozoic Volcanic regions

Hegau Volcanic field
type: Concept
created: 2021-07-23T08:59:09.073Z
creator: schmar
notation: DE-1005
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12243
definition: The Hegau Volcanic field subdomain belongs to the European Cenozoic Volcanic complex domain and is assumed to be associated with the Freidorf-Bonndorf fault system. Age outcrop: Middle Miocene (volcanics), Neogene (Molasse sediments)
scope note: We describe the Hegau as a volcanic field, whose boundaries are defined by the todays distribution of effusive rocks and volcanos. The here used outline is only a rough estimate of the volcanic region with regard to a further necessary inclusion of additional indications for volcanic activity (e.g. mofettes, seismicity - earthquake swarm regions, uplift). The outline of the volcanic field was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK1000. For References see also Tectonic boundaries in Germany.
broader: German Cenozoic Volcanic regions

Heldburg Gangschar
type: Concept
created: 2021-07-23T08:59:09.076Z
creator: schmar
notation: DE-995
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12243
definition: The Heldburg Gangschar subdomain belongs to the European Cenozoic Volcanic complex domain and is characterized by NNE to N striking volcanic dykes of Eocene to Middle Miocene age.
scope note: We describe the Heldburg Gangschar as a volcanic field, whose boundaries are defined by the todays distribution of effusive rocks and volcanos. The here used outline is only a rough estimate of the volcanic region with regard to a further necessary inclusion of additional indications for volcanic activity (e.g. mofettes, seismicity - earthquake swarm regions, uplift). The outline of the volcanic field was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK1000. For References see also Tectonic boundaries in Germany.
broader: German Cenozoic Volcanic regions

Hocheifel Volcanic field
type: Concept
created: 2021-07-23T08:59:09.080Z
creator: schmar
notation: DE-996
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12243
definition: The Hocheifel volcanic field subdomain belongs to the European Cenozoic Volcanic complex domain and the Eifel plume therein.
scope note: We describe the Hocheifel volcanic field as a volcanic field, whose boundaries are defined by the todays distribution of effusive rocks and volcanos. The here used outline is only a rough estimate of the volcanic region with regard to a further necessary inclusion of additional indications for volcanic activity (e.g. mofettes, seismicity - earthquake swarm regions, uplift). The outline of the volcanic field was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK1000. For References see also Tectonic boundaries in Germany.
broader: German Cenozoic Volcanic regions

Lausitz Volcanic complex
type: Concept
created: 2021-07-23T08:59:09.083Z
creator: schmar
notation: DE-997
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12243
definition: The Lausitz volcanic complex subdomain belongs to the European Cenozoic Volcanic complex domain and is located SE of the Lausitz Block domain.
scope note: We describe the Lausitz volcanic complex as a volcanic complex whose boundaries are defined by the todays distribution of effusive rocks and volcanos. The here used outline is only a rough estimate of the volcanic region with regard to a further necessary inclusion of additional indications for volcanic activity (e.g. mofettes, seismicity - earthquake swarm regions, uplift). The outline of the volcanic complex was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK1000. For References see also Tectonic boundaries in Germany.
broader: German Cenozoic Volcanic regions

North Hessian volcanic complex
type: Concept
created: 2021-07-23T08:59:09.086Z
creator: schmar
notation: DE-1012
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12243
definition: The North Hessian Volcanic complex subdomain belongs to the European Cenozoic Volcanic complex, is located within the Hessian depression and characterized by Rhenoherzynian basement.
scope note: We describe the North Hessian volcanic complex as a volcanic complex, whose boundaries are defined by the todays distribution of effusive rocks and volcanos. The here used outline is only a rough estimate of the volcanic region with regard to a further necessary inclusion of additional indications for volcanic activity (e.g. mofettes, seismicity - earthquake swarm regions, uplift). The outline of the volcanic complex was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK1000. For References see also Tectonic boundaries in Germany.
broader: German Cenozoic Volcanic regions

North German Basin - domain II: uplifted and/ or inverted southern regions of the North German Basin
type: Concept
created: 2021-07-23T08:59:08.212Z
creator: schmar
notation: DE-1066
narrower: southern Eichsfeld-Altmark Swell
narrower: Thuringian Depression
narrower: Gardelegen-Flechtingen-Rosslau Uplift
narrower: Subhercynian Basin
narrower: Harz fault set
narrower: Thuringian Forest fault set
narrower: southwestern fringe of the Bohemian Massif & the Thuringian Forest subdomains
narrower: Northwestern Saxony Basement Block
scope note: We define here the North German Basin - domain II as a tectonostratigraphic unit, whose boundaries are defined both by faults and fault systems, often fuzzy trends in the lithofacies and, in particular by the expression of deformation events. The division into two domains of the North German Basin (NGB) is intended to indicate in particular the uplift of some basin regions during the Late Cretaceous and the associated different levels of erosion in this region. Depending on the level of erosion and the preservation of signs of former deformation phases, this results in regionally partly different dominant fault patterns, even if these deformation phases have influenced almost the entire basin. The Lower Saxony Basin, which was actually also strongly inverted during the Late Cretaceous, should therefore actually be part of domain II of the NGB: uplifted and/ or inverted southern regions of the North German Basin. However, it is also largely part of the German lowlands. In this respect, the subdivision made here should only be understood as a rough classification. The extent of the tectonostratigraphic domain was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
narrower: Halle-Wittenberg Block
narrower: Prignitz-Lausitz-Riesengebirge Anticline
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/12192
references: https://data.geoscience.earth/ncl/geoera/ref/12215
references: https://data.geoscience.earth/ncl/geoera/ref/12223
references: https://data.geoscience.earth/ncl/geoera/ref/8022
narrower: Northern Kraichgau & Grabfeld Depression subdomain
definition: This tectonic domain covers uplifted areas of some regions of the southern NGB. Structures within the southern NGB were partly inverted or steep basement thrusts were created during the Late Cretaceous. The result is a much stronger erosion of the Mesozoic basin fill as in the northern parts of the NGB.
narrower: Hessian Depression
broader: Tectonic Boundary in Germany

southern Eichsfeld-Altmark Swell
type: Concept
created: 2021-07-23T08:59:08.312Z
creator: schmar
notation: DE-935
narrower: Leinetal graben fault system
narrower: Harz western boundary fault
narrower: Oberkatz graben fault system
narrower: Werra Uplift
scope note: We define here the Eichsfeld-Altmark Swell as a tectonostratigraphic sub-domain of the North German Basin, whose boundaries are not clearly defined by faults and fault systems. The outline of the domain can only be roughly defined based on lithostratigraphic trends and on the base of differences in the deformation pattern to surrounding areas. But several NNE-striking fault zones and grabens lies within this tectonic unit. Even though the main structures of this region have been described in detail (e. g. Röhling, 1991, Baldschuhn et al., 2001), no clear definition of the outline of this feature has been made to date. Even if the swell still includes large regions in the eastern LSB (DE-917) and along the area of the Braunschweig-Gifhorn-Lüneburg fault system (DE-937), only faults in the east of the Hessian Depression (southern segment of the swell) in particular are assigned to this domain in this classification. The extent of this tectonic unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
narrower: Gelliehausen fault zone
narrower: Rengelrode graben zone
references: https://data.geoscience.earth/ncl/geoera/ref/12162
references: https://data.geoscience.earth/ncl/geoera/ref/12230
references: https://data.geoscience.earth/ncl/geoera/ref/8092
definition: The Eichsfeld-Altmark Swell represents a supra-regional, long living swell, which has impact on the tectono-sedimentary development of several structural regions within the NGB, such as parts of the Thuringian Depression, the Braunschweig-Gifhorn-Lüneburg fault system, Altmark-Fläming Depression, Lower Saxony Basin or the Leinetal Graben and also on parts of the southwestern fringe of the Bohemian Massif subdomain. Domain type: Supra-regional long-living swell, Main-Activity: Permian, Triassic, important separating element during Late Cretaceous contraction; Basement: mainly Rhenohercynian, within the inner part also Northern Phyllite Zone and within the outer part also Avalonia & Saxothuringian.
broader: North German Basin - domain II: uplifted and/ or inverted southern regions of the North German Basin

Leinetal graben fault system
type: Concept
created: 2021-07-23T08:59:08.316Z
creator: schmar
notation: DE-139
notation: DE-140
notation: DE-141
notation: DE-145
notation: DE-440
notation: DE-441
notation: DE-857
notation: DE-864
notation: DE-865
notation: DE-905
in scheme: Tectonic Boundary Objects in Europe
broader: southern Eichsfeld-Altmark Swell

Harz western boundary fault
type: Concept
created: 2021-07-23T08:59:08.323Z
creator: schmar
notation: DE-147
in scheme: Tectonic Boundary Objects in Europe
definition: The Harz western boundary fault extends over 52 km in N-S direction along the western rim of the Harz.
broader: southern Eichsfeld-Altmark Swell

Oberkatz graben fault system
type: Concept
created: 2021-07-23T08:59:08.329Z
creator: schmar
notation: DE-250
in scheme: Tectonic Boundary Objects in Europe
broader: southern Eichsfeld-Altmark Swell

Werra Uplift
type: Concept
created: 2021-07-23T08:59:08.332Z
creator: schmar
notation: DE-1042
in scheme: Tectonic Boundary Objects in Europe
definition: The Werra Uplift is a ESE/SE striking Late Cretaceous basement high/anticline SW of the Harz between the Hessian Depression in the west and the Thuringian Syncline in the east. Paleozoic sediments are exposed in the core area of the uplift. However, the majority of this uplift structure is covered by Triassic sediments.
alternative label: faults in the Rhenohercynian units of the Werra Uplift
scope note: We describe the Werra Anticline as a tectonostratigraphic unit, whose boundaries are defined by faults and especially by outcop pattern of the Pre-Zechstein and Early Triassic. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK 1:200000 of Thuringia, GK 1:300000 of Hesse. For References see also Tectonic boundaries in Germany.
broader: southern Eichsfeld-Altmark Swell
broader: Rhenohercynian basement domain

Gelliehausen fault zone
type: Concept
created: 2021-07-23T08:59:08.343Z
creator: schmar
notation: DE-146
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The Gelliehausen fault is a NNE-SSW striking, narrow graben-like fault zone located predominantly within the western section of the Eichsfeld-Block with stratigraphic sequences of Middle Buntsandstein at the margins and deposits of Upper Buntsandstein and Lower Muschelkalk in the center of the fault zone. In the western Thuringian area this fault zone formed a narrow graben.
broader: Thuringian Syncline
broader: southern Eichsfeld-Altmark Swell

Rengelrode graben zone
type: Concept
created: 2021-07-23T08:59:08.346Z
creator: schmar
notation: DE-148
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The Rengelrode fault zone is a NNE-SSW striking narrow grabenin the southwestern section of the Eichsfeld Block with stratigraphic sequences of the Lower Muschelkalk as graben fill and deposits of the Middle Buntsandstein on the eastern flank and Upper Buntsandstein on the western flank.
broader: Thuringian Syncline
broader: southern Eichsfeld-Altmark Swell

southwestern fringe of the Bohemian Massif & the Thuringian Forest subdomains
references: https://data.geoscience.earth/ncl/geoera/ref/8031
type: Concept
created: 2021-07-23T08:59:08.978Z
creator: schmar
notation: DE-1026
notation: DE-1027
notation: DE-1028
notation: DE-1029
notation: DE-1030
notation: DE-1031
narrower: South Thuringian-Franconian fault zones & uplifts
narrower: Franconian Jurassic-Cretaceous Depression
narrower: Bodenwöhr half-graben
narrower: Weiden Basin
definition: It is an area under Mesozoic cover that is partly also uplifted but show also relicts of Jurassic in synforms and Upper Cretacous in foreland basins along the uplift of the Bohemian Massif. Several NW-SE striking Mesozoic fault zones (partly inverted) cross this structural unit and bound it in parts. The Northeastern part of this structural unit formed during the Late Cretaceous also belongs to the southern rim of the North German Basin.
scope note: We describe the southwestern fringe of Bohemian Massif & Thuringian Forest as a tectonostratigraphic unit, which is mainly influenced by uplift & denudation history of the Mid-German and Bohemian basement highs. The outline of this structural unit is mainly defined by the occurrence of basement uplifts under Mesozoic cover as well as the distributional pattern of Jurassic and Late Cretaceous. The northeastern border ist defined by the faults of the Franconian Lineament as well as the outcrops of Pre-Zechstein Basement. The transition to structural units to the West/Southwest is not always sharply defined. In the northwest, the Grabfeld flexure is a possible structure at which one could define the limit of the structural unit. The extent of this unit was newly created with a view to a structured assignment of generalized overview fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Bavaria (LFU) provides and describes a more detailed and partly updated fault data set of Bavaria within the framework of the HIKE project (DE-BY_1356). Map Reference: GK 1:200000 of Thuringia, GK 1:100000 of the Thuringian Forest (Kästner, 1996), GK 1:500000 of Bavaria (Freudenberger & Schwerd, 1996), tectonic map of Bavaria 1:1000000 (Freudenberger & Schwerd, 1996). For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12188
references: https://data.geoscience.earth/ncl/geoera/ref/12189
references: https://data.geoscience.earth/ncl/geoera/ref/12206
references: https://data.geoscience.earth/ncl/geoera/ref/12232
references: https://data.geoscience.earth/ncl/geoera/ref/753
alternative label: southwestern fringe of Bohemian Massif & Thuringian Forest
broader: Swabian - Franconian - South Thuringian Block
broader: North German Basin - domain II: uplifted and/ or inverted southern regions of the North German Basin

South Thuringian-Franconian fault zones & uplifts
notation: DE-1107
type: Concept
created: 2021-07-23T08:59:08.982Z
creator: schmar
scope note: We describe the South Thuringian-Franconian fault zones & uplifts as a tectonostratigraphic unit, whose boundaries are defined by faults and regional uplifts as well as the today's erosional pattern. The extent of this unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Bavaria (LFU) provides and describes a more detailed and partly updated fault data set of Bavaria within the framework of the HIKE project (DE-BY_1356). Map Reference: GK 1:1000000, GK 1:500000 of Bavaria (Freudenberger & Schwerd, 1996), tectonic map of Bavaria 1:1000000 (Freudenberger & Schwerd, 1996), HIKE (DE-BY 1356). For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
definition: Several NW-SE striking Mesozoic fault zones (partly inverted) cross this structural unit and bound it in parts. [Domain type: Basement uplifts under Mesozoic cover; Basement: Rhenohercynian/Saxothuringian/Moldanubian.]
broader: southwestern fringe of the Bohemian Massif & the Thuringian Forest subdomains

Franconian Jurassic-Cretaceous Depression
type: Concept
created: 2021-07-23T08:59:08.986Z
creator: schmar
notation: DE-1029
narrower: Vilseck Depression
narrower: Hollfeld-Veldenstein-Sulzbach-Kallmünz Depression
scope note: We describe the Franconian Jurassic-Cretaceous Depression as a tectonostratigraphic unit, whose boundaries are only in sections defined by faults but also are defined on the base of distributional pattern of Cretaceous and Jurassic sedimentary successions. The extent of this unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Bavaria (LFU) provides and describes a more detailed and partly updated fault data set of Bavaria within the framework of the HIKE project (DE-BY_1356). Map Reference: GK 1:1000000, GK 1:500000 of Bavaria (Freudenberger & Schwerd, 1996), tectonic map of Bavaria 1:1000000 (Freudenberger & Schwerd, 1996), HIKE (DE-BY 1356). For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12188
references: https://data.geoscience.earth/ncl/geoera/ref/12189
references: https://data.geoscience.earth/ncl/geoera/ref/12243
references: https://data.geoscience.earth/ncl/geoera/ref/753
definition: Domain type: Deformed sedimentary overburden, Basement: Moldanubian/Saxothuringian.
broader: southwestern fringe of the Bohemian Massif & the Thuringian Forest subdomains

Vilseck Depression
type: Concept
created: 2021-07-23T08:59:08.990Z
creator: schmar
notation: DE-1026
scope note: We describe the Vilseck Depression as a tectonostratigraphic sub-unit of the Franconian Jurassic-Cretaceous Depression, whose boundaries are only in sections defined by faults but also are defined on the base of distributional pattern of the Late Cretaceous sedimentary successions. The extent of this unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Bavaria (LFU) provides and describes a more detailed and partly updated fault data set of Bavaria within the framework of the HIKE project (DE-BY_1356). Map Reference: GK 1:1000000, GK 1:500000 of Bavaria (Freudenberger & Schwerd, 1996), tectonic map of Bavaria 1:1000000 (Freudenberger & Schwerd, 1996), HIKE (DE-BY 1356). For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12188
references: https://data.geoscience.earth/ncl/geoera/ref/12189
references: https://data.geoscience.earth/ncl/geoera/ref/12243
references: https://data.geoscience.earth/ncl/geoera/ref/753
definition: The Vilseck depression subdomain represents a Late Cretaceous foreland depression/graben and is located at the southwestern fringe of the Bohemian Massif. [Domain type: Late Cretaceous foreland basin, Basement: Moldanubian.]
broader: Franconian Jurassic-Cretaceous Depression

Hollfeld-Veldenstein-Sulzbach-Kallmünz Depression
type: Concept
created: 2021-07-23T08:59:08.994Z
creator: schmar
notation: DE-1027
scope note: We describe the Hollfeld-Veldenstein-Sulzbach-Kallmünz Depression as a tectonostratigraphic sub-unit of the Franconian Jurassic-Cretaceous Depression whose boundaries are only in sections defined by faults but also are defined on the base of distributional pattern of the Late Cretaceous sedimentary successions. The extent of this unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Bavaria (LFU) provides and describes a more detailed and partly updated fault data set of Bavaria within the framework of the HIKE project (DE-BY_1356). Map Reference: GK 1:1000000, GK 1:500000 of Bavaria (Freudenberger & Schwerd, 1996), tectonic map of Bavaria 1:1000000 (Freudenberger & Schwerd, 1996), HIKE (DE-BY 1356). For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12188
references: https://data.geoscience.earth/ncl/geoera/ref/12189
references: https://data.geoscience.earth/ncl/geoera/ref/12243
references: https://data.geoscience.earth/ncl/geoera/ref/753
definition: The Hollfeld - Veldenstein - Sulzbach - Kallmünz depression subdomain is located within the southwestern fringe of the Bohemian Massif and is characterized by the Hollfeld & Keilberg fault zone as the extension of the Bavarian Pfahl. [Domain type: Late Cretaceous foreland basin, Basement: Moldanubian/Saxothuringian.]
broader: Franconian Jurassic-Cretaceous Depression

Bodenwöhr half-graben
type: Concept
created: 2021-07-23T08:59:08.997Z
creator: schmar
notation: DE-1028
scope note: We describe the Bodenwöhr half-grabens as a tectonostratigraphic unit (Late Cretaceous foreland Basin of the uplifted Bohemian Massif), whose boundaries are defined by faults as well as the distribution of Late Cretaceous sediments. The extent of this unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Bavaria (LFU) provides and describes a more detailed and partly updated fault data set of Bavaria within the framework of the HIKE project (DE-BY_1356). Map Reference: GK 1:1000000, GK 1:500000 of Bavaria (Freudenberger & Schwerd, 1996), tectonic map of Bavaria 1:1000000 (Freudenberger & Schwerd, 1996), HIKE (DE-BY 1356). For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12188
references: https://data.geoscience.earth/ncl/geoera/ref/12189
references: https://data.geoscience.earth/ncl/geoera/ref/12243
references: https://data.geoscience.earth/ncl/geoera/ref/753
definition: The Bodenwöhr Half-graben subdomain is located within the southwestern fringe of the Bohemian Massif and is related to the Bavarian Pfahl. [Domain type: Late Cretaceous foreland basin, Basement: Moldanubian.]
broader: southwestern fringe of the Bohemian Massif & the Thuringian Forest subdomains

Weiden Basin
type: Concept
created: 2021-07-23T08:59:09.000Z
creator: schmar
notation: DE-1030
scope note: We describe the Weiden Basin as a tectonostratigraphic unit (Late Cretaceous foreland Basin of the uplifted Bohemian Massif), whose boundaries are defined by faults as well as the distribution of Late Cretaceous sediments. The extent of this unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Bavaria (LFU) provides and describes a more detailed and partly updated fault data set of Bavaria within the framework of the HIKE project (DE-BY_1356). Map Reference: GK 1:1000000, GK 1:500000 of Bavaria (Freudenberger & Schwerd, 1996), tectonic map of Bavaria 1:1000000 (Freudenberger & Schwerd, 1996), HIKE (DE-BY 1356). For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12188
references: https://data.geoscience.earth/ncl/geoera/ref/12189
references: https://data.geoscience.earth/ncl/geoera/ref/12243
references: https://data.geoscience.earth/ncl/geoera/ref/753
definition: The Weiden basin is located within the southwestern fringe of the Bohemian Massif and is related to the Franconian line. [Domain type: Late Cretaceous foreland basin, Basement: Moldanubian/Saxothuringian.]
broader: southwestern fringe of the Bohemian Massif & the Thuringian Forest subdomains

Subhercynian Basin
type: Concept
created: 2021-07-23T08:59:08.572Z
creator: schmar
notation: DE-1033
notation: DE-1034
narrower: Subhercynian Cretaceous Basin
narrower: Egge-Kellerwald fault system
narrower: Altmorschen-Neukirchen fault system
narrower: North Hessian & Solling Block
narrower: Leinetal Graben
narrower: Southern Hessian Depression
scope note: We describe the Subhercynian Basin as a tectonostratigraphic sub-unit within uplifted parts of the North German Basin. The boundaries of the Subhercynian Basin are defined mainly by fault zones and faulted flexures as well as by outcop pattern made by deep erosion as a result of Late Cretaceous compression and uplift of this tectonic blocks. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Saxony-Anhalt provides and describes a partly more detailed and updated fault data set of Saxony-Anhalt within the framework of the HIKE project (DE-ST-0, DE-ST-4000). Map Reference: Röllig et al. (1990), Beutler (2001), Martiklos et al. (2001), existing outlines: e.g. Katzung & Ehmke (1993), Franke (2020), Beutler (2001), Martiklos et al. (2001). For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12164
references: https://data.geoscience.earth/ncl/geoera/ref/8071
references: https://data.geoscience.earth/ncl/geoera/ref/8052
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: Strongly uplifted part of the North German Basin between the basement highs of Flechtingen-Roßlau in the north and the Harz in the south. The preserved Mesozoic sedimentary cover show mainly ESE/SE striking elements which have a Triassic extensional history and are later overprinted by Late Cretaceous contractional tectonics.
broader: North German Basin - domain II: uplifted and/ or inverted southern regions of the North German Basin

Subhercynian Cretaceous Basin
type: Concept
created: 2021-07-23T08:59:08.576Z
creator: schmar
notation: DE-1034
scope note: The Subhercynian Cretaceous Basin is a sub-unit of the Subhercynian Basin/depression. We describe the Subhercynian Cretaceous Basin as a tectonostratigraphic unit, whose boundaries are defined mainly by outcop pattern of Cretaceous north of the Harz Mountains. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Saxony-Anhalt provides and describes a partly more detailed and updated fault data set of Saxony-Anhalt within the framework of the HIKE project (DE-ST-0, DE-ST-4000). Map Reference: Röllig et al. (1990), Beutler (2001), Martiklos et al. (2001), existing outlines: e.g. Katzung & Ehmke (1993), Franke (2020), Beutler (2001), Martiklos et al. (2001). For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12164
references: https://data.geoscience.earth/ncl/geoera/ref/8071
references: https://data.geoscience.earth/ncl/geoera/ref/8052
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The Subhercynian Cretaceous Basin represents a Late Cretaceous foreland basin in front of the Harz Northern boundary fault. It is part of the Subhercynian Basin. [Domain type: Late Cretaceous forland basin, Basement type: Rhenohercynian.]
broader: Subhercynian Basin

Egge-Kellerwald fault system
scope note: We describe the Egge-Kellerwald fault system as a fault system which separates the Münsterland Basin from the Hessian Depressian of the southern North German Basin. The cluster of sub-parallel faults in this region can sometimes reach several km to a few tens of km in width, and a discrete transition between the Hessian depression and the Münsterland Basin cannot be clearly defined along the entire fault system. The extent of this unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK 1:300000 of Hesse, Baldschuhn et al. (2001), Ziegler (1990), GK 1:1000000 of Germany. For References see also Tectonic boundaries in Germany.
type: Concept
created: 2021-07-23T08:59:08.579Z
creator: schmar
notation: DE-1055
narrower: Fritzlar-Naumburg graben zone
in scheme: Tectonic Boundary Objects in Europe
definition: Predominantly N/NNW striking faults and Triassic grabens, with partially transpressive reactivation during Late Cretaceous times. The structural subdomain is characterized by a strongly deformed overburden. [Domain type: strongly deformed sedimentary overburden, Basement: mainly Rhenohercynian. Outcrop age: Triassic]
broader: Subhercynian Basin
broader: Hessian Depression

Fritzlar-Naumburg graben zone
type: Concept
created: 2021-07-23T08:59:08.583Z
creator: schmar
notation: DE-130
notation: DE-132
in scheme: Tectonic Boundary Objects in Europe
broader: Egge-Kellerwald fault system

Altmorschen-Neukirchen fault system
scope note: We describe the Altmorschen-Neukirchen fault system as a fault system which separates the Thuringian Basin and the structures of the eastern Eichsfeld-Altmark Swell from the Hessian Depressian. The cluster of sub-parallel faults in this region can sometimes reach several km to a few tens of km in width and a discrete transition between the Hessian depression and the Münsterland Basin cannot be clearly defined along the entire fault system. The extent of this unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK 1:300000 of Hesse, Baldschuhn et al. (2001), Ziegler (1990), GK 1:1000000 of Germany. For References see also Tectonic boundaries in Germany.
type: Concept
created: 2021-07-23T08:59:08.586Z
creator: schmar
notation: DE-1056
in scheme: Tectonic Boundary Objects in Europe
definition: NNE/NE Triassic faults and graben within the Hessian Trough/Depression. [Domain type: strongly deformed sedimentary overburden, Basement: Rhenohercynian. Outcrop age: Triassic]
broader: Subhercynian Basin
broader: Hessian Depression

North Hessian & Solling Block
type: Concept
created: 2021-07-23T08:59:08.589Z
creator: schmar
notation: DE-1057
scope note: We describe the North Hessian & Solling Block as a tectonostratigraphic sub-unit of the northern Hessian depression. The eastern and western boundaries of the Hessian Depression are today traced through larger fault systems. However, the actual structure has smooth transitions of paleofacial trends to neighbouring tectonostratigraphic blocks. In particular, the boundaries to the Lower Saxony Basin and to the Münsterland Basin cannot be clearly defined. The extent of this unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK 1:300000 of Hesse, Baldschuhn et al. (2001), Ziegler (1990), GK 1:1000000 of Germany. For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
narrower: Falkenhagen Graben
definition: The North Hessian and Solling Block represents the transition between the North German Basin domain and the Hessian Trough/Depression. The block is characterized by few deformation and scattered faults and grabens. The structural subdomain is characterized by a deformed overburden and mainly Rhenohercynian basement. [Outcrop age: Triassic]
broader: Subhercynian Basin
broader: Hessian Depression

Falkenhagen Graben
type: Concept
created: 2021-07-23T08:59:07.641Z
creator: schmar
notation: DE-856
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
broader: SE Lower Saxony Basin
broader: North Hessian & Solling Block

Leinetal Graben
type: Concept
created: 2021-07-23T08:59:08.596Z
creator: schmar
notation: DE-1058
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12213
definition: The Leinetal graben is a N/NNE striking Triassic (Keuperous?) graben, which was reactivated in Late Cretaceous times and presumably during the Cenozoic. The structural subdomain is characterized by a strongly deformed overburden and a Rhenohercynian basement. Outcrop age: Triassic
scope note: We describe the Leinetal Graben as a fault system in the northwest of the Hessian Depression. Even though the main structures of this region have been described in detail (e. g. Leiss et al. (2011)), no clear definition of the whole outline of this tectonic unit and associated fault system has been made to date. The extent of this unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK 1:300000 of Hesse, Baldschuhn et al. (2001). For References see also Tectonic boundaries in Germany.
broader: Subhercynian Basin
broader: Hessian Depression

Southern Hessian Depression
scope note: We describe the Southern Hessian Depression as a tectonostratigraphic sub-unit of the southern Hessian Depression/Trough. The structure has smooth transitions of paleofacial trends to neighbouring tectonostratigraphic blocks and is only partly bordered by faults. In particular, within this study the boundaries to neighbouring tectonostratigraphic units cannot be clearly defined. The extent of this unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: e.g. GK 1:300000 of Hesse, GK 1:1000000. For References see also Tectonic boundaries in Germany.
type: Concept
created: 2021-07-23T08:59:08.599Z
creator: schmar
notation: DE-1059
in scheme: Tectonic Boundary Objects in Europe
definition: The subdomain of the Southern Hessian Depression represents the less deformed part of the entire Hessian Depression and is characterized by partially slightly inverted Triassic grabens. The structural subdomain is characterized by a slightly deformed overburden and Northern Phyllite zone basement. [Outcrop age: Triassic, mainly BLower Triassic]
broader: Subhercynian Basin
broader: Hessian Depression

Prignitz-Lausitz-Riesengebirge Anticline
scope note: We describe the Prignitz-Lausitz-Riesengebirge Anticline as a tectonostratigraphic unit, whose boundaries are defined by faults and especially by distribution and outcop pattern of Mesozoic sedimentary successions at the Base of Tertiary and at the surface. The defined tectonostratigraphic unit lies within the two defined domains of the NGB (North German Basin - domain I: North German Plain & Central German North Sea / North German Basin - domain II: uplifted and/ or inverted southern regions of the North German Basin). Even though the main structures of this region have been described (e. g. Voigt., 2009), no clear definition of the outline of this basin part has been made to date. The extent of this tectonostratigraphic unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map reference: based on outlines from Röllig et al. 1990. Definition of outline is comprehensively described by Voigt (2009). Outlines recorded based on the circumscribing outcrop of Lower Cretaceous-Early Upper Cretaceous from Röllig et al. (1990) in the area of the North German Plain. To the southeast, the circumscribing outcrop of the Triassic around the Lusatian Block was followed (circumscribing also indicates uplift of the structure). Further to the SE, the boundaries of the basement unit Lusatian Block were traced, each of which is bordered by Upper Cretaceous basins. Uncertainties: Especially in the NW the unit is characterized by broad trend of a flat NW-SE striking anticline, which is not bordered by discrete structures. The extent is roughly derived from subsurface-outcrop maps. To the southeast, basement outcrops give no clear evidence for the underlying structure other…
type: Concept
created: 2021-07-23T08:59:07.925Z
creator: schmar
notation: DE-942
narrower: Prignitz Wall
definition: The NW-SE striking tectonostratigraphic domain of the Prignitz-Lausitz-Riesengebirge anticlinal zone is a summary of previously defined structural elements of the Tafeldeckgebirge and the basement that show similar development during Jurassic-Lower Cretaceous & Upper Cretaceous. A large number of the faults strike NW-SE, crossing elements such as the Triassic Rheinsberg Trough show NNE strike. The tectonostratigraphic domain describes an area characterized by Jurassic-Lower Cretaceous basin/graben formation as well as a Upper Cretaceous structural inversion (Voigt, 2009).Thereby this structure resembles in its development the Lower Saxony Basin or Broad Fourteens Basin. The southeastern area of the subdomain became more uplifted during the Upper Cretaceous than the remaining sections. The Saxony-Czech Cretaceous Basin (Elbkreide) adjacent to the south, proves the structural inversion along this subdomain. Towards the NW the amount of Cretaceous inversion decreases along the structure, so that in the northwestern area sediments of the Malm and Lower Cretaceous are still preserved. Domain type: Supra-regional uplift, Basement: Avalonia/Rhenohercynian/Saxothuringian/Moldanubian(?).
narrower: Rheinsberg Trough
in scheme: Tectonic Boundary Objects in Europe
narrower: Lausitz Block
references: https://data.geoscience.earth/ncl/geoera/ref/12244
references: https://data.geoscience.earth/ncl/geoera/ref/8071
broader: North German Basin - domain II: uplifted and/ or inverted southern regions of the North German Basin
broader: North German Basin - domain I: North German Plain & Central German North Sea

Rheinsberg Trough
scope note: We describe the Rheinsberg Trough as a tectonostratigraphic unit of the North German Basin. It is a pre-existing early to middle Mesozoic sedimentary trough crossed by the later Jurassic to Cretaceous structure of the Prignitz Wall. It is only roughly outlined by the Mesozoic fault and salt structure pattern. Even though the main structures of this region have been described (e. g. Scheck & Bayer, 1999), no clear definition of the outline of this basin part has been made to date. The extent of this tectonic unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map reference: Scheck & Bayer (1999). The outline is the sum of the envelope of the areas with the highest Jurassic and Keuper thicknesses (Scheck & Bayer, 1999) and the NNE striking Triassic structural elements according to Doornenbal & Stevenson (2010). The Rheinsberg Trough designation is based on thickness maps after Scheck & Bayer (1999). Their data basis is not clearly shown. Likewise, the trough is only traced in thickness trends. Only with the present thickness trends together with the salt structures of the region and the faults shown in Doornenbal & Stevenson (2010) a coherent structural picture emerges. The blocks and lineaments defined by Beutler & Stackebrandt (2012) partly give a completely opposite structural picture. Although the existence of this structure is undisputed, its outlines have not yet been clearly depicted with certainty. For References see also Tectonic boundaries in Germany.
type: Concept
created: 2021-07-23T08:59:07.918Z
creator: schmar
notation: DE-943
alternative label: Rheinsberg Trough subdomain
in scheme: Tectonic Boundary Objects in Europe
narrower: Rheinsberg deep fracture
references: https://data.geoscience.earth/ncl/geoera/ref/8022
references: https://data.geoscience.earth/ncl/geoera/ref/7996
references: https://data.geoscience.earth/ncl/geoera/ref/8097
definition: The subdomain of the Triassic to Jurassic Rheinsberg Trough runs transverse to the later developing structure of the Prignitz Wall. The general NW-SE alignment of the Prignitz Wall is interrupted in this area by a dominant NNE strike of the structures (faults, salt structures). [Domain type: Deformed sedimentary overburden, Basement: Avalonia/Rhenohercynian.]
broader: North German Basin - domain I: North German Plain & Central German North Sea
broader: Prignitz-Lausitz-Riesengebirge Anticline

Rheinsberg deep fracture
type: Concept
created: 2021-07-23T08:59:07.958Z
creator: schmar
notation: DE-569
notation: DE-570
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The 108 km long, NNW-SSW running Rheinberg deep fracture belongs to the Rheinsberg Trough and crosses to the Prignitz-Lausitz-Riesengebirge Anticline subdomain.
broader: Prignitz Wall
broader: Rheinsberg Trough

Prignitz Wall
narrower: Schönewalde fault
narrower: Wittenberg fault
type: Concept
created: 2021-07-23T08:59:07.928Z
creator: schmar
notation: DE-1067
narrower: Schweinitz fault
narrower: Potsdam fault
narrower: Hoyerswerda fault
narrower: Groß-Köris-Merzdorf fault system
narrower: Rheinsberg deep fracture
narrower: Lausitz Escarpment
scope note: We describe the Prignitz Wall as a tectonostratigraphic unit, whose boundaries are defined by faults and especially by the distribution and outcop pattern of sedimentary successions at the Base of Tertiary and at the surface. Even though the main structures of this region have been described (e. g. Voigt., 2009), no clear definition of the outline of this basin part has been made to date. The extent of this tectonostratigraphic unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Saxony-Anhalt provides and describes a partly more detailed and updated fault data set of Saxony-Anhalt within the framework of the HIKE project (DE-ST-0, DE-ST-1000). Map reference: based on outlines from Röllig et al. (1990). Outlines recorded based on the circumscribing outcrop of Lower Cretaceous-Early Upper Cretaceous from Röllig et al. (1990) in the area of the North German Plain. Especially in the NW the unit is characterized by broad trend of a flat NW-SE striking anticline, which is not bordered by discrete structures. The extent is roughly derived from subsurface-outcrop maps. Individual structural elements are named and described in Katzung & Ehmke (1993) and Franke (2020). For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
narrower: Lower Elbe fault
references: https://data.geoscience.earth/ncl/geoera/ref/12244
references: https://data.geoscience.earth/ncl/geoera/ref/8071
definition: It is defined as a NW-SE elongated sedimentary high of Jurassic to Lower Cretaceous strata below Tertiary cover. Within this region Jurassic to Lower Cretaceous strata show partly higher thicknesses as the surrounding. Voigt (2009) interpreted this structure as an inverted Jurassic-Lower Cretaceous Basin /Graben which was inverted during the Late Cretaceous.
broader: Prignitz-Lausitz-Riesengebirge Anticline

Groß-Köris-Merzdorf fault system
type: Concept
created: 2021-07-23T08:59:07.860Z
creator: schmar
notation: DE-621
notation: DE-623
notation: DE-625
notation: DE-634
alternative label: Groß Köris - Merzdorfer fault zone
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The NW-SE running Groß-Köris-Merzdorf fault system is a ca. 100 km long, SW-dipping zone with associated salt structures in the East Brandenburg-North Sudetes depression within the thrusted Central North German basin. The fault system consists of several single faults.
broader: Prignitz Wall
broader: East-Brandenburg - North Sudetes Depression

Lausitz Escarpment
alternative label: Lausitz fault
type: Concept
created: 2021-07-23T08:59:08.276Z
creator: schmar
notation: DE-635
in scheme: Tectonic Boundary Objects in Europe
definition: The NW-SE running Lausitz fault is a probably young paleozoic formed, several times reactivated deep fault located between the East Brandenburg-North Sudetes depression and the Prignitz-Lausitz-Riesengebirge Anticlinal zone in the SW. Within the SE-part this fault represents the separation between the variscian Paleozoic of the Görlitz Syncline and the young-paleozoic to mesozoic cover of the North Sudetes depression. The throw of the normal fault decreases in NW-direction continuously. Several NE-SW running faults interesect the Lausitz fault. Major activity is documented inbetween Buntsandstein and Upper Cretaceous times, younger activity is documented for Lower Miocene and only minor activity during post-Miocene.
references: https://data.geoscience.earth/ncl/geoera/ref/8031
broader: Prignitz Wall
broader: Lausitz Anticlinorium
broader: Görlitz Synclinorium subdomain
broader: East-Brandenburg - North Sudetes Depression

Hoyerswerda fault
type: Concept
created: 2021-07-23T08:59:07.948Z
creator: schmar
notation: DE-630
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The NNE-SSW oriented and 29 km long Hoyerswerda fault is located within the Prignitz-Lausitz-Riesengebirge Anticline subdomain, and represents a prominent cross fault of the Lausitz fault (DE-635). Fault activity is documented up to the Cenozoic.
broader: Görlitz Synclinorium subdomain
broader: Prignitz Wall
broader: Lausitz Anticlinorium

Schönewalde fault
type: Concept
created: 2021-07-23T08:59:08.718Z
creator: schmar
notation: DE-560
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The 58 km long, NW-SE running Schönewalde fault is located within the Prignitz-Lausitz-Riesengebirge Anticline subdomain. The SW-dipping fault shows throws of 100 to 200 m, recent reactivations are documented.
broader: Prignitz Wall
broader: Torgau-Doberlug Synclinorium

Wittenberg fault
type: Concept
created: 2021-07-23T08:59:08.528Z
creator: schmar
notation: DE-540
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8071
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The 106 km long, NW-SE oriented Wittenberg fault represents in the SE-part the border between the Prignitz-Lausitz-Riesengebirge anticline subdomain and the Halle-Wittenberg Block subdomain, and in the NW-part the border between the subdomains Altmark Fläming depression and Gardelegen-Flechtingen-Rosslau uplift. The Wittenberg fault is a listric, SW-dipping reverse fault, that was formed during inversion in Uppper Cretaceous times. Throws of up to >2000 m are documented.
broader: Halle-Wittenberg Block
broader: Altmark Fläming Depression
broader: Prignitz Wall

Schweinitz fault
type: Concept
created: 2021-07-23T08:59:07.938Z
creator: schmar
notation: DE-543
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12164
definition: The 23 km long, NW-SE running Schweinitz fault is located within the Prignitz-Lausitz-Riesengebirge Anticline subdomain.
broader: Prignitz Wall

Potsdam fault
related: Potsdam Fault Zone
type: Concept
created: 2021-07-23T08:59:07.945Z
creator: schmar
notation: DE-561
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The 42 km long, W-E oriented Potsdam fault is located within the Prignitz-Lausitz-Riesengebirge Anticline subdomain, and is interpreted as the western extension of the Buckow fault. A fault throw between 250-300 m is documented.
broader: Prignitz Wall

Lower Elbe fault
related: Lower Elbe Lineament - Barenthin Fault
type: Concept
created: 2021-07-23T08:59:08.150Z
creator: schmar
notation: DE-507
in scheme: Tectonic Boundary Objects in Europe
alternative label: Unterelbe fault
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The 24 km long, WNW-ESE running Lower Elbe fault is located with the eastern part within the Prignitz-Lausitz-Riesengebirge Antinclinal zone and with the northwestern part within the Central North German Basin (Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression). The fault is a listric, SW-dipping reverse fault that was reactivated in the course of Upper Cretaceous inversion.
broader: Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression
broader: Prignitz Wall

Lausitz Block
narrower: Torgau-Doberlug Synclinorium
type: Concept
created: 2021-07-23T08:59:09.251Z
creator: schmar
notation: DE-960
notation: DE-1053
notation: DE-1054
narrower: Görlitz Synclinorium subdomain
in scheme: Tectonic Boundary Objects in Europe
narrower: Mühlberg Depression
notation: DE-1064
narrower: Lausitz Anticlinorium
references: https://data.geoscience.earth/ncl/geoera/ref/12232
references: https://data.geoscience.earth/ncl/geoera/ref/8052
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: A Basment High which is partly under Tertiary cover. The outcropping basement show mainly Variscan deformation. This Basement High is part and presumably the most uplifted part of the Late Cretaceous anticlinal uplift of the Prignitz-Lausitz-Riesengebirge Anticline. [Domain type: Variscan to Pre-Variscan basement block, Basement: Saxothuringian.]
scope note: We describe the Lausitz Block as a tectonic basement unit, whose boundaries are defined by faults and especially by outcop pattern of the Pre-Zechstein Basement. The extent of this tectonostratigraphic unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: Röllig et al. (1990), existing outlines: e.g. Katzung & Ehmke (1993), Franke (2020)
broader: Bohemian Massif & East German Variscan to Pre-Variscan basement highs
broader: Saxothuringian basement domain
broader: Prignitz-Lausitz-Riesengebirge Anticline

Torgau-Doberlug Synclinorium
type: Concept
created: 2021-07-23T08:59:08.705Z
creator: schmar
notation: DE-1053
narrower: Doberlug fault zone
narrower: Schönewalde fault
in scheme: Tectonic Boundary Objects in Europe
narrower: Finsterwald fault zone
narrower: Großenhain fault
alternative label: Torgau-Doberlug Synclinorium subdomain
references: https://data.geoscience.earth/ncl/geoera/ref/12232
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/8052
definition: The Torgau-Doberlug Synclinorium subdomain is one of structural elements that mantle the Bohemian Massif in the north. This subdomain show mainly Paleozoic rocks with Variscan age deformation and belongs to the Lausitz Block. [Domain type: Variscan basement block, Basement: Saxothuringian.]
scope note: We describe the Torgau-Doberlug Synclinorium as a tectonic basement unit, whose boundaries are defined by faults and especially by outcop pattern of the Pre-Zechstein Basement. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: Röllig et al. (1990), existing outlines: e.g. Katzung & Ehmke (1993), Franke (2020). For References see also Tectonic boundaries in Germany.
broader: Lausitz Block

Finsterwald fault zone
type: Concept
created: 2021-07-23T08:59:08.269Z
creator: schmar
notation: DE-559
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8052
definition: The 36 km long, WSE-ENE oriented Finsterwald fault zone is located within the Prignitz-Lausitz-Riesengebirge Anticline subdomain.
broader: Lausitz Anticlinorium
broader: Torgau-Doberlug Synclinorium

Doberlug fault zone
type: Concept
created: 2021-07-23T08:59:08.711Z
creator: schmar
notation: DE-556
in scheme: Tectonic Boundary Objects in Europe
definition: The 32 km long, WSW-ENE oriented Doberlug fault is located within the Prignitz-Lausitz-Riesengebirge Anticline subdomain.
broader: Torgau-Doberlug Synclinorium
broader: Mühlberg Depression

Großenhain fault
type: Concept
created: 2021-07-23T08:59:08.724Z
creator: schmar
notation: DE-555
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The 87 km long, NW-SE oriented Großenhain fault is is located within the Prignitz-Lausitz-Riesengebirge Anticline subdomain. While the fault is characterized by a 200 m wide ductile fault zone in the SE, the fault shows brittle deformation and high fracturing/joins in the NW.
broader: Torgau-Doberlug Synclinorium
broader: Mühlberg Depression
broader: Lausitz Anticlinorium
broader: Halle-Wittenberg Block

Görlitz Synclinorium subdomain
type: Concept
created: 2021-07-23T08:59:09.255Z
creator: schmar
notation: DE-960
in scheme: Tectonic Boundary Objects in Europe
narrower: Hoyerswerda fault
alternative label: Görlitz Synclinorium
narrower: Inner Lausitz fault
narrower: Lausitz Escarpment
references: https://data.geoscience.earth/ncl/geoera/ref/12232
references: https://data.geoscience.earth/ncl/geoera/ref/8052
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The Görlitz Synclinorium is one of structural elements that mantle the Bohemian Massif in the north. This subdomain show mainly Paleozoic rocks with Variscan age deformation and belongs to the Lausitz Block. [Domain type: Variscan basement block, Basement: Saxothuringian.]
scope note: We describe the Görlitz Synclinorium as a tectonic basement unit, whose boundaries are defined by faults and especially by outcop pattern of the Pre-Zechstein basement. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: Röllig et al. (1990), Existing outlines: e.g. Katzung & Ehmke (1993), Franke (2020). For References see also Tectonic boundaries in Germany.
broader: Lausitz Block

Inner Lausitz fault
type: Concept
created: 2021-07-23T08:59:08.737Z
creator: schmar
notation: DE-637
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12229
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: WNW-ESE oriented and 36 km long fault within the Prignitz-Lausitz-Riesengebirge Anticline subdomain. Fault throws of up to 800-1000 m are observed.
broader: Görlitz Synclinorium subdomain
broader: Lausitz Anticlinorium

Mühlberg Depression
type: Concept
created: 2021-07-23T08:59:08.253Z
creator: schmar
notation: DE-1054
in scheme: Tectonic Boundary Objects in Europe
narrower: Doberlug fault zone
narrower: Großenhain fault
references: https://data.geoscience.earth/ncl/geoera/ref/12232
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/8052
definition: The Mühlberg depression subdomain represents an uplifted part of the North German basin. It represent Lower Triassic to Rotliegend remnants of the NGB and adjacent platform parts. It can be interpreted as a foreland syncline of an Upper Cretaceous active thrust. [Domain type: foreland syncline of a thrust fault, Basement: Saxothuringian.]
scope note: We describe the Mühlberg Depression as a tectonostratigraphic unit (erosional relict on top of basement high) whose boundaries are defined by faults and especially by outcop pattern of the Triassic as well as Zechstein and Upper Rotliegend. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: Röllig et al. (1990), existing outlines: e.g. Katzung & Ehmke (1993), Franke (2020). For References see also Tectonic boundaries in Germany.
broader: Lausitz Block

Lausitz Anticlinorium
narrower: Finsterwald fault zone
narrower: Lausitz Escarpment
type: Concept
created: 2021-07-23T08:59:08.721Z
creator: schmar
notation: DE-1060
narrower: Großenhain fault
narrower: Inner Lausitz fault
narrower: Lausitz thrust
in scheme: Tectonic Boundary Objects in Europe
narrower: Hoyerswerda fault
references: https://data.geoscience.earth/ncl/geoera/ref/12232
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/8052
definition: The Lausitz Anticlinorium is one of structural elements that mantle the Bohemian Massif in the north. This subdomain show mainly Paleozoic rocks with Variscan age deformation and belongs to the Lausitz Block. [Domain type: Variscan basement block, Basement: Saxothuringian.]
scope note: We describe the Lausitz Anticlinorium as a tectonic basement unit, whose boundaries are defined by faults and especially by outcop pattern of the Pre-Zechstein basement. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: Röllig et al. (1990), existing outlines: e.g. Katzung & Ehmke (1993), Franke (2020)
broader: Lausitz Block

Lausitz thrust
type: Concept
created: 2021-07-23T08:59:08.740Z
creator: schmar
notation: DE-639
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12232
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The 48 km long, WNW-ESE running Lusatian overthrust fault is located at the Prignitz-Lausitz-Riesengebirge Anticline subdomain and the Lausitz block therein. The SW-dipping reverse fault is characterized by Lower Cretaceous main activity and a throw of 500-1000 m.
broader: Lausitz Anticlinorium

Hessian Depression
created: 2021-08-31T12:26:04.246Z
type: Concept
creator: schmar
in scheme: Tectonic Boundary Objects in Europe
notation: DE-1055
notation: DE-1056
notation: DE-1057
notation: DE-1058
notation: DE-1059
preferred label: Hessische Senke @de
alternative label: Hessian Trough
alternative label: Hessischer Trog @de
scope note: We describe the "Hessian Depression" as a tectonostratigraphic sub-unit within uplifted parts of the North German Basin. The East and West boundaries of the Hessian Depression are today traced through larger fault systems. However, the actual structure has smooth transitions of paleofacial trends to neighbouring tectonostratigraphic blocks. In particular, the boundaries to the Lower Saxony Basin and to the structures of the "süddeutsche Großscholle" cannot be clearly defined. The extent of this unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK 1:300000 of Hesse, Baldschuhn et al. (2001), Ziegler (1990), GK 1:1000000 of Germany. For References see also „Tectonic boundaries in Germany”.
definition: The Hessian Depression is a NNE-SSW elongated sub-basin of the NGB and is more or less aligned and controlled during the Triassic - Jurassic(?) by surrounding swells like the Eichsfeld-Altmark swell. As a result this sub-basin of the NGB show a Triassic basin evolution, as well as in parts graben tectonics (e.g. Leinetal Graben) and a Late Cretaceous contractional/transpressional overprint. The southern part of the Hessian Depression is also influenced by Tertiary evolution of the European Rift system and is parlty covered by Tertiary basin sediments. The region is also characterised by intense volcanic activity during the Tertiary period and is overlain in the south by the largest Tertiary volcanic complex known in Germany (Vogelsberg complex).
references: https://data.geoscience.earth/ncl/geoera/ref/12241
narrower: Egge-Kellerwald fault system
narrower: Altmorschen-Neukirchen fault system
narrower: North Hessian & Solling Block
narrower: Leinetal Graben
narrower: Southern Hessian Depression
broader: North German Basin - domain II: uplifted and/ or inverted southern regions of the North German Basin

Gardelegen-Flechtingen-Rosslau Uplift
type: Concept
created: 2021-07-23T08:59:08.561Z
creator: schmar
notation: DE-986
narrower: Gardelegen uplift
scope note: We describe the Gardelegen-Flechtingen-Rosslau Uplift as a tectonostratigraphic unit, whose boundaries are defined mainly by faultzones and faulted flexures as well as by outcop pattern made by deep erosion as a result of Late Cretaceous compression and uplift of this tectonic blocks. The Flechtingen-Rosslau Uplift is a strongly uplifted part of the Southern North German Basin basement on which minor synsedimentary deposits of the NGB have been preserved. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Saxony-Anhalt provides and describes a partly more detailed and updated fault data set of Saxony-Anhalt within the framework of the HIKE project (DE-ST-0, DE-ST-3000, DE-ST-2000). Map Reference: Röllig et al. (1990), Beutler (2001), Martiklos et al. (2001), existing outlines: e.g. Katzung & Ehmke (1993), Franke (2020), Beutler (2001), Martiklos et al. (2001). For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
narrower: Haldensleben-Wittenberg uplift
references: https://data.geoscience.earth/ncl/geoera/ref/12164
references: https://data.geoscience.earth/ncl/geoera/ref/8071
references: https://data.geoscience.earth/ncl/geoera/ref/8052
definition: The Gardelegen-Flechtingen-Rosslau uplift domain belongs to the during the Late Cretaceous uplifed southern rim of North German Basin. [Domain type: Mixed basement and sedimentary cover, Basement: Rhenohercynian.]
broader: North German Basin - domain II: uplifted and/ or inverted southern regions of the North German Basin

Haldensleben-Wittenberg uplift
scope note: We describe the Haldensleben-Wittenberg uplift as a tectonostratigraphic basement unit, whose boundaries are defined mainly by fault zones and faulted flexures as well as by outcop pattern made by deep erosion as a result of Late Cretaceous compression and uplift of this tectonic blocks. The Haldensleben-Wittenberg uplift is a strongly uplifted part of the Southern North German Basin basement on which no/minor synsedimentary deposits of the NGB have been preserved. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Saxony-Anhalt provides and describes a partly more detailed and updated fault data set of Saxony-Anhalt within the framework of the HIKE project (DE-ST-0, DE-ST-2000, DE-ST-3000). Map Reference: Röllig et al. (1990), Beutler (2001), Martiklos et al. (2001), existing outlines: e.g. Katzung & Ehmke (1993), Franke (2020), Beutler (2001), Martiklos et al. (2001). For References see also Tectonic boundaries in Germany.
type: Concept
created: 2021-07-23T08:59:09.405Z
creator: schmar
notation: DE-988
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12164
references: https://data.geoscience.earth/ncl/geoera/ref/8071
references: https://data.geoscience.earth/ncl/geoera/ref/8052
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: Late Cretaceous basement uplift. The Mesozoic basin fill is only preserved in synforms that can be interpreted as foreland synclines in front of basement thrusts or faulted flexures. [Domain type: Variscan to Post-Variscan basement block, Basement: Rhenohercynian.]
broader: Gardelegen-Flechtingen-Rosslau Uplift
broader: Rhenohercynian basement domain

Gardelegen uplift
type: Concept
created: 2021-07-23T08:59:08.565Z
creator: schmar
notation: DE-987
scope note: We describe the Gardelegen Uplift as a tectonic unit, whose boundaries are defined mainly by fault zones and faulted flexures as well as by outcop pattern made by deep erosion as a result of Late Cretaceous compression and uplift of this tectonic blocks. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Saxony-Anhalt provides and describes a partly more detailed and updated fault data set of Saxony-Anhalt within the framework of the HIKE project (DE-ST-0, DE-ST-2000). Map Reference: Röllig et al. (1990), Beutler (2001), Martiklos et al. (2001), existing outlines: e.g. Katzung & Ehmke (1993), Franke (2020), Beutler (2001), Martiklos et al. (2001). For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12164
references: https://data.geoscience.earth/ncl/geoera/ref/8071
references: https://data.geoscience.earth/ncl/geoera/ref/8052
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: Late Cretaceous basement uplift under Triassic cover. [Domain type: Basement uplifts under Triassic cover, Basement: Rhenohercyonian.]
broader: Gardelegen-Flechtingen-Rosslau Uplift

Harz fault set
scope note: We describe the Harz as a tectonostratigraphic basement unit, whose boundaries are defined by faults in the north and especially by outcop pattern of the Pre-Zechstein in the south. The Harz is a strongly uplifted part of the Southern North German Basin basement on which no synsedimentary deposits of the NGB have been preserved. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: Martiklos et al. (2001), existing outlines: e.g. Katzung & Ehmke (1993), Franke (2020), Martiklos et al. (2001). For References see also Tectonic boundaries in Germany.
type: Concept
created: 2021-07-23T08:59:08.602Z
creator: schmar
notation: DE-992
narrower: Ilfeld Basin fault set
alternative label: Harz Rhenohercynian
definition: The Harz domain is a regional geological unit in the central section of the Rheno-Hercynian zone, which emerges from its environment of Late Paleozoic-Mesozoic-Cenozoic overlays as a horst-like Block running approximately orthogonal to the strike of the Variscan structures. A sharp boundary of the Harz domain is represented by the Harznordrand fault in the northeast, where it may have been overthrust by as much as 5-7 km, but at least 2-3 km, against the Subhercynian Basin. In the southeast, southwest and northwest, the boundary to the surrounding stuctural regions is characterized by unconformities of stratigraphic sequences of the Permosilesian molasse basement and Triassic on the Variscan basement. The Harz is the most prominent Late Cretaceous basement uplift of Mid-Germany. It is the result of NNE directed compression and the northern border fault of the Harz is the main fault of this anticlinal uplift. The Harz Nordrand fault is a steep south dipping basement fault and show partly characteristics of a faulted flexure. [Domain type: Variscan to Post-Variscan basement outcrop, Basement: Mainly Rhenohercynian, in SE Northern Phyllitic zone.]
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
broader: Rhenohercynian basement domain
broader: North German Basin - domain II: uplifted and/ or inverted southern regions of the North German Basin

Ilfeld Basin fault set
type: Concept
created: 2021-07-23T08:59:08.605Z
creator: schmar
notation: DE-993
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12225
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: [Permo-Carboniferous basin; erosional relict. Domain type: Post-Variscan basement outcrop; Basement: Rhenohercynian.]
scope note: We describe the Illfeld Basin as a tectonostratigraphic basement sub-unit, whose boundaries are defined especially by outcop pattern of the Permo-Carboniferous. It lies on the Rhenohercynian basement rocks of the Harz. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: Martiklos et al. (2001), existing outlines: e.g. Katzung & Ehmke (1993), Franke (2020), Martiklos et al. (2001). For References see also Tectonic boundaries in Germany.
broader: Harz fault set

Northwestern Saxony Basement Block
scope note: We describe the Northwestern Saxony Basement Block as a tectonostratigraphic basement unit, whose boundaries are defined by faults in the north and south as well as by outcrop pattern of the Pre-Zechstein. Besides basement outcrops of the Saxothuringian, the northwestern Saxony Basement Block show mostly outcrops of the Permo-Carboniferous Übergangsstockwerk. Northwestern parts of this block also represent uplifted basement of the NGB. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: Franke (2020), Röllig et al. (1990), existing outlines: e.g. Katzung & Ehmke (1993), Franke (2020). For References see also Tectonic boundaries in Germany.
type: Concept
created: 2021-07-23T08:59:09.108Z
creator: schmar
notation: DE-1072
narrower: Landsberg-Naunhof fault
narrower: Marbach fault zone
narrower: Halle fault
in scheme: Tectonic Boundary Objects in Europe
narrower: Köthen-Bitterfeld fault
narrower: Bitterfeld-Wermsdorf fault
narrower: Rötha fault
references: https://data.geoscience.earth/ncl/geoera/ref/12232
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/8052
definition: A basement high with Variscan to Post-Variscan outcrops which is mainly covered by Tertiary sediments. The uplift is the result of Late Cretaceous NNE directed compression. Fault strike: 1st order SE; 2nd order: ENE-NE/NNE
broader: North German Basin - domain II: uplifted and/ or inverted southern regions of the North German Basin
broader: Saxothuringian basement domain
broader: Tectonostratigraphic Permo-Caboniferous Übergangsstockwerk

Landsberg-Naunhof fault
type: Concept
created: 2021-07-23T08:59:09.124Z
creator: schmar
notation: DE-667
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12232
definition: The 42 km long, NW-SE running Landsberg-Naunhof fault is located with the NW-part within the Halle-Wittenberg Block subdomain.
broader: Northwestern Saxony Basement Block
broader: Halle-Wittenberg Block

Marbach fault zone
type: Concept
created: 2021-07-23T08:59:09.128Z
creator: schmar
notation: DE-673
in scheme: Tectonic Boundary Objects in Europe
broader: Northwestern Saxony Basement Block

Köthen-Bitterfeld fault
type: Concept
created: 2021-07-23T08:59:09.269Z
creator: schmar
notation: DE-523
in scheme: Tectonic Boundary Objects in Europe
alternative label: Köthen-Bitterfeld fault zone
references: https://data.geoscience.earth/ncl/geoera/ref/8071
definition: The 67 km long, NW-SE running Köthen-Bitterfeld fault zone is located in the central part of the Halle-Wittenberg Block subdomain.
broader: Halle-Wittenberg Block
broader: Northwestern Saxony Basement Block

Bitterfeld-Wermsdorf fault
type: Concept
created: 2021-07-23T08:59:09.335Z
creator: schmar
notation: DE-557
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12232
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The 35 km long, WNW-ESE running Bitterfeld-Wermsdorf fault is located within the eastern part of the Halle-Wittenberg Block. In this area the Halle-Wittenberg Block shows the highest subsidence, and aside from Siliesian, Permian and Triassic sediments several NW-SE oriented graben-and synclines occur.
broader: Halle-Wittenberg Block
broader: Northwestern Saxony Basement Block

Halle fault
type: Concept
created: 2021-07-23T08:59:09.274Z
creator: schmar
notation: DE-525
in scheme: Tectonic Boundary Objects in Europe
notation: DE-678
references: https://data.geoscience.earth/ncl/geoera/ref/8071
definition: The 50 km long, WNW-ESE running Halle fault represents the border between the Merseburg block subdomain and the Halle-Wittenburg Block subdomain. This variscian fault was reactivated within Upper Jurassic to Cretaceous times. The northeastern located Halle-Wittenberg block was discplaced against the southwestern Merseburg block abouth 600 m, locally 1500 m.
broader: Mansfeld Syncline
broader: Northwestern Saxony Basement Block
broader: Halle-Wittenberg Block

Rötha fault
type: Concept
created: 2021-07-23T08:59:08.492Z
creator: schmar
notation: DE-531
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The 50 km long, WNW-ESE running Rötha fault is located at the border between the Northwestsaxonian Block in the northeast and the eastern part of the Thuringian Syncline in the southwest.
broader: Borna depression
broader: Northwestern Saxony Basement Block
broader: Sangerhausen & Querfurt depressions

Halle-Wittenberg Block
narrower: Wittenberg fault
narrower: Gräfenhainichen fault
type: Concept
created: 2021-07-23T08:59:09.306Z
creator: schmar
notation: DE-954
narrower: Rosslau fault
narrower: Halberstadt fault
narrower: Bitterfeld-Wermsdorf fault
narrower: Löbejün-Brehna fault
in scheme: Tectonic Boundary Objects in Europe
narrower: Torgau fault system
narrower: Großenhain fault
narrower: Halle fault
narrower: Landsberg-Naunhof fault
references: https://data.geoscience.earth/ncl/geoera/ref/12164
references: https://data.geoscience.earth/ncl/geoera/ref/12232
references: https://data.geoscience.earth/ncl/geoera/ref/8071
references: https://data.geoscience.earth/ncl/geoera/ref/8052
references: https://data.geoscience.earth/ncl/geoera/ref/8031
narrower: Köthen-Bitterfeld fault
definition: The subdomain of the Halle-Wittenberg block is a basement high (mostly Permo-Carboniferous) under Tertiary cover. In the eastern part, a band of smaller half-grabens/synclines with Mesozoic and Upper Rotliegend fill runs along the boundary of the block. To the south, these structures are sharply demarcated (probably also foreland depressions of Upper Cretaceous uplifts and thus protected by erosion). Erosion of possibly up to 5 km, today partly under Tertiary cover. Domain type: Predominantly Variscan-to Post-Variscan basement block, partly Mesozoic strata is preserved within Late Cretaceous foreland foreland synclines; Basement: Saxothruringian, locally Mid-German Crystalline High.
scope note: We describe the Halle-Wittenberg Block as a tectonostratigraphic basement unit, whose boundaries are defined by faults and especially by outcop pattern of the Permo-Carboniferous under Tertiary cover. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: Röllig et al. (1990), Beutler (2001), Martiklos et al. (2001), existing outlines: e.g. Katzung & Ehmke (1993), Franke (2020), Beutler (2001), Martiklos et al. (2001). For References see also Tectonic boundaries in Germany.
narrower: Bitterfeld Graben
narrower: Düben Depression
broader: Mid-German Crystalline High
broader: North German Basin - domain II: uplifted and/ or inverted southern regions of the North German Basin

Rosslau fault
type: Concept
created: 2021-07-23T08:59:09.324Z
creator: schmar
notation: DE-542
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8071
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The 25 km long, NE-SW runnig Rosslau fault represents within the pre-Cenozoic the border between the subdomains of the Rosslau-Gardelegen uplift and the Halle-Wittenberg Block. In this sense, the fault represents the boundary between the Northern Phyllite Zone in the northwest and the Mitteldeutsche Crystalline Zone in the southeast.
broader: Halle-Wittenberg Block

Halberstadt fault
type: Concept
created: 2021-07-23T08:59:09.328Z
creator: schmar
notation: DE-553
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8071
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The 20 km long, WNW-ESE running Halberstadt fault is located with the NW-part within the subhercynian basin subdomain and the the SE-part within the Halle-Wittenberg block subdomain.
broader: Halle-Wittenberg Block

Löbejün-Brehna fault
type: Concept
created: 2021-07-23T08:59:09.339Z
creator: schmar
notation: DE-666
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12232
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The 25 km long, WNW-ESE running Lobejün-Brehna fault is located within the southwestern part of the Halle-Wittenberg Block subdomain.
broader: Halle-Wittenberg Block

Bitterfeld Graben
type: Concept
creator: schmar
created: 2021-08-31T12:40:35.440Z
in scheme: Tectonic Boundary Objects in Europe
notation: DE-1102
preferred label: Bitterfelder Graben @de
scope note: We describe the "Bitterfeld Graben" as a tectonostratigraphic unit (erosional relict on top of basement high) whose boundaries are defined by faults and especially by outcop pattern of the Triassic as well as Zechstein and Upper Rotliegend. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: Röllig et al. (1990), existing outlines: e.g. Katzung & Ehmke (1993), Franke (2020). For References see also „Tectonic boundaries in Germany”.
definition: Permian to Lower Triassic sedimentary relict of the NGB. It can be interpreted as a Late Cretaceous thrust foreland depression. Outcrop age: Tertiary - Quaternary cover, Lower Triassic - Permian basin relicts; Basement: Saxothuringian - Mid-German crystalline High; partly covered by Permo-Carboniferous volcanics; fault strike: 1st order: SE / 2nd order: NE
references: https://data.geoscience.earth/ncl/geoera/ref/12164
references: https://data.geoscience.earth/ncl/geoera/ref/8071
references: https://data.geoscience.earth/ncl/geoera/ref/8052
references: https://data.geoscience.earth/ncl/geoera/ref/8031
broader: Halle-Wittenberg Block

Torgau fault system
type: Concept
created: 2021-07-23T08:59:08.553Z
creator: schmar
notation: DE-672
notation: DE-681
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12232
definition: The 40 km long, NNW-SSE running Torgau fault system is located within the northern part of the Halle-Wittenberg Block subdomain. To the south, this fault system is continued by the Großenhain fault.
broader: Halle-Wittenberg Block

Gräfenhainichen fault
type: Concept
created: 2021-07-23T08:59:08.557Z
creator: schmar
notation: DE-916
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8071
definition: The 63 km long, NW-SE running fault is located within the central part of the Halle-Wittenberg Block subdomain.
broader: Halle-Wittenberg Block

Düben Depression
creator: schmar
created: 2021-08-31T12:43:09.326Z
type: Concept
in scheme: Tectonic Boundary Objects in Europe
notation: DE-1103
preferred label: Dübener Becken @de
scope note: We describe the "Düben Depression" as a tectonostratigraphic unit (erosional relict on top of basement high) whose boundaries are defined by faults and especially by outcop pattern of the Triassic as well as Zechstein and Upper Rotliegend. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: Röllig et al. (1990), existing outlines: e.g. Katzung & Ehmke (1993), Franke (2020). For References see also „Tectonic boundaries in Germany”.
definition: Permian to Lower Triassic sedimentary relict of the NGB. It can be interpreted as a Late Cretaceous thrust foreland depression. Outcrop age: Tertiary - Quaternary cover, Lower Triassic - Permian basin relicts, Basement: Saxothuringian; partly covered by Permo-Carboniferous volcanics, fault strike: 1st order: ENE;E/SE / 2nd order: SSE/NNE
references: https://data.geoscience.earth/ncl/geoera/ref/12164
references: https://data.geoscience.earth/ncl/geoera/ref/8071
references: https://data.geoscience.earth/ncl/geoera/ref/8052
references: https://data.geoscience.earth/ncl/geoera/ref/8031
broader: Halle-Wittenberg Block

Thuringian Depression
type: Concept
created: 2021-07-23T08:59:08.336Z
creator: schmar
notation: DE-920
narrower: Thuringian Syncline
narrower: Hermundurian Block
narrower: Mansfeld Syncline
narrower: NW Thuringian Depression (Ohmgebirge, Leinefeld Anticline, Bleicherode Depression)
narrower: Sangerhausen & Querfurt depressions
narrower: Zeitz-Schmölln depression
narrower: Borna depression
definition: The Thuringian Depression is an uplifted and deeply eroded marginal area of the North German Basin in Thuringia. During the Late Cretaceous (Santonian to Campanian) this basin part of the SPB/NGB (uplift after Beyer (2015) 1500 m to 3700 m) as well as the surrounding basement highs (uplift up to 5000 m and more) were uplifted. The main structure representing a NW-SE striking syncline, which is located in between the more strongly uplifted Variscian to Rotliegend basement of the Thuringian forest and Thuringian Schiefergebirge in the south and of the Palaeozoic outcrops of the Harz in the North (Fig. 9, Fig. 11 country sheet). The basin is limited in the West by the Eichsfeld-Altmark Swell and further west by NNE-SSW striking grabens (e.g. Leinetal Graben, Altmorschener Graben) within the northern Hessian Depression. To the NE the basin is limited by several smaller highs (Kyffhäuser, Bottendorfer Höhenzug) along the Kyffhäuser- Crimmitschauer fault zones. The uplifted basin part north of this fault zone is called the Mansfelder Mulde, which in turn is limited to the north by the Halle fault. Accompanying to the broad uplift of this region several NW-SE striking Late Triassic to Jurassic (maybe Early Cretaceous) small grabens were structurally inverted during the Late Cretaceous. Prominent examples for faults and fault zones are the Finne fault, the Kyffhäuser-Crimitschauer or the Eichenberg-Gotha-Saalfelder fault zone. These grabens and fault zones dominate with the exception of a few NNE-SSW striking elements (e.g. Ohmgebirge Graben) and WNW-ESE elongated minor oval uplifts the structural pattern of the Thuringian “Syncline.
scope note: We describe the Thuringian depression as a tectonostratigraphic unit, whose boundaries are defined by basement highs, faults & fault systems as well as of the Eichsfeld-Altmark Swell in the west. Even though the main structures of this region have been described in detail (e. g. Katzung & Ehmke, 1993; Franke, 2020; Seidel, 2003), no clear definition of the outline of this basin part has been made to date. The extent of this tectonostratigraphic unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Saxony-Anhalt provides and describes a partly more detailed and updated fault data set of Saxony-Anhalt within the framework of the HIKE project (DE-ST-0, DE-ST-5000). For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12165
references: https://data.geoscience.earth/ncl/geoera/ref/12238
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/8052
references: https://data.geoscience.earth/ncl/geoera/ref/8101
broader: North German Basin - domain II: uplifted and/ or inverted southern regions of the North German Basin

Zeitz-Schmölln depression
type: Concept
created: 2021-07-23T08:59:08.502Z
creator: schmar
notation: DE-1075
narrower: Crimmitschau fault zone
scope note: We describe the Zeitz-Schmölln depression subdomain as a tectonic sub-unit in the east of the Thuringian depression. The boundaries of the block only partially follow faults. Predominantly, the delineation is based on changes in the dip of the Thuringian depression. The unit corresponds to a 2nd order syncline with NW/WNW-SE/ESE strike. Even though the main structures of this region have been described in detail (e. g. Katzung & Ehmke, 1993; Franke, 2020; Seidel, 2003), no clear definition of the whole outline of this tectonic unit and associated fault system has been made to date. The extent of this tectonic unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
narrower: Elstertal fault
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/8052
references: https://data.geoscience.earth/ncl/geoera/ref/8101
definition: Strongly uplifted basin part of the NGB eroded down to the Lower Triassic. The WNW/NW-ESE/SE elongated synform is presumably the result of NNE directed Late Cretaceous contraction.
broader: Thuringian Depression

Crimmitschau fault zone
type: Concept
created: 2021-07-23T08:59:08.508Z
creator: schmar
notation: DE-554
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The 15 km long and NW-SE running Crimmitschau fault zone represents the southeastern section of the Kyffhausen-Crimmitschau fault zone (DE-536) and is located at the northern boundary of the Hermundurian Block. Reverse faults within the pre-Zechstein basement indicate weak compressions still in the Eocene. The fault zone belong to the supraregional Gera-Jáchimov fault zone.
broader: Hermundurian Block
broader: Zeitz-Schmölln depression

Elstertal fault
type: Concept
created: 2021-07-23T08:59:08.495Z
creator: schmar
notation: DE-532
in scheme: Tectonic Boundary Objects in Europe
definition: The 15 km long, NNE-SSW running Elster fault is located within the southeastern part of the Merseburg Block and belongs to the subdomain of the Sangerhausen & Querfurt depression.
broader: Sangerhausen & Querfurt depressions
broader: Zeitz-Schmölln depression

Sangerhausen & Querfurt depressions
type: Concept
created: 2021-07-23T08:59:08.469Z
creator: schmar
notation: DE-1074
narrower: Hornburg deep fault
narrower: Blankenheim-Geiseltal fault
narrower: Nebra fault
narrower: Rötha fault
narrower: Elstertal fault
scope note: We describe the Sangerhausen & Querfurt depression as a tectonic sub-unit of the Thuringian depression. The boundaries of the block only partially follow faults. Predominantly, the delineation is based on changes in the dip of the Thuringian depression. The unit corresponds to a 2nd order syncline. Even though the main structures of this region have been described in detail (e. g. Katzung & Ehmke, 1993; Franke, 2020; Seidel, 2003), no clear definition of the whole outline of this tectonic unit and associated fault system has been made to date. The extent of this tectonic unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Saxony-Anhalt provides and describes a partly more detailed and updated fault data set of Saxony-Anhalt within the framework of the HIKE project (DE-ST-0, DE-ST-5000). For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
narrower: Kelbra fault
narrower: Kyffhäuser Northeastern Boundary fault
narrower: Kyffhäuser-Crimmitschau fault zone
narrower: Lauchstädt fault
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/8052
references: https://data.geoscience.earth/ncl/geoera/ref/8101
definition: Strongly uplifted basin part of the NGB eroded down to the Lower to Middle Triassic.
broader: Thuringian Depression

Kyffhäuser-Crimmitschau fault zone
type: Concept
created: 2021-07-23T08:59:08.437Z
creator: schmar
notation: DE-536
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The 56 km long and NW-SE running Kyffhäuser-Crimmitschau fault zone borders the Hermundurian Block in the south from the Merseburg Block in the north east. Associated faults are the Kyffhauser fault in the northwest and the Crimmitschau fault in the southeast. The fault zone is interpreted as northwestern Northeast-part of the supraregional Gera-Jáchymov zone.
broader: Hermundurian Block
broader: Sangerhausen & Querfurt depressions

Hornburg deep fault
type: Concept
created: 2021-07-23T08:59:08.475Z
creator: schmar
notation: DE-487
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The 61 km long, WSW-ENE running Hornburg Deep fault is predominantly located within the northern part of the Merseburg Block. At the SW-end the fault separates the Kyffhausen Block in the northwest from the Hermundurian Block in the southeast. The northeast border of the fault is found at the Halle fault, the southwestern end is represented at the Finne fault.
broader: Hermundurian Block
broader: Sangerhausen & Querfurt depressions
broader: Mansfeld Syncline

Blankenheim-Geiseltal fault
type: Concept
created: 2021-07-23T08:59:08.479Z
creator: schmar
notation: DE-526
notation: DE-529
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The 54 km long, WNW-ESE running Blankenheim-Geiseltal fault is located within the Merseburg Block and belongs to the subdomain of the Sangerhausen & Querfurt depression. Already in the Rotliegend this fault exerted influence on sedimentation or magmatic activities. She is a parallel fault to the Halle fault, which was also active in the Rotliegend.
broader: Sangerhausen & Querfurt depressions

Nebra fault
type: Concept
created: 2021-07-23T08:59:08.489Z
creator: schmar
notation: DE-530
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The 29 km long, NE-SW running Nebra fault is located within the central part of the Merseburg Block and belongs to the subdomain of the Sangerhausen & Querfurt depression. A surface-near observation is not possible.
broader: Sangerhausen & Querfurt depressions
broader: Hermundurian Block

Lauchstädt fault
type: Concept
created: 2021-07-23T08:59:08.456Z
creator: schmar
notation: DE-528
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The 16 km long, NW-SE running Lauchstädt fault is located within the northern part of the Merseburg Block, belongs to the subdomain of the Sangerhausen & Querfurt depression and shows a fault throw of up to 500 m.
broader: Sangerhausen & Querfurt depressions
broader: Mansfeld Syncline

Kyffhäuser Northeastern Boundary fault
type: Concept
created: 2021-07-23T08:59:08.427Z
creator: schmar
notation: DE-448
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The 33 km long, WNW-ESE runnig Kyffhausen NE-boundary fault is the western section of the Kyffhausen-Crimmitschau fault zone and is located at the northern boundary of the Hermundurian Block. At this fault together with the Kelbra fault the Kyffhausen mountains were uplifted successivly since the Upper Cretacous. The fault zones is interpreted as both normal and reverse fault, represents the northwestern end of the supraregional Gera-Jáchimov zone and is assumed to be the northwestward connection the the South Harz fault system. Furthermore, the fault is considered as a terrane boundary between the Central German Crystalline Zone and the Rhenoherzynian Zone.
broader: Sangerhausen & Querfurt depressions
broader: Hermundurian Block

Kelbra fault
type: Concept
created: 2021-07-23T08:59:08.430Z
creator: schmar
notation: DE-506
notation: DE-527
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The 20 km long, W-E-running Kelba fault is located at the northern boundary of the Hermundurian block and belongs to the subdomain of the Sangerhausen & Querfurt depression. Together with the Kyffhausen NE-boundary fault the Kyffhausen mountains were uplifted successively since Upper Cretaceous times.
broader: Sangerhausen & Querfurt depressions
broader: Hermundurian Block

Borna depression
type: Concept
created: 2021-07-23T08:59:08.511Z
creator: schmar
notation: DE-1076
scope note: We describe the Borna depression as a tectonic sub-unit in the east of the Thuringian depression. The boundaries of the block only partially follow faults. Predominantly, the delineation is based on changes in the dip of the Thuringian depression. The unit corresponds to a 2nd order syncline with NW/WNW-SE/ESE strike. Even though the main structures of this region have been described in detail (e. g. Katzung & Ehmke, 1993; Franke, 2020; Seidel, 2003), no clear definition of the whole outline of this tectonic unit and associated fault system has been made to date. The extent of this tectonic unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
narrower: Rötha fault
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/8052
references: https://data.geoscience.earth/ncl/geoera/ref/8101
definition: Strongly uplifted basin part of the NGB eroded down to the Lower Triassic. The WNW/NW-ESE/SE elongated synform is presumably the result of NNE directed Late Cretaceous contraction.
broader: Thuringian Depression

Mansfeld Syncline
type: Concept
created: 2021-07-23T08:59:08.446Z
creator: schmar
notation: DE-1079
narrower: Lauchstädt fault
scope note: We describe the Mansfeld Syncline as a tectonic sub-unit in the north of the Thuringian depression. The tectonic unit boundaries are defined in the north and partly in the south by faults & fault zones. The unit corresponds to a 2nd order syncline with NW/WNW-SE/ESE strike. The demarcation to the tectonic blocks in the east and west can only be determined with uncertainty. Even though the main structures of this region have been described in detail (e. g. Katzung & Ehmke, 1993; Franke, 2020), no clear definition of the whole outline of this tectonic unit and associated fault system has been made to date. The extent of this tectonic unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Saxony-Anhalt provides and describes a partly more detailed and updated fault data set of Saxony-Anhalt within the framework of the HIKE project (DE-ST-0, DE-ST-5000). For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
narrower: Halle fault
narrower: Hornburg deep fault
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/8052
references: https://data.geoscience.earth/ncl/geoera/ref/8101
definition: Strongly uplifted basin part of the NGB eroded down to the Middle Triassic. The syncline is the result of NNE directed Late Cretaceous contraction.
broader: Thuringian Depression

Hermundurian Block
type: Concept
created: 2021-07-23T08:59:08.418Z
creator: schmar
notation: DE-927
narrower: Finne fault zone
narrower: Eisenberg-Pohlen fault zone
narrower: Kyffhäuser Northeastern Boundary fault
narrower: Kelbra fault
narrower: Kyffhäuser-Crimmitschau fault zone
scope note: We describe the Hermundurian Block as a tectonic sub-unit of the Thuringian depression, which borders the Thuringian Syncline in the north. The tectonic unit boundaries are defined by faults & fault zones and the orientation of the basement high. Even though the main structures of this region have been described in detail (e. g. Katzung & Ehmke, 1993; Franke, 2020; Seidel, 2003), no clear definition of the whole outline of this tectonic unit and associated fault system has been made to date. The extent of this tectonic unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Saxony-Anhalt provides and describes a partly more detailed and updated fault data set of Saxony-Anhalt within the framework of the HIKE project (DE-ST-0, DE-ST-5000). For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
narrower: Crimmitschau fault zone
narrower: Hornburg deep fault
narrower: Nebra fault
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/8052
references: https://data.geoscience.earth/ncl/geoera/ref/8101
definition: The 10-12 km wide and 120 km Hermundurian Block was uplifted 600 m in Upper-Cretaceous to Cenozoic times, and borders in the south to the Thuringian syncline at the Finne fault and to the north at the Kyffhäuser NE-boundary fault, the Kyffhäuser-Crimmitschauer fault zone and the Crimmitschauer fault zone. [Domain type: Basement uplifts, partly under coverage; Basement: Northern Phyllitic zone/ Saxothuringian.]
broader: Thuringian Depression

Finne fault zone
type: Concept
created: 2021-07-23T08:59:08.421Z
creator: schmar
notation: DE-485
notation: DE-486
definition: The ca. 100 km long, WNW-ESE running Finne-Eisenberg fault zone represents the North eastern border of the Thuringian syncline. This very prominent, narrow fault zone expresses itself very differently in its course on the surface and in its structural style, sometimes it has an overthrusting character, sometimes flexure-like. The system of the Finne fault zone shows a nearly 100-km-long straight flexure that symbolizes the morphological and geological northeastern border of the Thuringian depression. The fault zone is up to 2 km wide and shows an average dip of 30°. In the central part, which should be surveyed here, the fault zone corresponds to a distinctive narrow band of highly deformed Triassic sedimentary rocks. The northwestern and especially the southeastern parts of the research area are developed as several parallel branch faults. In the southeastern elongation of the fault zone, which is not part of our survey, the sedimentary cover is missing. Here, it is possible to gain insight to the fact that the basement is also involved to the kinematics of the fault zone. The fault zone is interpreted also as northwestern Southwest-part of the supraregional Gera-Jáchymov-Zone.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8065
broader: Hermundurian Block
broader: Thuringian Syncline

Eisenberg-Pohlen fault zone
type: Concept
created: 2021-07-23T08:59:08.424Z
creator: schmar
notation: DE-488
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The Eisenberg-Pohlen fault runs NW-SE to WNW-ESE running fault zone within the eastern part of the Thuriningian syncline and southeastern part of the Finne-Eisenberg fault zone as well as central part of the overregional Gera-Jáchymov zone. The northwestern part shows thrust character.
broader: Thuringian Syncline
broader: Hermundurian Block

NW Thuringian Depression (Ohmgebirge, Leinefeld Anticline, Bleicherode Depression)
type: Concept
created: 2021-07-23T08:59:08.459Z
creator: schmar
notation: DE-1073
narrower: Rengelrode graben fault zone
narrower: Ohmgebirge graben fault zone
scope note: We describe the NW Thuringian depression (Ohmgebirge, Leinefeld Anticline, Bleicherode Depression) as a tectonic sub-unit in the northwest of the Thuringian depression in the transition to the Harz Mountains. The boundaries of the block only partially follow faults. Predominantly, the delineation is based on changes in the dip of the Thuringian depression. The unit corresponds to a 2nd order syncline. Even though the main structures of this region have been described in detail (e. g. Katzung & Ehmke, 1993; Franke, 2020; Seidel, 2003), no definition of the here used/outlined higher-level structure in this form has been made to date. The extent of this tectonic unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/8052
references: https://data.geoscience.earth/ncl/geoera/ref/8101
definition: Strongly uplifted basin part of the NGB eroded down to the Middle Triassic. The Ohmgebirge graben as well as the minor anticlinal and synclinal structures are the result of Late Cretaceous contractional tectonics and partly of the inversion of Triassic structures.
broader: Thuringian Depression

Rengelrode graben fault zone
type: Concept
created: 2021-07-23T08:59:08.462Z
creator: schmar
notation: DE-148
in scheme: Tectonic Boundary Objects in Europe
broader: NW Thuringian Depression (Ohmgebirge, Leinefeld Anticline, Bleicherode Depression)

Ohmgebirge graben fault zone
type: Concept
created: 2021-07-23T08:59:08.466Z
creator: schmar
notation: DE-477
notation: DE-478
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The NNE-SSW striking Saxon Ohm graben fault zone is located in the NNW margin of the Thuringian depression and consists of the Worbiser Graben in the southwest and the Holunger Graben in the northeast. Significant is the evidence of Cenomanian sediments in both sections of the graben zone.
broader: NW Thuringian Depression (Ohmgebirge, Leinefeld Anticline, Bleicherode Depression)

Thuringian Syncline
scope note: We describe the Thuringian syncline as a tectonic unit, whose boundaries are defined by faults & fault systems as well as of bordering basement highs. The Thuringian Syncline is part of the Thuringian depression. Even though the main structures of this region have been described in detail (e. g. Katzung & Ehmke, 1993; Franke, 2020; Seidel, 2003), no clear definition of the outline of this basin part has been made to date. The extent of this tectonic unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
type: Concept
created: 2021-07-23T08:59:08.339Z
creator: schmar
notation: DE-1046
narrower: Gelliehausen fault zone
narrower: Rengelrode graben zone
narrower: Küllstedt fault zone
narrower: Kleinbucha fault zone
narrower: Erfurt fault zone
narrower: Schlotheim graben fault system
narrower: Ilmtal-Magdala-Leutra fault zone
narrower: Leuchtenburg fault zone
narrower: Eichenberg-Gotha-Saalfeld fault system
narrower: northwestern Thuringian forest border zone
in scheme: Tectonic Boundary Objects in Europe
narrower: Eisenberg-Pohlen fault zone
narrower: Finne fault zone
narrower: Thuringian Forest NE boundary fault
references: https://data.geoscience.earth/ncl/geoera/ref/12165
references: https://data.geoscience.earth/ncl/geoera/ref/12238
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/8052
references: https://data.geoscience.earth/ncl/geoera/ref/8101
definition: The Thuringian Syncline as part of the Thuringian Depression is a during the Upper Cretaceous strongly uplifted part of the North German Basin. As a result of Late Cretaceous contractional tectonics this part of the NGB is uplifted at the northern and southern rim along steeply dipping basement thrusts and additionally the whole basin part was deformed to a broad ESE,SE-WNW/NW elongated Syncline. [Domain type: Deformed sedimentary overburden, Basement: Rhenohercynian/Saxothuringian.]
broader: Thuringian Depression

northwestern Thuringian forest border zone
type: Concept
created: 2021-07-23T08:59:08.397Z
creator: schmar
notation: DE-1077
narrower: Netra-Creuzburg Graben fault system
narrower: Thuringian Forest NE boundary fault
narrower: Sättelstädt fault zone
narrower: Sontra graben fault zone
scope note: We describe the northwestern Thuringian forest border zone as a highly deformed tectonic unit, which borders in the north the Thuringian forest. The tectonic unit boundaries are defined by faults & fault zones. The northwestern Thuringian forest border zone is part of the Thuringian depression. The defined unit was not described in this form before. Internal structural elements have been described in detail (e. g. Katzung & Ehmke, 1993; Franke, 2020; Seidel, 2003), but there exist no clear definition of the outline of this tectonic unit. The extent of this tectonic unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/8052
references: https://data.geoscience.earth/ncl/geoera/ref/8101
definition: Uplifted southern parts of the Thuringian Syncline. Basement thrusts under Triassic cover or inverted grabens fringe the Thuringian forest in the north. The today's structural pattern is mainly the result of Triassic extensional tectonics and Late Cretaceous contractional tectonics.
broader: Thuringian Syncline

Netra-Creuzburg Graben fault system
type: Concept
created: 2021-07-23T08:59:08.401Z
creator: schmar
notation: DE-142
notation: DE-143
notation: DE-432
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The Netra-Creuzburg Graben system represents a NW-SE elongated graben structure with its western section lying on Hessian territory. Here one of the few occurrences of the Rhaetian and Lower Jurassic deposits is found, which has been preserved within the Thuringian Depression. The structure is the western end member of the supra-regional Creuzburg-Ilmenau fault zone and consists of a complex system of numerous smaller grabens, horsts and faults. During the Late Cretaceous the graben is partly inverted and to the south is overthrusted by Paleozoic sediments and crystalline of the Thuringian Forest.
broader: northwestern Thuringian forest border zone

Thuringian Forest NE boundary fault
type: Concept
created: 2021-07-23T08:59:08.405Z
creator: schmar
notation: DE-434
notation: DE-465
in scheme: Tectonic Boundary Objects in Europe
notation: DE-491
notation: DE-444
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The Thuringian forest NE-boundary fault represents a NW-SE striking dislocation zone, probably initiated in Variscan or Pre-Variscan time and finally inverted or newly formed as major thrust/reverse fault, separating the Permo-Carboniferous of Thuringian Forest in the southwest from the Upper Paleozoic-Mesozoic platform cover of the Thuringian syncline in the northeast. The structural style of the fault is very heterogeneous and changes several times along the 30 km long running zone. In the west (Werra area), only a shallow flexure occurs, while towards southeast (Eisenach area) the flexure becomes steeper and changes into an reverse fault. At the northern edge of the so-called Ruhlaer Kristallin, a flexure occurs again, which further southeast again changes into an reverse fault.
broader: northwestern Thuringian forest border zone
broader: Thuringian Syncline

Sättelstädt fault zone
type: Concept
created: 2021-07-23T08:59:08.410Z
creator: schmar
notation: DE-466
in scheme: Tectonic Boundary Objects in Europe
definition: The Sattelstädt fault is a 30 km long and NW-SE striking fault, which runs almost in extension of the Netra-Creuzburg graben fault system.
broader: northwestern Thuringian forest border zone

Sontra graben fault zone
type: Concept
created: 2021-07-23T08:59:08.414Z
creator: schmar
notation: DE-687
in scheme: Tectonic Boundary Objects in Europe
broader: northwestern Thuringian forest border zone

Küllstedt fault zone
type: Concept
created: 2021-07-23T08:59:08.355Z
creator: schmar
notation: DE-472
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The Küllstedt fault zone is a NW-SE striking saxonic fault structure in the southeastern part of the Thuringian depression and is located on the northwestern margin of the Mühlhausen-Orlamünd Block. In the pre-Permian basement, it forms together with the Eichenberg-Saalfeld fault zone the northern occurence of equivalents of the Ruhla Crystalline and the Thuringian Main granite.
broader: Thuringian Syncline

Kleinbucha fault zone
type: Concept
created: 2021-07-23T08:59:08.360Z
creator: schmar
notation: DE-480
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The Kleinbucha fault zone is a NW-SE striking saxonic fault zone consisting of several individual elements in the SSE area of the Thuringian Basin and forms the southeastern end member of the Erfurt-Kleinbucha fault zone. The fault zone is a graben structure with approximately 800 m segments. The total subsidence amounts to a maximum of 140 m. Likewise, deep drilling results do not exclude an already pre-Permian initiation of the fault zone.
broader: Thuringian Syncline

Erfurt fault zone
type: Concept
created: 2021-07-23T08:59:08.364Z
creator: schmar
notation: DE-481
notation: DE-479
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The Erfurt fault zone is a NW-SE striking saxonic fault structure in the central section of the Thuringian depression and displaces the stratigraphic sequences of the Keuper in the northeast against series of the Upper Muschelkalk in the southwest. The fault zone appears as a horst structure, but partly also as a graben. Normal faulting often is observed on fault segments, and tectonic folding of higher order was found.
broader: Thuringian Syncline

Schlotheim graben fault system
type: Concept
created: 2021-07-23T08:59:08.368Z
creator: schmar
notation: DE-482
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The NW-SE running Schlotheim graben fault system is located within the central part of the Thuringian depression. Aside from normal faults, also reverse faults are observed locally.The graben forms the southwestern end of the Kyffhäuser magnetic anomaly. The continuation of the Schlotheim Graben to the southeast is formed by the Ilmtal-Magdala-Leutraer Graben.
broader: Thuringian Syncline

Ilmtal-Magdala-Leutra fault zone
type: Concept
created: 2021-07-23T08:59:08.373Z
creator: schmar
notation: DE-483
in scheme: Tectonic Boundary Objects in Europe
definition: The Ilmtal-Magdala-Leutra fault zone is located within the central part of the Thuringian depression, 40 km long and running NW-SE.
broader: Thuringian Syncline

Leuchtenburg fault zone
type: Concept
created: 2021-07-23T08:59:08.377Z
creator: schmar
notation: DE-484
in scheme: Tectonic Boundary Objects in Europe
definition: The Leuchtenberg fault zone is located within the central part of the Thuringian depression, 27 km long and running WNW-ESE.
broader: Thuringian Syncline

Eichenberg-Gotha-Saalfeld fault system
scope note: We describe the Eichenberg-Gotha-Saalfeld fault system as a fault system, whose boundaries are defined by faults & fault zones. The Eichenberg-Gotha-Saalfeld fault system is part of the Thuringian syncline. Even though the main structures of this region have been described in detail (e. g. Katzung & Ehmke, 1993; Franke, 2020; Seidel, 2003), no clear definition of the whole outline of this fault system has been made to date. The extent of this tectonic unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
type: Concept
created: 2021-07-23T08:59:08.389Z
creator: schmar
notation: DE-1078
narrower: Remda fault zone
definition: The Eichenberg-Gotha-Saalfeld fault system is a WNW-ESE to NW-SE running complex fault system that extends over 130 km in centre of the Thuringian depression, from the Leinetalgraben in the west to the northern margin of the Thuringian Slate Mountains. The fault system was initiated in pre-Mesozoic times and was further formed in saxonian times, fault throw is about 500 m within the southwestern part of the Thuringian syncline. In the western section the fault system is characterized by a system of grabens, horsts and normal faults, while compressional elements are almost absent. Further southeast compressional structures, such as thrust and folds, occur until Arnstadt. At the SE-end thrusts dominate the fault zone. The extensional stage inbetween Triassic and Upper Cretaceous was followed by an compressional/transpressive stage in Santonina/Campanian times.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
broader: Thuringian Syncline

Remda fault zone
type: Concept
created: 2021-07-23T08:59:08.393Z
creator: schmar
notation: DE-469
notation: DE-471
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The Remda fault zone is a broad NW-SE striking saxonic fault structure in the southern part of the Thuringian syncline, often subdivided into a Northern Remda fault zone and a Southern Remda fault zone. Predominantly normal faults characterize the fault zone, only stronger compression have particularly affected the central part of the fault zone.
broader: Eichenberg-Gotha-Saalfeld fault system

Thuringian Forest fault set
narrower: Schiefergebirge nappe of Schmiedefeld Vesser
scope note: We describe the Thuringian Forest as a tectonostratigraphic basement unit, whose boundaries are defined by faults in the north and south as well as by outcop pattern of the Pre-Zechstein. The Thuringian Forest is a strongly uplifted part of the Southern North German Basin basement on which no/minor synsedimentary deposits of the NGB have been preserved. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK 1:200000 of Thuringia, Franke (2020), GK 1:100000 of the Thuringian Forest (Kästner, 1996), existing outlines: e.g. Katzung & Ehmke (1993), Franke (2020), Seidel (2003). For References see also Tectonic boundaries in Germany.
type: Concept
created: 2021-07-23T08:59:08.608Z
creator: schmar
notation: DE-1035
narrower: Ruhla Crystalline Complex
in scheme: Tectonic Boundary Objects in Europe
alternative label: Thuringian Forest
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/8101
definition: The Thuringian Forest is a Late Creataceous basement uplift covered with mainly Late Carboniferous to Lower Rotliegend continental redbeds and volcanics. In contrast to the Harz Mountains, the Thuringian Forest is bordered by Cretaceous reverse faults in the north as well as in the south (Franconian Lineament). In the NW the Ruhla crystalline represent Variscan partly high metamorphic basement outcrops.
broader: North German Basin - domain II: uplifted and/ or inverted southern regions of the North German Basin
broader: Mid-German Crystalline High
broader: Tectonostratigraphic Permo-Caboniferous Übergangsstockwerk

Schiefergebirge nappe of Schmiedefeld Vesser
type: Concept
created: 2021-07-23T08:59:09.231Z
creator: schmar
notation: DE-1036
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12239
references: https://data.geoscience.earth/ncl/geoera/ref/8052
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The allochthonous nappe of Schmiedefeld Vesser represents a part of the Thuringian Forest that belongs to the Thuringian-Franconian-Voigtland Schiefergebirge. [Domain type: Variscan basement block, Basement: Saxothuringian.]
scope note: We describe the Schiefergebirge nappe of Schmiedefeld Vesser as a allochthonous tectonostratigraphic basement unit on top of the basement unit of the Thuringian Forest. Its boundaries are defined by faults. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK 1:250000 of Thuringia, Franke (2020), GK 1:100000 of the Thuringian Forest (Kästner, 1996), existing outlines: e.g. Katzung & Ehmke (1993), Franke (2020), Seidel (2003). For References see also Tectonic boundaries in Germany.
broader: Saxothuringian basement domain
broader: Thuringian Forest fault set

Ruhla Crystalline Complex
type: Concept
created: 2021-07-23T08:59:08.614Z
creator: schmar
notation: DE-1037
narrower: Klinger fault
narrower: Stahlberg fault
narrower: Heßleser fault
narrower: Inselberg fault
scope note: We describe the Ruhla Crystalline Complex as a crystalline basement unit within the northwestern Thuringian Forest. Its boundaries are defined by faults and discrete lithological change to the Permo-Carboniferous of the surrounding Thuringian Forest. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK 1:250000 of Thuringia, Franke (2020), GK 1:100000 of the Thuringian Forest (Kästner, 1996), existing outlines: e.g. Katzung & Ehmke (1993), Franke (2020), Seidel (2003). For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
narrower: Franconian Lineament
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The Ruhla crystalline complex is a Variscan age basement outcrop of the NW Thuringian Forest. As the name suggests, this region is predominantly characterised by crystalline rocks, some of which are highly metamorphic. [Domain type: Variscan basement block, Basement: Saxothuringian- Mid-German Crystalline High.]
broader: Thuringian Forest fault set

Klinger fault
type: Concept
created: 2021-07-23T08:59:08.621Z
creator: schmar
notation: DE-454
in scheme: Tectonic Boundary Objects in Europe
broader: Ruhla Crystalline Complex

Inselberg fault
type: Concept
created: 2021-07-23T08:59:09.362Z
creator: schmar
notation: DE-690
in scheme: Tectonic Boundary Objects in Europe
broader: Ruhla Crystalline Complex

Stahlberg fault
type: Concept
created: 2021-07-23T08:59:08.624Z
creator: schmar
notation: DE-455
in scheme: Tectonic Boundary Objects in Europe
broader: Ruhla Crystalline Complex

Heßleser fault
type: Concept
created: 2021-07-23T08:59:08.627Z
creator: schmar
notation: DE-457
in scheme: Tectonic Boundary Objects in Europe
broader: Ruhla Crystalline Complex

Franconian Lineament
type: Concept
created: 2021-07-23T08:59:09.376Z
creator: schmar
notation: DE-458
in scheme: Tectonic Boundary Objects in Europe
broader: Ruhla Crystalline Complex

Northern Kraichgau & Grabfeld Depression subdomain
type: Concept
created: 2021-07-23T08:59:08.974Z
creator: schmar
notation: DE-991
scope note: We describe the Northern Kraichgau & Grabfeld Depression subdomain as a tectonostratigraphic unit, whose boundaries are only in sections defined by faults but also are defined on the base of partly fuzzy trends of the lithofacies and paleofacies. The extent of this unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Bavaria (LFU) provides and describes a more detailed and partly updated fault data set of Bavaria within the framework of the HIKE project (DE-BY_1356). Map Reference: GK 1:1000000, GK 1:500000 of Bavaria (Freudenberger & Schwerd, 1996), tectonic map of Bavaria 1:1000000 (Freudenberger & Schwerd, 1996), HIKE (DE-BY 1356). For References see also Tectonic boundaries in Germany.
alternative label: Northern Kraichgau & Grabfeld Depression fault set
in scheme: Tectonic Boundary Objects in Europe
definition: The Northern Kraichgau & Grabfeld depression subdomain is characterized by inverted Mesozoic graben and a decrease of Late Cretaceous overprint towards SW within the subdomain. [Domain type: Deformed sedimentary overburden, Basement: Mainly Saxothuringian.]
broader: North German Basin - domain II: uplifted and/ or inverted southern regions of the North German Basin
broader: Swabian - Franconian - South Thuringian Block

transition North German Basin / Anglo Dutch Basin
creator: schmar
created: 2021-09-06T16:03:36.899Z
type: Concept
in scheme: Tectonic Boundary Objects in Europe
scope note: Since no clear transition between the Anglo-Dutch Basin and the North German Basin can be defined (e.g. Geluk 2005, Doornenbal & Stevenson 2010, Wong et al. 2007), it is advisable to define a transition zone between the regions that can be clearly assigned to the respective basins. For the classification chosen here, all areas between Horn Graben and Central Graben and west of the line Ems lineament - Borkum fault - Harald lineament are assigned to this transition zone.
narrower: southwestern branch Horn Graben
narrower: Schillgrund Platform
narrower: Schillgrund High
narrower: G+L Platform
references: https://data.geoscience.earth/ncl/geoera/ref/12249
references: https://data.geoscience.earth/ncl/geoera/ref/8022
broader: Tectonic Boundary in Germany

southwestern branch Horn Graben
type: Concept
created: 2021-09-06T16:04:45.736Z
creator: schmar
scope note: "We describe here the "Southwestern branch of Horn Graben (Gerd Graben)" as a tectonostratigraphic unit whose boundaries are with the exception of the southern end are defined by faults and fault systems (e.g. the Nordschillgrund fault, Gernot fault, Weisse Bank Escarpment), but as well salt structures. Even though the main structures of this unit have been described in detail (e.g. Kockel et al. 1991, Kockel 1995), no clear definition of the outline of the structural unit has been made to date. The extent of this tectonostratigraphic sub-domain of the ""transition region North German Basin/ Anglo Dutch Basin"" was newly created with a view to a structured assignment of fault data and the assignment of an uniform structural history for this sub-domain. The outline is based on the analysis of a large number of partly contradictory map series and citations that were generalised for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Redefined and summarized from Baldschuhn et al. (1996) (especially structural maps and profiles), Baldschuhn et al. (2001), and the structure of the Base Zechstein based on Baldschuhn et al. (2001). Outline definition is especially related to the profiles of the GTA (Baldschuhn et al. 1996) and existing 3D models (BGR, 2021).
in scheme: Tectonic Boundary Objects in Europe
notation: DE-1094
definition: "The Southwestern branch of Horn Graben (Gerd Graben)" highlight the early structural evolution of the Horn Graben during the Lower and Mid-Triassic (SW-NE). During the Mid to Upper Triassic the Horn Graben then received its now dominant structural directions (N-S/SSE-NNW) (Jähne-Klingberg et al. 2018).
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/12430
references: https://data.geoscience.earth/ncl/geoera/ref/12431
references: https://data.geoscience.earth/ncl/geoera/ref/12159
references: https://data.geoscience.earth/ncl/geoera/ref/12432
broader: transition North German Basin / Anglo Dutch Basin

Schillgrund Platform
creator: schmar
created: 2021-09-06T16:06:20.794Z
type: Concept
in scheme: Tectonic Boundary Objects in Europe
scope note: We describe here the "Schillgrund Platform" as a tectonostratigraphic unit whose boundaries are only in parts defined by faults and fault systems (e.g. the Nordschillgrund fault, Gernot fault, Weisse Bank Escarpment), but as well as partly fuzzy trends in the lithofacies and especially the distributional pattern of Mesozoic below the Late Cimmerian unconformity (Jakobsen et al. 2020). The region is less deeply eroded than the Schillgrund High and is still covered by Zechstein and Lower Triassic sediments as well as Mid-Triassic to Upper Triassic in the Dutch sector. Even though the main structures of this unit have been described in detail (e.g. Kockel et al. 1991, Kockel 1995, Doornenbal & Stevenson 2010), no clear definition of the outline of the structural unit has been made to date. The extent of this tectonostratigraphic sub-domain of the ""transition region North German Basin/ Anglo Dutch Basin"" was newly created with a view to a structured assignment of fault data and the assignment of an uniform structural history for this sub-domain. The outline is based on the analysis of a large number of partly contradictory map series and citations that were generalised for this purpose. Both the transition to the Schillgrund Hoch and to the G+L Platform cannot be clearly defined. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Redefined and summarized from Baldschuhn et al. (1996) (especially structural maps and profiles), Baldschuhn et al. (2001), Wong et al. (2007), and the structure of the Base Zechstein based on Baldschuhn et al. (2001). Outline definition is especially related to the profiles of the GTA (Baldschuhn et al. 1996) and existing 3D models (BGR, 2021).
notation: DE-1095
definition: The Schillgrund Platform is characterized by subcrop of Triassic sediments below the Late Cimmerian unconformity, in parts already Kimmeridgian and Portlandian sediments (Kockel 1995, Jakobsen et al. 2020). The deep erosion in the area of the Schillgrund Platform is among other things the result of a large-scale uplift due to the formation of the North Sea dome (e.g, Doornenbal & Stevenson, 2010). The region shows predominantly salt pillows, but also isolated diapirs, whereby contrary to adjacent regions, the structures show only partial preferential directions.
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/12159
references: https://data.geoscience.earth/ncl/geoera/ref/12430
references: https://data.geoscience.earth/ncl/geoera/ref/12431
references: https://data.geoscience.earth/ncl/geoera/ref/8022
references: https://data.geoscience.earth/ncl/geoera/ref/12432
broader: transition North German Basin / Anglo Dutch Basin

Schillgrund High
created: 2021-09-06T16:08:05.429Z
type: Concept
creator: schmar
in scheme: Tectonic Boundary Objects in Europe
notation: DE-1096
scope note: We describe here the "Schillgrund High" as a tectonostratigraphic unit whose boundaries are only in parts defined by faults and fault systems (along the Nordschillgrund fault), but as well as partly fuzzy trends in the lithofacies and especially the distributional pattern of Mesozoic relicts below the Late Cimmerian unconformity. The region is more deeply eroded than the Schillgrund Platform but, in contrast to the adjacent East North Sea High to the north, is still covered by Zechstein sediments. Even though the main structures of this unit have been described in detail (e.g. Kockel et al. 1991, Kockel 1995), no clear definition of the outline of the structural unit has been made to date. The extent of this tectonostratigraphic sub-domain of the ""transition region North German Basin/ Anglo Dutch Basin"" was newly created with a view to a structured assignment of fault data and the assignment of an uniform structural history for this sub-domain. The outline is based on the analysis of a large number of partly contradictory map series and citations that were generalised for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Redefined and summarized from Baldschuhn et al. (1996) (especially structural maps and profiles), Baldschuhn et al. (2001). Outline definition is especially related to the profiles of the GTA (Baldschuhn et al. 1996) and existing 3D models (BGR, 2021).
definition: The Schillgrund High is characterized by shallow position of the pre-Permian basement below the Late Cimmerian unconformity and by the subcrop of partly pre-Permian and thin Zechstein below the Early Cretaceous, in parts already Kimmeridgian and Portlandian sediments (Kockel 1995, Jakobsen et al. 2020). The deep erosion in the area of the Schillgrund High is the result of a large-scale uplift due to the formation of the North Sea dome but especially due to the rifting and rift-shoulder uplift of the Central Graben (e.g, Doornenbal & Stevenson, 2010). The demarcation to the Schillgrund Platform is rather vague.
references: https://data.geoscience.earth/ncl/geoera/ref/12159
references: https://data.geoscience.earth/ncl/geoera/ref/12431
references: https://data.geoscience.earth/ncl/geoera/ref/8022
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/12432
references: https://data.geoscience.earth/ncl/geoera/ref/12430
broader: transition North German Basin / Anglo Dutch Basin

G+L Platform
creator: schmar
created: 2021-09-06T16:09:43.503Z
type: Concept
in scheme: Tectonic Boundary Objects in Europe
notation: DE-1091
scope note: We describe here the "G+L Platform" as a tectonostratigraphic unit whose boundaries are defined both by faults and fault systems, salt structures as well as partly fuzzy trends in the lithofacies and thickness of stratigraphic units. Even though the main structures of this unit have been described in detail (e.g. Kockel et al. 1991, Kockel 1995), no clear definition of the outline of the structural unit has been made to date. The extent of this tectonostratigraphic sub-domain of the "transition region North German Basin/ Anglo Dutch Basin" was newly created with a view to a structured assignment of fault data and the assignment of an uniform structural history for this sub-domain. The outline is based on the analysis of a large number of partly contradictory map series and citations that were generalised for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Redefined and summarized from Baldschuhn et al. (1996) (especially structural maps and profiles), and the structure of the Base Zechstein based on Baldschuhn et al. (2001). Outline definition is especially related to the profiles of the GTA (Baldschuhn et al. 1996) and existing 3D models (BGR, 2021). Uncertainties depend on whether the outline is drawn based on the structure of the top basement or the distribution of sediments and fault pattern in the overburden, there may be major differences (salt tectonics/tectonic decoupling).
definition: A Mesozoic Platform area which is bounded to the east by the Harald Lineament and the Borkum Fault (Kockel 1995). The G+L platform is characterized structurally by the general subcrop of Middle Buntsandstein to Muschelkalk below the Late Cimmerian unconformity (Jakobsen et al. 2020), by the lack of major basement faults. Within the German North Sea sector this structural unit is bordered by long elongated salt-walls often in the near vicinity of major basement faults (e.g. Borkum fault). These salt walls, in turn, often have complex crestal fault systems. The demarcation to the Ameland & Schillgrund Platform is rather vague.
references: https://data.geoscience.earth/ncl/geoera/ref/12159
references: https://data.geoscience.earth/ncl/geoera/ref/12430
references: https://data.geoscience.earth/ncl/geoera/ref/12433
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/12432
references: https://data.geoscience.earth/ncl/geoera/ref/12431
broader: transition North German Basin / Anglo Dutch Basin

Anglo-Dutch Basin
type: Concept
creator: schmar
created: 2021-09-06T16:11:20.339Z
in scheme: Tectonic Boundary Objects in Europe
notation: DE-1101
scope note: We describe the "Anglo-Dutch Basin" as a sub-basin within the western Southern Permian Basin. Here we define this major basin as a tectonostratigraphic domain whose boundaries are not clearly defined by faults and fault systems. The outline of the domain can only be roughly defined based on lithostratigraphic trends and on the base of differences in the thickness and paleogeographical pattern of the Rotliegend and Zechstein. Even though the structure have been described (e. g. Geluk, 2005), no clear definition of the outline of this tectonostratigraphic unit has been made to date. Especially the border to the North German Basin can only be roughly defined but crosses/ is part of the tectonic sub-domains of the German North Sea sector. The extent of this tectonostratigraphic unit was newly created with a view to a structured assignment of fault data and the assignment of an uniform structural history for this sub-domain. The here used definition of the outline is based on a large number of partly contradictory map series and citations that were generalised for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future.
definition: Although the Southern Permian Basin is often viewed as one basin, it is comprises three main tectonic units (Anglo-Dutch Basin, North German Basin, Polish Trough) as can be observed on the isopach map of the Rotliegend Sediments (Geluk, 2005). These three basins have a different origin; in part they are successor basins of the Variscan Foreland Basin, but mainly they represent new basins, which developed in response to latest Carboniferous to Early Permian wrenching/rifting and related volcanism. The Netherlands belongs to two of these basins. The NE onshore and northern offshore of the country belonged to the realm of the North German Basin, whereas the southern onshore and western offshore belonged to the Anglo-Dutch Basin (Geluk, 2005).
narrower: Central Graben
references: https://data.geoscience.earth/ncl/geoera/ref/8022
broader: Tectonic Boundary in Germany

Central Graben
creator: schmar
created: 2021-09-06T16:13:05.371Z
type: Concept
in scheme: Tectonic Boundary Objects in Europe
notation: DE-1100
scope note: We describe here the "Central Graben" as a tectonostratigraphic unit whose boundaries are defined both by faults and fault systems, as well as partly fuzzy trends in the thickness and facies of stratigraphic units (Jakobsen et al. 2020). Even though the main structures of this unit have been described in detail (e.g. Arfai et al. 2014, Evans et al. 2003, Wride 1995), existing outlines of the large structure differ in part significantly. The main units of the Graben are: 1.) the Step Graben system with the Outer Rough Basin as well as adjacent minor horsts and grabens; 2.) the central deep subsided parts of the Graben system with the sub units: Tail End Graben, Dutch Central Graben, Salt Dome Province, the German John & Mads Graben, the German Clemens Basin and Clemens Graben. The extent of this tectonic domain was newly created with a view to a structured assignment of fault data and the assignment of an uniform structural history for this sub-domain. The outline is based on the analysis of a large number of partly contradictory map series and citations that were generalised for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. The Central Graben belongs to both the South Permian Basin in the area of the Anglo-Dutch Basin and the North Permian Basin. The graben also crosses the Mid/East North Sea - Rinköbing Fyn High. Uncertainties depend on whether the outline is drawn based on the structure of the top basement or the distribution of sediments and fault pattern in the overburden, there may be major differences (salt tectonics/tectonic decoupling).
definition: The Central Graben is a half-graben that runs over 500 km S-N towards the Dutch, German, Danish as well as the British and Norwegian offshore sectors. Not least because of a comprehensive 3D seismic data coverage, the Central Graben represents the most explored one of the graben systems of the Southern and SE North Sea (Glückstadt Graben, Horn Graben, Central Graben), although, as it was affected by several different tectonic phases, it shows the highest structural complexity of the North Sea rifts. This high degree in structural complexity complicates the understanding of its structural evolution (Arfai et al. 2014, Thöle et al. 2021). In comparison to the Horn Graben & Glückstadt Graben, the Central Graben is the most developed half-graben with large listric fault systems at its eastern border (Nordschillgrund fault, Coffee Soil fault), while its less pronounced western flank (i.e. Step Graben system) is dissected in several smaller horst and grabens. Major tectonic subsidence activity in the Central Graben started in Keuper times, coinciding with renewed rise of activity in the Horn Graben and the Glückstadt Graben. However, there is also evidence of a Lower Triassic to Middle Triassic basin development, which probably did not lead to the formation of major faults. A second major phase of activity in the Central Graben lasted from the Upper Jurassic to the Lower Cretaceous, while in the Horn Graben only minor subsidence can be observed during this period. In the Late Cretaceous, the Central Graben was partly affected by structural inversion (e.g. Arfai et al. 2014), while the Horn Graben shows only minor renewed halotectonic activity with bulging of the roof of most of the salt diapirs.
references: https://data.geoscience.earth/ncl/geoera/ref/12434
references: https://data.geoscience.earth/ncl/geoera/ref/12433
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/7697
broader: Anglo-Dutch Basin

Trier Bight & Gulf of Luxembourg domain
type: Concept
created: 2021-07-23T08:59:08.923Z
creator: schmar
notation: DE-961
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12212
references: https://data.geoscience.earth/ncl/geoera/ref/12243
definition: The Trier Bight & Gulf of Luxembourg domain contains a fault set of NE-SW oriented faults. The domain is characterized by Triassic overburden underlying Rhenish massif. [Domain type: Sedimentary overburden, Basement: Rhenohercynian.]
scope note: We describe the Trier Bight & Gulf of Luxembourg domain as a Mesozoic tectonostratigraphic unit on top of Rhenohercynian & Mid-German Crystalline High basement. The boundaries are defined by distribution of Jurassic to Upper Triassic sediments and the basement outcrops of the Rhenish Massif. The extent of this unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK1000, The Geological overview map of Rheinland Pfalz. For References see also Tectonic boundaries in Germany.
broader: Tectonic Boundary in Germany

Saar-Nahe Basin domain
type: Concept
created: 2021-07-23T08:59:08.928Z
creator: schmar
notation: DE-963
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12201
references: https://data.geoscience.earth/ncl/geoera/ref/12212
references: https://data.geoscience.earth/ncl/geoera/ref/12243
scope note: We describe the Saar-Nahe Basin as a tectonostratigraphic Permo-Carboniferous basement outcrop (or under Quaternary cover of the Northern Upper Rhine Graben) on top of Northern Phyllite Zone & Mid-German Crystalline High basement. The boundaries of this structural unit are defined by faults and especially by lithological changes. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK1000. For References see also Tectonic boundaries in Germany.
definition: The tectonic development of the Saar-Nahe Basin as a large Late Variscan molasse basin began simultaneously with the sedimentation of the oldest Upper Carboniferous (border between Namur and Westphalia) and was completed at the end of the Rotliegend. After Henk (1993) the basin is formed in the hanging wall of a major detachment which soles out about a depth of 16 km. The structural style of the basin is characterized by normal faults running parallel NE-SW oriented basin axis and orthogonal to this by transfer fault zones (Fig. 16b, country sheet). In the course of the postvariscan tectonic development older NE-SW striking faults seem to have been reactivated (Rein et al .2011). [Domain type: Post-Variscan basement block, Basement: Northern Phyllitic Zone & Saxothuringian to Mid-Crystalline High.]
alternative label: Saar-Nahe Basin
broader: Tectonostratigraphic Permo-Caboniferous Übergangsstockwerk
broader: Tectonic Boundary in Germany

Upper Rhine Graben
definition: The Upper Rhine graben belongs to the Cenozoic rift system (Ziegler 1992; ECRIS; see also Country Sheet) and predominantly is oriented NEE-SWW, in the line from Frankfurt to Basel. The graben is differentiated in three segments, each up to 100 km long (Grimmer et al. 2017). The evolution of the graben was controlled by multiple change of the stress field and a reactivation of Permo-Carbonifereous crustal discontinuities (Schuhmacher 2002). The formation and subsidence of the Upper Rhine Graben starts in the south during lower Eocene by NNW-SSE-extension, in the north during the Upper Eocene. The main rift stage began in the Lower Oligocene with continuous northward movements of the Alps (Dézes et al. 2004). During the early Miocene (Aquitanian), a major reorientation of the regional stress field is held responsible for the main subsidence phase of the northern parts of the Upper Rhine Graben. This is reflected by a counterclockwise rotation and northeastward shift of the depocenter axis and later by the middle Miocene uplift and erosion of the southern parts of the Upper Rhine Graben. The fault throw amounts to in the south about 5000 m and in the northern part above 4000 m. The offset of the eastern flank is up to 1000 m higher than on the western side. With rotation of the stress field from NNE-SSW within the Eocene before 6-7 Ma to NW-SO, transtensive strike-slip movements characterize the recent activity of the Upper Rhine graben. Today´s morphology of the flanks and the graben itself is characterized by great amount of normal faults or stepped faults and strike slip faults. After e.g. Derer et al. (2005) the fault pattern might be complex as illustrated in Fig. 13a (HIKE Country Sheet for Germany), where tilted fault blocks are bounded by growth faults. The complex, internal structural inventory of the graben is also revealed when looking at Fig. 13 b (Country Sheet), which Grimmer et al (2017) compiled and (re-)interpreted from numerous studies. The geological…
type: Concept
created: 2021-07-23T08:59:08.815Z
creator: schmar
notation: DE-956
narrower: Western segment subdomain
narrower: Northern segment subdomain
narrower: Ilfeld-Bruchsal fault system
narrower: Kaiserstuhl Block subdomain
narrower: Southern segment subdomain
narrower: Eastern border zone subdomain
narrower: Northern marginal area subdomain
scope note: We define here the Upper Rhine Graben as a superior Cenozoic tectonostratigraphic, unit, whose boundaries are defined by faults and fault systems, in particular by the distribution of thickened Cenozoic to Quaternary sedimentary successions. Partly the defined outline overlap with neighbouring tectonic units, because influence of rifting is also visible in adjacent basement highs and along the rift-shoulders. The sub-domains here used are based on the classification of the GEORG project. The extent of the tectonostratigraphic domain was partly edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map reference: GK 300 of Hesse, GeORG-Projektteam (2013). For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12179
references: https://data.geoscience.earth/ncl/geoera/ref/12181
references: https://data.geoscience.earth/ncl/geoera/ref/12193
references: https://data.geoscience.earth/ncl/geoera/ref/12200
references: https://data.geoscience.earth/ncl/geoera/ref/12212
references: https://data.geoscience.earth/ncl/geoera/ref/12236
references: https://data.geoscience.earth/ncl/geoera/ref/12250
broader: Tectonic Boundary in Germany

Western segment subdomain
type: Concept
created: 2021-07-23T08:59:08.820Z
creator: schmar
notation: DE-1047
scope note: We define here the western segment subdomain as a Cenozoic tectonostratigraphic sub-unit of the Upper Rhine Graben, whose boundaries are defined by faults and fault systems, in particular by differences in thicknesses & facies of Cenozoic to Quaternary sedimentary successions. Partly the defined outline overlap with neighbouring tectonic units, because influence of rifting is also visible in adjacent basement highs and along the rift-shoulders. The sub-domains here used are based on the classification of the GEORG project. The extent of the tectonostratigraphic domain was partly edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map reference: GK 1000, GeORG-Projektteam (2013). For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12193
references: https://data.geoscience.earth/ncl/geoera/ref/12194
definition: N-S, NNW-SSE and NNE-SSW running faults within the western segment of the Upper Rhine graben. The length of the individual faults, with exception of the graben major faults, covers a range of ~ 10 to 30 km. The NNE-SSW oriented major graben rim faults extend over a lenght of 209 km (DE-160) and 106 km (DE-161) respectively. [Domain type: Strongly deformed sedimentary overburden, Basement: Saxothuringian/Moldanubian.]
broader: Upper Rhine Graben

Northern segment subdomain
type: Concept
created: 2021-07-23T08:59:08.824Z
creator: schmar
notation: DE-1048
scope note: We define here the northern segment subdomain as a Cenozoic tectonostratigraphic sub-unit of the Upper Rhine Graben, whose boundaries are defined by faults and fault systems, in particular by differences in thicknesses & facies of Cenozoic to Quaternary sedimentary successions. Partly the defined outline overlap with neighbouring tectonic units, because influence of rifting is also visible in adjacent basement highs and along the rift-shoulders. The sub-domains here used are based on the classification of the GEORG project. The extent of the tectonostratigraphic domain was partly edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map reference: GK 300 of Hesse, GK 1000, GeORG-Projektteam (2013). For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12193
references: https://data.geoscience.earth/ncl/geoera/ref/12194
references: https://data.geoscience.earth/ncl/geoera/ref/12195
definition: N-S, NNW-SSE and NNE-SSW running faults within the western segment of the Upper Rhine graben. The length of the individual faults, with exception of the graben major faults, covers a range of ~ 10 to 30 km. [Domain type: Strongly deformed sedimentary overburden, Basement: Saxothuringian.]
broader: Upper Rhine Graben

Ilfeld-Bruchsal fault system
type: Concept
created: 2021-07-23T08:59:08.829Z
creator: schmar
notation: DE-1049
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12193
scope note: We define here the Ilfeld-Bruchsal fault system as a Cenozoic fault system of the Upper Rhine Graben, whose boundaries are defined by faults. Partly the defined outline can overlap with neighbouring tectonic units, because influence of rifting is also visible in adjacent basement highs and along the rift-shoulders. The sub-domains here used are based on the classification of the GEORG project. The extent of the tectonostratigraphic domain was partly edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations, that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map reference: GK 1000, GeORG-Projektteam (2013). For References see also Tectonic boundaries in Germany.
references: https://data.geoscience.earth/ncl/geoera/ref/12194
definition: The Ilfeld-Bruchsal fault system within the Upper Rhine Graben is characterized by predominantly NNE and subordinate SE-SSE and E-NNE striking faults. The length of the individual faults cover a range of ~ 10 to 30 km. The region of the Ilfeld-Bruchsal fault system shows a strongly deformed overburden and the basement belongs to the Saxothuringian/Moldanubian. [Main fault activity: Tertiary/Quaternary. Domain type: Strongly deformed sedimentary overburden, Basement: Saxothuringian/Moldanubian.]
broader: Upper Rhine Graben

Kaiserstuhl Block subdomain
type: Concept
created: 2021-07-23T08:59:08.832Z
creator: schmar
notation: DE-1050
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12193
references: https://data.geoscience.earth/ncl/geoera/ref/12194
scope note: We define here the Kaiserstuhl Block subdomain as a Cenozoic tectonostratigraphic sub-unit of the Upper Rhine Graben, whose boundaries are partly defined by faults and fault systems, in particular by differences in thicknesses & facies of Cenozoic to Quaternary sedimentary successions (in this case mostly volcanics). The sub-domains here used are based on the classification of the GEORG project. The extent of the tectonostratigraphic domain was partly edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map reference: GK 1000, GeORG-Projektteam (2013). For References see also Tectonic boundaries in Germany.
definition: The Kaiserstuhl Block within the Upper Rhingraben belongs to the Cenozoic volcanic complex (European Cenozoic Volcanic province), characterized by Tertiary/Quaternary main fault activity and subordinate fault activity during Jurassic, with NNE/N-S strike. [Domain type: Cenozoic volcanic complex, Basement: Moldanubian.]
broader: Upper Rhine Graben

Southern segment subdomain
scope note: We define here the southern segment subdomain as a Cenozoic tectonostratigraphic sub-unit of the Upper Rhine Graben whose boundaries are partly defined by faults and fault systems, in particular by differences in thicknesses & facies of Cenozoic to Quaternary sedimentary successions. The sub-domains here used are based on the classification of the GEORG project. The extent of the tectonostratigraphic domain was partly edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map reference: GK 1000, GeORG-Projektteam (2013). For References see also Tectonic boundaries in Germany.
type: Concept
created: 2021-07-23T08:59:08.836Z
creator: schmar
notation: DE-1052
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12193
references: https://data.geoscience.earth/ncl/geoera/ref/12194
definition: [Domain type: Stronlgy deformed sedimentary overburden, Basement type: Moldanubian.]
broader: Upper Rhine Graben

Eastern border zone subdomain
type: Concept
created: 2021-07-23T08:59:08.840Z
creator: schmar
notation: DE-1051
scope note: We define here the Eastern border zone subdomain as a Cenozoic tectonostratigraphic sub-unit of the Upper Rhine Graben, whose boundaries are partly defined by faults and fault systems, in particular by differences in thicknesses & facies of Cenozoic to Quaternary sedimentary successions. Partly the defined outline overlap with neighbouring tectonic units, because influence of rifting is also visible in adjacent basement highs and along the rift-shoulders. The sub-domains here used are based on the classification of the GEORG project. The extent of the tectonostratigraphic domain was partly edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map reference: GK 1000, GeORG-Projektteam (2013). For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12193
references: https://data.geoscience.earth/ncl/geoera/ref/12194
definition: The faults at the eastern border zone of the Upper Rhine graben show a predominanlty strike of NNE/NE and subordinate ENE/SE. Main fault activity is documented for Teritary-Quaternary, and subordinate for Triassic, Jurassic age. [Domain type: Strongly deformed sedimentary overburden, Basement: Saxothuringian/Moldanubian.]
broader: Upper Rhine Graben

Northern marginal area subdomain
type: Concept
created: 2021-07-23T08:59:08.843Z
creator: schmar
notation: DE-1015
notation: DE-1016
narrower: Mainz Basin
narrower: Hanau-Seligenstadt Basin
narrower: Amöneburg Basin
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12193
references: https://data.geoscience.earth/ncl/geoera/ref/12194
definition: Cenozoic-Quaternary marginal basins of the Upper Rhine Graben
scope note: We define here the Northern marginal area subdomain as a Cenozoic-Quaternary tectonostratigraphic sub-unit of the Upper Rhine Graben, whose boundaries are partly defined by faults and fault systems, in particular by differences in thicknesses & facies of Cenozoic to Quaternary sedimentary successions. The extent of the tectonostratigraphic domain was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map reference: GK 1000, GK 300 of Hesse. For References see also Tectonic boundaries in Germany.
broader: Upper Rhine Graben

Amöneburg Basin
type: Concept
created: 2021-07-23T08:59:08.853Z
creator: schmar
notation: DE-1016
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12212
references: https://data.geoscience.earth/ncl/geoera/ref/12194
references: https://data.geoscience.earth/ncl/geoera/ref/12195
definition: Cenozoic-Quaternary sub-basin within the northern marginal areas of the Upper Rhine Graben. [Domain type: Sedimentary overburden, Basement: Rhenohercynian]
scope note: We define here the Amöneburg Basin as a Cenozoic-Quaternary sub-basin within the northern marginal areas of the Upper Rhine Graben, whose boundaries are partly defined by faults and fault systems, in particular by differences in thicknesses & facies of Cenozoic to Quaternary sedimentary successions. The extent of the tectonostratigraphic domain was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map reference: GK 1000, GK 300 of Hesse.
broader: Northern marginal area subdomain

Mainz Basin
type: Concept
created: 2021-07-23T08:59:08.846Z
creator: schmar
notation: DE-1014
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12212
references: https://data.geoscience.earth/ncl/geoera/ref/12194
references: https://data.geoscience.earth/ncl/geoera/ref/12195
definition: Cenozoic-Quaternary sub-basin within the northern marginal areas of the Upper Rhine Graben. [Domain type: Sedimentary overburden, Basement: Saxothuringian & Northern Phyllitic zone]
scope note: We define here the Mainz Basin as a Cenozoic-Quaternary tectonostratigraphic sub-basin of the northern Upper Rhine Graben, whose boundaries are partly defined by faults and fault systems, in particular by differences in thicknesses & facies of Cenozoic to Quaternary sedimentary successions. The extent of the tectonostratigraphic domain was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map reference: GK 1000, GK 300 of Hesse. For References see also Tectonic boundaries in Germany.
broader: Northern marginal area subdomain

Hanau-Seligenstadt Basin
type: Concept
created: 2021-07-23T08:59:08.849Z
creator: schmar
notation: DE-1015
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12212
references: https://data.geoscience.earth/ncl/geoera/ref/12194
references: https://data.geoscience.earth/ncl/geoera/ref/12195
definition: Cenozoic-Quaternary sub-basin within the northern marginal areas of the Upper Rhine Graben [Domain type: Sedimentary overburden, Basement: Saxothuringian, subordinated Northern Phyllitic zone.]
scope note: We define here the Hanau-Seligenstadt Basin as a Cenozoic-Quaternary sub-basin within the northern marginal areas of the Upper Rhine Graben, whose boundaries are partly defined by faults and fault systems, in particular by differences in thicknesses & facies of Cenozoic to Quaternary sedimentary successions. The extent of the tectonostratigraphic domain was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map reference: GK 1000, GK 300 of Hesse. For References see also Tectonic boundaries in Germany.
broader: Northern marginal area subdomain

Lower Rhine Bight
type: Concept
created: 2021-07-23T08:59:08.857Z
creator: schmar
notation: DE-957
narrower: Erft Block
narrower: Peel Horst
narrower: Roer Valley Graben subdomain
narrower: Venlo graben
narrower: Krefeld Block
narrower: Cologne Block
definition: The NW-SE striking lower Rhine Bight, a recently seismically active, Cenozoic rifting zone, is bordered in the West and South by the Eifel and the Westerwald respectively, and rises up into the Rheinisches Schiefergebirge (Fig. 14a, HIKE country sheet for Germany). The formation of the still subsiding graben structure started in the Early Oligocene at around 36 Ma (Zijerveld et al. 1992) and therefore is younger than the Upper Rhine graben. Several major blocks and grabens characterize the area, each bounded by NW-SE striking faults, such as the Krefeld Block, the Köln Block, the Erft Block, the Peel Block as well as the the Roer Valley and Venlo graben (Fig. 14a, b, HIKE country sheet for Germany). According to Ahorner (1975) the initiation of rifting along NW-SE oriented basement faults probably was caused by a counterclockwise rotation of the regional stress field from NE-SW to NW-SE (Ahorner 1975). Recently recorded earthquakes indicate a stress field that is characterized by a subvertical σ1 and a subhorizontal NE-SW oriented σ3 indicating almost pure dip-slip for the predominately NW-SE striking normal faults (Hinzen 2003). Additionally to NW-SE striking fault zones and, to a lesser extent, WNW-ESE ones, large strike-slip faults characterize the recent structural style of the active graben. Highest fault offsets are found at the Erft and Rurrand faults with 100 -180 m (Hinzen 2003).
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12154
references: https://data.geoscience.earth/ncl/geoera/ref/12203
references: https://data.geoscience.earth/ncl/geoera/ref/12228
references: https://data.geoscience.earth/ncl/geoera/ref/12251
scope note: The extent of the Cenozoic tectonostratigraphic domain was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map reference: e.g. Reicherter et al. (2008). For References see also Tectonic boundaries in Germany.
narrower: South Limburg Block
broader: Tectonic Boundary in Germany

Erft Block
type: Concept
created: 2021-07-23T08:59:08.860Z
creator: schmar
notation: DE-998
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12154
references: https://data.geoscience.earth/ncl/geoera/ref/12203
references: https://data.geoscience.earth/ncl/geoera/ref/12228
definition: [Domain type: Strongly deformed Tertiary sedimentary overburden, Basement: Rhenohercynian.]
scope note: The extent of the Cenozoic tectonostratigraphic sub-domain was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map reference: e.g. Reicherter et al. (2008). For References see also Tectonic boundaries in Germany.
broader: Lower Rhine Bight

Peel Horst
type: Concept
created: 2021-07-23T08:59:08.864Z
creator: schmar
notation: DE-999
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12154
references: https://data.geoscience.earth/ncl/geoera/ref/12203
references: https://data.geoscience.earth/ncl/geoera/ref/12228
definition: [Domain type: Strongly deformed Tertiary sedimentary overburden, Basement: Rhenohercynian/Avalonia(?).]
scope note: The extent of the Cenozoic tectonostratigraphic sub-domain was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map reference: e.g. Reicherter et al. (2008). For References see also Tectonic boundaries in Germany.
broader: Lower Rhine Bight

Roer Valley Graben subdomain
type: Concept
created: 2021-07-23T08:59:08.867Z
creator: schmar
notation: DE-1000
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12154
references: https://data.geoscience.earth/ncl/geoera/ref/12203
references: https://data.geoscience.earth/ncl/geoera/ref/12228
definition: [Domain type: Strongly deformed Tertiary sedimentary overburden, Basement: mainly Rhenohercynian/Avalonia(?).]
scope note: The extent of the Cenozoic tectonostratigraphic sub-domain was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map reference: e.g. Reicherter et al. (2008). For References see also Tectonic boundaries in Germany.
broader: Lower Rhine Bight

Venlo graben
type: Concept
created: 2021-07-23T08:59:08.870Z
creator: schmar
notation: DE-1001
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12154
references: https://data.geoscience.earth/ncl/geoera/ref/12203
references: https://data.geoscience.earth/ncl/geoera/ref/12228
definition: [Domain type: Strongly deformed Tertiary sedimentary overburden, Basement: Rhenohercynian/Avalonia(?).]
scope note: The extent of the Cenozoic tectonostratigraphic sub-domain was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map reference: e.g. Reicherter et al. (2008). For References see also Tectonic boundaries in Germany.
broader: Lower Rhine Bight

Krefeld Block
type: Concept
created: 2021-07-23T08:59:08.873Z
creator: schmar
notation: DE-1002
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12154
references: https://data.geoscience.earth/ncl/geoera/ref/12203
references: https://data.geoscience.earth/ncl/geoera/ref/12228
definition: [Domain type: Deformed sedimentary overburden, Basement: Rhenohercynian/Avalonia(?).]
scope note: The extent of the Cenozoic tectonostratigraphic sub-domain was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map reference: e.g. Reicherter et al. (2008). For References see also Tectonic boundaries in Germany.
broader: Lower Rhine Bight

Cologne Block
type: Concept
created: 2021-07-23T08:59:08.876Z
creator: schmar
notation: DE-1003
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12154
references: https://data.geoscience.earth/ncl/geoera/ref/12203
references: https://data.geoscience.earth/ncl/geoera/ref/12228
definition: [Domain type: Deformed sedimentary overburden, Basement: Rhenohercynian/Avalonia(?).]
scope note: The extent of the Cenozoic tectonostratigraphic sub-domain was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map reference: e.g. Reicherter et al. (2008). For References see also Tectonic boundaries in Germany.
broader: Lower Rhine Bight

South Limburg Block
type: Concept
created: 2021-08-31T12:48:29.153Z
creator: schmar
in scheme: Tectonic Boundary Objects in Europe
notation: DE-1104
preferred label: Süd-Limburg-Block @de
scope note: The extent of the tectonostratigraphic sub-domain was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map reference: e.g. Reicherter et al. (2008). For References see also „Tectonic boundaries in Germany”.
definition: Rim of the Lower Rhine Bight. Only small parts of this structural unit are on German territory. Domain Type: sedimentary overburden; basement: Rhenohercynian; Outcrop age: 1st: L. Cret., Tertiary - Quaternary; 2nd: Paleozoic; Fault strike: SE/NE within basement /2nd: ESE
references: https://data.geoscience.earth/ncl/geoera/ref/12154
references: https://data.geoscience.earth/ncl/geoera/ref/12203
references: https://data.geoscience.earth/ncl/geoera/ref/12228
broader: Lower Rhine Bight

Merziger Graben & SW Saarland Triassic platform domain
scope note: We describe the Merziger Graben & SW Saarland Triassic platform domain as a Mesozoic tectonostratigraphic unit east of the Trier Bight on top of the Permo-Carboniferous of the Saar-Nahe Basin (DE-963). The boundary in the NE is defined by outcrop pattern of the Triassic . A clear boundary to the Trier Bight (DE-961) and the Pfalz-Pirmasens-Nancy Trough (DE-964) is not recognizable. The extent of this unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK1000, The Geological overview map of Rheinland Pfalz. For References see also Tectonic boundaries in Germany.
type: Concept
created: 2021-07-23T08:59:08.932Z
creator: schmar
notation: DE-962
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12223
definition: The Merziger graben & SW Saarland Triassic platform are located west of the Saar Nahe basin and contains a fault set with NNW-SSE and WSW-ENE running faults. The domain probably was a post-Triassic subsidence area. [Domain type: Sedimentary overburden, Basement: Saxothuringian.]
broader: Tectonic Boundary in Germany

Pfalz-Pirmasens-Nancy Trough
type: Concept
created: 2021-07-23T08:59:08.938Z
creator: schmar
notation: DE-964
in scheme: Tectonic Boundary Objects in Europe
definition: The Pfalz-Pirmasens-Nancy trough is located at the French-German border close the the Upper Rhine graben domain, and presents a Triassic through structure. [Domain type: Sedimentary overburden, Basement: Saxothuringian-Mid-German Crystalline High.]
scope note: We describe the Pfalz-Pirmasens-Nancy Trough as a Triassic tectonostratigraphic unit, whose boundaries are defined by faults, the outcrop of the Saar-Nahe Basin in the north as well as based on partly fuzzy trends of the lithofacies and thickness of the Triassic. The extent of this structural unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK1000, The Geological overview map of Rheinland Pfalz. For References see also Tectonic boundaries in Germany.
broader: Tectonic Boundary in Germany

Skurup Block
type: Concept
created: 2021-07-23T08:59:09.564Z
creator: schmar
notation: DE-1024
in scheme: Tectonic Boundary Objects in Europe
narrower: Skurup fault
narrower: Gat fault
references: https://data.geoscience.earth/ncl/geoera/ref/12155
references: https://data.geoscience.earth/ncl/geoera/ref/12237
references: https://data.geoscience.earth/ncl/geoera/ref/12238
references: https://data.geoscience.earth/ncl/geoera/ref/12233
definition: The Skurup Block is located within the Baltic Sea, is associated with the Teisseyre-Tornquist Zone and the Danish-Norwegian Basin. Domain type: deformed sedimentary overburden, Basement Domain: Baltica.
scope note: We describe the Skurup Block as a tectonostratigraphic unit, whose boundaries are only partly defined by faults. The outline of this tectonostratigraphic unit can be also defined based on lithostratigraphic trends. Even though the structure have been described (e. g. Seidel, 2019), no clear definition of the outline of this tectonostratigraphic unit has been made to date. The extent of this tectonic unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
broader: Tectonic Boundary in Germany

Skurup fault
type: Concept
created: 2021-07-23T08:59:09.536Z
creator: schmar
notation: DE-9023
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12237
references: https://data.geoscience.earth/ncl/geoera/ref/12238
references: https://data.geoscience.earth/ncl/geoera/ref/12233
definition: The NNW-SSE running Skurup fault close to the Danish border belongs to basement faults which are responsible for the stepwise southwestward dipping of Baltica (Seidel 2019).
broader: Skurup Block
broader: Møn-Arkona High

Gat fault
type: Concept
created: 2021-07-23T08:59:09.592Z
creator: schmar
notation: DE-9011
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12199
references: https://data.geoscience.earth/ncl/geoera/ref/12237
definition: The N-S running Gat fault close to the Danish border belongs to basement faults which are responsible for the stepwise southwestward dipping of Baltica (Seidel 2019).
broader: Gryfice Block
broader: Skurup Block

Münsterland Cretaceous Basin
notation: DE-1105
type: Concept
created: 2021-07-23T08:59:08.743Z
creator: schmar
narrower: Kurl fault
narrower: Wilhelmine-Victoria fault
narrower: Hervester fault
narrower: Thyssen-Westende fault
narrower: Achenbach fault
narrower: Königsborn fault
narrower: Flierich fault
narrower: Sachsen fault
narrower: Münster fault
narrower: Schwelgern fault
narrower: Rauendahl fault
narrower: Haltern fault
narrower: Alstätte fault
narrower: Wendfeld fault
narrower: Stadtlohn fault
narrower: Winterswijk fault
narrower: Öding fault
narrower: Weseke fault
narrower: Drevenacker fault
definition: The Münsterland Cretaceous Basin is located south of the Lower Saxony Basin and is characterized mostly by nearly flat lying solid Upper Cretaceous limestones near the surface and residual preserved Lower Cretaceous, which lie directly on Paleozoic rocks. Due to Late Cretaceous inversion tectonics Upper Cretaceous sediments are thickened and strongly faulted in the vicinity of the Osning thrust system (northern border fault system). This basin area on the southern margin of the North German Basin was a sedimentary platform with only low subsidence rates for most of the Mesozoic. Presumably parts of this region were uplifted with the Rhenish Massif during the Jurassic. The bedding conditions of the Upper Cretaceous of the central Münsterland are considered relatively undisturbed (Dölling & Juch 2009). The rocks below the Upper Cretaceous (locally also Lower Cretaceous) form the coal-bearing strata of the Upper Carboniferous and are intensively folded as a result of the Variscan orogeny (Drozdzweski & Wrede 1994). The SW-NE striking Variscan folds are displaced by NNW-SSE striking cross faults, such as the Rheinpreußen or Fliericher Sprung, Sekundus-, Teritus- or the Drevenacker fault. [Domain type: Late Cretaceous foreland basin, Basement: Rhenohercynian/Avalonia(?).]
scope note: We define here the Münsterland Cretaceous Basin as a Late Cretaceous tectonostratigraphic unit, whose boundaries are defined both by faults and fault systems, partly fuzzy trends in the lithofacies and, in particular by the distribution of Cretaceous sedimentary successions. To the Lower Saxony Basin, the boundary of the basin runs along the Osning thrust. Because of that, the extent/outline of the Münsterland Basin overlaps with the extent/outline of the Lower Saxony Basin in this region. To the east this tectonostratigraphic unit overlap with the Egge - Kellerwald fault system (DE-1055). A discrete boundary cannot be clearly identified. But the extent to the west and south is defined by the today distribution of the Cretaceous. The extent of the tectonostratigraphic domain was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map reference: GK 200 (map-sheet 3902, 3910, 3918, 4702, 4710, 4718), Baldschuhn et al. (1996, 1997, 2001). For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12184
references: https://data.geoscience.earth/ncl/geoera/ref/12185
broader: Tectonic Boundary in Germany

Münster fault
type: Concept
created: 2021-07-23T08:59:08.773Z
creator: schmar
notation: DE-305
in scheme: Tectonic Boundary Objects in Europe
definition: Undefined fault within the Münsterland Cretaceous Basin
broader: Münsterland Cretaceous Basin

Schwelgern fault
type: Concept
created: 2021-07-23T08:59:08.776Z
creator: schmar
notation: DE-430
in scheme: Tectonic Boundary Objects in Europe
definition: Undefined fault within the Münsterland Cretaceous Basin
broader: Münsterland Cretaceous Basin

Kurl fault
type: Concept
created: 2021-07-23T08:59:08.747Z
creator: schmar
notation: DE-209
in scheme: Tectonic Boundary Objects in Europe
definition: Undefined fault within the Münsterland Cretaceous Basin
broader: Münsterland Cretaceous Basin

Haltern fault
type: Concept
created: 2021-07-23T08:59:08.783Z
creator: schmar
notation: DE-685
in scheme: Tectonic Boundary Objects in Europe
definition: Undefined fault within the Münsterland Cretaceous Basin
broader: Münsterland Cretaceous Basin

Wilhelmine-Victoria fault
type: Concept
created: 2021-07-23T08:59:08.750Z
creator: schmar
notation: DE-295
in scheme: Tectonic Boundary Objects in Europe
definition: Undefined fault within the Münsterland Cretaceous Basin
broader: Münsterland Cretaceous Basin

Alstätte fault
type: Concept
created: 2021-07-23T08:59:08.787Z
creator: schmar
notation: DE-837
in scheme: Tectonic Boundary Objects in Europe
definition: WNW-ESE running faults within the NW-part of the Münsterland Cretaceous Basin, close to the Dutch border.
broader: Münsterland Cretaceous Basin

Hervester fault
type: Concept
created: 2021-07-23T08:59:08.753Z
creator: schmar
notation: DE-296
in scheme: Tectonic Boundary Objects in Europe
definition: Undefined fault within the Münsterland Cretaceous Basin
broader: Münsterland Cretaceous Basin

Wendfeld fault
type: Concept
created: 2021-07-23T08:59:08.791Z
creator: schmar
notation: DE-840
in scheme: Tectonic Boundary Objects in Europe
definition: WNW-ESE running faults within the NW-part of the Münsterland Cretaceous Basin, close to the Dutch border.
broader: Münsterland Cretaceous Basin

Thyssen-Westende fault
type: Concept
created: 2021-07-23T08:59:08.756Z
creator: schmar
notation: DE-300
in scheme: Tectonic Boundary Objects in Europe
definition: Undefined fault within the Münsterland Cretaceous Basin
broader: Münsterland Cretaceous Basin

Stadtlohn fault
type: Concept
created: 2021-07-23T08:59:08.795Z
creator: schmar
notation: DE-841
in scheme: Tectonic Boundary Objects in Europe
definition: WNW-ESE running faults within the NW-part of the Münsterland Cretaceous Basin, close to the Dutch border.
broader: Münsterland Cretaceous Basin

Achenbach fault
type: Concept
created: 2021-07-23T08:59:08.760Z
creator: schmar
notation: DE-301
in scheme: Tectonic Boundary Objects in Europe
definition: Undefined fault within the Münsterland Cretaceous Basin
broader: Münsterland Cretaceous Basin

Winterswijk fault
type: Concept
created: 2021-07-23T08:59:08.799Z
creator: schmar
notation: DE-846
in scheme: Tectonic Boundary Objects in Europe
definition: WNW-ESE running faults within the NW-part of the Münsterland Cretaceous Basin, close to the Dutch border.
broader: Münsterland Cretaceous Basin

Königsborn fault
type: Concept
created: 2021-07-23T08:59:08.763Z
creator: schmar
notation: DE-302
in scheme: Tectonic Boundary Objects in Europe
definition: Undefined fault within the Münsterland Cretaceous Basin
broader: Münsterland Cretaceous Basin

Öding fault
type: Concept
created: 2021-07-23T08:59:08.803Z
creator: schmar
notation: DE-848
in scheme: Tectonic Boundary Objects in Europe
definition: WNW-ESE running faults within the NW-part of the Münsterland Cretaceous Basin, close to the Dutch border.
broader: Münsterland Cretaceous Basin

Flierich fault
type: Concept
created: 2021-07-23T08:59:08.766Z
creator: schmar
notation: DE-303
in scheme: Tectonic Boundary Objects in Europe
definition: Undefined fault within the Münsterland Cretaceous Basin
broader: Münsterland Cretaceous Basin

Weseke fault
type: Concept
created: 2021-07-23T08:59:08.807Z
creator: schmar
notation: DE-850
in scheme: Tectonic Boundary Objects in Europe
definition: WNW-ESE running faults within the NW-part of the Münsterland Cretaceous Basin, close to the Dutch border.
broader: Münsterland Cretaceous Basin

Sachsen fault
type: Concept
created: 2021-07-23T08:59:08.769Z
creator: schmar
notation: DE-304
in scheme: Tectonic Boundary Objects in Europe
definition: Undefined fault within the Münsterland Cretaceous Basin
broader: Münsterland Cretaceous Basin

Drevenacker fault
type: Concept
created: 2021-07-23T08:59:08.811Z
creator: schmar
notation: DE-294
in scheme: Tectonic Boundary Objects in Europe
broader: Münsterland Cretaceous Basin

Cenozoic impact Nördlinger Ries
type: Concept
created: 2021-07-23T08:59:09.098Z
creator: schmar
notation: DE-1011
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12227
definition: The Nördlinger Ries structure is a Cenozoic (14.6 Ma) impact structure of 24 km in diameter, which is located between the Swabian and Franconian Alb.
broader: Tectonic Boundary in Germany

German basement highs
type: Concept
created: 2021-07-23T08:59:09.102Z
creator: schmar
narrower: Tectonostratigraphic Permo-Caboniferous Übergangsstockwerk
narrower: Moldanubian basement domain
narrower: Teplá-Barrandium domain
narrower: Saxothuringian basement domain
narrower: Mid-German Crystalline High
narrower: Rhenohercynian basement domain
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Germany

Moldanubian basement domain
type: Concept
created: 2021-07-23T08:59:09.169Z
creator: schmar
narrower: Bavarian-Bohemian Moldanubian fault set
narrower: Black Forest domain
in scheme: Tectonic Boundary Objects in Europe
definition: Variscan basement domain
broader: German basement highs

Bavarian-Bohemian Moldanubian fault set
definition: The Bavarian-Bohemian Moldanubian subdomain belongs to the Bohemian Massif domain and is located at the southwestern rim therein. The subdomain is characterized by SE/ESE striking faults and Late Cretaceous-Tertiary uplift of the long-living basement high. [Outcrop age: Proterozoic, Domain type: Variscan basement block, Basement: Moldanubian.]
type: Concept
created: 2021-07-23T08:59:09.172Z
creator: schmar
notation: DE-976
alternative label: Bavarian - Bohemian Moldanubian
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12188
references: https://data.geoscience.earth/ncl/geoera/ref/12189
references: https://data.geoscience.earth/ncl/geoera/ref/753
scope note: We describe the Bavarian - Bohemian Moldanubian as a tectonostratigraphic basement unit, whose boundaries are defined by faults and lithological changes. It's a combination of the Moldanubian basement rock outcrops of the Bavarian Forest and the Bohemian Massif. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Bavaria (LFU) provides and describes a more detailed and partly updated fault data set of Bavaria within the framework of the HIKE project (DE-BY_1531). Map Reference: GK 1:500000 of Bavaria (Freudenberger & Schwerd, 1996), tectonic map of Bavaria 1:1000000 (Freudenberger & Schwerd, 1996), HIKE (DE-BY 1531). For References see also Tectonic boundaries in Germany.
broader: Bohemian Massif & East German Variscan to Pre-Variscan basement highs
broader: Moldanubian basement domain

Black Forest domain
type: Concept
created: 2021-07-23T08:59:09.175Z
creator: schmar
notation: DE-969
narrower: Badenweiler-Lenzkirch fault system
narrower: Freiburg-Bonndorf-Bodensee fault system
scope note: We describe the Black Forest domain as the sum of the outcropping Moldanubian basement unit, whose boundaries are defined by faults, lithological changes as well as the outcrop of Pre-Zechstein basement, but also as a broad strongly uplifted region along the eastern shoulder of the Upper Rhine graben (Black Forest uplift). The region of the Black Forest uplift overlap partly with other defined structural regions (DE-990, DE-989, DE-1025, DE-985). The extent of this unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK 1000, geological overview map of Baden-Würtemberg, tectonic overview map of Baden Würtemberg. For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
narrower: Black forest basement high subdomain
references: https://data.geoscience.earth/ncl/geoera/ref/12243
references: https://data.geoscience.earth/ncl/geoera/ref/12197
references: https://data.geoscience.earth/ncl/geoera/ref/6390
definition: This subdomain represents the part of the Black Forest domain which is characterized by strong Cenozoic uplift and Moldanubian (partially Saxothuringian) basement. SE/NNE/ESE-SE striking faults within the structural domain of the Black Forest. Outcrop age: Proterozoic-Paleozoic
broader: Moldanubian basement domain

Black forest basement high subdomain
type: Concept
created: 2021-07-23T08:59:08.950Z
creator: schmar
notation: DE-971
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12243
references: https://data.geoscience.earth/ncl/geoera/ref/12197
references: https://data.geoscience.earth/ncl/geoera/ref/6390
alternative label: Black forrest basement high
definition: The Black Forest basement high subdomain represents the part of the Black Forest, which consists of outcropping pre-Zechstein basement (Moldanubian) and is characterized by predominantly SE/E-ESE striking faults. [Domain type: Variscan basement block, Basement: Moldanubian.]
scope note: We describe the Black Forest basement high as a outcropping Moldanubian basement unit, whose boundaries are defined by faults, lithological changes as well as the outcrop of Pre-Zechstein basement. The extent of this unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK 1000, geological overview map of Baden-Würtemberg, tectonic overview map of Baden Würtemberg. For References see also Tectonic boundaries in Germany.
broader: Black Forest domain

Badenweiler-Lenzkirch fault system
type: Concept
created: 2021-07-23T08:59:09.178Z
creator: schmar
notation: DE-970
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12243
references: https://data.geoscience.earth/ncl/geoera/ref/12197
references: https://data.geoscience.earth/ncl/geoera/ref/6390
definition: The Badenweiler-Lenzkirch fault system within the Black Forest, which probably was active in Cenozoic times and represents a pre-Variscian suture zone. The subdomain is characterized by strongly deformed basement and ESE-SE/NNE striking faults. [Domain type: Strongly deformed basement, Basement: Moldanubian. Outcrop age: Proterozoic to Early Paleozoic]
scope note: We describe the Badenweiler-Lenzkirch fault system as a strongly faulted basement block within the Black Forest basement domain, whose boundaries are defined by faults & lithological changes. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK 1000, geological overview map of Baden-Würtemberg, tectonic overview map of Baden Würtemberg . For References see also Tectonic boundaries in Germany.
broader: Black Forest domain

Freiburg-Bonndorf-Bodensee fault system
scope note: We describe the Freiburg-Bonndorf-Bodensee fault system as a major fault system crossing the Black Forest, but strikes also more westward towards the Kaiserstuhl within the Rhein Graben and more eastward towards the Molassse Basin and the Hegau volcanic field. The boundaries of this strongly faulted block are defined by fault zones with mostly SE/ESE strike. The extent of this unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK 1000, geological overview map of Baden-Würtemberg, tectonic overview map of Baden Würtemberg. For References see also Tectonic boundaries in Germany.
type: Concept
created: 2021-07-23T08:59:09.187Z
creator: schmar
notation: DE-985
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12243
references: https://data.geoscience.earth/ncl/geoera/ref/12197
references: https://data.geoscience.earth/ncl/geoera/ref/6390
definition: The Freiburg-Bonndorf-Bodensee fault system is a Cenozoic active structural element with a main strike direction ESE/SE and is located in strike of Cenozoic volcanic fields. [Domain type: Mixed basement and sedimentary coverage, Basement: Moldanubian, Outcrop age: Proterozoic-Paleozoic, Triassic, Jurassic]
broader: Black Forest domain

Saxothuringian basement domain
type: Concept
created: 2021-07-23T08:59:09.208Z
creator: schmar
narrower: Bohemian Massif & Variscan to Pre-Variscan fringe of the Bohemian Massif subdomain
narrower: Schiefergebirge nappe of Schmiedefeld Vesser
narrower: Elbezone
narrower: Lausitz Block
in scheme: Tectonic Boundary Objects in Europe
narrower: Northwestern Saxony Basement Block
definition: Variscan basement domain
broader: German basement highs

Elbezone
type: Concept
created: 2021-07-23T08:59:09.235Z
creator: schmar
notation: DE-980
narrower: Elbe Zone (Basement outcrops)
narrower: Saxonian Bohemian Cretaceous Basin
narrower: Mügeln depression
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12232
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: Variscan basement outcrops covered in parts by a Late Cretaceous foreland basin. This basement block borders the Erzgebirge to the SW and the Lausitz Block to the NW.
scope note: We describe the Elbe Zone as a tectonostratigraphic basement unit, whose boundaries are defined by faults and lithological changes. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: Röllig et al. (1990), Franke (2020)
broader: Saxothuringian basement domain

Saxonian Bohemian Cretaceous Basin
type: Concept
created: 2021-07-23T08:59:09.242Z
creator: schmar
notation: DE-982
notation: DE-639
notation: DE-638
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12232
references: https://data.geoscience.earth/ncl/geoera/ref/12196
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The Saxonian-Bohemian Cretaceous Basin represents a Cretaceous thrust foreland basin in the south of the uplifted Lausitz-Block. It lies on residual Triassic and Saxothuringian basement of the Saxony-Czech Elbe Zone. [Domain type: Late Cretaceous foreland basin]
scope note: The Saxonian Bohemian Cretaceous Basin is not part of the Saxothuringian basement domain of the Elbe Zone, but lies in the top of them. The here defined extent results from the today distribution of Upper Cretaceous sediments (Röllig et al. 1990, Katzung & Ehmke, 1993, digital GK 400 of Saxony).
broader: Elbezone

Mügeln depression
type: Concept
created: 2021-07-23T08:59:09.247Z
creator: schmar
notation: DE-983
notation: DE-638
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12232
references: https://data.geoscience.earth/ncl/geoera/ref/12196
references: https://data.geoscience.earth/ncl/geoera/ref/8031
scope note: The Mügeln Depression is not part of the Saxothuringian basement domain of the Elbe Zone, but lies in the top of them. The here defined extent results from the today distribution of Triassic to Late Permian sediments (Röllig et al. 1990, Katzung & Ehmke, 1993, digital GK 400 of Saxony).
definition: The Mügeln depression represents a sedimentary Permo-Triassic relict surrounded in east and west by faults which are probably active during the Late Cretaceous. Those faults have partly Mesozoic to Paleozoic pre-cursors which are partly reactivated as reverse faults or define the strike of faults during Late Cretaceous. Because of wide-scale uplift and related intense erosion, Permo-Triassic remnants are often only preserved in the footwall of reverse faults. The Pre-Permian basement in the footwall of the Mügeln depression belongs to the Northwestern Saxony Basement Block and the Elbe Zone. The Permo-Triassic of this depression represents a rim facies of the North German Basin. This erosional relict is covered by Tertiary to Quaternary sediments. [Domain type: foreland syncline, Basement: Saxothuringian/ Permo-Carboniferous Post-Variscan basement unit]
broader: Elbezone

Elbe Zone (Basement outcrops)
type: Concept
created: 2021-07-23T08:59:08.680Z
creator: schmar
notation: DE-981
alternative label: Basement outcrops
references: https://data.geoscience.earth/ncl/geoera/ref/12232
in scheme: Tectonic Boundary Objects in Europe
definition: The basement subdomain of the Elbe zone domain is located at the northern rim of the Bohemian Massif, characterized by Saxothuringan basement and shows NW-SE running faults. [Domain type: Mixed basement and sedimentary coverage, Basement: Saxothuringian. Outcrop age: Paleozoic basement, Late Cretaceous, Neogene cover.]
references: https://data.geoscience.earth/ncl/geoera/ref/8031
scope note: We describe the Elbe Zone as a tectonostratigraphic basement unit, whose boundaries are defined by faults and lithological changes. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: Röllig et al. (1990), Franke (2020). For References see also Tectonic boundaries in Germany.
broader: Bohemian Massif & East German Variscan to Pre-Variscan basement highs
broader: Elbezone

Bohemian Massif & Variscan to Pre-Variscan fringe of the Bohemian Massif subdomain
type: Concept
created: 2021-07-23T08:59:09.212Z
creator: schmar
in scheme: Tectonic Boundary Objects in Europe
narrower: Erzgebirge fault set
narrower: Fichtelgebirge fault set
narrower: Granulitgebirge fault set
narrower: Thuringian-Franconian-Voigtland Schiefergebirge fault set
definition: Variscan basement outcrops
broader: Saxothuringian basement domain

Fichtelgebirge fault set
type: Concept
created: 2021-07-23T08:59:08.660Z
creator: schmar
notation: DE-974
scope note: We describe the Fichtelgebirge as a tectonostratigraphic basement unit, whose boundaries are defined by faults and lithological changes. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Bavaria (LFU) provides and describes a more detailed and partly updated fault data set of Bavaria within the framework of the HIKE project (DE-BY_1531). Map Reference: GK 1:500000 of Bavaria (Freudenberger & Schwerd, 1996), HIKE (DE-BY_1531). For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
alternative label: Fichtelgebirge
references: https://data.geoscience.earth/ncl/geoera/ref/753
definition: The Fichtelgebirge belongs to the Bohemian Massif domain and is located at the northwestern rim therein. The subdomain consists of Saxonthuringian basement and is characterized by SE-ESE striking faults. [Outcrop age: Proterozoic-Paleozoic, Domain type: Variscan basement block, Basement: Saxothuringian.]
broader: Bohemian Massif & Variscan to Pre-Variscan fringe of the Bohemian Massif subdomain
broader: Bohemian Massif & East German Variscan to Pre-Variscan basement highs

Thuringian-Franconian-Voigtland Schiefergebirge fault set
type: Concept
created: 2021-07-23T08:59:08.667Z
creator: schmar
notation: DE-975
scope note: We describe the Thuringian-Franconian-Voigtland Schiefergebirge as a tectonostratigraphic basement unit, whose boundaries are defined by faults and lithological changes. It's a combination of the Schiefergebirge units of Franconia, Thuringia & the Voigtland. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Bavaria (LFU) provides and describes a more detailed and partly updated fault data set of Bavaria within the framework of the HIKE project (DE-BY_1531). Map Reference: GK 1:200000 of Thuringia, GK 1:100000 of the Thuringian Forest (Kästner, 1996), GK 1:500000 of Bavaria (Freudenberger & Schwerd, 1996), tectonic map of Bavaria 1:1000000 (Freudenberger & Schwerd, 1996), Röllig et al. (1990). For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
alternative label: Thuringian-Franconian-Voigtland Schiefergebirge
references: https://data.geoscience.earth/ncl/geoera/ref/753
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The Thuringian-Franconian-Voigtland Schiefergebirge subdomain belongs to the Bohemian Massif domain and is located at the northwesternmost rim therein. The subdomain consists of Saxonthuringian basement and is characterized by SE-SSE/SSE striking faults. [Outcrop age: Ordovician-Carboniferous, Domain type: Variscan basement block, Basement: Saxothuringian.]
broader: Bohemian Massif & East German Variscan to Pre-Variscan basement highs
broader: Bohemian Massif & Variscan to Pre-Variscan fringe of the Bohemian Massif subdomain

Granulitgebirge fault set
type: Concept
created: 2021-07-23T08:59:08.648Z
creator: schmar
notation: DE-972
in scheme: Tectonic Boundary Objects in Europe
alternative label: Granulitgebirge
references: https://data.geoscience.earth/ncl/geoera/ref/12232
references: https://data.geoscience.earth/ncl/geoera/ref/12221
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/8052
definition: The Granulitgebirge is one of structural elements that mantle the Bohemian Massif in the north. The subdomain consists of Saxonthuringian basement and is characterized by SE striking faults. [Outcrop age: Proterozoic, Domain type: Variscan basement block, Basement: Saxothuringian.]
scope note: We describe the Granulitgebirge as a tectonostratigraphic basement unit, whose boundaries are defined by faults and lithological changes. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: Röllig et al. (1990), existing outlines: e.g. Katzung & Ehmke (1993), Franke (2020). For References see also Tectonic boundaries in Germany.
broader: Bohemian Massif & Variscan to Pre-Variscan fringe of the Bohemian Massif subdomain
broader: Bohemian Massif & East German Variscan to Pre-Variscan basement highs

Erzgebirge fault set
type: Concept
created: 2021-07-23T08:59:08.652Z
creator: schmar
notation: DE-973
in scheme: Tectonic Boundary Objects in Europe
narrower: Gera-Jachimov fault system
alternative label: Erzgebirge
references: https://data.geoscience.earth/ncl/geoera/ref/12232
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/8052
definition: The Erzgebirge subdomain belongs to the Bohemian Massif domain and is located at the northern rim therein. The subdomain consists of Saxonthuringian basement and is characterized by prominent SE/NE striking faults. [Outcrop age: Proterozoic-Early Paleozoic, Domain type: Variscan basement block, Basement: Saxothuringian]
scope note: We describe the Erzgebirge as a tectonostratigraphic basement unit, whose boundaries are defined by faults and lithological changes. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: Röllig et al. (1990), existing outlines: e.g. Katzung & Ehmke (1993), Franke (2020). For References see also Tectonic boundaries in Germany.
broader: Bohemian Massif & East German Variscan to Pre-Variscan basement highs
broader: Bohemian Massif & Variscan to Pre-Variscan fringe of the Bohemian Massif subdomain

Gera-Jachimov fault system
type: Concept
created: 2021-07-23T08:59:09.221Z
creator: schmar
notation: DE-977
notation: DE-649
notation: DE-640
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12232
references: https://data.geoscience.earth/ncl/geoera/ref/8052
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: Long living (Pre-Permian? - Permo-Carboniferous to Late Ctretaceous) fault system located within the Erzgebirge. The strongly deformed basement belongs to the Saxothuringian. [Outcrop age: Paleozoic, Domain type: Strongly deformed basement, Basement: Saxothuringian.]
scope note: We describe the Gera-Jachimov fault system as a strongly faulted block, whose boundaries are defined by faults. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: Röllig et al. (1990), existing outlines: e.g. Franke (2020). For References see also Tectonic boundaries in Germany.
broader: Erzgebirge fault set

Tectonostratigraphic Permo-Caboniferous Übergangsstockwerk
type: Concept
created: 2021-07-23T08:59:09.105Z
creator: schmar
narrower: Northwestern Saxony Basement Block
narrower: Vorerzgebirge depression & Nossen-Wilsdruff Schiefergebirge
narrower: Wittlich Depression subdomain
in scheme: Tectonic Boundary Objects in Europe
narrower: Thuringian Forest fault set
narrower: Saar-Nahe Basin domain
definition: Post-Variscan basement domain
broader: German basement highs

Vorerzgebirge depression & Nossen-Wilsdruff Schiefergebirge
type: Concept
created: 2021-07-23T08:59:09.132Z
creator: schmar
notation: DE-1041
narrower: Hohenstein-Arnsdorf fault
narrower: Riechberg fault
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12232
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/8052
definition: A basement high with Variscan outcrops
scope note: We describe the Vorerzgebirge depression & Nossen-Wilsdruff Schiefergebirge as a tectonostratigraphic basement unit, whose boundaries are defined by faults in the north and south as well as by outcrop pattern of the Permo-Carboniferous Übergangsstockwerk. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: Franke (2020), Röllig et al. (1990), existing outlines: e.g. Katzung & Ehmke (1993), Franke (2020).
broader: Tectonostratigraphic Permo-Caboniferous Übergangsstockwerk

Hohenstein-Arnsdorf fault
type: Concept
created: 2021-07-23T08:59:09.135Z
creator: schmar
notation: DE-663
in scheme: Tectonic Boundary Objects in Europe
broader: Vorerzgebirge depression & Nossen-Wilsdruff Schiefergebirge

Riechberg fault
type: Concept
created: 2021-07-23T08:59:09.139Z
creator: schmar
notation: DE-664
in scheme: Tectonic Boundary Objects in Europe
broader: Vorerzgebirge depression & Nossen-Wilsdruff Schiefergebirge

Mid-German Crystalline High
type: Concept
created: 2021-07-23T08:59:09.302Z
creator: schmar
narrower: Halle-Wittenberg Block
narrower: Odenwald
narrower: Spessart
in scheme: Tectonic Boundary Objects in Europe
narrower: Thuringian Forest fault set
definition: Variscan basement domain
broader: German basement highs

Odenwald
type: Concept
created: 2021-07-23T08:59:09.379Z
creator: schmar
notation: DE-1017
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12241
references: https://data.geoscience.earth/ncl/geoera/ref/12243
references: https://data.geoscience.earth/ncl/geoera/ref/12195
definition: The Odenwald domain represents a Tertiary uplift, is located at the NNE rim of the Upper Rhine graben and is characterized by NNE-SSW running faults. [Domain type: Mixed basement and sedimentary coverage/variscan basement block, Basement: Saxothuringian - Mid-German Crystalline High.]
scope note: We describe the Odenwald as a tectonostratigraphic basement unit, whose boundaries are defined by faults and the outcrop of the Pre-Zechstein. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK 1:1000000 of Germany, GK 1:300000 of Hesse
broader: Mid-German Crystalline High

Spessart
type: Concept
created: 2021-07-23T08:59:09.383Z
creator: schmar
notation: DE-1032
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12241
references: https://data.geoscience.earth/ncl/geoera/ref/12243
references: https://data.geoscience.earth/ncl/geoera/ref/12195
definition: The Spessart basement high domain represents an uplifted/eroded part of the eastern shoulder of the Upper Rhine graben. [Domain type: Variscan basement block, Basement: Saxothuringian - Mid-German Crystlline High.]
scope note: We describe the Spessart as a tectonostratigraphic basement unit, whose boundaries are defined by faults and the outcrop of the Pre-Zechstein. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK 1:1000000 of Germany, GK 1:300000 of Hesse
broader: Mid-German Crystalline High

Rhenohercynian basement domain
type: Concept
created: 2021-07-23T08:59:09.387Z
creator: schmar
narrower: Harz fault set
narrower: Werra Uplift
narrower: Transition Harz - Halle-Wittenberg Block (Hettstedter Sattel)
narrower: Haldensleben-Wittenberg uplift
narrower: Rhenish Massif domain
in scheme: Tectonic Boundary Objects in Europe
broader: German basement highs

Transition Harz - Halle-Wittenberg Block (Hettstedter Sattel)
type: Concept
created: 2021-07-23T08:59:09.400Z
creator: schmar
notation: DE-1038
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8071
references: https://data.geoscience.earth/ncl/geoera/ref/8052
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: A narrow W-E oriented basement high with mainly metamorphic rocks belong to the Phyllitic Zone and the Mid-German crystalline High
scope note: We describe the Transition Harz - Halle-Wittenberg Block (Hettstedter Sattel) as a tectonostratigraphic basement unit, whose boundaries are defined by faults and especially by outcop pattern of the Pre-Zechstein. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: Martiklos et al. (2001), existing outlines: e.g. Katzung & Ehmke (1993), Franke (2020), Martiklos et al. (2001)
broader: Rhenohercynian basement domain

Teplá-Barrandium domain
type: Concept
created: 2021-07-23T08:59:09.190Z
creator: schmar
narrower: Bohemian Massif
in scheme: Tectonic Boundary Objects in Europe
definition: Variscan Basement domain
broader: German basement highs

Bohemian Massif
type: Concept
created: 2021-07-23T08:59:09.193Z
creator: schmar
narrower: Marienbad-Complex / Western Bohemian Shearzone / Tepla-Domazlice Zone
narrower: Tirschenreuth-Mähring Zone
narrower: Erbendorf-Vohenstrauss Zone
narrower: Münchberg Crystalline complex
scope note: We describe the Bohemian (Teplá-Barrandium) block as a tectonostratigraphic basement unit, whose boundaries are defined by faults and lithological changes. It's a combination of the Tepla-Barrandium basement rock outcrops of the Bavarian Forest and the Bohemian Massif. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Bavaria (LFU) provides and describes a more detailed and partly updated fault data set of Bavaria within the framework of the HIKE project (DE-BY_1531). Map Reference: GK 1:500000 of Bavaria (Freudenberger & Schwerd, 1996), tectonic map of Bavaria 1:1000000 (Freudenberger & Schwerd, 1996), HIKE-BY (<https://repository.europe-geology.eu/egdidocs/hike/7488_hike_fault_de-by_1494.jpg)
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12188
references: https://data.geoscience.earth/ncl/geoera/ref/12189
references: https://data.geoscience.earth/ncl/geoera/ref/753
definition: Variscan basement outcrop/high
broader: Teplá-Barrandium domain

Tirschenreuth-Mähring Zone
type: Concept
created: 2021-07-23T08:59:09.200Z
creator: schmar
notation: DE-1081
scope note: We describe the Tirschenreuth-Mähring Zone as a tectonostratigraphic basement unit (Teplá-Barrandium), whose boundaries are defined by faults and lithological changes. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Bavaria (LFU) provides and describes a more detailed and partly updated fault data set of Bavaria within the framework of the HIKE project (DE-BY_1531). Map Reference: GK 1:500000 of Bavaria (Freudenberger & Schwerd, 1996), tectonic map of Bavaria 1:1000000 (Freudenberger & Schwerd, 1996), HIKE-BY (<https://repository.europe-geology.eu/egdidocs/hike/7488_hike_fault_de-by_1494.jpg)
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12188
references: https://data.geoscience.earth/ncl/geoera/ref/12189
references: https://data.geoscience.earth/ncl/geoera/ref/753
definition: Variscan basement outcrop/high
broader: Bohemian Massif

Erbendorf-Vohenstrauss Zone
type: Concept
created: 2021-07-23T08:59:09.202Z
creator: schmar
notation: DE-1080
scope note: We describe the Erbendorf-Vohenstrauss Zone as a tectonostratigraphic basement unit (Teplá-Barrandium), whose boundaries are defined by faults and lithological changes. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations, that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Bavaria (LFU) provides and describes a more detailed and partly updated fault data set of Bavaria within the framework of the HIKE project (DE-BY_1531). Map Reference: GK 1:500000 of Bavaria (Freudenberger & Schwerd, 1996), tectonic map of Bavaria 1:1000000 (Freudenberger & Schwerd, 1996), HIKE-BY (<https://repository.europe-geology.eu/egdidocs/hike/7488_hike_fault_de-by_1494.jpg)
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12188
references: https://data.geoscience.earth/ncl/geoera/ref/12189
references: https://data.geoscience.earth/ncl/geoera/ref/753
definition: Variscan basement outcrop/high
broader: Bohemian Massif

Münchberg Crystalline complex
scope note: We describe the Münchberg Crystalline complex as a tectonostratigraphic basement unit (Teplá-Barrandium), whose boundaries are defined by faults and lithological changes. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Bavaria (LFU) provides and describes a more detailed and partly updated fault data set of Bavaria within the framework of the HIKE project (DE-BY_1531). Map Reference: GK 1:500000 of Bavaria (Freudenberger & Schwerd, 1996), HIKE-BY (<https://repository.europe-geology.eu/egdidocs/hike/7488_hike_fault_de-by_1494.jpg)
type: Concept
created: 2021-07-23T08:59:09.206Z
creator: schmar
notation: DE-1010
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12188
references: https://data.geoscience.earth/ncl/geoera/ref/12189
references: https://data.geoscience.earth/ncl/geoera/ref/753
definition: The allochthonous Münchberg crystalline complex/nappe belongs to the Teplá-Barrandium and is located within the Bohemian Massif. [Domain type: Variscan basement block, Basement: Teplá-Barrandium]
broader: Bohemian Massif & East German Variscan to Pre-Variscan basement highs
broader: Bohemian Massif

Marienbad-Complex / Western Bohemian Shearzone / Tepla-Domazlice Zone
alternative label: Marienbad-Complex / Western Bohemian Shearzone / Teplá-Domazlice zone
type: Concept
created: 2021-07-23T08:59:09.196Z
creator: schmar
notation: DE-1071
scope note: We describe the Marienbad-Complex / Western Bohemian Shearzone / Teplá-Domazlice zone as a tectonostratigraphic basement unit (Teplá-Barrandium) and major Basement Shear Zone whose boundaries are defined by faults and lithological changes. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Bavaria (LFU) provides and describes a more detailed and partly updated fault data set of Bavaria within the framework of the HIKE project (DE-BY_1531). Map Reference: GK 1:500000 of Bavaria (Freudenberger & Schwerd, 1996), tectonic map of Bavaria 1:1000000 (Freudenberger & Schwerd, 1996), HIKE (DE-BY 1531). For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12188
references: https://data.geoscience.earth/ncl/geoera/ref/12189
references: https://data.geoscience.earth/ncl/geoera/ref/753
definition: Domain type: Variscan basement block, Basement: Moldanubian.
broader: Bavarian - Bohemian Teplá-Barrandian
broader: Bohemian Massif

North German Basin - domain I: North German Plain & Central German North Sea
narrower: West Schleswig Block
narrower: southern branch Horn Graben
narrower: Horn Graben
narrower: East Frisia – Ems Estuary Region
narrower: Thrusted Central North German Basin sub-domains
narrower: Rheinsberg Trough
narrower: Lower Saxony Basin
narrower: Ems Lineament
narrower: Glückstadt Graben
definition: The western and central part of the North German Basin (NGB) is characterized by a very complex pattern of grabens and structural highs, while the south is dominated by compressional structures. Due to pronounced overprint by salt tectonics, the causal tectonic influences on the structural genesis, however, is difficult to determine (Müller et al. 2016). The northern part of the NGB, especially in the German North Sea sector and in Schleswig-Holstein, is significantly influenced by the N-S-running Glückstadt Graben, Horn Graben and - in the very northwest - bordered by the Central Graben within the so called Entenschnabel area. The latter is moreover limited to the Central German North Sea by the North Schillgrund / Coffee Soil Fault. The formation of these large intracontinental rifts and the system of interconnected smaller Lower Rotliegend graben structures, as assumed by Gast (1988), is directly related in time to the disintegration of Pangaea and the development of large rift structures in the area of today's North Atlantic (i.a. Rockall-Faeroe Rift; Ziegler 1990). As structural highs, platform areas and sedimentary basin areas with only minor tectonics respectively, e.g. the Schillgrund High, G+L-Platform, the West Schleswig Block, the Mecklenburg Brandenburg Depression characterize the western and central part of the North German Basin. Towards the south, the structures of the German North Sea Sector and the Glückstadt Graben continuously merge into a not clear distinct structural region the Pompeckj Scholle (or Pompeckj Block). This Jurassic to Cretaceous platform to high is dissected by several, mostly already Triassic, fault zones, such as the Leer-Bremen Lineament or the Uelzen Lineament. As this structural region cannot be distinguished from neighboring parts of the basin in north-eastern Germany, neither in terms of facial nor structural aspects, the necessity of this structural division is questioned in recent literature (Müller et al., 2016). The faul…
scope note: We define here the North German Basin - domain I as a tectonostratigraphic unit, whose boundaries are defined both by faults and fault systems, often fuzzy trends in the lithofacies and, in particular by the expression of deformation events. The division into two domains of the North German Basin (NGB) is intended to indicate in particular the uplift of some basin regions during the Late Cretaceous and the associated different levels of erosion in this region. Depending on the level of erosion and the preservation of signs of former deformation phases, this results in regionally partly different dominant fault patterns, even if these deformation phases have influenced almost the entire basin. The Lower Saxony Basin, which was actually also strongly inverted during the Late Cretaceous, should therefore actually be part of domain II of the NGB: uplifted and/ or inverted southern regions of the North German Basin. However, it is also largely part of the German lowlands. In this respect, the subdivision made here should only be understood as a rough classification. The extent of the tectonostratigraphic domain was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described or discussed in detail in the future. For References see also Tectonic boundaries in Germany.
type: Concept
created: 2021-07-23T08:59:09.455Z
creator: schmar
notation: DE-1065
narrower: Northeastern rim of the North German Basin
in scheme: Tectonic Boundary Objects in Europe
narrower: Central North German Basin
narrower: Braunschweig-Gifhorn-Lüneburg fault system
narrower: Eastern rim of the North German Basin/ Szczecin-Kaliesz-East Brandenburg Swell
narrower: Prignitz-Lausitz-Riesengebirge Anticline
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/12192
references: https://data.geoscience.earth/ncl/geoera/ref/12198
references: https://data.geoscience.earth/ncl/geoera/ref/12210
references: https://data.geoscience.earth/ncl/geoera/ref/12215
references: https://data.geoscience.earth/ncl/geoera/ref/12217
references: https://data.geoscience.earth/ncl/geoera/ref/12223
references: https://data.geoscience.earth/ncl/geoera/ref/8033
references: https://data.geoscience.earth/ncl/geoera/ref/8022
references: https://data.geoscience.earth/ncl/geoera/ref/91
broader: Tectonic Boundary in Germany

West Schleswig Block
created: 2021-09-06T15:55:18.880Z
creator: schmar
type: Concept
in scheme: Tectonic Boundary Objects in Europe
notation: DE-1089
scope note: We describe here the "West Schleswig Block" as a tectonostratigraphic unit whose boundaries are defined both by faults and fault systems, salt structures as well as partly fuzzy trends in the lithofacies and thickness of stratigraphic units. Even though the main structures of this unit have been described in detail (e.g. Kockel et al. 1991, Kockel, 1995), no clear definition of the outline of the structural unit has been made to date. The extent of this tectonostratigraphic sub-domain of the "North German Basin" was newly created with a view to a structured assignment of fault data and the assignment of an uniform structural history for this sub-domain. The outline is based on the analysis of a large number of partly contradictory map series and citations that were generalised for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Outline definition is redefined and summarized from Baldschuhn et al. (1996) (especially structural maps and profiles), Baldschuhn et al. (2001), and the structure of the Base Zechstein based on Baldschuhn et al. (2001) & Doornenbal & Stevenson (2010) and is especially related to the profiles of the GTA (Baldschuhn et al. 1996) and existing 3D models (BGR, 2021) observed major offsets in the base Zechstein as well as high thicknesses of the Keuper, Buntsandstein. Uncertainties depend on whether the outline is drawn based on the structure of the top basement or the distribution of sediments and fault pattern in the overburden, there may be major differences (salt tectonics/tectonic decoupling).
definition: Following Kockel (1995), this unit covers the greatest part of the German North Sea sector. lt is bordered in the west and southwest by the salt structures Erika-Dina-Hilde-Helma-Hannelore, Heike, Hilda Nord-Hilda Süd and Herta-Halla-Lollo. The southern border runs from Julia and Jasmin to Jette and north of Johanna, Josephine and Feuerschiff Elbe I to the Eiderstedt peninsula. In the north, the southern margin of the Ringköbing-Fyn High borders the West Schleswig Block and in the east the Oldenswort - Mildstedt salt structure. In the SW a narrow promontory, characterized by the salt pillows Henni, Henni Nord and Hulda reaches the Harald Lineament, which belongs to the Horn Graben system. The West Schleswig Block is characterized structurally by the general subcrop of Keuper or Muschelkalk-Upper Buntsandstein below the Late Cimmerian unconformity, by the lack of major basement faults and the absence of salt diapirs. A few basement faults of minor importance parallel to the eastern Horn Graben boundary fault have been observed in the west, straddled by the salt pillows Elisa, Jutta and Helen. In the east, basement faults again occur below the Rochelsteert salt pillow. The rest of the West Schleswig Block is exceptionally little deformed. The broad, very flat salt pillows do not show any preferred direction. The salt movements into the sa!t pillows on the West Schleswig Block began by pre-Early Cretaceous times in most cases and often continued during the Late Cretaceous and Early Tertiary. The Helgoland salt pillow has not yet reached the diapiric stage and only a crestal graben originated in post-Middle Miocene times (BINOT 1988, 1991). In the context of the entire North German Basin, the WSB can rather be regarded as a sediment platform most of the time without major fluctuations in the thickness distribution of the Mesozoic.
references: https://data.geoscience.earth/ncl/geoera/ref/8022
references: https://data.geoscience.earth/ncl/geoera/ref/12159
references: https://data.geoscience.earth/ncl/geoera/ref/12431
references: https://data.geoscience.earth/ncl/geoera/ref/12432
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/12430
broader: North German Basin - domain I: North German Plain & Central German North Sea

southern branch Horn Graben
type: Concept
created: 2021-09-06T15:57:04.961Z
creator: schmar
in scheme: Tectonic Boundary Objects in Europe
notation: DE-1092
scope note: We describe here the "southern branch of the Horn Graben" as a tectonic unit whose boundaries are defined both by faults and fault systems, salt structures as well as partly fuzzy trends in the thickness of stratigraphic units. Even though the main structures of this unit have been described in detail (e.g. Kockel et al. 1991, Kockel, 1995), no clear definition of the outline of the structural unit has been made to date. The extent of this tectonic sub-domain of the "North German Basin" was newly created with a view to a structured assignment of fault data and the assignment of an uniform structural history for this sub-domain. The outline is based on the analysis of a large number of partly contradictory map series and citations that were generalised for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Redefined and summarized from Baldschuhn et al. (1996) (especially structural maps and profiles), Baldschuhn et al. (2001), and the structure of the Base Zechstein based on Baldschuhn et al. (2001). The outline definition is especially related to the profiles of the GTA (Baldschuhn et al. 1996) and existing 3D models (BGR, 2021). Uncertainties depend on whether the outline is drawn based on the structure of the top basement or the distribution of sediments and fault pattern in the overburden, there may be major differences (salt tectonics/tectonic decoupling).
definition: This southern extension of the Horn Graben developed from the Middle to the Upper Triassic. The Harald Lineament, the Hanno & Heiner Escarpment connect the northern extensions of the Ems Lineament with the central part of the Horn Graben. The interplay of rifting and reactive diapirism led to the formation of assymetric diapirs and salt mini-basins and was described by Thieme & Rockenbauch (1999) as example for raft tectonics.
references: https://data.geoscience.earth/ncl/geoera/ref/12159
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/12431
references: https://data.geoscience.earth/ncl/geoera/ref/12430
references: https://data.geoscience.earth/ncl/geoera/ref/12432
broader: North German Basin - domain I: North German Plain & Central German North Sea

Horn Graben
creator: schmar
created: 2021-09-06T15:58:47.341Z
type: Concept
in scheme: Tectonic Boundary Objects in Europe
notation: DE-1093
scope note: We describe here the "Horn Graben" as a tectonostratigraphic unit whose boundaries are defined both by faults and fault systems, salt structures as well as partly fuzzy trends in the lithofacies and thickness of stratigraphic units. Even though the main structures of this unit have been described in detail (e.g. Kockel et al. 1991, Kockel, 1995, Best 1983), no clear definition of the outline of the structural unit has been made to date. The extent of this tectonostratigraphic sub-domain of the "North German Basin" was newly created with a view to a structured assignment of fault data and the assignment of an uniform structural history for this sub-domain. The outline is based on the analysis of a large number of partly contradictory map series and citations that were generalised for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Redefined and summarized from Baldschuhn et al. (1996) (especially structural maps and profiles), Baldschuhn et al. (2001), and the structure of the Base Zechstein based on Baldschuhn et al. (2001). Outline definition is especially related to the profiles of the GTA (Baldschuhn et al. 1996) and existing 3D models (BGR, 2021) observed major offsets in the base Zechstein as well as high thicknesses of the Triassic (esp. Middle Buntsandstein and partly Mid-Triassic). Uncertainties depend on whether the outline is drawn based on the structure of the top basement or the distribution of sediments and fault pattern in the overburden, there may be major differences (salt tectonics/tectonic decoupling).
definition: The Horn Graben is the most prominent structural element of the Central German North Sea. It is a up to roughly 10000 m deep aborted rift with the main activity during the Triassic. The graben show besides halotectonic mobilization of thick Zechstein salt also the mobilization of Upper Rotliegend formations (Jähne-Klingberg et al. 2018b). The Horn Graben shows similarities but also clear differences to the neighbouring rifts (Central Graben & Glückstadt Graben) (Jähne-Klingberg et al. 2018). @de
references: https://data.geoscience.earth/ncl/geoera/ref/12159
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/12431
references: https://data.geoscience.earth/ncl/geoera/ref/12430
references: https://data.geoscience.earth/ncl/geoera/ref/12204
references: https://data.geoscience.earth/ncl/geoera/ref/12432
broader: North German Basin - domain I: North German Plain & Central German North Sea

Central North German Basin
scope note: We describe the Central North German Basin as a tectonostratigraphic sub-domain of the North German Basin whose boundaries are not clearly defined by faults and fault systems. The outline of the domain can only be roughly defined based on lithostratigraphic trends and on the base of differences in the deformation pattern to surrounding areas. Even though the main structures, Basin Centre within the Northwestern part of the North German Basin / the West-Mecklenburg Block / The Mecklenburg-Brandenburg Depression, of this region have been described in detail (e. g. Baldschuhn et al., 2001; Katzung & Ehmke, 1993), no clear definition of the outline of this basin part has been made to date. The extent of this tectonic unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Saxony-Anhalt provides and describes a partly more detailed and updated fault data set of Saxony-Anhalt within the framework of the HIKE project (DE-ST-0, DE-ST-1000). Definition of the outline: deepest parts of the North German Basin basin outside of grabens (e.g. Glückstadt Graben) were summarized as well as areas with low deformation in the Mesozoic-Cenozoic overburden and only minor offsets at the base Zechstein. Uncertainties: The following transitions cannot be clearly defined because they are not tied to discrete structures: 1.) Transition to the east to the element eastern rim NGB, 2.) Transition to the NE to the element northeastern rim NGB, 3.) Transition to the Prignitz Wall (an anticline with major erosion in the top), 4.) Transition to the East Brandenburg-North Sudete…
type: Concept
created: 2021-07-23T08:59:08.143Z
creator: schmar
notation: DE-952
narrower: Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression
definition: The Central German basin subdomain is defined by several grouped blocks (defined in the GTA) in the central, deeply subsided area of the NGB. It is characterized by thermal subsidence and no clear overprinting by Upper Cretaceous contractional tectonics. In the eastern part of the basin, many ESE/SE longitudinally elongated salt structures occur (presumed relation to raft-tectonics), and it is also characterized by fewer diapirs or salt walls than in the surrounding structural areas. Large regions in the western and central parts are characterized by deep ablation before and during the Upper Jurassic and deepest Lower Cretaceous, as well as deposition of only low thickness marine younger Lower Cretaceous and a thick Upper Cretaceous cover. This typical Tectonostratigraphy is also summarized under the name Pompeckj block. In addition to a generally low degree of structuring, the subdomain is characterized by relatively high stratiform salt thicknesses of the Zechstein and Oberrotliegend. Embedded in the eastern basin part, the NNE striking Rheinsberg Trough crosses the subdomain (could also be considered part of the central basin part. Map reference: redefined and summarized from Baldschuhn et al. (1996) (esp. structural maps and profiles), Baldschuhn et al. (1997) & Katzung & Ehmke (1993), and base Zechstein from Doornenbal & Stevenson (2010). [Domain type: Sedimentary overburden, Basement: Avalonia/Rhenohercynian.]
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12159
references: https://data.geoscience.earth/ncl/geoera/ref/12161
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/8052
broader: North German Basin - domain I: North German Plain & Central German North Sea

Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression
type: Concept
created: 2021-07-23T08:59:08.146Z
creator: schmar
notation: DE-953
narrower: Lower Elbe fault
narrower: Arendsee Deep fracture fault
narrower: Rockenthin fault
narrower: Salzwedel fault
narrower: Bedekaspel-Marga fault zone
narrower: Quickborn fault
narrower: Stade-Langenfeld fault zone
narrower: Witzhave-Segeberg-Plön fault zone
narrower: Bahlburg-Hohenhorn fault zone
narrower: Moisburg-Reitbrook fault zone
narrower: Lübtheen-Camin fault
narrower: Strackholt-Langeoog-Mira fault zone
narrower: Gudow-Gülze-Sumte fault zone
narrower: Oldendorf-Adolphsdorf fault zone
narrower: Berdum-Jaderberg-Sagermeer fault
narrower: Uelzen lineament
scope note: The Center of the NGB can be subdivided in three sub-domains (Basin Centre within the Northwestern part of the North German Basin / the West-Mecklenburg Block / The Mecklenburg-Brandenburg Depression). Those can be described as tectonostratigraphic sub-domains of the North German Basin, whose boundaries are not clearly defined by faults and fault systems. The outline of the sub-domains can only be roughly defined based on lithostratigraphic trends and on the base of differences in the deformation pattern to surrounding areas. Even though the main structures of this region have been described in detail (e. g. Baldschuhn et al., 2001; Katzung & Ehmke, 1993), no clear definition of the outline of this basin part has been made to date. The extent of this tectonic unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12159
references: https://data.geoscience.earth/ncl/geoera/ref/12161
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/8052
broader: Central North German Basin

Salzwedel fault
type: Concept
created: 2021-07-23T08:59:08.160Z
creator: schmar
notation: DE-512
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The western part of the 74 km long, WNW-ESE running Salzwedel fault is located at the northern rim of the Altmark-Fläming depression and merges with the Central North German Basin (Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression) in the eastern part. This listric fault is a southwest dipping reverse fault that was reactivated during Uppper Cretaceous inversion.
broader: Altmark Fläming Depression
broader: Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression

Berdum-Jaderberg-Sagermeer fault
type: Concept
created: 2021-07-23T08:59:08.196Z
creator: schmar
notation: DE-758
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12190
definition: The 93 km long, NNW-SSE running Berdum-Jaderberg-Saagermeer fault zone is located with the southern part in the Südoldenburg-Hoya block (the thrusted part of the Central North German basin) and in the northern part within the Central North German basin (Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression). Associated with this fault zone are the salt structures Saagermeer, Jaderberg and Berdum-Jever.
broader: Südoldenburg & Hoya Block
broader: Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression

Bedekaspel-Marga fault zone
type: Concept
created: 2021-07-23T08:59:08.163Z
creator: schmar
notation: DE-717
notation: DE-719
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 21 km and respectively 37 km long, N-S oriented Bedekaspel-Marga fault zone is located within the Central North German basin (Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression).
broader: Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression

Uelzen lineament
type: Concept
created: 2021-07-23T08:59:08.199Z
creator: schmar
notation: DE-767
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12190
definition: The 126 km long, NW-SE Uelzen fault zone is running at the northern rim of the Rotenburg-Soltau-Eldingen block, which belongs to the thrusted part of the Central North German basin, an runs further north into the Central North German Basin (Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression). In the southern section this fault zone was involved in the sedimentary and structural development of the Eichsfeld Altmark swell. Above this fault zone synsedimentary grabens, horsts, and half grabens originated in the Early Triassic rocks.
broader: Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression
broader: Rotenburg-Soltau-Eldingen Block

Quickborn fault
type: Concept
created: 2021-07-23T08:59:08.166Z
creator: schmar
notation: DE-722
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 23 km long, N-S oriented Quickborn fault is located within the Central North German basin (Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression), close to the Glückstadt graben subdomain.
broader: Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression

Stade-Langenfeld fault zone
type: Concept
created: 2021-07-23T08:59:08.169Z
creator: schmar
notation: DE-723
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 55 km long, WNW-ESE oriented Stade-Langenfeld fault zone is located within the Central North German basin (Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression), close to the Glückstadt graben subdomain.
broader: Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression

Witzhave-Segeberg-Plön fault zone
type: Concept
created: 2021-07-23T08:59:08.172Z
creator: schmar
notation: DE-726
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 94 km long, N-S oriented Witzhave-Segeberg-Plön fault zone is located within the Central North German basin (Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression), close to the Glückstadt graben subdomain.
broader: Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression
broader: eastern branch Glückstadt Graben

Bahlburg-Hohenhorn fault zone
type: Concept
created: 2021-07-23T08:59:08.176Z
creator: schmar
notation: DE-733
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 70 km long, NNE-SSW oriented Bahlburg-Hohenhorn fault zone is located within the Central North German basin (Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression) and borders to the thrusted part of the basin - the Rotenburg-Soltau-Eldingen Block.
broader: Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression

Moisburg-Reitbrook fault zone
type: Concept
created: 2021-07-23T08:59:08.179Z
creator: schmar
notation: DE-737
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 41 km long, WSW-ENE oriented Moisburg-Reitbrook fault is located within the Central North German basin (Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression).
broader: Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression

Lübtheen-Camin fault
type: Concept
created: 2021-07-23T08:59:08.182Z
creator: schmar
notation: DE-738
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 42 km long, N-S oriented Lübtheen-Camin fault is located within the Central North German basin (Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression).
broader: Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression

Strackholt-Langeoog-Mira fault zone
type: Concept
created: 2021-07-23T08:59:08.186Z
creator: schmar
notation: DE-739
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 57 km long, N-S oriented Strackholt-Langeoog-Mira fault zone is located within the Central North German basin (Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression) and is characterized by normal faults within the overburden of the associated salt diapirs.
broader: Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression

Arendsee Deep fracture fault
type: Concept
created: 2021-07-23T08:59:08.153Z
creator: schmar
notation: DE-508
in scheme: Tectonic Boundary Objects in Europe
notation: DE-513
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The 28 km/18 km long, NNE-SSW running Arendsee deep fracture fault is a basement fault located within the NW-part of the Altmark-Fläming depression of the thrusted Central North German Basin and within the Central North German Basin (Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression) respectively. The southern part of the fault also is associated with the Eichsfeld-Altmark swell.
broader: Altmark Fläming Depression
broader: Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression

Gudow-Gülze-Sumte fault zone
type: Concept
created: 2021-07-23T08:59:08.189Z
creator: schmar
notation: DE-741
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 32 km long, NNW-SSE oriented Gudow-Gülze-Sumte fault zone is located within the eastern area of the Central North German basin (Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression).
broader: Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression

Rockenthin fault
type: Concept
created: 2021-07-23T08:59:08.156Z
creator: schmar
notation: DE-509
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The 8 km long, NNE-SSW running Rockenthin fault is located at the southern tip within the Altmark Fläming depression of the thrusted Central North German Basin and at the northern part within the Central North German basin (Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression) and the Eichsfeld-Altmark swell. Fault activity already observable during Triassic times, main activity of the reverse fault during Upper Cretaceous and related graben structures show Lower Cretaceous infill.
broader: Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression
broader: Altmark Fläming Depression

Oldendorf-Adolphsdorf fault zone
type: Concept
created: 2021-07-23T08:59:08.193Z
creator: schmar
notation: DE-743
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 35 km long, NNW-SSE oriented Oldenforf-Adolphsdorf fault zone is located within the western area of the Central North German basin (Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression).
broader: Central NWGB - Ostholstein-West-Mecklenburg Block - Mecklenburg-Brandenburg Depression
broader: Southern Glückstadt Graben - Krummendeich - Hohenlockstedt Graben

East Frisia – Ems Estuary Region
type: Concept
created: 2021-09-06T16:00:24.080Z
creator: schmar
in scheme: Tectonic Boundary Objects in Europe
notation: DE-1090
scope note: We describe here the "East Frisia – Ems Estuary Region" as a tectonostratigraphic unit whose boundaries are defined both by faults and fault systems, salt structures as well as partly fuzzy trends in the lithofacies and thickness of stratigraphic units. Even though the main structures of this unit have been described in detail (e.g. Kockel et al. 1991, Kockel, 1995), no clear definition of the outline of the structural unit has been made to date. The extent of this tectonostratigraphic sub-domain of the "North German Basin" was newly created with a view to a structured assignment of fault data and the assignment of an uniform structural history for this sub-domain. The outline is based on the analysis of a large number of partly contradictory map series and citations that were generalised for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Redefined and summarized from Baldschuhn et al. (1996) (especially structural maps and profiles), Baldschuhn et al. (2001), and the structure of the Base Zechstein based on Baldschuhn et al. (2001). Outline definition is especially related to the profiles of the GTA (Baldschuhn et al. 1996) and existing 3D models (BGR, 2021). Uncertainties depend on whether the outline is drawn based on the structure of the top basement or the distribution of sediments and fault pattern in the overburden, there may be major differences (salt tectonics/tectonic decoupling).
definition: This structural region lies in the northern extension of the Ems Lineament. Five NNE striking fault systems with associated salt walls cross and border this structural region.
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/12430
references: https://data.geoscience.earth/ncl/geoera/ref/12431
references: https://data.geoscience.earth/ncl/geoera/ref/12432
references: https://data.geoscience.earth/ncl/geoera/ref/12159
broader: North German Basin - domain I: North German Plain & Central German North Sea

Glückstadt Graben
scope note: We describe here the Glückstadt Graben as a tectonostratigraphic unit, divided into 7 blocks, whose boundaries are defined both by faults and fault systems as well as partly fuzzy trends in the lithofacies. Even though the main structures of this basin have been described in detail (e.g. Baldschuhn et al., 2001), no clear definition of the outline of the graben and the structures within has been made to date. The extent of this tectonostratigraphic sub-domain of the North German Basin was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: Redefined and summarized from Baldschuhn et al. (1996, 1997), Doornenbal & Stevenson (2010). Redefined and summarized from Baldschuhn et al. (1996) (especially structural maps and profiles), Baldschuhn et al. (1997), and the structure of the Base Zechstein based on the GTA & Doornenbal & Stevenson (2010). Especially related to the profiles of the GTA and observed major offsets in the base Z as well as high thicknesses of the Keuper, Buntsandstein. NNE striking salt walls of the region were taken into account as limiting structures of internal teconic units. Depending on whether the contours are drawn based on the structure of the top basement or the distribution of sediments in the overburden, there may be major differences (salt tectonics/tectonic decoupling). The transition to the south into the Central Northwest German Basin cannot be clearly defined. For References see also Tectonic boundaries in Germany.
type: Concept
created: 2021-07-23T08:59:08.008Z
creator: schmar
notation: DE-947
narrower: Central Glückstadt Graben
narrower: Mittelschleswig-Neumünster Block
narrower: Southern Glückstadt Graben - Krummendeich - Hohenlockstedt Graben
narrower: Western branch Glückstadt Graben
narrower: Southwestern Glückstadt Graben
narrower: eastern branch Glückstadt Graben
narrower: Emtinghausen-Krautsand fault system
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12159
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/12173
references: https://data.geoscience.earth/ncl/geoera/ref/12248
definition: The Glückstadt Graben subdomain represents an aborted intracontinental rift and deepest of Mesozoic rifts in the Southern Permian Basin. The subdomain is characterized by high thicknesses of the Buntsandstein, Keuper and younger Mesozoic sediments in the rim synclines of salt walls. Moreover, intensive salt tectonics with intensive mobilization of the thick Rotliegend salinar are observed (References: e.g. Warsitzka et al. (2016)). [Domain type: Deformed sedimentary overburden, Basement: Avalonia]
broader: North German Basin - domain I: North German Plain & Central German North Sea

Southern Glückstadt Graben - Krummendeich - Hohenlockstedt Graben
narrower: Süderhastedt-Sieverstedt fault zone
scope note: We describe here the Southern Glückstadt Graben - Krummendeich - Hohenlockstedt Graben as a separate tectonic block of the Glückstadt-Graben, whose boundaries are defined both by faults and fault systems as well as salt walls. Even though the main structures of this region have been described in detail (e.g. Baldschuhn et al., 2001), no clear definition of the outline of the tectonic unit and the structures within has been made to date. The extent of this tectonostratigraphic sub-domain of the Southern Glückstadt Graben - Krummendeich - Hohenlockstedt Graben was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: Redefined and summarized from Baldschuhn et al. (1996, 1997), Doornenbal & Stevenson (2010). Outline definition: a) Redefined and summarized from Baldschuhn et al. (1996) (especially structural maps and profiles), Baldschuhn et al. (1997), and the structure of the Base Zechstein based on the GTA & Doornenbal & Stevenson (2010). b) Especially related to the profiles of the GTA and observed major offsets in the base Z as well as high thicknesses of the Keuper, Buntsandstein. c) NNE striking salt walls of the region were taken into account as limiting structures of internal teconic units. Uncertainties: Depending on whether the contours are drawn based on the structure of the top basement or the distribution of sediments in the overburden, there may be major differences (salt tectonics/tectonic decoupling). The transition to the south into the Central Northwest German Basin cannot be clearly defined. For References see also Tectonic boundaries in Germany.
type: Concept
created: 2021-07-23T08:59:08.049Z
creator: schmar
notation: DE-949
narrower: Sushörn fault
narrower: Itzehoe fault
narrower: Allstedt-Altenbruch fault zone
narrower: Basdahl-Belmhusen fault zone
in scheme: Tectonic Boundary Objects in Europe
narrower: Krempe-Lägerdorf fault zone
narrower: Oldendorf-Adolphsdorf fault zone
references: https://data.geoscience.earth/ncl/geoera/ref/12159
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The subdomain of the Southern Glückstadt Graben/Krummendeich-Hohenlockstedt Block represents a summary of southern parts and already defined blocks of the Glückstadt graben with similar characteristics. In this region, the dominant structural trend with NNE strikes is disturbed by ESE striking cross elements. From there, the impression of undulating salt structures in the overburden is created. Bounded to the east by the Emtinghausen-Krautsand lineament. [Domain type: Deformed sedimentary overburden, Basement: Avalonia.]
broader: Glückstadt Graben

Krempe-Lägerdorf fault zone
type: Concept
created: 2021-07-23T08:59:08.121Z
creator: schmar
notation: DE-711
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 41 km long, WSW-ENE oriented Krämpe-Lägerdorf fault zone is located within the region of the Eastern and Southern Glückstadt Graben - Krummendeich - Hohenlockstedt Block and belongs superordinately to the Glückstadt graben subdomain.
broader: Southern Glückstadt Graben - Krummendeich - Hohenlockstedt Graben
broader: eastern branch Glückstadt Graben

Sushörn fault
type: Concept
created: 2021-07-23T08:59:08.052Z
creator: schmar
notation: DE-702
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 29 km long, WNW-ESE oriented Sushörn fault belongs superordinately to the Glückstadt graben subdomain, and is located with the southern part within the region of the Southern Glückstadt Graben - Krummendeich - Hohenlockstedt Block and with the northern part within the western branch of the Glückstadt graben.
broader: Southern Glückstadt Graben - Krummendeich - Hohenlockstedt Graben

Süderhastedt-Sieverstedt fault zone
type: Concept
created: 2021-07-23T08:59:08.092Z
creator: schmar
notation: DE-869
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 60 km long, NNE-SSW oriented Süderhastedt-Sieverstadt fault zone is located within the western branch of the Glückstadt graben.
broader: Western branch Glückstadt Graben
broader: Southern Glückstadt Graben - Krummendeich - Hohenlockstedt Graben

Itzehoe fault
type: Concept
created: 2021-07-23T08:59:08.056Z
creator: schmar
notation: DE-706
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 42 km long, NW-SE oriented Itzehoe fault belongs superordinately to the Glückstadt graben subdomain, and is located with the SE-part within the region of the Southern Glückstadt Graben - Krummendeich - Hohenlockstedt Block and with the NW-part within the western branch of the Glückstadt graben.
broader: Southern Glückstadt Graben - Krummendeich - Hohenlockstedt Graben

Allstedt-Altenbruch fault zone
type: Concept
created: 2021-07-23T08:59:08.062Z
creator: schmar
notation: DE-714
notation: DE-727
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 47 km long, NNW-SSW/ NNW-SSE oriented Allstedt-Altenbruch fault zone belongs superordinately to the Glückstadt graben subdomain, and is located within the region of the Southern Glückstadt Graben - Krummendeich - Hohenlockstedt Block and partially runs within the south western Glückstadt graben.
broader: Southern Glückstadt Graben - Krummendeich - Hohenlockstedt Graben
broader: Southwestern Glückstadt Graben

Basdahl-Belmhusen fault zone
type: Concept
created: 2021-07-23T08:59:08.066Z
creator: schmar
notation: DE-735
notation: DE-886
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 57 km long, N-S/NE-SW oriented Basdahl-Belmhusen fault zone is located within the region of the Southern Glückstadt Graben - Krummendeich - Hohenlockstedt Block and belongs superordinately to the Glückstadt graben subdomain.
broader: Southern Glückstadt Graben - Krummendeich - Hohenlockstedt Graben

Southwestern Glückstadt Graben
scope note: We describe here the Southwestern Glückstadt Graben as a separate tectonostratigraphic block of the Glückstadt-Graben, whose boundaries are defined both by faults and salt walls as well as partly fuzzy trends in the lithofacies. Even though the main structures of this region have been described in detail (e.g. Baldschuhn et al., 2001), no clear definition of the outline of the tectonic block and the structures within has been made to date. The extent of this tectonostratigraphic sub-domain of the Southwestern Glückstadt Graben was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: Redefined and summarized from Baldschuhn et al. (1996, 1997), Doornenbal & Stevenson (2010). Outline definition: a) Redefined and summarized from Baldschuhn et al. (1996) (especially structural maps and profiles), Baldschuhn et al. (1997), and the structure of the Base Zechstein based on the GTA & Doornenbal & Stevenson (2010). b) Especially related to the profiles of the GTA and observed major offsets in the base Z as well as high thicknesses of the Keuper, Buntsandstein. c) NNE striking salt walls of the region were taken into account as limiting structures of internal teconic units. Uncertainties: Depending on whether the contours are drawn based on the structure of the top basement or the distribution of sediments in the overburden, there may be major differences (salt tectonics/tectonic decoupling). The transition to the south into the Central Northwest German Basin cannot be clearly defined. For References see also Tectonic boundaries in Germany.
type: Concept
created: 2021-07-23T08:59:08.095Z
creator: schmar
notation: DE-951
narrower: Cuxhaven-Büsum fault zone
narrower: Wangerooge-Midlum fault
narrower: Rüstringen fault zone
narrower: Dedesdorf fault
in scheme: Tectonic Boundary Objects in Europe
narrower: Allstedt-Altenbruch fault zone
references: https://data.geoscience.earth/ncl/geoera/ref/12159
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The subdomain of the southwestern Glückstadt graben represents a summary of southwestern parts, south of the ESE striking Neufeld Sand fault. the subdomain is also intersected by the ESE striking Wangerooge-Midlum fault. In this area, the Glückstadt graben trends S/SW into the Central North German Basin. [Domain type: Deformed sedimentary overburden, Basement: Avalonia.]
broader: Glückstadt Graben

Cuxhaven-Büsum fault zone
type: Concept
created: 2021-07-23T08:59:08.098Z
creator: schmar
notation: DE-709
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 54 km long, NNE-SSW oriented Cuxhaven-Büsum fault zone is located with the NW-part within the western branch of the Glückstadt graben and with the SW-part within the southwestern Glückstadt graben.
broader: Southwestern Glückstadt Graben
broader: Western branch Glückstadt Graben

Wangerooge-Midlum fault
type: Concept
created: 2021-07-23T08:59:08.105Z
creator: schmar
notation: DE-715
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 66 km long, WNW-ESE oriented Wangerooge-Midlum fault zone belongs superordinately to the Glückstadt graben subdomain, and is located within the region of the Southern Glückstadt Graben - Krummendeich - Hohenlockstedt Block and the Central North German basin.
broader: Southwestern Glückstadt Graben

Rüstringen fault zone
type: Concept
created: 2021-07-23T08:59:08.108Z
creator: schmar
notation: DE-716
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 30 km long, NE-SW oriented Rüstringen fault zone belongs superordinately to the Glückstadt graben, and is located within the southwestern part therein.
broader: Southwestern Glückstadt Graben

Dedesdorf fault
type: Concept
created: 2021-07-23T08:59:08.111Z
creator: schmar
notation: DE-728
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 30 km long, NNW-SSE oriented Dedesdorf fault belongs superordinately to the Glückstadt graben, and is located within the southwestern part therein.
broader: Southwestern Glückstadt Graben

Emtinghausen-Krautsand fault system
type: Concept
created: 2021-07-23T08:59:08.136Z
creator: schmar
notation: DE-984
narrower: Emtinghausen-Krautsand lineament
scope note: We describe the Emtinghausen-Krautsand fault system as a prominent narrow fault system which separates tectonic units in the centre of the northwestern part of the North German Basin and to the north seperates internal tectonic blocks of the Glückstadt Graben. Even though the main structures of this faulted region have been described in detail (e.g. Baldschuhn et al., 2001), no clear definition of the outline of this strongly deformed block has been made to date. The extent of this fault system was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12190
definition: A N/NNE striking fault zone mostly with only minor offsets in base Zechstein (except in Glückstadt Graben). Characterized in the overburden by a chain of diapirs and salt walls with crestal structures. Crosses & bounds various parts of the NW part of the North German Basin - from the South Oldenburg Block to the southern Glückstadt Graben. The overriding fault pattern appears to be offset N-S along this zone, large-scale facies/strat. trends, on the other hand, seem to be only slightly influenced (e.g. Frisch & Kockel (2004). [Domain type: Strongly deformed sedimentary overburden, Basement: Avalonia.]
broader: Glückstadt Graben

Emtinghausen-Krautsand lineament
type: Concept
created: 2021-07-23T08:59:08.139Z
creator: schmar
notation: DE-885
in scheme: Tectonic Boundary Objects in Europe
broader: Emtinghausen-Krautsand fault system
broader: eastern branch Glückstadt Graben

Mittelschleswig-Neumünster Block
scope note: We describe here the Mittelschleswig-Neumünster Block as a separate tectonic block of the Glückstadt-Graben, whose boundaries are defined both by faults and fault systems as well as salt walls. Even though the main structures of this region have been described in detail (e.g. Baldschuhn et al., 2001), no clear definition of the outline of the tectonic block and the structures within has been made to date. The extent of this tectonostratigraphic sub-domain of the Mittelschleswig-Neumünster Block was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Redefined and summarized from Baldschuhn et al. (1996, 1997), Doornenbal & Stevenson (2010). Outline definition: a) Redefined and summarized from Baldschuhn et al. (1996) (especially structural maps and profiles), Baldschuhn et al. (1997), and the structure of the Base Zechstein based on the GTA & Doornenbal & Stevenson (2010). b) Especially related to the profiles of the GTA and observed major offsets in the base Z as well as high thicknesses of the Keuper, Buntsandstein. c) NNE striking salt walls of the region were taken into account as limiting structures of internal teconic units. Uncertainties: Depending on whether the contours are drawn based on the structure of the top basement or the distribution of sediments in the overburden, there may be major differences (salt tectonics/tectonic decoupling). The transition to the south into the Central Northwest German Basin cannot be clearly defined. Uncertainties: 1.) Transition to CNGB is not clear in detail, 2.) Overburden structures are decoupled from the basement by halotectonics - thus overburden structures only approximately trace structures of the basement. F…
type: Concept
created: 2021-07-23T08:59:08.029Z
creator: schmar
notation: DE-948
narrower: Sterup fault
narrower: Osterby-Schinkel fault
narrower: Flensburg fault
narrower: Holnis fault
in scheme: Tectonic Boundary Objects in Europe
narrower: Mönkloh-Waabs fault zone
references: https://data.geoscience.earth/ncl/geoera/ref/12159
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The subdomain of the Mittelschleswig-Neumünster block represents the graben area east and north of the central area. Similar structural areas were grouped together. [Domain type: Deformed sedimentary overburden, Basement: Avalonia.]
broader: Glückstadt Graben

Sterup fault
type: Concept
created: 2021-07-23T08:59:08.032Z
creator: schmar
notation: DE-693
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 33 km long, N-S oriented Sterup fault is located within the Mittelschleswig-Neumünster block of the Glückstadt Graben subdomain.
broader: Mittelschleswig-Neumünster Block

Osterby-Schinkel fault
type: Concept
created: 2021-07-23T08:59:08.036Z
creator: schmar
notation: DE-696
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 36 km long, NW-SE oriented Osterby-Schinkel fault is located within the Mittelschleswig-Neumünster block of the Glückstadt Graben subdomain.
broader: Mittelschleswig-Neumünster Block

Flensburg fault
type: Concept
created: 2021-07-23T08:59:08.039Z
creator: schmar
notation: DE-701
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 40 km long, N-S oriented Flensburg fault is located within the Mittelschleswig-Neumünster block of the Glückstadt Graben subdomain.
broader: Mittelschleswig-Neumünster Block

Holnis fault
type: Concept
created: 2021-07-23T08:59:08.046Z
creator: schmar
notation: DE-883
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 33 km long, N-S oriented Hölnis fault is located within the Mittelschleswig-Neumünster block of the Glückstadt Graben subdomain.
broader: Mittelschleswig-Neumünster Block

Mönkloh-Waabs fault zone
type: Concept
created: 2021-07-23T08:59:08.118Z
creator: schmar
notation: DE-705
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
broader: eastern branch Glückstadt Graben
broader: Mittelschleswig-Neumünster Block

Western branch Glückstadt Graben
scope note: We describe here the Western branch Glückstadt Graben as a separate tectonostratigraphic block of the Glückstadt-Graben, whose boundaries are defined both by faults and salt walls as well as partly fuzzy trends in the lithofacies. Even though the main structures of this region have been described in detail (e.g. Baldschuhn et al., 2001), no clear definition of the outline of the tectonic block and the structures within has been made to date. The extent of this tectonostratigraphic sub-domain of the Western branch Glückstadt Graben was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: Redefined and summarized from Baldschuhn et al. (1996, 1997), Doornenbal & Stevenson (2010). Outline definition: a) Redefined and summarized from Baldschuhn et al. (1996) (especially structural maps and profiles), Baldschuhn et al. (1997), and the structure of the Base Zechstein based on the GTA & Doornenbal & Stevenson (2010). b) Especially related to the profiles of the GTA and observed major offsets in the base Z as well as high thicknesses of the Keuper, Buntsandstein. c) NNE striking salt walls of the region were taken into account as limiting structures of internal teconic units. Uncertainties: Depending on whether the contours are drawn based on the structure of the top basement or the distribution of sediments in the overburden, there may be major differences (salt tectonics/tectonic decoupling). The transition to the south into the Central Northwest German Basin cannot be clearly defined. For References see also Tectonic boundaries in Germany.
type: Concept
created: 2021-07-23T08:59:08.076Z
creator: schmar
notation: DE-950
narrower: Oldenswort-Mildstedt fault zone
narrower: Marne-Süderstapel fault zone
narrower: Neufelder-Sand fault
narrower: Süderhastedt-Sieverstedt fault zone
in scheme: Tectonic Boundary Objects in Europe
narrower: Cuxhaven-Büsum fault zone
references: https://data.geoscience.earth/ncl/geoera/ref/12159
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The subdomain of the western margin of the Glückstadt Graben represents a summary of western parts of the Glückstadt Graben. Several NNE striking salt walls in the overburden and underlying not always clearly defined basement faults. The domain is to the NW delineated from the West Schleswig Block by an ambiguous but steep slope (blind or previously unmapped basement fault). [Domain type: Deformed sedimentary overburden, Basement: Avalonia.]
broader: Glückstadt Graben

Neufelder-Sand fault
type: Concept
created: 2021-07-23T08:59:08.085Z
creator: schmar
notation: DE-708
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 54 km long, WNW-ESE oriented Neufelder-Sand fault is located within the western branch of the Glückstadt graben.
broader: Western branch Glückstadt Graben

Oldenswort-Mildstedt fault zone
type: Concept
created: 2021-07-23T08:59:08.079Z
creator: schmar
notation: DE-699
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 77 km long, NE-SW oriented Oldenswort-Mildstedt fault zone is located within the western branch of the Glückstadt graben.
broader: Western branch Glückstadt Graben

Marne-Süderstapel fault zone
type: Concept
created: 2021-07-23T08:59:08.082Z
creator: schmar
notation: DE-704
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 85 km long, NNE-SSW oriented Marne-Süderstapel fault zone is located within the western branch of the Glückstadt graben.
broader: Western branch Glückstadt Graben

Central Glückstadt Graben
scope note: We describe here theCentral Glückstadt Graben as a separate tectonic block of the Glückstadt Graben, whose boundaries are defined both by faults and fault systems as well as salt walls. Even though the main structures of this basin have been described in detail (e.g. Baldschuhn et al., 2001), no clear definition of the outline of tectonic block and the structures within has been made to date. The extent of this tectonostratigraphic sub-domain of the Central Glückstadt Graben was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Redefined and summarized from Baldschuhn et al. (1996, 1997), Doornenbal & Stevenson (2010). Outline definition: a) Redefined and summarized from Baldschuhn et al. (1996) (especially structural maps and profiles), Baldschuhn et al. (1997), and the structure of the Base Zechstein based on the GTA & Doornenbal & Stevenson (2010). b) Especially related to the profiles of the GTA and observed major offsets in the base Z as well as high thicknesses of the Keuper, Buntsandstein. c) NNE striking salt walls of the region were taken into account as limiting structures of internal teconic units. Uncertainties: Depending on whether the contours are drawn based on the structure of the top basement or the distribution of sediments in the overburden, there may be major differences (salt tectonics/tectonic decoupling). The transition to the south into the Central Northwest German Basin cannot be clearly defined. For References see also Tectonic boundaries in Germany.
type: Concept
created: 2021-07-23T08:59:08.013Z
creator: schmar
notation: DE-946
narrower: Oldenbüttel-Langsee fault zone
narrower: Rendsburg fault zone
narrower: Peissen-Westensee fault zone
narrower: Looft fault zone
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12159
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/12173
references: https://data.geoscience.earth/ncl/geoera/ref/12248
definition: The subdomain of the Central Glückstadt graben represents the central part of the entire graben with the highest Triassic subsidence (reference e.g. Warsitzka et al. (2019), Baldschuhn et al. (1996, 1997)). [Domain type: Deformed sedimentary overburden, Basement: Avalonia.]
broader: Glückstadt Graben

Oldenbüttel-Langsee fault zone
type: Concept
created: 2021-07-23T08:59:08.016Z
creator: schmar
notation: DE-695
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 57 km long, NNE-SSW oriented Oldenbüttel-Langsee fault zone is located within the Central Glückstadt Graben.
broader: Central Glückstadt Graben

Rendsburg fault zone
type: Concept
created: 2021-07-23T08:59:08.019Z
creator: schmar
notation: DE-697
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 39 km long, W-E oriented Rendsburg fault zone belongs superordinately to the Glückstadt Graben subdomain and is located with the eastern part within the Central Glückstadt Graben, and with the western part within the western branch of the Glückstadt Graben.
broader: Central Glückstadt Graben

Peissen-Westensee fault zone
type: Concept
created: 2021-07-23T08:59:08.023Z
creator: schmar
notation: DE-700
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 42 km long, NNE-SSW oriented Peissen-Westensee fault zone is located within the Central Glückstadt graben.
broader: Central Glückstadt Graben

Looft fault zone
type: Concept
created: 2021-07-23T08:59:08.026Z
creator: schmar
notation: DE-703
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 34 km long, NW-SE oriented Looft fault zone is located within the Central Glückstadt Graben.
broader: Central Glückstadt Graben

eastern branch Glückstadt Graben
narrower: Witzhave-Segeberg-Plön fault zone
scope note: We describe here the eastern branch Glückstadt Graben as a separate tectonostratigraphic block of the Glückstadt-Graben, whose boundaries are defined both by faults and salt walls as well as partly fuzzy trends in the lithofacies. Even though the main structures of this region have been described in detail (e.g. Baldschuhn et al., 2001), no clear definition of the outline of the tectonic block and the structures within has been made to date. The extent of this tectonostratigraphic sub-domain of the eastern branch Glückstadt Graben was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: Redefined and summarized from Baldschuhn et al. (1996, 1997), Doornenbal & Stevenson (2010). Outline definition: a) Redefined and summarized from Baldschuhn et al. (1996) (especially structural maps and profiles), Baldschuhn et al. (1997), and the structure of the Base Zechstein based on the GTA & Doornenbal & Stevenson (2010). b) Especially related to the profiles of the GTA and observed major offsets in the base Z as well as high thicknesses of the Keuper, Buntsandstein. c) NNE striking salt walls of the region were taken into account as limiting structures of internal teconic units. Uncertainties: Depending on whether the contours are drawn based on the structure of the top basement or the distribution of sediments in the overburden, there may be major differences (salt tectonics/tectonic decoupling). The transition to the south into the Central Northwest German Basin cannot be clearly defined. For References see also Tectonic boundaries in Germany.
type: Concept
created: 2021-07-23T08:59:08.114Z
creator: schmar
notation: DE-1063
narrower: Mönkloh-Waabs fault zone
narrower: Krempe-Lägerdorf fault zone
narrower: Elmshorn-Sievershütten fault zone
in scheme: Tectonic Boundary Objects in Europe
narrower: Emtinghausen-Krautsand lineament
references: https://data.geoscience.earth/ncl/geoera/ref/12159
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/12173
broader: Glückstadt Graben

Elmshorn-Sievershütten fault zone
type: Concept
created: 2021-07-23T08:59:08.125Z
creator: schmar
notation: DE-712
in scheme: Tectonic Boundary Objects in Europe
broader: eastern branch Glückstadt Graben

Northeastern rim of the North German Basin
definition: The NE rim of the North German Basin subdomain roughly traces the NE rim of the NGB. Several units with a similar genesis were grouped together to a ESE striking sub-domain. The subdomain is characterized by a roughly south-dipping basin-slope and north-facing platform areas. A mostly concordant bedding of Mesozoic age smoothly transitions into shallow angular unconformities towards north. The subdomain include the Grimmen Wall, Rügen Depression and the Mecklenburg Bay. In addition, the east of this domain is characterized by SE to ESE running mainly normal faults of the the Vorpommern fault system. From the Grimmen High to the Agricola Fault System in the north, which is the border to the Arkona High, the domain is marked by a Jurassic rim basin of the North German basin, which is crossed by several SE striking faults. The most prominent of this fault zones/ grabens are the Werre & Prerow fault zones (Ahlrich et al. 2020). Uplift and moderate deformation characterize the subdomain during the Upper Cretaceous (uplift of the basin margins in the eastern part of the North German Basin) and the Jurassic basin of this area is inverted to a turtle-like structure. Domain type: Deformed sedimentary overburden, Basement: Avalonia/Baltica.
scope note: We describe the Northeastern rim of the North German Basin as a tectonostratigraphic unit along the norteastern rim of the North German Basin whose boundaries are not well defined. The outline is mainly derived from partly fuzzy trends in the lithofacies and local structural trends. Even though the main structures of this region have been described (e. g. Katzung & Ehmke, 1993), no clear definition of the outline of this basin part has been made to date. The extent of this tectonostratigraphic unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalised for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future.
type: Concept
created: 2021-07-23T08:59:09.459Z
creator: schmar
notation: DE-945
narrower: Vorpommern Fault System-Arkona High - Grimmen High
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12153
references: https://data.geoscience.earth/ncl/geoera/ref/12180
references: https://data.geoscience.earth/ncl/geoera/ref/12237
references: https://data.geoscience.earth/ncl/geoera/ref/12238
references: https://data.geoscience.earth/ncl/geoera/ref/8052
broader: North German Basin - domain I: North German Plain & Central German North Sea

Vorpommern Fault System-Arkona High - Grimmen High
narrower: Reinberg fault zone
narrower: Samtens fault zone
narrower: Prerow fault
definition: The Vorpommeranian fault system - Grimmen Wall subdomain mainly shows SSE/SE striking faults between the Anklam fault in the S and the Bergen fault in the N. Most of the faults developed during the Triassic but also show partly Jurassic and Late Cretaceous activity.
scope note: We describe the Vorpommern fault system - Grimmen Wall as a tectonic sub-unit of the Northeastern rim region of the North German Basin. The outline is mainly derived from Mesozoic fault pattern (region with predominant SE/SSE striking fault zones). Even though the main structures of this region have been described (e. g. Krauss & Mayer, 2004), no clear definition of the outline of this basin part has been made to date. The extent of this tectonostratigraphic unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
alternative label: Vorpommern fault system - Grimmen Wall
notation: DE-1068
type: Concept
created: 2021-07-23T08:59:09.462Z
creator: schmar
narrower: Wiek fault
narrower: North Jasmund fault
narrower: Schaabe fault
narrower: Samtens fault
narrower: Wiek fault system
narrower: Caledonian deformation front large-scale fault system
narrower: Agricola-Svedala fault
narrower: Freest fault zone
in scheme: Tectonic Boundary Objects in Europe
narrower: Werre fault
narrower: Greifswald-Poseritz fault zone
narrower: Adler-Kamien fault
references: https://data.geoscience.earth/ncl/geoera/ref/12180
references: https://data.geoscience.earth/ncl/geoera/ref/12210
references: https://data.geoscience.earth/ncl/geoera/ref/12237
references: https://data.geoscience.earth/ncl/geoera/ref/12238
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/8033
broader: Northeastern rim of the North German Basin

Samtens fault
type: Concept
created: 2021-07-23T08:59:09.487Z
creator: schmar
notation: DE-9021
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12210
definition: The WNW-ESE running Samtens fault zone represents the northermost section of the supraregional Vorpommern fault system. The fault zone was formed during pre-Westfalian times and is characterized in the mesozoic overburden by an old-kimmerian, up to 6 km wide, alternating system of y-grabens.
broader: Vorpommern Fault System-Arkona High - Grimmen High

Wiek fault system
type: Concept
created: 2021-07-23T08:59:09.491Z
creator: schmar
notation: DE-9029
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12238
definition: The Wiek fault system defined by Seidel et al. (2018) represents a summary of the faults east of Rügen, crossing the Middle Rügen and Wolin blocks. The fault system consists of about 60 faults, flexures and other weakness zones. The fault system strikes from NW (Jasmund, Rügen) to SE until the Adler Kamien fault zone.
broader: Vorpommern Fault System-Arkona High - Grimmen High

Samtens fault zone
type: Concept
created: 2021-07-23T08:59:07.992Z
creator: schmar
notation: DE-596
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8033
definition: The 31 km long, up to 6 km wide WNW-ESE running Samtens fault zone is located within the subdomain Northeastern rim of North German Basin. The fault zone is characterized by alternating Y-grabens preserving Jurassic and locally Lower-Cretaceous sediments. The fault zone also represents the northern part of the overregional Vorpommeranian Fault system.
broader: Vorpommern Fault System-Arkona High - Grimmen High

Greifswald-Poseritz fault zone
type: Concept
created: 2021-07-23T08:59:07.996Z
creator: schmar
notation: DE-600
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8033
definition: The 34 km long, NNW-SSE oriented Greifswald-Poseritz fault zone is located in the NE rim of the North German Basin, and belongs to the eastern part of the Vorpommeranian fault system. The fault system is characterized by graben-like structures within the mesozoic overburden.
broader: Vorpommern Fault System-Arkona High - Grimmen High

Reinberg fault zone
type: Concept
created: 2021-07-23T08:59:07.999Z
creator: schmar
notation: DE-601
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8033
definition: The 44 km long, NW-SE oriented Reinberg fault zone is located in the NE rim of the North German Basin, and belongs to the western part of the Vorpommern fault system. The fault system is characterized by grabenlike structures within the Mesozoic overburden.
broader: Vorpommern Fault System-Arkona High - Grimmen High

Werre fault
type: Concept
created: 2021-07-23T08:59:08.002Z
creator: schmar
notation: DE-605
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12180
references: https://data.geoscience.earth/ncl/geoera/ref/12238
definition: 17 km long, NNW-SSE oriented fault within the subdomain of Vorpommeranian Fault System - Grimmen Wall, located at the NE rim of the North German Basin.
broader: Vorpommern Fault System-Arkona High - Grimmen High

Prerow fault
type: Concept
created: 2021-07-23T08:59:08.005Z
creator: schmar
notation: DE-606
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8033
definition: The 13 km long, W-E oriented Prerow fault is located at the NE rim of the North German basin and belongs to the Vorpommeranian fault system - Grimmen wall subdomain. Isolated remnants of Lower Cretaceous deposits (Wealden) with thicknesses inbetween 130 and 360 m occur.
broader: Vorpommern Fault System-Arkona High - Grimmen High

Caledonian deformation front large-scale fault system
type: Concept
created: 2021-07-23T08:59:09.495Z
creator: schmar
notation: DE-9058
in scheme: Tectonic Boundary Objects in Europe
definition: The Caledonian Deformation Front is characterized by a discordance, which represents the northernmost extension of the Caledonian accretionary wedge, located between over‐thrusting Ordovician sediments onto the southwestern margin of Baltica.
broader: Vorpommern Fault System-Arkona High - Grimmen High
broader: Møn-Arkona High
broader: Gryfice Block
broader: Kolobrzeg Block

Agricola-Svedala fault
type: Concept
created: 2021-07-23T08:59:09.499Z
creator: schmar
notation: DE-9059
in scheme: Tectonic Boundary Objects in Europe
notation: DE-9005
references: https://data.geoscience.earth/ncl/geoera/ref/12202
references: https://data.geoscience.earth/ncl/geoera/ref/12237
references: https://data.geoscience.earth/ncl/geoera/ref/12240
references: https://data.geoscience.earth/ncl/geoera/ref/12242
definition: The Agricola‐Svedala Fault is located close to the Danish offshore region and shows an almost N‐S strike direction and dips steeply towards the west. According to Seidel (2019) the Cretaceous succession is especially affected by normal flexure causing an offset of about 25 ms.
broader: Møn-Arkona High
broader: Vorpommern Fault System-Arkona High - Grimmen High

Freest fault zone
type: Concept
created: 2021-07-23T08:59:09.503Z
creator: schmar
notation: DE-9061
in scheme: Tectonic Boundary Objects in Europe
definition: NNW-SSE running fault zone within the Northeastern rim of the North German basin.
broader: Vorpommern Fault System-Arkona High - Grimmen High

Wiek fault
type: Concept
created: 2021-07-23T08:59:09.470Z
creator: schmar
notation: DE-9012
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12186
references: https://data.geoscience.earth/ncl/geoera/ref/12218
references: https://data.geoscience.earth/ncl/geoera/ref/12226
definition: The Wiek fault, located west of Rügen, is a prominent WNW-ESE running fault, which was formed during pre-Westfalian and reactivated in younger epochs. Fault throw are asssumed to be >3500 m, maximal values around 5 to 6 km. The fault is associated with a larger fault system, the Odense-Wiek fault system.
broader: Møn-Arkona High
broader: Vorpommern Fault System-Arkona High - Grimmen High

North Jasmund fault
type: Concept
created: 2021-07-23T08:59:09.475Z
creator: schmar
notation: DE-9013
notation: DE-9014
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12186
references: https://data.geoscience.earth/ncl/geoera/ref/12211
references: https://data.geoscience.earth/ncl/geoera/ref/12233
definition: The North Jasmund fault is a NW-SE running and southwest dipping, pre-Westfalian fault with throws of up to 3000 m. The fault is interpreted to be a part of the Wiek fault and the larger Odense-Wiek fault zone.
broader: Vorpommern Fault System-Arkona High - Grimmen High

Adler-Kamien fault
type: Concept
created: 2021-07-23T08:59:09.597Z
creator: schmar
notation: DE-9017
in scheme: Tectonic Boundary Objects in Europe
broader: Gryfice Block
broader: Vorpommern Fault System-Arkona High - Grimmen High
broader: Møn-Arkona High

Schaabe fault
type: Concept
created: 2021-07-23T08:59:09.479Z
creator: schmar
notation: DE-9015
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12218
references: https://data.geoscience.earth/ncl/geoera/ref/12226
definition: The NW-SE running Schaabe fault was formed during the pre-Westfalian, dips northeast and is a normal fault.
broader: Vorpommern Fault System-Arkona High - Grimmen High

Eastern rim of the North German Basin/ Szczecin-Kaliesz-East Brandenburg Swell
type: Concept
created: 2021-07-23T08:59:07.971Z
creator: schmar
notation: DE-944
narrower: Buckow fault
narrower: Möckow-Dargibell fault zone
narrower: Usedom fault zone
scope note: We describe the Eastern rim of the North German Basin/ Szczecin-Kaliesz-East Brandenburg Swell as a tectonostratigraphic unit along the western rim of the North German Basin, whose boundaries are not well defined. The outline is mainly derived from partly fuzzy trends in the lithofacies and local structural trends. Even though the main structures of this region have been described (e. g. Katzung & Ehmke, 1993), no clear definition of the outline of this basin part has been made to date. The extent of this tectonostratigraphic unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/8052
definition: The subdomain of the eastern margin of the North German Basin represents a NNW striking structural unit and describes a roughly west-dipping basin slope. Mostly concordant bedding or shallow angular unconformities are found. To the west, the structural area is roughly separated from the Mecklenburg-Brandenburg depression by NNE to NNW striking basement faults. The region is characterized by enhanced Late-Triassic to Cretaceous stratigraphic hiatus. The northern boundary is roughly formed by the Anklam fault. Within this subdomain the eastern part of the NGB merges to the east into the Szczecin-Kaliesz-East Brandenburg Swell (Ostbrandenburg Schwelle), which delimits the NGB from the eastwardly adjoining Wolsztyn High and Mid-Polish Trough. [Domain type: Sedimentary overburden, Basement: Avalonia/Rhenohercynian/Saxothuringian.]
broader: North German Basin - domain I: North German Plain & Central German North Sea

Usedom fault zone
type: Concept
created: 2021-07-23T08:59:07.981Z
creator: schmar
notation: DE-593
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8022
references: https://data.geoscience.earth/ncl/geoera/ref/8052
definition: The 35 km long and NNW-SSE running Usedom fault zone is located within the subdomain Eastern rim of North German basin. The fault zone is characterized by a graben with a major normal fault at the eastern flank.
broader: Eastern rim of the North German Basin/ Szczecin-Kaliesz-East Brandenburg Swell

Buckow fault
type: Concept
created: 2021-07-23T08:59:07.974Z
creator: schmar
notation: DE-574
notation: DE-575
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8022
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/8052
definition: The NNE-SSW striking Buckow fault is located southeast of the Mecklenburg-Brandenburg depression, and is often interpreted as the eastern part or eastern extension of the Potsdam fault. The Buckow fault crosses as reverse fault the Buckow salt pillows Buckow and Bad Freienwalde.
broader: Eastern rim of the North German Basin/ Szczecin-Kaliesz-East Brandenburg Swell
broader: East-Brandenburg - North Sudetes Depression

Möckow-Dargibell fault zone
type: Concept
created: 2021-07-23T08:59:07.978Z
creator: schmar
notation: DE-592
notation: DE-594
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12198
references: https://data.geoscience.earth/ncl/geoera/ref/8022
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The 50 km long, 5 km wide and NNW-SSE running Möckow-Dargibell fault zone is located within the subdomain Eastern rim of North German basin. The fault zone is characterized by a graben, with a major normal fault at the eastern flank and belongs to the Vorpommern Fault system.
broader: Eastern rim of the North German Basin/ Szczecin-Kaliesz-East Brandenburg Swell

Thrusted Central North German Basin sub-domains
type: Concept
created: 2021-07-23T08:59:07.802Z
creator: schmar
notation: DE-937
notation: DE-938
notation: DE-939
notation: DE-940
narrower: Altmark Fläming Depression
narrower: East-Brandenburg - North Sudetes Depression
narrower: Südoldenburg & Hoya Block
narrower: Rotenburg-Soltau-Eldingen Block
scope note: We describe the thrusted Central North German Basin sub-domains as a summary of separate tectonic units, which show great similarities in the type of deformation, their basin location and the orientation of faults and salt structures. The outline of the summarized units are predominantly defined both faults and fault systems. Areas of significant Upper Cretaceous contractional deformation of the Mesozoic overburden within the Central North German Basin were summarized to specific tectonic units. Even though the main structures of this regions have been described partly in detail (e. g. Baldschuhn et al., 2001), no clear definition of the outline of this basin part has been made to date. The extent of this tectonostratigraphic unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain border and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Based on a compilation of Baldschuhn et al. (1996, 1997), Röllig et al. (1990). Outline definition/ existing outlines based after fault and deformation pattern (Late Cretaceous deformationa) in the Mesozoic overburden; considering of strike-domain pattern and orientation of the salt structures. Designation is based on overview maps and assumed outcrop geometries in the case of Röllig et al. (1990). The structural subdomains are not bounded at all their boundaries by discrete faults, but also by outcrop patterns of stratigraphies. For References see also Tectonic boundaries in Germany.
definition: The subdomains of the thrusted Central North German basin are a summary of a total of four structural regions separated from each other, which in turn are subdivided by further blocks in the literature. However, these regions show great similarities in the type of deformation, their basin location, orientation of faults and salt structures. These structural domains fringe/adhere to the north of strongly inverted areas or areas uplifted during the Upper Cretaceous. However, these regions as a whole are assigned to the central area of the NGB in subsidence history & corresponding to facies and lithostratigraphy (central basin location/relatively submerged). The structural domains are characterized by a dominance of ESE to SE striking faults, often associated with salt structures elongated in the same direction in the Mesozoic overburden. Partially, areas are also assigned in former literature to the Pompeckj Block region. Among others, Müller et al. (2016) discussed the non-conforming subdivision and designation of the Pompeckj Block. Irrespective of the partly strong structuring of the Mesozoic overburden of these regions, the base Zechstein often shows only minor vertical offsets.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12160
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/12223
references: https://data.geoscience.earth/ncl/geoera/ref/12232
broader: North German Basin - domain I: North German Plain & Central German North Sea

Rotenburg-Soltau-Eldingen Block
narrower: Uelzen lineament
type: Concept
created: 2021-07-23T08:59:07.887Z
creator: schmar
notation: DE-940
narrower: Taaken fault
narrower: Volkwardingen fault
narrower: Süstedt-Bahnsen-Fassberg fault zone
narrower: Scheessel-Fallingbostel fault zone
narrower: Böstlingen-Unterlüß fault zone
narrower: Lüdingen fault
narrower: Wardböhmen fault
scope note: We describe the Rotenburg-Soltau-Eldingen Block as a seperate tectonic unit of the sub-domain thrusted Central North German Basin. The outline of this tectonic unit is predominantly defined by Mesozoic, esp. Late Cretacous structural pattern. Neighbouring areas of significant Upper Cretaceous contractional deformation of the Mesozoic overburden within the Central North German Basin were summarized to this specific tectonic unit. Even though the main structures of this regions have been described partly in detail, no clear definition of the outline of this basin part has been made to date. The extent of this tectonostratigraphic unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. New defined and summarized from Baldschuhn et al. (1996); especially from structural maps and profiles), Baldschuhn et al. (1997), as well as the structure of Base Zechstein. Definition of outline mainly oriented to Baldschuhn et al. (1997). Uncertainties: Different definitions in dependence to different interpretation of structural pattern in the overburden and basement. For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12159
references: https://data.geoscience.earth/ncl/geoera/ref/12160
definition: The subdomain of the Rotenburg-Soltau-Eldingen block is located in the area of moderate to minor Upper Cretaceous contraction north of the Allertal fault system. After Baldschuhn et al. (1997) this region is subdivided into a number of individual basement blocks (Rotenburg/Schneverdingen/Soltau/Munster/Schmarbeck/Bahnsen/Eldingen/Wesendorf). This pattern also coincides in large parts with the pattern of the Mesozoic overburden. The lithostratigraphic sequence of this region follows in large parts the pattern described as the Pompeckj Block. In the west the subdomain is bounded by the Emtinghausen-Krautsand lineament and to the east by the Braunschweig-Gifhorn fault zone. An important lineament in the north of the unit is formed by the Uelzen lineament. Domain type: Deformed sedimentary overburden, Basement: Avalonia/Rhenohercynian(?).
broader: Thrusted Central North German Basin sub-domains

Scheessel-Fallingbostel fault zone
type: Concept
created: 2021-07-23T08:59:07.899Z
creator: schmar
notation: DE-761
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12190
definition: The 42 km long, NNW-SSE running Scheesel-Fallingbostel fault zone is located in the central part of the Rotenburg-Soltau-Eldingen block and belongs to the thrusted part of the Central North German basin. In the northern part normal faults dominate the kinematics.
broader: Rotenburg-Soltau-Eldingen Block

Süstedt-Bahnsen-Fassberg fault zone
type: Concept
created: 2021-07-23T08:59:07.896Z
creator: schmar
notation: DE-755
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12190
definition: The 23 km long, WSW-ENE running Südstedt-Bahnsen-Fassberg fault zone is located in the central part of the Rotenburg-Soltau-Eldingen block and belongs to the thrusted part of the Central North German basin. The fault zone is characterzied by the associated salt structures Bahnsen and Niendorf II, the inversion structure Fassberg and the graben Bahnsen.
broader: Rotenburg-Soltau-Eldingen Block

Volkwardingen fault
type: Concept
created: 2021-07-23T08:59:07.893Z
creator: schmar
notation: DE-748
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12190
definition: The 62 km long, W-E running and S-dipping Volkwardingen basement fault is located at the northern rim of the Rotenburg-Soltau-Eldingen block and belongs to the thrusted part of the Central North German basin. With this fault the salt structures Scheessel, Stemmen, Otter-Todtshorn and Volkwardingen are associated.
broader: Rotenburg-Soltau-Eldingen Block

Taaken fault
type: Concept
created: 2021-07-23T08:59:07.890Z
creator: schmar
notation: DE-744
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12190
definition: The 37 km long, W-E running and S-dipping Taaken basement fault is located at the northern rim of the Rotenburg-Soltau-Eldingen block and belongs to the thrusted part of the Central North German basin. With this fault the salt structures Taaken, Scheessel and Ostervesede are associated.
broader: Rotenburg-Soltau-Eldingen Block

Wardböhmen fault
type: Concept
created: 2021-07-23T08:59:07.912Z
creator: schmar
notation: DE-874
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12190
definition: The 9 km long, WSW-ENE running Wardböhmen normal fault is located close to the SW-border of the Rotenburg-Soltau-Eldingen block and belongs to the thrusted part of the Central North German basin. Associated with this fault is the salt structure Wardböhmen (Frisch & Kockel 2004).
broader: Rotenburg-Soltau-Eldingen Block

Lüdingen fault
type: Concept
created: 2021-07-23T08:59:07.909Z
creator: schmar
notation: DE-873
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12190
definition: The 19 km long, NNE-SSW running Lüdingen normal fault is located at the SW-border of the Rotenburg-Soltau-Eldingen block and belongs to the thrusted part of the Central North German basin. In the southern part the fault is located within the Allertal fault system. Associated with this fault is the salt structure Lüdingen.
broader: Rotenburg-Soltau-Eldingen Block

Böstlingen-Unterlüß fault zone
type: Concept
created: 2021-07-23T08:59:07.902Z
creator: schmar
notation: DE-764
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12192
definition: The 62 km long, W-E running Böstlingen-Unterlüss fault zone is located in the southern part of the Rotenburg-Soltau-Eldingen block and belongs to the thrusted part of the Central North German basin. This fault zone is associated with inversion and salt structures and is predefined by basement faults, which show Lower Permian synsedimentary activity.
broader: Rotenburg-Soltau-Eldingen Block

East-Brandenburg - North Sudetes Depression
scope note: We describe the East-Brandenburg - North Sudetes Depression as a separate tectonic unit of the subdomain thrusted Central North German Basin. The outline of this tectonic unit is predominantly defined by distributional/erosional pattern and prominent faults. Neighbouring areas of significant Upper Cretaceous contractional deformation of the Mesozoic overburden within the Central North German Basin were summarized to this specific tectonic unit. Even though the main structures of this regions have been described partly in detail, no clear definition of the outline of this basin part has been made to date. The extent of this tectonostratigraphic unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: Voigt (2009), Röllig et al. (1990). Outline definition: The outline based on the outcrop of Upper Cretaceous sediments after Röllig et al. (1990) and encloses the major SE-striking structural features of the region. The NW boundary was drawn at the Rüdersdorfer Salzkisssen, although no clear boundary to northwest-adjacent basin parts is evident. The envelope includes basin areas with clear Upper Cretaceous overprint. Uncertainties: (a) boundary to the NW to the tectonostratigraphic domain Central North German Basin not unambiguous; (b) boundary to the structure of the Prignitz-Lausitz Wall not to be unambiguously fixed to structures - from there fixed by the outline of the Upper Cretaceous. Existing outlines: Depicted in Voigt (2009), among others. This outline presented here oriented on structures did not exist in this form so far. For References see also Tectonic boundaries in Germany.
type: Concept
created: 2021-07-23T08:59:07.846Z
creator: schmar
notation: DE-938
narrower: Rüdersdorf fault
narrower: Fürstenwalde-Gubener fault zone
narrower: Groß-Köris-Merzdorf fault system
narrower: Lausitz Escarpment
in scheme: Tectonic Boundary Objects in Europe
narrower: Buckow fault
references: https://data.geoscience.earth/ncl/geoera/ref/12232
references: https://data.geoscience.earth/ncl/geoera/ref/12244
definition: The East Brandenburg-North Sudetes depression subdomain is an Upper Cretaceous foreland basin located between the uplifts of the Lusatian-Riesengebirge anticlinal zone and the North Sudetes anticlinal zone. The structural domain is traversed by partly complex SE-striking inverted graben zones/fault zones. The best known of these is the Fürstenwalde-Guben fault zone. In general, it is an area of minor to moderate shortening during the Upper Cretaceous. Beutler & Stackebrandt (2012) subdivide the domain into the Mittenwald & Guben Block. [Domain type: Late Cretaceous sedimentary basin; Basement: Rhenohercynian/Saxothuringian]
broader: Thrusted Central North German Basin sub-domains

Fürstenwalde-Gubener fault zone
type: Concept
created: 2021-07-23T08:59:07.856Z
creator: schmar
notation: DE-576
notation: DE-578
notation: DE-585
notation: DE-894
notation: DE-896
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The Fürstenwalde-Guben fault zone is a NW-SE to NNW-SSE dipping wide fault zone in the East Brandenburg-North Sudetes depression within the thrusted Central North German basin. The fault zone is characterized by anticlines with horst-like and locally intrasalinar-tectonic structures.
broader: East-Brandenburg - North Sudetes Depression

Rüdersdorf fault
type: Concept
created: 2021-07-23T08:59:07.849Z
creator: schmar
notation: DE-562
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The Rüdersdorf fault is located in the East Brandenburg-North Sudetes depression within the thrusted Central North German basin, extends over 32 km, runs WSW-ENE and is associated with the Rüdersdorf salt pillow.
broader: East-Brandenburg - North Sudetes Depression

Altmark Fläming Depression
narrower: Salzwedel fault
narrower: Wittenberg fault
scope note: We describe the Altmark Fläming Depression as a seperate tectonic unit of the subdomain thrusted Central North German Basin. The outline of this tectonic unit is predominantly defined both by faults and fault systems. Neighbouring areas of significant Upper Cretaceous contractional deformation of the Mesozoic overburden within the Central North German Basin were summarized to this specific tectonic unit. Even though the main structures of this regions have been described partly in detail, no clear definition of the outline of this basin part has been made to date. The extent of this tectonostratigraphic unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Saxony-Anhalt provides and describes a partly more detailed and updated fault data set of Saxony-Anhalt within the framework of the HIKE project (DE-ST-0, DE-ST-1000). Outline definition based on outcrops of the Mesozoic at the base Tertiary esp. from Röllig et al. (1990) & Martiklos et al. (2001). Also referring to Baldschuhn et al. (1996). Uncertainties: a) diffuse transition to the Prignitz Wall and the northward following central less deformed basin parts b) overthrusted from the south - thus in detail overlapping of the outlined blocks c) slightly different boundary drawing depending on which outcrop at the base Cenozoic in the overburden is followed if not explicitly a fault is shown as boundary. In this case the outline of the Upper Cretaceous was followed. As a region in a lot of the literature designated among others Katzung & Ehmke (1993), but never discretely outlined until now.
type: Concept
created: 2021-07-23T08:59:07.806Z
creator: schmar
notation: DE-937
narrower: Apenburg-Wernstedt fault
narrower: Ahlum fault
narrower: Altmersleben-Demker zone
narrower: Genthin fault
narrower: Gardelegen fault
narrower: Liebenwalde fault
narrower: Rosenthal-Gülden-Braudel-Peckensen fault zone
definition: The subdomain of the Altmark-Fläming Depression represents the area north of the basement uplifts of Gardelegen & the Upper Cretaceous uplifted Halle-Wittenberg Block in the south and the inverted basin areas in the strike of the structural unit Prignitz - Lausitz - Riesengebirge Anticlinal Zone (in this area Prignitz wall). Bounded to the west by the NNE/N trending Brunswick-Gifhorn-Lüneburg fault system. Especially the western parts of the structural unit are influenced by movements along the Eichsfeld-Altmark sill (esp. in the Buntsandstein, Rotliegend, Keuper). The overburden is characterized by several SE-striking syncline-anticline structures caused by foreland thrusting of the Gardelegen thrust (e.g. Jähne & Kley, 2008). Thick synkinematic Upper Cretaceous is deposited in the synclines. The anticlinal structures coincide with salt structure lineaments. In contrast, the base Zechstein shows only minor offsets. Further REF: Jähne & Kley (2008), Benox et al. (1997), Otto (2003), Malz et al. (2020). Map Reference: Based on compilation of Baldschuhn et al. (1996) (overburden structures) and Martiklos et al. (2001), Röllig et al. (1990).[Domain type: Deformed sedimentary overburden; Basement: Avalonia]
in scheme: Tectonic Boundary Objects in Europe
narrower: Arendsee Deep fracture fault
narrower: Rockenthin fault
references: https://data.geoscience.earth/ncl/geoera/ref/12208
references: https://data.geoscience.earth/ncl/geoera/ref/12223
references: https://data.geoscience.earth/ncl/geoera/ref/12232
references: https://data.geoscience.earth/ncl/geoera/ref/8071
references: https://data.geoscience.earth/ncl/geoera/ref/7994
broader: Thrusted Central North German Basin sub-domains

Altmersleben-Demker zone
type: Concept
created: 2021-07-23T08:59:07.827Z
creator: schmar
notation: DE-534
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The Altermersleben-Demker structural zone is located within the Altmark-Fläming depression of the thrusted Central North German basin, extends over a length of 29 km and is oriented NW-SE.
broader: Altmark Fläming Depression

Ahlum fault
type: Concept
created: 2021-07-23T08:59:07.824Z
creator: schmar
notation: DE-533
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The 11 km long, WNW-ESE running Ahlum fault is a asymmetric and compressive overprinted and salt core containing fault.
broader: Altmark Fläming Depression

Apenburg-Wernstedt fault
type: Concept
created: 2021-07-23T08:59:07.812Z
creator: schmar
notation: DE-511
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/7994
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The NW-SE running Apenburg-Wernstedt fault is located within the centre of the Altmark-Fläming depression and extends over 37 km.
broader: Altmark Fläming Depression

Rosenthal-Gülden-Braudel-Peckensen fault zone
alternative label: Rosenthal-Gülden-Peckensen fault zone
definition: The 23 km long, N-S running fault system is located at the eastern rim of the eastern part of the Lower Saxony Basin, and runs almost parallel to the Braunschweig-Gifhorn fault system.
type: Concept
created: 2021-07-23T08:59:07.843Z
creator: schmar
notation: DE-778
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The N-S running Rosenthal-Gülden-Braudel-Peckensen fault zone extends over 103 km, representing at the southern tip the border between the Gardelegen-Rosslau uplift and the Braunschweig-Gifhorn-Lüneburg fault system, in the middle section representing the border between the Braunschweig-Gifhorn-Lüneburg fault system and the Altmark-Fläming depression and at the northern part the border between the Braunschweig-Gifhorn-Lüneburg fault system and the Central North German basin.
broader: Altmark Fläming Depression
broader: Dipping Harz structure & Sack depression

Liebenwalde fault
type: Concept
created: 2021-07-23T08:59:07.840Z
creator: schmar
notation: DE-541
in scheme: Tectonic Boundary Objects in Europe
definition: The 7 km long, NNE-SSW running Liebenwalde fault represents the southwestern section of the Liebenwalde-Torgelow fault. The Liebenwalde fault is located within the SE area of the Altmark-Fläming depression of the thrusted Central North German basin.
broader: Altmark Fläming Depression

Gardelegen fault
type: Concept
created: 2021-07-23T08:59:07.833Z
creator: schmar
notation: DE-538
notation: DE-822
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The 153 km long, WNW-ESE running Gardelegen fault is located at the southern boundary of the Altmark Fläming depression within the thrusted part of the Central North German basin. The fault represents a listric, SW-dipping steep reverse fault that was formed in the course of Upper Cretaceous inversion. Due to seismic data, the fault reaches a depth of up to 25 km.
broader: Altmark Fläming Depression

Genthin fault
type: Concept
created: 2021-07-23T08:59:07.830Z
creator: schmar
notation: DE-537
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The 90 km long, WNW-ESE running Genthin fault represents a listric, SW-dipping reverse fault, that was reactivated in the course of Upper Cretaceous inversion.
broader: Altmark Fläming Depression

Südoldenburg & Hoya Block
type: Concept
created: 2021-07-23T08:59:07.867Z
creator: schmar
notation: DE-939
narrower: Jemgum fault
scope note: We describe the Südoldenburg & Hoya Block as a seperate tectonic unit of the subdomain thrusted Central North German Basin. The outline of this tectonic unit is predominantly defined by Mesozoic, esp. Late Cretacous structural pattern. Neighbouring areas of significant Upper Cretaceous contractional deformation of the Mesozoic overburden within the Central North German Basin were summarized to this specific tectonic unit. Even though the main structures of this regions have been described partly in detail, no clear definition of the outline of this basin part has been made to date. The extent of this tectonostratigraphic unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map reference: Based on a compilation by Baldschuhn et al. (1996, 1997). Outline of structure is based on Mesozoic structures as defined by Baldschuhn et al. (1996). Uncertainties: (a) diffuse transition in the area of the Hoya Block towards the Lower Saxony Basin and its sub-units; (b) partly overlain in the south by the inverted LSB - thus actually an overlap of structural areas; (c) slightly different boundary drawing depending on designation according to basement or overburden structure; (d) whether areas further west were also shortened by the Upper Cretaceous and show similar deformation is difficult to prove at present. If so then the boundary could also coincide with the Ems lineament. Currently this structural area borders the unit East Frisia - Ems Estuary Region. For References see also Tectonic boundaries in Germany.
narrower: Vegesack-Lilienthal fault zone
narrower: Leer-Bremen fault zone
in scheme: Tectonic Boundary Objects in Europe
narrower: Berdum-Jaderberg-Sagermeer fault
references: https://data.geoscience.earth/ncl/geoera/ref/12159
references: https://data.geoscience.earth/ncl/geoera/ref/12161
references: https://data.geoscience.earth/ncl/geoera/ref/12158
definition: The subdomain of the Südoldenburg & Hoya block is located north of the Lower Saxony Basin. In the south it is bounded by the partially overlapping structural features Rheder Moor - Oythe & Goldenstedt - Blenhorst and in the north by the less constricted Leer-Bremen lineament. To the north of the LSB, an Upper Cretaceous foreland basin has developed on the Ostfriesland Block. To the east, the subdomain is separated from the NE Lower Saxony Basin by the Emtinghausen-Krautsand fault zone. To the west, the boundary roughly coincides with the overturning Jemgum structure and associated Jemgum fault. Domain type: Deformed sedimentary overburden, Basement: Avalonia.
broader: Thrusted Central North German Basin sub-domains

Leer-Bremen fault zone
type: Concept
created: 2021-07-23T08:59:07.880Z
creator: schmar
notation: DE-750
notation: DE-751
notation: DE-903
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12190
definition: The 130 km long, NW-SE/WNW-ESE running Leer-Bremen fault zone is located in the Südoldenburg-Hoya block and belongs to the thrusted part of the Central North German basin, to which several inversion structures are associated.
broader: Südoldenburg & Hoya Block

Vegesack-Lilienthal fault zone
type: Concept
created: 2021-07-23T08:59:07.877Z
creator: schmar
notation: DE-749
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12190
definition: The 55 km long, WNW-ESE running Vegesack-Lilienthal fault zone is located in the Südoldenburg-Hoya block and belongs to the thrusted part of the Central North German basin. Associated with this fault zone are the inversion structure Bremen, salt structure Lilienthal, inversion structure Wührden, salt structure Lesum and inversion structure Vegesack.
broader: Südoldenburg & Hoya Block

Jemgum fault
type: Concept
created: 2021-07-23T08:59:07.870Z
creator: schmar
notation: DE-745
in scheme: Tectonic Boundary Objects in Europe
definition: The 34 km long, NNE-SSW running Jemgum fault is located in the Südoldenburg-Hoya block and belongs to the thrusted part of the Central North German basin.
broader: Südoldenburg & Hoya Block

Braunschweig-Gifhorn-Lüneburg fault system
type: Concept
created: 2021-07-23T08:59:07.799Z
creator: schmar
notation: DE-931
in scheme: Tectonic Boundary Objects in Europe
definition: The Lutter-Salzgitter fault zone is a 14 km long fault zone in the southern extension of the Braunschweig-Gifhorn-Lüneburg fault system and with a NNE-strike. This fault zone crosses the Subhercynian Cretaceous Basin and transfers offsets to the adjacent Harz fault system to the south.
broader: North German Basin - domain I: North German Plain & Central German North Sea

Lower Saxony Basin
type: Concept
created: 2021-07-23T08:59:07.517Z
creator: schmar
notation: DE-917
narrower: Central Lower Saxony Basin
narrower: NE Lower Saxony Basin
narrower: SE Lower Saxony Basin
definition: The Lower Saxony Basin is located in the southwest of the North German basin (NGB), which is itself a segment of the NGB. Including its uplifted parts the LSB is approx. 250 km long in a NW-SE direction and from 60 km to more than 100 km wide. Its structural and sedimentary evolution diverges from the rest of the NGB in Late Jurassic to Early Cretaceous time. Besides increased subsidence of the entire LSB, several mostly ESE to SE trending grabens and half-grabens evolved and are connected by major fault systems which enclose most of the basin (e.g. Allertal Lineament). The central part of the LSB (Central Lower Saxony Basin subdomain) shows little Late Jurassic to Early Cretaceous faulting. Late Cretaceous contraction of the LSB takes different forms in the Mesozoic basin fill, but NNE/NE dip-slip contraction is suggested by the majority of structures such as: a) A broad anticlinal inversion of the entire basin, with maximum uplift over the former centre of the LSB, b) Major reactivation and inversion of grabens and faults along the borders of the LSB. Often entire grabens are upwarped while normal offsets on faults are preserved, c) Broad regional uplift in the hanging wall of the Osning Thrust, d) Bulging of formerly flat-lying Upper Jurassic or Lower Cretaceous sub-basin fills, e) Compressional overprinting of different forms of salt diapirs, f) Formation of compressional salt-anticlines, g) Subordinate formation of new thrust and reverse faults, h) Indications for strike-slip faulting and strain partitioning along unfavourably oriented NNE striking lineaments (e.g. Gifhorn-Braunschweig fault zone) but no clear evidence for NE/NNE dip-slip contraction. Up to 7 kilometres of Triassic to Upper Cretaceous sedimentary strata may have been eroded along the southern rim of the Central Lower Saxony subdomain. The uplift is related to the reactivation and inversion of the southern border fault system (Osning Lineament) of the LSB, but the strong erosion of its hanging-w…
narrower: Steinhuder Meer-Stemmer Berg-Limberg fault system
narrower: Western Lower Saxony Basin
narrower: Osning-Wiehengebirge thrust unit/ uplift
narrower: Dipping Harz structure & Sack depression
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12157
references: https://data.geoscience.earth/ncl/geoera/ref/12161
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/11969
references: https://data.geoscience.earth/ncl/geoera/ref/12173
references: https://data.geoscience.earth/ncl/geoera/ref/12174
references: https://data.geoscience.earth/ncl/geoera/ref/12204
broader: North German Basin - domain I: North German Plain & Central German North Sea

NE Lower Saxony Basin
type: Concept
created: 2021-07-23T08:59:07.584Z
creator: schmar
notation: DE-1006
narrower: Linsburg fault
narrower: Marienburg-Wienhausen fault zone
narrower: Mölme-Stederdorf-Plockhorst fault zone
narrower: Allertal fault system
in scheme: Tectonic Boundary Objects in Europe
narrower: Lauenau-Bad Münder fault
references: https://data.geoscience.earth/ncl/geoera/ref/12157
references: https://data.geoscience.earth/ncl/geoera/ref/12161
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/11969
references: https://data.geoscience.earth/ncl/geoera/ref/12173
references: https://data.geoscience.earth/ncl/geoera/ref/12174
references: https://data.geoscience.earth/ncl/geoera/ref/12204
definition: NE-part of the Lower Saxony Basin. This part of the basin is bounded NE by the Allertal fault system, east by the Braunschweig-Gifhorn fault system, SE by the Steinhuder Meer - Stemmer Berg - Limberg fault system. As the Central Lower Saxony basin towards SW, this basin part shows also a broad anticlinal basin inversion but in a more moderate style. [Domain type: deformed sedimentary overburden, Basement: Rhenohercynian/Avalonia.]
scope note: We describe the Northeastern Lower Saxony Basin as a tectonostratigraphic unit, whose boundaries are defined both by faults and fault systems as well as partly fuzzy trends in the lithofacies. Even though the main structures of this region have been described in detail (e. g. Baldschuhn et al., 2001), no clear definition of the outline of this basin part has been made to date. The extent of this tectonostratigraphic unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
broader: Lower Saxony Basin

Marienburg-Wienhausen fault zone
type: Concept
created: 2021-07-23T08:59:07.594Z
creator: schmar
notation: DE-826
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12156
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 57 km long, NE-SW running Marienburg-Wienhausen fault zone is located within the NE-Lower Saxony Basin at the northern tip within the Allertal fault system. Along this basement fault zone, salt diapirs and inverted grabens are associated in the overburden (Baldschuhn & Kockel 1998).
broader: NE Lower Saxony Basin

Linsburg fault
type: Concept
created: 2021-07-23T08:59:07.590Z
creator: schmar
notation: DE-786
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
broader: NE Lower Saxony Basin

Lauenau-Bad Münder fault
type: Concept
created: 2021-07-23T08:59:07.634Z
creator: schmar
notation: DE-827
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12156
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The Lauenau-Bad Münder fault is a 33 km long, WNW-ESE striking normal fault in the eastern extension to the Petershagen fault (DE-817). Associated with this fault is a halfgraben at Bad Münder.
broader: NE Lower Saxony Basin
broader: SE Lower Saxony Basin

Allertal fault system
type: Concept
created: 2021-07-23T08:59:07.605Z
creator: schmar
notation: DE-941
narrower: Verden-Wietze fault zone
narrower: Bassen-Celle fault zone
narrower: Wietze graben fault system
in scheme: Tectonic Boundary Objects in Europe
narrower: Martfeld-Hope fault zone
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/12190
definition: The Lower Saxony Basin is bounded to northeast by a complex lineament consisting of shortened diapirs and inverted grabens (Allertal Lineament). It is a several kilometer broad and an intensely structured zone, which can be subdivided into several inverted and shortened structures, with mostly ESE/SE strike in the Mesozoic overburden. However, the base Zechstein shows only little relief. The geometry of the salt structures along the lineament is highly variable with occurrence of lateral salt intrusions into Mesozoic salt formations and salt-filled fault zones. [Domain type: strongly deformed overburden, Basement: Avalonia/Rhenohercynian(?)]
scope note: We describe the Allertal fault system as a sub-region of the Northeastern Lower Saxony Basin which is highly dissected by several major sub-parallel fault zones with a mostly similar development history. Even though the main structures of this region have been described in detail (e.g. Baldschuhn et al., 2001), no clear definition of the outline of this strongly deformed block has been made to date. The extent of this faulted block was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
broader: NE Lower Saxony Basin

Wietze graben fault system
type: Concept
created: 2021-07-23T08:59:07.621Z
creator: schmar
notation: DE-875
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12156
references: https://data.geoscience.earth/ncl/geoera/ref/12173
references: https://data.geoscience.earth/ncl/geoera/ref/12190
definition: The 8 km long, NE-SE running Wietze graben fault system is located within the Allertal fault system. The graben is characterized by two SE-dipping normal faults and an antithetic SE-dipping normal fault causing a Y-graben, reaching up to the Lower Cretacous (Barreme). Movements along the SE-dipping major faults are documented for Keuper and Lower/Midlle Jurassic times, inversion during Coniac-Santon results in the uplift of of the southeastern flank.
broader: Allertal fault system

Bassen-Celle fault zone
type: Concept
created: 2021-07-23T08:59:07.617Z
creator: schmar
notation: DE-790
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12156
references: https://data.geoscience.earth/ncl/geoera/ref/12173
references: https://data.geoscience.earth/ncl/geoera/ref/12190
definition: The Bassen-Celle fault zone extends over 121 km length and belongs genetically to the Allertal fault zone. As main structural elements of the Bassen-Celle fault zone graben in the basement and horsts are documented for Buntsandstein times. Several times active since Lower Bunter times, this fault zone represents as normal fault the northern rim of the Lower Saxony basin since the Middle Jurassic, especially within the Upper Jurassic and Lower Cretaceous. This structure was compressively overprinted and partly inverted during the Upper Cretaceous.
broader: Allertal fault system

Martfeld-Hope fault zone
type: Concept
created: 2021-07-23T08:59:07.613Z
creator: schmar
notation: DE-785
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
references: https://data.geoscience.earth/ncl/geoera/ref/12190
definition: The 60 km long, WNW-ESE oriented Martfeld-Hope fault zone is located at the southwestern border of the Allertal fault system. This structure was compressively overprinted and partly inverted during the Upper Cretaceous.
broader: Allertal fault system

Verden-Wietze fault zone
type: Concept
created: 2021-07-23T08:59:07.609Z
creator: schmar
notation: DE-766
notation: DE-876
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/12173
references: https://data.geoscience.earth/ncl/geoera/ref/12190
definition: The NW-SE running Verden-Wietze fault zone is located within the central part of the Alltertal fault system, is 78 km long and since the Triassic was (re)activated several times, sometimes as NE-normal fault, sometimes as SW-normal fault. Subsequently, this structure was strongly compressively overprinted during the Upper Cretaceous.
broader: Allertal fault system

Mölme-Stederdorf-Plockhorst fault zone
type: Concept
created: 2021-07-23T08:59:07.601Z
creator: schmar
notation: DE-828
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12156
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: This 40 km long, NNE-SSW running fault zone is associated with two graben structures, the Stederdorf graben and the Plockhorst graben as well as two salt structures. The fault zone is located in the eastern part of the Lower Saxony Basin and separates the Hildesheim Block in a western and eastern part.
broader: NE Lower Saxony Basin

SE Lower Saxony Basin
type: Concept
created: 2021-07-23T08:59:07.626Z
creator: schmar
notation: DE-1007
narrower: Lauenau-Bad Münder fault
narrower: Hameln-Elfas-Salzderhelden fault system
narrower: Falkenhagen Graben
narrower: Brünninghausen-Leinetal fault zone
narrower: Lübbecke fault
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12157
references: https://data.geoscience.earth/ncl/geoera/ref/12161
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/11969
references: https://data.geoscience.earth/ncl/geoera/ref/12173
references: https://data.geoscience.earth/ncl/geoera/ref/12174
references: https://data.geoscience.earth/ncl/geoera/ref/12204
definition: This structural domain is a less deformed and less inverted basin part of the Lower Saxony Basin southwest of the Steinhuder Meer - Stemmer Berg - Limberg fault system. [Main Strike: ESE/SE, Domain type: Sedimentary overburden, Basement: Rhenohercynian.]
scope note: We describe the Southeastern Lower Saxony Basin as a tectonostratigraphic unit, whose boundaries are defined both by faults and fault systems as well as partly fuzzy trends in the lithofacies. Even though the main structures of this region have been described in detail (e. g. Baldschuhn et al., 2001), no clear definition of the outline of this basin part has been made to date. The extent of this tectonostratigraphic unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
broader: Lower Saxony Basin

Lübbecke fault
type: Concept
created: 2021-07-23T08:59:07.648Z
creator: schmar
notation: DE-813
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The Lübbecke fault has a length of 20 km, runs from northeast to southwest and connects the Petershagen fault with the Wiehengebirgs fault.
broader: SE Lower Saxony Basin
broader: Central Lower Saxony Basin

Brünninghausen-Leinetal fault zone
type: Concept
created: 2021-07-23T08:59:07.645Z
creator: schmar
notation: DE-853
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
broader: SE Lower Saxony Basin

Hameln-Elfas-Salzderhelden fault system
type: Concept
created: 2021-07-23T08:59:07.638Z
creator: schmar
notation: DE-860
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12156
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The NW-SE oriented Hameln-Elfas-Salzderhelden fault zone represents one segment of the southern border of the Lower Saxony Basin east of the Weser river. This fault zone separates the Solling block in NE from the Hils block. Most important element of this fault zone is the Elfas thrust, active in the Upper Cretaceous.
broader: SE Lower Saxony Basin

Osning-Wiehengebirge thrust unit/ uplift
type: Concept
created: 2021-07-23T08:59:07.705Z
creator: schmar
notation: DE-918
narrower: Wiehengebirge fault zone
narrower: Wiehengebirgs-Wesergebirgs fault zone
narrower: Osning fault system
narrower: Bad Meinberg-Egge fault zone
narrower: Neukirchen fault
narrower: Suttrup-Schapen fault
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12157
references: https://data.geoscience.earth/ncl/geoera/ref/12161
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/11969
references: https://data.geoscience.earth/ncl/geoera/ref/12173
references: https://data.geoscience.earth/ncl/geoera/ref/12174
references: https://data.geoscience.earth/ncl/geoera/ref/12204
definition: Uplifted part of the Southern Lower Saxony Basin in the hanging wall of the north east dipping Osning fault. The inversion of the Lower Saxony Basin reaches up to 7 km. The Osning thrust borders the domain in the south to the Münsterland Basin, which does not belong to the North German Basin. [Domain type: Basement uplifts under coverage, Basement: Rhenohercynian/Avalonia]
scope note: We describe the Osning-Wiehengebirge thrust unit/ uplift as an uplifted strongly faulted sub-unit of the western Lower Saxony Basin in the west of the Ems Lineament. Even though the main structures of this faulted region have been described in detail (e.g. Baldschuhn & Kockel, 1999, Baldschuhn et al., 2001), no clear definition of the outline of this strongly deformed block has been made to date. The extent of this faulted block was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
broader: Lower Saxony Basin

Wiehengebirgs-Wesergebirgs fault zone
type: Concept
created: 2021-07-23T08:59:07.712Z
creator: schmar
notation: DE-823
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12157
definition: The 42 km long Wiehengebirge-Weser fault system is part of a wide partly broken flexure along the northern border of the Osning Wiehengebirge thrust unit of the Lower Saxony Basin. This fault system also is associated to the Wiehengebirgs fault system further west (DE-814).
broader: Osning-Wiehengebirge thrust unit/ uplift

Wiehengebirge fault zone
type: Concept
created: 2021-07-23T08:59:07.708Z
creator: schmar
notation: DE-814
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12157
definition: The 35 km long Wiehengebirge fault system is part of a wide partly broken flexure along the northern border of the Osning Wiehengebirge thrust unit of the Lower Saxony Basin. This fault system also is associated to the Wiehengebirgs-Wesergebirgs fault system (DE-823). This flexure merges into the Lübbecke and Neuenkirchen fault zones and is presumably the result of a blind thrust zone.
broader: Osning-Wiehengebirge thrust unit/ uplift

Neukirchen fault
type: Concept
created: 2021-07-23T08:59:07.566Z
creator: schmar
notation: DE-802
definition: The Neuenkirch fault is a 39 km long, NW-SE running reverse fault partly belonging to Osning Wiehengebirge thrust unit of the Lower Saxony Basin and partly to the North Westphalia Lippe subfault system, and borders the Neuenkirchen Block.
alternative label: Neuenkirchen fault
in scheme: Tectonic Boundary Objects in Europe
broader: Osning-Wiehengebirge thrust unit/ uplift
broader: Central Lower Saxony Basin

Suttrup-Schapen fault
type: Concept
created: 2021-07-23T08:59:07.725Z
creator: schmar
notation: DE-808
in scheme: Tectonic Boundary Objects in Europe
definition: The NNW-SSE running Suttrup-Schapen fault is located in Osning Wiehengebirge thrust unit of the Lower Saxony Basin east of the Ems lineament, and is 32 km long.
broader: Osning-Wiehengebirge thrust unit/ uplift

Bad Meinberg-Egge fault zone
type: Concept
created: 2021-07-23T08:59:07.718Z
creator: schmar
notation: DE-847
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12157
definition: The N-S running Bad Meinberg-Egge fault zone is a complex fault zone of 65 km length, that separates the North Westfalia subfault system and the Westfalien bight subdomain in the west to the Pyrmont and Solling Block in the East. Eastern border of the Osning Wiehengebirge thrust unit. During Late Cretaceous transpressiv/ dextral movement.
broader: Osning-Wiehengebirge thrust unit/ uplift

Osning fault system
type: Concept
created: 2021-07-23T08:59:07.715Z
creator: schmar
notation: DE-831
notation: DE-854
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12157
definition: Prominent fault system located at the southern rim of the Lower saxony Basin, creates locally as much as 7 km vertical offset. Due to structural inversion during the Upper Cretaceous and associated deep erosion, these high vertical offsets are not obvious in the today’s geological maps. WNW-ESE running faults of a length of 43 and 53 km respectively.
broader: Osning-Wiehengebirge thrust unit/ uplift

Western Lower Saxony Basin
type: Concept
created: 2021-07-23T08:59:07.656Z
creator: schmar
notation: DE-919
narrower: Ratzel fault
narrower: Laar-Völzel fault
narrower: Neuringe-Osterbrock fault
narrower: Esche-Laar fault
narrower: Emelichheim-Schoonebeck fault
narrower: Gronau-Waldhügel-Nordhorn thrust unit/ uplift
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12157
references: https://data.geoscience.earth/ncl/geoera/ref/12161
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/11969
references: https://data.geoscience.earth/ncl/geoera/ref/12173
references: https://data.geoscience.earth/ncl/geoera/ref/12174
references: https://data.geoscience.earth/ncl/geoera/ref/12204
definition: Basin parts of the LSB west of the Ems-Linemaent. [Domain type: deformed overburden, Basement: Avalonia]
scope note: We describe the western Lower Saxony Basin as a tectonostratigraphic unit, whose boundaries are defined both by faults and fault systems as well as partly fuzzy trends in the lithofacies. Even though the main structures of this region have been described in detail (e.g. Baldschuhn & Kockel, 1999, Baldschuhn et al., 2001), no clear definition of the outline of this basin part has been made to date. The extent of this tectonostratigraphic unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
broader: Lower Saxony Basin

Neuringe-Osterbrock fault
type: Concept
created: 2021-07-23T08:59:07.669Z
creator: schmar
notation: DE-787
definition: The Schale fault is an 18 km long, NNW-SSE running reverse fault in the western part of the Lower Saxony Basin.
alternative label: Neuringe Osterbrock fault
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
broader: Dipping Harz structure & Sack depression
broader: Western Lower Saxony Basin

Laar-Völzel fault
type: Concept
created: 2021-07-23T08:59:07.665Z
creator: schmar
notation: DE-880
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
broader: Western Lower Saxony Basin

Ratzel fault
type: Concept
created: 2021-07-23T08:59:07.660Z
creator: schmar
notation: DE-879
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
broader: Western Lower Saxony Basin

Gronau-Waldhügel-Nordhorn thrust unit/ uplift
type: Concept
created: 2021-07-23T08:59:07.683Z
creator: schmar
notation: DE-1061
narrower: Schuttorf graben fault system
narrower: Gronau-Waldhügel fault zone
narrower: Reutum fault
narrower: Balderhaar fault
narrower: Neuenhaus fault
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12157
references: https://data.geoscience.earth/ncl/geoera/ref/12161
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/11969
references: https://data.geoscience.earth/ncl/geoera/ref/12173
references: https://data.geoscience.earth/ncl/geoera/ref/12174
references: https://data.geoscience.earth/ncl/geoera/ref/12204
definition: During the Late Cretacous strongly uplifted marginal area of the Western Lower Saxony Basin similar to Osning Wiehengebirge thrust unit. The most prominent structures are the inverted Gronau - Waldhügel fault zone/graben and the Nordhorn fault.
scope note: We describe the Gronau-Waldhügel-Nordhorn thrust unit/ uplift as an uplifted strongly faulted sub-unit of the western Lower Saxony Basin in the west of the Ems Lineament. Even though the main structures of this faulted region have been described in detail (e.g. Baldschuhn & Kockel, 1999, Baldschuhn et al., 2001), no clear definition of the outline of this strongly deformed block has been made to date. The extent of this faulted block was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
broader: Western Lower Saxony Basin

Neuenhaus fault
type: Concept
created: 2021-07-23T08:59:07.702Z
creator: schmar
notation: DE-793
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
broader: Gronau-Waldhügel-Nordhorn thrust unit/ uplift

Balderhaar fault
type: Concept
created: 2021-07-23T08:59:07.698Z
creator: schmar
notation: DE-807
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The Balderhaar fault is located within the Balderhaar Block, is 19 km long and oriented NW-SE.
broader: Gronau-Waldhügel-Nordhorn thrust unit/ uplift

Reutum fault
type: Concept
created: 2021-07-23T08:59:07.695Z
creator: schmar
notation: DE-881
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
broader: Gronau-Waldhügel-Nordhorn thrust unit/ uplift

Gronau-Waldhügel fault zone
type: Concept
created: 2021-07-23T08:59:07.691Z
creator: schmar
notation: DE-824
alternative label: Gronau Waldhügel fault zone
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12157
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The 44 km long, W-E running Gronau-Waldhügel fault zone represents the western extension of the Osning fault system. The fault zone borders the SSW-rim of the Lower Saxony Basin against the Westfalian Bight.
broader: Dipping Harz structure & Sack depression
broader: Gronau-Waldhügel-Nordhorn thrust unit/ uplift

Schuttorf graben fault system
type: Concept
created: 2021-07-23T08:59:07.687Z
creator: schmar
notation: DE-815
notation: DE-821
notation: DE-318
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The Schuttorf fault system is a N-S /NNW-SSE running graben system, is located in southern extension of the Ems Graben and belongs to the Schuttorf Block. It extends from 17 (DE-815) to 29 km (DE-821) respectively.
broader: Gronau-Waldhügel-Nordhorn thrust unit/ uplift

Emelichheim-Schoonebeck fault
type: Concept
created: 2021-07-23T08:59:07.680Z
creator: schmar
notation: DE-878
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
broader: Western Lower Saxony Basin

Esche-Laar fault
type: Concept
created: 2021-07-23T08:59:07.677Z
creator: schmar
notation: DE-882
notation: DE-870
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The Esche-Laar fault is 14 km long and runs NNW-SSE within the Western part of the Lower Saxony Basin.
broader: Western Lower Saxony Basin

Steinhuder Meer-Stemmer Berg-Limberg fault system
type: Concept
created: 2021-07-23T08:59:07.653Z
creator: schmar
notation: DE-1008
scope note: We describe the Steinhuder Meer-Stemmer Berg-Limberg fault system as a prominent narrow fault system which separates the Northeastern Lower Saxony Basin from the Central Lower Saxony Basin and the Southeastern Lower Saxony Basin. Even though the main structures of this faulted region have been described in detail (e.g. Baldschuhn et al., 2001), no clear definition of the outline of this strongly deformed block has been made to date. The extent of this faulted block was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12161
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/11969
references: https://data.geoscience.earth/ncl/geoera/ref/12173
references: https://data.geoscience.earth/ncl/geoera/ref/12174
references: https://data.geoscience.earth/ncl/geoera/ref/12204
definition: The NNE-SSW running, 56 km long Steinuder Meer-Stemmer Berg-Limberg fault system is located at the border between the Central and Eastern part of the Lower Saxony Basin. [Domain type: Strongly deformed sedimentary overburden, inverted structure (Late Cretaceous), partly prominent thrusts Basement: Rhenohercynian/Avalonia.]
broader: Lower Saxony Basin

Dipping Harz structure & Sack depression
type: Concept
created: 2021-07-23T08:59:07.728Z
creator: schmar
notation: DE-978
narrower: Ems graben fault system
narrower: Ems fault system
narrower: Southern Ems fault system
narrower: Rühle fault
narrower: Braunschweig-Gifhorn fault zone
narrower: Bechtsbüttel-Vordorf fault zone
narrower: Broidstedt-Wittingen fault zone
narrower: Flachstöckheim-Immendorf fault zone
narrower: Weddingen-Nettgau fault zone
narrower: Horndorf Rosche Thondorf fault zone
narrower: Waddekath Bonese fault zone
narrower: Lutter-Salzgitter fault zone
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12161
references: https://data.geoscience.earth/ncl/geoera/ref/12158
narrower: Gronau-Waldhügel fault zone
narrower: Neuringe-Osterbrock fault
narrower: Rosenthal-Gülden-Braudel-Peckensen fault zone
definition: Dipping of the Harz anticline below thick Mesozoic overburden. The Mesozoic overburden is characterized by thrusts, which borders synclines with Jurassic to Cretaceous outcrops. It is a marginal part of the Lower Saxon Basin but strongly influenced by NNE striking elements aligned along the Eichsfeld-Altmark swell. [Outcrop age: Triassic, Cretaceous; Domain type: Basement uplifts under coverage, Basement: Rhenohercynian.]
scope note: We describe the dipping Harz structure & the Sack depression as a tectonic sub-unit of the Lower Saxony Basin whose boundaries are defined both by faults and fault systems as well as by the structure of the Pre-Zechstein. Even though the main structures of this region have been described in detail (e. g. Baldschuhn et al., 2001), no clear definition of the outline of this basin part has been made to date. The extent of this tectonic unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
broader: Lower Saxony Basin

Waddekath Bonese fault zone
type: Concept
created: 2021-07-23T08:59:07.788Z
creator: schmar
notation: DE-775
in scheme: Tectonic Boundary Objects in Europe
definition: The Rosenthal-Gülden-Braudel-Peckensen fault zone predominantly is located within the northern Eichsmark-Altmark Swell, while the southern tip is associated with the Braunschweig Gifhorn fault system. The southern extension is formed by the Weddingen-Nettgau fault zone (DE-884).
broader: Dipping Harz structure & Sack depression

Horndorf Rosche Thondorf fault zone
type: Concept
created: 2021-07-23T08:59:07.785Z
creator: schmar
notation: DE-752
in scheme: Tectonic Boundary Objects in Europe
definition: 55 km long, NNE-SSW running fault within the Braunschweig-Gifhorn-Lüneburg fault system.
broader: Dipping Harz structure & Sack depression

Southern Ems fault system
type: Concept
created: 2021-07-23T08:59:07.738Z
creator: schmar
notation: DE-810
narrower: Lohne Pollersand fault
narrower: Southern Ems fault
narrower: Schale fault
in scheme: Tectonic Boundary Objects in Europe
broader: Dipping Harz structure & Sack depression

Schale fault
type: Concept
created: 2021-07-23T08:59:07.748Z
creator: schmar
notation: DE-799
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12157
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The NNW-SSE running Ems fault system is located in southern extension of the Ems graben structure, has a length of 16 km and represents the border between the western and central part of the Lower Saxony Basin. The lineament is not affected by strike-slip movements of the crossing Osning lineament (Baldschuhn & Kockel 1999)
broader: Southern Ems fault system

Southern Ems fault
type: Concept
created: 2021-07-23T08:59:07.745Z
creator: schmar
notation: DE-819
notation: DE-804
in scheme: Tectonic Boundary Objects in Europe
definition: The Lohne-Pollersand fault is a 43 km long, NW-SE running fault within the central part of the Lower Saxony Basin and runs almost parallel to the Ems lineament in the west and to the Schale Störung in the east.
broader: Southern Ems fault system

Lohne Pollersand fault
type: Concept
created: 2021-07-23T08:59:07.742Z
creator: schmar
notation: DE-809
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
broader: Southern Ems fault system

Weddingen-Nettgau fault zone
type: Concept
created: 2021-07-23T08:59:07.776Z
creator: schmar
notation: DE-884
in scheme: Tectonic Boundary Objects in Europe
definition: The 64 km long, NNE-SSW running Broistedt-Wittingen fault zone is located at the W-border of the Braunschweig-Gifhorn-Lüneburg fault system and borders in the northern part to the Allertal fault system. The fault zone was involved in the sedimentary and structural development of the Eichsfeld Altmark Swell.
broader: Dipping Harz structure & Sack depression

Ems fault system
type: Concept
created: 2021-07-23T08:59:07.735Z
creator: schmar
notation: DE-757
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
broader: Dipping Harz structure & Sack depression

Flachstöckheim-Immendorf fault zone
type: Concept
created: 2021-07-23T08:59:07.773Z
creator: schmar
notation: DE-843
in scheme: Tectonic Boundary Objects in Europe
definition: The NNW-SSE running Bechtsbüttel-Vordorf fault zone is located within the eastern part of the Lower Saxony Basin, has a length of 20 km and is located close to the Braunschweig-Gifhorn fault zone. The fault zone is associated with the salt diapir Bechtbüttel.
broader: Dipping Harz structure & Sack depression

Ems graben fault system
type: Concept
created: 2021-07-23T08:59:07.732Z
creator: schmar
notation: DE-768
notation: DE-771
notation: DE-780
scope note: We describe the Ems Lineament as a prominent strongly faulted unit with grabens and mostly subparallel fault-zones (generalized interpreted as fault system), which crosses or borders several structural units of the North German Basin. Even though the main structures of this faulted region have been described in detail (e.g. Baldschuhn et al., 2001), no clear definition of the outline of this strongly deformed block has been made to date. The extent of this faulted block was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/12207
definition: The Ems fault system is a 140 km long, NNW-SSE running system of mainly SSE striking grabens and fault zones. It crosses the Lower Saxony Basin in the East. Many of the WNW-ESE fault zones of the central part of the Lower Saxony Basin end or lose significant offset in the Ems lineament area. The Ems Lineament can be broadly regarded as the western boundary of the North German Basin and thus represents the transition to the Anglo-Dutch Basin. The Ems lineament is the southern part of a larger system of predominantly SSE striking elements that can be traced into the Horn Graben. Rifting of the Ems graben within the Lower Saxony Basin started in Lower Gipskeuper times, continued until Upper Gipskeuper times and was followed by inversion in Late Cretaceous (Kockel 2002). [Domain type: Strongly deformed overburden, basement: Avalonia]
broader: Dipping Harz structure & Sack depression

Broidstedt-Wittingen fault zone
type: Concept
created: 2021-07-23T08:59:07.769Z
creator: schmar
notation: DE-829
notation: DE-776
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/12248
definition: The Braunschweig-Gifhorn fault system represents the eastern border of the Lower Saxony Basin and consists of several segments, predominantly oriented N/NNE-S/SSW and subordinate NE-SE and NW-SE respectively. During Early to Middle Buntsandstein time an early stage of reactive salt diapirism takes place followed by sub-salt normal faulting and reactive diapirism in the Late Buntsandstein to Muschelkalk in this fault zone (Warsitzka et al. 2018).
broader: Dipping Harz structure & Sack depression

Bechtsbüttel-Vordorf fault zone
type: Concept
created: 2021-07-23T08:59:07.765Z
creator: schmar
notation: DE-820
scope note: We describe the Braunschweig-Gifhorn-Lüneburg fault system as a prominent strongly faulted unit with mostly subparallel fault zones (generalized interpreted as fault system), which crosses or borders several structural units of the North German Basin. The structural unit defined here is a generalization of contiguous fault systems. Even though the main structures of this faulted region have been described in detail (e.g. Baldschuhn et al., 2001), no clear definition of the outline of this strongly deformed block has been made to date. The extent of this faulted block was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12158
definition: Mainly NNE striking faults. Most of the Mesozoic this structural element show predominantly extensional tectonics (mainly westward dipping, salt influenced extensional structures) but also a strike-slip component can be assumed (especially during the Permian and Late Cretaceous). [tectonic style: halo-tectonics, extensional tectonics, partly strike-slip tectonics; Domain: Stronlgy deformed overburden, Basement: Rhenohercynian/ Avalonia(?)]
broader: Dipping Harz structure & Sack depression

Braunschweig-Gifhorn fault zone
type: Concept
created: 2021-07-23T08:59:07.762Z
creator: schmar
notation: DE-792
notation: DE-798
notation: DE-811
notation: DE-832
notation: DE-844
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12157
references: https://data.geoscience.earth/ncl/geoera/ref/12158
definition: The 44 km long Gronau-Waldhügel fault zone represents the southern border of the Lower Saxony Basin. It crosses the Ems fault system domain without major strike-slip offset.
broader: Dipping Harz structure & Sack depression

Rühle fault
type: Concept
created: 2021-07-23T08:59:07.755Z
creator: schmar
notation: DE-781
in scheme: Tectonic Boundary Objects in Europe
definition: E-W striking fault crossing the Ems fault system.
broader: Dipping Harz structure & Sack depression

Lutter-Salzgitter fault zone
type: Concept
created: 2021-07-23T08:59:07.792Z
creator: schmar
notation: DE-845
in scheme: Tectonic Boundary Objects in Europe
broader: Dipping Harz structure & Sack depression

Central Lower Saxony Basin
type: Concept
created: 2021-07-23T08:59:07.521Z
creator: schmar
notation: DE-932
narrower: Central Lower Saxony Basin fault system
narrower: Kalkriese-Hunteburg fault
narrower: Neukirchen fault
narrower: Rehburg fault system
narrower: Bad Nenndorf fault system
narrower: Petershagen fault
in scheme: Tectonic Boundary Objects in Europe
narrower: Lübbecke fault
references: https://data.geoscience.earth/ncl/geoera/ref/12157
references: https://data.geoscience.earth/ncl/geoera/ref/12161
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/11969
references: https://data.geoscience.earth/ncl/geoera/ref/12173
references: https://data.geoscience.earth/ncl/geoera/ref/12174
references: https://data.geoscience.earth/ncl/geoera/ref/12204
definition: Jurassic to Wealden basin center. The whole Central Lower Saxony Basin was inverted during the Late Cretaceous as a broad anticlinal uplift. Most of the faults run along the northern and southern edges of the structural domain. [type: deformed sedimentary overburden, Basement: Avalonia.]
broader: Lower Saxony Basin

Petershagen fault
type: Concept
created: 2021-07-23T08:59:07.577Z
creator: schmar
notation: DE-817
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12156
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The Petershagen fault represents the southern graben fault of the WNW-ESE running Rehburg graben, is located within the central part of the Lower Saxony Basin and extends over a length of 59 km.
broader: Central Lower Saxony Basin

Bad Nenndorf fault system
type: Concept
created: 2021-07-23T08:59:07.573Z
creator: schmar
notation: DE-812
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12156
definition: The Bad Nenndorf fault system is a 13 km long, ENE-WSE running graben. The graben was initiated within the Middle Jurassic, was intensified within the Lower Cretaceous and lasted until Aptian times. No indications are found for inversion of the graben during Coniac - Santonian times.
broader: Central Lower Saxony Basin

Rehburg fault system
type: Concept
created: 2021-07-23T08:59:07.570Z
creator: schmar
notation: DE-806
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12156
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The Rehburg fault system is a WNW-ESE running graben structure of 53 km length and 14 km width. The northern border of this graben is the southward dipping and listric Rehburg fault, the southern border the northward dipping Petershagen fault.
broader: Central Lower Saxony Basin

Central Lower Saxony Basin fault system
type: Concept
created: 2021-07-23T08:59:07.524Z
creator: schmar
notation: DE-1062
narrower: Aschen fault
narrower: Rheder-Moor-Oythe fault zone
narrower: Goldenhorst-Blenhorst fault zone
narrower: Addrup fault
narrower: Hemmelte-Bokern fault
narrower: Voigtei fault
narrower: Deblinghausen fault
narrower: Oberlanger Tenge - Löningen fault zone
narrower: Neufeld Rehburg fault
narrower: Rehden fault
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12157
references: https://data.geoscience.earth/ncl/geoera/ref/12161
references: https://data.geoscience.earth/ncl/geoera/ref/12158
references: https://data.geoscience.earth/ncl/geoera/ref/11969
references: https://data.geoscience.earth/ncl/geoera/ref/12173
references: https://data.geoscience.earth/ncl/geoera/ref/12174
references: https://data.geoscience.earth/ncl/geoera/ref/12204
definition: The Anticlinal uplift of the Central Lower Saxony Basin is bounded to the north by several ESE/SE striking faults. These faults show both normal and reverse components and are often part of inverted graben structures.
broader: Central Lower Saxony Basin

Deblinghausen fault
type: Concept
created: 2021-07-23T08:59:07.549Z
creator: schmar
notation: DE-791
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: A 37 km long, W-E running fault within the Lower Saxony Basin.
broader: Central Lower Saxony Basin fault system

Voigtei fault
type: Concept
created: 2021-07-23T08:59:07.545Z
creator: schmar
notation: DE-784
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The Voigtei fault borders the Voigtei block, extends over 34 km, strikes W-E and almost parallel to the Rheder Moor Oythe fault zone further North. The fault is located in the central part of the Lower Saxony Basin.
broader: Central Lower Saxony Basin fault system

Hemmelte-Bokern fault
type: Concept
created: 2021-07-23T08:59:07.542Z
creator: schmar
notation: DE-783
notation: DE-794
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The Hemmelte-Bokern fault extends over 48 km, strikes WNW-ESE and is located at the northern rim within the central part of the Lower Saxony Basin.
broader: Central Lower Saxony Basin fault system

Addrup fault
type: Concept
created: 2021-07-23T08:59:07.538Z
creator: schmar
notation: DE-779
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
broader: Central Lower Saxony Basin fault system

Goldenhorst-Blenhorst fault zone
type: Concept
created: 2021-07-23T08:59:07.535Z
creator: schmar
notation: DE-773
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: A 72 km long and W-E striking fault zone and along the northern rim of the Lower Saxony basin.
broader: Central Lower Saxony Basin fault system

Rheder-Moor-Oythe fault zone
type: Concept
created: 2021-07-23T08:59:07.531Z
creator: schmar
notation: DE-765
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: A 140 km long and WNW-ESE striking fault zone, representing the northern rim of the Lower Saxony basin.
broader: Central Lower Saxony Basin fault system

Aschen fault
type: Concept
created: 2021-07-23T08:59:07.527Z
creator: schmar
notation: DE-782
notation: DE-754
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: A 90 km long, WNE-ESE striking fault in elgongation to Neufeld-Rehburg fault.
broader: Central Lower Saxony Basin fault system

Rehden fault
type: Concept
created: 2021-07-23T08:59:07.559Z
creator: schmar
notation: DE-877
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
broader: Central Lower Saxony Basin fault system

Neufeld Rehburg fault
type: Concept
created: 2021-07-23T08:59:07.556Z
creator: schmar
notation: DE-796
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: A 56 km long, WNW-ESE running normal fault in the central part of the Lower Saxony Basin. The fault represents the northern flank of the Rehburg Graben.
broader: Central Lower Saxony Basin fault system

Oberlanger Tenge - Löningen fault zone
type: Concept
created: 2021-07-23T08:59:07.552Z
creator: schmar
notation: DE-795
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: A 125 km long lineament, with WNW-ESE strike in the north of the Osning lineament.
broader: Central Lower Saxony Basin fault system

Kalkriese-Hunteburg fault
type: Concept
created: 2021-07-23T08:59:07.563Z
creator: schmar
notation: DE-800
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12173
definition: The Kalkriese-Hunteburg fault runs W-E, extends over 44 km and is located close to the transition from the Central Lower Saxony Basin to the North Westphalia Lippe Subfault system.
broader: Central Lower Saxony Basin

Ems Lineament
type: Concept
created: 2021-07-23T08:59:07.795Z
creator: schmar
notation: DE-1045
in scheme: Tectonic Boundary Objects in Europe
broader: North German Basin - domain I: North German Plain & Central German North Sea

Teisseyre-Tornquist Zone (TTZ)
scope note: We describe the Teisseyre-Tornquist zone (TTZ) as a tectonic unit, whose boundaries are mainly defined by faults and the extend of grabens (e.g. Rønne Graben). The outline of this tectonostratigraphic unit can be also defined by differences in the Tectonostratigraphy to the surrounding areas. Even though the structure have been described (e. g. Seidel, 2019, Mazur et al., 2017, Mazur et al., 2015), no standardised definition of the outline of this tectonostratigraphic unit has been made to date. The extent of this tectonic unit was newly created/generalised with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
type: Concept
created: 2021-07-23T08:59:09.575Z
creator: schmar
notation: DE-1085
narrower: Gryfice Block
narrower: Kolobrzeg Block
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12220
references: https://data.geoscience.earth/ncl/geoera/ref/12219
references: https://data.geoscience.earth/ncl/geoera/ref/12237
definition: The Teisseyre-Tornquist Zone (TTZ) is generally regarded as a fossil plate boundary in Europe that extends 2000km from the Baltic Sea to the Black Sea (Mazur et al., 2015). The suture is presumed to separate the East European Craton (EEC) from the Paleozoic terranes of Western Europe. In the Paleozoic to Mesozoic cover of this presumed suture zone a complex fault-system developed during the Mesozoic. This major fault system shows different characteristics at different times and shows both extensional structures (Most of Triassic until Jurassic), strike-slip elements (Permian, partly within the Mesozoic?) and contractional to transpressive structures (Upper Cretaceous).
narrower: Rønne Graben
broader: Tectonic Boundary in Germany

Rønne Graben
creator: schmar
created: 2021-08-31T12:36:07.943Z
type: Concept
in scheme: Tectonic Boundary Objects in Europe
notation: DE-1088
preferred label: Rønne-Graben @de
scope note: We describe the "Rønne Graben" as a tectonic unit, whose boundaries are mainly defined by faults and the extend of graben. The outline of this tectonostratigraphic unit can be also defined by differences in the tectonostratigraphy to the surrounding areas. Even though the structure have been described (e. g. Seidel, 2019), no standardised definition of the outline of this tectonostratigraphic unit has been made to date. This tectonic unit is listed here only for completeness and is not part of German territory. The extent of this tectonic unit was newly created/generalised with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also „Tectonic boundaries in Germany”. @de
definition: NNE-SSW stiking transfer element between the Sorgenfrei-Tornquist Zone and the Teisseyre-Tornquist Zone (e.g. Liboriussen et al., 1987)
references: https://data.geoscience.earth/ncl/geoera/ref/12214
references: https://data.geoscience.earth/ncl/geoera/ref/12236
broader: Teisseyre-Tornquist Zone (TTZ)

Kolobrzeg Block
scope note: We describe the Kolobrzeg Block as a tectonic unit, whose boundaries are mainly defined by faults. The outline of this tectonostratigraphic unit can be also defined by differences in the tectonostratigraphy to the surrounding areas. Even though the structure have been described (e. g. Seidel, 2019; Kosakowski et al., 2010), no standardised definition of the outline of this tectonostratigraphic unit has been made to date. This tectonic unit is only listed here for the sake of completeness and only a small part of it lies on German territory. The extent of this tectonic unit was newly created/generalised with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
type: Concept
created: 2021-07-23T08:59:09.605Z
creator: schmar
notation: DE-1087
in scheme: Tectonic Boundary Objects in Europe
narrower: Caledonian deformation front large-scale fault system
references: https://data.geoscience.earth/ncl/geoera/ref/12209
references: https://data.geoscience.earth/ncl/geoera/ref/12237
definition: The Kolobrzeg block is a tectonic block of the northwestern Teisseyre-Tornquist zone.
broader: Teisseyre-Tornquist Zone (TTZ)

Gryfice Block
scope note: We describe the Gryfice Block as a tectonic unit, whose boundaries are mainly defined by faults. The outline of this tectonostratigraphic unit can be also defined by differences in the tectonostratigraphy to the surrounding areas. Even though the structure have been described (e. g. Seidel, 2019; Kosakowski et al., 2010), no standardised definition of the outline of this tectonostratigraphic unit has been made to date. The extent of this tectonic unit was newly created/generalised with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
type: Concept
created: 2021-07-23T08:59:09.579Z
creator: schmar
notation: DE-1086
narrower: Pernille fault
narrower: Gat fault
narrower: Adler-Kamien fault
narrower: Gryfice fault zone
in scheme: Tectonic Boundary Objects in Europe
narrower: Caledonian deformation front large-scale fault system
references: https://data.geoscience.earth/ncl/geoera/ref/12177
references: https://data.geoscience.earth/ncl/geoera/ref/12199
references: https://data.geoscience.earth/ncl/geoera/ref/8053
definition: The Gryfice Block is one major block, that belongs to the TTZ. It is bordered by the Adler Kamien fault zone to the southwest and in the north by the Rønne Graben (GRAVERSEN 2004). According to DADLEZ (2003) and KIERSNOWSKIE & BUNIAK (2006), the block continues in southeast direction as part of the onshore Mid Polish Trough or Pomeranian Segment.
broader: Teisseyre-Tornquist Zone (TTZ)

Pernille fault
type: Concept
created: 2021-07-23T08:59:09.588Z
creator: schmar
notation: DE-9018
notation: DE-9060
in scheme: Tectonic Boundary Objects in Europe
broader: Gryfice Block

Gryfice fault zone
type: Concept
created: 2021-07-23T08:59:09.601Z
creator: schmar
notation: DE-9016
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12237
references: https://data.geoscience.earth/ncl/geoera/ref/12238
definition: The Gryfice fault zone is located above a Palaeozoic high (Seidel 2019). This high is probably formed by Rotliegend volcanics or an unidentified tilted horst block. The fault zone strikes NW towards the Skurup Fault. It is formed by five major subparallel fault planes. One is located within the Palaeozoic strata and connected to the Palaeozoic high. The assumed rotated block might be bordered to the east by the northeastward dipping GRY_deep fault plane.
broader: Gryfice Block

Swabian - Franconian - South Thuringian Block
type: Concept
created: 2021-07-23T08:59:08.958Z
creator: schmar
notation: DE-989
notation: DE-1025
notation: DE-990
notation: DE-991
narrower: Southern Franconian - Swabian Escarpments
narrower: Southern Kraichgau Depression & Franconian Platform subdomain
narrower: Northern Kraichgau & Grabfeld Depression subdomain
narrower: southwestern fringe of the Bohemian Massif & the Thuringian Forest subdomains
scope note: We describe the Swabian - Franconian - South Thuringian Block as the sum of neighbouring tectonostratigraphic structural units, whose boundaries are defined by faults and/or on the base of partly fuzzy trends of the lithofacies and paleofacies. The extent of this tectonostratigraphic units was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Bavaria (LFU) provides and describes a more detailed and partly updated fault data set of Bavaria within the framework of the HIKE project (DE-BY_1356). Map Reference: Röllig et al. (1990), GK 1:1000000, GK 1:500000 of Bavaria (Freudenberger & Schwerd, 1996), tectonic map of Bavaria 1:1000000 (Freudenberger & Schwerd, 1996), HIKE (DE-BY 1536). For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12188
references: https://data.geoscience.earth/ncl/geoera/ref/12189
references: https://data.geoscience.earth/ncl/geoera/ref/753
broader: Tectonic Boundary in Germany

Southern Franconian - Swabian Escarpments
type: Concept
created: 2021-07-23T08:59:08.962Z
creator: schmar
notation: DE-989
narrower: Freudenstadt-Hohenzollern-Filder-Bodensee Graben system
scope note: We describe the Southern Franconian - Swabian Escarpments as a tectonostratigraphic unit, whose boundaries are defined by faults and/or on the base of partly fuzzy trends of the lithofacies and paleofacies as well as geomorphological aspects. The extent of this unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Bavaria (LFU) provides and describes a more detailed and partly updated fault data set of Bavaria within the framework of the HIKE project (DE-BY_1356). Map Reference: GK 1:1000000, GK 1:500000 of Bavaria (Freudenberger & Schwerd, 1996), tectonic map of Bavaria 1:1000000 (Freudenberger & Schwerd, 1996), HIKE (DE-BY 1356). For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
definition: The Southern Franconian-Swabian Escarment subdomain is characterized by long-distance impact of the Alpine orogeny and by the long living, ENE striking lineaments such as the Schwarzwald-Bayerwald line. [Domain type: Deformed sedimentary overburden, Basement: Moldanubian.]
broader: Swabian - Franconian - South Thuringian Block

Freudenstadt-Hohenzollern-Filder-Bodensee Graben system
type: Concept
created: 2021-07-23T08:59:08.966Z
creator: schmar
notation: DE-1025
in scheme: Tectonic Boundary Objects in Europe
scope note: We describe the Freudenstadt-Hohenzollern-Filder-Bodensee Graben system as a cluster with intersecting Cenozoic-Quaternary faults. The outline frames the occurence of the fault of the graben system. The extent of this unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK 1:1000000. For References see also Tectonic boundaries in Germany.
broader: Southern Franconian - Swabian Escarpments

Southern Kraichgau Depression & Franconian Platform subdomain
type: Concept
created: 2021-07-23T08:59:08.970Z
creator: schmar
notation: DE-990
scope note: We describe the Southern Kraichgau Depression & Franconian Platform subdomain as a tectonostratigraphic unit, whose boundaries are only in sections defined by faults but also are defined on the base of partly fuzzy trends of the lithofacies and paleofacies. The extent of this unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Bavaria (LFU) provides and describes a more detailed and partly updated fault data set of Bavaria within the framework of the HIKE project (DE-BY_1356). Map Reference: GK 1:1000000, GK 1:500000 of Bavaria (Freudenberger & Schwerd, 1996), tectonic map of Bavaria 1:1000000 (Freudenberger & Schwerd, 1996), HIKE (DE-BY 1356). For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
definition: Domain type: sedimentary overburden, Basement: Mainly Saxothuringian.
broader: Swabian - Franconian - South Thuringian Block

German Alps
type: Concept
created: 2021-07-23T08:59:09.037Z
creator: schmar
narrower: Folded Molasse Basin
narrower: Königsee-Traunsee fault system
narrower: Northern Calcerous Alps (Bavarian Nappe System)
narrower: Helveticum
narrower: Rhenodanubian Flysch
scope note: We describe the German Alps as a superordinate tectonostratigraphic basement, unit, whose boundaries are defined by faults (thrusts) and lithological changes. It's a combination of tectonostratigraphic units, which show predominantly Alpidic deformation structures. The subdivision of this domain is based on the Austrian subdivision for the HIKE project. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Map Reference: GK 1:500000 of Bavaria (Freudenberger & Schwerd, 1996), tectonic map of Bavaria 1:1000000 (Freudenberger & Schwerd, 1996), GK 1:1000000. For References see also Tectonic boundaries in Germany.
definition: The structural units of the European Alps consist of the Helvetic, the Penninic, the Ostalpin and the Südalpin. The Bavarian Alps consist of the superordinate units of Folded Molasse (Faltenmolasse) with upright Molasse, the Helvetic, the Ultra-Helvetic, the Feuerstätter Flysch, the Rhenodanubikum, the Arosa zone and the Northern Calcareous Alps (Nördliche Kalkalpen) (Fig. 18). Due to Upper Cretaceous´ nappe and flake tectonics, reverse-and thrust faults, strike slip but also normal faults were formed, which separate at the same time the nappes and flakes. The W-E to WSE-ENE running fault zones separate the individual nappes, and often are transferred by NW-SE and NE-SW running strike slip fault. Prominent examples At diagonal and transverse fault systems (lateral ramps, strike-slip faults) the geometry of folds and thusts often changes abruptly in the strike, whereby the amount of the total shortening between individually often differently deformed segments within an thrust belt (transfer faults) remain preserved and fault offset amounts of up to several kilometers can add up. Further characteristics for the structural style are strike-slip fault systems and associated compressional- and extensional structures. These were formed during Oligocene-Miocene N-S compression caused by eastward directed shift of the central East-Alp block. Examples for these fault systems are Innsbruck-Salzburg-Amstetten fault Salzach–Ennstal fault, Königsee–Traunsee fault.[Domain type: Cenozoic basement block, Basement: Moldanubian /Alpine orogeny.]
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12188
references: https://data.geoscience.earth/ncl/geoera/ref/12189
references: https://data.geoscience.earth/ncl/geoera/ref/1242
references: https://data.geoscience.earth/ncl/geoera/ref/753
broader: Tectonic Boundary in Germany

Rhenodanubian Flysch
type: Concept
created: 2021-07-23T08:59:09.054Z
creator: schmar
notation: DE-925
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12188
references: https://data.geoscience.earth/ncl/geoera/ref/12189
references: https://data.geoscience.earth/ncl/geoera/ref/753
scope note: Rheno Danube Flysch @de
definition: The Rhenodanube-Flysch subdomain belongs to the Helveticum-Arosa zone of the Alps. Domain: Cenozoic basement block, Basement: Moldanubian/Alpine orogeny.
scope note: The here used extent of this structural unit is based on Freudenberger & Schwerd (1996). The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
broader: German Alps

Folded Molasse Basin
type: Concept
created: 2021-07-23T08:59:09.041Z
creator: schmar
notation: DE-924
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12188
references: https://data.geoscience.earth/ncl/geoera/ref/12189
references: https://data.geoscience.earth/ncl/geoera/ref/753
scope note: The here used extent of this structural unit is based on Freudenberger & Schwerd (1996). The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
broader: German Alps

Königsee-Traunsee fault system
type: Concept
created: 2021-07-23T08:59:09.044Z
creator: schmar
notation: DE-201
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12188
references: https://data.geoscience.earth/ncl/geoera/ref/12189
references: https://data.geoscience.earth/ncl/geoera/ref/753
definition: The Königsee-Traunstein fault system is located within the Staufen-Höllengebirge Nappe and borders to the Hallstätter Nappe in the north. The fault system extends over c. 20 km and runs WSE-ENE.
scope note: The here used extent of this structural unit is based on Freudenberger & Schwerd (1996). The exact definition of the fault domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
broader: German Alps

Northern Calcerous Alps (Bavarian Nappe System)
type: Concept
created: 2021-07-23T08:59:09.048Z
creator: schmar
notation: DE-922
notation: DE-923
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12188
references: https://data.geoscience.earth/ncl/geoera/ref/12189
references: https://data.geoscience.earth/ncl/geoera/ref/753
scope note: The extent of this structural unit is based on Freudenberger & Schwerd (1996). The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
broader: German Alps

Helveticum
type: Concept
created: 2021-07-23T08:59:09.051Z
creator: schmar
notation: DE-926
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12188
references: https://data.geoscience.earth/ncl/geoera/ref/12189
references: https://data.geoscience.earth/ncl/geoera/ref/753
scope note: Helveticum @de
scope note: The here used extent of this structural unit is based on Freudenberger & Schwerd (1996). The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
broader: German Alps

Rynkøbing-Fyn-Møn-Arkona highs
scope note: We describe the Rynkøbing-Fyn-Møn-Arkona highs as a WNW-ESE striking chain of highs in the north of the Southern Permian Basin. Here we define this chain of structural highs as a tectonostratigraphic domain whose boundaries are not clearly defined by faults and fault systems. The outline of the domain can only be roughly defined based on lithostratigraphic trends and on the base of differences in the deformation pattern and differences of the erosional level to surrounding areas. Even though the structure have been described (e. g. Doornenbal & Stevenson, 2010), no clear definition of the outline of this tectonostratigraphic unit has been made to date. The extent of this tectonic unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
type: Concept
created: 2021-07-23T08:59:09.507Z
creator: schmar
notation: DE-1069
narrower: Møn-Arkona High
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12176
references: https://data.geoscience.earth/ncl/geoera/ref/12205
references: https://data.geoscience.earth/ncl/geoera/ref/12223
references: https://data.geoscience.earth/ncl/geoera/ref/8022
definition: The Ringkøbing-Fyn High separates the Danish subsurface into the Norwegian-Danish Basin to the north and the North German Basin to the south. The Ringkøbing-Fyn High consists of relatively shallow basement rocks as compared to the Norwegian-Danish Basin which is cut by the approximately north-south trending Horn Graben. The western fraction of the high is bounded by the Central Graben in the West and the Horn Graben in the East which is characterized by ESE-WNW to E-W to ENE-WSW to NE-SE trending extensional faults, displaying half-graben structural settings (Javed, 2012).
broader: Tectonic Boundary in Germany

Møn-Arkona High
narrower: Wiek fault
scope note: We describe the Møn-Arkona High as part of a WNW-ESE striking chain of highs in the north of the Southern Permian Basin. Here we define Møn-Arkona High as a tectonostratigraphic unit, whose boundaries are not clearly defined by faults. The outline of this tectonostratigraphic unit can be also defined based on lithostratigraphic trends and on the base of differences in the deformation pattern and differences of the erosional level to surrounding areas. Even though the structure have been described (e. g. Seidel, 2019), no clear definition of the outline of this tectonostratigraphic unit has been made to date. The extent of this tectonic unit was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
type: Concept
created: 2021-07-23T08:59:09.511Z
creator: schmar
notation: DE-1009
narrower: Hiddensee fault
narrower: Arkona fault
narrower: Juetland-Moen fault zone
narrower: Binz Hamrane fault
narrower: Skurup fault
narrower: Basement step I
narrower: Basement step II
narrower: Basement step III
narrower: Basement step IV
narrower: Basement step V
narrower: Agricola Svedala fault II
in scheme: Tectonic Boundary Objects in Europe
narrower: Adler-Kamien fault
narrower: Agricola-Svedala fault
narrower: Caledonian deformation front large-scale fault system
references: https://data.geoscience.earth/ncl/geoera/ref/12237
references: https://data.geoscience.earth/ncl/geoera/ref/8031
definition: The Møn-Arkona high domain represents a summary of the Møn High and Arkona High, both located in the Baltic Sea and is associated to the Ringkøbing-Fyn High. Domain type: Paleozoic basement high below relatively thin Cenozoic/Cretaceous to Mesozoic (?) sedimentary coverage, Basement Domain: Baltica.
broader: Rynkøbing-Fyn-Møn-Arkona highs

Juetland-Moen fault zone
type: Concept
created: 2021-07-23T08:59:09.523Z
creator: schmar
notation: DE-9002
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12186
references: https://data.geoscience.earth/ncl/geoera/ref/12237
definition: The Jütland‐Møn fault zone forms WNW striking steps of the southwestward dipping crust of Baltica (EEC) and its Late Proterozoic to Early‐Palaeozoic cover, below the thick (500‐2500 ms) thrust and folded Ordovician. According to Seidel (2019) the fault zone belongs to basement faults, which are responsible for the stepwiese southwestward dipping of Baltica. The fault zone can be traced over 70 km from the Adler‐Kamień Fault Zone (DE-9017) in a WNW direction, dipping towards SSW. Seven separate single normal fault planes can be traced: Jütland‐Møn 1‐4, Basement_step 1, 4 & 5 . The vertical displacement reaches up to 600 ms, but decreases towards the WNW to an offset of about 100 ms.
broader: Møn-Arkona High

Binz Hamrane fault
type: Concept
created: 2021-07-23T08:59:09.526Z
creator: schmar
notation: DE-9008
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12237
definition: The NNE-SSW-running Binz-Hamrane fault probably has a strike slip character (Seidel 2019) and is located NE of Rügen.
broader: Møn-Arkona High

Basement step I
type: Concept
created: 2021-07-23T08:59:09.539Z
creator: schmar
notation: DE-9024
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12238
broader: Møn-Arkona High

Basement step II
type: Concept
created: 2021-07-23T08:59:09.542Z
creator: schmar
notation: DE-9025
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12238
broader: Møn-Arkona High

Basement step III
type: Concept
created: 2021-07-23T08:59:09.545Z
creator: schmar
notation: DE-9026
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12238
broader: Møn-Arkona High

Basement step IV
type: Concept
created: 2021-07-23T08:59:09.549Z
creator: schmar
notation: DE-9027
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12238
broader: Møn-Arkona High

Hiddensee fault
type: Concept
created: 2021-07-23T08:59:09.517Z
creator: schmar
notation: DE-9001
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12237
definition: NNE-SSW running normal fault in northern extension of isle of Rügen that belongs to basement faults, which are responsible for the stepwise southwestward dipping of Baltica (Seidel 2019).
broader: Møn-Arkona High

Basement step V
type: Concept
created: 2021-07-23T08:59:09.553Z
creator: schmar
notation: DE-9028
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12238
broader: Møn-Arkona High

Arkona fault
type: Concept
created: 2021-07-23T08:59:09.520Z
creator: schmar
notation: DE-9000
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12237
references: https://data.geoscience.earth/ncl/geoera/ref/12238
definition: The WNW-ESE striking Arkona fault is a normal fault, characterized by no massive offsets and partially formed as a flexure. This fault belongs to Paleozoic-Mesozoic faults whtin the accretionaly wedge and younger overlying successions (Seidel 2019).
broader: Møn-Arkona High

Agricola Svedala fault II
type: Concept
created: 2021-07-23T08:59:09.556Z
creator: schmar
notation: DE-9059
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12202
references: https://data.geoscience.earth/ncl/geoera/ref/12240
references: https://data.geoscience.earth/ncl/geoera/ref/12242
definition: The Agricola‐Svedala Fault is located close to the Danish offshore region and shows an almost N‐S strike direction and dips steeply towards the west. According to Seidel (2019) the Cretaceous succession is especially affected by normal flexure causing an offset of about 25 ms.
broader: Møn-Arkona High

Bohemian Massif & East German Variscan to Pre-Variscan basement highs
type: Concept
created: 2021-07-23T08:59:08.644Z
creator: schmar
notation: DE-972
notation: DE-973
notation: DE-974
notation: DE-975
notation: DE-976
notation: DE-977
notation: DE-1064
notation: DE-1070
notation: DE-1071
notation: DE-960
notation: DE-1053
notation: DE-1054
notation: DE-1060
narrower: Granulitgebirge fault set
narrower: Erzgebirge fault set
narrower: Fichtelgebirge fault set
narrower: Thuringian-Franconian-Voigtland Schiefergebirge fault set
narrower: Bavarian - Bohemian Teplá-Barrandian
narrower: Elbe Zone (Basement outcrops)
scope note: We describe the Bohemian Massif & East German Variscan to Pre-Variscan basement Highs as tectonostratigraphic basement units, whose boundaries are defined by faults and/or lithological changes. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Bavaria (LFU) provides and describes a more detailed and partly updated fault data set of Bavaria within the framework of the HIKE project (DE-BY_1531). Map Reference: Röllig et al. (1990), GK 1:1000000. For References see also Tectonic boundaries in Germany.
narrower: Bavarian-Bohemian Moldanubian fault set
in scheme: Tectonic Boundary Objects in Europe
narrower: Lausitz Block
narrower: Münchberg Crystalline complex
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/753
definition: [Domain type: Variscan basement block, Basement: Saxothuringian.]
broader: Tectonic Boundary in Germany

Bavarian - Bohemian Teplá-Barrandian
type: Concept
created: 2021-07-23T08:59:08.674Z
creator: schmar
notation: DE-1070
narrower: Marienbad-Complex / Western Bohemian Shearzone / Tepla-Domazlice Zone
scope note: We describe the Bohemian (Teplá-Barrandium) block as a tectonostratigraphic basement unit, whose boundaries are defined by faults and lithological changes. It's a combination of the Tepla-Barrandium basement rock outcrops of the Bavarian Forest and the Bohemian Massif. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Besides the presented generalized overview fault-data (Schulz et al., 2013), the geological state authority of Bavaria (LFU) provides and describes a more detailed and partly updated fault data set of Bavaria within the framework of the HIKE project (DE-BY_1531). Map Reference: GK 1:500000 of Bavaria (Freudenberger & Schwerd, 1996), tectonic map of Bavaria 1:1000000 (Freudenberger & Schwerd, 1996), HIKE (DE-BY 1531). For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/753
definition: Domain type: Variscan basement block, Basement: Moldanubian.
broader: Bohemian Massif & East German Variscan to Pre-Variscan basement highs

SE Central Netherlands Basin domain
type: Concept
created: 2021-07-23T08:59:08.879Z
creator: schmar
notation: DE-1022
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12249
references: https://data.geoscience.earth/ncl/geoera/ref/12251
scope note: The extent of the Cenozoic tectonostratigraphic domain was newly created with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. For References see also Tectonic boundaries in Germany.
definition: The SE Central Netherlands basin domain is a Mesozoic basin west of the Münsterland Cretaceous basin and is characterized by WNW-ESE striking faults. During the Paleocene Laramide inversion, the West and Central Netherlands basins were both further uplifted and deeply eroded, locally down to the Triassic (Wong et al., 2007). The Subhercynian inversion in the Central Netherlands Basin is less well documented, as due to deep erosion during later phases no Upper Cretaceous deposits are preserved, but also there in several wells Danian chalk overlies pre-Cretaceous successions (Wong et al., 2007). [Domain type: Sedimentary overburden, Basement: Avalonia.]
broader: Tectonic Boundary in Germany

South German Molasse Basin
definition: The European Molasse Basin is a Tertiary foreland basin at the northern front the Alps and extends over parts of France, Switzerland, Germany and Austria and was build some 35 Million years ago. This large asymmetrical syncline is filled with mostly clastic sediments originating from erosional processes of Alps, and is underlain by Mesozoic sedimentary successions. The typically wedge shape of the basin evolved in consequence of the Euro-Adriatic continental collision and the rise of the Alps since the Cretaceous (Berge and Veal 2005). Those sediments are partly overrun and folded due to the ongoing plate movement of the Euro-Adriatic continental collision (Schmid et al. 2008). In general, foreland basins are known to contain complex fault pattern due to the tectonic development (Beaumont 1981, Decelles & Giles 1996) and are characterized by thrusts close to the deformation front due to plate convergence and normal faults at the foreland, due to extensional stresses, which lead to basin subsidence foreland bulge development (Bergerat 1987, Bradley & Kidd 1991). Example for this complexity of fault pattern also within the South German Molasse basin are recent studies on a 3D seismic cube around Munich (von Hartmann et al. 2016). Here, large normal faults show lateral alternating dips that displace the Molasse sediments. Although they are disconnected, they strike parallel to fault lineaments of the underlying carbonate platform. Von Hartmann et al. (2016) suggest that these faults grew both upward and downward from the middle of the Molasse package, are newly initiated within the Molasse sediments and not caused by reactivation of the faults in the carbonate platform and/or crystalline basement. Aside from these locally observed characteristics, main structural elements in the South German Molasse (Fig. 17 a, country sheet) are found in the North the “Folded Molasse (directly in front of the Alps and therefore involved within the nappes), which is bordered by the Alp…
type: Concept
created: 2021-07-23T08:59:09.003Z
creator: schmar
notation: DE-921
narrower: Donau Escarpment
narrower: Schwarzwald-Bayerwald fault zone
narrower: Landshut-Neuöttinger Escarpment
narrower: Pfullendorf fault system
narrower: Keilberg fault
narrower: Lauchert graben fault system
scope note: We describe the South German Molasse Basin as a tectonostratigraphic unit in the northern foreland of the Alps. To the south this tectonostratigraphic domain is borderd by thrusts of the Folded Molasse. However, the actual structure is a result of erosion and especially to the north a discrete outline cannot be clearly defined. The extent of this unit was edited with a view to a structured assignment of fault data for the HIKE project and is based on a large number of partly contradictory map series and citations that were generalized for this purpose. The exact definition of the domain borders and the remaining uncertainties therein in some areas is still to be described/discussed in detail in the future. Due to increased exploration within this region for hydrocarbons, and in recent years also for geothermal energy, a large amount of seismic data (also 3D) has been collected. In recent years, new interpretations have been carried out based on this data and new fault maps have been developed. Since the generalized fault dataset (Schulz et al., 2013) presented here contains datasets older than the 1990's, some lineaments contradict the latest findings. The most up-to-date data for this region, with a higher level of detail, is provided by the LFU for Bavaria in the Hike project. Map Reference: Map Reference: GK 1:500000 of Bavaria (Freudenberger & Schwerd, 1996), tectonic map of Bavaria 1:1000000 (Freudenberger & Schwerd, 1996), GK1000, HIKE (HotLime_Case_Study_1). For References see also Tectonic boundaries in Germany.
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12163
references: https://data.geoscience.earth/ncl/geoera/ref/12172
references: https://data.geoscience.earth/ncl/geoera/ref/12178
references: https://data.geoscience.earth/ncl/geoera/ref/12234
references: https://data.geoscience.earth/ncl/geoera/ref/12245
references: https://data.geoscience.earth/ncl/geoera/ref/753
broader: Tectonic Boundary in Germany

Landshut-Neuöttinger Escarpment
type: Concept
created: 2021-07-23T08:59:09.016Z
creator: schmar
notation: DE-292
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/789
definition: The Landshut-Neuötting fault zone, located in front of the Donau-Randabbruch fault zone, borders the crystalline of the Landshut-Neuötting high towards SW. The fault zone has a length of c. 50 km and runs WNW-ESE.
broader: South German Molasse Basin

Pfullendorf fault system
type: Concept
created: 2021-07-23T08:59:09.019Z
creator: schmar
notation: DE-338
in scheme: Tectonic Boundary Objects in Europe
notation: DE-364
notation: DE-365
notation: DE-276
definition: WSW-ENE-running fault of a length of < 40 km located in the western area of the South German Molasse Basin.
broader: South German Molasse Basin

Keilberg fault
type: Concept
created: 2021-07-23T08:59:09.022Z
creator: schmar
notation: DE-349
in scheme: Tectonic Boundary Objects in Europe
definition: The c. 40 km long, NNW-SSE-running Keilberg fault displaces the Bohemian Massif up to 1200 m against the South German Großscholle.
broader: South German Molasse Basin

Lauchert graben fault system
type: Concept
created: 2021-07-23T08:59:09.026Z
creator: schmar
notation: DE-352
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12175
definition: The c. 13 km long, N-S-running Lauchert graben fault system is located at the NW-margin of the South German Molasse basin and close to the Hohenzollern graben fault system.
broader: South German Molasse Basin

Donau Escarpment
type: Concept
created: 2021-07-23T08:59:09.006Z
creator: schmar
notation: DE-272
notation: DE-449
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12191
references: https://data.geoscience.earth/ncl/geoera/ref/12231
definition: Northeastern boundary of the Southern Molasse Basin and simultaneous southwestern boundary to the Bavarian Forest, running WNW-ESE with a length c. 130 km. At this fault zone, the basement of the Bavarian Forest has been uplifted by more than 1300 m (Rohrmüller et al. 1996) compared to its foreland and locally a fault zone width of 5 km has been documented (Führer & Soffel 1975). The fault was initiated during the Variscan orogeny about 330 million years ago. During Alpidic orogeny, the fault was reactivated, especially from the Cretaceous until the Tertiary. The Danube rim fault has a jump
broader: South German Molasse Basin

Schwarzwald-Bayerwald fault zone
type: Concept
created: 2021-07-23T08:59:09.009Z
creator: schmar
notation: DE-273
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/12247
definition: The Schwarzwald-Bayerwald fault zone represents the western extension of the Donau Escarpment and is located at the N-margin of the South German Molasse Basin. The W-E-running fault zone often shows minor fault throws of 10-30 m, very locally up to 70 m (Walter 1995) and extends over a lenght of < 20 km.
broader: South German Molasse Basin

Tectonic Boundary in Ukraine
type: Concept
top concept of: Tectonic Boundary Objects in Europe
created: 2020-11-27T09:00:42.747Z
preferred label: Тектонична границя в Україні @uk
notation: UA-1000
narrower: Fault systems of the Volyn-Podolian structure
narrower: Fault system of the North-Ukrainian hand zone
narrower: The Carpathian fault systems
narrower: Fault systems of the Ukrainian shield
narrower: Fault systems of the South Ukrainian monoclinal
narrower: Fault systems of the Crimea
narrower: Fault systems of the Pre-Dobruja
narrower: Fault systems of the Dnieper-Donetsk Rift
narrower: Fault system of the crystalline Basement
narrower: Fault systems of the Folded Donbass
scope note: All named tectonic boundary objects that are located (at least partly) in Ukraine, are identified by an ID with the prefix „UA“ listed in the notation. Fault systems and/or fault domains can cross political borders and are therefore shared by several countries. Therefore, they can contain faults from different countries, indicated by country-specific prefixes to the respective ID.
definition: Fault in Ukraine displayed in the HIKE European fault database, taken from the tectonic map of Ukraine 1:1.000.000
in scheme: Tectonic Boundary Objects in Europe

Fault systems of the Ukrainian shield
type: Concept
created: 2020-11-27T09:00:43.948Z
preferred label: Система розломів Українського щита @uk
definition: Fault systems of the Ukrainian shelf are limited by the Prychernomorska Lowland to the south, The river Prypyat and its tributaries to the north, Prydniprovska Lowland to the east and the Volynska and Podilska Uplands to the west
definition: Системи розломів українського шельфу обмежені Причерноморською низовиною на південь, річкою Прип'ять та її притоками на півночі, Придніпровською низовиною на сході та Волинською та Подільською височинами на заході @uk
scope note: Fault systems of the Ukrainian shelf are limited by the Prychernomorska Lowland to the south, The river Prypyat and its tributaries to the north, Prydniprovska Lowland to the east and the Volynska and Podilska Uplands to the west
notation: UA-1003
narrower: Faults of the South Donbass block tectonic zone
narrower: Sushchansko-Perzhansko-Surozkyi Fault
narrower: Brusylivsky Fault (243)
narrower: Tsentralny Fault
narrower: Brusylivsky Fault (247, 248)
narrower: Bershadsky Fault
narrower: Letychivsky Fault
narrower: Odesko-Talnivsky deep fault zone
narrower: Buzky Fault (255)
narrower: Chernobylskyi Fault
narrower: [UA-263]
narrower: Yadlovo-Traktemirovsky Fault (265)
narrower: Pervomaisko-Traktemyrivsky Fault
narrower: Dashevsky Fault
narrower: Gvozdavsky Fault
narrower: Vradievsky Fault
narrower: Pervomaisky Fault (266, 280)
narrower: Voznesensky Fault
narrower: Tsentralno-Buzky Fault
narrower: Zvenigorodsko-Annivsky Fault
narrower: Bokovy Faultansky Fault
narrower: Inguletsky Fault
narrower: Zakhidno-Inguletsky Fault
narrower: Smelyansky Fault
narrower: Orikhovo-Pavlogradsky Fault (304, 340)
narrower: Devladivsky Fault (306)
narrower: Derezuvatsky Fault (310)
narrower: Khortytsky Fault (311)
narrower: Derezuvatsky Fault (312)
narrower: Konksky Fault (319)
narrower: Verkhivtsevsky Fault
narrower: Kommissarivsky Fault
narrower: Dzerzhinsky Fault
narrower: Azovo-Pavlogradsky Fault
narrower: Khortytsky Fault (344)
narrower: Konksky Fault (353, 354, 355)
narrower: Mushketivsky Fault
narrower: Sarnensko-Varvarivsky Fault (410)
narrower: Andrushivsky Fault
narrower: Sarnensko-Varvarivsky Fault (413)
narrower: Zvizdal-Zalіsky Fault
narrower: Nemyrivsky Fault
narrower: Teterivsky Fault (418)
narrower: Buzky Fault (420)
narrower: Talnivsky Faulti
narrower: Pervomaisky Fault (422)
narrower: Kirovogradsky Fault
narrower: Ky Faultrovogradsky Fault
narrower: Zakhidnoinguletsky Fault
narrower: Kry Faultvorizhsko-Kremenchutsky Fault
narrower: Derezuvatsky Fault (433)
narrower: Malokatery Faultnivsky Fault
narrower: Orikhovo-Pavlogradsky Fault (435)
narrower: Derezuvatsky Fault (436, 437)
narrower: Korsatsky Fault
narrower: South Donbass block tectonic zone
narrower: Devladivskyi Fault (445)
narrower: [UA-446]
narrower: Brusylivsky Fault (447)
narrower: Yadlovo-Traktemirovsky Fault (448)
narrower: Pervomaisky Fault (449)
narrower: y Faultemilchy Faultnsky Fault
narrower: Brusylivskyi Fault (456)
narrower: [UA-457]
narrower: Orikhovo-Pavlogradsky Fault (459)
narrower: [UA-462]
narrower: [UA-468]
narrower: Teterivsky Fault (472)
narrower: Odeskyi Fault (473)
narrower: Odeskyi Fault (474)
narrower: Suschano-Perzhansky Fault
in scheme: Tectonic Boundary Objects in Europe

[UA-263]
type: Concept
created: 2020-11-27T09:00:44.257Z
preferred label: Система розломів Українського щита @uk
notation: UA-263
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Teterivsky Fault (418)
type: Concept
created: 2020-11-27T09:00:45.170Z
preferred label: Тетерівський @uk
definition: The fault zone is traced from Hrytsiv town in the southwest to the river Pripyat in the northeast (on the border with Belarus) and passes into the territory of this country.
definition: Зона розлому стежиться від м. Грицев на південному заході до річки Прип´ять на північному сході ( на кордоні з Білоруссю) і переходить на територію цієї країни @uk
notation: UA-418
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Chernobylskyi Fault
type: Concept
created: 2020-11-27T09:00:44.229Z
preferred label: Чорнобильський @uk
definition: From Bila Krynytsia village in the south-west it is traced in the north-eastern direction to Chornobyl city
definition: Від селища Біла Криниця на південному заході трасується в північно-східному напрямку до м. Чорнобиль @uk
alternative label: Loevsky Fault
alternative label: Лоєвський @uk
notation: UA-259
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Nemyrivsky Fault
type: Concept
created: 2020-11-27T09:00:45.142Z
definition: Traces from the Dniester River near Mohyliv-Podilskyi town in the southwest to the Yadlovo-Traktemirovska fault zone in the north-eastern direction to Berezan town
definition: Трасується від р. Дністер поблизу м. Могилів-Подільський на південному заході до Ядлово-Трактеміровської зони розломів в північно східному напрямку на м. Березань @uk
notation: UA-415
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Buzky Fault (255)
type: Concept
created: 2020-11-27T09:00:44.199Z
preferred label: Бузький @uk
definition: It is traced from Bershad town on the south-east to the intersection with the Nemyrivskyn fault near Nemyriv town on the north-west.
definition: Стежиться від м. Бершадь на ПдСх до перетину з Немирівським розломом біля м. Немирів на ПнЗх @uk
alternative label: Khmilnyкsky Fault
alternative label: Хмільникський @uk
notation: UA-255
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Zvizdal-Zalіsky Fault
type: Concept
created: 2020-11-27T09:00:45.115Z
preferred label: Звіздаль-Заліський @uk
definition: Observed from Ilyintsi village in the south to the Andrushivky fault in the north near Andrushivka village
definition: Спостерігається від с. Ільїнці на півдні до Андрушівського розлому на півночі поблизу селища Андрушівка @uk
notation: UA-414
references: https://data.geoscience.earth/ncl/geoera/ref/7009
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Odesko-Talnivsky deep fault zone
type: Concept
created: 2020-11-27T09:00:44.171Z
preferred label: без назви @uk
definition: Chip-type faults to the Odesko-Talnivsky deep fault zone near Haivoron town
definition: Розломи сколового типу до Одесько-Тальнівської зони глибинного розлому поблизу м. Гайворон @uk
notation: UA-252
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Letychivsky Fault
type: Concept
created: 2020-11-27T09:00:44.144Z
preferred label: Летичівський @uk
definition: Followed from Shpykov village in the southeast to the river Sluch near Starokostiantyniv town in the northwest
definition: Стежиться від с. Шпиков на південному сході до річки Случь поблизу м. Старокостянтинів на північному заході @uk
notation: UA-251
notation: UA-252
notation: UA-253
notation: UA-256
notation: UA-276
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Bershadsky Fault
type: Concept
created: 2020-11-27T09:00:44.116Z
preferred label: Бершадський @uk
definition: It can be traced from Bershad in the southwest to the Nemyrivsky fault near Shpykov village in the northwest
definition: Простежується від м Бершадь на південному заході до Немирівського розлому поблизу селища Шпиков на північному заході @uk
notation: UA-250
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Brusylivsky Fault (247, 248)
type: Concept
created: 2020-11-27T09:00:44.088Z
preferred label: Брусилівський @uk
definition: It is traced from Skvira town in the south to Kornin village in the north
definition: Стежиться від м. Сквіри на півдні до селища Корнін на півночі @uk
notation: UA-247
notation: UA-248
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Tsentralny Fault
type: Concept
created: 2020-11-27T09:00:44.060Z
preferred label: Центральний @uk
notation: UA-244
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Brusylivsky Fault (243)
type: Concept
created: 2020-11-27T09:00:44.032Z
preferred label: Брусилівський @uk
definition: It is traced in the submeridional direction in the form of fragments from the village of Kornin in the south and is cut by the Teterivsky fault in the north near the country's border.
definition: Стежиться в субмеридіональному напрямку у вигляді фрагментів від селища Корнін на півдні і зрізається Тетерівським розломом на півночі біля кордону країни @uk
alternative label: Boguslavsky Fault
alternative label: Богуславський @uk
notation: UA-243
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Sushchansko-Perzhansko-Surozkyi Fault
type: Concept
created: 2020-11-27T09:00:44.004Z
preferred label: Сущано-Пержансько-Сурозький @uk
notation: UA-193
notation: UA-196
notation: UA-197
references: https://data.geoscience.earth/ncl/geoera/ref/7008
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Kry Faultvorizhsko-Kremenchutsky Fault
type: Concept
created: 2020-11-27T09:00:45.362Z
preferred label: Криворізько-Кременчуцький @uk
definition: Within the USh is traced from Snihurivka village in the south to the border of DDZ in the northeast (Nov.Galeshchyna village) and further to the northeast in the EEP foundation
definition: В межах УЩ трасується від с. Снігурівка на півдні до границі ДДЗ на північному сході (с. Нов.Галещина) і далі на північний схід у фундаменті СЄП @uk
notation: UA-432
references: https://data.geoscience.earth/ncl/geoera/ref/7011
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Zakhidnoinguletsky Fault
type: Concept
created: 2020-11-27T09:00:45.335Z
preferred label: Західноінгулецький @uk
definition: In the south near the settlement of Bila Krynytsia it is limited by the Kryvorizhsko-Kremenchugsky deep fault, in the north near Hradynsk village it is blocked by DDZ deposits.
definition: На півдні в районі селища Біла Криниця обмежений Криворізько-Кременчуцьким глибинним розломом, на півночі поблизу селища Градинськ перекривається відкладами ДДЗ @uk
notation: UA-430
notation: UA-431
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Ky Faultrovogradsky Fault
type: Concept
created: 2020-11-27T09:00:45.307Z
preferred label: Кіровоградський @uk
definition: t is observed in the form of a tectonic zone from Bashtanka town in the south, through Kropyvnytskyi (Kirovohrad) city and further in the area of ​​ Zolotonosha town in the north.
definition: Спостерігається у вигляді тектонічної зони від м. Баштанка на півдні, через м. Кропивницький (Кіровоград) і далі в районі міста Золотоноша на півночі стежиться у фундаменті ДДЗ @uk
notation: UA-427
notation: UA-428
references: https://data.geoscience.earth/ncl/geoera/ref/7009
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Kirovogradsky Fault
type: Concept
created: 2020-11-27T09:00:45.280Z
preferred label: Кіровоградський @uk
definition: It is observed in the form of a tectonic zone from Bashtanka town in the south, through Kropyvnytskyi (Kirovohrad) city and further in the area of Zolotonosha town in the north.
definition: Спостерігається у вигляді тектонічної зони від м. Баштанка на півдні, через м. Кропивницький (Кіровоград) і далі в районі міста Золотоноша на півночі стежиться у фундаменті ДДЗ @uk
notation: UA-423
notation: UA-424
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Pervomaisky Fault (422)
type: Concept
created: 2020-11-27T09:00:45.252Z
preferred label: Первомайський @uk
definition: Traces from Mykolayiv in the southeast to Pervomaisk in the northwest
definition: Трасується від м Миколаїв на південному сході до м. Первомайськ на північному заході @uk
notation: UA-422
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Talnivsky Faulti
type: Concept
created: 2020-11-27T09:00:45.225Z
preferred label: Тальнівський @uk
definition: It is traced from the Sinitsa River (east of Gaivoron town to Talne village on the Girsky Tikich River
definition: Стежиться від р. Синиця (на схід від м. Гайворон до селища Тальне на р. Гірський Тікич @uk
notation: UA-421
references: https://data.geoscience.earth/ncl/geoera/ref/7009
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Buzky Fault (420)
type: Concept
created: 2020-11-27T09:00:45.197Z
preferred label: Бузький @uk
definition: It is traced from Bershad town on the south-east to the intersection with the Nemyrivsky fault near Nemyriv town on the north-west.
definition: Стежиться від м. Бершадь на ПдСх до перетину з Немирівським розломом біля м. Немирів на ПнЗх @uk
alternative label: Khmіlnyksky Fault
alternative label: Хмільникський @uk
notation: UA-420
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Sarnensko-Varvarivsky Fault (413)
type: Concept
created: 2020-11-27T09:00:45.087Z
preferred label: Сарненсько-Варварівський @uk
notation: UA-413
references: https://data.geoscience.earth/ncl/geoera/ref/7009
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Andrushivsky Fault
type: Concept
created: 2020-11-27T09:00:45.059Z
preferred label: Андрушівський @uk
definition: It is traced in the sublatitudinal direction from Hrytsev village in the west to the Boguslav submeridional fault near Kornin town in the east
definition: Стежиться в субширотному напрямку від селища Грицев на заході до Богуславського субмеридіонального розлому біля містечка Корнін на сході @uk
notation: UA-412
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Sarnensko-Varvarivsky Fault (410)
type: Concept
created: 2020-11-27T09:00:45.032Z
preferred label: Сарненсько-Варварівський @uk
notation: UA-410
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Suschano-Perzhansky Fault
type: Concept
created: 2020-11-27T09:00:45.943Z
preferred label: Сущано-Пержанський @uk
definition: North-eastern continuation of the Kremenetsky fault within the USh from the river Sluch (Sosnove village) to the border of Ukraine and further to the territory of Belarus
definition: Північно-східне продовження Кременецького розлому в межах УЩ від річки Случь (с. Соснове) до кордону України і далі на територію Білорусі @uk
notation: UA-499
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Mushketivsky Fault
type: Concept
created: 2020-11-27T09:00:45.004Z
preferred label: Мушкетівський @uk
notation: UA-367
references: https://data.geoscience.earth/ncl/geoera/ref/7009
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Konksky Fault (353, 354, 355)
type: Concept
created: 2020-11-27T09:00:44.976Z
preferred label: Конкський @uk
definition: The system of sublatitudinal faults is limited by the Kryvorizhsko-Kremenchugky fault in the west and at the latitude of Kamyanka-Dniprovska is limited by the Malokaterynivka fault.
definition: Система субширотних роломів обмежується Криворізько-Кременчуцьким розломом на заході і на широті м. Кам’янка-Дніпровська обмежується Малокатеринівським розломом @uk
notation: UA-353
notation: UA-354
notation: UA-355
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Khortytsky Fault (344)
type: Concept
created: 2020-11-27T09:00:44.948Z
preferred label: Хортицький @uk
definition: Traced from the shore of the ​​Azov Sea near Berdyansk in the north-western direction to Malokaterynivka village
definition: Трасується від берега Азовського моря неподалік м. Бердянськ в північно-західному напрямку до селища Малокатеринівка @uk
notation: UA-344
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Azovo-Pavlogradsky Fault
type: Concept
created: 2020-11-27T09:00:44.920Z
preferred label: Азово-Павлоградский @uk
definition: Within the USh it is observed from Milky estuary on the coast of the Azov Sea in the south to Pavlograd city in the north
definition: В межах УЩ спостерігається від Молочного лиману на березі Азовського моря на півдні до м. Павлоград на півночі @uk
notation: UA-331
notation: UA-335
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Dzerzhinsky Fault
type: Concept
created: 2020-11-27T09:00:44.893Z
preferred label: Дзержинський @uk
definition: Traces from the Derezuvatsky fault in the southeast (Solone village ) to Verkhnodniprovsk town in the northwest
definition: Трасується від Дерезуватського розлому на південному сході (с.Солоне) до містечка Верхньодніпровськ на північному заході @uk
notation: UA-325
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Kommissarivsky Fault
type: Concept
created: 2020-11-27T09:00:44.866Z
preferred label: Комісарівський @uk
definition: It can be traced from Zhovti Vody town on the south-west in the direction of Verkhnodniprovsk city
definition: Простежується від м. Жовті Води на ПдЗх в напрямку м. Верхньодніпровськ на ПнСх @uk
notation: UA-323
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Verkhivtsevsky Fault
type: Concept
created: 2020-11-27T09:00:44.838Z
preferred label: Верхівцевський @uk
notation: UA-321
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Faults of the South Donbass block tectonic zone
type: Concept
created: 2020-11-27T09:00:43.976Z
preferred label: Розломи Південнодонбаської брилової тектонічної зони @uk
definition: Fault-type faults are common in the southern part of Donbass from Kurakhove town in the west to Amvrosiyivka in the east
definition: Розломи скидового типу поширені в південній частині Донбасу від м. Курахове на заході до м. Амвросіївка на сході @uk
notation: UA-47
notation: UA-48
notation: UA-49
notation: UA-50
notation: UA-51
notation: UA-52
notation: UA-53
notation: UA-54
notation: UA-55
notation: UA-56
notation: UA-57
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Orikhovo-Pavlogradsky Fault (459)
type: Concept
created: 2020-11-27T09:00:45.778Z
preferred label: Оріхово-Павлоградський @uk
definition: Within the USh it is traced from Melitopol city in the south-west in the direction of Orikhiv and further with a change in the direction of north-west to Pavlograd with continuation in the foundation of DDZ
definition: В межах УЩ трасується від міста Мелітополь на південному заході в напрямку м. Оріхів і далі зі зміною напрямку па ПнЗх до м. Павлоград з продовженням у фундаменті ДДЗ @uk
notation: UA-459
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

[UA-457]
type: Concept
created: 2020-11-27T09:00:45.750Z
preferred label: Комісарівський @uk
definition: It is bounded by the Teteriv fault in the south near the town of Polonne and runs north, northeast to the village. Gorodnitsa
definition: Обмежений Тетерівським розломом на півдні в районі містечка Полонне і трасується північ, північний схід до с. Городниця @uk
notation: UA-457
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Konksky Fault (319)
type: Concept
created: 2020-11-27T09:00:44.811Z
preferred label: Конкський @uk
definition: The system of sublatitudinal faults is limited by the Kryvorizhsko-Kremenchugky fault in the west and at the latitude of Kamyanka-Dniprovska is limited by the Malokaterynivka fault.
definition: Система субширотних роломів обмежується Криворізько-Кременчуцьким розломом на заході і на широті м. Кам’янка-Дніпровська обмежується Малокатеринівським розломом @uk
notation: UA-319
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Brusylivskyi Fault (456)
type: Concept
created: 2020-11-27T09:00:45.723Z
preferred label: Брусилівський @uk
definition: It is traced in the submeridional direction in the form of fragments from Kornin village in the south and is cut by the Teterivsky fault in the north near the country's border.It is bounded by the Teterivsky fault in the south near Polonne town and runs north, northeast to Gorodnitsa village
definition: Стежиться в субмеридіональному напрямку у вигляді фрагментів від селища Корнін на півдні і зрізається Тетерівським розломом на півночі біля кордону країни @uk
alternative label: Богуславський @uk
notation: UA-456
references: https://data.geoscience.earth/ncl/geoera/ref/7011
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Derezuvatsky Fault (312)
type: Concept
created: 2020-11-27T09:00:44.783Z
preferred label: Дерезуватський @uk
definition: Within the USh is traced from Kalinovske village in the south-west in the direction of Nikopol, Ordzhonikidze and is limited by the system of faults of the Orikhovo-Pavlograd fault in the northeast (east of Novomoskovsk)
definition: В межах УЩ трасується від с. Калинівське на південному заході в напрямку на м. Нікополь, Орджонікідзе і обмежується системою розломів Оріхово-Павлоградського розлому на північному сході (на схід від м.Новомосковськ) @uk
notation: UA-312
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

y Faultemilchy Faultnsky Fault
type: Concept
created: 2020-11-27T09:00:45.695Z
preferred label: Ємильчинський @uk
definition: It is traced from the Teterivsky fault in the south-east (Bykivka village) to the Sushchano-Perzhansky fault in the north-east (near Olevsk).
definition: Стежиться від Тетерівського розлому на південному сході (с. Биківка) до Сущано-Пержанського розлому на північному сході (поблизу м. Олевськ) @uk
notation: UA-450
references: https://data.geoscience.earth/ncl/geoera/ref/7011
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Khortytsky Fault (311)
type: Concept
created: 2020-11-27T09:00:44.756Z
preferred label: Хортицький @uk
definition: Traced from the shore of the Azov Sea near Berdyansk in the north-western direction to Malokaterynivka village
definition: Трасується від берега Азовського моря неподалік м. Бердянськ в північно-західному напрямку до селища Малокатеринівка @uk
notation: UA-311
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Pervomaisky Fault (449)
type: Concept
created: 2020-11-27T09:00:45.666Z
preferred label: Первомайський @uk
definition: Traces from Mykolayiv in the southeast to Pervomaisk in the northwest
definition: Трасується від м Миколаїв на південному сході до м. Первомайськ на північному заході @uk
notation: UA-449
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Derezuvatsky Fault (310)
type: Concept
created: 2020-11-27T09:00:44.729Z
preferred label: Дерезуватський @uk
definition: Within the USh is traced from Kalinovske village in the south-west in the direction of Nikopol, Ordzhonikidze and is limited by the system of faults of the Orikhovo-Pavlograd fault in the northeast (east of Novomoskovsk)
definition: В межах УЩ трасується від с. Калинівське на південному заході в напрямку на м. Нікополь, Орджонікідзе і обмежується системою розломів Оріхово-Павлоградського розлому на північному сході (на схід від м.Новомосковськ) @uk
notation: UA-310
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Devladivsky Fault (306)
type: Concept
created: 2020-11-27T09:00:44.701Z
preferred label: Девладівський @uk
definition: It is bounded by the Kryvorizhsko-Kremenchugsky fault in the west (near Gleyuvatka village), in the east by the Orikhovo-Pavlogradsky fault (near Novomykolayivka village).
definition: Обмежений Криворізько-Кременчуцьким розломом на заході (біля с. Глеюватка), на сході - Оріхово-Павлоградським розломом (біля с. Новомиколаївка) @uk
notation: UA-306
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Orikhovo-Pavlogradsky Fault (304, 340)
type: Concept
created: 2020-11-27T09:00:44.674Z
preferred label: Оріхово-Павлоградський @uk
definition: Within the USh it is traced from Melitopol city in the south-west in the direction of Orikhiv and further with a change in the direction of north-west to Pavlograd with continuation in the foundation of DDZ
definition: В межах УЩ трасується від міста Мелітополь на південному заході в напрямку м. Оріхів і далі зі зміною напрямку па ПнЗх до м. Павлоград з продовженням у фундаменті ДДЗ @uk
notation: UA-304
notation: UA-340
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Smelyansky Fault
type: Concept
created: 2020-11-27T09:00:44.646Z
preferred label: Смелянский @uk
notation: UA-300
references: https://data.geoscience.earth/ncl/geoera/ref/7008
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Zakhidno-Inguletsky Fault
type: Concept
created: 2020-11-27T09:00:44.618Z
preferred label: Західно-Інгулецький @uk
notation: UA-298
references: https://data.geoscience.earth/ncl/geoera/ref/7008
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Inguletsky Fault
type: Concept
created: 2020-11-27T09:00:44.591Z
preferred label: Інгулецький @uk
definition: In the south it is limited by the Bokovyansky fault, in the north it can be traced outside the USh (with Globyne) in the DDZ foundation
definition: На півдні обмежений Боковянським розломом, на півночі простежується і за межами УЩ (с Глобине) у фундаменті ДДЗ @uk
notation: UA-296
notation: UA-297
references: https://data.geoscience.earth/ncl/geoera/ref/7008
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Bokovy Faultansky Fault
type: Concept
created: 2020-11-27T09:00:44.563Z
preferred label: Боковянський @uk
definition: Bounded in the southeast by the Kryvorizhsko-Kremenchugsky deep fault near Kryvyi Rih city, in the northwest it subsides near Rotmistrovka village.
definition: Обмежений на південному сході Криворізько-Кременчуцьким глибинним розломом неподалік м. Кривий Ріг , на північному заході затухає поблизу селища Ротмістровка @uk
notation: UA-295
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Odeskyi Fault (474)
type: Concept
created: 2020-11-27T09:00:45.916Z
preferred label: Одеський @uk
definition: Within the USC stretches from the village of Tsebrykovo in the south in a northerly direction to the town of Blagoveshchensk (Ulyanovka) Cherkasy region
definition: В межах УЩ простягається від селища Цебриково на півдні в північному напрямку до містечка Благовіщенське (Ульянівка) Черкаської області @uk
notation: UA-474
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Odeskyi Fault (473)
type: Concept
created: 2020-11-27T09:00:45.888Z
preferred label: Одеський @uk
definition: Within the USh stretches from Tsebrykovo village in the south in a northerly direction to the town of Blagoveshchensk (Ulyanovka) town Cherkasy region
definition: В межах УЩ простягається від селища Цебриково на півдні в північному напрямку до містечка Благовіщенське (Ульянівка) Черкаської області @uk
notation: UA-473
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Teterivsky Fault (472)
type: Concept
created: 2020-11-27T09:00:45.861Z
preferred label: Тетерівський @uk
definition: The fault zone is traced from Hrytsiv town in the southwest to the river Pripyat in the northeast (on the border with Belarus) and passes into the territory of this country.
definition: Зона розлому стежиться від м. Грицев на південному заході до річки Прип´ять на північному сході ( на кордоні з Білоруссю) і переходить на територію цієї країни @uk
notation: UA-472
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

[UA-468]
type: Concept
created: 2020-11-27T09:00:45.833Z
preferred label: Хмільникський @uk
definition: Traced from Nemyriv town in the southeast through Khmilnyk town and is limited by the Volodymyr-Volynsky fault near the village of Hrytsev village in the northeast.
definition: Трасується від м. Немирів на південному сході через м. Хмільник і обмежується Володимир-Волинським розломом поблизу селаща Грицев на північному сході. @uk
notation: UA-468
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

[UA-462]
type: Concept
created: 2020-11-27T09:00:45.805Z
preferred label: Субоцько-Мошоринський @uk
definition: Traced in the sublatitudinal direction, bounded by the Zvenigorodsko-Annivsky fault in the west (at the latitude of Novoarkhangelsk), in the east – Kryvvorizhsko-Kremenchugsky
definition: Трасується в субширотному напрямку, обмежений Звенігородсько-Аннівським розломом на заході (на широті м. Новоархангельск), на сході - Криворізько-Кременчуцьким @uk
notation: UA-462
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Derezuvatsky Fault (436, 437)
type: Concept
created: 2020-11-27T09:00:45.473Z
preferred label: Дерезуватський @uk
definition: Within the USh is traced from Kalinovske village in the southwest in the direction of Nikopol, Ordzhonikidze and is limited by the system of the Orikhovo-Pavlogradsky fault in the northeast (east of Novomoskovsk town)
definition: В межах УЩ трасується від с. Калинівське на південному заході в напрямку на м. Нікополь, Орджонікідзе і обмежується системою розломів Оріхово-Павлоградського розлому на північному сході (на схід від м.Новомосковськ) @uk
notation: UA-436
notation: UA-437
references: https://data.geoscience.earth/ncl/geoera/ref/7011
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Zvenigorodsko-Annivsky Fault
type: Concept
created: 2020-11-27T09:00:44.535Z
preferred label: Звенігородсько-Аннівський @uk
definition: Traces from Snihurivka vilage in the southeast to the Pervomaisky fault at the foot of the mountain Tikich
definition: Трасується від селища Снігурівка на південному сході до Первомайського розлому біля гирла р. Гірський Тікич @uk
notation: UA-294
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Orikhovo-Pavlogradsky Fault (435)
type: Concept
created: 2020-11-27T09:00:45.446Z
preferred label: Оріхово-Павлоградський @uk
definition: Within the USh it is traced from Melitopol city in the south-west in the direction of Orikhiv and further with a change in the direction of north-west to Pavlograd with continuation in the foundation of DDZ
definition: В межах УЩ трасується від міста Мелітополь на південному заході в напрямку м. Оріхів і далі зі зміною напрямку па ПнЗх до м. Павлоград з продовженням у фундаменті ДДЗ @uk
notation: UA-435
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Tsentralno-Buzky Fault
type: Concept
created: 2020-11-27T09:00:44.507Z
preferred label: Центрально-Бузький @uk
definition: Bounded by the Pervomaisk fault near the city of Pervomaisk in the southeast and Talnivsky in the northwest
definition: Обмежений Первомайським розломом поблизу м. Первомайськ на південному сході та Тальнівським на північному заході @uk
notation: UA-293
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Malokatery Faultnivsky Fault
type: Concept
created: 2020-11-27T09:00:45.418Z
preferred label: Малокатеринівський @uk
definition: Within the limits of USh it is traced from N. Sirogoza village in the southwest to Devladovsky fault in the northeast near Novomykolayivka village
definition: В межах УЩ стежиться від селища Н. Сірогози на південному заході до Девладовського розлому на північному сході в районі селища Новомиколаївка @uk
notation: UA-434
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Voznesensky Fault
type: Concept
created: 2020-11-27T09:00:44.479Z
preferred label: Вознесенський @uk
definition: Observed from Voznesensk on the south-west to Pidhorodnia on the north-west, where it is cut by the Pervomaisky fault
definition: Спостерігається від м. Вознесенськ на ПдСх до м. Підгородня на ПнЗх, де зрізається Первомайським розломом @uk
notation: UA-288
notation: UA-289
notation: UA-291
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Derezuvatsky Fault (433)
type: Concept
created: 2020-11-27T09:00:45.390Z
preferred label: Дерезуватський @uk
definition: Within the USh is traced from Kalinovske village in the southwest in the direction of Nikopol, Ordzhonikidze and is limited by the system of the Orikhovo-Pavlogradsky fault in the northeast (east of Novomoskovsk town)
definition: В межах УЩ трасується від с. Калинівське на південному заході в напрямку на м. Нікополь, Орджонікідзе і обмежується системою розломів Оріхово-Павлоградського розлому на північному сході (на схід від м.Новомосковськ) @uk
notation: UA-433
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Pervomaisky Fault (266, 280)
type: Concept
created: 2020-11-27T09:00:44.424Z
preferred label: Первомайський @uk
definition: Traces from Mykolayiv in the southeast to Pervomaisk in the northwest
definition: Трасується від м Миколаїв на південному сході до м. Первомайськ на північному заході @uk
notation: UA-280
notation: UA-266
narrower: Pervomaisky Transfer Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Pervomaisky Transfer Fault
type: Concept
created: 2020-11-27T09:00:44.451Z
preferred label: Без назви @uk
definition: Local transverse faults to the Pervomaisky fault in the section from Nova Odesa on the south-east to Voznesensk on the north-west
definition: Локальні поперечні розломи до Первомайського розлому на ділянці від м. Нова Одеса на ПдСх до м. Вознесенськ на ПнЗх @uk
notation: UA-281
notation: UA-292
in scheme: Tectonic Boundary Objects in Europe
broader: Pervomaisky Fault (266, 280)

Vradievsky Fault
type: Concept
created: 2020-11-27T09:00:44.396Z
preferred label: Врадієвський @uk
definition: Within the limits of the USh it is traced from the sources of the Berezan river in the south-east in the direction of Vradiyivka town in the north-west.
definition: В межах УЩ стежиться від витоків р. Березань на південному сході в напрямку м. Врадієвка на північному заході @uk
notation: UA-279
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Gvozdavsky Fault
type: Concept
created: 2020-11-27T09:00:44.368Z
preferred label: Гвоздавський @uk
definition: It is traced from Berezivka town on the south-west Lyubashivka town on the north-west, where it is cut by the Odesky fault
definition: Стежиться від м. Березівка на ПдСх до м. Любашівка на ПнЗх, де зрізається Одеським розломом @uk
notation: UA-278
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Dashevsky Fault
type: Concept
created: 2020-11-27T09:00:44.340Z
preferred label: Дашевський @uk
definition: It is bounded on the southeast by the Talnivsky deep fault, and on the northwest by the Nemyrivsky fault near Illintsi village.
definition: Обмежений на південному сході Тальнівським глибинним розломом , на північному заході - Немирівським розломом в районі селища Іллінці @uk
notation: UA-277
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Pervomaisko-Traktemyrivsky Fault
type: Concept
created: 2020-11-27T09:00:44.312Z
preferred label: Первомайський @uk
definition: Traces in the northern direction from Pervomaisk in the south to Novoarkhangelsk and further to Talne village in the north
definition: Трасується в північному напрямку від м. Первомайськ на півдні до м. Новоархангельск і далі до селища Тальне на півночі @uk
notation: UA-267
references: https://data.geoscience.earth/ncl/geoera/ref/7008
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Yadlovo-Traktemirovsky Fault (265)
type: Concept
created: 2020-11-27T09:00:44.285Z
preferred label: Ядлово-Трактемирівський @uk
notation: UA-265
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Yadlovo-Traktemirovsky Fault (448)
type: Concept
created: 2020-11-27T09:00:45.639Z
preferred label: Ядлово-Трактеміровський @uk
definition: The fragment of the fault is traced from Gogolivna village in the south to the border of the country in the north-eastern direction to Pripyat town
definition: Фрагмент розлому трасується від селища Гоголівна півдні до кордону країни в північно-східному напрямку на м.Прип´ять @uk
notation: UA-448
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Brusylivsky Fault (447)
type: Concept
created: 2020-11-27T09:00:45.611Z
preferred label: Брусилівський @uk
definition: It is traced in the submeridional direction in the form of fragments from Kornin village in the south and is cut by the Teteriv fault in the north near the country's border.
definition: Стежиться в субмеридіональному напрямку у вигляді фрагментів від селища Корнін на півдні і зрізається Тетерівським розломом на півночі біля кордону країни @uk
alternative label: Boguslavsky Fault
notation: UA-447
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

[UA-446]
type: Concept
created: 2020-11-27T09:00:45.584Z
notation: UA-446
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Devladivskyi Fault (445)
type: Concept
created: 2020-11-27T09:00:45.556Z
preferred label: Девладівський @uk
notation: UA-445
references: https://data.geoscience.earth/ncl/geoera/ref/7011
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

South Donbass block tectonic zone
type: Concept
created: 2020-11-27T09:00:45.528Z
preferred label: Південнодонбаська брилова тектонічна зона @uk
definition: Fault-type faults are common in the southern part of Donbass from Kurakhove in the west to Amvrosiyivka in the east
definition: Розломи скидового типу поширені в південній частині Донбасу від м. Курахове на заході до м. Амвросіївка на сході @uk
notation: UA-443
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

Korsatsky Fault
type: Concept
created: 2020-11-27T09:00:45.501Z
preferred label: Корсацький @uk
definition: Within the USh it is observed from Primorsk city in the south and is limited by the Azovo-Pavlogradsky fault in the northwest
definition: В межах УЩ спостерігається від м. Приморськ на півдні і обмежений Азово-Павлоградським розломом на північному заході @uk
notation: UA-438
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Ukrainian shield

The Carpathian fault systems
type: Concept
created: 2020-11-27T09:00:43.305Z
preferred label: Система розломів Карпат @uk
definition: Fault systems of the Carpathian are limited by the river Dniester and its tributaries to the east and river Tisa and its tributaries to the west and by the Carpathian mountains to the north and to the south
definition: Системи розломів Карпат обмежені річкою Дністер та її притоками на сході та рікою Тисою та її притоками на заході та Карпатами на півночі та на півдні @uk
notation: UA-1002
narrower: Krakovetsky Fault
narrower: Rava-Rusky Fault
narrower: Radekhivsko-Rogatynsky Fault
narrower: Shepitsky Fault
narrower: Zeleno-Kamy Faultansky Fault
narrower: Rozhansky Fault
narrower: Bory Faultslavo-Pokutsky Fault
narrower: Beregovy Fault
narrower: Orivsky Fault
narrower: Skolivsky Fault
narrower: Stebnytsky Fault
narrower: Parashky Fault
narrower: Pry Faultpannonsky Fault
narrower: Oashsky Fault
narrower: Stryisky Fault
narrower: Chernivetsky Fault
narrower: Peredkarpatsky Fault
narrower: Zakarpatsky Fault
narrower: Berdo-Narol Fault (381)
narrower: Kalusky Fault
narrower: Slavsky Fault
narrower: Gorodetsky Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Ukraine

Krakovetsky Fault
type: Concept
created: 2020-11-27T09:00:43.333Z
preferred label: Краковецький @uk
notation: UA-68
references: https://data.geoscience.earth/ncl/geoera/ref/7010
in scheme: Tectonic Boundary Objects in Europe
broader: The Carpathian fault systems

Parashky Fault
type: Concept
created: 2020-11-27T09:00:43.640Z
preferred label: Парашки @uk
notation: UA-102
references: https://data.geoscience.earth/ncl/geoera/ref/7006
in scheme: Tectonic Boundary Objects in Europe
broader: The Carpathian fault systems

Stebnytsky Fault
type: Concept
created: 2020-11-27T09:00:43.613Z
preferred label: Cтебницький @uk
notation: UA-101
references: https://data.geoscience.earth/ncl/geoera/ref/7006
in scheme: Tectonic Boundary Objects in Europe
broader: The Carpathian fault systems

Gorodetsky Fault
type: Concept
created: 2020-11-27T09:00:43.920Z
preferred label: Городецький @uk
notation: UA-497
references: https://data.geoscience.earth/ncl/geoera/ref/7006
in scheme: Tectonic Boundary Objects in Europe
broader: The Carpathian fault systems

Skolivsky Fault
type: Concept
created: 2020-11-27T09:00:43.585Z
preferred label: Сколівський @uk
notation: UA-100
references: https://data.geoscience.earth/ncl/geoera/ref/7006
in scheme: Tectonic Boundary Objects in Europe
broader: The Carpathian fault systems

Slavsky Fault
type: Concept
created: 2020-11-27T09:00:43.893Z
preferred label: Славський @uk
notation: UA-469
references: https://data.geoscience.earth/ncl/geoera/ref/7006
in scheme: Tectonic Boundary Objects in Europe
broader: The Carpathian fault systems

Orivsky Fault
type: Concept
created: 2020-11-27T09:00:43.557Z
preferred label: Орівський @uk
notation: UA-99
references: https://data.geoscience.earth/ncl/geoera/ref/7006
in scheme: Tectonic Boundary Objects in Europe
broader: The Carpathian fault systems

Kalusky Fault
type: Concept
created: 2020-11-27T09:00:43.864Z
preferred label: Калушський @uk
notation: UA-454
references: https://data.geoscience.earth/ncl/geoera/ref/7006
in scheme: Tectonic Boundary Objects in Europe
broader: The Carpathian fault systems

Beregovy Fault
type: Concept
created: 2020-11-27T09:00:43.529Z
preferred label: Береговий @uk
notation: UA-98
references: https://data.geoscience.earth/ncl/geoera/ref/7006
in scheme: Tectonic Boundary Objects in Europe
broader: The Carpathian fault systems

Berdo-Narol Fault (381)
type: Concept
created: 2020-11-27T09:00:43.836Z
preferred label: Бердо-Нароль @uk
notation: UA-381
references: https://data.geoscience.earth/ncl/geoera/ref/7006
in scheme: Tectonic Boundary Objects in Europe
broader: The Carpathian fault systems

Bory Faultslavo-Pokutsky Fault
type: Concept
created: 2020-11-27T09:00:43.501Z
preferred label: Бориславо-Покутский @uk
notation: UA-97
references: https://data.geoscience.earth/ncl/geoera/ref/7006
in scheme: Tectonic Boundary Objects in Europe
broader: The Carpathian fault systems

Zakarpatsky Fault
type: Concept
created: 2020-11-27T09:00:43.808Z
preferred label: Закарпацький @uk
notation: UA-236
references: https://data.geoscience.earth/ncl/geoera/ref/7006
in scheme: Tectonic Boundary Objects in Europe
broader: The Carpathian fault systems

Rozhansky Fault
type: Concept
created: 2020-11-27T09:00:43.474Z
preferred label: Рожанський @uk
notation: UA-96
references: https://data.geoscience.earth/ncl/geoera/ref/7006
in scheme: Tectonic Boundary Objects in Europe
broader: The Carpathian fault systems

Peredkarpatsky Fault
type: Concept
created: 2020-11-27T09:00:43.780Z
preferred label: Передкарпацький @uk
notation: UA-208
references: https://data.geoscience.earth/ncl/geoera/ref/7006
in scheme: Tectonic Boundary Objects in Europe
broader: The Carpathian fault systems

Zeleno-Kamy Faultansky Fault
type: Concept
created: 2020-11-27T09:00:43.445Z
preferred label: Зелено-Камянский @uk
notation: UA-95
references: https://data.geoscience.earth/ncl/geoera/ref/7006
in scheme: Tectonic Boundary Objects in Europe
broader: The Carpathian fault systems

Chernivetsky Fault
type: Concept
created: 2020-11-27T09:00:43.752Z
preferred label: Чернівецький @uk
notation: UA-207
references: https://data.geoscience.earth/ncl/geoera/ref/7006
in scheme: Tectonic Boundary Objects in Europe
broader: The Carpathian fault systems

Stryisky Fault
type: Concept
created: 2020-11-27T09:00:43.724Z
preferred label: Стрийський @uk
notation: UA-204
references: https://data.geoscience.earth/ncl/geoera/ref/7006
in scheme: Tectonic Boundary Objects in Europe
broader: The Carpathian fault systems

Shepitsky Fault
type: Concept
created: 2020-11-27T09:00:43.417Z
preferred label: Шепітський @uk
notation: UA-79
references: https://data.geoscience.earth/ncl/geoera/ref/7010
in scheme: Tectonic Boundary Objects in Europe
broader: The Carpathian fault systems

Radekhivsko-Rogatynsky Fault
type: Concept
created: 2020-11-27T09:00:43.388Z
preferred label: Радехівсько-Рогатинський @uk
notation: UA-78
references: https://data.geoscience.earth/ncl/geoera/ref/7010
in scheme: Tectonic Boundary Objects in Europe
broader: The Carpathian fault systems

Oashsky Fault
type: Concept
created: 2020-11-27T09:00:43.696Z
preferred label: Оашський @uk
notation: UA-201
references: https://data.geoscience.earth/ncl/geoera/ref/7006
in scheme: Tectonic Boundary Objects in Europe
broader: The Carpathian fault systems

Rava-Rusky Fault
type: Concept
created: 2020-11-27T09:00:43.361Z
preferred label: Рава-Руський @uk
notation: UA-69
references: https://data.geoscience.earth/ncl/geoera/ref/7010
in scheme: Tectonic Boundary Objects in Europe
broader: The Carpathian fault systems

Pry Faultpannonsky Fault
type: Concept
created: 2020-11-27T09:00:43.668Z
preferred label: Припаннонський @uk
notation: UA-127
references: https://data.geoscience.earth/ncl/geoera/ref/7006
in scheme: Tectonic Boundary Objects in Europe
broader: The Carpathian fault systems

Fault systems of the Dnieper-Donetsk Rift
type: Concept
created: 2020-11-27T09:00:46.330Z
preferred label: Система розломів Дніпровсько-Донецької западини @uk
definition: Fault systems of the Dnieper-Donetsk rift are located on the Poltavska plain and Prydniprovska lowland and are limited by the Pryazovska upland to the south-east and the Donetskyi ridge from the east, some water reservoir to the west and the river Dnieper and its tributaries to the north
definition: Системи розломів Дніпровсько-Донецького рифту розташовані на Полтавській рівнині та Придніпровській низовині та обмежені Прязовською височиною на південному сході та Донецьким хребтом зі сходу, деякими водосховищами на заході та річкою Дніпро та його притоками на півночі @uk
notation: UA-1007
narrower: Lutuginskyi
narrower: Faults of the southern marginal zone
narrower: Tsentralno-Donetskyi Fault
narrower: Poliskyi Fault
narrower: Tsentralnyi Fault
narrower: Korulsko-Krasnopilskyi
narrower: Donetsko-Kadiivskyi
narrower: Dniprovsko-Prypyatskyi
narrower: Krasnorichinsky (on the border with the Folded Donbass), then the faults of the Northern side zone
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Ukraine

Faults of the southern marginal zone
type: Concept
created: 2020-11-27T09:00:46.385Z
preferred label: Розломи південної крайової зони @uk
definition: Traced from Slavutych in the northwest to Volnovakha in the southeast
definition: Простежуються від м.Славутич на північному заході до м. Волноваха на південному сході @uk
notation: UA-5
notation: UA-6
notation: UA-43
notation: UA-44
notation: UA-45
notation: UA-46
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Dnieper-Donetsk Rift

Lutuginskyi
type: Concept
created: 2020-11-27T09:00:46.357Z
preferred label: Лутугінский @uk
notation: UA-4
references: https://data.geoscience.earth/ncl/geoera/ref/7012
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Dnieper-Donetsk Rift

Krasnorichinsky (on the border with the Folded Donbass), then the faults of the Northern side zone
type: Concept
created: 2020-11-27T09:00:46.578Z
preferred label: Краснорічинський (на межі із Складчастим Донбасом), далі розломи Північної бортової зони @uk
definition: The Seversky Donets River in the southeast and the Dnieper River in the northwest are limited within the borders of Ukraine.
definition: Обмежуються в кордонах України р. Сіверський Донець на південному сході та р. Дніпро на північному заході @uk
notation: UA-484
references: https://data.geoscience.earth/ncl/geoera/ref/7012
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Dnieper-Donetsk Rift

Dniprovsko-Prypyatskyi
type: Concept
created: 2020-11-27T09:00:46.550Z
preferred label: Дніпровсько-Припятський @uk
notation: UA-475
references: https://data.geoscience.earth/ncl/geoera/ref/7012
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Dnieper-Donetsk Rift

Donetsko-Kadiivskyi
type: Concept
created: 2020-11-27T09:00:46.522Z
preferred label: Донецько-Кадіївський @uk
notation: UA-27
references: https://data.geoscience.earth/ncl/geoera/ref/7012
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Dnieper-Donetsk Rift

Korulsko-Krasnopilskyi
type: Concept
created: 2020-11-27T09:00:46.495Z
preferred label: Корульсько-Краснопільський @uk
notation: UA-20
references: https://data.geoscience.earth/ncl/geoera/ref/7012
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Dnieper-Donetsk Rift

Tsentralnyi Fault
type: Concept
created: 2020-11-27T09:00:46.468Z
preferred label: Центральний @uk
notation: UA-11
notation: UA-12
notation: UA-13
references: https://data.geoscience.earth/ncl/geoera/ref/7012
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Dnieper-Donetsk Rift

Poliskyi Fault
type: Concept
created: 2020-11-27T09:00:46.440Z
preferred label: Поліський @uk
notation: UA-9
references: https://data.geoscience.earth/ncl/geoera/ref/7012
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Dnieper-Donetsk Rift

Tsentralno-Donetskyi Fault
type: Concept
created: 2020-11-27T09:00:46.413Z
preferred label: Центрально-Донецький @uk
notation: UA-8
references: https://data.geoscience.earth/ncl/geoera/ref/7012
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Dnieper-Donetsk Rift

Fault system of the North-Ukrainian hand zone
type: Concept
created: 2020-11-27T09:00:43.249Z
preferred label: Система розломів Північно-української горстової зони @uk
definition: Traced in fragments in the sublatitudinal direction south of Ratne town to Kamin-Kashirsky
definition: Трасується фрагментарно в субширотному напрямку південніше м. Ратне до м. Камінь-Каширський @uk
notation: UA-169
narrower: Pivdennoratnivsky Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Ukraine

Pivdennoratnivsky Fault
type: Concept
created: 2020-11-27T09:00:43.277Z
preferred label: Південноратнівський @uk
definition: Traced in fragments in the sublatitudinal direction south of Ratne town to Kamin-Kashirsky
definition: Трасується фрагментарно в субширотному напрямку південніше м. Ратне до м. Камінь-Каширський @uk
notation: UA-170
notation: UA-407
in scheme: Tectonic Boundary Objects in Europe
broader: Fault system of the North-Ukrainian hand zone

Fault system of the crystalline Basement
type: Concept
created: 2020-11-27T09:00:46.605Z
preferred label: Система розломів кристалічного фундамента СЄП в ДДЗ @uk
narrower: Yadlovo-Traktemirovsky
narrower: Kryvorizhsko-Kremenchutskyi
narrower: Orikhovo-Pavlogradskyi
narrower: Kharkivsky
narrower: Glukhivsky
narrower: Pereyaslav-Khmelnytskyi-Prylukskyi
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Ukraine

Orikhovo-Pavlogradskyi
type: Concept
created: 2020-11-27T09:00:46.690Z
preferred label: Оріхово-Павлоградський @uk
definition: Traced from Pavlograd in the southeast to the border with Russia in the northwest, passes by Sumy
definition: Простежений від м. Павлоград на південному сході до кордону з РФ на північному заході, проходить повз м. Суми @uk
notation: UA-477
references: https://data.geoscience.earth/ncl/geoera/ref/7012
in scheme: Tectonic Boundary Objects in Europe
broader: Fault system of the crystalline Basement

Kryvorizhsko-Kremenchutskyi
type: Concept
created: 2020-11-27T09:00:46.662Z
preferred label: Криворізько-Кременчуцький @uk
definition: Traced from Globyne village in the south through the DDZ in the northern, northeastern direction to the border with Russia in the area of Middle Buddha
definition: Простежується від селища Глобине на півдні через ДДЗ в північному, північно-східному напрямку до кордону з РФ в районі с. Середина Буда @uk
notation: UA-476
references: https://data.geoscience.earth/ncl/geoera/ref/7012
in scheme: Tectonic Boundary Objects in Europe
broader: Fault system of the crystalline Basement

Yadlovo-Traktemirovsky
type: Concept
created: 2020-11-27T09:00:46.634Z
preferred label: Ядлово-Трактеміровський @uk
definition: Continuation in the northern direction of the USH fault from the southern side of the DDZ near Gogoliv village to the Desna River in the north
definition: Продовження в північному напрямку розлому УЩ від південного борту ДДЗ в районі селища Гоголів до річки Десна на півночі @uk
notation: UA-470
in scheme: Tectonic Boundary Objects in Europe
broader: Fault system of the crystalline Basement

Pereyaslav-Khmelnytskyi-Prylukskyi
type: Concept
created: 2020-11-27T09:00:46.772Z
preferred label: Переяслав-Хмельницький-Прилуцький (Кіровоградський) @uk
definition: Traced according to geophysical data from Zolotosha town in the south to the border with Russia near Semenivka town in the north
definition: Трасується за геофізичними даними від м. Золотоша на півдні до кордону з Росією поблизу м . Семенівка на півночі @uk
notation: UA-487
references: https://data.geoscience.earth/ncl/geoera/ref/7012
in scheme: Tectonic Boundary Objects in Europe
broader: Fault system of the crystalline Basement

Glukhivsky
type: Concept
created: 2020-11-27T09:00:46.745Z
preferred label: Глухівський @uk
definition: Traces from the river Snov in the west to the border with Russia in the east in the direction of Rylsk
definition: Трасується від річки Снов на заході до кордону з Росією на сході в напрямку м. Рильск @uk
notation: UA-486
in scheme: Tectonic Boundary Objects in Europe
broader: Fault system of the crystalline Basement

Kharkivsky
type: Concept
created: 2020-11-27T09:00:46.717Z
preferred label: Харківський @uk
definition: Bounded in the south by the Kuibyshevsky fault east of Pereshchepyne village, in the northeast it extends beyond Ukraine to the north of Kharkiv
definition: Обмежений на півдні Куйбишівським розломом східніше селища Перещепине, на північному сході виходить за межі Украіни на північ від м. Харків @uk
notation: UA-483
references: https://data.geoscience.earth/ncl/geoera/ref/7012
in scheme: Tectonic Boundary Objects in Europe
broader: Fault system of the crystalline Basement

Fault systems of the South Ukrainian monoclinal
type: Concept
created: 2020-11-27T09:00:45.971Z
preferred label: Система розломів Південно-Української монокліналі @uk
definition: Fault systems of South Ukrainian monoklinal are located on the Prychernomorska lowland and limited by the Black sea and Azov from the south, the river Dniester from the west, the Pryazovska upland from the east and the Prydniprovska and the Podilska uplands from the north
definition: Системи розломів південноукраїнського монокліналу розташовані на Причерноморській низовині та обмежені Чорним морем та Азовом з півдня, річкою Дністер із заходу, Приазовською височиною зі сходу та Придніпровською та Подільською височинами з півночі @uk
notation: UA-1004
narrower: Khersonskyi Fault
narrower: Odeskyi Fault
narrower: Golitsynskyi Fault
narrower: Mykhailivskyi Fault
narrower: Sulynsko-Tarkhankutskyi Fault
narrower: Krakovetskyi Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Ukraine

Mykhailivskyi Fault
type: Concept
created: 2020-11-27T09:00:46.082Z
preferred label: Михайлівський @uk
notation: UA-372
references: https://data.geoscience.earth/ncl/geoera/ref/7013
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the South Ukrainian monoclinal

Golitsynskyi Fault
type: Concept
created: 2020-11-27T09:00:46.054Z
preferred label: Голіцинський @uk
notation: UA-371
references: https://data.geoscience.earth/ncl/geoera/ref/7013
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the South Ukrainian monoclinal

Odeskyi Fault
type: Concept
created: 2020-11-27T09:00:46.026Z
preferred label: Одеський @uk
definition: Traced according to geophysical data from Tsebrikovo villagre on the NW in the south-eastern direction near Odessa on the shelf of Zakhidnochornomorska depression
definition: Трасується за геофізичними даними від селища Цебриково на ПнЗх в південно-східному напрямку повз м. Одеса на шельф Західно-Чорноморської западини @uk
notation: UA-370
references: https://data.geoscience.earth/ncl/geoera/ref/7013
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the South Ukrainian monoclinal

Khersonskyi Fault
type: Concept
created: 2020-11-27T09:00:45.999Z
preferred label: Система розломів Південно-Української монокліналі @uk
alternative label: Херсонський @uk
notation: UA-228
references: https://data.geoscience.earth/ncl/geoera/ref/7013
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the South Ukrainian monoclinal

Krakovetskyi Fault
type: Concept
created: 2020-11-27T09:00:46.137Z
preferred label: Краковецький @uk
notation: UA-374
references: https://data.geoscience.earth/ncl/geoera/ref/7013
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the South Ukrainian monoclinal

Sulynsko-Tarkhankutskyi Fault
type: Concept
created: 2020-11-27T09:00:46.110Z
preferred label: Сулинсько-Тарханкутський @uk
notation: UA-373
references: https://data.geoscience.earth/ncl/geoera/ref/7013
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the South Ukrainian monoclinal

Fault systems of the Pre-Dobruja
type: Concept
created: 2020-11-27T09:00:46.248Z
preferred label: Система розломів Преддобруджи @uk
definition: Fault systems of the Pre-Dobruja are located on the Prychernomorska lowland and limited by the Black sea from the east and some lakes from the south, the river Dniester from the north and row of rivers from the east
definition: Системи розломів Переддобруджі розташовані на Причерноморській низовині та обмежені Чорним морем зі сходу та деякими озерами з півдня, річкою Дністер з півночі та низкою річок зі сходу @uk
notation: UA-1006
narrower: Kagul-Izmailskyi Fault
narrower: Bystriiskyi Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Ukraine

Bystriiskyi Fault
type: Concept
created: 2020-11-27T09:00:46.303Z
preferred label: Бистрівський @uk
notation: UA-496
references: https://data.geoscience.earth/ncl/geoera/ref/7005
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Pre-Dobruja

Kagul-Izmailskyi Fault
type: Concept
created: 2020-11-27T09:00:46.275Z
preferred label: Кагул-Ізмаїльський @uk
notation: UA-453
references: https://data.geoscience.earth/ncl/geoera/ref/7005
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Pre-Dobruja

Fault systems of the Folded Donbass
type: Concept
created: 2020-11-27T09:00:46.799Z
preferred label: Система розломів Складчастого Донбасу @uk
definition: Fault systems of the Folded Donbass are located on the Donetskyi ridge and are limited by the river Siverskyi Donets to the north-east and the Pryazovska upland to the south-west and row of rivers to the west
definition: Системи розломів Складчастого Донбасу розташовані на Донецькому хребті і обмежені річкою Сіверський Донець на північному сході та Приазовською височиною на південному заході та низкою річок на заході @uk
notation: UA-1008
narrower: Pivnichno-Donetskyi Fault
narrower: Rovenkivskyi Fault
narrower: Donetsko-Kadiivskyi Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Ukraine

Donetsko-Kadiivskyi Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7012
type: Concept
created: 2020-11-27T09:00:46.883Z
preferred label: Донецько-Кадіївський @uk
definition: Traced from the town of Volnovakha in the southwest to the border of Ukraine in the direction of the village of Milerovo, Russia
definition: Простежується від м. Волноваха на південному заході до кордону України в напрямку селища Мілерово Росії @uk
notation: UA-485
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Folded Donbass

Rovenkivskyi Fault
type: Concept
created: 2020-11-27T09:00:46.855Z
preferred label: Донецько-Кадієвський @uk
definition: Traced from Volnovakhatown in the southwest to the border of Ukraine in the direction of Milerovo village, Russia
definition: Простежується від м. Волноваха на південному заході до кордону України в напрямку селища Мілерово Росії @uk
notation: UA-478
references: https://data.geoscience.earth/ncl/geoera/ref/7012
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Folded Donbass

Pivnichno-Donetskyi Fault
type: Concept
created: 2020-11-27T09:00:46.827Z
preferred label: Pivnichno-Donetskyi @uk
notation: UA-26
references: https://data.geoscience.earth/ncl/geoera/ref/7012
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Folded Donbass

Fault systems of the Crimea
type: Concept
created: 2020-11-27T09:00:46.165Z
preferred label: Система розломів Криму @uk
definition: Fault systems of the Crimea are limited by Zakhidnochornomorska depression in the Black sea from the south and Sorokina depression from the east, the peninsula Crimea from the north and the Vylkivskyi shaft to the west
definition: Системи розломів Криму обмежені Західночорноморською западиною в Чорному морі з півдня та Сорокинською западиною зі сходу, півостровом Крим з півночі та Вильківським валом на заході @uk
notation: UA-1005
narrower: Zakhidno-Krymskyi Fault
narrower: Pivdennoberezhnyi Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Ukraine

Pivdennoberezhnyi Fault
type: Concept
created: 2020-11-27T09:00:46.220Z
preferred label: Південнобережний @uk
notation: UA-226
notation: UA-227
references: https://data.geoscience.earth/ncl/geoera/ref/7007
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Crimea

Zakhidno-Krymskyi Fault
type: Concept
created: 2020-11-27T09:00:46.192Z
preferred label: Західно-Кримський @uk
notation: UA-225
references: https://data.geoscience.earth/ncl/geoera/ref/7007
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Crimea

Fault systems of the Volyn-Podolian structure
type: Concept
created: 2020-11-27T09:00:42.774Z
preferred label: Система розломів Волино-Подільської структури @uk
definition: Fault systems of the Volyn-Podolian structure are limited by the river Dniester and its tributaries to the west and south, the Poliska Lowland to the north and the Kievske plateau to the west
definition: Cистеми розломів Волино-Подільської структури обмежені річкою Дністер та її притоками на захід та південь, Поліською низовиною на півночі та Київським плато на заході @uk
notation: UA-1001
narrower: Terebovlyansky Fault
narrower: Povchano-Ustetskyi Fault
narrower: Suschano-Perzhansko-Kremenetsky Fault
narrower: Kremenetsko-Perzhansky Fault
narrower: Berzh-Baluchynskyi Fault
narrower: Dniprovsko-Prypyatsky Fault
narrower: Rivnensky Fault
narrower: Andrushchivsky Fault
narrower: Monastyrsky Fault
narrower: Lutsky Fault
narrower: Berezhansky Fault
narrower: Teterivsky Fault
narrower: Troyanivsko-Gutsulsky Fault
narrower: Tovtrovy Fault
narrower: Berdo-Narol Fault (395)
narrower: Podilsky Fault
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Ukraine

Monastyrsky Fault
type: Concept
created: 2020-11-27T09:00:43.026Z
preferred label: Монастирський @uk
notation: UA-200
references: https://data.geoscience.earth/ncl/geoera/ref/7009
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Volyn-Podolian structure

Andrushchivsky Fault
type: Concept
created: 2020-11-27T09:00:42.998Z
preferred label: Андрущивський @uk
notation: UA-151
references: https://data.geoscience.earth/ncl/geoera/ref/7009
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Volyn-Podolian structure

Rivnensky Fault
type: Concept
created: 2020-11-27T09:00:42.970Z
preferred label: Рівненьський @uk
notation: UA-148
references: https://data.geoscience.earth/ncl/geoera/ref/7009
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Volyn-Podolian structure

Dniprovsko-Prypyatsky Fault
type: Concept
created: 2020-11-27T09:00:42.942Z
preferred label: Великомосиївський @uk
references: https://data.geoscience.earth/ncl/geoera/ref/7009
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Volyn-Podolian structure

Berzh-Baluchynskyi Fault
type: Concept
created: 2020-11-27T09:00:42.914Z
preferred label: Берз-Балучинський @uk
notation: UA-144
references: https://data.geoscience.earth/ncl/geoera/ref/7009
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Volyn-Podolian structure

Podilsky Fault
type: Concept
created: 2020-11-27T09:00:43.221Z
preferred label: Подільський @uk
notation: UA-429
references: https://data.geoscience.earth/ncl/geoera/ref/7009
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Volyn-Podolian structure

Kremenetsko-Perzhansky Fault
type: Concept
created: 2020-11-27T09:00:42.886Z
preferred label: Кременецько-Пержанський @uk
notation: UA-141
references: https://data.geoscience.earth/ncl/geoera/ref/7009
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Volyn-Podolian structure

Berdo-Narol Fault (395)
type: Concept
created: 2020-11-27T09:00:43.193Z
preferred label: Бердо-Нароль @uk
notation: UA-395
references: https://data.geoscience.earth/ncl/geoera/ref/7009
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Volyn-Podolian structure

Tovtrovy Fault
type: Concept
created: 2020-11-27T09:00:43.165Z
preferred label: Товтровий @uk
notation: UA-394
references: https://data.geoscience.earth/ncl/geoera/ref/7009
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Volyn-Podolian structure

Suschano-Perzhansko-Kremenetsky Fault
type: Concept
created: 2020-11-27T09:00:42.858Z
preferred label: Сущано-Пержансько-Кременецький @uk
definition: Bounded by the Prydnistrovskyi fault in the northwest near the Pomoriany village, on the northeastern flank near Koretsе town turns into Sushchano-Perzhansky fault
definition: Обмежений Придністровським розломом на північному заході в районі селища Поморяни, на північно-східному фланзі в районі м Корець переходить в Сущано-Пержанський розлом @uk
alternative label: Кременецький @uk
notation: UA-138
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Volyn-Podolian structure

Povchano-Ustetskyi Fault
type: Concept
created: 2020-11-27T09:00:42.830Z
preferred label: Повчано-Устецький @uk
notation: UA-137
references: https://data.geoscience.earth/ncl/geoera/ref/7009
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Volyn-Podolian structure

Troyanivsko-Gutsulsky Fault
type: Concept
created: 2020-11-27T09:00:43.137Z
preferred label: Троянівсько-Гуцульський @uk
notation: UA-393
references: https://data.geoscience.earth/ncl/geoera/ref/7009
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Volyn-Podolian structure

Terebovlyansky Fault
type: Concept
created: 2020-11-27T09:00:42.802Z
preferred label: Теребовлянський @uk
notation: UA-136
references: https://data.geoscience.earth/ncl/geoera/ref/7009
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Volyn-Podolian structure

Teterivsky Fault
type: Concept
created: 2020-11-27T09:00:43.109Z
preferred label: Тетерівський @uk
notation: UA-392
references: https://data.geoscience.earth/ncl/geoera/ref/7009
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Volyn-Podolian structure

Berezhansky Fault
type: Concept
created: 2020-11-27T09:00:43.081Z
preferred label: Бережанський @uk
notation: UA-391
references: https://data.geoscience.earth/ncl/geoera/ref/7009
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Volyn-Podolian structure

Lutsky Fault
type: Concept
created: 2020-11-27T09:00:43.053Z
preferred label: Луцький @uk
notation: UA-383
references: https://data.geoscience.earth/ncl/geoera/ref/7009
in scheme: Tectonic Boundary Objects in Europe
broader: Fault systems of the Volyn-Podolian structure

Tectonic Boundaries in Bavaria
narrower: 1: Tectonic Boundary Objects in the central part of the North Alpine Molasse Basin and northward adjoining areas
references: https://data.geoscience.earth/ncl/geoera/ref/7675
created: 2021-01-25T14:19:43.717Z
top concept of: Tectonic Boundary Objects in Europe
type: Concept
preferred label: Tektonische Grenzflächen in Bayern @de
definition: Konzepte der in der Europäischen Störungsdatenbank im Detailierungsgrad von größer 1:200.000 gespeicherten und abrufbaren tektonischen Grenzflächen Bayerns, Stand 12/2020. Berücksichtig sind bedeutende Störungen und Störungssysteme in den geologischen Großeinheiten und strukturellen Domänen Bayerns, mit Ausnahme der Alpen, wie in verschiedenen Maßstäben kartiert oder aus indirekten Hinweisen unter Verwendung geeigneter Methoden abgeleitet. Diese Bestandsaufnahme zielt weniger auf eine vollständige Zusammenstellung wesentlicher tektonischer Elemente ab, als vielmehr auf die Betonung des kontextuellen Zusammenhangs des Störungs-Netzwerks, um das regionale tektonische Regime als Ergebnis großräumiger Krustenbewegungen zu erläutern. Die Erfassung tektonischer Elemente in Bayern und deren kontextuelle Klassifikation dauert an. Diese Bestandsaufnahme ist daher Gegenstand künftiger Fortschreibung. Diese „DE-BY“ Konzepte beschreiben das Störungsnetzwerk Bayern in einem höheren Detailierungsgrad als das deutschlandweite „DE“ Schema @de
narrower: 3: Bohemian Massif domain
narrower: Schichtstufenland Domäne (N und NW Bayern)
references: https://data.geoscience.earth/ncl/geoera/ref/7268
references: https://data.geoscience.earth/ncl/geoera/ref/7269
notation: DE-BY-0
definition: Concepts of tectonic boundaries in Bavaria, corresponding to scales of 1:200,000 and smaller, as stored in and retrievable from the European Fault Data Base, state 12-2020. Considered are major faults and fault systems from all geological units / structural domains of Bavaria, except for the German Alps Domain, as mapped in various scales or inferred from indirect evidence using various methods deemed appropriate in the respective geological settings. Rather than giving a full inventory of principal tectonic features, this compilation aims at stressing the contextual relationship of the fault network in order to elucidate the regional tectonic regime as the result of large-scale crustal movements. In Bavaria, tectonic boundary objects detection and contextual classification is an ongoing process. Hence, this inventory is subject to future upgrading and change. These “DE-BY” concepts, describe the Bavarian fault network at a level of detail beyond the Germany-wide scheme prefixed DE.
in scheme: Tectonic Boundary Objects in Europe
propagate type: Fault
type: Fault
type: Limit

Schichtstufenland Domäne (N und NW Bayern)
in scheme: GC3D limits
type: Fault
type: Limit
narrower: Pisamberg-Hofstetten Fault
narrower: Schöllesberg Fault
narrower: Laufen-Autenberg Fault
narrower: Hainberg-Kirchhöhe Fault
narrower: Hainberg Cross-Fault
narrower: Oberbessenbach-Heimbuchenthal Fault
narrower: Wagenmühle-Erlenbach Fault
narrower: Altenbuch Fault
narrower: Soden-Oberwintersbach Fault
narrower: Anterior Spessart faults
narrower: Hanau-Seligenstadt Basin faults
narrower: Baden Baden-Nuremberg-Erbendorf Line
type: Concept
created: 2021-01-25T14:23:21.358Z
notation: DE-BY_1356
scope note: The tectonic boundaries of the sedimentary cover of the South German block, the Bavarian Scarpland, in parts can be directly observed, otherwise are extrapolated from outcrop evidence or inferred from contour lines pattern. The tectonic boundary inventory of the Scarpland presently is under revision and contextual classification. Many faults and fault zones, thus, are represented and described generalized, resembling a 1:1 m scale. The faults of Bavaria's small share of the Upper Rhine Graben subbasin Hanau-Seligenstadt Basin in the very northwest are described corresponding to a 1:50,000 scale.
scope note: Die Störungen im sedimentären Deckgebirge der Süddeutschen Großscholle, dem Bayerischen Schichtstufenland, sind hauptsächlich an der Oberfläche und in Aufschlüssen zu kartieren oder können aus Streichlinien-Mustern abgeleitet werden. Das Störungsinventar des Schichtstufenlandes ist derzeit in Überprüfung und kontextueller Klassifizierung. Viele der Störungen und Störungszonen sind daher nur generalisiert beschrieben und einem Maßstab entsprechend 1:1 Mio. dargestellt. Die Störungen des geringen bayerischen Anteils am Randbecken des Oberrheingrabens, der Hanau-Seligenstädter Senke, sind einem Maßstab von ca. 1:50 000 entsprechend beschrieben. @de
definition: Die tektonischen Bauelemente der Süddeutschen Großscholle sind teils weitgespannte Aufwölbungen und Einmuldungen, teils weit durchziehende Bruchzonen. Die Störungen im sedimentären Deckgebirge, dem Bayerischen Schichtstufenland, streichen hauptsächlich in flach-herzynischer (WNW-ESE) bzw. steil-herzynischer oder fränkischer (NW-SE) Richtung und zeigen Anzeichen mehrphasiger Dehnung und Kompression (Graben und Horst). Die Verformungsstrukturen beinhalten Faltungen, Abschiebungen, Aufschiebungen und Überschiebungen. @de
definition: Die tektonischen Bauelemente der Süddeutschen Großscholle sind teils weitgespannte Aufwölbungen und Einmuldungen, teils weit durchziehende Bruchzonen. Die Störungen im sedimentären Deckgebirge, dem Bayerischen Schichtstufenland, streichen hauptsächlich in flach-herzynischer (WNW-ESE) bzw. steil-herzynischer oder fränkischer (NW-SE) Richtung und zeigen Anzeichen mehrphasiger Dehnung und Kompression (Graben und Horst), zuletzt durch Reaktivierung während der saxonischen Bruchschollentektonik (Oberkreide bis Neogen), als Fernwirkung der alpidischen Gebirgsbildung. Die Verformungsstrukturen beinhalten Faltungen, Abschiebungen, Aufschiebungen und selten Überschiebungen.
narrower: Ahorntal-Anticline Fault
narrower: Asslitz-Saas Fault
narrower: Atzhausen-Kleinlangheim Fault Zone
narrower: Auerbach Fault
narrower: Baad Fault
narrower: Bad Brückenau graben faults
narrower: Bamberg-Neuses Fault Zone
narrower: Baunachtal Fault
narrower: Bieber Fault
narrower: Birk-Stegenthumbach Fault
narrower: Bischofsheim Fault
narrower: Breitenbuch Fault Zone
narrower: Brücklein Fault Zone
narrower: Coburg Fault
narrower: Creussen Fault
narrower: Donnersdorf-Karbach Fault Zone
narrower: Ehrenbach Fault
narrower: Eichelsbach Fault
narrower: Eisfeld-Kulmbach Fault Zone
narrower: Eschlipper Tal Fault
narrower: Fenkensses-Brüderes Fault
narrower: Freiberg-Döringstadt Fault
narrower: Gräfenberg Fault
narrower: Grettstadt-Aschbach Fault Zone
narrower: Hafenprepach Fault
narrower: Haidenaab Fault
narrower: Hainbach Fault
narrower: Harrbach Fault
narrower: Harres Fault
narrower: Hassberg Fault
narrower: Herrnneuses Fault
narrower: Hersbruck Fault
narrower: Eltersdorf-Röthenbach-Weigenhofen Fault
narrower: Heustreu Fault Zone
narrower: Hollfeld Fault Zone
narrower: Itztal Fault
narrower: Karlstadt-Würzburg-Kitzingen Fault Zone
narrower: Kemnath-Waldeck Fault
narrower: Kilianshof Fault
narrower: Kissingen-Hassfurt Fault Zone
narrower: Kist-Fuchsstadt Fault Zone
narrower: Kronach Fault
narrower: Kümmelberg Fault
narrower: Laudenbach Fault
narrower: Leidersbach-Hobbach Fault
narrower: Lichtenfels Fault
narrower: Lindelbach-Erlach Fault Zone
narrower: Mitwitz Fault
narrower: Mönchberg Fault
narrower: Motten Fault Zone
narrower: Muggenbach Fault
narrower: Neuhütten Fault
narrower: Nordheim Fault
narrower: Oberkatz Fault Zone
narrower: Pautzfeld Fault Zone
narrower: Pegnitz Fault
narrower: Regnitz Valley Fault

GC3D limits
type: ConceptScheme
created: 2020-07-09T13:21:39.619Z
description: .. here should be a short, 3-line text - describing the relevant scheme and allow the user to get started with the topic via the listed top concepts ..

Hersbruck Fault
type: Limit
type: Fault
type: Concept
created: 2021-01-25T14:23:22.328Z
preferred label: Hersbruck Störung @de
notation: DE-BY_967
definition: W-E streichende Abschiebung mit Einfallrichtung N @de
definition: W-E trending normal fault with dip direction N
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_967
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Herrnneuses Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.299Z
preferred label: Herrnneuses Störung @de
notation: DE-BY_1066
definition: SW-NE streichende Abschiebung mit Einfallrichtung NW @de
definition: SW-NE trending normal fault with dip direction NW
references: https://data.geoscience.earth/ncl/geoera/ref/7269
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1066
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Hassberg Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.272Z
preferred label: Hassberg Störung @de
notation: DE-BY_987
definition: NW-SE streichende Abschiebung mit Einfallrichtung NE @de
definition: NW-SE trending normal fault with dip direction NE
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
references: https://data.geoscience.earth/ncl/geoera/ref/6372
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_987
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Harres Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.244Z
preferred label: Harres Störung @de
notation: DE-BY_1015
definition: NW-SE streichende Abschiebung mit Einfallrichtung NE @de
definition: NW-SE trending normal fault with dip direction NE
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1015
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Harrbach Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.216Z
preferred label: Harrbach Störung @de
notation: DE-BY_979
definition: NW-SE streichende Abschiebung mit Einfallrichtung SW @de
definition: NW-SE trending normal fault with dip direction SW
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_979
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Hainbach Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.188Z
preferred label: Hainbach Störung @de
notation: DE-BY_1058
definition: NW-SE streichende Abschiebung mit Einfallrichtung SW (revers invertiert) @de
definition: NW-SE trending normal fault with dip direction SW (reversly inverted)
references: https://data.geoscience.earth/ncl/geoera/ref/6372
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1058
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Haidenaab Fault
limit type: reverseFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.161Z
preferred label: Haidenaab Störung @de
notation: DE-BY_1050
definition: NW-SE streichende Aufschiebung mit Einfallrichtung NE @de
definition: NW-SE trending reverse fault with dip direction NE
references: https://data.geoscience.earth/ncl/geoera/ref/7375
references: https://data.geoscience.earth/ncl/geoera/ref/7295
references: https://data.geoscience.earth/ncl/geoera/ref/7343
references: https://data.geoscience.earth/ncl/geoera/ref/7292
references: https://data.geoscience.earth/ncl/geoera/ref/6372
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1050
broader: Schichtstufenland Domäne (N und NW Bayern)

Hanau-Seligenstadt Basin eastern margin
type: Fault
type: Limit
created: 2021-08-23T07:38:05.549Z
creator: schmar
type: Concept
in scheme: Tectonic Boundary Objects in Europe
in scheme: GC3D limits
notation: LfU-BY_1582
type: https://data.geoscience.earth/ncl/geoera/geoconnect3d/category/9754
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11887
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11722
narrower: Erlensee-Alzenau Fault
narrower: Wilmundsheim Graben eastern boundary
narrower: Kahl-Kleinostheim Fault
narrower: Karlstein-Langstadt Fault
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Erlensee-Alzenau Fault
type: Fault
type: Limit
type: Concept
created: 2021-03-16T09:56:26.943Z
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
notation: DE-BY_1559
definition: NNW-SSE trending, steeply WSW dipping normal fault featuring a throw of up to more than 200 m; northeastern boundary of Wilmundsheim Graben, a branch of Hanau-Seligenstadt Basin.
preferred label: Erlensee-Alzenau Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/8475
references: https://data.geoscience.earth/ncl/geoera/ref/8474
sf touches: Hahnenkamm Scarp
sf touches: Anterior Spessart western boundary
sf touches: Wilmundsheim Graben eastern boundary
in scheme: Tectonic Boundary Objects in Europe
in scheme: GC3D limits
notation: LfU-BY_1559
limit type: normalFault
broader: Hanau-Seligenstadt Basin eastern margin
broader: Hanau-Seligenstadt Basin faults

Wilmundsheim Graben eastern boundary
type: Fault
type: Limit
type: Concept
created: 2021-03-16T09:56:26.889Z
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
notation: DE-BY_1558
definition: N-S- trending, steeply W dipping normal fault; lower step of Anterior Spessart western boundary [DE-BY_1557], eastern boundary of Wilmundsheim Graben, a branch of Hanau-Seligenstadt Basin.
preferred label: Wilmundsheim Graben Ostrand @de
references: https://data.geoscience.earth/ncl/geoera/ref/8475
references: https://data.geoscience.earth/ncl/geoera/ref/8474
sf touches: Anterior Spessart western boundary
sf touches: Erlensee-Alzenau Fault
in scheme: Tectonic Boundary Objects in Europe
in scheme: GC3D limits
notation: LfU-BY_1558
limit type: normalFault
broader: Hanau-Seligenstadt Basin eastern margin
broader: Spessart Borderfault

Karlstein-Langstadt Fault
type: Fault
type: Limit
type: Concept
created: 2021-03-16T09:56:26.967Z
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
notation: DE-BY_1577
definition: Western boundary of Stockstadt-Gross-Umstadt Block, the northern extension of Odenwald. On Bavarian territory, SW-NE trending, steeply NW dipping normal fault with a throw up to more than 200 m, offset 2 km to SE in between Kahl-Stockstadt Fault [DE-BY_1561] and Stockstadt-Obernburg Graben Fault [DE-BY_1574]. Here it forms the southeastern boundary of Kleinwelzheim Horst towards the Stockstadt-Obernburg Graben.
preferred label: Karlstein-Langstadt Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/8475
references: https://data.geoscience.earth/ncl/geoera/ref/8474
in scheme: Tectonic Boundary Objects in Europe
in scheme: GC3D limits
notation: LfU-BY_1577
limit type: normalFault
broader: Hanau-Seligenstadt Basin faults
broader: Hanau-Seligenstadt Basin eastern margin

Kahl-Kleinostheim Fault
type: Fault
type: Limit
type: Concept
created: 2021-03-16T09:56:26.952Z
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
notation: DE-BY_1560
definition: NNW-SSE striking, steeply ENE dipping normal fault featuring a throw of up to 200 m; northeastern boundary of Kleinwelzheim Horst towards Wilmundsheim Graben, a branch of Hanau-Seligenstadt Basin.
preferred label: Kahl-Kleinostheim Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/8475
references: https://data.geoscience.earth/ncl/geoera/ref/8474
sf touches: Anterior Spessart western boundary
sf touches: Karlstein-Langstadt Fault
in scheme: Tectonic Boundary Objects in Europe
in scheme: GC3D limits
notation: LfU-BY_1560
limit type: normalFault
broader: Hanau-Seligenstadt Basin faults
broader: Hanau-Seligenstadt Basin eastern margin

Spessart-Odenwald Borderfault System
type: Fault
type: Limit
scope note: Revised concept as of 2021-03-15, after the HIKE editorial deadline. Corresponding fault geometries in the HIKE Fault Data Base not adjusted accordingly.
scope note: Überarbeitetes Konzept von 2021-03-15, nach HIKE Redaktionsschluss. Die entsprechenden Störungs-Geometrien in der HIKE Störungsdatenbank wurden nicht angepasst. @de
narrower: Stockstadt-Obernburg Graben Eastern Flank
narrower: Stockstadt-Obernburg Graben Fault
narrower: Stockstadt-Obernburg Graben Western Flank
narrower: Klingenberg-Graben
type: Concept
created: 2021-01-25T14:23:23.520Z
preferred label: Spessart-Odenwald Randstörungssystem @de
notation: DE-BY_985
definition: Geknickt, insgesamt N-S streichende Abschiebung mit Einfallsrichtung ± W und westlich (sub)parallele ± E fallende Abschiebungen, die zusammen den Stockstadt-Obernburg Graben und Klingenberg Graben bilden. @de
definition: Kinked, overall N-S trending normal fault with dip direction ± W paralleling a set of ± E dipping normal faults in the west, forming Stockstadt-Obernburg and Klingenberg Grabens.
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_985
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Stockstadt-Obernburg Graben Eastern Flank
type: Fault
type: Limit
type: Concept
created: 2021-03-16T09:56:26.893Z
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
notation: DE-BY_1575
definition: NNW-SSE to NNE-SSW trending, steeply WSW to WNW dipping normal fault forming the western scarp of Spessart mountains and the eastern boundary of Stockstadt-Obernburg Graben with main movement phases during Oligocene and Pliocene.
preferred label: Stockstadt-Obernburg Graben Ostflanke @de
alternative label: Obernauer Randverwerfung @de
references: https://data.geoscience.earth/ncl/geoera/ref/8471
references: https://data.geoscience.earth/ncl/geoera/ref/7320
references: https://data.geoscience.earth/ncl/geoera/ref/8474
sf touches: Hahnenkamm Scarp
sf touches: Eichelsbach Fault
sf touches: Klingenberg-Graben
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1575
limit type: normalFault
broader: Spessart-Odenwald Borderfault System

Klingenberg-Graben
type: Fault
type: Limit
scope note: Überarbeitetes Konzept von 2021-03-15, nach HIKE Redaktionsschluss. Die entsprechenden Störungs-Geometrien in der HIKE Störungsdatenbank wurden nicht angepasst. @de
scope note: Revised concept as of 2021-03-15, after the HIKE editorial deadline. Corresponding fault geometries in the HIKE Fault Data Base not adjusted accordingly.
type: Concept
created: 2021-01-25T14:23:22.771Z
notation: DE-BY_1022
definition: Paar NW-SE streichender Abschiebungen mit Einfallsrichtung zum Grabeninneren. @de
definition: Pair of NW-SE trending normal faults with a inward graben dip.
references: https://data.geoscience.earth/ncl/geoera/ref/7292
sf touches: Schippach Fault
sf touches: Laudenbach Fault
sf touches: Stockstadt-Obernburg Graben Eastern Flank
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1022
limit type: normalFault
broader: Spessart-Odenwald Borderfault System

Stockstadt-Obernburg Graben Western Flank
type: Fault
type: Limit
type: Concept
created: 2021-03-16T09:56:26.905Z
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
notation: DE-BY_1565
definition: NNW-SSE to NNE-SSW trending, steeply ENE to ESE dipping normal fault featuring a throw of up to 150 m; western boundary of Stockstadt-Obernburg Graben with main movement phases during Oligocene and Pliocene.
preferred label: Stockstadt-Obernburg Graben Westflanke @de
alternative label: Randverwerfung Obernburg-Großostheim @de
references: https://data.geoscience.earth/ncl/geoera/ref/8474
references: https://data.geoscience.earth/ncl/geoera/ref/7320
sf touches: Ringheim-Eisenbach Fault
sf touches: Kahl-Kleinostheim Fault
sf touches: Karlstein-Langstadt Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1565
limit type: normalFault
broader: Spessart-Odenwald Borderfault System

Stockstadt-Obernburg Graben Fault
type: Fault
type: Limit
type: Concept
created: 2021-03-16T09:56:26.902Z
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
notation: DE-BY_1574
definition: NNW-SSE trending fault running within Stockstadt-Obernburg Graben.
preferred label: Stockstadt-Obernburg Graben-Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/8474
sf touches: Karlstein-Langstadt Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1574
broader: Spessart-Odenwald Borderfault System

Spessart Borderfault
type: Fault
type: Limit
scope note: Überarbeitetes Konzept von 2021-03-15, nach HIKE Redaktionsschluss. Die entsprechenden Störungs-Geometrien in der HIKE Störungsdatenbank wurden nicht angepasst. @de
scope note: Revised concept as of 2021-03-15, after the HIKE editorial deadline. Corresponding fault geometries in the HIKE Fault Data Base not adjusted accordingly. @de
narrower: Michelbach Thrust
narrower: Hahnenkamm Scarp
narrower: Anterior Spessart western boundary
narrower: Wilmundsheim Graben eastern boundary
type: Concept
created: 2021-01-25T14:23:23.492Z
preferred label: Spessartrand Störung @de
notation: DE-BY_984
definition: Insgesamt N-S streichendes System W fallender Abschiebung, bildet im nördlichen Abschnitt die Ostgrenze der Hanau-Seligenstädter Senke. @de
definition: Overall N-S trending system of normal faults with dip direction W, in the northern part eastern boundary of Hanau-Seligenstadt Basin.
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_984
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Anterior Spessart western boundary
type: Fault
type: Limit
type: Concept
created: 2021-03-16T09:56:26.886Z
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
notation: DE-BY_1557
definition: N-S trending, veering to NNW-SSE in the south, main step of the Spessart Borderfault towards the Hanau-Seligenstadt Basin; continuing as Stockstadt-Obernburg Graben Eastern Flank [DE-BY_1575] in the south.
preferred label: Vorspessart Randstörung @de
alternative label: Spessartrandverwerfung @de
alternative label: Spessartrandbruch @de
references: https://data.geoscience.earth/ncl/geoera/ref/8474
references: https://data.geoscience.earth/ncl/geoera/ref/7320
references: https://data.geoscience.earth/ncl/geoera/ref/8472
references: https://data.geoscience.earth/ncl/geoera/ref/8473
sf touches: Hahnenkamm Scarp
sf touches: Wilmundsheim Graben eastern boundary
sf touches: Erlensee-Alzenau Fault
sf touches: Kahl-Kleinostheim Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1557
limit type: normalFault
broader: Spessart Borderfault

Hahnenkamm Scarp
type: Fault
type: Limit
type: Concept
created: 2021-03-16T09:56:26.882Z
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
notation: DE-BY_1556
definition: N-S trending eastern branch of the Anterior Spessart western boundary.
preferred label: Hahnenkamm Westabbruch @de
references: https://data.geoscience.earth/ncl/geoera/ref/8473
references: https://data.geoscience.earth/ncl/geoera/ref/8472
references: https://data.geoscience.earth/ncl/geoera/ref/7320
references: https://data.geoscience.earth/ncl/geoera/ref/8474
sf touches: Michelbach Thrust
sf touches: Anterior Spessart western boundary
sf touches: Erlensee-Alzenau Fault
sf touches: Stockstadt-Obernburg Graben Eastern Flank
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1556
limit type: normalFault
broader: Spessart Borderfault

Michelbach Thrust
limit type: thrustFault
type: Fault
type: Limit
type: Concept
created: 2021-03-16T09:56:26.878Z
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
notation: DE-BY_1549
definition: SW-NE striking, approx. 60° SE dipping thrust fault running from Wasserlos to Freigericht in Hesse; in sections northwestern boundary of Anterior Spessart basement swell.
preferred label: Michelbach Überschiebung @de
references: https://data.geoscience.earth/ncl/geoera/ref/8473
references: https://data.geoscience.earth/ncl/geoera/ref/8472
references: https://data.geoscience.earth/ncl/geoera/ref/7320
references: https://data.geoscience.earth/ncl/geoera/ref/8474
sf touches: Hahnenkamm Scarp
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1549
broader: Spessart Borderfault

Weiden Basin western margin
creator: schmar
created: 2021-08-23T07:26:53.965Z
type: Concept
in scheme: Tectonic Boundary Objects in Europe
in scheme: GC3D limits
notation: LfU-BY_9915
type: Limit
type: https://data.geoscience.earth/ncl/geoera/geoconnect3d/category/9754
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11573
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11887
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11694
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11693
preferred label: Westrand des Weidener Beckens @de
definition: Western boundary of Weiden Basin, in its north towards the adjoining, buried and desintegrated remnants of Naab Basin Rotliegend deposits. Consisting of segments of, from N to S, Weidenberg Fault [LfU-BY_959], Birk-Stegenthumbach Fault [LfU-BY_1042], Fenkensees-Brüderes Fault [LfU-BY_1049] and the Freihung Fault System [LfU-BY_1388], plus an link between the faults, assumed due to the lack of borehole or seismic evidence.
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7343
references: https://data.geoscience.earth/ncl/geoera/ref/7375
type: Fault
narrower: Weidenberg Fault
narrower: Fenkensses-Brüderes Fault
narrower: Birk-Stegenthumbach Fault
narrower: Freihung Fault System
broader: Schichtstufenland Domäne (N und NW Bayern)

Fenkensses-Brüderes Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.023Z
preferred label: Fenkensses-Brüderes Störung @de
notation: DE-BY_1049
definition: N-S streichende Abschiebung mit Einfallrichtung E @de
definition: N-S trending normal fault with dip direction E
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
sf touches: Eisfeld-Kulmbach Fault Zone Segment 2
sf touches: Weidenberg Fault
in scheme: Tectonic Boundary Objects in Europe
in scheme: GC3D limits
notation: LfU-BY_1049
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)
broader: Weiden Basin western margin

Birk-Stegenthumbach Fault
limit type: reverseFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:21.662Z
preferred label: Birk-Stegenthumbach Störung @de
notation: DE-BY_1042
alternative label: Stegenthumbacher Störung @de
definition: NNW-SSE streichende Abschiebung mit Einfallrichtung WSW (später aufschiebend invertiert) @de
definition: NNW-SSE trending normal fault with dip direction WSW (later reversly inverted)
references: https://data.geoscience.earth/ncl/geoera/ref/7356
references: https://data.geoscience.earth/ncl/geoera/ref/7293
references: https://data.geoscience.earth/ncl/geoera/ref/7343
references: https://data.geoscience.earth/ncl/geoera/ref/7292
references: https://data.geoscience.earth/ncl/geoera/ref/6372
in scheme: Tectonic Boundary Objects in Europe
in scheme: GC3D limits
notation: LfU-BY_1042
broader: Schichtstufenland Domäne (N und NW Bayern)
broader: Weiden Basin western margin

Freihung Fault System
limit type: reverseFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:24.050Z
preferred label: Freihunger Störungssystem @de
notation: DE-BY_1388
alternative label: Freihunger Störungszone @de
definition: Von Kirchenthumbach bis zur Luhe Line [DE-BY_1387] bei Ehenfeld ziehende, NW-SE verlaufende, steil nach NE einfallendes Aufschiebungs-System mit einer (kumulativen) Sprunghöhe von bis zu mehr als 1,2 km. Mehrfach von Querstörungen versetzt und streckenweise als einzelne Groß-Aufschiebung ausgebildet. Im südlichen Abschnitt SW-Grenze der Weidener Bucht mit Rotliegend Ablagerungen. @de
definition: Running from Kirchenthumbach to Luhe Line [DE-BY_1387] near Ehenfeld, NW-SE trending, steeply NE dipping system of reverse faults with a cumulative throw up to more than 1.2 km, in parts merging into one single reverse fault and offset by lateral faults. In its southern part, southwestern boundary of Weidener Bucht (Weiden embayment) of exposed/subcropping Rotliegend deposits.
narrower: Freihung Fault
narrower: Elbart Subfault
narrower: Tanzfleck Fault
narrower: Glosenrangen Cross Fault
narrower: Zissenhof-Pappenberg Fault
narrower: Kirchenthumbach-Pappenberg Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/7367
references: https://data.geoscience.earth/ncl/geoera/ref/7368
references: https://data.geoscience.earth/ncl/geoera/ref/7267
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7343
in scheme: Tectonic Boundary Objects in Europe
in scheme: GC3D limits
notation: LfU-BY_1388
broader: Weiden Basin western margin
broader: Schichtstufenland Domäne (N und NW Bayern)

Tanzfleck Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:24.160Z
preferred label: Tanzfleck Störung @de
notation: DE-BY_1390
definition: Gewellt NW-SE verlaufende ca. 75° nach NE einfallende listrische Aufschiebung mit einen Vertikalversatz von etwa 400 m. Die Tanzfleck Störung zeigt eine ausgeprägte Abwärtsschleppung der Schichten der Liegendscholle, was eine zeitweise abschiebende Invertierung andeutet. @de
definition: Undulate NW-SE trending approx. 75° NE dipping listric reverse fault with a throw of about 400 m and featuring a pronounced downward drag of strata in the food wall down block, implying a normal inversion at times.
references: https://data.geoscience.earth/ncl/geoera/ref/7368
sf touches: Freihung cross-faults
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1390
broader: Freihung Fault System

Elbart Subfault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:24.133Z
preferred label: Elbart Nebenstörung @de
notation: DE-BY_1389
definition: Gewellt, ingesamt N-S verlaufende Nebenstörung zwischen der Freihung Störung [DE-BY_990] im Westen und der Tanzfleck Störung [DE-BY_1390] im Osten. @de
definition: Undulate, overall N-S trending subfault in between Freihung Fault [DE-BY_990] to the west and Tanzfleck Fault [DE-BY_1390] to the east.
references: https://data.geoscience.earth/ncl/geoera/ref/7367
references: https://data.geoscience.earth/ncl/geoera/ref/7368
references: https://data.geoscience.earth/ncl/geoera/ref/7267
sf touches: Freihung Fault
sf touches: Freihung cross-faults
sf touches: Tanzfleck Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1389
broader: Freihung Fault System

Freihung Fault
limit type: reverseFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:24.078Z
preferred label: Freihunger Störung @de
notation: DE-BY_990
alternative label: Freihunger Überschiebung @de
definition: NNW-SSE verlaufende Hauptstörung der Freihunger Störungszone [DE-BY_1388]. Steil nach NE einfallende Aufschiebung mit einer Sprunghöhe von bis zu 1,2 km, mehrfach von Querstörungen versetzt. @de
definition: NNW-SSE trending principal fault of Freihung Fault System [DE-BY_1388]. Steeply NE dipping reverse fault with a throw up to 1.2 km, repeatedly displaced by lateral faults.
narrower: Freihung cross-faults
references: https://data.geoscience.earth/ncl/geoera/ref/7367
references: https://data.geoscience.earth/ncl/geoera/ref/7368
references: https://data.geoscience.earth/ncl/geoera/ref/7267
sf touches: Kindlas Fault
sf touches: Birk-Stegenthumbach Fault
sf touches: Freihung cross-faults
sf touches: Elbart Subfault
sf touches: Glosenrangen Cross Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_990
broader: Freihung Fault System

Freihung cross-faults
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:24.105Z
preferred label: Freihunger Querstörungen @de
notation: DE-BY_1395
definition: SW-NE bis W-E streichende, saigere bis subvertikale Störungen die die Freihung Störung [DE-BY_990] und Elbart Nebenstörung [DE-BY_1389] versetzen und abschnittsweise zusammenführen. @de
definition: SW-NE to W-E striking, vertical to subvertical faults displacing Freihung Fault [DE-BY_990] and Elbart Subfault [DE-BY_1389] and merging them in sections.
references: https://data.geoscience.earth/ncl/geoera/ref/7368
sf touches: Freihung Fault
sf touches: Elbart Subfault
sf touches: Tanzfleck Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1395
broader: Freihung Fault

Kirchenthumbach-Pappenberg Fault Zone
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:24.242Z
preferred label: Kirchenthumbach-Pappenberg Störungszone @de
notation: DE-BY_1393
definition: Südliche Fortsetzung der Creußen Störung [DE-BY_961]. NNW-SSE streichendes Abschiebungssystem mit Einfallrichtung ENE, durch Querstörungen gegliedert @de
definition: Southern continuation of Creussen Fault [DE-BY_961]. NNW-SSE trending normal fault system with dip direction ENE, structured by transverse faults.
references: https://data.geoscience.earth/ncl/geoera/ref/7345
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1393
broader: Freihung Fault System

Zissenhof-Pappenberg Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:24.214Z
preferred label: Zißenhof-Pappenberg- Störung @de
notation: DE-BY_1392
definition: NNW-SSE verlaufende, steil nach NE einfallende Abschiebung mit einem Vertikalversatz von ca. 100 m. @de
definition: NNW-SSE trending, steeply NE dipping normal fault featuring a throw of about 100 m.
references: https://data.geoscience.earth/ncl/geoera/ref/7345
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1392
broader: Freihung Fault System

Glosenrangen Cross Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:24.187Z
preferred label: Glosenrangen Querstörung @de
notation: DE-BY_1391
definition: W-E bis SW-NE verlaufender Querbruch (Durchbruch) einer Akkommodationszone (breached relay ramp) im Überlappungsbereich der Zißenhof-Pappenberg Störung [DE-BY_1392] und Freihung Störung [DE-BY_990]. @de
definition: W-E to SW-NE trending connecting fault of a breached relay ramp as the overlap bridging between Freihung Fault [DE-BY_990] and Zissenhof-Pappenberg Fault [DE-BY_1392].
references: https://data.geoscience.earth/ncl/geoera/ref/7345
sf touches: Pegnitz Fault
sf touches: Freihung Fault
sf touches: Zissenhof-Pappenberg Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1391
broader: Freihung Fault System

Weidenberg Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.883Z
preferred label: Weidenberg Störung @de
notation: DE-BY_959
alternative label: Weidenberger Störung @de
definition: NW-SE streichende Ab- bzw. Steitenverschiebung mit Einfallrichtung NE @de
definition: NW-SE trending normal/strike-slip fault with dip direction NE
references: https://data.geoscience.earth/ncl/geoera/ref/7283
references: https://data.geoscience.earth/ncl/geoera/ref/7292
sf touches: Fenkensses-Brüderes Fault
sf touches: Kemnath-Waldeck Fault
sf touches: Tiefenthal Fault
in scheme: Tectonic Boundary Objects in Europe
in scheme: GC3D limits
notation: LfU-BY_959
broader: Weiden Basin western margin
broader: Schichtstufenland Domäne (N und NW Bayern)

Singenrain Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.464Z
preferred label: Singenrain Störung @de
notation: DE-BY_1012
definition: N-S streichende Abschiebung mit Einfallrichtung W @de
definition: N-S trending normal fault with dip direction W
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1012
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Sesslach Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.436Z
preferred label: Sesslach Störung @de
notation: DE-BY_996
definition: NNW-SSE streichende Abschiebung mit Einfallrichtung ENE @de
definition: NNW-SSE trending normal fault with dip direction ENE
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_996
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Sennfeld-Weyer Fault Zone
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.408Z
preferred label: Sennfeld-Weyer Störungszone @de
notation: DE-BY_1031
definition: NW-SE streichende Abschiebung mit Einfallrichtung SW @de
definition: NW-SE trending normal fault with dip direction SW
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1031
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Seligenstadt-Brück Fault Zone
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.381Z
preferred label: Seligenstadt-Brück Störungszone @de
notation: DE-BY_1018
definition: NW-SE streichende Abschiebung mit Einfallrichtung SW @de
definition: NW-SE trending normal fault with dip direction SW
references: https://data.geoscience.earth/ncl/geoera/ref/7269
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1018
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Seifriedsburg Fault Zone
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.352Z
preferred label: Seifriedsburg Störungszone @de
notation: DE-BY_1017
definition: NW-SE streichende Abschiebung (Graben mit dextraler Seitenverschiebung? ) @de
definition: NW-SE trending normal fault (graben with dextral strike-slip?)
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1017
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Hollfeld Fault Zone
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.410Z
preferred label: Hollfelder Störungszone @de
notation: DE-BY_1043
definition: NW-SE streichende Abschiebung mit Einfallrichtung SW (später revers invertiert), Nordost-Grenze der Frankenalb Furche. @de
definition: NW-SE trending normal fault with dip direction SW (later reversly inverted), northeastern boundary of Frankenalb trough.
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
references: https://data.geoscience.earth/ncl/geoera/ref/6372
sf touches: Ahorntal-Anticline Fault
sf touches: Hainbach Fault
sf touches: Pegnitz Fault
in scheme: Tectonic Boundary Objects in Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11692
notation: LfU-BY_1043
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Schippach Fault
type: Fault
type: Limit
narrower: Schippach Graben Western Flank
alternative label: Schippacher Sprung @de
scope note: Revised concept as of 2021-03-15, after the HIKE editorial deadline. Corresponding fault geometries in the HIKE Fault Data Base not adjusted accordingly.
scope note: Überarbeitetes Konzept von 2021-03-15, nach HIKE Redaktionsschluss. Die entsprechenden Störungs-Geometrien in der HIKE Störungsdatenbank wurden nicht angepasst. @de
references: https://data.geoscience.earth/ncl/geoera/ref/8471
references: https://data.geoscience.earth/ncl/geoera/ref/7320
references: https://data.geoscience.earth/ncl/geoera/ref/8472
type: Concept
created: 2021-01-25T14:23:23.325Z
preferred label: Schippach Störung @de
notation: DE-BY_1021
definition: N-S streichende, steil nach W einfallende Abschiebung mit einer Sprunghöhe von ca. 220 m; Ostflanke des Schippacher Grabens. @de
definition: N-S trending, steeply W dipping normal fault wit a throw of about 220 m; eastern flank of Schippach Graben.
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
sf touches: Klingenberg-Graben
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1021
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Schippach Graben Western Flank
type: Fault
type: Limit
created: 2021-03-16T09:42:26.709Z
type: Concept
notation: DE-BY_1576
preferred label: Schippacher Graben Westflanke @de
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
definition: N-S trending, steeply E dipping normal fault wit a throw of about 150 m; western flank of Schippach Graben.
definition: N-S streichende, steil nach E einfallende Abschiebung mit einer Sprunghöhe von ca. 150 m; Westflanke des Schippacher Grabens. @de
references: https://data.geoscience.earth/ncl/geoera/ref/8472
references: https://data.geoscience.earth/ncl/geoera/ref/8471
references: https://data.geoscience.earth/ncl/geoera/ref/7320
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1576
limit type: normalFault
broader: Schippach Fault

Heustreu Fault Zone
limit type: strikeSlipFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.383Z
preferred label: Heustreuer Störungszone @de
notation: DE-BY_1047
definition: NW-SE streichende dextrale Seitenverschiebung @de
definition: NW-SE trending dextral strike-slip fault
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1047
broader: Schichtstufenland Domäne (N und NW Bayern)

Rodach Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.297Z
preferred label: Rodach Störung @de
notation: DE-BY_994
definition: SW-NE streichende Abschiebung mit Einfallrichtung SE @de
definition: SW-NE trending normal fault with dip direction SE
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_994
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Eltersdorf-Röthenbach-Weigenhofen Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.355Z
preferred label: Eltersdorf-Röthenbach-Weigenhofen Störung @de
notation: DE-BY_1533
definition: Insgesamt WNE-ESE verlaufende, steil nach NNE einfallende Abschiebung mit einer Sprunghöhe bis zu 40 m. @de
definition: Overall WNW-ESE trending, steeply NNE dipping normal fault featuring a throw of up to 40 m.
references: https://data.geoscience.earth/ncl/geoera/ref/7299
references: https://data.geoscience.earth/ncl/geoera/ref/7371
references: https://data.geoscience.earth/ncl/geoera/ref/7271
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1533
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Rodenbach-Duttenbrunn Fault Zone
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.269Z
preferred label: Rodenbach-Duttenbrunn Störungszone @de
notation: DE-BY_982
definition: SW-NE streichende Abschiebung mit Einfallrichtung SE (Graben) @de
definition: SW-NE trending normal fault with dip direction SE (graben)
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_982
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Eschlipper Tal Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:21.995Z
preferred label: Eschlipper Tal Störung @de
notation: DE-BY_1059
definition: NW-SE streichende Abschiebung mit Einfallrichtung NE @de
definition: NW-SE trending normal fault with dip direction NE
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
references: https://data.geoscience.earth/ncl/geoera/ref/6372
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1059
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Eisfeld-Kulmbach Fault Zone
limit type: strikeSlipFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:21.911Z
preferred label: Eisfeld-Kulmbach Störungszone @de
notation: DE-BY_1376
definition: NW-SE streichende Seitenverschiebung mit Einfallrichtung NE (revers aufschiebend invertiert, max. Versatz von 900 m) @de
definition: NW-SE trending strike-slip fault with dip direction NE (reversly inverted, max. displacement of 900 m)
narrower: Eisfeld-Kulmbach Fault Zone Segment 1
narrower: Eisfeld-Kulmbach Fault Zone Segment 2
references: https://data.geoscience.earth/ncl/geoera/ref/6372
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1376
broader: Schichtstufenland Domäne (N und NW Bayern)

Eisfeld-Kulmbach Fault Zone Segment 2
limit type: reverseFault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/7682
type: Concept
created: 2021-01-25T14:23:21.966Z
preferred label: Eisfeld-Kulmbach Störungszone Segment 2 @de
notation: DE-BY_956
definition: NW-SE streichende Aufschiebung mit Einfallrichtung NE (max. Versatz von 900 m) @de
definition: NW-SE trending reverse fault with dip direction NE (max. displacement of 900 m)
hidden label: Culmbacher Spalte @de
references: https://data.geoscience.earth/ncl/geoera/ref/6372
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
references: https://data.geoscience.earth/ncl/geoera/ref/7678
sf touches: Asslitz-Saas Fault
sf touches: Creussen Fault
sf touches: Eisfeld-Kulmbach Fault Zone Segment 1
sf touches: Fenkensses-Brüderes Fault
sf touches: Kronach Fault
sf touches: Kümmelberg Fault
sf touches: Mitwitz Fault
sf touches: Rodach Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_956
broader: Eisfeld-Kulmbach Fault Zone

Eisfeld-Kulmbach Fault Zone Segment 1
limit type: strikeSlipFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:21.939Z
preferred label: Eisfeld-Kulmbach Störungszone Segment 1 @de
notation: DE-BY_1000
definition: NW-SE streichende Seitenverschiebung mit Einfallrichtung NE (revers invertiert) @de
definition: NW-SE trending strike-slip fault with dip direction NE (reversly inverted)
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
references: https://data.geoscience.earth/ncl/geoera/ref/6372
sf touches: Asslitz-Saas Fault
sf touches: Eisfeld-Kulmbach Fault Zone Segment 2
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1000
broader: Eisfeld-Kulmbach Fault Zone

Eichelsbach Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:21.883Z
preferred label: Eichelsbach Störung @de
notation: DE-BY_1003
definition: WNW-ESE streichende Abschiebung mit Einfallrichtung SSW @de
definition: WNW-ESE trending normal fault with dip direction SSW
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1003
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Bamberg-Neuses Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.242Z
preferred label: Bamberg-Neuses Störung @de
notation: DE-BY_1060
definition: NW-SE streichende dextrale Abschiebung mit Einfallrichtung NE @de
definition: NW-SE trending normal or dextral strike slipe fault with dip direction NE
references: https://data.geoscience.earth/ncl/geoera/ref/7292
references: https://data.geoscience.earth/ncl/geoera/ref/6372
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1060
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Regnitz Valley Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.214Z
preferred label: Regnitztal Störung @de
notation: DE-BY_971
definition: Gewellt N-S bis NNW-SSE verlaufende Abschiebung mit Einfallrichtung E @de
definition: Undulate N-S to NNW-SSE trending normal fault with dip direction E
references: https://data.geoscience.earth/ncl/geoera/ref/7271
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_971
broader: Schichtstufenland Domäne (N und NW Bayern)

Pegnitz Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.186Z
preferred label: Pegnitz Störung @de
notation: DE-BY_1045
definition: NW-SE streichende dextrale Steitenverschiebung @de
definition: NW-SE trending dextral strike-slip fault
references: https://data.geoscience.earth/ncl/geoera/ref/7292
references: https://data.geoscience.earth/ncl/geoera/ref/6372
sf touches: Hollfeld Fault Zone
sf touches: Staffelstein Fault Zone
sf touches: Glosenrangen Cross Fault
sf touches: Zissenhof-Pappenberg Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1045
broader: Schichtstufenland Domäne (N und NW Bayern)

Pautzfeld Fault Zone
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.159Z
preferred label: Pautzfeld Störungszone @de
notation: DE-BY_1027
definition: N-S streichende Abschiebung mit Einfallrichtung N @de
definition: N-S trending normal fault with dip direction N
references: https://data.geoscience.earth/ncl/geoera/ref/6372
references: https://data.geoscience.earth/ncl/geoera/ref/7292
sf touches: Bamberg-Neuses Fault Zone
sf touches: Ehrenbach Fault
sf touches: Bamberg-Neuses Fault
sf touches: Wiesenttal Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1027
broader: Schichtstufenland Domäne (N und NW Bayern)

Oberkatz Fault Zone
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.131Z
preferred label: Oberkatz Störungszone @de
notation: DE-BY_1014
definition: N-S streichende Abschiebung mit Einfallrichtung W (Graben) @de
definition: N-S trending normal fault with dip direction W (graben)
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
sf touches: Heustreu Fault Zone
sf touches: Stetten Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1014
broader: Schichtstufenland Domäne (N und NW Bayern)

Nordheim Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.103Z
preferred label: Nordheim Störung @de
notation: DE-BY_1028
definition: NW-SE streichende Aufschiebung mit Einfallrichtung NE @de
definition: NW-SE trending reverse fault with dip direction NE
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1028
broader: Schichtstufenland Domäne (N und NW Bayern)

Neuhütten Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.076Z
preferred label: Neuhütten Störung @de
notation: DE-BY_981
definition: NW-SE streichende Abschiebung mit Einfallrichtung NE @de
definition: NW-SE trending normal fault with dip direction NE
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_981
broader: Schichtstufenland Domäne (N und NW Bayern)

Hafenprepach Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.133Z
preferred label: Hafenprepach Störung @de
notation: DE-BY_963
definition: WNW-ESE streichende Abschiebung mit Einfallrichtung SSW @de
definition: WNW-ESE trending normal fault with dip direction SSW
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
references: https://data.geoscience.earth/ncl/geoera/ref/6372
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_963
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Muggenbach Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.048Z
preferred label: Muggenbach Störung @de
notation: DE-BY_1044
definition: N-S streichende Ab- bzw. Steitenverschiebung mit Einfallrichtung E @de
definition: N-S trending normal/strike-slip fault with dip direction E
references: https://data.geoscience.earth/ncl/geoera/ref/6372
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1044
broader: Schichtstufenland Domäne (N und NW Bayern)

Grettstadt-Aschbach Fault Zone
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.106Z
preferred label: Grettstadt-Aschbach Störungszone @de
notation: DE-BY_977
definition: NW-SE streichende Abschiebung mit Einfallrichtung SW (dextral seitenverschiebend?) @de
definition: NW-SE trending normal fault with dip direction SW (dextral strike-slip?)
references: https://data.geoscience.earth/ncl/geoera/ref/7354
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_977
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Motten Fault Zone
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.020Z
preferred label: Motten Störungszone @de
notation: DE-BY_1048
definition: NW-SE streichende Abschiebung (Graben) @de
definition: NW-SE trending normal fault (graben)
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1048
broader: Schichtstufenland Domäne (N und NW Bayern)

Gräfenberg Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.078Z
preferred label: Gräfenberg Störung @de
notation: DE-BY_1007
definition: N-S streichende Abschiebung mit Einfallrichtung E @de
definition: N-S trending normal fault with dip direction E
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1007
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Mönchberg Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.993Z
preferred label: Mönchberg Störung @de
notation: DE-BY_974
definition: SSW-NNE streichende sinistrale Steitenverschiebung mit Einfallrichtung WNW (100-320 m Versatz) @de
definition: SSW-NNE trending sinistral strike-slip fault with dip direction WNW (100-320 m displacement)
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_974
broader: Schichtstufenland Domäne (N und NW Bayern)

Freiberg-Döringstadt Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.050Z
preferred label: Freiberg-Döringstadt Störung @de
notation: DE-BY_992
definition: NW-SE streichende Abschiebung mit Einfallrichtung NE @de
definition: NW-SE trending normal fault with dip direction NE
references: https://data.geoscience.earth/ncl/geoera/ref/6372
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_992
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Breitenbuch Fault Zone
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:21.717Z
preferred label: Breitenbuch Störungszone @de
notation: DE-BY_1030
definition: N-S streichende Abschiebung mit Einfallrichtung W @de
definition: N-S trending normal fault with dip direction W
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1030
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Bischofsheim Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:21.689Z
preferred label: Bischofsheim Störung @de
notation: DE-BY_1010
definition: WNW-ESE streichende Abschiebung mit Einfallrichtung NNE @de
definition: WNW-ESE trending normal fault with dip direction NNE
references: https://data.geoscience.earth/ncl/geoera/ref/7291
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1010
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Bieber Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:21.634Z
preferred label: Bieber Störung @de
notation: DE-BY_978
definition: WNW-ESE streichende Abschiebung mit Einfallrichtung SSW @de
definition: WNW-ESE trending normal fault with dip direction SSW
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_978
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Baunachtal Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:21.606Z
preferred label: Baunachtal Störung @de
notation: DE-BY_991
definition: NNW-SSE streichende Abschiebung mit Einfallrichtung ENE (seitenverschiebend?) @de
definition: NNW-SSE trending normal fault with dip direction ENE (strike-slip?)
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_991
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Mitwitz Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.965Z
preferred label: Mitwitz Störung @de
notation: DE-BY_998
definition: NW-SE streichende Ab- oder Aufschiebung mit Einfallrichtung SW oder NE @de
definition: NW-SE trending normal or reverse fault with dip direction SW or NE
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_998
broader: Schichtstufenland Domäne (N und NW Bayern)

Lindelbach-Erlach Fault Zone
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.938Z
preferred label: Lindelbach-Erlach Störungszone @de
notation: DE-BY_1020
definition: WNW-ESE streichende Abschiebung mit Einfallrichtung NNE @de
definition: WNW-ESE trending normal fault with dip direction NNE
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1020
broader: Schichtstufenland Domäne (N und NW Bayern)

Lichtenfels Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.910Z
preferred label: Lichtenfels Störung @de
notation: DE-BY_962
definition: NW-SE streichende Abschiebung mit Einfallrichtung SW (später zu Aufschiebung invertiert) @de
definition: NW-SE trending normal fault with dip direction SW (later reversly inverted)
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_962
broader: Schichtstufenland Domäne (N und NW Bayern)

Leidersbach-Hobbach Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.882Z
preferred label: Leidersbach-Hobbach Störung @de
notation: DE-BY_1005
definition: NNW-SSE streichende Abschiebung mit Einfallrichtung WSW @de
definition: NNW-SSE trending normal fault with dip direction WSW
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1005
broader: Schichtstufenland Domäne (N und NW Bayern)

Laudenbach Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.854Z
preferred label: Laudenbach Störung @de
notation: DE-BY_1023
definition: N-S streichende Abschiebung mit Einfallrichtung E @de
definition: N-S trending normal fault with dip direction E
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1023
broader: Schichtstufenland Domäne (N und NW Bayern)

Kümmelberg Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.827Z
preferred label: Kümmelberg Störung @de
notation: DE-BY_995
definition: NW-SE streichende Abschiebung mit Einfallrichtung SW @de
definition: NW-SE trending normal fault with dip direction SW
references: https://data.geoscience.earth/ncl/geoera/ref/6372
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_995
broader: Schichtstufenland Domäne (N und NW Bayern)

Kronach Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.799Z
preferred label: Kronach Störung @de
notation: DE-BY_993
alternative label: Kronacher Verwerfung @de
definition: SW-NE streichende Abschiebung mit Einfallrichtung SE; versetzt die Leuschberg-Rennesberg Störungen [DE-BY_1477] und Letzenhof Störung [DE-BY_1430] ab und endet am Frankenwald-Randbruch [DE-BY_1431]. @de
definition: SW-NE trending normal fault with dip direction SE; offsets Leuschberg-Rennesberg Faults [DE-BY_1477] and Letzenhof Fault [DE-BY_1430] and truncated at Franconian Forest Scarp [DE-BY_1431].
references: https://data.geoscience.earth/ncl/geoera/ref/6372
references: https://data.geoscience.earth/ncl/geoera/ref/7282
references: https://data.geoscience.earth/ncl/geoera/ref/7292
references: https://data.geoscience.earth/ncl/geoera/ref/7678
sf touches: Luhe Fault
sf touches: Franconian Forest Scarp
sf touches: Leuschberg-Rennesberg Faults
sf touches: Letzenhof Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_993
broader: Schichtstufenland Domäne (N und NW Bayern)

Ehrenbach Fault
type: Limit
type: Fault
type: Concept
created: 2021-01-25T14:23:21.856Z
preferred label: Ehrenbach Störung @de
notation: DE-BY_969
definition: NW-SE streichende Abschiebung mit Einfallrichtung NE @de
definition: NW-SE trending normal fault with dip direction NE
references: https://data.geoscience.earth/ncl/geoera/ref/7327
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
references: https://data.geoscience.earth/ncl/geoera/ref/6372
sf touches: Hersbruck Fault
sf touches: Pautzfeld Fault Zone
sf touches: Wiesenttal Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_969
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Donnersdorf-Karbach Fault Zone
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:21.828Z
preferred label: Donnersdorf-Karbach Störungszone @de
notation: DE-BY_1029
definition: NW-SE streichende Abschiebung mit Einfallrichtung SW (dextral seitenverschiebend?) @de
definition: NW-SE trending normal fault with dip direction SW (dextral strike-slip?)
references: https://data.geoscience.earth/ncl/geoera/ref/7268
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1029
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Kist-Fuchsstadt Fault Zone
type: Limit
type: Fault
type: Concept
created: 2021-01-25T14:23:22.744Z
preferred label: Kist-Fuchsstadt Störungszone @de
notation: DE-BY_1008
definition: NW-SE streichende Aufschiebung mit Einfallrichtung NE (invertierter Graben?) @de
definition: NW-SE trending reverse fault with dip direction NE (inverted graben)
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1008
broader: Schichtstufenland Domäne (N und NW Bayern)

Creussen Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:21.800Z
preferred label: Creußen Störung @de
notation: DE-BY_961
definition: NNW-SSE streichende Abschiebung mit Einfallrichtung ENE @de
definition: NNW-SSE trending normal fault with dip direction ENE
references: https://data.geoscience.earth/ncl/geoera/ref/6372
references: https://data.geoscience.earth/ncl/geoera/ref/7293
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
sf touches: Eisfeld-Kulmbach Fault Zone Segment 2
sf touches: Zissenhof-Pappenberg Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_961
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Coburg Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:21.772Z
preferred label: Coburg Störung @de
notation: DE-BY_943
definition: NW-SE streichende Abschiebung mit Einfallrichtung SW @de
definition: NW-SE trending normal fault with dip direction SW
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_943
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Brücklein Fault Zone
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6372
type: Concept
created: 2021-01-25T14:23:21.745Z
preferred label: Brücklein Störungszone @de
notation: DE-BY_1032
definition: NW-SE streichende Abschiebung mit Einfallrichtung SW @de
definition: NW-SE trending normal fault with dip direction SW
references: https://data.geoscience.earth/ncl/geoera/ref/7349
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1032
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Ahorntal-Anticline Fault
limit type: strikeSlipFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:21.386Z
preferred label: Ahorntal-Antikline Störung @de
notation: DE-BY_1065
definition: SW-NE streichende sinistrale Seitenverschiebung @de
definition: SW-NE trending sinistral strike-slip fault
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1065
broader: Schichtstufenland Domäne (N und NW Bayern)

Bamberg-Neuses Fault Zone
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:21.579Z
preferred label: Bamberg-Neuses Störungszone @de
notation: DE-BY_1026
definition: NW-SE streichende dextrale Ab- und Seitenverschiebung mit Einfallrichtung NE @de
definition: NW-SE trending dextral normal fault with dip direction NE
references: https://data.geoscience.earth/ncl/geoera/ref/7268
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
references: https://data.geoscience.earth/ncl/geoera/ref/6372
sf touches: Itztal Fault
sf touches: Hassfurt-Bischberg Fault
sf touches: Wonfurt-Aurach Fault Zone
sf touches: Pautzfeld Fault Zone
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1026
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Bad Brückenau graben faults
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:21.551Z
preferred label: Bad Brückenauer Graben Störungen @de
notation: DE-BY_1009
definition: NNW-SSE streichende Abschiebung @de
definition: NNW-SSE trending normal fault
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1009
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Baad Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:21.524Z
preferred label: Baad Störung @de
notation: DE-BY_1061
definition: NW-SE streichende Abschiebung mit Einfallrichtung NW @de
definition: NW-SE trending normal fault with dip direction NW
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
references: https://data.geoscience.earth/ncl/geoera/ref/6372
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1061
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Auerbach Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:21.496Z
preferred label: Auerbach Störung @de
notation: DE-BY_1025
definition: SSW-NNE streichende Abschiebung mit Einfallrichtung WNW @de
definition: SSW-NNE trending normal fault with dip direction WNW
references: https://data.geoscience.earth/ncl/geoera/ref/7292
references: https://data.geoscience.earth/ncl/geoera/ref/6372
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1025
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Atzhausen-Kleinlangheim Fault Zone
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:21.468Z
preferred label: Atzhausen-Kleinlangheim Störungszone @de
notation: DE-BY_1019
definition: NW-SE streichende Abschiebung mit Einfallrichtung SW @de
definition: NW-SE trending normal fault with dip direction SW
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1019
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Asslitz-Saas Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:21.441Z
preferred label: Asslitz-Saas Störung @de
notation: DE-BY_960
definition: NW-SE streichende Abschiebung mit Einfallrichtung SW (Döllnitz-Jösleiner und Motschenbacher Störung, abschiebend einfallend nach SW, aufschiebend einfallend nach NE) @de
definition: NW-SE trending normal fault with dip direction SW (Döllnitz-Jösleiner and Motschenbacher Fault, normal dip SW or reverse dip NE)
references: https://data.geoscience.earth/ncl/geoera/ref/7349
references: https://data.geoscience.earth/ncl/geoera/ref/7372
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
references: https://data.geoscience.earth/ncl/geoera/ref/7682
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_960
broader: Schichtstufenland Domäne (N und NW Bayern)

Ruppersdorf-Moratneustetten Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:24.460Z
preferred label: Ruppersdorf-Moratneustettener Störung @de
notation: DE-BY_1446
definition: NW-SE (herzynisch) verlaufende, steil nach WSW einfallende Abschiebung mit einer Sprunghöhe bis zu ca. 40 m. @de
definition: NNW-SSE trending, steeply WSW dipping normal fault with a vertical offset up to approx. 40 m.
references: https://data.geoscience.earth/ncl/geoera/ref/7303
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1446
broader: Schichtstufenland Domäne (N und NW Bayern)

Ballstadt Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:24.432Z
preferred label: Ballstädter Störung @de
notation: DE-BY_1445
definition: WNW-ESE verlaufende, steil nach SSW einfallende Abschiebung mit einer Sprunghöhe bis über 30 m. @de
definition: WNW-ESE striking, steeply SSW dipping normal fault with a vertical offset up to more than 30 m.
references: https://data.geoscience.earth/ncl/geoera/ref/7303
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1445
broader: Schichtstufenland Domäne (N und NW Bayern)

Elpersdorf Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:24.405Z
preferred label: Elpersdorfer Störung @de
notation: DE-BY_1444
definition: NW-SE (herzynisch) verlaufende, steil nach SW einfallende Abschiebung mit einer Sprunghöhe bis zu 30 m. @de
definition: NW-SE trending, steeply SW dipping normal fault with a vertical offset up to 30 m.
references: https://data.geoscience.earth/ncl/geoera/ref/7302
sf touches: Frommetsfelden Fault
sf touches: Tiefenthal Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1444
broader: Schichtstufenland Domäne (N und NW Bayern)

Tiefenthal Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:24.378Z
preferred label: Tiefenthaler Verwerfung @de
notation: DE-BY_1443
definition: NW-SE (herzynisch) verlaufende, steil nach SW einfallende Abschiebung mit einer Sprunghöhe bis zu 30 m. @de
definition: NW-SE trending, steeply SW dipping normal fault with a throw up to 30 m.
references: https://data.geoscience.earth/ncl/geoera/ref/7304
sf touches: Frommetsfelden Fault
sf touches: Elpersdorf Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1443
broader: Schichtstufenland Domäne (N und NW Bayern)

Oberbessenbach-Heimbuchenthal Fault
type: Fault
type: Limit
type: Concept
created: 2021-03-16T09:56:26.989Z
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
notation: DE-BY_1569
definition: NW-SE trending, steeply SW dipping normal fault with a throw of up to 80 m.
preferred label: Oberbessenbach-Heimbuchenthal Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/8476
references: https://data.geoscience.earth/ncl/geoera/ref/8472
references: https://data.geoscience.earth/ncl/geoera/ref/8471
references: https://data.geoscience.earth/ncl/geoera/ref/7320
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1569
broader: Schichtstufenland Domäne (N und NW Bayern)

Soden-Oberwintersbach Fault
type: Fault
type: Limit
type: Concept
created: 2021-03-16T09:56:26.985Z
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
notation: DE-BY_1568
definition: NW-SE trending, steeply SW dipping normal fault with a throw of about 60 m.
preferred label: Soden-Oberwintersbach Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/8476
references: https://data.geoscience.earth/ncl/geoera/ref/8472
references: https://data.geoscience.earth/ncl/geoera/ref/8471
references: https://data.geoscience.earth/ncl/geoera/ref/7320
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1568
broader: Schichtstufenland Domäne (N und NW Bayern)

Schöllesberg Fault
type: Fault
type: Limit
type: Concept
created: 2021-03-16T09:56:26.982Z
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
notation: DE-BY_1567
definition: NW-SE striking, steeply SW dipping normal fault
preferred label: Schöllesberg Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/7320
sf touches: Mönchberg Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1567
broader: Schichtstufenland Domäne (N und NW Bayern)

Pisamberg-Hofstetten Fault
type: Fault
type: Limit
type: Concept
created: 2021-03-16T09:56:26.978Z
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
notation: DE-BY_1566
definition: NW-SE trending, steeply SW dipping normal fault featuring a throw of up to 80 m.
preferred label: Pisamberg-Hofstetten Störung @de
alternative label: Hofstettener Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/8472
references: https://data.geoscience.earth/ncl/geoera/ref/8471
references: https://data.geoscience.earth/ncl/geoera/ref/7320
sf touches: Eichelsbach Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1566
broader: Schichtstufenland Domäne (N und NW Bayern)

Baden Baden-Nuremberg-Erbendorf Line
type: Fault
type: Limit
alternative label: Tepla-Barrandium Suture
references: https://data.geoscience.earth/ncl/geoera/ref/7675
references: https://data.geoscience.earth/ncl/geoera/ref/8470
type: Concept
created: 2021-01-25T14:23:19.802Z
preferred label: Baden Baden-Nürnberg-Erbendorf Linie @de
notation: DE-BY_1547
alternative label: Tepla-Barrandium Sutur @de
definition: Das Grundgebirge im südlichen und mittleren Deutschland ist Teil des variszischen Kollisionsorogens, das Kossmat (1927) in stratigraphisch-lithologisch-tektonische Zonen gliederte, von Nord nach Süd, Rhenoherzynikum, Saxothuringikum und Moldanubikum. Die Sutur zwischen dem Moldanubikum und dem Saxothuringikum wird von der Baden Baden-Nürnberg-Erbendorf Linie (Reinhold 2005) markiert, die zwischen dem Schwarzwald und der Böhmischen Masse, überdeckt von der mächtigen Abfolge permo-mesozoischer Sedimente des Süddeutschen Schichtstufenlandes, nirgends direkt nachgewiesen ist. Ihr Verlauf ist aus geophysikalischen Vermessungen und wenigen tiefen Bohrungen abgeleitet. @de
definition: Kossmat (1927) subdivided the basement of the Variscan collision orogen in central and southern Germany in three stratigraphic-lithologic-tectonic zones, from north to south, Rhenohercynian, Saxothuringian, and Moldanubian Zones. In between the Black Forest in the west and the Bohemian Massif in the east the suture between the Saxothuringian and Moldanubian Zones, the Baden Baden-Nuremberg-Erbendorf Linie (Reinhold 2005), has not been evidenced directly as covered by a thick Permo-Mesozoic sedimentary sequence of the South German Scarpland. Its trend is inferred from geophysical surveys and few deep drillings.
references: https://data.geoscience.earth/ncl/geoera/ref/7324
references: https://data.geoscience.earth/ncl/geoera/ref/7346
in scheme: Tectonic Boundary Objects in Europe
broader: Schichtstufenland Domäne (N und NW Bayern)
broader: 3: Bohemian Massif domain

Hainberg-Kirchhöhe Fault
type: Fault
type: Limit
type: Concept
created: 2021-03-16T09:56:26.974Z
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
notation: DE-BY_1564
definition: NW-SE trending, steeply NE dipping normal fault.
preferred label: Hainberg-Kirchhöhe Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/8474
references: https://data.geoscience.earth/ncl/geoera/ref/7320
sf touches: Hainberg Cross-Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1564
broader: Schichtstufenland Domäne (N und NW Bayern)

Laufen-Autenberg Fault
type: Fault
type: Limit
type: Concept
created: 2021-03-16T09:56:26.970Z
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
notation: DE-BY_1552
definition: NW-SE trending, steeply SW dipping normal fault featuring a throw of up to 50 m.
preferred label: Laufen-Autenberg Störung @de
alternative label: Kehlrein-Kreuzberg Verwerfung @de
references: https://data.geoscience.earth/ncl/geoera/ref/8476
references: https://data.geoscience.earth/ncl/geoera/ref/8472
references: https://data.geoscience.earth/ncl/geoera/ref/7320
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1552
broader: Schichtstufenland Domäne (N und NW Bayern)

Frommetsfelden Fault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/7675
type: Concept
created: 2021-01-25T14:23:24.350Z
preferred label: Frommetsfeldener Verwerfung @de
notation: DE-BY_1442
definition: NW-SE (herzynisch) verlaufende, steil nach SW einfallende Abschiebung mit einem Vertikalversatz bis zu 60 m. @de
definition: NW-SE trending, steeply SW dipping normal fault with a vertical offset up to 60 m.
references: https://data.geoscience.earth/ncl/geoera/ref/7304
sf touches: Tiefenthal Fault
sf touches: Elpersdorf Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1442
broader: Schichtstufenland Domäne (N und NW Bayern)

Frankenheim Fault Zone
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/7675
type: Concept
created: 2021-01-25T14:23:24.323Z
preferred label: Frankenheimer Störungszone @de
notation: DE-BY_1441
alternative label: Schillingsfürster Verwerfung @de
alternative label: Frankenheimer Verwerfung @de
definition: NW-SE (herzynisch) verlaufende, steil nach SW einfallende Abschiebung mit einer Sprunghöhe bis zu 35 m. @de
definition: NW-SE trending, steeply SW dipping normal fault with a vertical offset up to 35 m.
references: https://data.geoscience.earth/ncl/geoera/ref/7305
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1441
broader: Schichtstufenland Domäne (N und NW Bayern)

Kaltenbronn-Kaierberg-Lölldorf Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:24.296Z
preferred label: Kaltenbronn-Kaierberg-Lölldorfer Verwerfung @de
notation: DE-BY_1440
definition: WSW-ENE verlaufende Gruppe verzweigter steil nach NNW einfallender Abschiebungen mit einer Sprunghöhe bis zu 30 m als Fortsetzung der baden-württembergischen Neckar-Jagst Furche, einer Scherzone, die die Baden Baden-Nürnberg-Erbendorf Line [DE-BY_1547] begleitet (Reinhold 2005). @de
definition: WSW-ENE trending array of branched steeply NNW dipping normal faults featuring a throw up to 30 m. This fault zone forms the on strike continuation of Neckar-Jagst Trough on Baden-Württemberg territory in the east, a shear zone inferred to accompany Baden Baden-Nuremberg-Erbendorf Line [DE-BY_1547] (Reinhold 2005).
references: https://data.geoscience.earth/ncl/geoera/ref/7306
references: https://data.geoscience.earth/ncl/geoera/ref/7301
references: https://data.geoscience.earth/ncl/geoera/ref/7346
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1440
broader: Schichtstufenland Domäne (N und NW Bayern)

Edelsfeld-Irlbach Fault Zone
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:24.269Z
preferred label: Edelsfeld-Irlbacher Störungszone @de
notation: DE-BY_1439
definition: Insgesamt W-E bis WNW-ESE verlaufende, steil nach ± S einfallende Aufschiebungen mit einer Sprunghöhe bis 70 m. @de
definition: Overall W-E to WNW-ESE trending, steeply ± S dipping reverse faults with a vertical displacement of up to 70 m.
references: https://data.geoscience.earth/ncl/geoera/ref/7298
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1439
broader: Schichtstufenland Domäne (N und NW Bayern)

Hainberg Cross-Fault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/7320
references: https://data.geoscience.earth/ncl/geoera/ref/8474
type: Concept
created: 2021-03-16T09:56:27.000Z
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
notation: DE-BY_1573
definition: SW-NE striking fault offsetting Auhof-Hainberg Fault [DE-BY_1562] to the SW.
preferred label: Hainberg Querstörung @de
sf touches: Auhof-Hainberg Fault
sf touches: Hainberg-Kirchhöhe Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1573
broader: Schichtstufenland Domäne (N und NW Bayern)

Wagenmühle-Erlenbach Fault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/8472
references: https://data.geoscience.earth/ncl/geoera/ref/7320
references: https://data.geoscience.earth/ncl/geoera/ref/8480
type: Concept
created: 2021-03-16T09:56:26.996Z
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
notation: DE-BY_1571
definition: NW-SE striking, steeply NE dipping normal fault featuring a throw of up to 65 m.
preferred label: Wagenmühle-Erlenbach Störung @de
alternative label: Erlenbach Störung @de
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1571
broader: Schichtstufenland Domäne (N und NW Bayern)

Altenbuch Fault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/8479
references: https://data.geoscience.earth/ncl/geoera/ref/8472
type: Concept
created: 2021-03-16T09:56:26.993Z
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
notation: DE-BY_1570
definition: NNW-SSE to NW-SE trending, steeply ± NE dipping normal fault featuring a throw of up to 50 m.
preferred label: Altenbuch Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/7320
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1570
broader: Schichtstufenland Domäne (N und NW Bayern)

Hanau-Seligenstadt Basin faults
type: Fault
type: Limit
type: Concept
created: 2021-03-16T09:56:26.939Z
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
notation: DE-BY_1578
definition: Beneath the Lower Main Plain west of Spessart and north of Odenwald, overlapping the border between Hesse and Bavaria with only a minor part in the east on Bavarian territory, the Hanau-Seligenstadt Basin represents a low subsidence Cenozoic subbasin of the Upper Rhine Graben. It is dominated by N-S to NNW-SSE trending normal faults structuring the basin into several horsts and grabens.
preferred label: Störungen der Hanau-Seligenstädter Senke @de
narrower: Erlensee-Alzenau Fault
narrower: Kahl-Kleinostheim Fault
narrower: Kahl-Stockstadt Fault
narrower: Auhof-Hainberg Fault
narrower: Ringheim-Eisenbach Fault
narrower: Karlstein-Langstadt Fault
references: https://data.geoscience.earth/ncl/geoera/ref/8473
references: https://data.geoscience.earth/ncl/geoera/ref/8478
references: https://data.geoscience.earth/ncl/geoera/ref/8475
references: https://data.geoscience.earth/ncl/geoera/ref/8474
in scheme: Tectonic Boundary Objects in Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11722
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11887
notation: LfU-BY_1578
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Ringheim-Eisenbach Fault
type: Fault
type: Limit
type: Concept
created: 2021-03-16T09:56:26.963Z
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
notation: DE-BY_1563
definition: Intersecting Stockstadt-Gross-Umstadt Block, NNW-SSE trending, in the south veering to WNW-ESE along Mümling valley, vertical to steeply ± NE dipping normal fault.
preferred label: Ringheim-Eisenbach Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/8474
references: https://data.geoscience.earth/ncl/geoera/ref/7320
sf touches: Karlstein-Langstadt Fault
sf touches: Stockstadt-Obernburg Graben Western Flank
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1563
limit type: normalFault
broader: Hanau-Seligenstadt Basin faults

Auhof-Hainberg Fault
type: Fault
type: Limit
type: Concept
created: 2021-03-16T09:56:26.959Z
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
notation: DE-BY_1562
definition: Intersecting Stockstadt-Gross-Umstadt Block, NNW-SSE striking, steeply ENE dipping normal fault.
preferred label: Auhof-Hainberg Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/8474
references: https://data.geoscience.earth/ncl/geoera/ref/7320
sf touches: Hainberg Cross-Fault
sf touches: Karlstein-Langstadt Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1562
limit type: normalFault
broader: Hanau-Seligenstadt Basin faults

Kahl-Stockstadt Fault
type: Fault
type: Limit
type: Concept
created: 2021-03-16T09:56:26.955Z
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
notation: DE-BY_1561
definition: NNW-SSE trending, steeply WSW dipping normal fault featuring a throw of up to 170 m. Southwestern boundary of Kleinwelzheim Horst towards Hanau-Seligenstadt Basin, continuing as ENE dipping Stockstadt-Obernburg Graben Western Flank [DE-BY_1565] in the south.
preferred label: Kahl-Stockstadt Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/8475
references: https://data.geoscience.earth/ncl/geoera/ref/8474
sf touches: Karlstein-Langstadt Fault
sf touches: Stockstadt-Obernburg Graben Western Flank
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1561
limit type: normalFault
broader: Hanau-Seligenstadt Basin faults

Ubstadt-Walldürn Fault Zone
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.824Z
preferred label: Ubstadt-Walldürn Störungszone @de
notation: DE-BY_973
definition: SW-NE streichende sinistrale Steitenverschiebung mit Einfallrichtung NW @de
definition: SW-NE trending sinistral strike-slip fault with dip direction NW
references: https://data.geoscience.earth/ncl/geoera/ref/7292
sf touches: Karlstadt-Würzburg-Kitzingen Fault Zone
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_973
broader: Schichtstufenland Domäne (N und NW Bayern)

Wöllriederhof-Biebelried Fault Zone
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:24.022Z
preferred label: Wöllriederhof-Biebelried Störungszone @de
notation: DE-BY_1004
definition: WNW-ESE streichende Abschiebung mit Einfallrichtung SSW @de
definition: WNW-ESE trending normal fault with dip direction SSW
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1004
broader: Schichtstufenland Domäne (N und NW Bayern)

Woffendorf Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.993Z
preferred label: Woffendorf Störung @de
notation: DE-BY_997
definition: N-S streichende Abschiebung mit Einfallrichtung W @de
definition: N-S trending normal fault with dip direction W
references: https://data.geoscience.earth/ncl/geoera/ref/7292
sf touches: Asslitz-Saas Fault
sf touches: Weismain Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_997
broader: Schichtstufenland Domäne (N und NW Bayern)

Wippfeld-Prichsenstadt Fault Zone
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.965Z
preferred label: Wippfeld-Prichsenstadt Störungszone @de
notation: DE-BY_976
definition: NW-SE streichende dextrale Ab- und Seitenverschiebung mit Einfallrichtung SW @de
definition: NW-SE trending dextral normal/strike-slip fault with dip direction SW
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_976
broader: Schichtstufenland Domäne (N und NW Bayern)

Wiesenttal Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.938Z
preferred label: Wiesenttal Störung @de
notation: DE-BY_1033
definition: SW-NE streichende Abschiebung mit Einfallrichtung SE @de
definition: SW-NE trending normal fault with dip direction SE
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1033
broader: Schichtstufenland Domäne (N und NW Bayern)

Weismain Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.910Z
preferred label: Weismain Störung @de
notation: DE-BY_1001
definition: NW-SE streichende Abschiebung mit Einfallrichtung SW (revers invertiert Einfallrichtung NE) @de
definition: NW-SE trending normal fault with dip direction SW (reversly inverted dip NE)
references: https://data.geoscience.earth/ncl/geoera/ref/6372
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1001
broader: Schichtstufenland Domäne (N und NW Bayern)

Staffelberg Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.547Z
preferred label: Staffelberg Störung @de
notation: DE-BY_1002
definition: NW-SE streichende Abschiebung mit Einfallrichtung NE @de
definition: NW-SE trending normal fault with dip direction NE
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1002
broader: Schichtstufenland Domäne (N und NW Bayern)

Kissingen-Hassfurt Fault Zone
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.548Z
preferred label: Kissingen-Hassfurt Störungszone @de
notation: DE-BY_1377
definition: Allgemein NW-SE streichende Ab- und Seitenverschiebung mit Einfallrichtung NE, möglicherweise revers invertiert im NW und dominierender Abschliebungskomponente im SE Teil @de
definition: Generally NW-SE trending dextral normal fault with dip direction NE, probably reversely inverted in the NW and dominating normal faulting behaviour in the SE part
narrower: Stangenroth-Kissingen Fault
narrower: Arnshausen-Wittersberg Fault
narrower: Oerlenbach-Waldsachsen Fault
narrower: Hassfurt-Bischberg Fault
narrower: Oberleichtersbach-Kissingen Fault Zone
narrower: Wonfurt-Aurach Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/7348
references: https://data.geoscience.earth/ncl/geoera/ref/7347
references: https://data.geoscience.earth/ncl/geoera/ref/7272
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1377
broader: Schichtstufenland Domäne (N und NW Bayern)

Oerlenbach-Waldsachsen Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.633Z
preferred label: Oerlenbach-Waldsachsen Störung @de
notation: DE-BY_1055
alternative label: Kissingen-Hassfurt Störungszone Segment 3 @de
definition: NW-SO streichende dextrale Ab- und Seitenverschiebung mit Einfallrichtung NE @de
definition: NW-SE trending dextral normal fault with dip direction NE
references: https://data.geoscience.earth/ncl/geoera/ref/7348
references: https://data.geoscience.earth/ncl/geoera/ref/7347
references: https://data.geoscience.earth/ncl/geoera/ref/7272
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
sf touches: Arnshausen-Wittersberg Fault
sf touches: Hassfurt-Bischberg Fault
sf touches: Wonfurt-Aurach Fault Zone
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1055
broader: Kissingen-Hassfurt Fault Zone

Arnshausen-Wittersberg Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.605Z
preferred label: Arnshausen-Wittersberg Störung @de
notation: DE-BY_986
alternative label: Kissingen-Hassfurt Störungszone Segment 2 @de
definition: N-S streichende dextrale Schrägabschiebung mit Einfallrichtung E @de
references: https://data.geoscience.earth/ncl/geoera/ref/7307
references: https://data.geoscience.earth/ncl/geoera/ref/7311
references: https://data.geoscience.earth/ncl/geoera/ref/7292
definition: N-S trending dextral oblique-slip normal fault with dip direction E
sf touches: Stangenroth-Kissingen Fault
sf touches: Oerlenbach-Waldsachsen Fault
sf touches: Oberleichtersbach-Kissingen Fault Zone
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_986
broader: Kissingen-Hassfurt Fault Zone

Stangenroth-Kissingen Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.577Z
preferred label: Stangenroth-Kissingen Störung @de
notation: DE-BY_1052
alternative label: Kissingen-Hassfurt Störungszone Segment 1 @de
definition: NW-SO streichende dextrale Ab- und Seitenverschiebung mit Einfallrichtung NE (revers invertiert?) @de
definition: NW-SE trending dextral normal fault with dip direction NE (reversly inverted?)
references: https://data.geoscience.earth/ncl/geoera/ref/7348
references: https://data.geoscience.earth/ncl/geoera/ref/7347
references: https://data.geoscience.earth/ncl/geoera/ref/7272
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1052
broader: Kissingen-Hassfurt Fault Zone

Wonfurt-Aurach Fault Zone
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.716Z
preferred label: Wonfurt-Aurach Störungszone @de
notation: DE-BY_988
definition: NW-SE streichende dextrale Abschiebung mit Einfallrichtung NE @de
definition: NW-SE trending normal or dextral strike slipe fault with dip direction NE
references: https://data.geoscience.earth/ncl/geoera/ref/7292
sf touches: Bamberg-Neuses Fault Zone
sf touches: Oerlenbach-Waldsachsen Fault
sf touches: Hassfurt-Bischberg Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_988
broader: Kissingen-Hassfurt Fault Zone

Oberleichtersbach-Kissingen Fault Zone
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.688Z
preferred label: Oberleichtersbach-Kissingen Störungszone @de
notation: DE-BY_972
alternative label: Kissingen-Hassfurt Störungszone Segment 5 @de
definition: NW-SE streichende dextrale Steitenverschiebung @de
definition: NW-SE trending dextral strike-slip fault
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
sf touches: Arnshausen-Wittersberg Fault
sf touches: Singenrain Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_972
broader: Kissingen-Hassfurt Fault Zone

Hassfurt-Bischberg Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.661Z
preferred label: Hassfurt-Bischberg Störung @de
notation: DE-BY_968
alternative label: Kissingen-Hassfurt Störungszone Segment 4 @de
definition: NW-SE streichende Abschiebung mit Einfallrichtung NE @de
definition: NW-SE trending normal fault with dip direction NE
references: https://data.geoscience.earth/ncl/geoera/ref/7348
references: https://data.geoscience.earth/ncl/geoera/ref/7347
references: https://data.geoscience.earth/ncl/geoera/ref/7272
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
sf touches: Oerlenbach-Waldsachsen Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_968
broader: Kissingen-Hassfurt Fault Zone

Kilianshof Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.521Z
preferred label: Kilianshof Störung @de
notation: DE-BY_1011
definition: NW-SE streichende Abschiebung mit Einfallrichtung SW (Graben) @de
definition: NW-SE trending normal fault with dip direction SW (graben)
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1011
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Kemnath-Waldeck Fault
limit type: obliqueSlipFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.493Z
notation: DE-BY_1024
definition: E-W streichende Ab- bzw. Steitenverschiebung mit Einfallrichtung S @de
definition: E-W trending normal/strike-slip fault with dip direction S
references: https://data.geoscience.earth/ncl/geoera/ref/6372
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
preferred label: Kemnath-Waldeck Störung @de
sf touches: Waldeck Fault
sf touches: Altenparkstein Fault
sf touches: Weidenberg Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1024
broader: Schichtstufenland Domäne (N und NW Bayern)

Karlstadt-Würzburg-Kitzingen Fault Zone
limit type: strikeSlipFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:22.465Z
preferred label: Karlstadt-Würzburg-Kitzingen Störungszone @de
notation: DE-BY_975
definition: NW-SE streichende dextrale Ab- und Seitenverschiebung mit Einfallrichtung SW @de
definition: NW-SE trending dextral normal/strike-slip fault with dip direction SW
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_975
broader: Schichtstufenland Domäne (N und NW Bayern)

Itztal Fault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6372
type: Concept
created: 2021-01-25T14:23:22.438Z
preferred label: Itztal Störung @de
notation: DE-BY_1046
definition: N-S streichende Abschiebung mit Einfallrichtung E @de
definition: N-S trending normal fault with dip direction E
references: https://data.geoscience.earth/ncl/geoera/ref/7292
sf touches: Bamberg-Neuses Fault Zone
sf touches: Baunachtal Fault
sf touches: Hassfurt-Bischberg Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1046
limit type: normalFault
broader: Schichtstufenland Domäne (N und NW Bayern)

Trebgast Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.797Z
preferred label: Trebgast Störung @de
notation: DE-BY_958
definition: NW-SE streichende Abschiebung mit Einfallrichtung NE @de
definition: NW-SE trending normal fault with dip direction NE
references: https://data.geoscience.earth/ncl/geoera/ref/6372
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_958
broader: Schichtstufenland Domäne (N und NW Bayern)

Sulzbach Syncline NE boundary
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.686Z
preferred label: Sulzbacher Mulde NE Rand @de
notation: DE-BY_1542
definition: Nordwest-Rand der Sulzbacher Mulde und der südlich anschließenden Kallmünzer Mulde (Frankenalb Mulde) gebildet von Aufschiebungen und einer Abschiebung (invertierte Aufschiebung?). @de
definition: Northwestern margin of Sulzbach syncline and its southward transition to Kallmünz syncline (Frankenalb syncline) formed by reverse faults and normal (inverted reverse?) fault.
narrower: Sulzbach Fault
narrower: Sulzbach-Amberg Fault
narrower: Amberg-Diebis-Thanheim Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7298
references: https://data.geoscience.earth/ncl/geoera/ref/4114
references: https://data.geoscience.earth/ncl/geoera/ref/7322
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1542
broader: Schichtstufenland Domäne (N und NW Bayern)

Amberg-Diebis-Thanheim Fault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/4114
type: Concept
created: 2021-01-25T14:23:23.769Z
preferred label: Amberg-Diebis-Thanheim Störung @de
notation: DE-BY_1543
definition: Von der Pfahl-Aufschiebung [DE-BY_1364] bei Krumbach nahe Amberg, westlich subparallel zur Fensterbach [DE-BY_1376] und Pittersberger [DE-BY_1374] Störung ziehende, NW-SE verlaufende, steil nach NE einfallende Abschiebung (invertierte Aufschiebung?) mit einem Vertikalversatz von bis zu 150 m, abschnittsweise wohl als Flexur (Nordost-Flanke des Ebermannsdorfer Sattels nach Meyer 2000). Im Süden bei stark abnehmender Sprunghöhe auf NE-SW umbiegend. Nordwest-Rand des Übergangsbereichs von der Sulzbacher zur Kallmünzer Mulde im SW zum Pittersberger Sattel im NE. @de
definition: From Pfahl Reverse Fault [DE-BY_1364] at Krumbach near Amberg, paralleling the trends of Fensterbach [DE-BY_1376] and Pittersberg [DE-BY_1374] faults, NW-SE trending, steeply NE dipping normal fault (inverted reverse fault?) featuring a throw of up to 150 m, in parts arguably as a flexure (NE flank of Ebermannsdorf anticline after Meyer 2000). In its south veering to a NE-SW trend with decreasing throw. Northwestern margin of Sulzbach to Kallmünz syncline transition zone in the SW towards Pittersberg anticline in the NE.
references: https://data.geoscience.earth/ncl/geoera/ref/7322
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1543
broader: Sulzbach Syncline NE boundary

Sulzbach-Amberg Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.741Z
preferred label: Sulzbach-Amberg Störung @de
notation: DE-BY_999
alternative label: Amberg-Sulzbacher Störungszone @de
definition: NW-SE streichende Aufschiebung mit Einfallrichtung NE und einem Vertikalversatz bis zu 150 m. @de
definition: NW-SE trending reverse fault with dip direction NE featuring a throw of up to 150 m.
references: https://data.geoscience.earth/ncl/geoera/ref/6372
references: https://data.geoscience.earth/ncl/geoera/ref/7292
sf touches: Sesslach Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_999
broader: Sulzbach Syncline NE boundary

Sulzbach Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.713Z
preferred label: Sulzbach Störung @de
notation: DE-BY_966
alternative label: Sulzbacher Störungszone @de
definition: NW-SE streichende Aufschiebung mit Einfallrichtung NE und einen Vertikalversatz von bis zu 200 m. @de
definition: NW-SE trending reverse fault with dip direction NE, featuring a throw of up to 200 m.
references: https://data.geoscience.earth/ncl/geoera/ref/6372
references: https://data.geoscience.earth/ncl/geoera/ref/7298
sf touches: Sulzbach-Amberg Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_966
broader: Sulzbach Syncline NE boundary

Strahlungen-Münnerstadt-Graben
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.658Z
notation: DE-BY_980
definition: Nördlich von Münnerstadt SW-NE, südlich davon N-S streichendes Abschiebungs-Paar (abschnittsweise Staffelbrüche), die einen auffälligen, geknickten Graben bilden. @de
definition: North of Münnerstadt SW-NE, south of N-S striking pair normal faults (in sections step faults) forming a conspicuous kinked graben structure.
references: https://data.geoscience.earth/ncl/geoera/ref/7312
references: https://data.geoscience.earth/ncl/geoera/ref/7292
sf touches: Oerlenbach-Waldsachsen Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_980
broader: Schichtstufenland Domäne (N und NW Bayern)

Anterior Spessart faults
type: Fault
type: Limit
type: Concept
created: 2021-03-16T09:56:26.909Z
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
notation: DE-BY_1579
definition: The Anterior Spessart (Kristalliner Vorspessart) is the only place on Bavarian territory where the basement of the Mid-German Crystalline Rise (Mitteldeutsche Kristallinschwelle) emerges, the swell between the Saxothuringian and Rhenohercynian Zones interpreted an island arc. Two predominant structures characterize the basement: the SW-NE striking Variscan fold architecture and the NW-SE (Hercynian) striking late to post-Variscan faults, reactivated during Late Cretaceous and Tertiary generating up- and down faulted blocks (Saxonian brittle tectonics). Most faults, also those transecting the surrounding Buntsandstein-Spessart, more or less follow the Hercynian trend, predominant in the entire Bavarian Scarp Land.
preferred label: Störungen im Kristallinen Vorspessart @de
narrower: Geiselbach-Vormwald Fault
narrower: Rubenberg-Bischlingsberg Fault
narrower: Bauersberg Fault
narrower: Stempelhöhe-Goldbach Fault
narrower: Oberwald-Hohl Fault
narrower: Schimborn-Laufach Fault
references: https://data.geoscience.earth/ncl/geoera/ref/8476
references: https://data.geoscience.earth/ncl/geoera/ref/8473
references: https://data.geoscience.earth/ncl/geoera/ref/8472
references: https://data.geoscience.earth/ncl/geoera/ref/7320
references: https://data.geoscience.earth/ncl/geoera/ref/8477
narrower: Waldaschaff Fault Zone
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1579
broader: Schichtstufenland Domäne (N und NW Bayern)

Waldaschaff Fault Zone
type: Fault
type: Limit
scope note: Revised concept as of 2021-03-15, after the HIKE editorial deadline. Corresponding fault geometries in the HIKE Fault Data Base not adjusted accordingly.
scope note: Überarbeitetes Konzept von 2021-03-15, nach HIKE Redaktionsschluss. Die entsprechenden Störungs-Geometrien in der HIKE Störungsdatenbank wurden nicht angepasst. @de
references: https://data.geoscience.earth/ncl/geoera/ref/8476
references: https://data.geoscience.earth/ncl/geoera/ref/8477
alternative label: Mittelgrund-Verwerfung @de
type: Concept
definition: NW-SE trending normal faults with a steep dip direction SW; the southern branch, Mittelgrund Fault, running from Waldaschaff to Heimbuchenthal, features a throw of up to 85 m.
created: 2021-01-25T14:23:23.852Z
preferred label: Waldaschaff Störungszone @de
notation: DE-BY_1006
definition: NW-SE streichende Abschiebung mit Einfallrichtung SW @de
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1006
broader: Anterior Spessart faults

Schimborn-Laufach Fault
type: Fault
type: Limit
type: Concept
created: 2021-03-16T09:56:26.935Z
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
notation: DE-BY_1572
definition: NW-SE trending, steeply SW dipping normal fault featuring a throw of up to 50 m.
preferred label: Schimborn-Laufach Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/8477
references: https://data.geoscience.earth/ncl/geoera/ref/8472
references: https://data.geoscience.earth/ncl/geoera/ref/7320
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1572
broader: Anterior Spessart faults

Oberwald-Hohl Fault
type: Fault
type: Limit
type: Concept
created: 2021-03-16T09:56:26.931Z
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
notation: DE-BY_1555
definition: Slightly arcuate NW-SE trending oblique-slip normal fault
preferred label: Oberwald-Hohl Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/8476
references: https://data.geoscience.earth/ncl/geoera/ref/8472
references: https://data.geoscience.earth/ncl/geoera/ref/7320
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1555
broader: Anterior Spessart faults

Stempelhöhe-Goldbach Fault
type: Fault
type: Limit
type: Concept
created: 2021-03-16T09:56:26.927Z
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
notation: DE-BY_1554
definition: Slightly undulate NW-SE trending oblique-slip normal fault
preferred label: Stempelhöhe-Goldbach Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/8473
references: https://data.geoscience.earth/ncl/geoera/ref/8472
references: https://data.geoscience.earth/ncl/geoera/ref/7320
references: https://data.geoscience.earth/ncl/geoera/ref/8478
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1554
broader: Anterior Spessart faults

Bauersberg Fault
type: Fault
type: Limit
type: Concept
created: 2021-03-16T09:56:26.923Z
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
notation: DE-BY_1553
definition: NW-SE trending oblique-slip normal fault featuring an offset of about 200 m.
preferred label: Bauersberg Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/8477
references: https://data.geoscience.earth/ncl/geoera/ref/8473
references: https://data.geoscience.earth/ncl/geoera/ref/8472
references: https://data.geoscience.earth/ncl/geoera/ref/7320
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1553
broader: Anterior Spessart faults

Rubenberg-Bischlingsberg Fault
type: Fault
type: Limit
type: Concept
created: 2021-03-16T09:56:26.919Z
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
notation: DE-BY_1551
definition: Slightly arcuate NW-SE trending, steeply SW dipping normal fault.
preferred label: Rubenberg-Bischlingsberg Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/8477
references: https://data.geoscience.earth/ncl/geoera/ref/8472
references: https://data.geoscience.earth/ncl/geoera/ref/7320
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1551
broader: Anterior Spessart faults

Geiselbach-Vormwald Fault
type: Fault
type: Limit
type: Concept
created: 2021-03-16T09:56:26.914Z
scope note: New concept as of 2021-03-15, after the HIKE editorial deadline – no corresponding fault geometries in the HIKE Fault Data Base.
scope note: Neues Konzept von 2021-03-15, nach HIKE Redaktionsschluss – entsprechende Störungs-Geometrien in der HIKE Störungsdatenbank fehlen. @de
notation: DE-BY_1550
definition: NW-SE trending, steeply SW dipping minor offset sinistral normal oblique-slip fault.
preferred label: Geiselbach-Vormwald Störung @de
alternative label: Geiselbacher Sprung @de
references: https://data.geoscience.earth/ncl/geoera/ref/8477
references: https://data.geoscience.earth/ncl/geoera/ref/8472
references: https://data.geoscience.earth/ncl/geoera/ref/7320
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1550
broader: Anterior Spessart faults

Stetten Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.630Z
preferred label: Stetten Störung @de
notation: DE-BY_1013
definition: NW-SE streichende Abschiebung mit Einfallrichtung SW (oder dextrale Seitenverschiebung?) @de
definition: NW-SE trending normal fault with dip direction SW (or dextral strike-slip?)
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1013
broader: Schichtstufenland Domäne (N und NW Bayern)

Steinbach-Steinfeld-Retzbach Fault Zone
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.603Z
preferred label: Steinbach-Steinfeld-Retzbach Störungszone @de
notation: DE-BY_1016
definition: NW-SE streichende Abschiebung mit Einfallrichtung NE @de
definition: NW-SE trending normal fault with dip direction NE
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1016
broader: Schichtstufenland Domäne (N und NW Bayern)

Staffelstein Fault Zone
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:23.575Z
preferred label: Staffelstein Störungszone @de
notation: DE-BY_964
definition: NW-SE streichende Abschiebung mit Einfallrichtung NE, Südwestrand des Staffelsteiner Grabens. @de
definition: NW-SE trending normal fault with dip direction NE, southwestern boundary of Staffelstein Graben.
references: https://data.geoscience.earth/ncl/geoera/ref/6372
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11692
notation: LfU-BY_964
broader: Schichtstufenland Domäne (N und NW Bayern)

3: Bohemian Massif domain
in scheme: GC3D limits
type: Fault
type: Limit
narrower: Bohemian Massif Western Margin System
type: Concept
created: 2021-01-25T14:23:17.949Z
preferred label: Grundgebirge der Böhmischen Masse @de
notation: DE-BY_1531
scope note: The tectonic boundary inventory within the verdant Bohemian Massif rock suites, apart from larger scale faults manifested in fractured zones and tectonites or evidence in scarce quarries, only rarely can be observed directly. Fault pattern are inferred mostly from indirect field evidence such as conspicuous lithological changes, joint system measurements, linear features like quartz veins, aligned with remote sensing data and geophysical surveys in few areas. By nature, these investigations do not allow for exact information on the dip angle and vertical displacement. Accordingly, the concepts’ statements on these parameters shall be considered an assumption. Small-scale faults and fractures of fragmented plutonic complexes (granite tectonics) are not considered.
scope note: Das Inventar tektonischer Grenzflächen in den Gesteinen der stark bewachsenen Böhmischen Masse, kann, mit Ausnahme größerer Störungszonen die sich in Zerrüttungszonen und dem Vorkommen von Tektoniten ausdrücken, sowie den Beobachtungen in Steinbrüchen, nur selten direkt eruiert werden. Die Störungsmuster sind daher meist aus indirekten Geländebefunden abgeleitet, wie abrupte Gesteinswechsel, Kluftmessungs-Diagrammen oder linearen Bildungen wie Quarzgängen, z. T. im Kontext mit Fernerkundungsdaten und geophysikalischen Untersuchungen in ausgesuchten Gebieten. Naturgemäß sind aus solchen Informationen keine genauen Aussagen zum Einfallswinkel und Sprunghöhe der Störungen zu treffen; die Angaben zu diesen Parametern in den Konzepten sind daher als Annahmen zu verstehen. Texturen und Kleinstrukturen fragmentierter Plutonit-Komplexe (Granittektonik) sind in den Konzepten nicht berücksichtigt. @de
definition: Das Störungsmuster aller größeren stratigraphisch-lithologisch-tektonischen Einheiten der Böhmischen Masse in Bayern, Saxothuringikum, Moldanubikum und Münchberger Masse (eine Überschiebungsinsel des Teplá-Barrandiums), wird von grob NW-SE, flach herzynisch (100-120°) bis steil herzynisch (130-140°) verlaufenden Störungen oder Störungszonen dominiert. Diese bilden insbesondere im Moldanubikum großräumige polyphase Scherzonen, die teilweise bis weit in das permo-mesozoische Vorland reichen. Querstörungen, im Süden überwiegend ± N-S verlaufend, im Norden meist ± SW-NE, parallel zu den Suturen der variszischen Kollisionstektonik, ergänzen das Gesamtbild. @de
definition: Overlapping the principal stratigraphic-lithologic-tectonic zones of the Bohemian Massif in Bavaria, Saxothuringian Zone, Moldanubian Zone and Münchberg Klippe (a Teplá-Barrandian thrust outlier), roughly NW-SE, flat-angle Hercynian (100-120°) to high-angle Hercynian (130-140°) trending faults or fault zones prevail the tectonic boundaries pattern, particularly in the Moldanubian Zone forming large-scale polyphase shear zones partially protruding into the Permo-mesozoic foreland. Transverse faults, predominantly ± N-S trending in the south, prevalently ± SW-NE in the north, resuming the orientation of accreted terranes sutures, complement the overall picture.
narrower: Moldanubian Zone tectonic boundaries
narrower: Teplá-Barrandian Terrane boundary
narrower: Baden Baden-Nuremberg-Erbendorf Line
narrower: Erbendorf Line
narrower: Saxothuringian Zone tectonic boundaries
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7285
references: https://data.geoscience.earth/ncl/geoera/ref/7295
references: https://data.geoscience.earth/ncl/geoera/ref/6358
in scheme: Tectonic Boundary Objects in Europe
narrower: ZTM Southern Boundary
notation: LfU-BY_1531
broader: Tectonic Boundaries in Bavaria

Erbendorf Line
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.830Z
preferred label: Erbendorfer Linie @de
notation: DE-BY_1447
alternative label: Tepla-Barrandium Sutur @de
definition: Östlich der Fränkischen Linie [DE-BY_1398], wo das variszische Grundgebirge zu Tage tritt, ist die Sutur zwischen dem niedrig metamorphen Saxothuringikum und dem hoch metamorphen Moldanubikum streckenweise aufgeschlossen, oft jedoch durch granitische Intrusionen ersetzt oder von jüngeren (tertiären) Sedimenten verdeckt. Im äußersten Westen und im Osten, wo sich die Struktur auf Tschechischen Territorium bis zur Westböhmischen Scherzone [DE-BY_1353] fortsetzt, markiert die Erbendorf Linie den Nordrand des Teplá-Barrandiums bzw. von Klippen sehr ähnlicher Lithologie (Zone von Erbendorf-Vohenstrauß). @de
definition: East of the Franconian Line [DE-BY_1398] where the Variscan Basement emerges, the suture separating the high-grade metamorphic Moldanubian Zone to the south and the low-grade metamorphic Saxothuringian Zone to the north, the Baden Baden-Nuremberg-Erbendorf Line, subcrops in certain sections but is replaced by granitic intrusions or concealed by younger (Tertiary) deposits in large areas. In its very west and to the east, continuing on Czech territory to the West Bohemian Shear Zone [DE-BY_1353], Erbendorf Line marks the northern limit of the Teplá-Barrandian Zone or its outliers (Erbendorf-Vohenstrauss Zone).
narrower: Hahneneggaten-Grötschenreuth Fault
narrower: Grötschenreuth-Siegritz Fault
narrower: Wetzldorf Fault
narrower: Mitterteich Graben boundaries
narrower: Leonberg-Wondreb Fault
narrower: Pilmersreuth-Mähring Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7360
references: https://data.geoscience.earth/ncl/geoera/ref/7310
references: https://data.geoscience.earth/ncl/geoera/ref/7309
references: https://data.geoscience.earth/ncl/geoera/ref/7295
in scheme: Tectonic Boundary Objects in Europe
broader: 3: Bohemian Massif domain

Grötschenreuth-Siegritz Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.885Z
preferred label: Grötschenreuth-Siegritz Störung @de
notation: DE-BY_1449
definition: Insgesamt W-E verlaufender Abschnitt der Erbendorfer Linie [DE-BY_1447] östlich der Fichtelnaab Störungszone [DE-BY_1451]. @de
definition: Overall W-E trending segment of Erbendorf Line [DE-BY_1447] east of Fichtelnaab Fault Zone [DE-BY_1451].
references: https://data.geoscience.earth/ncl/geoera/ref/7360
references: https://data.geoscience.earth/ncl/geoera/ref/7295
sf touches: Fichtelnaab Fault Zone
sf touches: Wetzldorf Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1449
broader: Erbendorf Line

Hahneneggaten-Grötschenreuth Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.857Z
preferred label: Hahneneggaten-Grötschenreuth Störung @de
notation: DE-BY_1448
definition: Westlichster Abschnitt der Erbendorfer Linie [DE-BY_1447], W-E streichende nördliche Grenze der Erbendorf-Vohenstrauß Zone [vgl. DE-BY_1451], einem isolierten Vorkommen (Klippe) des Teplá-Barrandiums. @de
definition: Western section of Erbendorf Line [DE-BY_1447], W-E striking northern boundary of the Erbendorf-Vohenstrauss Zone [cf. DE-BY_1451], an outlier of the Teplá-Barrandian Terrane.
references: https://data.geoscience.earth/ncl/geoera/ref/7360
references: https://data.geoscience.earth/ncl/geoera/ref/7295
sf touches: Waldeck-Klobenreuth Fault
sf touches: Fichtelnaab Fault Zone
in scheme: Tectonic Boundary Objects in Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11578
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11574
notation: LfU-BY_1448
broader: Erbendorf Line

Pilmersreuth-Mähring Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.995Z
preferred label: Pilmersreuth-Mähring Störung @de
notation: DE-BY_1490
definition: Insgesamt WSW-ENE verlaufende, saigere bis subvertikale Störung die der Erbendorfer Linie [DE-BY_1447] zugerechnet wird; mehrfach von den herzynischen Störungen des Stiftslands [DE-BY_1455] versetzt. @de
definition: Overall WSW-ENE trending vertical to subvertical fault assigned to Erbendorf Line [DE-BY_1447], multiply offset by Stiftsland Hercynian faults [DE-BY_1455].
references: https://data.geoscience.earth/ncl/geoera/ref/7362
references: https://data.geoscience.earth/ncl/geoera/ref/7295
references: https://data.geoscience.earth/ncl/geoera/ref/7320
sf touches: Leonberg-Wondreb Fault
sf touches: Stiftsland Hercynian faults
sf touches: Muglberg-Mähring Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1490
broader: Erbendorf Line

Leonberg-Wondreb Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.967Z
preferred label: Leonberg-Wondreb Störung @de
notation: DE-BY_1456
definition: NW-SE verlaufende, saigere bis subvertikale Störung die die Erbendorfer Linie [DE-BY_1447] mehr als 10 km nach SE versetzt. @de
definition: NW-SE trending vertical to subvertical fault offsetting Erbendorf Line [DE-BY_1447] by more than 10 km to the SE.
references: https://data.geoscience.earth/ncl/geoera/ref/7362
references: https://data.geoscience.earth/ncl/geoera/ref/7344
sf touches: Pilmersreuth-Mähring Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1456
broader: Erbendorf Line

Mitterteich Graben boundaries
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.940Z
preferred label: Mitterteich Grabenränder @de
notation: DE-BY_1458
definition: Nach den unterschiedlichen Bohrtiefen der Basis der unverfestigten Tertiär-Ablagerungen des Mitterteicher Beckens, erscheint eine grabenartige Struktur in Grundgebirge gesichert. Der Verlauf der gegensinnig einfallenden Bruchstaffeln der Grabenflanken parallel zur Erbendorfer Linie [DE-BY_1447] jedoch ist angenommen, da Nachweise zur Verlaufsrichtung bisher fehlen. @de
definition: Infrerred from the different depths of the base of Mitterteich Basin Tertiary unconsolidated deposits in various drillings, the existence of a graben-like structure is assured. However, the WSW-ENE trend of the inversely arranged step faults forming the flanks of the graben parallel to Erbendorf Line [DE-BY_1447] is assumed only as there is no evidence substantiating this orientation.
references: https://data.geoscience.earth/ncl/geoera/ref/7344
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1458
limit type: normalFault
broader: Erbendorf Line

Wetzldorf Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.912Z
preferred label: Wetzldorf Störung @de
notation: DE-BY_1450
definition: NW-SE streichende Querstörung zur Grötschenreuth-Siegritz Störung [DE-BY_1449]. @de
definition: NW-SE striking lateral fault of Grötschenreuth-Siegritz Fault [DE-BY_1449].
references: https://data.geoscience.earth/ncl/geoera/ref/7360
references: https://data.geoscience.earth/ncl/geoera/ref/7295
sf touches: Grötschenreuth-Siegritz Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1450
broader: Erbendorf Line

ZTM Southern Boundary
limit type: thrustFault
type: Fault
type: Limit
creator: schmar
type: Concept
created: 2021-08-23T08:33:31.229Z
in scheme: Tectonic Boundary Objects in Europe
in scheme: GC3D limits
notation: LfU-BY_1581
type: https://data.geoscience.earth/ncl/geoera/geoconnect3d/category/9754
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11855
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11579
preferred label: ZTM Südgrenze @de
definition: Southern Boundary of the Tischenreuth-Mähring Zone (ZTM) an thrust outlier resembling the lithology of the Teplá-Barrandian Block, to the north bound by Erbendorf Line [LfU-BY_1447].
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7295
broader: 3: Bohemian Massif domain

Moldanubian Zone tectonic boundaries
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6358
type: Concept
created: 2021-01-25T14:23:17.978Z
preferred label: Tektonische Grenzflächen des Moldanubikums @de
notation: DE-BY_1532
definition: Das Moldanubikum wird von spät-variszischen Blattverschiebungs-Bewegungen dominiert, die sich in NW-SE verlaufenden Scherzonen ausdrücken. Dementsprechend wird das Moldanubikum von grob NW-SE, flach herzynisch (100-120°) bis steil herzynisch (130-140°) streichenden, steilstehenden bis saigeren Störungen (sub-)parallel zu diesen Scherzonen charakterisiert und den kinematisch verbundenen, spitzwinklig dazu verlaufenden Nebenstörungen. Insbesondere der Bayerische Wald wird zudem von einer Vielzahl an mehr oder weniger N-S gerichteten Störungen durchsetzt. Der Ostrand der Bodenwöhrer Senke wird durch ein solches Störungsbündel begrenzt, das zu einem großen, sich nach Süden zur Stallwanger Furche fortsetzenden Störungssystem gehört. Östlich vom Cham, am Hohen Bogen, wurde die südwestliche Ausbuchtung des Teplá-Barrandiums in und auf das Moldanubikum s. str. geschoben und endet dort an einer bogenförmigen Scherzone aus invertierten Aufschiebungen. @de
definition: Late Varican strike-slip faulting dominates the Moldanubian Zone, manifested in the extensive NW-SE trending shear zones. Accordingly, the Moldanubian Zone is characterized by roughly NW-SE, flat-angle Hercynian (100-120°) to high-angle Hercynian (130-140°) striking, subvertical to vertical faults (sub-)parallel to these shear zones and their acute-angled kinematically connected subsidiary faults. In addition, specifically the Bavarian Forest features a multitude of more or less N-S oriented faults. The eastern margin of Bodenwöhr Trough is bounded by a set of such faults, which are part of a major fault system continuing south to Stallwang Trench (Stallwanger Furche). East of Cham, the southwestern bulge of the Teplá-Barrandian Terrane is thrusted into the Moldanubian s. str., manifested in a bow-shaped shear zone system of inverted thrust faults.
narrower: Bavarian Pfahl
narrower: Runding Zone
narrower: Rattenberg Zone
narrower: Bayerwald Meridional Faults
narrower: Falkenstein-Frauenau Fault
narrower: Cham Fault
narrower: Weisser Regen Fault
narrower: Trasching-Michelsneukirchen Faults
narrower: Schwaighof-Momansfelden Fault
narrower: Falkensteiner Vorwald Faults
narrower: Kittenrain Faults
narrower: Upper Palatine Forest SW-NE faults
narrower: Pamsendorf Fault Set
narrower: Wölsendorf Fault
narrower: Schmidgaden Rotliegend Graben boundaries
narrower: Hildenbach Fault
narrower: Stockbach Fault
narrower: Kemnath Fault
narrower: Neuersdorf Fault
narrower: Weidelbach Fault
narrower: Schnaittenbach Fault
narrower: Tiefenbach-Treffelstein Fault
narrower: Waldmünchen Faults
narrower: Waldmünchen-Gleissenberg Fault
narrower: Upper Palatine Forest Hercynian structures
narrower: Waldthurn-Vohenstrauss Fault
narrower: Fichtelnaab Fault Zone
narrower: Fichtelnaab lateral faults
narrower: Nottersdorf Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/7255
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1532
broader: 3: Bohemian Massif domain

Weisser Regen Fault
limit type: strikeSlipFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:18.972Z
preferred label: Weißer Regen Störung @de
notation: DE-BY_1541
definition: Im östlichen Lamer Winkel entlang des Weißen Regens, leicht gewellt NW-SE verlaufende, saigere bis subvertikale Blattverschiebung grob parallel zur Rundinger Zone [DE-BY_1348]. @de
definition: Following Weisser Regen river valley in the east of Lamer Winkel, slightly undulate NW-SE trending vertical to subvertical strike-slip fault roughly parallel to Runding Zone [DE-BY_1348].
references: https://data.geoscience.earth/ncl/geoera/ref/6358
sf touches: Bayerwald Meridional Faults
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1541
broader: Moldanubian Zone tectonic boundaries

Nottersdorf Fault Zone
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.580Z
preferred label: Nottersdorf Störungszone @de
notation: DE-BY_1453
definition: NNW-SSE streichende, steil nach ENE einfallende Aufschiebung, entsprechend dem Versatz von Markerzonen (Wagner et al. 1997) mit einem Vertikalversatz von ca. 1,8 km. @de
definition: NNW-SSE striking, steeply ENE dipping reverse fault, according to the vertical displacement of marker horizons (Wagner et al. 1997) featuring a vertical offset of about 1.8 km.
references: https://data.geoscience.earth/ncl/geoera/ref/7360
references: https://data.geoscience.earth/ncl/geoera/ref/7310
references: https://data.geoscience.earth/ncl/geoera/ref/7309
references: https://data.geoscience.earth/ncl/geoera/ref/7373
references: https://data.geoscience.earth/ncl/geoera/ref/7295
sf touches: Fichtelnaab Fault Zone
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1453
broader: Moldanubian Zone tectonic boundaries

Fichtelnaab lateral faults
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.552Z
preferred label: Fichtelnaab Quer-Störungen @de
notation: DE-BY_1452
definition: Schar SW-NE streichender, saigerer bis subvertikaler Störungen die rechtwinklig bis stumpfwinklig zur Fichtelnaab Störungstone [DE-BY_1451] verlaufen. @de
definition: Set of SW-NE striking, vertical to subvertical faults trending perpendicular to obtuse-angled to Fichtelnaab Fault Zone [DE-BY_1451].
references: https://data.geoscience.earth/ncl/geoera/ref/7360
references: https://data.geoscience.earth/ncl/geoera/ref/7295
sf touches: Fichtelnaab Fault Zone
sf touches: Nottersdorf Fault Zone
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1452
broader: Moldanubian Zone tectonic boundaries

Fichtelnaab Fault Zone
limit type: reverseFault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/7309
type: Concept
created: 2021-01-25T14:23:19.525Z
preferred label: Fichtelnaab Störungszone @de
notation: DE-BY_1451
alternative label: Fichtelnaab Fault
alternative label: SE4 (Seismic Event 4)
alternative label: Fichtelnaab Störung @de
alternative label: Seismischer Reflektor SE3 @de
definition: NW-SE to W-E trending, steeply to intermediately NE to N dipping major tectonic structure branching off and kinematically related to Franconian Line [DE-BY_1398] with a (cumulative) vertical displacement of about 1.7 km (Wagner et al. 1997). Main development phases have been late Variscan NE-SW compression, dextral movement during Early Cretaceous, and the uplift of the Variscan Basement and the overthrust of the foreland during Late Cretaceous and Paleogene (Zulauf 1991). In its northern part eastern boundary of the Zone of Erbendorf-Vohenstrauss (ZEV) featuring a composition very much resembling the lithological units of the Teplá-Barrandian Terrane, thus considered an outlier of the “Bohemicum”, to the west bound by Franconian Line [DE-BY_1398] and in the south reaching to Luhe Fault [DE-BY_965].
definition: NW-SW bis W-E verlaufende, steil bis mäßig steil nach NE bis N einfallende Großstruktur die von der Fränkischen Linie [DE-BY_1398] abzweigt, mit dieser kinematisch verbunden ist und nach Markerzonen (Wagner et al. 1997) einen (kumulativen) Vertikalversatz von etwa 1,7 km aufweist. Haupt-Entstehungsphasen waren nach Zulauf (1991): Anlage während der postvarizischen NE-SW Kompression, dextrale Bewegungen während der N-S Kompression in der Unterkreide, Aufschiebung und Hebung des Grundgebirges auf das Vorland während der alpidischen Gebirgsbildung (Oberkreide bis Paläogen). Östliche Begrenzung der Zone von Erbendorf-Vohenstrauß (ZEV), die kompositionell stark den lithologischen Einheiten des Teplá-Barrandiums gleicht und daher als Überschiebungsklippe des "Bohemikum" angesehen wird, die sich im Süden bis zur Luhe Störung [DE-BY_965] erstreckt und im Westen von der Fränkischen Linie [DE-BY_1398] begrenzt wird. @de
references: https://data.geoscience.earth/ncl/geoera/ref/7376
references: https://data.geoscience.earth/ncl/geoera/ref/7360
references: https://data.geoscience.earth/ncl/geoera/ref/7373
references: https://data.geoscience.earth/ncl/geoera/ref/7295
sf touches: Fichtelnaab lateral faults
sf touches: Nottersdorf Fault Zone
sf touches: Hahneneggaten-Grötschenreuth Fault
in scheme: Tectonic Boundary Objects in Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11578
notation: LfU-BY_1451
broader: Moldanubian Zone tectonic boundaries

Runding Zone
limit type: https://data.geoscience.earth/ncl/geoera/geoconnect3d/category/57
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6358
type: Concept
created: 2021-01-25T14:23:18.282Z
preferred label: Rundinger Zone @de
notation: DE-BY_1348
definition: Von Pempfling NW von Cham, verzweigt in zwei Teiläste nach Langdorf und Regen, über ca. 50 km ziehende, NW-SE verlaufende, steil nach NE einfallende spätvariszische mylonitische Scherzone parallel zur Pfahl Scherzone [DE-BY_1362] (Regen Ast: parallel zum NNW-SSE Trend der Rattenberg Zone [DE-BY_1349]). Diese Scherzone wird von späteren vertikalen Störungen und Mineralgängen gekreuzt, weist aber keinen hydrothermalen Gangquarz im Streichen auf. @de
definition: Running for about 50 km from Pempfling NW of Cham, branched in two tail ends to Langdorf and Regen. This overall NW-SE trending steeply NE dipping Late Varican mylonitic shear zone parallel to Pfahl Shear Zone [DE-BY_1362] (Regen branch: paralleling the NNW-SSE trend of Rattenberg Zone [DE-BY_1349]) is intersected by later vertical faults and mineral veins but does not feature hydrothermal vein quartz along the strike.
narrower: Runding Zone Subsidiary Faults
narrower: Runding Zone Lateral Faults
narrower: Runding Zone extension faults
narrower: Runding Zone Horsetail Splay
references: https://data.geoscience.earth/ncl/geoera/ref/4151
references: https://data.geoscience.earth/ncl/geoera/ref/7258
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1348
broader: Moldanubian Zone tectonic boundaries

Runding Zone extension faults
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:18.365Z
preferred label: Rundinger Zone Längsstörungen @de
notation: DE-BY_1476
definition: Grob NW-SE verlaufende, saigere bis subvertikale Störungen die die Hauptstreichrichtung der Rundiger Zone nach SE hin fortsetzen. @de
definition: Roughly NW-SE trending vertical to subvertical faults sustaining the principal strike direction of Runding Zone to the southeast.
references: https://data.geoscience.earth/ncl/geoera/ref/7261
references: https://data.geoscience.earth/ncl/geoera/ref/6358
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1476
broader: Runding Zone

Runding Zone Lateral Faults
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:18.337Z
preferred label: Rundinger Zone Querstörungen @de
notation: DE-BY_1474
definition: Saigere bis subvertikale Störungen senkrecht zum Streichen der Rundinger Zone verlaufen. @de
definition: Vertical to subvertical faults trending perpendicular to the strike of Runding Zone.
references: https://data.geoscience.earth/ncl/geoera/ref/7342
references: https://data.geoscience.earth/ncl/geoera/ref/6358
sf touches: Runding Zone
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1474
broader: Runding Zone

Runding Zone Subsidiary Faults
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:18.309Z
preferred label: Rundinger Zone Nebenstörungen @de
notation: DE-BY_1473
definition: Saigere bis subvertikale Störungen die subparallel bis spitzwinklig zum Streichen der Rundinger Zone verlaufen. @de
definition: Vertical to subvertical faults trending subparallel or acute-angled to the strike of Runding Zone.
references: https://data.geoscience.earth/ncl/geoera/ref/6358
references: https://data.geoscience.earth/ncl/geoera/ref/7342
references: https://data.geoscience.earth/ncl/geoera/ref/7258
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1473
broader: Runding Zone

Runding Zone Horsetail Splay
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6358
type: Concept
created: 2021-01-25T14:23:18.392Z
preferred label: Rundinger Zone Wedel @de
notation: DE-BY_1475
definition: Gleich wie die Abteiland Diagonal Störungen [DE-BY_1416] für die Pfahl Scherzone werden diese kleinräumigen, saigeren bis sub-vertikalen Störungen östlich von Zwiesel, die radialstrahlig SSW-NNE bis WNW-ESE verlaufen, als "Pferdeschwanz"-Auffiederungen (horsetail splays) der Rundinger Zone [DE-BY_1348] interpretiert (Eberts et al. 2021). @de
definition: Likewise Abteiland Diagonal Faults [DE-BY_1416] for the Pfahl Shear Zone, these small-scale vertical to subvertical faults east of Zwiesel, trending radially SSW-NNE to WNW-ESE, are interpreted horsetail splays (Eberts et al. 2021) of Runding Zone [DE-BY_1348].
references: https://data.geoscience.earth/ncl/geoera/ref/7279
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1475
broader: Runding Zone

Waldthurn-Vohenstrauss Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.497Z
preferred label: Waldthurn-Vohenstrauß Störung @de
notation: DE-BY_1492
definition: Zwischen Ellenbach und Kößing verfolgbare Ostgrenze der Zone von Erbendorf-Vohenstrauß (ZEV), einer Überschiebungsinsel der Teplá-Barrandium Domäne. Insgesamt N-S verlaufende, saigere bis subvertikale Störung, deren geknickter NNW-SSE und NNE-SSW Verlauf in Abschnitten dem Trend der Herzynische Strukturen des Oberpfälzer Waldes [DE-BY_1454] folgt. Verbindung zwischen der Luhe Störung [DE-BY_965] und der Cham Störung [DE-BY_1408]. @de
definition: Traceable between Ellenbach and Kössing eastern boundary of Erbendorf-Vohenstrauss Zone (ZEV), an outlier of Teplá-Barrandian domain. Overall N-S trending, vertical to subvertical fault. Its kinked NNW-SSE and NNE-SSW trend in segments resumes the strike of the Upper Palatine Forest Hercynian structures [DE-BY_1454]. Link between Luhe Fault [DE-BY_965] and Cham Fault [DE-BY_1408].
references: https://data.geoscience.earth/ncl/geoera/ref/7295
sf touches: Cham Fault
sf touches: Luhe Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1492
broader: Moldanubian Zone tectonic boundaries

Upper Palatine Forest Hercynian structures
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.469Z
preferred label: Herzynische Strukturen des Oberpfälzer Waldes @de
notation: DE-BY_1454
definition: Flach herzynisch (100-120°) streichende, saigere bis subvertikale Störungen und Quarzgänge, ± parallel zur Westböhmischen Scherzone [DE-BY_1353] auf tschechischem Gebiet. @de
definition: Flat-angle Hercynian (100-120°) striking, vertical to subvertical faults and quartz veins, more or less paralleling West Bohemian Shear Zone [DE-BY_1353] on Czech territory.
references: https://data.geoscience.earth/ncl/geoera/ref/7295
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1454
broader: Moldanubian Zone tectonic boundaries

Waldmünchen-Gleissenberg Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.441Z
preferred label: Waldmünchen-Gleißenberg Störung @de
notation: DE-BY_1472
definition: NNW-SSE streichende Hauptstörung mit einer NNE-SSW verlaufenden Zweigstörung in der Überganszone der Bayerwald Meridional Störungen [DE-BY_1350] zu den herzynischen Strukturen des Oberpfälzer Waldes [DE-BY_1454]. Die Hauptstörung übernimmt dabei den Trend der herzynischen Strukturen des Oberpfälzer Waldes [DE-BY_1454], mehr oder weniger parallel zum Verlauf der Westböhmischen Scherzone [DE-BY_1353] auf tschechischem Gebiet. @de
definition: NNW-SSE striking main fault with a NNE-SSW trending branch overlapping the transition zone of Bayerwald Meridional Faults [DE-BY_1350] and Upper Palatine Forest Hercynian structures [DE-BY_1454]. The main fault adopts the strike of Upper Palatine Forest Hercynian structures [DE-BY_1454], more or less paralleling West Bohemian Shear Zone [DE-BY_1353] on Czech territory.
references: https://data.geoscience.earth/ncl/geoera/ref/7334
references: https://data.geoscience.earth/ncl/geoera/ref/7295
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1472
broader: Moldanubian Zone tectonic boundaries

Waldmünchen Faults
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.414Z
preferred label: Waldmünchen Störungen @de
notation: DE-BY_1471
definition: Schar NNW-SSE bis NW-SE verlaufender, ± vertikaler Störungen in der Überganszone der Bayerwald Meridional Störungen [DE-BY_1350] zu den herzynischen Strukturen des Oberpfälzer Waldes [DE-BY_1454]. @de
definition: Array of NNW-SSE to NW-SE trending ± vertical faults in the transition zone of Bayerwald Meridional Faults [DE-BY_1350] and Upper Palatine Forest Hercynian structures [DE-BY_1454].
references: https://data.geoscience.earth/ncl/geoera/ref/7334
references: https://data.geoscience.earth/ncl/geoera/ref/7295
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1471
broader: Moldanubian Zone tectonic boundaries

Tiefenbach-Treffelstein Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.386Z
preferred label: Tiefenbach-Treffelstein Störung @de
notation: DE-BY_1470
definition: NW-SE streichende, saigere bis subvertikale Störung in der Überganszone der Bayerwald Meridional Störungen [DE-BY_1350] zu den herzynischen Strukturen des Oberpfälzer Waldes [DE-BY_1454]. @de
definition: NW-SE striking vertical to subvertical fault in the transition zone of Bayerwald Meridional Faults [DE-BY_1350] and Upper Palatine Forest Hercynian structures [DE-BY_1454].
references: https://data.geoscience.earth/ncl/geoera/ref/7334
references: https://data.geoscience.earth/ncl/geoera/ref/7295
sf touches: Bayerwald Meridional Faults
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1470
broader: Moldanubian Zone tectonic boundaries

Bayerwald Meridional Faults
limit type: strikeSlipFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:18.530Z
preferred label: Bayerwald Meridional Störungen @de
notation: DE-BY_1350
definition: Überwiegend aus dem Verlauf von Tälern abgeleitet, im km-Bereich weitständig subparallel, übergeordnet N-S (NNW-SSE bis NNE-SSW) verlaufende Störungsschar steil einfallender bis saigerer Störungen vorwiegend im Vorderen Bayerischen Wald. Diese stumpfwinklig zur Pfahl Scherzone [DE-BY_1362] und Rundinger Zone [DE-BY_1348] verlaufenden Scherbrüche können als R‘- oder P'-Riedelbrüche interpretiert werden, die während der frühen Stadien der Scherung angelegt werden, aber sich dabei nicht weit fortpflanzen, als präexistente Klüfte bei einer späteren Reaktivierung aber vergrößert und verlängert wurden. Bedingt durch die spät- bis postvariszische bruchhaft-spröde Deformation und Hebung, und deren Reaktivierung während der Unterkreide und im Alttertiär als Fernwirkung der alpinen Gebirgsbildung, wird das Terrain schollenartig zerlegt (Teipel et al. 2013) und die tertiäre Talbildung vorgezeichnet. @de
definition: Mostly inferred from the conspicuous trend of valleys, array of subparallel, km-spaced, overall N-S (NNW-SSE to NNE-SSW) trending, steeply dipping to vertical faults predominantly transecting the Anterior Bavarian Forest aka Danube Hills. These faults, obtuse angled with respect to the Pfahl Shear Zone [DE-BY_1362] and Runding Zone [DE-BY_1348] may be interpreted R’- or P'-Riedel shears, i.e. subsidiary shear fractures accommodating strain in the fault zone, coeval with the main wrench faulting and propagating a short distance out it, however enlarged and extended during later reactivation. This late to post-Variscan brittle deformation and the uplift of the terrain led to a slab-like fragmentation, reactivated during Late Cretaceous and Paleogene as a distant effect of the Alpine orogenesis, and predetermined the Tertiary valley formation (Teipel et al. 2013).
narrower: Teisnach-Deggendorf Fault
narrower: Hunderdorf Fault
narrower: Kollnburg-Schwarzach Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7255
references: https://data.geoscience.earth/ncl/geoera/ref/6358
references: https://data.geoscience.earth/ncl/geoera/ref/7340
references: https://data.geoscience.earth/ncl/geoera/ref/7363
sf touches: Bavarian Pfahl
sf touches: Abteiland Diagonal Faults
sf touches: Runding Zone
sf touches: Runding Zone extension faults
sf touches: Grötschenreuth-Siegritz Fault
sf touches: Steinach-Deggendorf Fault
sf touches: Münster Fault
sf touches: Donaurand Fault Scarp
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1350
broader: Moldanubian Zone tectonic boundaries

Kollnburg-Schwarzach Fault
limit type: obliqueSlipFault
type: Fault
type: Limit
definition: N-S bis NNW-SSE verlaufender Störungszug steil einfallender bis saigerer Bayerwald Meridional Störungen zwischen Kollnburg nahe der Pfahl Scherzone [DE-BY_1362] und dem Donaurandbruch [DE-BY_698] südlich von Schwarzach. Die südlichen Abschnitte bilden den Ostrand der Stallwanger Furche. @de
type: Concept
created: 2021-01-25T14:23:18.612Z
preferred label: Kollnburg-Schwarzach Störung @de
notation: DE-BY_1352
definition: Linear array of N-S to NNW-SSE trending steeply dipping to vertical Bayerwald Meridional Faults between Kollnburg close to the Pfahl Shear Zone [DE-BY_1362] and Donaurand Fault Scarp [DE-BY_698] south of Schwarzach. Southern sections form the eastern boundary of Stallwang Trench (Stallwanger Furche).
references: https://data.geoscience.earth/ncl/geoera/ref/6358
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1352
broader: Bayerwald Meridional Faults

Hunderdorf Fault
limit type: obliqueSlipFault
type: Fault
type: Limit
definition: Running from Hunderdorf to Danube river, NNW-SSE striking steeply dipping to vertical dextral oblique-slip fault slightly displacing the Danube Fault Scarp [DE-BY_698] and Steinach-Deggendorf Fault [DE-BY_1538].
definition: Von Hunderdorf zur Donau verlaufende, NNW-SSE streichende, steil einfallende bis saigere, rechtssinnige Querverschiebung, die den Donaurandbruch [DE-BY_698] und die Steinach-Deggendorf Fault [DE-BY_1538] leicht versetzt. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6358
type: Concept
created: 2021-01-25T14:23:18.585Z
preferred label: Hunderdorf Störung @de
notation: DE-BY_1535
references: https://data.geoscience.earth/ncl/geoera/ref/7325
references: https://data.geoscience.earth/ncl/geoera/ref/7279
sf touches: Donaurand Fault Scarp
sf touches: Steinach-Deggendorf Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1535
broader: Bayerwald Meridional Faults

Teisnach-Deggendorf Fault
limit type: obliqueSlipFault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6358
type: Concept
created: 2021-01-25T14:23:18.557Z
preferred label: Teisnach-Deggendorf Störung @de
notation: DE-BY_1351
definition: Von Asbach nördlich von Teisnach, über die Pfahl Scherzone [DE-BY_1362] bis nach Deggendorf verlaufender, längster und auffälligster Vertreter der Bayerwald Meridional Störungen. Setzt sich, im Kollbachtal verschoben, SSE-wärts bis in das randliche Molassebecken fort, wo die Störung den Donaurandbruch [DE-BY_698] leicht versetzt. @de
definition: The longest and most conspicuous member of the Bayerwald Meridional Fault running from Asbach north of Teisnach, crossing Pfahl Shear Zone [DE-BY_1362] at Pattersdorf, to Deggendorf and, offset in Kollbach Valley, further into the marginal Molasse Basin thereby slightly displacing the Danube Fault Scarp [DE-BY_698].
references: https://data.geoscience.earth/ncl/geoera/ref/7341
references: https://data.geoscience.earth/ncl/geoera/ref/7326
sf touches: Bavarian Pfahl
sf touches: Donaurand Fault Scarp
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1351
broader: Bayerwald Meridional Faults

Kittenrain Faults
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.083Z
preferred label: Kittenrain Störungen @de
notation: DE-BY_1482
definition: Subparalleles Paar NW-SW verlaufender, saigerer bis subvertikaler Störungen überwiegend als Quarz (+ Flußspat) Gänge, im Süden vom Donaurandbruch [DE-BY_698] begrenzt. @de
definition: Subparallel pair of NW-SW trending, vertical to subvertical faults predominantly manifested in quartz (+ fluorite) veins, in the south truncated by Donaurand Fault Scarp [DE-BY_698].
references: https://data.geoscience.earth/ncl/geoera/ref/6358
references: https://data.geoscience.earth/ncl/geoera/ref/7300
references: https://data.geoscience.earth/ncl/geoera/ref/7320
sf touches: Keilberg-Burgberg Faults
sf touches: Donaurand Fault Scarp
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1482
broader: Moldanubian Zone tectonic boundaries

Falkensteiner Vorwald Faults
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.055Z
preferred label: Falkensteiner Vorwald Störungen @de
notation: DE-BY_1481
definition: Der Falkensteiner Vorwald, der westlichste Ausläufer des Bayerischen Waldes, wird von plutonischer Kleintektonik der karbonischen Granit-Komplexe dominiert. Neben diesen kleinräumigen Texturen treten nur wenige ± vertikale Störungen, ohne vorherrschende Streichrichtung auf. Demgegenüber zeigen die post-granitischen Gänge, die im Westteil des Falkensteiner Vorwalds gehäuft auftreten, eine bevorzugte Orientierung subparallel zum Keilberg Störungssystem [DE-BY_1484] und den Bayerwald Meridional Störungen [DE-BY_1350]. @de
definition: The Falkensteiner Vorwald (Falkenstein Anterior Forest), the westernmost foothills of the Bavarian Forest, is dominated by primary features of the Carboniferous granite batholith complexes. Beyond these small-scale textures only few ± vertical faults occur featuring no predominant strike direction. The post-granitic dykes accumulating in the western part of Falkensteiner Vorwald, however, show a preferred orientation subparallel to Keilberg Fault System [DE-BY_1484] and the Bayerwald Meridional Faults [DE-BY_1350].
references: https://data.geoscience.earth/ncl/geoera/ref/7320
references: https://data.geoscience.earth/ncl/geoera/ref/6358
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1481
broader: Moldanubian Zone tectonic boundaries

Rattenberg Zone
narrower: Dietersdorf Fault
limit type: https://data.geoscience.earth/ncl/geoera/geoconnect3d/category/57
type: Fault
type: Limit
definition: NNW-SSE trending, vertical to steeply WSW dipping Late Variscan mylonitic shear zone running from Dietersdorf to Haigrub; eastern boundary of Stallwang Trench (Stallwanger Furche).
references: https://data.geoscience.earth/ncl/geoera/ref/4151
type: Concept
created: 2021-01-25T14:23:18.420Z
preferred label: Rattenberger Zone @de
notation: DE-BY_1349
definition: NNW-SSE verlaufende, saigere bis steil nach WSW einfallende spätvariszische mylonitische Scherzone zwischen Dietersdorf und Haigrub; Ostrand der Stallwanger Furche. @de
narrower: St. Englmar Fault
narrower: Rattenberg-Haselbach Fault
references: https://data.geoscience.earth/ncl/geoera/ref/6358
references: https://data.geoscience.earth/ncl/geoera/ref/7339
sf touches: Bayerwald Meridional Faults
in scheme: Tectonic Boundary Objects in Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11690
notation: LfU-BY_1349
broader: Moldanubian Zone tectonic boundaries

Rattenberg-Haselbach Fault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6358
type: Concept
created: 2021-01-25T14:23:18.502Z
preferred label: Rattenberg-Haselbach Störung @de
notation: DE-BY_1536
definition: N-S bis NNE-SSW verlaufende, saigere bis steil einfallende Störung; vermuteter Ostrand der Stallwanger Furche. @de
definition: N-S to NNE-SSW trending, vertical to steeply dipping fault; assumed eastern boundary of Stallwang Trench (Stallwanger Furche).
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1536
broader: Rattenberg Zone

St. Englmar Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:18.475Z
preferred label: St. Englmar Störung @de
notation: DE-BY_1359
definition: NNW-SSE streichende, saigere bis steil einfallende Störung, im Nordteil mit der Rattenberger Zone [DE-BY_1349] zusammenlaufend, im Südteil parallel zum südlichen Ausläufer dieser mylonitischen Scherzone. @de
definition: NNW-SSE striking, vertical to steeply dipping fault converging with Rattenberg Zone [DE-BY_1349] in the north and paralleling the southern tail of this mylonitic shear zone in the south.
references: https://data.geoscience.earth/ncl/geoera/ref/6358
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1359
broader: Rattenberg Zone

Dietersdorf Fault
definition: Slightly arcuate N-S to NNW-SSE trending, vertical to steeply dipping fault, in its northern part truncating Rattenberg Zone [DE-BY_1349], in its southern part paralleling this mylonitic shear zone. Assumed eastern boundary of Stallwang Trench (Stallwanger Furche).
type: Concept
created: 2021-01-25T14:23:18.447Z
preferred label: Dietersdorf Störung @de
notation: DE-BY_1358
definition: Leicht gebogen N-S bis NNW-SSE verlaufende, saigere bis steil einfallende Störung, im Nordteil Begrenzung der Rattenberger Zone [DE-BY_1349], im Südteil parallel zu dieser mylonitischen Scherzone. Vermuteter Ostrand der Stallwanger Furche. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6358
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1358
broader: Rattenberg Zone

Schwaighof-Momansfelden Fault
limit type: reverseFault
type: Fault
type: Limit
preferred label: Schwaighof-Momansfelden Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/6358
type: Concept
created: 2021-01-25T14:23:19.027Z
notation: DE-BY_1480
definition: NW-SE verlaufende, steil nach NE einfallende Intra-Grundgebirge Störung, wahrscheinlich Aufschiebung. @de
definition: NW-SE trending, steeply NE dipping intra-basement fault, probably reverse fault.
references: https://data.geoscience.earth/ncl/geoera/ref/7323
references: https://data.geoscience.earth/ncl/geoera/ref/7320
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1480
broader: Moldanubian Zone tectonic boundaries

Trasching-Michelsneukirchen Faults
limit type: reverseFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.000Z
preferred label: Trasching-Michelsneukirchen Störungen @de
notation: DE-BY_1478
definition: Am Südwest-Rand der Bodenwöhrer Senke parallel zur Nordrand-Störung, dem Pfahl Überschiebungssystem [DE-BY_ 1363], ziehende Störungen, die Grundgebirgs-Schollen auf die randlichen Kreide-Ablagerungen der Bödenwöhrer Senke aufschieben. Grob NW-SE bis WNW-ESE verlaufende, mäßig steil nach NE einfallende Auf- bzw. Überschiebungen mit einen (Residual-) Versatz von etwa 100 m. @de
definition: Forming the southwestern margin of Bodenwöhr Through with the same orientation as the northern margin Pfahl Reverse Fault System [DE-BY_ 1363], roughly NW-SE to WNW-ESE trending, moderately NE dipping reverse resp. thrust faults with a (residual) displacement of about 100 m, thrusting basement blocks onto the marginal Cretaceous deposits of Bodenwöhr Trough.
references: https://data.geoscience.earth/ncl/geoera/ref/6358
references: https://data.geoscience.earth/ncl/geoera/ref/7323
references: https://data.geoscience.earth/ncl/geoera/ref/7320
sf touches: Wetterfeld-Höhhof Fault
sf touches: Höhhof-Rattiszell Fault
in scheme: Tectonic Boundary Objects in Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11691
notation: LfU-BY_1478
broader: Moldanubian Zone tectonic boundaries

Cham Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:18.667Z
preferred label: Cham Störung @de
notation: DE-BY_1408
alternative label: Cham Fault System
alternative label: Cham Störungssystem @de
definition: NNW-SSE streichende tektonische Struktur krustalen Ausmaßes, die von nahe der Luhe Störung [DE-BY_965], im nördlichen Abschnitt parallel zur Westböhmischen Scherzone [DE-BY_1353] auf tschechischem Gebiet, den Bayerischen Pfahl [DE-BY_1347] bei Cham querend, bis zum Donaurandbruch [DE-BY_698] verläuft. Aus den Grenzlinien benachbarter Domänen unterschiedlicher Lithologie (Metamorphosegrad) abgeleitet, äußert sich diese bedeutende tektonische Struktur in diskontinuierlichen Segmenten aufgeschlossener Störungen oder Quarzgänge. @de
definition: NNW-SSE trending tectonic structure of crustal extend, running from close to Luhe Fault [DE-BY_965], in its northern part paralleling West Bohemian Shear Zone [DE-BY_1353] on Czech territory, across the Bavarian Pfahl [DE-BY_1347] near Cham to Donaurand Fault Scarp [DE-BY_698]. Inferred from the borderlines of juxtaposed contrasting lithological (metamorphic grade) domains this major tectonic structure is manifests itself in discontinuous exposed fault segments and quartz veins.
narrower: Obertresenfeld-Braunetsrieth dike swarm
narrower: Pullenried-Winklarn dike swarm
narrower: Thanstein Fault
narrower: Rötz-Grossenzenried Fault
narrower: Stamsried Fault
narrower: Bernried-Rattiszell Fault
narrower: Wetterfeld-Höhhof Fault
narrower: Höhhof-Rattiszell Fault
narrower: Ascha-Furth Fault
narrower: Mitterfels-Bogen Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7279
in scheme: Tectonic Boundary Objects in Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11690
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11691
notation: LfU-BY_1408
broader: Moldanubian Zone tectonic boundaries

Mitterfels-Bogen Fault
limit type: obliqueSlipFault
type: Fault
type: Limit
preferred label: Mitterfels-Bogen Störung @de
type: Concept
created: 2021-01-25T14:23:18.944Z
notation: DE-BY_1486
definition: Südlichstes Ost-Segment der Cham Störung [DE-BY_1408], als eine der größeren Bayerwald Meridional Störungen [DE-BY_1350]. N-S bis NNW-SSE verlaufende, steil bis senkrecht stehende rechtssinnige Schrägverschiebung die die Münster Graben Störung [DE-BY_1485] abschneidet und die Steinach-Deggendorf Störung [DE-BY_1538] sowie den Donaurandbruch [DE-BY_698] versetzt. @de
definition: Major Bayerwald Meridional Fault [DE-BY_1350] forming the southernmost eastern segment of Cham Fault [DE-BY_1408] . N-S to NNW-SSE trending, steeply dipping to vertical dextral oblique-slip fault truncating Münster Graben Fault [DE-BY_1485] and displacing Steinach-Deggendorf Fault [DE-BY_1538] as well as Donaurand Fault Scarp [DE-BY_698].
references: https://data.geoscience.earth/ncl/geoera/ref/7255
references: https://data.geoscience.earth/ncl/geoera/ref/7325
references: https://data.geoscience.earth/ncl/geoera/ref/7279
references: https://data.geoscience.earth/ncl/geoera/ref/6358
references: https://data.geoscience.earth/ncl/geoera/ref/7257
sf touches: Donaurand Fault Scarp
sf touches: Münster Fault
sf touches: Steinach-Deggendorf Fault
sf touches: Münster Graben Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1486
broader: Cham Fault

Ascha-Furth Fault
limit type: obliqueSlipFault
type: Fault
type: Limit
preferred label: Ascha-Furth Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/6358
type: Concept
created: 2021-01-25T14:23:18.917Z
notation: DE-BY_1537
definition: Südlichstes West-Segment der Cham Störung [DE-BY_1408], als eine der größeren Bayerwald Meridional Störungen [DE-BY_1350]. N-S bis NNW-SSE verlaufende, steil nach NE bis ENE einfallende bis senkrecht stehende rechtssinnige Schrägverschiebung die die Münster Störung [DE-BY_1539] abschneidet und die Steinach-Deggendorf Störung [DE-BY_1538] sowie den Donaurandbruch [DE-BY_698] versetzt. Westliche Grenze der Stallwanger Furche. @de
definition: Southernmost western segment of Cham Fault [DE-BY_1408] and a major Bayerwald Meridional Fault [DE-BY_1350]. N-S to NNW-SSE trending, steeply E to ENE dipping to vertical dextral oblique-slip fault truncating Münster Fault [DE-BY_1539] and displacing Steinach-Deggendorf Fault [DE-BY_1538] as well as Donaurand Fault Scarp [DE-BY_698]. Western boundary of Stallwang Trench (Stallwanger Furche).
references: https://data.geoscience.earth/ncl/geoera/ref/7255
references: https://data.geoscience.earth/ncl/geoera/ref/7352
references: https://data.geoscience.earth/ncl/geoera/ref/7279
references: https://data.geoscience.earth/ncl/geoera/ref/7257
sf touches: Donaurand Fault Scarp
sf touches: Münster Fault
sf touches: Steinach-Deggendorf Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1537
broader: Cham Fault

Höhhof-Rattiszell Fault
type: Fault
type: Limit
definition: Section of Cham Fault [DE-BY_1408] south of merger with Trasching-Michelsneukirchen Faults [DE-BY_1478] and western boundary of Stallwang Trench (Stallwanger Furche) as inferred by Eberts et al. (2021). Slightly undulate NNW-SSE trending, steeply ENE dipping to vertical normal fault, in sections manifested in quartz veins. Southern continuation of Wetterfeld-Höhhof Fault [DE-BY_1479], the structured Bodenwöhr Trough eastern boundary.
type: Concept
created: 2021-01-25T14:23:18.889Z
preferred label: Höhhof-Rattiszell Störung @de
notation: DE-BY_1360
definition: Abschnitt der Cham Störung [DE-BY_1408] südlich ihrer Verschmelzung mit den Trasching-Michelsneukirchen Störungen [DE-BY_1478] und der westlichen Begrenzung der Stallwanger Furche nach Eberts et al. (2021). Leicht gewellt NNW-SSE verlaufende, steil nach ENE einfallende bis senkrecht stehende Störung, abschnittsweise von Quarz-Gängen vertreten. Südliche Fortsetzung der Wetterfeld-Höhhof Fault [DE-BY_1479], als strukturiertem Ostrand der Bodenwöhrer Senke. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6358
references: https://data.geoscience.earth/ncl/geoera/ref/7323
references: https://data.geoscience.earth/ncl/geoera/ref/7279
sf touches: Trasching-Michelsneukirchen Faults
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1360
limit type: normalFault
broader: Cham Fault

Wetterfeld-Höhhof Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:18.861Z
preferred label: Wetterfeld-Höhhof Störung @de
notation: DE-BY_1479
definition: Abschnitt des West-Astes der Cham Störung [DE-BY_1408] als Ostgrenze der Bödenwöhrer Senke und von Eberts et al. (2021) abgeleitete westliche Begrenzung der Stallwanger Furche. Insgesamt NNW-SSE verlaufende, steil nach ENE einfallende bis saigere Abschiebung, abschnittsweise in zwei Äste aufgespalten und von Querstörungen versetzt. Setzt sich im Süden als Höhhof-Rattiszell Störung [DE-BY_1360] fort. @de
definition: Section of the western branch of Cham Fault [DE-BY_1408] representing the structured Bodenwöhr Trough eastern boundary and the inferred western boundary of Stallwang Trench (Stallwanger Furche) (Eberts et al. 2021). Overall NNW-SSE trending, steeply ENE dipping to vertical normal fault in sections split up in two branches and displaced by lateral faults. Continues as Höhhof-Rattiszell Fault [DE-BY_1360] in the south.
references: https://data.geoscience.earth/ncl/geoera/ref/6358
references: https://data.geoscience.earth/ncl/geoera/ref/7323
references: https://data.geoscience.earth/ncl/geoera/ref/7279
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1479
limit type: normalFault
broader: Cham Fault

Bernried-Rattiszell Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:18.833Z
preferred label: Bernried-Rattiszell Störung @de
notation: DE-BY_1357
definition: Östlicher Ast der Cham Störung [DE-BY_1408], im Norden über den Kleine(i)nzenrieder Nebenpfahl (Dorn 1936) mit dem West-Ast verbunden. Leicht gewellt N-S bis NNW-SSE verlaufende, diskontinuierliche und abschnittsweise von Quarz-Gängen vertretene, steil bis senkrecht stehende Störung, die die Pfahl Scherzone DE-BY_1362] im Regental westlich von Cham kreuzt. Im südlichen Abschnitt verläuft die Störung östlich subparallel zum strukturierten Ostrand der Bodenwöhrer Senke und der damit verbundenen Höhhof-Rattiszell Störung [DE-BY_1360]. @de
definition: Eastern branch of Cham Fault [DE-BY_1408], in the north merging with the western branch via Kleinenzenrieder Nebenpfahl (Dorn 1936). Slightly undulate N-S to NNW-SSE trending, discontinuous and in sections manifested in quartz veins, steeply dipping to vertical fault crossing Pfahl Shear Zone [DE-BY_1362] in the Regen river valley west of Cham. In its southern section running easterly subparallel to the structured Bodenwöhr Trough eastern boundary and linked Höhhof-Rattiszell Fault [DE-BY_1360].
references: https://data.geoscience.earth/ncl/geoera/ref/7365
references: https://data.geoscience.earth/ncl/geoera/ref/7323
references: https://data.geoscience.earth/ncl/geoera/ref/7277
references: https://data.geoscience.earth/ncl/geoera/ref/7320
references: https://data.geoscience.earth/ncl/geoera/ref/6358
sf touches: Bavarian Pfahl
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1357
broader: Cham Fault

Stamsried Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:18.805Z
preferred label: Stamsried Störung @de
notation: DE-BY_1413
definition: NNW-SSE verlaufendes, saiger bis steilstehendes Störungssegment des westlichen Astes der Cham Störung [DE-BY_1408]. Südliche Fortsetzung der Rötz-Großenzenried Störung [DE-BY_1412]. @de
definition: NNW-SSE trending, vertical to subvertical fault segment of Cham Fault [DE-BY_1408] western branch. Southern continuation of Rötz-Grossenzenried Fault [DE-BY_1412].
references: https://data.geoscience.earth/ncl/geoera/ref/6358
references: https://data.geoscience.earth/ncl/geoera/ref/7365
references: https://data.geoscience.earth/ncl/geoera/ref/7320
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1413
broader: Cham Fault

Rötz-Grossenzenried Fault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6358
type: Concept
created: 2021-01-25T14:23:18.777Z
preferred label: Rötz-Großenzenried Störung @de
notation: DE-BY_1412
definition: N-S verlaufender nördlicher Teil des westlichen Astes der Cham Störung [DE-BY_1408]. Läuft im Norden mit dem Kleine(i)nzenrieder Nebenpfahl (Dorn 1936) zusammen, der nördlichen Fortsetzung der Bernried-Rattiszell Störung [DE-BY_1357] als östlichem Ast der Cham Störung. @de
definition: N-S trending northern part of the western branch of Cham Fault [DE-BY_1408]. To the north merging with Kleinenzenrieder Nebenpfahl (Dorn 1936), the northern continuation of Bernried-Rattiszell Fault [DE-BY_1357] representing the Cham Fault Zone eastern branch.
references: https://data.geoscience.earth/ncl/geoera/ref/7335
references: https://data.geoscience.earth/ncl/geoera/ref/7277
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1412
broader: Cham Fault

Thanstein Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:18.750Z
preferred label: Thanstein Störung @de
notation: DE-BY_1411
definition: NNW-SSE verlaufendes, saiger bis steilstehendes Störungssegment der Cham Störung [DE-BY_1408]. @de
definition: NNW-SSE trending, vertical to subvertical fault segment of Cham Fault [DE-BY_1408].
references: https://data.geoscience.earth/ncl/geoera/ref/7335
references: https://data.geoscience.earth/ncl/geoera/ref/7320
references: https://data.geoscience.earth/ncl/geoera/ref/6358
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1411
broader: Cham Fault

Pullenried-Winklarn dike swarm
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:18.722Z
preferred label: Pullenried-Winklarn Gangschar @de
notation: DE-BY_1410
definition: Abfolge steil herzynisch (130-140°) bis NNW-SSE streichender, saigerer bis steilstehender Quarzgänge und kurzer Störungssegmente parallel zu den Herzynische Strukturen des Oberpfälzer Waldes [DE-BY_1454 im Norden und zu den Bayerwald Meridional Störungen [DE-BY_1350] im Süden. @de
definition: Succession of high-angle Hercynian (130-140°) to NNW-SSE striking, vertical to subvertical quartz veins and short fault segments, paralleling the Upper Palatine Forest Hercynian structures [DE-BY_1454] in the north and the Bayerwald Meridional Faults [DE-BY_1350] in the south.
references: https://data.geoscience.earth/ncl/geoera/ref/7278
references: https://data.geoscience.earth/ncl/geoera/ref/7295
references: https://data.geoscience.earth/ncl/geoera/ref/7320
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1410
broader: Cham Fault

Obertresenfeld-Braunetsrieth dike swarm
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:18.694Z
preferred label: Obertresenfeld-Braunetsrieth Gangschar @de
notation: DE-BY_1409
definition: Abfolge steil herzynisch (130-140°) streichender, saigerer bis steilstehender Quarzgänge und kurzer Störungssegmente parallel zu und Teil der Herzynische Strukturen des Oberpfälzer Waldes [DE-BY_1454]. @de
definition: Succession of high-angle Hercynian (130-140°) striking, vertical to subvertical quartz veins and short fault segments, parallel to and part of the Upper Palatine Forest Hercynian structures [DE-BY_1454].
references: https://data.geoscience.earth/ncl/geoera/ref/7287
references: https://data.geoscience.earth/ncl/geoera/ref/7295
references: https://data.geoscience.earth/ncl/geoera/ref/7320
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1409
broader: Cham Fault

Kemnath Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.275Z
preferred label: Kemnather Störung @de
notation: DE-BY_1465
definition: NNW-SSE verlaufende Störung, die im nördlichen Abschnitt Trias (im W) gegen Grundgebirge (im E) versetzt, im südlichen Teil im Grundgebirge verläuft. @de
definition: NNW-SSE trending fault, in its northern part offsetting Triassic deposits in the west towards the Variscan basement in the east, intra-basement in its southern part.
references: https://data.geoscience.earth/ncl/geoera/ref/7264
references: https://data.geoscience.earth/ncl/geoera/ref/7295
in scheme: Tectonic Boundary Objects in Europe
broader: Moldanubian Zone tectonic boundaries

Falkenstein-Frauenau Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:18.640Z
preferred label: Falkenstein-Frauenau Störung @de
notation: DE-BY_1415
definition: Leicht gebogen N-S bis NNW-SSE verlaufende steilstehende bis saigere Störung. @de
definition: Slightly arcuate N-S to NNW-SSE trending steeply dipping to vertical fault.
references: https://data.geoscience.earth/ncl/geoera/ref/7261
references: https://data.geoscience.earth/ncl/geoera/ref/6358
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1415
broader: Moldanubian Zone tectonic boundaries

Stockbach Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.248Z
preferred label: Stockbach Störung @de
notation: DE-BY_1464
definition: N-S streichende Störung westlich von Nabburg. @de
definition: N-S striking fault west of Nabburg.
references: https://data.geoscience.earth/ncl/geoera/ref/7264
references: https://data.geoscience.earth/ncl/geoera/ref/7295
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1464
broader: Moldanubian Zone tectonic boundaries

Bavarian Pfahl
limit type: https://data.geoscience.earth/ncl/geoera/geoconnect3d/category/57
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6358
type: Concept
created: 2021-01-25T14:23:18.007Z
preferred label: Bayerischer Pfahl @de
notation: DE-BY_1347
alternative label: Pfahl Fault System
alternative label: Pfahl-Störungssystem @de
definition: Von Amberg bis zur österreichischen Grenze nordöstlich von Passau und weiter zum Rodl-Kaplice Störungssystem südlich von Oberneukirchen (Oberösterreich) verlaufende, NW-SE streichende, mehr als 200 km lange spätvariszische Scherzone mit spröd-plastischer Deformation. Entstanden durch Krustendehnung mit Seitenverschiebungskomponente, überwiegend dextral, phasenweise sinistral, zeigt der großräumig als Mylonit ausgebildete südöstliche Abschnitt, die Pfahl Scherzone [DE-BY_1362], eine bruchhaft-spröde Reaktivierung mit der Bildung hydrothermaler Quarzgänge. Während der Heraushebung des Westrandes der Böhmischen Masse, als Fernwirkung der alpinen Gebirgsbildung in der Unterkreide und im Alttertiär, wirkte der nordwestliche Abschnitt, das Pfahl Aufschiebungssystem [DE-BY_1363], als Aufschiebungsfläche des Grundgebirges auf das permo-mesozoische Vorland. Hierdurch entstand die Bodenwöhrer Senke. @de
definition: Running from Amberg to the Austrian border NE of Passau and beyond to Rodl-Kaplice Fault System south of Oberneukirchen (Upper Austria), this NW-SE striking, more than 200 km long Late Varican shear zone, is associated with brittle-ductile deformation. Initially subject to rift- and wrench-tectonic with a predominantly dextral, in phases sinistral shearing, the large-scale mylonitic southeastern section, the Pfahl Shear Zone [DE-BY_1362], shows a conspicuous later hydrothermal quartz mineralization forming the nearly vertical zones of Pfahl quartz along the strike. On uplift of the western margins of the Bohemian Massif, as a distant effect of the Alpine orogenesis during Late Cretaceous and Paleogene, particularly in its northwestern section, the Pfahl Reverse Fault System [DE-BY_1363], forms the reverse fault ramp for the movement of the crystalline rocks over the Permo-Mesozoic foreland, shaping the Bodenwöhr Trough.
narrower: Pfahl Shear Zone
narrower: Pfahl Reverse Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/7880
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7296
references: https://data.geoscience.earth/ncl/geoera/ref/822
narrow match: http://resource.geolba.ac.at/structure/147
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1347
broader: Moldanubian Zone tectonic boundaries

Pfahl Shear Zone
limit type: https://data.geoscience.earth/ncl/geoera/geoconnect3d/category/57
type: Limit
type: Fault
references: https://data.geoscience.earth/ncl/geoera/ref/6358
references: https://data.geoscience.earth/ncl/geoera/ref/7880
type: Concept
created: 2021-01-25T14:23:18.033Z
preferred label: Pfahl Scherzone @de
notation: DE-BY_1362
definition: Das prägende Strukturelement des ostbayerischen Grundgebirges ist die Scherzone des Bayerischen Pfahls, eine im Perm angelegtes großräumiges Scherzonensystem, welches später mehrfach reaktiviert wurde. Typische Gesteine sind durch plastische (duktile) Deformation gebildete Mylonite („Pfahlschiefer“) und durch bruchhafte (spröde) Deformation entstandene Kataklasite. Morphologisch treten die verwitterungsresistenten, durch hydrothermale Aktivität und bruchhafte Deformation entstandenen polyphasen Quarzgangbreccien des Bayerischen Pfahls („Pfahlquarz“) am deutlichsten in Erscheinung und bilden häufig langgestreckte Härtlinge. Die ausgedehnten, insgesamt NW-SE verlaufenden Mylonit-Zonen des Pfahls werden bereichsweise von (sub-)parallelen Nebenstörungen und Quarzgängen [DE-BY_1361] begleitet und vereinzelt von den jüngeren Bayerwald Meridional Störungen [DE-BY_1350] versetzt. @de
definition: The Pfahl Shear Zone, one of the most striking tectonic structures of the east-Bavarian Varican Basement rock suites, is a Permian large-scale shear zone system, reactivated multiply in later times. Generic rock types are mylonites (“Pfahl schist”) formed by ductile deformation and cataclastic rocks formed by brittle deformation. Evolving from hydrothermal activity and subsequent brittle tectonics, almost vertical polyphase quartz vein breccia (“Pfahl quartz”), due to their weathering resistance nowadays appearing as elongate monadnocks, are the most prominent physiographical feature. The extensive, overall NW-SE trending mylonite zones are, in certain areas, accompanied by (sub-)parallel subsidiary faults and quartz veins [DE-BY_1361] and sporadically displaced by the younger Bayerwald Meridional Faults [DE-BY_1350].
narrower: Pfahl Shear Zone Subsidiary Faults
narrower: Abteiland Diagonal Faults
narrower: Altendorf-Friedersried Fault
references: https://data.geoscience.earth/ncl/geoera/ref/822
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7294
in scheme: Tectonic Boundary Objects in Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11690
notation: LfU-BY_1362
broader: Bavarian Pfahl

Pfahl Shear Zone Subsidiary Faults
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:18.061Z
preferred label: Pfahl Scherzone Nebenstörungen @de
notation: DE-BY_1361
alternative label: Pfahl Begleitstörungen @de
definition: Neben den großräumigen Strukturelementen wie der Rundinger Zone [DE-BY_1348], die als Nebenast des Pfahl Scherzone [DE-BY_1362] gedeutet wird, und dem Aicha-Halser Nebenpfahl [DE-BY_762], die dem Donaustörungssystem [DE-BY_697] zugrechnet wird, wird die Pfahl Scherzone von kleinräumigen, (sub-)parallel und in räumlicher Nähe NW-SE streichenden Störungen und Quarzgängen begleitet , was eine generische und kinematische Verwandtschaft nahelegt. Die die Mylonitgrenzen spitzwinklig schneidenden Elemente werden als Fiederspalten-System interpretiert (Hofmann 1962). @de
definition: Apart from the large-scale structural elements like Runding Zone [DE-BY_1348], construed as a branch of Pfahl Shear Zone [DE-BY_1362], and Aicha-Halser Nebenpfahl [DE-BY_762], assigned to Danube Fault System [DE-BY_697], Pfahl Shear Zone is accompanied by (sub-)parallel and close-by trending small-scale faults, implying a generic and kinematic relationship. Elements acute-angled to the boundaries of the mylonites are interpreted as tension gashes (Hofmann 1962).
references: https://data.geoscience.earth/ncl/geoera/ref/7313
references: https://data.geoscience.earth/ncl/geoera/ref/6358
references: https://data.geoscience.earth/ncl/geoera/ref/7255
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1361
broader: Pfahl Shear Zone

Altendorf-Friedersried Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:18.116Z
preferred label: Altendorf-Friedersried Störung @de
notation: DE-BY_1414
definition: NW-SE verlaufende, saigere bis sub-vertikale Störung, die spitzwinklig vom Nordwest-Ast der Pfahl Scherzone [DE-BY_1362] ausschert. @de
definition: NW-SE trending, vertical to subvertical fault, acute-angled veering off the northwestern limb of Pfahl Shear Zone [DE-BY_1362].
references: https://data.geoscience.earth/ncl/geoera/ref/6358
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1414
broader: Pfahl Shear Zone

Abteiland Diagonal Faults
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:18.089Z
preferred label: Abteiland Diagonal Störungen @de
notation: DE-BY_1416
definition: Kleinräumige, saiger bis steilstehende Störungen im südöstlichen Bayerischen Wald (Abteiland), die spitzwinklig vom WNW-ESE Haupttrend der Pfahl Scherzone [DE-BY_1362] abweichen und südlich des Pfahls ± NW-SE, nördlich des Pfahls ± WSW-ENE streichen. Diese Strukturen werden als "Pferdeschwanz"-Auffiederungen (horsetail splays) (Eberts et al. 2021) interpretiert oder können synthetische Wedel-förmige Auffiederungen der Hauptgleitfläche darstellen. @de
definition: Array of small-scale vertical to subvertical faults in the southeastern Bavarian Forest (Abteiland), acute-angled veering off the principal WNW-ESE trend of the Pfahl Shear Zone [DE-BY_1362], and striking ± NW-SE south of the Pfahl, ± WSW-ENE north of the Pfahl. These structures are interpreted as horsetail splays (Eberts et al. 2021) or may be frond-like synthetic splays of the main fault zone plane.
references: https://data.geoscience.earth/ncl/geoera/ref/7320
references: https://data.geoscience.earth/ncl/geoera/ref/7279
references: https://data.geoscience.earth/ncl/geoera/ref/6358
references: https://data.geoscience.earth/ncl/geoera/ref/7255
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1416
broader: Pfahl Shear Zone

Pfahl Reverse Fault System
limit type: reverseFault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6358
references: https://data.geoscience.earth/ncl/geoera/ref/4114
type: Concept
created: 2021-01-25T14:23:18.144Z
preferred label: Pfahl Aufschiebungssystem @de
notation: DE-BY_1363
alternative label: Pfahlstörungszone @de
definition: Von Pösing westlich Cham nach NW hin, wirkte der Bayerische Pfahl als Aufschiebungsfront des variszischen Grundgebirges der Böhmischen Masse auf das permo-mesozoische Vorland und bildet dabei den nordöstlichen Steilrand der Bodenwöhrer Senke. Westlich von Neukirchen-Balbini weicht der Verlauf des Pfahl Aufschiebungssystems leicht von der Pfahl Scherzone ab und bildet mit der unmittelbar südwestlich subparallel ziehenden Jura-Aufschiebung (Meyer & Mielke 1993) [DE-BY_1365] die Pfahl Störungszone (Meyer 2000), eine komplexe Aufschiebungszone entlang der steilen NE-Flanke der Bödenwöhrer Senke, die von einer intensiven jüngeren Quertektonik geprägt ist (wie die Bayerwald Meridional Störungen [DE-BE_1350] wahrscheinlich bei einer späteren Reaktivierung vergrößerte variszische R‘- und P‘-Riedelbrüche), hinter der die ältere Pfahltektonik zurücktritt (Meyer & Mielke 1993). Unter diesen Querstörungen ragt die Fensterbach Störung [DE-BY_970] heraus, die N von Freihöls die Pfahl Störungszone abschneidet und die Grenzlinie der Böhmischen Masse nach NNW ablenkt, wobei sich der Pfahl im permo-mesozoischen Vorland als „einzelne“ Aufschiebung nach WNW bis Amberg fortsetzt (Amberger Aufschiebung). @de
definition: Roughly northwestwards from Pösing west of Cham the Bavarian Pfahl forms the reverse fault ramp for the movement of the Bohemian Massif Variscan Basement over the Permo-Mesozoic foreland, representing the northeastern scarp of the Bodenwöhr Trough. Forking off from the Pfahl Shear Zone west of Neukirchen-Balbini, and running close to and subparallel with the Jura Reverse Fault [DE-BY_1365], these two faults define the limits of Pfahl Fault Zone (Meyer 2000), a complex reverse fault system characterized by intense lateral tectonics (likewise Bayerwald Meridional Faults [DE-BY_1350] probably R’- and P’-Riedel shears of Variscan deformation, enlarged during later reactivation) outreaching the Variscan shearing and Alpine reverse faulting (Meyer & Mielke 1993). The most conspicuous of these lateral faults, Fensterbach Fault [DE-BY_970], deflects the western boundary line of the Bohemian Massif to the NNW and truncates the Pfahl Fault Zone in between the Pfahl and the Jura Reverse Faults, with the Pfahl continuing as a “single” reverse fault in the Permo-Mesozoic foreland further WNW-wards to Amberg (Amberger Aufschiebung).
hidden label: Permo-Mesozoikum / Kristallin Randstörung @de
narrower: Pfahl Reverse Fault
narrower: Jura Reverse Fault
narrower: Lateral Faults of Pfahl Reverse Fault System
narrower: Erzhäuser-Blechhammer Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7332
references: https://data.geoscience.earth/ncl/geoera/ref/7366
sf touches: Fensterbach Fault
sf touches: Lateral Faults of Pfahl Reverse Fault System
sf touches: Erzhäuser-Blechhammer Fault
sf touches: Cham Fault
in scheme: Tectonic Boundary Objects in Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11691
notation: LfU-BY_1363
broader: Bavarian Pfahl

Erzhäuser-Blechhammer Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:18.254Z
preferred label: Erzhäuser-Blechhammer Störung @de
notation: DE-BY_1469
definition: N-S verlaufende Querstörung des Pfahl Aufschiebungssystems [DE-BY_1366]. @de
definition: N-S trending lateral fault of Pfahl Reverse Fault System [DE-BY_1366].
references: https://data.geoscience.earth/ncl/geoera/ref/6358
references: https://data.geoscience.earth/ncl/geoera/ref/7259
sf touches: Pfahl Reverse Fault System
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1469
broader: Pfahl Reverse Fault System

Lateral Faults of Pfahl Reverse Fault System
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6358
type: Concept
created: 2021-01-25T14:23:18.226Z
preferred label: Querstörungen des Pfahl Aufschiebungssystems @de
notation: DE-BY_1366
definition: Post Pfahl Querstörungen die die Pfahl-Aufschiebung [DE-BY_1364] und Jura-Aufschiebung [DE-BY_1365] versetzen. Das Pfahl Aufschiebungssystems [DE-BY_1363] ist von einer intensiven jüngeren Quertektonik geprägt, hinter der die ältere Pfahltektonik (Meyer & Mielke 1993), als auch die alpidische Aufschiebungstektonik zurücktritt - wie die Bayerwald Meridional Störungen [DE-BE_1350] wahrscheinlich bei der späteren Reaktivierung vergrößerte variszische R‘- und P‘-Riedelbrüche. @de
definition: Post Pfahl lateral faults offsetting the Pfahl Reverse Fault [DE-BY_1364] and Jura Reverse Fault [DE-BY_1365] within the Pfahl Reverse Fault System [DE-BY_1363] as the result of an intense tectonic outperforming the Variscan shearing (Meyer & Mielke 1993) and Alpine reverse faulting, thus of Miocene age or younger. Likewise Bayerwald Meridional Faults [DE-BY_1350] probably R’- and P’-Riedel shears of the Variscan deformation, enlarged during later reactivation.
references: https://data.geoscience.earth/ncl/geoera/ref/7332
references: https://data.geoscience.earth/ncl/geoera/ref/4114
references: https://data.geoscience.earth/ncl/geoera/ref/7336
sf touches: Pfahl Reverse Fault System
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1366
broader: Pfahl Reverse Fault System

Jura Reverse Fault
limit type: reverseFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:18.199Z
preferred label: Jura-Aufschiebung @de
notation: DE-BY_1365
definition: NW-SE verlaufene, steil nach NE einfallende Aufschiebung subparallel zur Pfahl Aufschiebung [DE-BY_1364] zwischen der Fensterbach Störung [DE-BY_970] und dem Cham Störungssystem [DE-BY_1408]. Bildet den SW Rand der Pfahl Störungszone (Meyer 2000) als nordöstlichem Steilrand der Bodenwöhrer Senke. Von zahlreichen Querstörungen [DE-BY_1366] des Miozäns oder jünger versetzt (Meyer & Mielke 1993). @de
definition: NW-SE trending steeply NE dipping reverse fault running subparallel to Pfahl Reverse Fault [DE-BY_1364] between Fensterbach Fault [DE-BY_970] and Cham Fault System [DE-BY_1408] forming Pfahl Fault Zone (Meyer 2000) as the the northeastern scarp of the Bodenwöhr Trough. Offset by numerous lateral faults [DE-BY_1366] of Miocene age or younger (Meyer & Mielke 1993.
references: https://data.geoscience.earth/ncl/geoera/ref/4114
references: https://data.geoscience.earth/ncl/geoera/ref/7332
sf touches: Fensterbach Fault
sf touches: Lateral Faults of Pfahl Reverse Fault System
sf touches: Erzhäuser-Blechhammer Fault
sf touches: Cham Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1365
broader: Pfahl Reverse Fault System

Pfahl Reverse Fault
limit type: reverseFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:18.171Z
preferred label: Pfahl-Aufschiebung @de
notation: DE-BY_1364
alternative label: Amberger Aufschiebung @de
definition: Von Amberg bis Pösing W Cham, NW-SE verlaufende, steil nach NE einfallende Aufschiebung, entstanden durch variszische Scherung und alpidische Aufschiebung und durch zahlreiche jüngere Querstörungen [DE-BY_1366] segmentiert (Meyer & Mielke 1993). Zwischen ihrer Kreuzung mit der Fensterbach Störung [DE-BY_970] im NW und dem Cham Störungssystem [DE-BY_1408] im SE verläuft die Störung subparallel zur Jura Abschiebung [DE-BY_1365], und bildet dabei die NE Grenze der Pfahl Störungszone (Meyer 2000) als nordöstlichem Steilrand der Bodenwöhrer Senke. @de
definition: Running from Amberg to Pösing west of Cham, NW-SE trending steeply NE dipping reverse fault featuring a Variscan shearing and Alpine reverse faulting and segmented by a later intense lateral tectonic [DE-BY_1366] (Meyer & Mielke 1993). Between its intersection with Fensterbach Fault [DE-BY_970] and Cham Fault System [DE-BY_1408] running subparallel to Jura Reverse Fault [DE-BY_1365], forming Pfahl Fault Zone (Meyer 2000) as the the northeastern scarp of the Bodenwöhr Trough.
references: https://data.geoscience.earth/ncl/geoera/ref/7369
references: https://data.geoscience.earth/ncl/geoera/ref/7332
references: https://data.geoscience.earth/ncl/geoera/ref/4114
references: https://data.geoscience.earth/ncl/geoera/ref/6358
sf touches: Fensterbach Fault
sf touches: Lateral Faults of Pfahl Reverse Fault System
sf touches: Erzhäuser-Blechhammer Fault
sf touches: Cham Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1364
broader: Pfahl Reverse Fault System

Hildenbach Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.220Z
preferred label: Hildenbach Störung @de
notation: DE-BY_1463
definition: NW-SE streichende Störung südlich der Schnaittenbacher Störung [DE-BY_1468]. @de
definition: NW-SE striking fault south of Schnaittenbach Fault [DE-BY_1468].
references: https://data.geoscience.earth/ncl/geoera/ref/7264
references: https://data.geoscience.earth/ncl/geoera/ref/7295
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1463
broader: Moldanubian Zone tectonic boundaries

Schmidgaden Rotliegend Graben boundaries
type: Limit
type: Fault
type: Concept
created: 2021-01-25T14:23:19.193Z
preferred label: Schmidgaden Rotliegend-Graben Randstörungen @de
notation: DE-BY_1462
definition: WNW-ESE verlaufende Störungen, teilweise N-S versetzt, in der Verlängerung der Pfahl Scherzone [DE-BY_1362] und subparallel zum Pfahl Aufschiebungssystem [DE-BY_1363], im Westen von der Fensterbach Störung [DE-BY_970] abgeschnitten. @de
definition: WNW-ESE trending faults with N-S offsets, on strike of Pfahl Shear Zone [DE-BY_1362] and subparallel to Pfahl Reverse Fault System [DE-BY_1363]; truncated by Fensterbach Fault [DE-BY_970] in the west.
references: https://data.geoscience.earth/ncl/geoera/ref/7265
references: https://data.geoscience.earth/ncl/geoera/ref/7295
references: https://data.geoscience.earth/ncl/geoera/ref/7320
sf touches: Fensterbach Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1462
broader: Moldanubian Zone tectonic boundaries

Wölsendorf Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.165Z
preferred label: Wölsendorf Störung @de
notation: DE-BY_1461
definition: WNW-ESE streichende Störung in der Verlängerung der Pfahl Scherzone [DE-BY_1362] und subparallel zum Pfahl Aufschiebungssystem [DE-BY_1363]. @de
definition: WNW-ESE striking fault on strike of Pfahl Shear Zone [DE-BY_1362] and subparallel to Pfahl Reverse Fault System [DE-BY_1363].
references: https://data.geoscience.earth/ncl/geoera/ref/6358
references: https://data.geoscience.earth/ncl/geoera/ref/7260
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1461
broader: Moldanubian Zone tectonic boundaries

Pamsendorf Fault Set
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.138Z
preferred label: Pamsendorf Störungsschar @de
notation: DE-BY_1460
definition: Schar W-E verlaufender, saigerer bis subvertikaler Störungen. @de
definition: Array of W-E trending vertical to subvertical faults.
references: https://data.geoscience.earth/ncl/geoera/ref/6358
references: https://data.geoscience.earth/ncl/geoera/ref/7260
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1460
broader: Moldanubian Zone tectonic boundaries

Upper Palatine Forest SW-NE faults
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.110Z
preferred label: SW-NE Störungen des Oberpfälzer Waldes @de
notation: DE-BY_1459
definition: SW-NE verlaufende, saigere bis subvertikale Störungen südlich der Luhe Störung [DE-BY_965], zwischen der Cham Störung [DE-BY_1408] und dem Naabgebirge, dem westlichen Sporn des Oberpfälzer Waldes. @de
definition: SW-NE trending vertical to subvertical faults south of Luhe Fault [DE-BY_965], between Cham Fault [DE-BY_1408] and Naabgebirge, the western spur of Upper Palatine Forest.
references: https://data.geoscience.earth/ncl/geoera/ref/6358
references: https://data.geoscience.earth/ncl/geoera/ref/7334
references: https://data.geoscience.earth/ncl/geoera/ref/7320
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1459
broader: Moldanubian Zone tectonic boundaries

Schnaittenbach Fault
limit type: reverseFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.359Z
preferred label: Schnaittenbacher Störung @de
notation: DE-BY_1468
alternative label: Demenrichter Sörung @de
definition: NNW-SSE verlaufende, ca. 60° nach WSW einfallende Aufschiebung des Grundgebirges auf die triassischen Einheiten im Osten. @de
definition: NNW-SSE trending, approx. 60° WSW dipping reverse fault, thrusting the Variscan basement onto the Triassic deposits in the east.
references: https://data.geoscience.earth/ncl/geoera/ref/7264
references: https://data.geoscience.earth/ncl/geoera/ref/7295
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1468
broader: Moldanubian Zone tectonic boundaries

Weidelbach Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.331Z
preferred label: Weidelbach Störung @de
notation: DE-BY_1467
definition: In nördlicher Verlängerung der Schnaittenbacher Störung [DE-BY_1467] NNW-SSE verlaufende Störung mit geringer Sprunghöhe in triassischen Schichten. @de
definition: NNW-SSE trending intra-Triassic minor throw fault northward on-strike of Schnaittenbach Fault [DE-BY_1467].
references: https://data.geoscience.earth/ncl/geoera/ref/7264
references: https://data.geoscience.earth/ncl/geoera/ref/7295
sf touches: Luhe Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1467
broader: Moldanubian Zone tectonic boundaries

Neuersdorf Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.303Z
preferred label: Neuersdorfer Störung @de
notation: DE-BY_1466
definition: In nördlicher Verlängerung der Kemnather Störung [DE-BY_1465] gewellt N-S verlaufende Störung mit geringer Sprunghöhe in triassischen Schichten. @de
definition: Undulate N-S trending intra-Triassic minor throw fault northward on-strike of Kemnath Fault [DE-BY_1465].
references: https://data.geoscience.earth/ncl/geoera/ref/7264
references: https://data.geoscience.earth/ncl/geoera/ref/7295
sf touches: Luhe Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1466
broader: Moldanubian Zone tectonic boundaries

Saxothuringian Zone tectonic boundaries
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.022Z
preferred label: Tektonische Grenzflächen der Saxothuringischen Zone @de
notation: DE-BY_1505
definition: Das Saxoturingium, der Teil der Böhmischen Masse nördlich der Erbendorfer Line [DE-BY_1447], der von „minimal“-metamorphen (anchimetamorphen) Gesteinen aufgebaut wird, ist durch NW-SE (steil herzynisch) bis WNW-ESE (flach herzynisch) verlaufende Störungen und Störungsscharen gekennzeichnet. Grob SW-NE streichende Störungen folgen i.d.R. den Trends von Großstrukturen wie der Erbendorfer Line [DE-BY_1447] oder der Längsseite der Münchberger Masse Basis-Überschiebung [DE-BY_1504], oder, besonders im Frankenwald, folgen den Faltenachsen der Einengungstektonik des Unterkarbons (Mississippium). @de
definition: The Saxothuringian Zone, the Bohemian Massif realm north of Erbendorf Line [DE-BY_1447] featuring very low grad metamorphic (anchimetamorphic) rocks, is characterized by NW-SE (high-angle Hercynian) to WNW-ESE (flat-angle Hercynian) trending faults and fault sets. The faults roughly trending SW-NE generally are paralleling major tectonic structures, such as Erbendorf Line [DE-BY_1447] or the longside of Münchberg Klippe basal thrust [DE-BY_1504], or, specifically in Franconian Forest, follow the fold axes of compressional tectonics during Early Carboniferous (Mississippian).
narrower: Stiftsland Hercynian faults
narrower: Holzmühle-Mohelenská pláň Fault
narrower: Birkstauden-Hardeck Fault
narrower: Arzberg Fault
narrower: Arzberg lateral faults
narrower: Fichtel Mountains faults
narrower: Münchberg Klippe faults
narrower: Epplas Fault
narrower: Keilstein Fault
narrower: Kemlas Fault
narrower: Issigau Faults
narrower: Gupfen Fault
narrower: Rudolphstein Fault
narrower: Blaue Leite-Moos Fault
narrower: Joditz Fault
narrower: Wiedersberg Fault
narrower: Feilitzsch Fault
narrower: Selbitztal Fault
narrower: Bad Steben Fault Zone
narrower: Heinersgrün Step Fault
narrower: Dürrenwaid Fault
narrower: Nordhalben-Lotharheil Fault
narrower: Teuschnitz Syncline longitudinal faults
narrower: Teuschnitz Syncline lateral faults
narrower: Trebesbach Fault
narrower: Ebersdorf-Teuschnitz Fault
narrower: Ludwigsstadt Fault
narrower: Ludwigsstadt-Lauenhain Fault
narrower: Tettau Fault
narrower: Buchbach Fault
narrower: Höllbach-Neuhausen Fault
narrower: Neugattendorf-Regnitzlosau Fault
narrower: Bärenholz Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7285
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1505
broader: 3: Bohemian Massif domain

Trebesbach Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:21.108Z
preferred label: Trebesbach Störung @de
notation: DE-BY_1429
definition: WNW-ESE verlaufende, südwestlichster Querbruch der Teuschnitzer Mulde, subparallel zum Frankenwald-Randbruch [DE-BY_1431]. @de
definition: WNW-ESE trending, southwestern-most Teuschnitz Syncline lateral fault, running subparallel Franconian Forest Scarp [DE-BY_1431].
references: https://data.geoscience.earth/ncl/geoera/ref/7282
references: https://data.geoscience.earth/ncl/geoera/ref/7317
sf touches: Teuschnitz Syncline longitudinal faults
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1429
broader: Saxothuringian Zone tectonic boundaries

Teuschnitz Syncline lateral faults
limit type: obliqueSlipFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:21.080Z
preferred label: Querbrüche der Teuschnitzer Mulde @de
notation: DE-BY_1422
definition: NW-SE verlaufende Schrägabschiebungen die die Faltenachsen bis zu wenigen hundert Metern versetzen. Im Endstadium der Faltung als linkssinnige Blattverschiebungen angelegt, wurden die Brüche im jüngeren Tertiär als Abschiebungen reaktiviert. @de
definition: NW-SE trending oblique-slip faults offsetting the fold axes up to few hundreds of meters. Formed as sinistral strike-slip lateral disruptions in the final stage of folding and reactivated as normal faults during younger Tertiary.
references: https://data.geoscience.earth/ncl/geoera/ref/7317
references: https://data.geoscience.earth/ncl/geoera/ref/7285
sf touches: Teuschnitz Syncline longitudinal faults
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1422
broader: Saxothuringian Zone tectonic boundaries

Teuschnitz Syncline longitudinal faults
limit type: reverseFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:21.052Z
preferred label: Faltungsbrüche der Teuschnitzer Mulde @de
notation: DE-BY_1421
definition: Parallel zu den Faltenachsen SW-NE verlaufende, steil nach NW einfallende Aufschiebungen, als Ergebnis der spät-synsedimentär einsetzenden Einengungstektonik des Unterkarbons (Mississippium). @de
definition: SW-NE trending steeply NW dipping reverse faults parallel to the fold axes, due to late depositional to immediately post-depositional compression tectonics during Early Carboniferous (Mississippian).
references: https://data.geoscience.earth/ncl/geoera/ref/7317
references: https://data.geoscience.earth/ncl/geoera/ref/7285
sf touches: Franconian Forest Scarp
sf touches: Teuschnitz Syncline lateral faults
sf touches: Ebersdorf-Teuschnitz Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1421
broader: Saxothuringian Zone tectonic boundaries

Arzberg Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.190Z
preferred label: Arzberger Störung @de
notation: DE-BY_1499
alternative label: Arzberger Linie @de
definition: Insgesamt SW-NE verlaufende, steil nach SW einfallende Abschiebung; Nordrand des Waldsassener Schiefergebirges, von den Arzberg Querstörungen [DE-BY_1524] mehrfach versetzt. @de
definition: Overall SW-NE trending, steeply SW dipping normal fault, northern boundary of Waldsassen Slate Mountains (Waldsassener Schiefergebirge), multiply offset by Arzberg lateral faults [DE-BY_1524].
references: https://data.geoscience.earth/ncl/geoera/ref/7285
references: https://data.geoscience.earth/ncl/geoera/ref/7360
references: https://data.geoscience.earth/ncl/geoera/ref/7295
references: https://data.geoscience.earth/ncl/geoera/ref/7320
sf touches: Arzberg lateral faults
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1499
broader: Saxothuringian Zone tectonic boundaries

Birkstauden-Hardeck Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.162Z
preferred label: Birkstauden-Hardeck Störung @de
notation: DE-BY_1498
definition: WSW-ENE verlaufende, steil nach SSE einfallende Störung die von der Erbendorfer Linie [DE-BY_1447] abzweigt; wird von herzynischen Störungen des Stiftslands [DE-BY_1455] und von der Poxdorf Störung [DE-BY_1493] versetzt. @de
definition: WSW-ENE trending, steeply SSE dipping fault branching of Erbendorf Line [DE-BY_1447], offset by Stiftsland Hercynian faults [DE-BY_1455] and Poxdorf Fault [DE-BY_1493].
references: https://data.geoscience.earth/ncl/geoera/ref/7295
references: https://data.geoscience.earth/ncl/geoera/ref/7320
sf touches: Stiftsland Hercynian faults
sf touches: Poxdorf Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1498
broader: Saxothuringian Zone tectonic boundaries

Holzmühle-Mohelenská pláň Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.134Z
preferred label: Holzmühle-Mohelenská pláň Störung @de
notation: DE-BY_1523
definition: SW-NE verlaufende, steil nach SE einfallende listrische Aufschiebung im südlichen Waldsassener Schiefergebirge subparallel zur Pilmersreuth-Mähring Störung [DE-BY_1490] bzw. Erbendorfer Linie [DE-BY_1447]; mehrfach von herzynischen Störungen des Stiftslands [DE-BY_1455] versetzt. @de
definition: SW-NE trending, steeply SE dipping listric reverse fault crossing the southern Waldsassen Slate Mountains (Waldsassener Schiefergebirge) subparallel to Pilmersreuth-Mähring Fault [DE-BY_1490] resp. Erbendorf Line [DE-BY_1447]; multiply offset by Stiftsland Hercynian faults [DE-BY_1455].
references: https://data.geoscience.earth/ncl/geoera/ref/7361
references: https://data.geoscience.earth/ncl/geoera/ref/7295
sf touches: Stiftsland Hercynian faults
sf touches: Muglberg-Mähring Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1523
broader: Saxothuringian Zone tectonic boundaries

Blaue Leite-Moos Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.745Z
preferred label: Blaue Leite-Moos Störung @de
notation: DE-BY_1522
definition: Gewellt SW-NE verlaufende, steil nach NW einfallende Abschiebung zwischen Kemlaser Störung [DE-BY_1437] und Gupfen Störung [DE-BY_1520], SE-wärts versetzte Fortsetzung der südlichen Issigauer Störung [DE-BY_1438], als Begrenzung eines Karbon "Horstes" im NW gegen Devon-Ablagerungen im SE. @de
definition: Undulate SW-NE trending steeply NW dipping normal fault in between Kemlas Fault [DE-BY_1437] and Gupfen Fault [DE-BY_1520], SE-ward displaced eastern continuation of southern Issigau Fault [DE-BY_1438] offsetting a Carboniferous "Horst" in NW from Devonian deposits in SE.
references: https://data.geoscience.earth/ncl/geoera/ref/7318
references: https://data.geoscience.earth/ncl/geoera/ref/7285
references: https://data.geoscience.earth/ncl/geoera/ref/7320
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1522
limit type: normalFault
broader: Saxothuringian Zone tectonic boundaries

Rudolphstein Fault
limit type: strikeSlipFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.717Z
preferred label: Rudolphstein Störung @de
notation: DE-BY_1521
definition: NW-SE streichende linkssinnige Blattverschiebung; versetzt die Issigauer Störungen [DE-BY_1438] ca. 800 m nach NW. @de
definition: NW-SE striking sinistral strike-slip fault offsetting Issigau Faults [DE-BY_1438] approx. 800 m to NW.
references: https://data.geoscience.earth/ncl/geoera/ref/7318
references: https://data.geoscience.earth/ncl/geoera/ref/7285
references: https://data.geoscience.earth/ncl/geoera/ref/7320
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1521
broader: Saxothuringian Zone tectonic boundaries

Gupfen Fault
limit type: strikeSlipFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.690Z
preferred label: Gupfen Störung @de
notation: DE-BY_1520
definition: NW-SE streichende rechtssinnige Blattverschiebung; versetzt die Issigauer Störungen [DE-BY_1438] ca. 1 km nach SE. @de
definition: NW-SE striking dextral strike-slip fault offsetting Issigau Faults [DE-BY_1438] about 1 km to SE.
references: https://data.geoscience.earth/ncl/geoera/ref/7318
references: https://data.geoscience.earth/ncl/geoera/ref/7285
references: https://data.geoscience.earth/ncl/geoera/ref/7320
sf touches: Issigau Faults
sf touches: Blaue Leite-Moos Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1520
broader: Saxothuringian Zone tectonic boundaries

Neugattendorf-Regnitzlosau Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:21.303Z
preferred label: Neugattendorf-Regnitzlosau Störung @de
notation: DE-BY_1529
definition: NW-SE verlaufende Störung östlich von Hof. @de
definition: NW-SE trending fault east of Hof.
references: https://data.geoscience.earth/ncl/geoera/ref/7314
references: https://data.geoscience.earth/ncl/geoera/ref/7285
references: https://data.geoscience.earth/ncl/geoera/ref/7320
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1529
broader: Saxothuringian Zone tectonic boundaries

Stiftsland Hercynian faults
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.050Z
preferred label: Herzynische Störungen des Stiftslands @de
notation: DE-BY_1455
definition: WNW-ESE (flach herzynisch) streichende, saigere bis subvertikale Blatt- oder Schrägverschiebungen; versetzen am Südrand des Saxothurigium die Pilmersreuth-Mähring Störung [DE-BY_1490]. @de
definition: WNW-ESE striking, vertical to subvertical strike-slip or oblique-slip faults offsetting Pilmersreuth-Mähring Faul [DE-BY_1490] at the southern boundary of Saxothuringian Zone.
narrower: Muglberg-Mähring Fault
narrower: Poxdorf Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7285
references: https://data.geoscience.earth/ncl/geoera/ref/7362
references: https://data.geoscience.earth/ncl/geoera/ref/7350
references: https://data.geoscience.earth/ncl/geoera/ref/7321
references: https://data.geoscience.earth/ncl/geoera/ref/7295
sf touches: Pilmersreuth-Mähring Fault
sf touches: Holzmühle-Mohelenská pláň Fault
sf touches: Birkstauden-Hardeck Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1455
broader: Saxothuringian Zone tectonic boundaries

Poxdorf Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.106Z
preferred label: Poxdorf Störung @de
notation: DE-BY_1493
definition: WNW-ESE bis NW-SE streichende, saigere bis subvertikale linkssinnige Blatt- oder Schrägverschiebung; versetzt die Birkstauden-Hardeck Störung [DE-BY_1498]. @de
definition: WNW-ESE to NW-SE striking, vertical to subvertical sinistral strike-slip or oblique-slip fault offsetting Birkstauden-Hardeck Fault [DE-BY_1498].
references: https://data.geoscience.earth/ncl/geoera/ref/7362
references: https://data.geoscience.earth/ncl/geoera/ref/7295
sf touches: Birkstauden-Hardeck Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1493
broader: Stiftsland Hercynian faults

Muglberg-Mähring Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.078Z
preferred label: Muglberg-Mähring Störung @de
notation: DE-BY_1457
definition: WNW-ESE (flach herzynisch) streichende, saigere bis subvertikale linkssinnige Blatt- oder Schrägverschiebung; versetzt die Pilmersreuth-Mähring Störung [DE-BY_1490] geringfügig. @de
references: https://data.geoscience.earth/ncl/geoera/ref/7362
references: https://data.geoscience.earth/ncl/geoera/ref/7295
references: https://data.geoscience.earth/ncl/geoera/ref/7320
definition: WNW-ESE striking, vertical to subvertical sinistral strike-slip or oblique-slip fault slightly displacing Pilmersreuth-Mähring Fault [DE-BY_1490]
sf touches: Pilmersreuth-Mähring Fault
sf touches: Holzmühle-Mohelenská pláň Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1457
broader: Stiftsland Hercynian faults

Issigau Faults
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.662Z
preferred label: Issigauer Störungen @de
notation: DE-BY_1438
definition: SW-NE verlaufende, steil nach NW einfallende Abschiebungen als Begrenzung eines Karbon "Horstes" zwischen devonischen Ablagerungen. Von der Kemlaser Störung [DE-BY_1437] ca. 800 m nach NW und, weiter im NE, von der Gupfen Störung [DE-BY_1520] ca. 1 km nach SE versetzt. @de
definition: SW-NE trending, steeply NW dipping normal faults confining a Carboniferous "Horst" within Devonian deposits. Offset approx. 800 m to NW by Kemlas Fault [DE-BY_1437] and, further to NE, about 1 km to SE by Gupfen Fault [DE-BY_1520].
references: https://data.geoscience.earth/ncl/geoera/ref/7318
references: https://data.geoscience.earth/ncl/geoera/ref/7316
references: https://data.geoscience.earth/ncl/geoera/ref/7317
sf touches: Kemlas Fault
sf touches: Gupfen Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1438
limit type: normalFault
broader: Saxothuringian Zone tectonic boundaries

Höllbach-Neuhausen Fault
limit type: obliqueSlipFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:21.275Z
preferred label: Höllbach-Neuhausen Störung @de
notation: DE-BY_1526
definition: NNW-SSE verlaufende, saigere bis subvertikale rechtsinnige Schrägabschiebung SE von Rehau. @de
definition: NNW-SSE trending, vertical to subvertical dextral oblique-slip normal fault SE of Rehau.
references: https://data.geoscience.earth/ncl/geoera/ref/7281
references: https://data.geoscience.earth/ncl/geoera/ref/7285
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1526
broader: Saxothuringian Zone tectonic boundaries

Kemlas Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.633Z
preferred label: Kemlaser Störung @de
notation: DE-BY_1437
definition: Gebogen NW-SE bis WNW-ESE verlaufende, steil nach SW einfallende linkssinnige Schrägabschiebung, in Abschnitten als Flußspat Gänge. Versetzt die Issigauer Störungen [DE-BY_1438] ca. 800 m nach NW; Teil der Südwest-Grenze der Frankenwälder Querzone. @de
definition: Arcuate NW-SE to WNW-ESE trending, steeply SW dipping sinistral oblique-slip normal fault, in segments manifested as flourite veins, offsetting Issigau Faults [DE-BY_1438] approx. 800 m to NW. Part of southwestern boundary of Frankenwälder Querzone (Franconian Forest Lateral Zone).
references: https://data.geoscience.earth/ncl/geoera/ref/7318
references: https://data.geoscience.earth/ncl/geoera/ref/7316
references: https://data.geoscience.earth/ncl/geoera/ref/7320
sf touches: Issigau Faults
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1437
broader: Saxothuringian Zone tectonic boundaries

Buchbach Fault
limit type: obliqueSlipFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:21.247Z
preferred label: Buchbach Störung @de
notation: DE-BY_1427
definition: NNW-SSE streichende linkssinnige Schrägabschiebung. @de
definition: NNW-SSE striking sinistral oblique-slip normal fault.
references: https://data.geoscience.earth/ncl/geoera/ref/7317
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1427
broader: Saxothuringian Zone tectonic boundaries

Keilstein Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.606Z
preferred label: Keilstein Störung @de
notation: DE-BY_1436
definition: NW-SE verlaufende, steil nach SW einfallende linkssinnige Schrägabschiebung; Teil der Südwest-Grenze der Frankenwälder Querzone. @de
definition: NW-SE trending steeply SW dipping sinistral oblique-slip normal fault, part of southwestern boundary of Frankenwälder Querzone (Franconian Forest Lateral Zone).
references: https://data.geoscience.earth/ncl/geoera/ref/7318
references: https://data.geoscience.earth/ncl/geoera/ref/7320
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1436
broader: Saxothuringian Zone tectonic boundaries

Tettau Fault
limit type: obliqueSlipFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:21.219Z
preferred label: Tettau Störung @de
notation: DE-BY_1426
definition: Schar NW-SE streichender linkssinniger Schrägabschiebungen. @de
definition: Set of NW-SE striking sinistral oblique-slip normal faults.
references: https://data.geoscience.earth/ncl/geoera/ref/7317
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1426
broader: Saxothuringian Zone tectonic boundaries

Epplas Fault
limit type: obliqueSlipFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.578Z
preferred label: Epplaser Störung @de
notation: DE-BY_1435
definition: NW-SE verlaufende, polyphas rechtssinnige Schrägverschiebung mit einem Vertikalversatz von etwa 1 km, die die Überschiebungsflächen sowohl der Bayerische Fazies [DE-BY_1525] als auch der Münchberger Masse [DE-BY_1504] versetzt bzw. abschneidet. Mäßig steil bis steil nach SW einfallende, oft mylonitisierte Störung prä-variszischer Entstehung und variszisch reaktiviert, zunächst als Schrägaufschiebung, später Abschiebung. @de
definition: NW-SE trending major structure offsetting / truncating the Bavarian Facies basal thrust [DE-BY_1525] as well as the Münchberg Klippe basal thrust [DE-BY_1504]. Intermediate to steeply SW dipping polyphase dextral oblique-slip fault, partly mylonite, featuring a vertical throw of about 1 km. Pre-Variscan origin, Variscan reactivation as an oblique-slip reverse fault, later normal fault.
references: https://data.geoscience.earth/ncl/geoera/ref/7314
references: https://data.geoscience.earth/ncl/geoera/ref/7318
references: https://data.geoscience.earth/ncl/geoera/ref/7316
sf touches: Bavarian Facies basal thrust
sf touches: Münchberg Klippe basal thrust
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1435
broader: Saxothuringian Zone tectonic boundaries

Ludwigsstadt-Lauenhain Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:21.191Z
preferred label: Ludwigsstadt-Lauenhain Störung @de
notation: DE-BY_1425
definition: Südwestliche Flanke des Gräfenwalder Horstes, einer der Hauptstrukturen der Frankenwälder Querzone. @de
definition: NW-SW trending southwestern flank of Gräfenwald Horst, a principal structure of Franconian Forest transverse zone (Frankenwälder Querzone).
references: https://data.geoscience.earth/ncl/geoera/ref/7317
sf touches: Ludwigsstadt Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1425
broader: Saxothuringian Zone tectonic boundaries

Ludwigsstadt Fault
type: Limit
type: Fault
type: Concept
created: 2021-01-25T14:23:21.164Z
preferred label: Ludwigsstadt Störung @de
notation: DE-BY_1424
definition: W-E streichende Störung bei Ludwigstadt, versetzt den Gräfenwalder Horst nach Westen. @de
definition: W-E striking fault at Ludwigstadt, displacing Gräfenwald Horst to the west.
references: https://data.geoscience.earth/ncl/geoera/ref/7317
sf touches: Ludwigsstadt-Lauenhain Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1424
broader: Saxothuringian Zone tectonic boundaries

Ebersdorf-Teuschnitz Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:21.136Z
preferred label: Ebersdorf-Teuschnitz Störung @de
notation: DE-BY_1423
definition: NW-SE verlaufende Störung, bildet in ihrem nördlichen Abschnitt die südwestliche Flanke des Gräfenwalder Horstes, einer der Hauptstrukturen der Frankenwälder Querzone. @de
definition: NW-SE trending fault, in its northern segment representing the southwestern boundary of Gräfenwald Horst, a principal structure of Franconian Forest transverse zone (Frankenwälder Querzone).
references: https://data.geoscience.earth/ncl/geoera/ref/7317
sf touches: Teuschnitz Syncline longitudinal faults
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1423
broader: Saxothuringian Zone tectonic boundaries

Wiedersberg Fault
limit type: obliqueSlipFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.801Z
preferred label: Wiedersberger Störung @de
notation: DE-BY_1509
alternative label: Wiedersberger Gang @de
definition: NW-SE verlaufende, mäßig steil nach SW einfallende rechtssinnige Schrägabschiebung. @de
definition: NW-SE trending, intermediately SW dipping, dextral oblique slip normal fault.
references: https://data.geoscience.earth/ncl/geoera/ref/7314
references: https://data.geoscience.earth/ncl/geoera/ref/7285
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1509
broader: Saxothuringian Zone tectonic boundaries

Joditz Fault
limit type: obliqueSlipFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.773Z
preferred label: Joditzer Störung @de
notation: DE-BY_1508
definition: Von Ludwigshöhe durch die Vogtland Mulde bis Unterkotzau ziehende, NW-SE verlaufende, mäßig steil nach SW einfallende rechtssinnige Schrägabschiebung. @de
definition: Running from Ludwigshöhe to Unterkotzau across Vogtland syncline, NW-SE trending, intermediately SW dipping, dextral oblique-slip normal fault.
references: https://data.geoscience.earth/ncl/geoera/ref/7314
references: https://data.geoscience.earth/ncl/geoera/ref/7318
references: https://data.geoscience.earth/ncl/geoera/ref/7320
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1508
broader: Saxothuringian Zone tectonic boundaries

Bärenholz Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:21.330Z
notation: DE-BY_1530
definition: NW-SE verlaufende Störung östlich von Hof. @de
definition: NW-SE trending fault east of Hof.
references: https://data.geoscience.earth/ncl/geoera/ref/7285
references: https://data.geoscience.earth/ncl/geoera/ref/7320
preferred label: Bärenholz Störung @de
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1530
broader: Saxothuringian Zone tectonic boundaries

Nordhalben-Lotharheil Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:21.025Z
preferred label: Nordhalben-Lotharheil Störung @de
notation: DE-BY_1517
definition: NNW-SSE verlaufende, subvertikale bis steil nach WSW einfallende Störung. @de
definition: NNW-SSE trending, subvertical to steeply ENE dipping fault.
references: https://data.geoscience.earth/ncl/geoera/ref/7315
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1517
broader: Saxothuringian Zone tectonic boundaries

Dürrenwaid Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.997Z
preferred label: Dürrenwaid Störung @de
notation: DE-BY_1516
definition: NNW-SSE verlaufende, subvertikale bis steil nach WSW einfallende Störung. @de
definition: NNW-SSE trending, subvertical to steeply WSW dipping fault.
references: https://data.geoscience.earth/ncl/geoera/ref/7315
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1516
broader: Saxothuringian Zone tectonic boundaries

Münchberg Klippe faults
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.356Z
preferred label: Münchberger Überschiebungsinsel Störungen @de
notation: DE-BY_1503
definition: Zwischen Frankenwald und Fichtelgebirge liegt eine fremdartige Gesteinsscholle - die Münchberger Masse - schüsselförmig eingesenkt im saxothuringischen Grundgebirge aus paläozoischen Gesteinen der Bayerischen Fazies über Thüringer Fazies. Die Münchberger Gneissmasse wird als Überschiebungsinsel (Klippe) eines inversen (höchster Metamorphosegrad am Top) Deckenstapels interpretiert, dessen Einheiten im Devon bis Unterkarbon übereinandergeschoben wurden. Die Basis der Müchberger Klippe und der unterlagernden und umgebenden Bayerischen Fazies werden von flachen Überschiebungen gebildet, die spät- bis postvariszisch zerlegt wurden und von einer steilstehenden, verschuppten im Südosten-Grenze zum Fichtelgebirge. @de
definition: In between the Fichtel Mountains to the southeast and the Franconian Forest to the northwest, an exotic block - the Münchberg Klippe - bowl-like rests upon the Saxothuringian basement made up of Bavarian Facies Paleozoic deposits thrusted over Thuringian Facies Paleozoic rocks. Münchberg Klippe is considered a thrust-outlier featuring an inverse stack of nappes with the highest-grade metamorphic rocks on top, piled up by thrusting during Devonian and Early Carboniferous (Mississippian). Münchberg Klippe basal thrust, as well as the thrust plain of its fringe and footwall - Bavarian Facies - form flat overthrusts disaggregated by late and post-Varican faulting and a steep, imbricate southeastern boundary towards Fichtel Mountains rock association.
narrower: Bavarian Facies basal thrust
narrower: Münchberg Klippe basal thrust
narrower: Münchberg Klippe longitudinal faults
narrower: Münchberg Klippe lateral faults
references: https://data.geoscience.earth/ncl/geoera/ref/7288
references: https://data.geoscience.earth/ncl/geoera/ref/7280
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1503
broader: Saxothuringian Zone tectonic boundaries

Münchberg Klippe basal thrust
limit type: thrustFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.495Z
preferred label: Münchberger Masse Basis-Überschiebung @de
notation: DE-BY_1504
definition: SW-NE gestreckt schüsselförmige, flach bis mäßig steil einfallende Überschiebungsfläche der Basis der Münchberger Masse über die Bayerische Fazies. Von den Münchberger Masse Quer-Störungen [DE-BY_1434] zerlegt und entlang der Fränkischen Linie [DE-BY_1398] abgeschnitten bzw. vertikal versetzt. Die steil einfallende und verschuppte Südost-Grenze ist das Ergebnis NW-SE einengender Bruchtektonik und Scherung. @de
definition: SW-NE elongated bowl-shaped gently dipping thrust plane of Münchberg Klippe base over the Bavarian Facies realm; disaggregated by Münchberg Klippe lateral faults [DE-BY_1434] and offset resp. downwarped along Franconian Line [DE-BY_1398] in the southwest. The sheer imbricate eastern boundary results from NW-SE compressional brittle tectonics and shearing.
references: https://data.geoscience.earth/ncl/geoera/ref/7288
references: https://data.geoscience.earth/ncl/geoera/ref/7280
sf touches: Münchberg Klippe lateral faults
in scheme: Tectonic Boundary Objects in Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11574
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11575
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11576
notation: LfU-BY_1504
broader: Münchberg Klippe faults

Bavarian Facies basal thrust
limit type: thrustFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.384Z
preferred label: Bayerische Fazies Basis-Überschiebung @de
notation: DE-BY_1525
definition: Basis der Bayerischen Fazies als unterste und äußere Überschiebung der Münchberger Klippe s. l.. Im Norden und Nordosten von Frankenwald Störungen zerlegt und verschoben und entlang der Fränkischen Linie [DE-BY_1398] abgeschnitten bzw. vertikal versetzt. Die steil einfallende und verschuppte Südost-Grenze ist das Ergebnis NW-SE einengender Bruchtektonik und Scherung. @de
definition: Lowest and outermost thrust of Münchberg Klippe s. l. stack of nappes, gently dipping basal thrust of the Bavarian Facies realm. In the northern and northwestern part disaggregated and offset by Franconian Forest faults and truncated resp. downwarped along Franconian Line [DE-BY_1398] in the southwest. Its sheer imbricate southeastern boundary results from NW-SE compressional brittle tectonics and shearing.
narrower: Wurbach-Wallenfels Fault
narrower: Geuser-Wallenfels Fault
narrower: Elbersreuth-Schwarzenstein-Schwarzenbach Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7288
references: https://data.geoscience.earth/ncl/geoera/ref/7280
sf touches: Fichtel Mountains Scarp
sf touches: Franconian Forest Scarp
sf touches: Fichtel Mountains lateral faults
sf touches: Münchberg Klippe basal thrust
sf touches: Epplas Fault
sf touches: Selbitztal Fault
in scheme: Tectonic Boundary Objects in Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11574
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11575
notation: LfU-BY_1525
broader: Münchberg Klippe faults

Elbersreuth-Schwarzenstein-Schwarzenbach Fault
limit type: thrustFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.467Z
preferred label: Elbersreuth-Schwarzenstein-Schwarzenbach Störung @de
notation: DE-BY_1534
definition: Insgesamt SSW-NNE verlaufender interne Überschiebung in der Bayerischen Fazies. @de
definition: Overall SSW-NNE trending internal thrust within the Bavarian Facies.
references: https://data.geoscience.earth/ncl/geoera/ref/7319
references: https://data.geoscience.earth/ncl/geoera/ref/7285
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1534
broader: Bavarian Facies basal thrust

Geuser-Wallenfels Fault
limit type: thrustFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.440Z
preferred label: Geuser-Wallenfels Störung @de
notation: DE-BY_1528
definition: Gewellt SSW-NNE verlaufende Störung, im nördlichen Abschnitt nordöstliche Begrenzung des Wallenfels Sporns der Bayerischen Fazies. @de
definition: Undulate SSW-NNE trending fault, in ist northern part northeastern boundary of Bavarian Facies Wallenfels spur.
references: https://data.geoscience.earth/ncl/geoera/ref/7282
references: https://data.geoscience.earth/ncl/geoera/ref/7285
sf touches: Bavarian Facies basal thrust
sf touches: Wurbach-Wallenfels Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1528
broader: Bavarian Facies basal thrust

Wurbach-Wallenfels Fault
limit type: thrustFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.412Z
preferred label: Wurbach-Wallenfels Störung @de
notation: DE-BY_1527
definition: Gewellt SW-NE verlaufende Störung, abschnittsweise nordwestliche Begrenzung des Wallenfels Sporns der Bayerischen Fazies. @de
definition: Undulate SW-NE trending fault, in segments northwestern boundary of Bavarian Facies Wallenfels spur.
references: https://data.geoscience.earth/ncl/geoera/ref/7282
references: https://data.geoscience.earth/ncl/geoera/ref/7285
sf touches: Franconian Forest Scarp
sf touches: Bavarian Facies basal thrust
sf touches: Geuser-Wallenfels Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1527
broader: Bavarian Facies basal thrust

Münchberg Klippe lateral faults
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.550Z
preferred label: Münchberger Masse Quer-Störungen @de
notation: DE-BY_1434
definition: Grob NW-SE verlaufende Störungen der Münchberger Masse, die die Münchberger Masse Basis-Überschiebung [DE-BY_1504] Ränder sowie die internen Überschiebungen des Deckenstapels versetzen. @de
definition: Roughly NW-SE trending faults of Münchberg Klippe, offsetting Münchberg Klippe basal thrust [DE-BY_1504] margins and the (internal) thrusts of the stack of nappes.
references: https://data.geoscience.earth/ncl/geoera/ref/7358
references: https://data.geoscience.earth/ncl/geoera/ref/7285
references: https://data.geoscience.earth/ncl/geoera/ref/7280
sf touches: Bavarian Facies basal thrust
sf touches: Münchberg Klippe basal thrust
sf touches: Münchberg Klippe longitudinal faults
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1434
broader: Münchberg Klippe faults

Münchberg Klippe longitudinal faults
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.522Z
preferred label: Münchberger Masse Längs-Störungen @de
notation: DE-BY_1433
definition: SW-NE verlaufende Störungen der Münchberger Masse. @de
definition: SW-NE trending faults of Münchberg Klippe.
references: https://data.geoscience.earth/ncl/geoera/ref/7358
references: https://data.geoscience.earth/ncl/geoera/ref/7285
references: https://data.geoscience.earth/ncl/geoera/ref/7280
sf touches: Münchberg Klippe lateral faults
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1433
broader: Münchberg Klippe faults

Heinersgrün Step Fault
limit type: obliqueSlipFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.969Z
preferred label: Heinersgrün Bruchstaffel @de
notation: DE-BY_1515
definition: NNW-SSE verlaufende Bruchstaffel subvertikal bis steil nach ENE einfallender linkssinniger Schrägabschiebungen. @de
definition: NNW-SSE trending, step fault of subvertical to steeply ENE dipping sinistral oblique-slip normal faults.
references: https://data.geoscience.earth/ncl/geoera/ref/7315
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1515
broader: Saxothuringian Zone tectonic boundaries

Bad Steben Fault Zone
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.886Z
preferred label: Bad Stebener Störungszone @de
notation: DE-BY_1512
definition: Von Carlsgrün nach Bobengrün NNW-SSE verlaufende, den Bergaer Sattel schneidende Grabenstruktur an deren Flanken Säuerlinge und Mineralgänge zu Tage treten. @de
definition: Running from Carlsgrün to Bobengrün crossing Berga anticline, NNW-SSE trending graben structure featuring acidulous springs and mineral veins at its flanks.
narrower: Carlsgrün-Horwagen faults
narrower: Mordlau-Bobengrün faults
references: https://data.geoscience.earth/ncl/geoera/ref/7315
references: https://data.geoscience.earth/ncl/geoera/ref/7316
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1512
limit type: normalFault
broader: Saxothuringian Zone tectonic boundaries

Mordlau-Bobengrün faults
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.941Z
preferred label: Mordlau-Bobengrün Störungen @de
notation: DE-BY_1514
definition: Östliche Flanke des Bad Stebener Grabens; NNW-SSE verlaufende, steil nach WSW einfallende Abschiebungen mit einer Sprunghöhe von bis zu 300 m, teilweise als Siderit-Gänge (Mordlauer Gangzug). @de
definition: Eastern scarp of Bad Steben Graben. NNW-SSE trending, steeply WSW dipping normal faults featuring a throw of up to more than 300 m, partly manifested as siderite veins (Mordlau train of veins).
references: https://data.geoscience.earth/ncl/geoera/ref/7315
references: https://data.geoscience.earth/ncl/geoera/ref/7316
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1514
limit type: normalFault
broader: Bad Steben Fault Zone

Carlsgrün-Horwagen faults
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.914Z
preferred label: Carlsgrün-Horwagen Störungen @de
notation: DE-BY_1513
definition: Westliche Flanke des Bad Stebener Grabens; NNW-SSE verlaufende, steil bis subvertikal nach ENE einfallende Abschiebungen mit einer Sprunghöhe bis zu 250 m, Aufstiegsbruch der Bad Stebener Säuerlinge. @de
definition: Western scarp of Bad Steben Graben. NNW-SSE trending, steeply to subvertical ENE dipping normal faults featuring a cumulative throw of up to 250 m; feeder conduits of Bad Steben acidulous springs.
references: https://data.geoscience.earth/ncl/geoera/ref/7315
references: https://data.geoscience.earth/ncl/geoera/ref/7316
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1513
limit type: normalFault
broader: Bad Steben Fault Zone

Fichtel Mountains faults
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.245Z
preferred label: Fichtelgebirge Störungen @de
notation: DE-BY_1502
definition: Das Fichtelgebirge zwischen der Erbendorfer Linie [DE-BY_ 1447] bzw. dem Waldsassener Schiefergebirge im Süden und der Münchberger Masse [vgl. DE-BY_1503] im Norden, wird von variszischen gering metamorphen und - vorherrschend - Granit Intrusionen aufgebaut. Drei Hauptrichtungen bestimmen das Störungsmuster der spätvariszisch angelegten und mehrfach (v.a. durch Krustenbewegungen der alpidischen Gebirgsbildung), zuletzt im Tertiär reaktivierten Störungen: WNW-ESE, NW-SE und SW-NE. @de
definition: The Fichtel Mountains, in between the Erbendorf Line [DE-BY_ 1447] resp. Waldsassen Slate Mountains (Waldsassener Schiefergebirge) to the south and Münchberg Klippe [cf. DE-BY_1503] to the north, is made up of Varican low-grade metamorphic, folded sedimentary rocks and predominant granite intrusions. Three principal trends prevail the pattern of the late-Variscan faults, multiply reactivated mainly due to Alpine Orogeny crustal movements, lastly in Tertiary: WNW-ESE, NW-SE, and SW-NE.
narrower: Fichtel Mountains longitudinal faults
narrower: Fichtel Mountains Hercynian faults
narrower: Fichtel Mountains lateral faults
references: https://data.geoscience.earth/ncl/geoera/ref/7357
references: https://data.geoscience.earth/ncl/geoera/ref/7285
references: https://data.geoscience.earth/ncl/geoera/ref/7338
references: https://data.geoscience.earth/ncl/geoera/ref/7280
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1502
broader: Saxothuringian Zone tectonic boundaries

Fichtel Mountains lateral faults
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.328Z
preferred label: Fichtelgebirge Quer-Störungen @de
notation: DE-BY_1420
definition: Insbesondere im Nahbereich der Fränkischen Linie [DE-BY_1398], hier: Fichtelgebirgs-Randbruch [DE-BY_1432], verbreitete, NW-SE gerichtete, mit Annäherung an den Fichtelgebirgs-Randbruch auf NNW-SSE drehende Störungen. @de
definition: Particularly widespread close to the Franconian Line [DE-BY_1398], here: the Fichtel Mountains Scarp [DE-BY_1432], NW-SE trending faults, veering to NNW-SSE when converging Fichtel Mountains Scarp.
references: https://data.geoscience.earth/ncl/geoera/ref/7357
references: https://data.geoscience.earth/ncl/geoera/ref/7359
references: https://data.geoscience.earth/ncl/geoera/ref/7283
references: https://data.geoscience.earth/ncl/geoera/ref/7320
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1420
broader: Fichtel Mountains faults

Fichtel Mountains Hercynian faults
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.301Z
preferred label: Herzynische Störungen im Fichtelgebirge @de
notation: DE-BY_1501
definition: Flach herzynisch (WNW-ESE) streichende Störungen vorwiegend in den Metasedimenten am Nordost-Rand des Fichtelgebirges. @de
definition: WNW-ESE (flat-angle Hercynian) striking faults predominantly in the meta-sediments of Fichtel Mountains northeastern margin.
references: https://data.geoscience.earth/ncl/geoera/ref/7338
references: https://data.geoscience.earth/ncl/geoera/ref/7285
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1501
broader: Fichtel Mountains faults

Fichtel Mountains longitudinal faults
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.273Z
preferred label: Fichtelgebirge Längs-Störungen @de
notation: DE-BY_1500
definition: SW-NE verlaufende, saigere bis subvertikale Störungen parallel zu den Faltenachsen, vorwiegend in den Metasedimenten am Nordost-Rand des Fichtelgebirges. @de
definition: SW-NE trending, vertical to subvertical faults parallel to the fold axes, predominantly in the low-grade meta-sediments of Fichtel Mountains northeastern margin.
references: https://data.geoscience.earth/ncl/geoera/ref/7357
references: https://data.geoscience.earth/ncl/geoera/ref/7285
references: https://data.geoscience.earth/ncl/geoera/ref/7338
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1500
broader: Fichtel Mountains faults

Selbitztal Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.858Z
preferred label: Selbitztal Störung @de
notation: DE-BY_1511
definition: Von Naila nach Selbitz ziehende, NW-SE bis WNW-ESE verlaufende Störung die den Garleswald Sporn der Bayerische Fazies im NE abschneidet und die Bayerische Fazies Basis-Überschiebung [DE-BY_1525] versetzt. @de
definition: Running from Naila to Selbitz, NW-SE to WNW-ESE trending fault truncating Bavarian Facies Garleswald spur in the NE thus offsetting the Bavarian Facies basal thrust [DE-BY_1525].
references: https://data.geoscience.earth/ncl/geoera/ref/7318
references: https://data.geoscience.earth/ncl/geoera/ref/7285
sf touches: Bavarian Facies basal thrust
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1511
broader: Saxothuringian Zone tectonic boundaries

Arzberg lateral faults
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.218Z
preferred label: Arzberg Querstörungen @de
notation: DE-BY_1524
definition: NW-SE bis N-S verlaufende Störungen ± senkrecht zur Arzberger Störung [DE-BY_1499], die von den Querstörungen versetzt wird. @de
definition: Set of NW-SE to N-S trending faults ± perpendicular to and offsetting Arzberg Fault [DE-BY_1499].
references: https://data.geoscience.earth/ncl/geoera/ref/7295
references: https://data.geoscience.earth/ncl/geoera/ref/7320
sf touches: Arzberg Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1524
broader: Saxothuringian Zone tectonic boundaries

Feilitzsch Fault
limit type: obliqueSlipFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:20.829Z
preferred label: Feilitzsch Störung @de
notation: DE-BY_1510
definition: NW-SE verlaufende rechtssinnige Schrägabschiebung. @de
definition: NW-SE trending dextral oblique slip normal fault.
references: https://data.geoscience.earth/ncl/geoera/ref/7314
references: https://data.geoscience.earth/ncl/geoera/ref/7285
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1510
broader: Saxothuringian Zone tectonic boundaries

Bohemian Massif Western Margin System
limit type: reverseFault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6358
narrower: Schwarzenfeld Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7269
alternative label: Bohemian Massif Western Margin tectonic boundaries
narrower: Franconian Line
references: https://data.geoscience.earth/ncl/geoera/ref/7295
definition: Durchquert auf mehr als 150 km bayerisches Gebiet, insgesamt NW-SE verlaufender Großschollenrand der die Böhmische Masse gegen das Süddeutsche Schichtstufenland begrenzt, meist in Form nach ± E einfallender Auf- und Überschiebungen. Mehrfach versetzt durch Quer-Störungssysteme und abschnittsweise durch jüngere Bildungen verdeckt. Wird im Süden vom Donaustörungssystem [DE-BY_697] abgeschnitten bzw. nach Osten und Südosten hin abgelenkt. Variszisch angelegt und danach mehrfach reaktiviert, erfolgte die Hauptphase der Heraushebung des Westrandes der Böhmischen Masse und Aufschiebung auf das permo-mesozoische Vorland während der Oberkreide und des Paläogens (Bayerisches Geologisches Landesamt 1996). @de
narrower: Fensterbach Fault
scope note: The Bohemian Massif Western Margin tectonic boundaries can be directly observed only in very few segments. In most cases, the faults’ trend is inferred from contour lines pattern of the Permo-mesozoic foreland and/or extrapolated from outcrop evidence, aligned with geophysical surveys interpretations or remote sensing data in few areas. As a rule, the top of the Varican basement serves as the reference horizon for the indication of the vertical displacement (throw). As the exposed Bohemian Massive has been subject to intense peneplanation during Tertiary, the figures given, thus, represent the present-day “residual” throw.
narrower: Luhe Line
scope note: Die tektonischen Bauelemente des Westrands der Böhmischen Masse können nur in wenigen Abschnitten direkt kartiert werden. Der Verlauf der Störungen ist größtenteils aus Streichlinien-Mustern im permo-mesozoischen Vorland abgeleitet und/oder aus Aufschluss-Befunden extrapoliert, im Kontext mit Fernerkundungsdaten und geophysikalischen Untersuchungen in ausgesuchten Gebieten. Für die Ermittlung des vertikalen Versatzes (Sprunghöhe) wird in der Regel die Oberfläche des Grundgebirges herangezogen. Da die zu Tage tretende Böhmische Masse insbesondere im Tertiär einer intensiven Einrumpfung unterlag, sind die ermittelten Sprunghöhen aktuelle (Residual-) Werte. @de
definition: Traversing Bavarian territory for more than 150 km, overall NW-SE trending borderline separating the Bohemian Massif to the east from the South German Scarpland to the west, primarily as a ± E dipping reverse or thrust fault (system). Multiply displaced by transverse fault systems and in sections obscured by younger deposits. In the south, truncated / deflected by the Danube Fault System [DE-BY_697] towards the east and southeast. Evolving during Variscan orogeny, afterward multiply reactivated, the main phase of the uplift of the western marginal zone of the Bohemian Massif, overthrusting the Permo-Mesozoic foreland, took place during Upper Cretaceous and Paleogene (Bayerisches Geologisches Landesamt 1996).
narrower: Keilberg Fault System
alternative label: Tektonische Grenzflächen des Westrands der Böhmischen Masse @de
narrower: Pittersberg Fault
created: 2020-10-29T14:47:52.875Z
type: Concept
preferred label: Störungssysteme des Westrands der Böhmischen Masse @de
notation: DE-BY_1345
references: https://data.geoscience.earth/ncl/geoera/ref/4073
sf touches: Danube Fault System
in scheme: Tectonic Boundary Objects in Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11691
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11855
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11887
type: https://data.geoscience.earth/ncl/geoera/geoconnect3d/category/9755
notation: LfU-BY_1583
notation: LfU-BY_1345
broader: 3: Bohemian Massif domain

Schwarzenfeld Fault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/4114
references: https://data.geoscience.earth/ncl/geoera/ref/6358
type: Concept
created: 2021-01-25T14:23:16.819Z
preferred label: Schwarzenfeld Störung @de
notation: DE-BY_1373
definition: SSW-NNE streichende, unter dem Naabtal Tertiär verborgene Schrägabschiebung, die das Pfahl Aufschiebungssystem [DE-BY_1363] ca. 1 km sinistral versetzt. Die wahrscheinlich W-vergente Störung weist eine von S nach N zunehmende Sprunghöhe bis zu 40 m auf. @de
definition: SSW-NNE striking oblique slip fault underneath the Tertiary deposits of Naab River Valley, displacing the Pfahl Reverse Fault System [DE-BY_1363], for about 1 km in a sinistral offset. The probably W dipping fault features, from S to N increasing, a throw of up to 40 m.
narrower: Krondorf Fault
sf touches: Krondorf Fault
sf touches: Pfahl Reverse Fault
sf touches: Jura Reverse Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1373
broader: Bohemian Massif Western Margin System

Krondorf Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:16.847Z
preferred label: Krondorf Störung @de
notation: DE-BY_1372
definition: N-S streichender Ast der Schwarzenfeld Störung [DE-BY_1373] mit einem Verwurf von bis zu 20 m. @de
definition: N-S striking branch of Schwarzenfeld Fault [DE-BY_1373] featuring a throw of up to 20 m.
references: https://data.geoscience.earth/ncl/geoera/ref/4114
sf touches: Schwarzenfeld Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1372
broader: Schwarzenfeld Fault

Luhe Line
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:17.132Z
preferred label: Luhe Linie @de
notation: DE-BY_1387
definition: SW-NE bis W-E verlaufende Störungslinie, die die Westgrenze der Böhmischen Masse um über 25 km versetzt. Westlich der Freihung Störung [DE-BY_990] nur in kurzen Abschnitten nachweisbar. @de
definition: SW-NE to W-E trending fault line offsetting the western margin of the Bohemian Massif for more than 25 km. West of Freihung Fault [DE-BY_990] evidenced in short sections only.
narrower: Krickelsdorf-Kainsricht Fault
narrower: Ehenbach Fault
narrower: Kindlas Fault
narrower: Luhe Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7295
references: https://data.geoscience.earth/ncl/geoera/ref/7320
references: https://data.geoscience.earth/ncl/geoera/ref/7343
in scheme: Tectonic Boundary Objects in Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11578
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11694
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11855
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11887
notation: LfU-BY_1387
broader: Bohemian Massif Western Margin System

Luhe Fault
limit type: scissorFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:17.254Z
preferred label: Luhe Störung @de
notation: DE-BY_965
alternative label: Luhe Fault System
alternative label: Luhe Störungssystem @de
alternative label: Neudorfer Störung @de
definition: Overall W-E trending, steeply S dipping polyphase reverse fault with a (final) rotational movement forming a scissors-fault (“tilted blocks crossover”, Steinlein 1953) with the pivot near Neudorf. In the west, featuring a throw of more than 400 m, the northern block forms the footwall, in the east, with a throw of up to more than 120 m, the hanging wall (Bauberger & Haunschild 1960). Kinematic history comprises reverse faulting during late Carboniferous, normal reactivation in early Cretaceous, and the late Cretaceous / early Tertiary rotational movement, i.e. inversion in the western part while normal reactivation in the eastern part (Peterek & Schröder 2017). East of Franconian Line [DE-BY_1398] resp. its southernmost section Gleitsbach-Windbühl Fault [DE-BY_1399] Luhe Fault forms the southern boundary of Erbendorf-Vohenstrauss Zone (ZEV), an outlier of Teplá-Barrandian Block.
definition: Insgesamt W-E verlaufende, steil Süd-fallende polyphase Aufschiebung mit einer (abschließenden) Rotationsbewegung, d.h. Scherenstörung (Kippschollen-Kreuzung nach Steinlein 1953), mit einer Drehachse bei Neudorf. Im Westen ist bei einer Mindestsprunghöhe von mehr als 400 m die nördliche Scholle herausgehoben, im Osten, bei einer Sprunghöhe bis über 120 m, die Südscholle (Bauberger & Haunschild 1960). Die kinematische Geschichte umfasst eine aufschiebende Tektonik im späten Karbon, eine abschiebende Reaktivierung in der frühen Kreide und, in der späten Kreide / Jungtertiär, eine Rotationsbewegung mit aufschiebender Inversionstektonik im westlichen Teil bei abschiebender Reaktivierung im östlichen Teil (Peterek & Schröder 2017). Östlich der Fränkischen Linie [DE-BY_1398] bzw. ihres südlichsten Abschnitts, der Gleitsbach-Windbühl Störung [DE-BY_1399], definiert die Luhe Störung die Südgrenze der Zone von Erbendorf-Vohenstrauß (ZEV), einer Überschiebungsinsel des Teplá-Barrandiums. @de
narrower: Engelshof Subfault
references: https://data.geoscience.earth/ncl/geoera/ref/7356
references: https://data.geoscience.earth/ncl/geoera/ref/7264
references: https://data.geoscience.earth/ncl/geoera/ref/7267
references: https://data.geoscience.earth/ncl/geoera/ref/7262
references: https://data.geoscience.earth/ncl/geoera/ref/7343
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_965
broader: Luhe Line

Engelshof Subfault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:17.281Z
preferred label: Engelshof Nebenstörung @de
notation: DE-BY_1396
definition: WSW-ENE bis W-E verlaufender Nord-Ast der Luhe Störung an der Kreuzung der Luhe Linie [DE-BY_1387] mit der Fränkischen Linie [DE-BY_1398]. @de
definition: WSW-ENE to W-E trending northern branch of Luhe Fault at the intersection of Luhe Line [DE-BY_1387] and Franconian Line [DE-BY_1398].
references: https://data.geoscience.earth/ncl/geoera/ref/7262
references: https://data.geoscience.earth/ncl/geoera/ref/7374
references: https://data.geoscience.earth/ncl/geoera/ref/7295
sf touches: Irchenried Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1396
broader: Luhe Fault

Kindlas Fault
limit type: reverseFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:17.225Z
preferred label: Kindlas Störung @de
notation: DE-BY_1384
definition: W-E verlaufende, steil nach N einfallende Aufschiebung als Verbindung der nach NW abdrehenden Luhe Störung [DE-BY_965] und der NW-SE verlaufenden Freihunger Störung [DE-BY_990]. @de
definition: W-E trending, steeply N dipping reverse fault connecting Luhe Fault [DE-BY_965] veering to the NW and NW-SE trending Freihung Fault [DE-BY_990].
references: https://data.geoscience.earth/ncl/geoera/ref/7267
references: https://data.geoscience.earth/ncl/geoera/ref/7320
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1384
broader: Luhe Line

Ehenbach Fault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/7295
type: Concept
created: 2021-01-25T14:23:17.189Z
preferred label: Ehenbach Störung @de
notation: DE-BY_1383
definition: WSW-ENE streichende Störung mit geringen Versatz als vermutete Verbindung zwischen der Krickelsdorf-Kainsricht Störung [DE-BY_1381] und Kindlas Störung [DE-BY_1384]. @de
definition: WSW-ENE striking fault featuring a minor throw, as the inferred link of Krickelsdorf-Kainsricht Fault [DE-BY_1381] and Kindlas Fault [DE-BY_1384].
references: https://data.geoscience.earth/ncl/geoera/ref/7267
references: https://data.geoscience.earth/ncl/geoera/ref/7320
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1383
broader: Luhe Line

Krickelsdorf-Kainsricht Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:17.161Z
preferred label: Krickelsdorf-Kainsrichter Störung @de
notation: DE-BY_1381
definition: SW-NE streichende Störung mit geringem Versatz als westliches Ende der Luhe Linie. @de
definition: SW-NE striking fault featuring a minor throw, as the inferred western termination of Luhe Line.
references: https://data.geoscience.earth/ncl/geoera/ref/7267
references: https://data.geoscience.earth/ncl/geoera/ref/7320
sf touches: Gebenbach-Krickelsdorf Fault
sf touches: Brunnhof Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1381
broader: Luhe Line

Fensterbach Fault
limit type: reverseFault
type: Fault
type: Limit
sf touches: Jura Reverse Fault
narrower: Urspring-Lintach Fault
sf touches: Pfahl Reverse Fault
sf touches: Schmidgaden Rotliegend Graben boundaries
type: Concept
created: 2021-01-25T14:23:16.902Z
preferred label: Fensterbach Störung @de
notation: DE-BY_970
alternative label: Fensterbach-Aufschiebung @de
alternative label: Naabgebirgs-Randstörung @de
definition: Von Gebenbach SW Hirschau bis Dürnsricht ziehende, großenteils dem von NNW-SSE auf NW-SE umbiegenden Fensterbachtal folgende, steil nach ± NE einfallende Aufschiebung mit einem Versatz von bis zu über 200 m. Südwestgrenze des Naabgebirges als westlicher Sporn der Böhmischen Masse. Schneidet sowohl die Jura-Aufschiebung [DE-BY_1365] des Pfahl Aufschiebungssystems [DE-BY_1363], als auch den Rotliegendgraben von Schmidgaden im Westen ab. Eine Verbindung zur Pittersberger Störung [DE-BY_1374] im Süden wird vermutet (Bauberger & Streit 1982), ist aber nicht nachgewiesen. @de
definition: Running from Gebenbach SW Hirschau on to Dürnsricht, largely tracing the Fensterbach Valley veering from NNW-SSE to NW-SE, steeply NE dipping reverse fault with a throw of up to more than 200 m. Southwestern borderline of the Naabgebirge, the western spur of the Bohemian Massif. Truncating the Jura Reverse Fault [DE-BY_1365] of the Pfahl Reverse Fault System [DE-BY_1363], as well as the Schmidgaden Rotliegend Graben, in the west. A connection / soft link with Pittersberg Fault [DE-BY_1374] in the south is assumed (Bauberger & Streit 1982) but not evidenced.
narrower: Gebenbach-Krondorf Fault
narrower: Scharhof Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4114
references: https://data.geoscience.earth/ncl/geoera/ref/7369
references: https://data.geoscience.earth/ncl/geoera/ref/7267
references: https://data.geoscience.earth/ncl/geoera/ref/7265
narrower: Brunnhof Fault
narrower: Wenzelberg Fault
sf touches: Krickelsdorf-Kainsricht Fault
narrower: Gebenbach-Krickelsdorf Fault
narrower: Gebenbach Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_970
broader: Bohemian Massif Western Margin System

Wenzelberg Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:17.098Z
preferred label: Wenzelberg Störung @de
notation: DE-BY_1386
definition: SW-NE verlaufende Grenzlinie zwischen der Permotrias im Norden und dem variszischen Grundgebirge im Süden. @de
definition: SW-NE trending fault marking the borderline between the Permo-Triassic to the north and the Variscan Basement to the south.
references: https://data.geoscience.earth/ncl/geoera/ref/7267
sf touches: Scharhof Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1386
broader: Fensterbach Fault

Scharhof Fault
limit type: reverseFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:17.069Z
preferred label: Scharhof Störung @de
notation: DE-BY_1385
definition: NNW-SSE verlaufende, ca. 60° nach WSW einfallende Aufschiebung mit einer Sprunghöhe von bis zu 35 m. @de
definition: NNW-SSE trending, approx. 60° WSW dipping reverse fault featuring a throw of up to 35 m.
references: https://data.geoscience.earth/ncl/geoera/ref/7356
references: https://data.geoscience.earth/ncl/geoera/ref/7267
sf touches: Wenzelberg Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1385
broader: Fensterbach Fault

Brunnhof Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:17.041Z
preferred label: Brunnhof Störung @de
notation: DE-BY_1382
definition: NW-SE bis N-S verlaufende Querstörung zur Krickelsdorf-Kainsricht Störung [DE-BY_1381]. Abschiebung mit einer Sprunghöhe bis zu 40 m. @de
definition: NW-SE to N-S trending lateral fault of Krickelsdorf-Kainsricht Fault [DE-BY_1381]. Normal fault with a throw of up to 40 m.
references: https://data.geoscience.earth/ncl/geoera/ref/7267
sf touches: Krickelsdorf-Kainsricht Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1382
limit type: normalFault
broader: Fensterbach Fault

Gebenbach-Krickelsdorf Fault
type: Fault
type: Limit
sf touches: Gebenbach Fault
sf touches: Krickelsdorf-Kainsricht Fault
type: Concept
created: 2021-01-25T14:23:17.014Z
preferred label: Gebenbach-Krickelsdorf Störung @de
notation: DE-BY_1397
definition: Aus dem 20 m Sprung der Streichlinien abgeleiteter, ostwärts gebogener, SSW-NNE verlaufender Ost-Ast der T-Verzweigung am Nordende der Fensterbach Störung [DE-BY_970], der diese mit der Krickelsdorf-Kainsricht Störung (DE-BY_1381] verbindet, dem westlichsten Ausläufer der Luhe Line [DE-BY_1387]. @de
definition: Inferred from the 20 m drop of contour line, eastward arcuate SSW-NNE trending eastern leg of T junction at the northern termination of Fensterbach Fault [DE-BY_970] linking that with Krickelsdorf-Kainsricht Fault (DE-BY_1381], the westernmost section of Luhe Line [DE-BY_1387].
references: https://data.geoscience.earth/ncl/geoera/ref/7267
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1397
broader: Fensterbach Fault

Gebenbach Fault
type: Fault
type: Limit
sf touches: Gebenbach-Krickelsdorf Fault
type: Concept
created: 2021-01-25T14:23:16.986Z
preferred label: Gebenbach Störung @de
notation: DE-BY_1380
alternative label: Gebenbacher Störung @de
definition: WNW-ESE verlaufender West-Ast der T-Verzweigung am Nordende der Fensterbach Störung [DE-BY_970] mit einer Sprunghöhe von bis zu 15 m. @de
definition: WNW-ESE trending western leg of T junction at the northern termination of Fensterbach Fault [DE-BY_970], featuring a throw of up to 15 m.
references: https://data.geoscience.earth/ncl/geoera/ref/7267
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1380
broader: Fensterbach Fault

Gebenbach-Krondorf Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:16.958Z
preferred label: Gebenbach-Krondorf Störung @de
notation: DE-BY_1379
alternative label: Krondorfer Störung @de
definition: Ostwärts gebogen, NNW-SSE verlaufender Zweig des nördlichen Ausläufers der Fensterbach Störung [DE-BY_970], mit einer nach N hin rasch abnehmenden Sprunghöhe von bis zu 130 m. @de
definition: NNW-SSE trending eastward arcuate branch of the northern tail of Fensterbach Fault [DE-BY_970]. Its throw of up to 130 m rapidly decreases to the north.
references: https://data.geoscience.earth/ncl/geoera/ref/7267
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1379
broader: Fensterbach Fault

Urspring-Lintach Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:16.930Z
preferred label: Urspring-Lintach Störung @de
notation: DE-BY_1375
alternative label: Urspringer Störung @de
definition: Gewellt NNW-SSE verlaufende Störung die der Fensterbach Störung [DE-BY_970] entspringt und subparallel zu dieser verläuft. @de
definition: Undulate NNW-SSE trending fault branching off and running subparallel to Fensterbach Fault [DE-BY_970].
references: https://data.geoscience.earth/ncl/geoera/ref/7267
references: https://data.geoscience.earth/ncl/geoera/ref/7369
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1375
broader: Fensterbach Fault

Keilberg Fault System
limit type: reverseFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:16.598Z
preferred label: Keilberg Störungssystem @de
notation: DE-BY_1484
definition: Mindestens von Büchelkühn S Schwandorf bis nach Regensburg ziehendes, N-S bis NNW-SSE verlaufendes Störungssystem bestehend aus einer östlichen, senkrecht stehenden bis 85° nach ± E einfallenden Aufschiebung mit großer Sprunghöhe und einer westlich subparallelen, steil (85°-60°) nach ± E einfallenden Abschiebung mäßiger Sprunghöhe, mit dazwischenliegenden Grabenstrukturen. @de
definition: Running at least from Büchelkühn south of Schwandorf to Regensburg, N-S to NNW-SSE trending fault system of an eastern vertical to 85° ± E dipping large throw reverse (step) fault and a subparallel vertical to steeply (85°-60°) ± E dipping moderate throw normal fault, forming a graben structure.
narrower: Keilberg Fault
narrower: Ponholz-Diesenbach Fault
narrower: Bubach-Maxhütte Fault
narrower: Büchelkühn-Bubach Fault
narrower: Kreuzbügerl Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7263
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7331
references: https://data.geoscience.earth/ncl/geoera/ref/6358
references: https://data.geoscience.earth/ncl/geoera/ref/4073
sf touches: Danube Fault System
narrower: Regen Valley Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1484
broader: Bohemian Massif Western Margin System

Kreuzbügerl Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:16.764Z
preferred label: Kreuzbügerl Störung @de
notation: DE-BY_1370
definition: Nördliche Fortsetzung der Keilberg Störung [DE-BY_761] nach ihrer Kreuzung mit der Bubach-Maxhütte Störung [DE-BY_1368]. Westwärts gebogene, insgesamt N-S verlaufende, saigere bis subvertikale Abschiebung mit einer Sprunghöhe von höchstens 50 m. @de
definition: Northern continuation of Keilberg Fault [DE-BY_761] after intersection with Bubach-Maxhütte Fault [DE-BY_1368]. Westward arcuate, overall N-S trending, vertical to subvertical reverse fault with a throw of less than 50 m.
narrower: Striessendorf Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7331
sf touches: Bubach-Maxhütte Fault
sf touches: Büchelkühn-Bubach Fault
sf touches: Striessendorf Fault
sf touches: Keilberg Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1370
broader: Keilberg Fault System

Striessendorf Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:16.791Z
preferred label: Striessendorf Querstörung @de
notation: DE-BY_1371
definition: W-E streichende Querstörung, die den nördlichen Teil der Kreuzbügerl Störung [DE-BY_1370] nach E hin versetzt. @de
definition: W-E striking lateral fault offsetting the northern section of Kreuzbügerl Fault [DE-BY_1370] to the east.
references: https://data.geoscience.earth/ncl/geoera/ref/7331
sf touches: Kreuzbügerl Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1371
broader: Kreuzbügerl Fault

Büchelkühn-Bubach Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:16.736Z
preferred label: Büchelkühn-Bubach Störung @de
notation: DE-BY_1369
definition: Nördliche Fortsetzung der Bubach-Maxhütte Störung [DE-BY_1368]. N-S streichende, saigere bis subvertikale Abschiebung mit einer Sprunghöhe von höchstens 50 m. Bildet mit der Bubach-Maxhütte Störung [DE-BY_1368] eine flachen Graben. @de
definition: Northern continuation of Bubach-Maxhütte Fault [DE-BY_1368]. N-S striking, vertical to subvertical normal fault with a throw of less than 50 m, forming a shallow graben with Bubach-Maxhütte Fault [DE-BY_1368].
references: https://data.geoscience.earth/ncl/geoera/ref/7331
references: https://data.geoscience.earth/ncl/geoera/ref/6358
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1369
limit type: normalFault
broader: Keilberg Fault System

Bubach-Maxhütte Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:16.708Z
preferred label: Bubach-Maxhütte Störung @de
notation: DE-BY_1368
definition: Gewellt NNW-SSE verlaufende, steil (85°-60°) nach ± E einfallende Abschiebung mit einem Vertikalversatz von etwa 20 m. Bildet mit der östlich parallel verlaufenden Keilberg Störung [DE-BY_761] eine flachen Graben. Vermutete nördliche Fortsetzung der Ponholz-Diesenbach Störung [DE-BY_1367] und, nach ihrer Kreuzung mit der Keilberg Störung [DE-BY_761], im Norden mit der Büchelkühn-Bubach Fault [DE-BY_1369] verbunden. @de
definition: Undulate NNW-SSE trending, steeply (85°-60°) ± E dipping normal fault featuring a throw of about 20 m, forming a shallow graben with Keilberg Fault [DE-BY_761] paralleling to the east. Inferred northern continuation of Ponholz-Diesenbach Fault [DE-BY_1367] and, after intersecting Keilberg Fault [DE-BY_761], connected to Büchelkühn-Bubach Fault [DE-BY_1369] in its north.
references: https://data.geoscience.earth/ncl/geoera/ref/6358
references: https://data.geoscience.earth/ncl/geoera/ref/7331
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1368
limit type: normalFault
broader: Keilberg Fault System

Ponholz-Diesenbach Fault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6358
type: Concept
created: 2021-01-25T14:23:16.681Z
preferred label: Ponholz-Diesenbach Störung @de
notation: DE-BY_1367
definition: Nördliche Fortsetzung der Regental Störung [DE-BY_1243]. Gewellt N-S verlaufende, steil (85°-60°) ± E einfallende Abschiebung parallel zur Keilberg Störung [DE-BY_761]. @de
definition: Northern continuation of Regen Valley Fault [DE-BY_1243] and connectetd to Bubach-Maxhütte Fault [DE-BY_1368] in its north. Undulate N-S trending, steeply (85°-60°) ± E dipping normal fault paralleling Keilberg Fault [DE-BY_761].
references: https://data.geoscience.earth/ncl/geoera/ref/7331
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1367
limit type: normalFault
broader: Keilberg Fault System

Regen Valley Fault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6358
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7331
references: https://data.geoscience.earth/ncl/geoera/ref/7263
definition: Gewellt N-S bis NNW-SSE verlaufende, steil (85°-60°) ± E einfallende Abschiebung zwischen Teublitz und Regensburg. Westgrenze der Grabenstrukturen von Maxhütte und Laub, parallel zur Keilberg-Störung [DE-BY_761]. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4073
definition: Undulate N-S to NNW-SSE trending, steeply (85°-60°) ± E dipping normal fault running from Teublitz to Regensburg. Western boundary of the graben structures of Maxhütte and Laub, paralleling Keilberg Fault [DE-BY_761].
type: Concept
created: 2020-10-09T11:35:35.757Z
notation: DE-BY_1243
preferred label: Regental Störung @de
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1243
limit type: normalFault
broader: Keilberg Fault System

Keilberg Fault
limit type: reverseFault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6358
references: https://data.geoscience.earth/ncl/geoera/ref/7269
definition: N-S bis NNW-SSE (eggisch) verlaufende, senkrecht stehende bis 85° nach ± E einfallende Aufschiebung zwischen Teublitz und Regensburg. Westliche Grenze der Böhmischen Masse mit Sprunghöhen bis zu 1,2 km. @de
definition: N-S to NNW-SSE trending, vertical to 85° ± E dipping reverse fault running from Teublitz to Regensburg. Principal tectonic boundary featuring throws up to 1.2 km, tracing the western limit of the Bohemian Massif.
references: https://data.geoscience.earth/ncl/geoera/ref/7331
references: https://data.geoscience.earth/ncl/geoera/ref/4073
sf touches: Donaurand Fault Scarp
sf touches: Deuerling Fault
alternative label: Keilberg-Sprung @de
references: https://data.geoscience.earth/ncl/geoera/ref/7263
type: Concept
created: 2020-10-09T11:35:35.729Z
notation: DE-BY_761
alternative label: Keilberg-Abbruch @de
preferred label: Keilberg Störung @de
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_761
broader: Keilberg Fault System

Pittersberg Fault
limit type: reverseFault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/4114
type: Concept
created: 2021-01-25T14:23:16.875Z
preferred label: Pittersberger Störung @de
notation: DE-BY_1374
definition: Von Freihöls bis Kreith ziehende, leicht gewellt NNW-SSE streichende, steil nach WSW einfallende Aufschiebung der Ostflanke des Pittersberger Sattels auf den Bodenwöhrer Senke. Geht nach SSE hin in eine Flexur und den Pittersberger Sattel über (möglicherweise drapierende Falte in Hangenden der tiefen Störung) und steht wohl mit den nördlichen Ausläufern der Keilberg Störung [DE-BY_761] bzw. Regental Störung [DE-BY_1243] in Verbindung (Bauberger & Streit 1982). Eine Verbindung zur Fensterbach Störung [DE-BY_970] im Norden wird vermutet (Bauberger & Streit 1982), ist aber nicht nachgewiesen. @de
definition: Running from Freihöls to Kreith, slightly undulate NNW-SSE trending, steeply WSW dipping reverse fault thrusting the eastern slope of the Pittersberg anticline onto the Bodenwöhr Trough. Towards the SSE, passing into a flexure and the southern Pittersberg anticline (possibly a drape fold passively conforming upon the faulted bedrock), the structure probably is connected to the extensions of Keilberg Fault [DE-BY_761] resp. Regen Valley Fault [DE-BY_1243] (Bauberger & Streit 1982). A connection (soft link) with Fensterbach Fault [DE-BY_970] to the north is assumed (Bauberger & Streit 1982) but not evidenced.
references: https://data.geoscience.earth/ncl/geoera/ref/7265
references: https://data.geoscience.earth/ncl/geoera/ref/7343
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1374
broader: Bohemian Massif Western Margin System

Franconian Line
limit type: reverseFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:17.309Z
preferred label: Fränkische Linie @de
notation: DE-BY_1398
definition: Tektonische Großstruktur an der Grenzlinie der Böhmischen Masse zur Süddeutschen Schichtstufenland, die sich grob NNW-SSE über mehr als 100 km von Stockheimer Becken an der Grenze zu Thüringen bis zur Luhe Line (DE-BY_1387] hinzieht. Auch wenn morphologische deutlich als Abbruch erkennbar, sind ihre nach NE hin einfallenden Auf- und Überschiebungen mit z.T. enormen Vertikalversätzen nur in Abschnitten kartierbar, da von mächtigen Schuttmassen überdeckt, sind geophysikalisch aber nachgewiesen. Nach Zulauf (1991) können die wesentlichen Deformationsphasen der Fränkischen Linie folgendermaßen skizziert werden: Anlage der Fränkischen Linie währen der postvarizischen NE-SW Kompression, dextrale Bewegungen während der N-S Kompression in der Unterkreide, Aufschiebung und Hebung des Grundgebirges auf das Vorland während der alpidischen Gebirgsbildung (Oberkreide bis Paläogen). @de
definition: Principal tectonic structure of eastern Bavaria, running for more than 100 km roughly NNW-SSE, from Thuringia (entering Bavaria at the Stockheim Rotliegend Trough) on to Luhe Line (DE-BY_1387], separating the Bohemian Massif to the east from the South German Scarpland to the west. Even though physiographically forming a conspicuous scarp, its NE dipping large throw reverse faults are mappable in certain segments only, as covered by thick debris, but are evidenced in geophysical surveys. Main movement stages involving the Franconian Line have been late Variscan NE-SW compression, dextral shearing during Early Cretaceous and the uplift of the Variscan Basement and the overthrust of the foreland during Alpine orogeny (Zulauf 1991).
narrower: Gleitsbach-Windbühl Fault
narrower: Irchenried Fault
narrower: Edeldorf-Almesbach Fault
narrower: Edeldorf-Töglersricht Fault
narrower: Klobenreuth-Edeldorf Fault
narrower: Klobenreuth-Neustadt Fault
narrower: Waldeck-Klobenreuth Fault
narrower: Altenparkstein Fault
narrower: Fichtel Mountains Scarp
narrower: Franconian Forest Scarp
narrower: Föritz-Pressig Faults
narrower: Burggrub Flexure
narrower: Föritz Fault
narrower: Sonneberg Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7295
references: https://data.geoscience.earth/ncl/geoera/ref/7282
references: https://data.geoscience.earth/ncl/geoera/ref/7283
references: https://data.geoscience.earth/ncl/geoera/ref/7376
in scheme: Tectonic Boundary Objects in Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11574
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11575
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11576
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11578
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11693
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11694
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11855
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11887
notation: LfU-BY_1398
broader: Bohemian Massif Western Margin System

Klobenreuth-Edeldorf Fault
limit type: reverseFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:17.449Z
preferred label: Klobenreuth-Edeldorf Störung @de
notation: DE-BY_1404
definition: NW-SE bis NNW-SSE verlaufender Haupt-Ast der Fränkischen Linie zwischen Obersdorf bei Klobenreuth und Edelhof, im nördlichen Teil SW-wärts parallel zur Klobenreuth-Neustadt Störung [DE-BY_1405]. Die beiden Teil-Äste laufen unter dem Waldnaabtal zusammen @de
definition: NW-SE to NNW-SSE trending main branch of Franconian Line running from Obersdorf near Klobenreuth to Edelhof, in its northwestern part SW-wards parallel to Klobenreuth-Neustadt Fault [DE-BY_1405]. The two branches merge underneath the Waldnaab valley.
references: https://data.geoscience.earth/ncl/geoera/ref/7374
references: https://data.geoscience.earth/ncl/geoera/ref/7295
sf touches: Altenparkstein Fault
sf touches: Klobenreuth-Neustadt Fault
sf touches: Waldeck-Klobenreuth Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1404
broader: Franconian Line

Föritz-Pressig Faults
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:17.727Z
preferred label: Föritz-Pressig Störungen @de
notation: DE-BY_1428
definition: Gruppe N-S bis NNW-SSE verlaufender Störungen die die Fränkische Linie nach Süden ablenken und das Stockheimer Becken in Horst- und Graben-artige Schollen zerlegen. Wahrscheinlich bei der Reaktivierung variszischer, NE-SE gerichteter Druckspannungsstrukturen während der dextralen Seitenverschiebung in der Unterkreide in einer Transferzone entstandene Blattverschiebungs­duplexe. In dehnenden Duplexstrukturen entstehen dabei Senken, in denen jüngere Ablagerungen, vor der Erosion geschützt, erhalten bleiben. Diese Strukturen wurden durch die Hebung und Aufschiebung des Grundgebirges auf das Vorland während der Oberkreide und im Paläogen überprägt. @de
definition: Array of N-S to NNW-SSE trending faults deflecting the direction of Franconian Line to the south, and, by fractionizing Stockheim Basin into subparallel fault-bound horst- and graben-like blocks, separating the crescent-shaped Rotliegend outlier of the trough. Probably strike-slip duplexes of a transfer zone generated by the dextral movement during Early Cretaceous, reactivating the NE-SW compressional structures created while Variscan orogeny. Extensional bends thereby create basins which might expose younger deposits preserved from erosion. These structures have been reshaped as the result of Bohemian Massif uplift and thrust onto the foreland during Late Cretaceous and Paleogene.
narrower: Föritz-Stockheim Fault
narrower: Stockheim Fault
narrower: Welitsch Fault
narrower: Pressig Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7317
references: https://data.geoscience.earth/ncl/geoera/ref/7289
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7280
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1428
broader: Franconian Line

Föritz-Stockheim Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:17.755Z
preferred label: Föritz-Stockheim Störung @de
notation: DE-BY_1506
definition: NE-wärts gebogen, insgesamt NNW-SSE verlaufende, nach WSW einfallende Abschiebung; bildet im Süden die Westgrenze des Traindorf Horsts gegen die Stockheimer (Graben-)Scholle. @de
definition: NE-wards arcuate, overall NNW-SSE trending, WSW dipping normal fault, in its south forming the western boundary of Traindorf Horst towards Stockheim (graben-)block.
references: https://data.geoscience.earth/ncl/geoera/ref/7317
references: https://data.geoscience.earth/ncl/geoera/ref/7289
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1506
limit type: normalFault
broader: Föritz-Pressig Faults

Pressig Fault
limit type: reverseFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:17.838Z
preferred label: Pressig Störung @de
notation: DE-BY_955
definition: NNW-SSE streichende Aufschiebung mit Einfallrichtung WSW, Ostrand des Spitzberg Horsts gegen die Grossauer (Graben-)Scholle. @de
definition: NNW-SSE trending reverse fault with dip direction WSW, eastern boundary of Spitzberg Horst towards Grossau (graben-)block.
references: https://data.geoscience.earth/ncl/geoera/ref/7317
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7289
references: https://data.geoscience.earth/ncl/geoera/ref/7280
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_955
broader: Föritz-Pressig Faults

Welitsch Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:17.810Z
preferred label: Welitsch Störung @de
notation: DE-BY_954
definition: NNW-SSE streichende Abschiebung mit Einfallrichtung WSW, Westrand des Spitzberg Horsts gegen die Reitscher (Graben-)Scholle. @de
definition: NNW-SSE trending normal fault with dip direction WSW, western boundary of Spitzberg Horst towards Reitsch (graben-)block.
references: https://data.geoscience.earth/ncl/geoera/ref/7317
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7280
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_954
limit type: normalFault
broader: Föritz-Pressig Faults

Stockheim Fault
limit type: reverseFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:17.782Z
preferred label: Stockheim Störung @de
notation: DE-BY_953
definition: NNW-SSE streichende Aufschiebung mit Einfallrichtung ENE (abschiebend/strike-slip invertiert). Westliche Begrenzung der Reitscher (Graben-)Scholle gegen den Traindorfer Horst. @de
definition: NNW-SSE trending reverse fault with dip direction ENE (normal/strike-slip inverted), western boundary of Reitsch (graben-)block towards Traindorf Horst.
references: https://data.geoscience.earth/ncl/geoera/ref/7317
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7280
references: https://data.geoscience.earth/ncl/geoera/ref/7292
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_953
broader: Föritz-Pressig Faults

Edeldorf-Töglersricht Fault
limit type: reverseFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:17.421Z
preferred label: Edeldorf-Töglersricht Störung @de
notation: DE-BY_1403
definition: Gewellt NNW-SSE verlaufender, steil bis mäßig steil nach ENE einfallender Haupt-Ast der Fränkischen Linie mit einer Sprunghöhe von bis zu 100 m. @de
definition: Undulate NNW-SSE trending, steeply to intermediately ENE dipping reverse fault featuring a throw of at least 100 m. Main branch of Franconian Line.
references: https://data.geoscience.earth/ncl/geoera/ref/7374
references: https://data.geoscience.earth/ncl/geoera/ref/7295
sf touches: Edeldorf-Almesbach Fault
sf touches: Gleitsbach-Windbühl Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1403
broader: Franconian Line

Edeldorf-Almesbach Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:17.393Z
preferred label: Edeldorf-Almesbach Störung @de
notation: DE-BY_1402
definition: Subparallel zur Edeldorf-Töglersricht Störung [DE-BY_1403] NNW-SSE verlaufender westlicher Ast der Fränkischen Linie; trennt Unter-Rotliegend im Westen von Oberkarbon im Osten. @de
definition: Offsetting Lower Rotliegend in the west from Upper Carboniferous in the east, NNW-SSE trending western branch of Franconian Line running subparallel to Edeldorf-Töglersricht Fault [DE-BY_1403].
references: https://data.geoscience.earth/ncl/geoera/ref/7374
references: https://data.geoscience.earth/ncl/geoera/ref/7295
sf touches: Edeldorf-Töglersricht Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1402
broader: Franconian Line

Irchenried Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:17.365Z
preferred label: Irchenried Störung @de
notation: DE-BY_1400
definition: Gewellt N-S verlaufender West-Ast der Gleitsbach-Windbühl Störung [DE-BY_1399], der das Unterrotliegend im Westen vom Oberkarbon im Osten abgrenzt. @de
definition: Undulate N-S trending western branch of Gleitsbach-Windbühl Fault [DE-BY_1399] offsetting Lower Rotliegend in the west from Upper Carboniferous (Pennsylvanian) in the east.
references: https://data.geoscience.earth/ncl/geoera/ref/7374
sf touches: Gleitsbach-Windbühl Fault
sf touches: Engelshof Subfault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1400
broader: Franconian Line

Gleitsbach-Windbühl Fault
limit type: reverseFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:17.337Z
preferred label: Gleitsbach-Windbühl Störung @de
notation: DE-BY_1399
definition: N-S bis NNW-SSE verlaufende, steil bis mäßig steil nach E einfallende Aufschiebung mit einem Versatz vom mindestens 100 m. Südlichster Abschnitt der Fränkischen Linie [DE-BY_1398] zwischen dem Gleitsbachtal im Norden und der Luhe Störung [DE-BY_965], die sie leicht versetzt, im Süden. Eine Fortsetzung, über die Luhe Störung hinaus, ist wahrscheinlich ("Oberpfalzlineament"), konnte bisher aber nicht nachgewiesen werden (Bauberger 1993). @de
definition: N-S to NNW-SSE trending, steeply to intermediately E dipping reverse fault featuring a throw of at least 100 m. Southernmost section of Franconian Line [DE-BY_1398] running from Gleitsbach valley in the north to Luhe Fault [DE-BY_965] in the south, slightly displacing Luhe Fault. A continuation beyond Luhe Fault further to the south is probable ("Oberpfalzlineament") but not evidenced yet (Bauberger 1993).
references: https://data.geoscience.earth/ncl/geoera/ref/7262
references: https://data.geoscience.earth/ncl/geoera/ref/7374
references: https://data.geoscience.earth/ncl/geoera/ref/7295
sf touches: Irchenried Fault
sf touches: Edeldorf-Almesbach Fault
sf touches: Luhe Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1399
broader: Franconian Line

Franconian Forest Scarp
limit type: reverseFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:17.644Z
preferred label: Frankenwald-Randbruch @de
notation: DE-BY_1431
alternative label: Frankenwaldrandstörung @de
definition: Abfolge von grob NW-SE verlaufenden, steil bis flach nach ± NE einfallenden Aufschiebungs-Segmenten am Südwest-Abbruch des Frankenwaldes. Polyphase Aufschiebungen, z.T. in mehrere Teilstörungen aufgespalten, mit einer Gesamt-Sprunghöhe bis über 1 km, wiederholt von kleinräumigen Querstörungen versetzt. @de
definition: Array of roughly NW-SE trending, steeply to gently ± NE dipping reverse fault segments, forming the southwestern scarp of the Franconian Forest. Polyphase reverse faults, partly split up in subfaults, featuring a (cumulative) throw of up to more than 1 km, repeatedly offset by small-scale lateral faults.
narrower: Leuschberg-Rennesberg Faults
narrower: Letzenhof Fault
sf touches: Teuschnitz Syncline longitudinal faults
references: https://data.geoscience.earth/ncl/geoera/ref/7284
references: https://data.geoscience.earth/ncl/geoera/ref/7286
references: https://data.geoscience.earth/ncl/geoera/ref/7282
references: https://data.geoscience.earth/ncl/geoera/ref/7297
references: https://data.geoscience.earth/ncl/geoera/ref/7308
sf touches: Münchberg Klippe basal thrust
sf touches: Bavarian Facies basal thrust
sf touches: Fichtel Mountains Scarp
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1431
broader: Franconian Line

Letzenhof Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:17.699Z
preferred label: Letzenhof Störung @de
notation: DE-BY_1430
definition: WNW-ESE verlaufende, steil nach NNE einfallende Nebenstörung des Frankenwald-Randbruchs. Wird im Osten von der Kronach Störung [DE-BY_993] abgeschnitten und setzt sich im Nordwesten über den Hauptast [DE-BY_1431] hinweg als Welitsch Störung [DE-BY_954] ins Stockheimer Becken fort. Wahrscheinlich, als ehemaliger, prä-Unterkreide-Dextral-Scherung, Hauptast des Frankenwald-Randbruchs, südlicher extensiver Bogen der Blattverschiebungs¬duplexe des Stockheimer Beckens [DE-BY_1428]. @de
definition: WNW-ESE trending, steeply NNE dipping subsidiary fault of Franconian Forest Scarp. Truncated by Kronach Fault [DE-BY_993] to the east and crossing today's main branch [DE-BY_1431], continuing as Welitsch Fault [DE-BY_954] in Stockheim Basin to the northwest. Probably southern extensional bend of the Stockheim Basin strike-slip duplexes [DE-BY_1428] as the pre-Early-Cretaceous-dextral-shearing main branch of the Franconian Forest Scarp.
references: https://data.geoscience.earth/ncl/geoera/ref/7282
references: https://data.geoscience.earth/ncl/geoera/ref/7317
references: https://data.geoscience.earth/ncl/geoera/ref/7678
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1430
broader: Franconian Forest Scarp

Leuschberg-Rennesberg Faults
limit type: reverseFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:17.671Z
preferred label: Leuschberg-Rennesberg Verwerfungen @de
notation: DE-BY_1477
definition: Gruppe NW-SE verlaufender, steil nach SW einfallender Abschiebungen mit einer Sprunghöhe bis zu 200 m, im Bogeninnern der WNW-ESE auf N-S Umlenkung des Frankenwald-Randbruchs bei Zeyern. Möglicherweise Blattverschiebungs­duplexe der dextralen Seitenveschiebung in der Unterkreide, während der die variszischen, NE-SE gerichteten Druckspannungsstrukturen reaktiviert wurden; durch die Hebung und Aufschiebung des Grundgebirges auf das Vorland während der Oberkreide und im Paläogen überprägt und von Querstörungen (z.B. Kronach Störung [DE-BY_993]) versetzt. @de
definition: Array of NW-SE trending, steeply SW dipping normal faults with a throw up to 200 m, running inwards the NE-ward arcuate Franconian Forest Scarp at Zeyern. Possibly strike-slip duplexes generated by the dextral movement during Early Cretaceous, reactivating the NE-SW compressional structures created while Variscan orogeny. Altered and offset by lateral faults (e.g. Kronach Fault [DE-BY_993]) as a result of Bohemian Massif uplift and thrust onto the foreland during Late Cretaceous and Paleogene.
references: https://data.geoscience.earth/ncl/geoera/ref/7282
references: https://data.geoscience.earth/ncl/geoera/ref/7678
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1477
broader: Franconian Forest Scarp

Sonneberg Fault
limit type: reverseFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:17.921Z
preferred label: Sonneberg Störung @de
notation: DE-BY_1507
definition: NW-SE verlaufende, nach NE einfallende Aufschiebung; Fortsetzung der Fränkischen Linie auf thüringer Gebiet. @de
definition: NW-SE trending, NE dipping reverse fault; continuation of Franconian Line on Thuringian territory.
references: https://data.geoscience.earth/ncl/geoera/ref/7289
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1507
broader: Franconian Line

Fichtel Mountains Scarp
limit type: reverseFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:17.588Z
preferred label: Fichtelgebirgs-Randbruch @de
notation: DE-BY_1432
alternative label: Fichtelgebirgsrandstörung @de
definition: NNW-SSE bis WNW-ESE verlaufender mittlerer Abschnitt der Fränkischen Linie zwischen der Müchberger Gneissmasse und der Erbendorfer Linie [DE-BY_1447]. Polyphase Abschiebungssegmente (z.T. als Staffelbruch) mit einer Gesamt-Sprunghöhe bis über 1 km, wiederholt von Querstörungen versetzt, wie z.B. der Muckenreuther Störung [DE-BY_1418]. @de
definition: Veering between a NNW-SSE to WNW-ESE trend, middle segment of Franconian Line running from Münchberg Klippe to Erbendorf Line [DE-BY_1447]. Polyphase reverse fault (or step fault) segments featuring a (cumulative) throw of up to more than 1 km, repeatedly offset by lateral faults such as Muckenreuth Fault [DE-BY_1418].
hidden label: Fichtelgebirgsrandspalte
narrower: Muckenreuth Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7283
references: https://data.geoscience.earth/ncl/geoera/ref/7333
references: https://data.geoscience.earth/ncl/geoera/ref/7353
references: https://data.geoscience.earth/ncl/geoera/ref/7359
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1432
broader: Franconian Line

Muckenreuth Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:17.616Z
preferred label: Muckenreuther Störung @de
notation: DE-BY_1418
definition: N-S streichende größere Querstörung die den Fichtelgebirgs-Randbruch sinistral versetzt. @de
definition: N-S striking major lateral fault sinistrally offsetting fault segments of the Fichtel Mountains Scarp.
references: https://data.geoscience.earth/ncl/geoera/ref/7283
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1418
broader: Fichtel Mountains Scarp

Föritz Fault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:17.893Z
preferred label: Föritz-Störung @de
notation: DE-BY_1051
definition: N-S streichende Abschiebung mit Einfallrichtung E @de
definition: N-S striking normal fault with dip direction E
references: https://data.geoscience.earth/ncl/geoera/ref/7289
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7280
references: https://data.geoscience.earth/ncl/geoera/ref/7292
sf touches: Burggrub Flexure
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1051
limit type: normalFault
broader: Franconian Line

Altenparkstein Fault
limit type: reverseFault
type: Fault
type: Limit
sf touches: Kemnath-Waldeck Fault
type: Concept
created: 2021-01-25T14:23:17.560Z
preferred label: Altenparkstein Störung @de
notation: DE-BY_1407
alternative label: SE1 (Seismic Event 1)
alternative label: Altenparkstein Störungszone @de
alternative label: Seismischer Reflektor SE1 @de
definition: Von Waldeck nach Neustadt/Waldnaab ziehende, NW-SE verlaufende, steil bis mäßig nach NE einfallende Aufschiebung subparallel zur Waldeck-Klobenreuth Störungszone [DE-BY_1406]. Nach Markerhorizonten weist die dieser Ast der Fränkischen Line im Bereich der Erbendorfer Linie [DE-BY_1447] einen Vertikalversatz von bis zu 3,5 km auf (Wagner et al. 1997). @de
definition: NW-SE trending, steeply to intermediately NE dipping reverse fault subparallel to Waldeck-Klobenreuth Fault Zone [DE-BY_1406], running from Waldeck to Neustadt/Waldnaab. Inferred from marker horizons (Wagner et al. 1997) this branch of Franconian Line in the area of Erbendorf Line [DE-BY_1447] features a vertical displacement of up to 3.5 km.
references: https://data.geoscience.earth/ncl/geoera/ref/7310
references: https://data.geoscience.earth/ncl/geoera/ref/7309
references: https://data.geoscience.earth/ncl/geoera/ref/7373
sf touches: Klobenreuth-Edeldorf Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1407
broader: Franconian Line

Burggrub Flexure
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:17.865Z
preferred label: Burggrub Flexur @de
notation: DE-BY_1519
definition: Südwestwärts gebogene, N-S bis E-W verlaufende SW-Grenze des Stockheimer Beckens. Flexurartiges "Fehlstück" im Verlauf der von N-S auf E-W drehenden Fränkischen Linie. @de
definition: SW-wards arcuate N-S to W-E trending SW boundary of Stockheim Basin. Flexure-like "missing link" of the Franconian Line veering from N-S to E-W.
references: https://data.geoscience.earth/ncl/geoera/ref/7682
references: https://data.geoscience.earth/ncl/geoera/ref/7282
references: https://data.geoscience.earth/ncl/geoera/ref/7289
sf touches: Föritz Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7678
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1519
broader: Franconian Line

Waldeck-Klobenreuth Fault
limit type: reverseFault
type: Fault
type: Limit
sf touches: Hahneneggaten-Grötschenreuth Fault
sf touches: Fichtelnaab lateral faults
type: Concept
created: 2021-01-25T14:23:17.505Z
preferred label: Waldeck-Klobenreuth Störung @de
notation: DE-BY_1406
alternative label: Waldeck-Klobenreuth Fault Zone
alternative label: SE2 (Seismic Event 2)
alternative label: Waldeck-Klobenreuth Störungszone @de
alternative label: Seismischer Reflektor SE2 @de
definition: NW-SE trending, intermediately NE dipping reverse fault subparallel to Altenparkstein Fault Zone [DE-BY_1407] running from Waldeck to Obersdorf near Klobenreuth. Inferred from marker horizons (Wagner et al. 1997) this branch of Franconian Line in the area of Erbendorf Line [DE-BY_1447] features a vertical displacement of up to 1.5 km.
definition: Von Waldeck nach Neustadt/Waldnaab ziehende, NW-SE verlaufende, mäßig steil nach NE einfallende Aufschiebung subparallel zur Altenparkstein Störungszone [DE-BY_1407]. Nach Markerhorizonten weist die dieser Ast der Fränkischen Line im Bereich der Erbendorfer Linie [DE-BY_1447] einen Vertikalversatz von bis zu 1,5 km auf (Wagner et al. 1997). @de
narrower: Waldeck Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7310
references: https://data.geoscience.earth/ncl/geoera/ref/7309
references: https://data.geoscience.earth/ncl/geoera/ref/7373
references: https://data.geoscience.earth/ncl/geoera/ref/7295
sf touches: Klobenreuth-Neustadt Fault
sf touches: Klobenreuth-Edeldorf Fault
sf touches: Fichtel Mountains Scarp
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1406
broader: Franconian Line

Waldeck Fault
limit type: reverseFault
type: Fault
type: Limit
sf touches: Kemnath-Waldeck Fault
type: Concept
created: 2021-01-25T14:23:17.532Z
preferred label: Waldeck Störung @de
notation: DE-BY_1419
definition: Kurze Abschiebung zwischen der Altenparkstein Störungszone [DE-BY_1407] und Waldeck-Klobenreuth Störungszone [DE-BY_1406]. @de
definition: Short reverse fault in between Altenparkstein Fault Zone [DE-BY_1407] and Waldeck-Klobenreuth Fault Zone [DE-BY_1406].
references: https://data.geoscience.earth/ncl/geoera/ref/7282
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1419
broader: Waldeck-Klobenreuth Fault

Klobenreuth-Neustadt Fault
limit type: reverseFault
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:17.477Z
preferred label: Klobenreuth-Neustadt Störung @de
notation: DE-BY_1405
definition: NW-SE streichende intra-Basement Nebenstörung der Fränkischen Linie NE-wärts parallel zur Klobenreuth-Edeldorf Störung [DE-BY_1404) zwischen Obersdorf bei Klobenreuth und Neustadt/Waldnaab, wo die Teil-Äste zusammenlaufen. @de
definition: NW-SE striking intra-basement subfault of Franconian Line running NE-wards parallel to Klobenreuth-Edeldorf Fault [DE-BY_1404] from Obersdorf near Klobenreuth to Neustadt/Waldnaab, where the two branches merge.
references: https://data.geoscience.earth/ncl/geoera/ref/7295
sf touches: Klobenreuth-Edeldorf Fault
sf touches: Edeldorf-Töglersricht Fault
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1405
broader: Franconian Line

Teplá-Barrandian Terrane boundary
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.608Z
preferred label: Tepla-Barrandium Domänengrenze @de
notation: DE-BY_1494
definition: Vergleichbar dem Bug eines Eisbrechers ragt die südwestliche Ausbuchtung des in Tschechien großräumig verbreiteten Teplá-Barrandiums am Hohen Bogen östlich vom Cham weit nach Bayern herein. Diese Gabbroamphibolitmasse des Neukirchen-Kdyně-Komplex ist entlang von zwei polyphasen Haupt-Scherzonen auf bzw. in das Moldanubikum s. str. geschoben und endet an einer bogenförmigen Störung im Südwesten. Die als Mylonit-Gürtel ausgebildeten, zum Teplá-Barrandium hin einfallenden Scherzonen weisen eine große Abschiebungskomponente auf: wobei das Teplá-Barrandium ggü. dem Moldanubikum um einen Vertikalversatz von über 10 km abgesenkt ist (Bues et al. 1998, Zulauf et al. 2002). @de
narrower: West Bohemian Shear Zone
narrower: Central Bohemian Shear Zone
narrower: Hoher Bogen Shear Zone
references: https://data.geoscience.earth/ncl/geoera/ref/6358
references: https://data.geoscience.earth/ncl/geoera/ref/7273
references: https://data.geoscience.earth/ncl/geoera/ref/7377
references: https://data.geoscience.earth/ncl/geoera/ref/7320
definition: Comparable to the ship's bow of an icebreaker the southwestern bulge of Teplá-Barrandian Terrane, widespread in Czechia, protrudes into Bavarian territory east of Cham. The Gabbroamphibolite body of Neukirchen-Kdyně-Complex is thrusted into the Moldanubian s. str. along two principal polyphase shear zones, headed by an arched thrust front in the southwest. These thrust zone have been subject to dip-slip or oblique-slip normal movements, moving down the Teplá-Barrandian unit with respect to the Moldanubian unit for more than 10 km, forming mylonite belt, dipping steeply towards the Teplá-Barrandian unit (Bues et al. 1998, Zulauf et al. 2002).
in scheme: Tectonic Boundary Objects in Europe
narrower: West Bohemian Shear Zone (CZ)
narrower: Tachov Fault Zone
narrower: Mariánské Lázně Fault Zone
narrower: Litoměřice / Ohře Fault
narrower: Krušné hory Fault
notation: LfU-BY_1494
broader: 3: Bohemian Massif domain

Krušné hory Fault
type: Limit
type: Concept
created: 2021-08-23T08:09:47.499Z
creator: schmar
in scheme: Tectonic Boundary Objects in Europe
type: Fault
notation: LfU-BY_9923
type: https://data.geoscience.earth/ncl/geoera/geoconnect3d/category/9754
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11705
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11574
definition: The Eger Graben northern marginal rift fault (Krušné hory Fault) is regarded a normal fault, conjugate to the southern marginal rift fault. Formed during the Cenozoic in several (reactivation) phases and due to the uplift of Krušné hory mountains block in Pliocene/Pleistocene, after the rift formation, it features a present day residual throw of more than 700 m.
alternative label: Eger Graben Northern Marginal Rift Fault
preferred label: Egergraben Nordrand- Verwerfung @de
limit type: normalFault
broader: Teplá-Barrandian Terrane boundary

Hoher Bogen Shear Zone
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6358
type: Concept
created: 2021-01-25T14:23:19.746Z
preferred label: Hoher Bogen Scherzone @de
notation: DE-BY_1355
alternative label: HBSZ
definition: Bogenförmige Stirn des Neukirchen-Kdyně Komplex. Steil nach ± NE einfallende Störung, zunächst Auf-/Überschiebung, danach (Rückgleite-) Abschiebung, als Verbindung zwischen der rechtssinnigen Westböhmischen Scherzone [DE-BY_1353] und der linkssinnigen Zentralböhmischen Scherzone [DE-BY_1354]. @de
definition: Frontal arch of the Neukirchen-Kdyně Complex Boundary. Steeply ± NE dipping initially reverse (“on-thrust”) fault, then inverted to a normal (“back-slip”) fault, connecting dextral West Bohemian Shear Zone [DE-BY_1353] and sinistral Central Bohemian Shear Zone [DE-BY_1354].
narrower: Hoher Bogen lateral faults
references: https://data.geoscience.earth/ncl/geoera/ref/7273
references: https://data.geoscience.earth/ncl/geoera/ref/7274
references: https://data.geoscience.earth/ncl/geoera/ref/7351
references: https://data.geoscience.earth/ncl/geoera/ref/7320
sf touches: West Bohemian Shear Zone
sf touches: Central Bohemian Shear Zone
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1355
limit type: normalFault
broader: Teplá-Barrandian Terrane boundary

Hoher Bogen lateral faults
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.774Z
preferred label: Hoher Bogen Querstörungen @de
notation: DE-BY_1497
definition: NNW-SSE to NNE-SSW trending faults within Neukirchen-Kdyně-Complex.
references: https://data.geoscience.earth/ncl/geoera/ref/6358
references: https://data.geoscience.earth/ncl/geoera/ref/7351
references: https://data.geoscience.earth/ncl/geoera/ref/7320
sf touches: Hoher Bogen Shear Zone
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1497
broader: Hoher Bogen Shear Zone

Central Bohemian Shear Zone
limit type: https://data.geoscience.earth/ncl/geoera/geoconnect3d/category/57
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.691Z
preferred label: Zentralböhmische Scherzone @de
notation: DE-BY_1354
alternative label: CBSZ
alternative label: Klattauer Störung @de
definition: Undulate WSW-ENE trending sinistral shear zone forming the southeastern Boundary of the Gabbroamphibolite body of Neukirchen-Kdyně-Complex of the Teplá-Barrandian Zone.
definition: Gewellt WSW-ENE verlaufende linkssinnige Scherzone als südöstliche Begrenzung der Gabbroamphibolitmasse des Neukirchen-Kdyně-Komplex im Teplá-Barrandium. @de
narrower: CBSZ subsidiary faults
references: https://data.geoscience.earth/ncl/geoera/ref/6358
references: https://data.geoscience.earth/ncl/geoera/ref/7273
references: https://data.geoscience.earth/ncl/geoera/ref/7274
references: https://data.geoscience.earth/ncl/geoera/ref/7351
references: https://data.geoscience.earth/ncl/geoera/ref/7320
sf touches: Hoher Bogen Shear Zone
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1354
broader: Teplá-Barrandian Terrane boundary

CBSZ subsidiary faults
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6358
type: Concept
created: 2021-01-25T14:23:19.718Z
preferred label: CBSZ Nebenstörungen @de
notation: DE-BY_1496
definition: WSW-ENE verlaufende linkssinnige Blatt- oder Schrägabschiebungen subparallel zur Zentralböhmischen Scherzone [DE-BY_1354). @de
definition: WSW-ENE trending subsidiary sinistral strike-slip or oblique-slip faults subparallel to Central Bohemian Shear Zone [DE-BY_1354].
references: https://data.geoscience.earth/ncl/geoera/ref/7351
references: https://data.geoscience.earth/ncl/geoera/ref/7320
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1496
broader: Central Bohemian Shear Zone

Tachov Fault Zone
limit type: https://data.geoscience.earth/ncl/geoera/geoconnect3d/category/57
type: Limit
type: Concept
created: 2021-08-23T08:08:19.713Z
creator: schmar
in scheme: Tectonic Boundary Objects in Europe
type: Fault
narrower: Tachov Fault Zone subsidiary faults
notation: LfU-BY_9920
type: https://data.geoscience.earth/ncl/geoera/geoconnect3d/category/9754
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11855
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11579
preferred label: Böhmischer Pfahl @de
alternative label: Bohemian Quartz Lode
definition: Overall NNW–SSE trending Tachov Fault presumably runs for more than 120 km from Aš NW of Cheb to HBSZ [LfU-BY_1355]. In the southern part, Tachov Fault Zone (TFZ), a wide belt of prevailing mylonites, is a synonym for West Bohemia Shear Zone (WBSZ) [LfU-BY_1353], and associated with quartz lodes, thus also referred to as Bohemian Quartz Lode or Bohemian Pfahl. Here, the western boundary of TFZ consists of a set of (sub-)parallel zones of the Bohemian Quartz Lode between the eastern suture-type Tachov Fault s.str. and the western Nemanice-Rozvadov Fault, both steeply ENE dipping to vertical polyphase dextral oblique-slip normal faults (Zulauf et al. 2002). In its central and southern sections, Tachov Fault represents the western flank of Cheb-Domažlice Graben (aka Cheb Basin / Chebská pánev / Egerer Becken and Tachov Trough / Tachovská brázda / Tachauer Furche).
broader: Teplá-Barrandian Terrane boundary

Tachov Fault Zone subsidiary faults
limit type: strikeSlipFault
type: Limit
created: 2021-08-23T08:08:44.268Z
creator: schmar
type: Concept
in scheme: Tectonic Boundary Objects in Europe
type: Fault
notation: LfU-BY_9924
type: https://data.geoscience.earth/ncl/geoera/geoconnect3d/category/930
preferred label: TFZ Nebenstörungen @de
alternative label: Böhmischer Pfahl Störungen @de
definition: NNW-SSE to N-S trending subsidiary dextral strike-slip or oblique-slip faults subparallel to Tachov Fault Zone [LfU-BY_9920], partly manifested as quartz lodes and pegmatite veins.
scope note: The trends and geometries of Tachov Fault Zone subsidiary faults are represented schematically only.
broader: Tachov Fault Zone

Mariánské Lázně Fault Zone
limit type: obliqueSlipFault
type: Limit
type: Concept
created: 2021-08-23T08:09:09.725Z
creator: schmar
in scheme: Tectonic Boundary Objects in Europe
type: Fault
notation: LfU-BY_9921
type: https://data.geoscience.earth/ncl/geoera/geoconnect3d/category/9754
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11574
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11705
preferred label: Marienbader Störungszone @de
alternative label: MLZ
definition: About 150 km long, prevailing NNW-SSE trending, morphologically conspicuous, principal tectonic structure in western Bohemia. Limit of several distinctive geological units of the Bohemian Massif: Saxothuringian Zone in the NW, Moldanubian s. str. in the S and SW, Teplá-Barrandian Block in the E and truncating Eger Graben. In its S, eastern boundary of Cheb-Domažlice Graben (Tachovská brázda /Tachauer Furche). The merger, respectively cross-over, of Mariánské Lázně Fault Zone with N-S striking Počatky-Plesná Fault Zone at Nový Kostel north of the Eger Graben is recurrently prone to earthquake swarms with a hypocenter at about 10 km, inferred to be caused by channeled ascent of fluids along the fault plane in the crust.
broader: Teplá-Barrandian Terrane boundary

Litoměřice / Ohře Fault
limit type: obliqueSlipFault
type: Limit
creator: schmar
created: 2021-08-23T08:09:27.353Z
type: Concept
in scheme: Tectonic Boundary Objects in Europe
type: Fault
notation: LfU-BY_9922
type: https://data.geoscience.earth/ncl/geoera/geoconnect3d/category/9754
preferred label: Egergraben Südrand-Verwerfung @de
alternative label: Eger Graben Southern Marginal Rift Fault
definition: The southern marginal rift fault (Litoměřice / Ohře Fault) is the surface outcrop of the deep-seated Litoměřice Fault, interpreted as a Variscan suture between the Saxothuringian and Tepla-Barrandian/Moldanubian zones, reactivated in Cenozoic times due to Alpine orogeny. This North Bohemian Sher Zone (NBSZ) is considered the original forming structure of the entire rift, composed of wide zone of (sub-)parallel faults and en-echelon structures.
broader: Teplá-Barrandian Terrane boundary

West Bohemian Shear Zone
limit type: https://data.geoscience.earth/ncl/geoera/geoconnect3d/category/57
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.635Z
preferred label: Westböhmische Scherzone @de
notation: DE-BY_1353
alternative label: WBSZ
definition: Von der Mariánské Lázně Störung bzw. dem Bor Granit bis zur HBSZ [DE-BY_1355] verlaufende, N-S bis NNW-SSE streichende, rechtssinnige Scherzone als westliche Begrenzung der Gabbroamphibolitmasse des Neukirchen-Kdyně-Komplex im Teplá-Barrandium. Die Hauptbewegungsphasen umfassen die NE-wärts einfallende Abschiebung vor ca. 360 Ma und die dextrale Seiten- bzw. Schrägabschiebung vor ca. 340 Ma (Zulauf et al. 2002). @de
definition: Running from Mariánské Lázně Fault resp. Bor granite to HBSZ [DE-BY_1355], N-S to NNW-SSE trending oblique-slip normal shear zone (main kinematic phases: NE dipping normal fault roughly 360 Ma ago, dextral shearing approx. 340 Ma ago (Zulauf et al. 2002)) forming the western boundary zone of Neukirchen-Kdyně-Complex of the Teplá-Barrandian Zone.
narrower: WBSZ subsidiary faults
references: https://data.geoscience.earth/ncl/geoera/ref/6358
references: https://data.geoscience.earth/ncl/geoera/ref/7377
references: https://data.geoscience.earth/ncl/geoera/ref/7337
references: https://data.geoscience.earth/ncl/geoera/ref/7320
sf touches: Hoher Bogen Shear Zone
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1353
broader: Teplá-Barrandian Terrane boundary

WBSZ subsidiary faults
type: Fault
type: Limit
type: Concept
created: 2021-01-25T14:23:19.663Z
preferred label: WBSZ Nebenstörungen @de
notation: DE-BY_1495
definition: NNW-SSE bis NNE-SSW verlaufende, dextrale Blatt- oder Schrägabschiebungen subparallel zur oder in der Verlängerung der Westböhmischen Scherzone [DE-BY_1353), z.T. als Quarz- und Pegmatit-Gänge. @de
definition: NNW-SSE to NNE-SSW trending subsidiary dextral strike-slip or oblique-slip faults subparallel to or extending West Bohemian Shear Zone [DE-BY_1353], partly manifested as quartz and pegmatite veins.
references: https://data.geoscience.earth/ncl/geoera/ref/6358
references: https://data.geoscience.earth/ncl/geoera/ref/7337
references: https://data.geoscience.earth/ncl/geoera/ref/7351
references: https://data.geoscience.earth/ncl/geoera/ref/7320
sf touches: Hoher Bogen Shear Zone
sf touches: Hoher Bogen lateral faults
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1495
broader: West Bohemian Shear Zone
broader: West Bohemian Shear Zone (CZ)

West Bohemian Shear Zone (CZ)
limit type: https://data.geoscience.earth/ncl/geoera/geoconnect3d/category/57
type: Limit
created: 2021-08-23T08:02:09.435Z
creator: schmar
type: Concept
in scheme: Tectonic Boundary Objects in Europe
type: Fault
notation: LfU-BY_9953
alternative label: WBSZ
definition: N-S to NNW-SSE trending eastern strand of WBSZ s.l., aka Bohemian Pfahl, running subparallel Tachov Fault Zone [LfU-BY_9920]. Eastern part of the stepped normal oblique-slip shear zone, main kinematic phases: NE dipping normal fault roughly 360 Ma ago, dextral shearing approx. 340 Ma ago (Zulauf et al. 2002), forming a ductile normal faulting shear zone.
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7377
type: https://data.geoscience.earth/ncl/geoera/geoconnect3d/category/9756
narrower: WBSZ subsidiary faults
broader: Teplá-Barrandian Terrane boundary

1: Tectonic Boundary Objects in the central part of the North Alpine Molasse Basin and northward adjoining areas
has map: https://data.geus.dk/egdi/
narrower: Lower Bavaria - Upper Austria Molasse Basin fault domain
preferred label: Tektonische Grenzflächen im mittleren Teil des Nordalpinen Molassebeckens und nördlich angrenzender Gebiete @de
narrower: Lower Bavaria - Upper Austria Molasse Basin Eastern Margin Fault Systems
type: SpatialObject
type: Concept
top concept of: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
created: 2020-10-09T11:35:26.475Z
notation: HotLime_Case_Study_1
definition: Concepts of tectonic boundaries in the Central North Alpine Molasse Basin, in terms of fault traces in the Upper Jurassic carbonates hydrothermal reservoir and hydraulically connected northward adjoining realms of outcropping reservoir rocks of the Swabian and Franconian Alb. Synopsis of basinal blind faults, predominantly interpreted from seismic surveys of various vintage and resolution or derived from borehole correlation in shallower marginal areas, as well as mapped superficial faults in exposed areas. This inventory, prepared within the scope of HotLime project case study 1, comprises tectonic boundaries in Baden-Wuerttemberg [DE-BW] and Upper Austria [AT] as well.
definition: Konzepte tektonischer Grenzflächen im zentralen nordalpinen Molassebecken, bezogen auf die Schnittspuren in den oberjurassischen Karbonaten des hydrothermalen Reservoirs, sowie den zu Tage tretenden Reservoirgesteinen in nördlich angrenzenden Bereichen, der Schwäbisch-Fränkischen Alb. Zusammenstellung der überdeckten Störungen im Becken, basierend auf der Interpretation seismischer Erkundungen aus fünf Jahrzehnten und mit unterschiedlicher Auflösung, oder abgeleitet aus Bohrloch-Korrelationen in seichteren Randbereichen, sowie kartierten Störungen im Ausstrichbereich. Dieses Inventar wurde im Rahmen des Projekts HotLime, Pilotgebiet 1, erstellt und umfasst auch tektonische Grenzflächen in Baden-Württemberg [DE-BW] und Oberösterreich [AT]. @de
narrower: Central Foreland Molasse Basin fault domain
references: https://data.geoscience.earth/ncl/geoera/ref/4097
narrower: Foreland Molasse Southern Margin Faults
narrower: Molasse Basin Northern Margin Fault System
narrower: Swabian-Franconian Alb fault domain
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
type: Fault
type: Limit
broader: Tectonic Boundaries in Bavaria

Lower Bavaria - Upper Austria Molasse Basin fault domain
in scheme: GC3D limits
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.946Z
scope note: All faults of the Lower Bavaria - Upper Austria Molasse Basin are blind faults 3D modelled based on evidence of seismic and gravity surveys and deep drillings. The concepts refer to the fault traces on the top of Upper Jurassic carbonate sequence as one of the principal reflectors in seismic surveys. Tectonic boundaries featuring throws of less than approximately 10 m, likewise soft links between faults, like relay ramps or horsetail splays, commonly are subseismic in legacy surveys and detectable only in novel 3D-seismics as carried out in few focus areas. The inventory, thus, cannot be complete with respect to these features, reflects the state of knowledge as of 2020 and is subject to future amendments.
scope note: Alle Störungen im niederbayerisch-oberösterreichischen Molassebecken sind überdeckte Störungen, die im 3D-Modell aus seismischen und Schwere-Messungen sowie Bohrungsbelegen abgeleitet wurden. Die Konzepte der tiefliegenden Störungen beziehen sich auf die im 3D-Modell ermittelten Schnittspuren an der Oberfläche der Weißjura Karbonat-Abfolge. Tektonische Grenzflächen mit Sprunghöhen von weniger als ca. 10 m, gleichermaßen Übergänge zwischen Störungen wie Relais Rampen (relay ramps) oder Auffiederungen (horsetail splays), sind in älteren seismischen Erkundungen gemeinhin nicht erkennbar (subseismisch) und nur in moderner, in wenigen Schwerpunktbereichen durchgeführter 3D-Seismik identifizierbar. Dementsprechend bleibt die Zusammenstellung, Stand 2020, im Hinblick auf solche Phänomene unvollständig und ist Gegenstand künftiger Fortschreibungen. @de
notation: DE-BY_1222
preferred label: Niederbayerisch-oberösterreichisches Molassebecken Störungs-Domäne @de
definition: The Lower Bavaria - Upper Austria Molasse Basin fault domain, overlapping the Austrian-German border, takes up the space in-between the southwestern scarp of the buried Landshut-Neuötting crystalline rise or Central Swell Zone to the southwest, the Franconian Alb to the northwest, the outcropping crystalline rock suites of the Bohemian Massif to the north and northeast, and the Alpine Thrust front to the south. It is characterized by syn- and antithetic normal faults running subparallel to the counterfort of the Alpine thrust formed by the Bohemian Massif, southwards increasingly crossed by faults subparallel to the Alpine Thrust Front. The roughly NW-SE trending (Variscan strike) reactivated Permo-Carboniferous lineaments subdivide specifically the Lower Bavaria Molasse Basin into sub-basins and troughs. All faults within the basin are blind faults, active until Badenian of mid-Miocene at the latest, solely evidenced by seismic surveys and drillings.
definition: Das niederbayerisch-oberösterreichische Molassebecken wird begrenzt durch den südwestlichen Abbruch des überdeckten Kristallins im Landshut-Neuöttinger Hoch bzw. der Zentralen Schwellenzone im Südwesten, die Fränkische Alb im Nordwesten, die anstehenden Kristallingesteine der Böhmischen Masse in Norden und Nordosten sowie die Alpine Überschiebungsfront im Süden. Für dieses Teilbecken sind syn- und antithetische Abschiebungen subparallel zur Böhmischen Masse, dem Widerlager des Alpenschubs, kennzeichnend, die nach Süden hin zunehmend von Alpenfront-parallelen Störungen überlagert werden. Die grob NW-SE (herzynisch) verlaufenden, reaktivierten permokarbonischen Lineamente untergliedern insbesondere das Niederbayerische Molassebecken in Teilbecken und Tröge. Alle Störungen innerhalb des Beckens sind überdeckte Störungen, die bis höchstens ins Badenium (mittleres Miozän) aktiv waren und nur durch seismische Untersuchungen und Bohrungen nachgewiesen sind. @de
narrower: Landshut-Neuötting Step Fault
narrower: Hohenthann-Wolkersdorf Fault
narrower: Rottenburg-Aham Fault
narrower: Abensberg-Rottenburg Fault
narrower: Dingolfing Fault
narrower: Schierling Fault
narrower: Haunersdorf-Perbing Fault
narrower: Jägerndorf-Holzhamm Fault
narrower: Jägerndorf-Schwarzenstein Fault
narrower: Holzhamm-Lanzing Fault
narrower: Hirschbach Fault
narrower: Wurmannsquick-Zeilarn Fault
narrower: Gumpersdorf-Schellenberg Fault
narrower: Stubenberg-Malching Fault
narrower: Rotthalmünster Fault
narrower: Geinberg-Simbach Fault
narrower: Altheim Fault
narrower: Nonsbach Fault
narrower: Aspach Fault
narrower: Fornach Fault
narrower: Steindlberg Fault
narrower: Mauerkirchen Fault
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
narrower: Regensburg-Straubing Trough SW Fringe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1222
broader: 1: Tectonic Boundary Objects in the central part of the North Alpine Molasse Basin and northward adjoining areas

Haunersdorf-Perbing Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:34.636Z
notation: DE-BY_1228
preferred label: Haunersdorf-Perbing Störung @de
definition: W-E striking, approx. 85° S dipping synthetic normal fault running south of and subparallel to Vils river SE of Landau / Isar.
definition: W-E streichende, ca. 85° nach S einfallende synthetische Abschiebung südlich und subparallel zur Vils SE von Landau / Isar. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4082
sf touches: Pfarrkirchen Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1228
limit type: normalFault
broader: Lower Bavaria - Upper Austria Molasse Basin fault domain

Landshut-Neuötting Step Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.975Z
notation: DE-BY_700
alternative label: Landshut-Neuötting fault scarp
alternative label: Landshut-Neuöttinger Abbruch @de
preferred label: Landshut-Neuötting Abbruch @de
definition: NW-SE trending step fault system of steeply SW dipping to vertical normal faults of hercynian (variscan) origin and Miocene reactivation. Southwestern boundary of Landshut-Neuötting crystalline rise, a tilted, gently northeast sloping fault-block featuring an only thin and discontinuous Mesozoic overburden resting upon the basement rocks.
definition: NW-SE (herzynisch) streichender, während der saxonischen Bruchtektonik angelegter, im Miozän reaktivierter Staffelbruch steil nach SW einfallender, bereichsweise vertikaler Abschiebungen. Südwestliche Begrenzung des Landshut-Neuöttinger Hochs, einer nach Nordosten hin flach abtauchenden Kippscholle, in deren Hochgebieten die mesozoische Auflage nur geringmächtig ausgebildet ist und bereichsweise fehlt. @de
narrower: Landshut-Neuötting Main Scarp
narrower: Landshut-Neuötting Fault Scarp 2
narrower: Landshut-Neuötting Fault Scarp 3
narrower: Grasset-Wechselberg Fault
narrower: Mehring-Seeham Fault
narrower: Eggelsbach Fault
narrower: Perach Fault
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/789
narrower: Handenberg Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
related: Landshut-Neuötting Fault System
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11680
notation: LfU-BY_700
limit type: normalFault
broader: Lower Bavaria - Upper Austria Molasse Basin fault domain

Landshut-Neuötting Fault Scarp 2
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:34.131Z
notation: DE-BY_702
preferred label: Landshut-Neuötting Abbruchstufe 2 @de
definition: Central scarp of Landshut-Neuötting Step Fault [DE-BY_700]. Undulate overall NW-SE trending, averaged approx. 70° SW dipping synthetic normal fault, running from Rudelzhausen to the Austrian Border near Burghausen and beyond.
definition: Mittlere Bruchstufe des Landshut-Neuötting Abbruchs [DE-BY_700], die sich von Rudelzhausen bis zur österreichischen Grenze bei Burghausen und darüber hinaus erstreckt. Gewellt, insgesamt NW-SE verlaufende, im Mittel ca. 70° nach SW einfallende synthetische Abschiebung. @de
narrower: Münchsdorf Fault
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/7269
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11681
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11888
notation: LfU-BY_702
limit type: normalFault
broader: Landshut-Neuötting Step Fault

Münchsdorf Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:34.161Z
notation: DE-BY_1223
preferred label: Münchsdorf Störung @de
definition: Subordinate scarp of Landshut-Neuötting Step Fault [DE-BY_700] close and parallel to Landshut-Neuötting Fault Scarp 2 [DE-BY_702]. Probably due to a mostly subseismic throw traceable in a short segment only.
definition: Untergeordnete Bruchstufe des Landshut-Neuötting Abbruchs [DE-BY_700] parallel zur Abbruchstufe 2 [DE-BY_702]. Wahrscheinlich bedingt durch einen überwiegend subseismischen Versatz nur in einem kurzen Abschnitt nachweisbar. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1223
limit type: normalFault
broader: Landshut-Neuötting Fault Scarp 2

Landshut-Neuötting Main Scarp
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:34.003Z
notation: DE-BY_701
alternative label: Landshut-Neuötting Abbruchstufe 1 @de
preferred label: Landshut-Neuötting Hauptabbruch @de
definition: Nordöstliche und größte Bruchstufe des Landshut-Neuötting Abbruchs [DE-BY_700], die sich von Volkenschwand bis zur österreichischen Grenze bei Burghausen und darüber hinaus erstreckt. Gewellt, insgesamt NW-SE verlaufende, im Mittel ca. 85° nach SW einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/7269
definition: Northeastern and principal scarp of Landshut-Neuötting Step Fault [DE-BY_700]. Undulate overall NW-SE trending, on average approx. 85° SW dipping synthetic normal fault, running from Volkenschwand to the Austrian Border near Burghausen and, as Handenberg Fault [AT_10655] further into Austrian territory.
narrower: Furth Fault
narrower: Landshut Fault
narrower: Volkenschwand Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11888
notation: LfU-BY_701
limit type: normalFault
broader: Landshut-Neuötting Step Fault

Volkenschwand Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:34.099Z
notation: DE-BY_706
preferred label: Volkenschwand Störung @de
definition: N-S striking, steeply (85°-60°) W dipping normal fault. Lateral fault of Landshut-Neuötting Main Scarp, western boundary of a horst-like structure, confined by Furth Fault [DE-BY_705] to the east, lacking Upper Jurassic deposits on top of the crystalline basement.
definition: N-S streichende steil (85°-60°) nach W einfallende Abschiebung. Querstörung zum Landshut-Neuötting Hauptabbruch. Bildet mit der Furth Störung [DE-BY_705] eine Horst-artige Struktur, in der Oberjura als Grundgebirgsüberdeckung fehlt. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4082
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_706
limit type: normalFault
broader: Landshut-Neuötting Main Scarp

Furth Fault
type: Limit
type: Fault
type: Concept
created: 2020-10-09T11:35:34.068Z
notation: DE-BY_705
preferred label: Furth Störung @de
definition: N-S striking, steeply (85°-60°) E dipping normal fault. Lateral fault of Landshut-Neuötting Main Scarp, eastern boundary of a horst-like structure, confined by Volkenschwand Fault [DE-BY_706] to the west, lacking Upper Jurassic deposits on top of the crystalline basement.
definition: N-S streichende, steil (85°-60°) nach E einfallende Abschiebung. Querstörung zum Landshut-Neuötting Hauptabbruch. Bildet mit der Volkenschwand Störung [DE-BY_706] eine Horst-artige Struktur, in der Oberjura als Grundgebirgsüberdeckung fehlt. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4082
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_705
limit type: normalFault
broader: Landshut-Neuötting Main Scarp

Landshut Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:34.035Z
notation: DE-BY_704
preferred label: Landshut Störung @de
definition: N-S striking, vertical to subvertical normal fault. Lateral fault of Landshut-Neuötting Main Scarp.
definition: N-S streichende, ± senkrecht stehende Abschiebung. Querstörung zum Landshut-Neuötting Hauptabbruch. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4082
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_704
limit type: normalFault
broader: Landshut-Neuötting Main Scarp

Perach Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:34.327Z
notation: DE-BY_862
preferred label: Perach Störung @de
definition: NW-SE striking, vertical to steeply SW dipping reverse fault northeastward subparallel to Landshut-Neuötting Main Scarp [DE-BY_701] north of Burghausen.
definition: NW-SE verlaufende, senkrecht stehende bis steil nach SW fallende Aufschiebung nordöstlich subparallel zum Landshut-Neuötting Hauptabbruch [DE-BY_701] nördlich von Burghausen. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4082
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_862
limit type: reverseFault
broader: Landshut-Neuötting Step Fault

Landshut-Neuötting Fault Scarp 3
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:34.189Z
notation: DE-BY_703
preferred label: Landshut-Neuötting Abbruchstufe 3 @de
definition: Southwestern scarp of Landshut-Neuötting Step Fault [DE-BY_700] running from Tattendorf south of Vilsbiburg to Altötting. Undulate overall NW-SE trending, averaged approx. 70° SW dipping synthetic normal fault.
definition: Südwestliche Bruchstufe des Landshut-Neuötting Abbruchs [DE-BY_700], die sich von Altfraunhofen S Landshut bis zur österreichischen Grenze und darüber hinaus erstreckt. Gewellt, insgesamt NW-SE verlaufende, im Mittel ca. 70° nach SW einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/7269
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11689
notation: LfU-BY_703
limit type: normalFault
broader: Landshut-Neuötting Step Fault

Rotthalmünster Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:34.861Z
notation: DE-BY_1236
preferred label: Rotthalmünster Störung @de
definition: W-E striking, approx. 85° S dipping synthetic normal fault running from Kirn to Birnbach-Füssing Step Fault [DE-BY_930].
definition: Von Kirn bis zum Birnbach-Füssinger Abbruch [DE-BY_930] verlaufende, W-E streichende, ca. 85° nach S einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4082
references: https://data.geoscience.earth/ncl/geoera/ref/4078
sf touches: Birnbach-Füssing Step Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1236
limit type: normalFault
broader: Lower Bavaria - Upper Austria Molasse Basin fault domain

Stubenberg-Malching Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:34.833Z
notation: DE-BY_1235
preferred label: Stubenberg-Malching Störung @de
definition: W-E striking, approx. 70° S dipping synthetic normal fault.
definition: W-E streichende, ca. 70° nach S einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4082
references: https://data.geoscience.earth/ncl/geoera/ref/4078
sf touches: Pfarrkirchen Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1235
limit type: normalFault
broader: Lower Bavaria - Upper Austria Molasse Basin fault domain

Gumpersdorf-Schellenberg Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:34.805Z
notation: DE-BY_1234
preferred label: Gumpersdorf-Schellenberg Störung @de
definition: WSW-ENE striking, approx. 85° NNW dipping antithetic normal fault north of Simbach am Inn
definition: WSW-ENE streichende, ca. 85° nach NNW einfallende antithetische Abschiebung nördlich von Simbach am Inn. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4082
sf touches: Pfarrkirchen Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1234
limit type: normalFault
broader: Lower Bavaria - Upper Austria Molasse Basin fault domain

Schierling Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:34.467Z
notation: DE-BY_752
preferred label: Schierling Störung @de
definition: Die WNW-ESE streichende, im Mittel ca. 70° nach SSW einfallende synthetische Abschiebung verläuft im Molasseuntergrund von Hausen via Schierling bis Landau/Isar. @de
narrower: Landau Fault
type: SpatialObject
definition: The WNW-ESE striking synthetic normal fault runs at the Molasse subsurface from Hausen via Schierling to Landau/Isar. At average, it dips towards approx. 70° SSW.
notation: AT-10447
alternative label: Schierling-Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/753
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/4151
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11683
notation: LfU-BY_752
limit type: normalFault
broader: Lower Bavaria - Upper Austria Molasse Basin fault domain

Landau Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:34.495Z
notation: DE-BY_1226
preferred label: Landau Störung @de
definition: SSW-NNE striking, approx. 85° ESE dipping to vertical synthetic normal fault.
definition: SSW-NNE streichende, ca. 85° nach ESE einfallende bis saigere synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4082
sf touches: Schierling Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1226
limit type: normalFault
broader: Schierling Fault

Wurmannsquick-Zeilarn Fault
type: Limit
type: Fault
type: Concept
created: 2020-10-09T11:35:34.777Z
notation: DE-BY_1233
preferred label: Wurmannsquick-Zeilarn Störung @de
definition: NW-SE trending, approx. 85° NE dipping reverse fault south of Eggenfelden.
definition: NW-SE verlaufende, ca. 85° nach NE einfallende Aufschiebung südlich Eggenfelden. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4082
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1233
limit type: reverseFault
broader: Lower Bavaria - Upper Austria Molasse Basin fault domain

Hirschbach Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:34.749Z
notation: DE-BY_1232
preferred label: Hirschbach Störung @de
definition: Northward arcuate W-E trending, approx. 70° N dipping antithetic normal fault running from Pfarrkirchen to Grottham north of Bad Birnbach.
definition: Nordwärts gebogen W-E verlaufende, ca. 70° nach N einfallende antithetische Abschiebung zwischen Pfarrkirchen und Grottham nördlich Bad Birnbach. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4082
references: https://data.geoscience.earth/ncl/geoera/ref/4078
sf touches: Pfarrkirchen Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1232
limit type: normalFault
broader: Lower Bavaria - Upper Austria Molasse Basin fault domain

Dingolfing Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:34.439Z
notation: DE-BY_783
preferred label: Dingolfing Störung @de
definition: Running from Herrngiersdorf to Marklkofen, NW-SE trending, averaged approx. 70° ± SW dipping normal fault.
definition: NW-SE verlaufende, im Mittel ca. 70° nach ± SW einfallende Abschiebung zwischen Herrngiersdorf und Marklkofen. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4151
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_783
limit type: normalFault
broader: Lower Bavaria - Upper Austria Molasse Basin fault domain

Abensberg-Rottenburg Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:34.411Z
notation: DE-BY_812
preferred label: Abensberg-Rottenburg Störung @de
definition: Northeastward arcuate NW-SE trending, steeply (85°-60°) SW dipping synthetic normal fault.
definition: Nordostwärts gebogen NW-SE verlaufene, steil (85°-60°) nach SW einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4082
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_812
limit type: normalFault
broader: Lower Bavaria - Upper Austria Molasse Basin fault domain

Holzhamm-Lanzing Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:34.721Z
notation: DE-BY_1231
preferred label: Holzhamm-Lanzing Störung @de
definition: WSW-ENE striking, approx. 85° NNW dipping antithetic normal fault north of Pfarrkirchen.
definition: WSW-ENE streichende, ca. 85° nach NNW einfallende antithetische Abschiebung nördlich von Pfarrkirchen. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4082
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1231
limit type: normalFault
broader: Lower Bavaria - Upper Austria Molasse Basin fault domain

Rottenburg-Aham Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:34.383Z
notation: DE-BY_784
preferred label: Rottenburg-Aham Störung @de
definition: WNW-ESE to NW-SE trending, predominantly vertical normal fault.
definition: WNW-ESE bis NW-SE verlaufende, überwiegend senkrecht stehende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4082
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_784
limit type: normalFault
broader: Lower Bavaria - Upper Austria Molasse Basin fault domain

Jägerndorf-Schwarzenstein Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:34.693Z
notation: DE-BY_1230
preferred label: Jägerndorf-Schwarzenstein Störung @de
definition: NW-SE striking, approx. 85° NE dipping antithetic normal fault between Arnstorf and Pfarrkirchen.
definition: NW-SE streichende, ca. 85° nach NE einfallende antithetische Abschiebung zwischen Arnstorf und Pfarrkirchen. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4082
sf touches: Jägerndorf-Holzhamm Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1230
limit type: normalFault
broader: Lower Bavaria - Upper Austria Molasse Basin fault domain

Hohenthann-Wolkersdorf Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:34.355Z
notation: DE-BY_786
preferred label: Hohenthann-Wolkersdorf Störung @de
definition: NW-SE trending steeply SW dipping to vertical normal fault.
definition: NW-SE (herzynisch) verlaufende, steil nach SW einfallende bis vertikale Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4082
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_786
limit type: normalFault
broader: Lower Bavaria - Upper Austria Molasse Basin fault domain

Jägerndorf-Holzhamm Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:34.665Z
notation: DE-BY_1229
preferred label: Jägerndorf-Holzhamm Störung @de
definition: N-S striking, approx. 80° E dipping antithetic normal fault between Arnstorf and Pfarrkirchen.
definition: N-S streichende, ca. 80° nach E einfallende antithetische Abschiebung zwischen Arnstorf und Pfarrkirchen. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4082
references: https://data.geoscience.earth/ncl/geoera/ref/4078
sf touches: Jägerndorf-Schwarzenstein Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1229
limit type: normalFault
broader: Lower Bavaria - Upper Austria Molasse Basin fault domain

Regensburg-Straubing Trough SW Fringe
type: Fault
type: Limit
definition: Linear array of roughly NW-SE trending, steeply ± NE dipping normal faults, southwestern limit of Regensburg-Straubing Trough.
narrower: Oberschneiding Transverse Fault
narrower: Pfarrkirchen Fault
type: Concept
created: 2020-10-29T12:33:52.116Z
type: SpatialObject
preferred label: Regensburg-Straubinger Senke SW Rand @de
notation: DE-BY_1344
definition: Abfolge von etwa NW-SE verlaufenden, steil nach ± NE einfallender Abschiebungen die den südwestlichen Rand der Regensburg-Straubinger Senke bilden. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4152
references: https://data.geoscience.earth/ncl/geoera/ref/4082
narrower: Köfering Fault
narrower: Hagelstadt-Oberschneiding Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1344
limit type: normalFault
broader: Lower Bavaria - Upper Austria Molasse Basin fault domain

Oberschneiding Transverse Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:34.552Z
notation: DE-BY_923
preferred label: Oberschneiding Querstörung @de
definition: WSW-ENE striking, approx. 85° NNW dipping to vertical antithetic normal fault linking Hagelstadt-Oberschneiding Fault [DE-BY_931] and Pfarrkirchen Fault [DE-BY_763].
definition: WSW-ENE streichende, ca. 85° nach NNW einfallende bis saigere antithetische Abschiebung als Verbindung von Hagelstadt-Oberschneiding Störung [DE-BY_931] and Pfarrkirchen Störung [DE-BY_763]. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4082
sf touches: Hagelstadt-Oberschneiding Fault
sf touches: Pfarrkirchen Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11684
notation: LfU-BY_923
limit type: normalFault
broader: Regensburg-Straubing Trough SW Fringe

Köfering Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:35.140Z
notation: DE-BY_928
preferred label: Köfering Störung @de
definition: WNW-ESE striking, approx. 70° NNE dipping normal fault running from Hohengebraching to Moosham.
definition: WNW-ESE streichende, ca. 70° nach NNE einfallende Abschiebung zwischen Hohengebraching und Moosham. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4151
references: https://data.geoscience.earth/ncl/geoera/ref/4082
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11684
notation: LfU-BY_928
limit type: normalFault
broader: Regensburg-Straubing Trough SW Fringe

Hagelstadt-Oberschneiding Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:34.524Z
notation: DE-BY_931
preferred label: Hagelstadt-Oberschneiding Störung @de
definition: NW-SE striking, approx. 70° NE dipping antithetic normal fault running from Hagelstadt to Oberschneiding. Offset northeastwards by Oberschneiding Transverse Fault [DE-BY_923] it continues to Simbach as Pfarrkirchen Fault [DE-BY_ 763] and further into Austrian territory.
definition: NW-SE streichende, ca. 70° nach NE einfallende synthetische Abschiebung zwischen Hagelstadt und Oberschneiding. Nordostwärts versetzt durch die Oberschneiding Querstörung [DE-BY_923], setzt sie sich als Pfarrkirchen Störung [DE-BY_763] nach Simbach und weiter nach Österreich fort. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4151
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4082
sf touches: Oberschneiding Transverse Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11684
notation: LfU-BY_931
limit type: normalFault
broader: Regensburg-Straubing Trough SW Fringe

Swabian-Franconian Alb fault domain
in scheme: GC3D limits
type: Fault
type: Limit
narrower: Krachenhausen-Dornau Fault
narrower: Krachenhausen-Holzheim Fault
narrower: Sandbreite Fault
narrower: Schlossberg Fault
narrower: Rohrbach Fault
narrower: Mühltal Fault
narrower: Oberbügl-Michelsberg Fault
narrower: Mitterbügl Cross Fault
narrower: Grünschlag-Neuhof Fault
narrower: Parsberg Fault
narrower: Maierleite-Breitenbrunn Fault
narrower: Riedenburg Fault
narrower: Lautersee Fault
narrower: Hattenhausen Fault
narrower: Thannhausen Fault
type: SpatialObject
scope note: In the Swabian-Franconian Alb, evidencing of tectonic boundaries is aggravated by small scale facies changes in the carbonate rocks, including a massive facies, which does not allow contouring of stratification. The concepts of tectonic boundaries in the Swabian-Franconian Alb are thus based on extrapolations on strike of short segments of mapped faults and/or derived from offsets, mismatches or narrowing intervals of contour lines, inferred from borehole correlation or the survey of lineaments. Except for the direct observation these methods are rather imprecise with respect to the dip angle, which, hence, have to be considered a rough estimate.
scope note: In der Schwäbisch-Fränkischen Alb wird der Nachweis tektonischer Grenzflächen durch rasche Fazieswechsel der Karbonatgesteine, darunter Massenfazies, die keine Konstruktion von Streichlinien erlaubt, erschwert. Die Konzepte tektonischer Grenzlinien der Schwäbisch-Fränkischen Alb basieren daher auf der Extrapolation kurzer Abschnitte kartierter Störungen im Streichen und/oder sind aus dem Versatz oder dem Zusammenlaufen von Streichlinien abgeleitet, oder beruhen auf Bohrloch-Korrelationen. Genaue Einfallswinkel der Störungen lassen sich daraus nur selten Ableiten; diese Angaben sind daher nur als grobe Schätzung zu betrachten. @de
definition: The Swabian-Franconian Alb is made up of Upper Jurassic carbonate rocks forming the uppermost cuesta of the South German Scarpland, the Southern Cuesta Terrain. In its major part, the elongated, SW-NE trending ridge overlapping the territories of Baden-Württemberg and Bavaria forms a gently SE dipping platform submerging underneath the Tertiary sedimentary sequence of the Molasse Basin. In its east, except for the faults and flexures relatable to the Schwarzwald-Bayerwald Line [DE-BY_1255] no prevailing tectonic structures are conspicuous. The predominant strike directions of micro-tectonics SSW-NNE (Rhenish) and SE-NW (Variscan / Hercynian) are evidenced by the fault network in few areas only, however, in the west, are manifested in local graben structures. The most striking structural feature of Swabian-Franconian Alb is atectonic: the almost circular crater rim of the 14.6 Ma old Ries asteroid impact.
definition: Die Schwäbisch-Fränkische Alb wird von oberjurassischen Karbonatgesteinen aufgebaut, die die oberste Schichtstufe des Süddeutschen Schichtstufenlands, das Südliche Schichtstufenland bilden. Der SW-NE verlaufende, langgesteckte Höhenzug der Schwäbischen und südlichen Fränkischen Alb, der Gebiete in Baden-Württemberg und Bayern einnimmt, bildet grob betrachtet eine schräggestellte, nach leicht SE einfallende Gesteinsplatte, die nach Süden hin unter die Tertiärablagerungen des Molassebeckens abtaucht. Mit Ausnahme der Störungen und Flexuren die der Schwarzwald-Bayerwald Linie [DE-BY_1255] zugeschrieben werden, sind im Osten (Fränkische Alb) keine übergeordneten tektonischen Strukturen erkennbar. Die vorherrschenden Kluftrichtungen, rheinisch (SSW-NNE) und herzynisch (NW-SE), zeigen sich nur bereichsweise in Störungsnetzwerk, manifestieren sich aber im Westen (Schwäbische Alb) in lokalen Grabenstrukturen. Das auffälligste Strukturelement der Schwäbisch-Fränkischen Alb ist atektonisch: der fast kreisrunde Kraterrand des Ries Asteroideneinschlags vor 14,6 Mio. Jahren. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6360
references: https://data.geoscience.earth/ncl/geoera/ref/6393
narrower: Erlinghofen Fault
narrower: Euerwang Fault
narrower: Frauenleite Fault
narrower: Schellenburg Horsts Scarps
narrower: Hagenau Fault
narrower: Spindeltal-Gammersfeld Fault
narrower: [geola_002]
narrower: Eger Valley Line 2
narrower: Eger Valley Line 3
narrower: Ipf North-South Fault
narrower: [geola_008]
narrower: Frieding Fault
narrower: [geola_011]
narrower: [geola_012]
narrower: Albstadt Shear Zone
narrower: Filstal Graben
narrower: Südschwarzwald-Dinkelberg-Hegau Region Faults
narrower: Freiburg-Bonndorf-Lake Constance Fault Zone
narrower: Swabian Lineament
narrower: Eger Valley Line 1
narrower: [geola_009]
narrower: Lauchert Graben
narrower: Mindelsee Fault
references: https://data.geoscience.earth/ncl/geoera/ref/6372
references: https://data.geoscience.earth/ncl/geoera/ref/7269
narrower: Hohenfels-Machtelwies Fault
narrower: Unterödenhart Fault
narrower: Vils Valley train of faults
preferred label: Schwäbisch-Fränkische Alb Störungs Domäne @de
narrower: Ries Crater Rim
narrower: Schafshill-Neuenhizenhausen Fault
type: Concept
created: 2020-10-09T11:35:36.120Z
notation: DE-BY_1253
narrower: Mödingen Fault
narrower: Schwarzwald-Bayerwald Line
narrower: Ursheim Fault
narrower: Judenbuck-Pappenheim Fault
narrower: Lichtenberg Step Fault
narrower: Preith-Walting Lineament
narrower: Kaldorf-Tafelmühle Fault
narrower: Fuchsberg Fault
narrower: Konstein Fault
narrower: Eibichel-Treidelheim Fault
narrower: Ammerfeld-Rohrbach Fault
narrower: Frauenholz-Hainberg Fault
narrower: Hainberg-Gietlhausen Fault
narrower: Bergen Fault
narrower: Pfaffengrund Fault
narrower: Bittenbrunn-Sehensand Fault
narrower: Lenting-Hepberg Fault
narrower: Hepberg Cross Fault
narrower: Kösching-Bettbrunn Fault
narrower: Demling-Vohburg Fault

[geola_012]
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6382
created: 2020-11-23T14:50:43.823Z
definition: WSW-ENE streichende, nach SSE einfallende Abschiebung mit unbekanntem Einfallswinkel. @de
type: Concept
definition: WSW-ENE striking normal fault, dipping SSE with unknown angle
notation: geola_012
notation: DE-BW_208
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Swabian-Franconian Alb fault domain

Freiburg-Bonndorf-Lake Constance Fault Zone
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/7675
definition: In der Freiburg-Bonndorf-Bodensee Störungszone, als Nordteil der Südschwarzwald-Dinkelberg-Hegau Störungs-Region, treten NW-SE streichende Elemente in den Vordergrund. Wegen des Höhenversatzes werden die Strukturen meist als tektonische Gräben und Horste dargestellt, doch zeigen Harnischflächen und Herdflächenlösungen rezenter Erdbeben rechtslaterale (NW-SE Brüche) bzw. linkslaterale (SSW-NNE Brüche) Bewegungen. Die vertikalen Sprunghöhen sind diesen Horizontalbewegungen offenbar nachgeordnet. @de
preferred label: Freiburg-Bonndorf-Bodensee Störungszone @de
references: https://data.geoscience.earth/ncl/geoera/ref/6359
narrower: Freiburg-Bonndorf-Lake Constance Fault 2
narrower: Bonndorf Fault Zone
narrower: Freiburg-Bonndorf-Lake Constance Fault 1
type: Concept
definition: Within the Freiburg-Bonndorf-Lake Constance Fault Zone, as the northern part of the Southern Black Forest-Dinkelberg-Hegau Fault Domain, NW-SE trending features prevail. Due to their significant vertical throw the tectonic boundaries mostly are assigned to horst and graben structures, however, slickenside surfaces and hypocenter retracing of recent earthquakes show dextral (for NW-SE faults) and sinistral (for SSW-NNE faults) movements, obviously superordinate to the vertical throw.
narrower: Freiburg-Bonndorf-Lake Constance Fault 3
created: 2020-11-23T14:50:45.050Z
notation: DE-BW_913
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Swabian-Franconian Alb fault domain

Freiburg-Bonndorf-Lake Constance Fault 1
type: Fault
type: Limit
notation: geola_064
type: Concept
definition: NW-SE streichende, nach SW einfallende Abschiebung mit unbekanntem Einfallswinkel. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6382
created: 2020-11-23T14:50:45.361Z
preferred label: Freiburg-Bonndorf-Bodensee Störung 1 @de
notation: DE-BW_270
definition: NW-SE striking normal fault, dipping SW with unknown angle
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Freiburg-Bonndorf-Lake Constance Fault Zone

Bonndorf Fault Zone
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/7675
preferred label: Bonndorfer Störungszone @de
narrower: Bonndorf Zone Fault 6
type: Concept
narrower: Bonndorf Zone Fault 1
narrower: Bonndorf Zone Fault 2
notation: DE-BW_914
narrower: Bonndorf Zone Fault 3
narrower: Bonndorf Zone Fault 4
created: 2020-11-23T14:50:45.079Z
narrower: Bonndorf Zone Fault 5
definition: Predominantly NW-SE to WNW-ESE striking dextral strike-slip faults with a subordinate vertical movement (oblique slip).
definition: Überwiegend NW-SE bis WNW-ESE verlaufende, rechtssinnige Blattverschiebungen mit untergeordnetem vertikalen Versatz. @de
narrower: Bonndorf Zone Fault 7
narrower: Bonndorf Zone Fault 8
narrower: Bonndorf Zone Fault 9
references: https://data.geoscience.earth/ncl/geoera/ref/6359
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Freiburg-Bonndorf-Lake Constance Fault Zone

Bonndorf Zone Fault 9
type: Fault
type: Limit
definition: WNW-ESE streichende Blattverschiebung; NW-SE bis NNW-SSE streichende Abschnitte als Abschiebung Richtung NNE mit unbekanntem Einfallswinkel ausgeprägt. @de
definition: WNW-ESE trending strike-slip fault; NW-SE to NNW-SSE striking parts as normal faults dipping NNE with unknown angle
notation: DE-BW_269
notation: geola_063
references: https://data.geoscience.earth/ncl/geoera/ref/6382
type: Concept
preferred label: Bonndorfer Störungszone Verwerfung 9 @de
created: 2020-11-23T14:50:45.333Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Bonndorf Fault Zone

Bonndorf Zone Fault 2
type: Fault
type: Limit
definition: NW-SE striking strike-slip fault
type: Concept
definition: NW-SE streichende Blattverschiebung. @de
created: 2020-11-23T14:50:45.135Z
notation: geola_056
preferred label: Bonndorfer Störungszone Verwerfung 2 @de
notation: DE-BW_262
references: https://data.geoscience.earth/ncl/geoera/ref/6382
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Bonndorf Fault Zone

Bonndorf Zone Fault 1
type: Fault
type: Limit
definition: WNW-ESE streichende Blattverschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6382
definition: WNW-ESE striking strike-slip fault
created: 2020-11-23T14:50:45.107Z
notation: geola_055
preferred label: Bonndorfer Störungszone Verwerfung 1 @de
notation: DE-BW_261
type: Concept
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Bonndorf Fault Zone

Bonndorf Zone Fault 4
type: Fault
type: Limit
notation: geola_058
definition: WNW-ESE striking strike-slip fault
type: Concept
definition: WNW-ESE streichende Blattverschiebung. @de
notation: DE-BW_264
references: https://data.geoscience.earth/ncl/geoera/ref/6382
preferred label: Bonndorfer Störungszone Verwerfung 4 @de
created: 2020-11-23T14:50:45.191Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Bonndorf Fault Zone

Bonndorf Zone Fault 3
type: Fault
type: Limit
notation: geola_057
references: https://data.geoscience.earth/ncl/geoera/ref/6382
definition: NW-SE striking strike-slip fault
notation: DE-BW_263
type: Concept
created: 2020-11-23T14:50:45.163Z
preferred label: Bonndorfer Störungszone Verwerfung 3 @de
definition: NW-SE streichende Blattverschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Bonndorf Fault Zone

Bonndorf Zone Fault 6
type: Fault
type: Limit
type: Concept
definition: NW-SE striking strike-slip fault
definition: NW-SE streichende Blattverschiebung. @de
preferred label: Bonndorfer Störungszone Verwerfung 6 @de
notation: geola_060
created: 2020-11-23T14:50:45.247Z
notation: DE-BW_266
references: https://data.geoscience.earth/ncl/geoera/ref/6382
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Bonndorf Fault Zone

Bonndorf Zone Fault 5
type: Fault
type: Limit
notation: geola_059
references: https://data.geoscience.earth/ncl/geoera/ref/6382
definition: NW-SE striking strike-slip fault
type: Concept
notation: DE-BW_265
created: 2020-11-23T14:50:45.219Z
preferred label: Bonndorfer Störungszone Verwerfung 5 @de
definition: NW-SE streichende Blattverschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Bonndorf Fault Zone

Bonndorf Zone Fault 8
type: Limit
type: Fault
notation: DE-BW_268
definition: WSW-ENE striking strike-slip fault
notation: geola_062
type: Concept
created: 2020-11-23T14:50:45.304Z
definition: WSW-ENE streichende Blattverschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6382
preferred label: Bonndorfer Störungszone Verwerfung 8 @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Bonndorf Fault Zone

Bonndorf Zone Fault 7
type: Fault
type: Limit
notation: DE-BW_267
references: https://data.geoscience.earth/ncl/geoera/ref/6382
created: 2020-11-23T14:50:45.276Z
notation: geola_061
type: Concept
definition: NW-SE striking strike-slip fault
preferred label: Bonndorfer Störungszone Verwerfung 7 @de
definition: NW-SE streichende Blattverschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Bonndorf Fault Zone

Freiburg-Bonndorf-Lake Constance Fault 2
type: Fault
type: Limit
type: Concept
notation: DE-BW_271
references: https://data.geoscience.earth/ncl/geoera/ref/6382
preferred label: Freiburg-Bonndorf-Bodensee Störung 2 @de
definition: WNW-ESE streichende, nach NNE einfallende Abschiebung mit unbekanntem Einfallswinkel. @de
created: 2020-11-23T14:50:45.388Z
notation: geola_065
definition: WNW-ESE striking normal fault, dipping NNE with unknown angle
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Freiburg-Bonndorf-Lake Constance Fault Zone

Freiburg-Bonndorf-Lake Constance Fault 3
type: Fault
type: Limit
notation: DE-BW_272
preferred label: Freiburg-Bonndorf-Bodensee Störung 3 @de
type: Concept
definition: W-E streichende, nach S einfallende Abschiebung mit unbekanntem Einfallswinkel. @de
created: 2020-11-23T14:50:45.416Z
definition: W-E striking normal fault, dipping S with unknown angle
references: https://data.geoscience.earth/ncl/geoera/ref/6382
notation: geola_066
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Freiburg-Bonndorf-Lake Constance Fault Zone

[geola_011]
type: Fault
type: Limit
type: Concept
definition: SSW-NNE striking normal fault, dipping ESE with unknown angle
references: https://data.geoscience.earth/ncl/geoera/ref/6382
created: 2020-11-23T14:50:43.794Z
notation: geola_011
notation: DE-BW_207
definition: SSW-NNE streichende, nach ESE einfallende Abschiebung mit unbekanntem Einfallswinkel. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Swabian-Franconian Alb fault domain

Südschwarzwald-Dinkelberg-Hegau Region Faults
type: Fault
type: Limit
type: Concept
definition: The roughly triangular area between Lörrach, Denzlingen and Konstanz is clearly separated from the Upper Rhine Rift as well as from the Upper Swabian Molasse Basin and the Southern Cuesta Terrain due to its structural division. It is the most uplifted and tilted area in Baden-Württemberg. The region between the southern Upper Rhine Graben and Lake Constance is intensively structured by fractures trending NW -SE and SSW-NNE with a height offset between a few meters and almost 200 m. In the north of the area (southern Black Forest-Randen-Hegau), within the Freiburg-Bonndorf-Lake Constance fault zone, the NW-SE trending elements come to the fore while in the south (Dinkelberg, High Rhine, continued in the Table Jura) the SSW-NNE trending elements are more prominent, without completely displacing the other. Because of the significant offset, the structures are mostly represented as tectonic graben and horst structures, but slickenside surfaces and displacements at rupture surfaces from recent earthquakes show right-lateral (NW-SE) or left-lateral (SSW-NNE fractures) movements. The throw of faults are obviously subordinate to these horizontal movements and possibly secondary compensatory movements due to the bulging and tilting of the crust between the Jura and Upper Rhine Rifts.
references: https://data.geoscience.earth/ncl/geoera/ref/6360
preferred label: Südschwarzwald-Dinkelberg-Hegau Region Störungen @de
created: 2020-11-23T14:50:45.020Z
notation: DE-BW_912
definition: Das etwa dreieckige Gebiet zwischen Lörrach, Denzlingen und Konstanz ist durch seine strukturelle Gliederung sowohl gegen den Oberrheingraben als auch gegen das oberschwäbische Molassebecken und das Südliche Schichtstufenland deutlich abgesetzt. Es handelt sich um das am stärksten gehobene und verkippte Gebiet in Baden-Württemberg. Die Region zwischen südlichem Oberrheingraben und Bodensee ist intensiv durch NW-SE- und SSW-NNE-streichende Brüche mit einem Höhenversatz zwischen wenigen Metern und annähernd 200 m gegliedert. Im Norden des Gebiets (Südschwarzwald–Randen–Hegau) treten dabei in der Freiburg–Bonndorf–Bodensee-Störungszone die NW-SE-, im Süden (Dinkelberg, Hochrhein, fortgesetzt im Tafeljura) die SSW-NNE-streichenden Elemente in den Vordergrund, ohne die jeweils anderen ganz zu verdrängen. Wegen des Höhenversatzes werden die Strukturen meist als tektonische Gräben und Horste dargestellt, doch zeigen Harnischflächen und Herdflächenlösungen rezenter Erdbeben rechtslaterale (NW-SE-) bzw. linkslaterale (SSW-NNE-Brüche) Bewegungen. Die vertikalen Sprunghöhen sind diesen Horizontalbewegungen offenbar nachgeordnet und möglicherweise sekundäre Ausgleichsbewegungen infolge der Aufwölbung und Verkippung der Kruste zwischen Faltenjura und Oberrheingraben. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Swabian-Franconian Alb fault domain

Albstadt Shear Zone
type: Fault
type: Limit
created: 2020-11-23T14:50:43.851Z
references: https://data.geoscience.earth/ncl/geoera/ref/6398
narrower: Teck Fault 3
narrower: Steinhilbe Fault 2
narrower: Teck Fault 1
preferred label: Albstadt Scherzone @de
narrower: Teck Fault 2
references: https://data.geoscience.earth/ncl/geoera/ref/6359
narrower: Teck Fault 4
notation: DE-BW_908
narrower: Teck Fault 5
narrower: Römerstein Fault
narrower: Steinhilben Fault 1
definition: According to the structure of the overburden, the southern layer plain is divided into two segments. To the west of the Lauchert-Mulde, which strikes about N-S, there is an approximately triangular block complex as a western slope of the Central Black Forest uniformly against ESE, which is bounded in the north by the Elztal and Bebenhausen fault zone, in the south by the Freiburg-Bonndorf-Lake Constance fault zone . According to the distribution of the recent earthquake epicentres, there is a left-lateral shear zone several kilometers wide in the basement, which is called the Albstadt shear zone, on the eastern edge of this western segment. The sinistral offset of this zone manifests itself on the surface in right-lateral-transtensive fractures (Hohenzollern-Graben, Achalm-Halfgraben) and in a parallel flexure-like offset of the Swabian lineament.
narrower: Trochtelfingen Fault 1
narrower: Zwiefalten Faultzone
narrower: Trochtelfingen Fault 2
narrower: Hohenzollern Graben
narrower: Pfronstetten-Kettenacker-Ittenhausen Fault
narrower: Achalm-Halfgraben
references: https://data.geoscience.earth/ncl/geoera/ref/6380
narrower: Indelhausen-Oberwilzingen Fault
type: Concept
narrower: Teck Fault 6
narrower: Lautertal Fault
references: https://data.geoscience.earth/ncl/geoera/ref/6389
narrower: Gauingen Fault
definition: Nach der Struktur des Deckgebirges zerfällt das Südliche Schichtstufenland in zwei Segmente. Westlich der etwa N-S streichenden Lauchert-Mulde fällt ein im Norden von Elztal- und Bebenhausen-Störungszone, im Süden von der Freiburg–Bonn­dorf – Bodensee-Störungszone etwa dreieckig begrenzter Schollenkomplex als Westabdachung des Zentralschwarzwaldes einheitlich gegen ESE ein. Nach der Ver­teilung der rezenten Erdbeben-Epizentren befindet sich am Ostrand dieses westlichen Segments eine mehrere Kilometer breite linkslaterale Scherzone im Grundgebirge, die als Albstadt-Scherzone bezeich­net wird. Der sinistrale Versatz dieser Zone äußert sich an der Oberfläche in fiederartig ange­legten Dehnungsbrüchen (Hohenzollern-Graben, Achalm-Halbgraben) und in parallelem flexurartigem Versatz von Klifflinie und Schwäbischem Lineament. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Swabian-Franconian Alb fault domain

Trochtelfingen Fault 1
type: Fault
type: Limit
preferred label: Trochtelfinger Verwerfung 1 @de
created: 2020-11-23T14:50:44.130Z
definition: SSW-NNE striking normal fault, dipping ESE with unknown angle
type: Concept
notation: DE-BW_213
definition: SSW-NNE streichende, nach ESE einfallende Abschiebung mit unbekanntem Einfallswinkel. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6382
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Albstadt Shear Zone

Steinhilben Fault 1
type: Fault
type: Limit
definition: SSW-NNE streichende, nach ESE einfallende Abschiebung mit unbekanntem Einfallswinkel. @de
preferred label: Steinhilbener Verwerfung 1 @de
created: 2020-11-23T14:50:44.103Z
references: https://data.geoscience.earth/ncl/geoera/ref/6382
notation: DE-BW_212
definition: SSW-NNE striking fault, dipping ESE with unknown angle
type: Concept
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Albstadt Shear Zone

Teck Fault 1
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6382
type: Concept
preferred label: Teck-Störung 1 @de
definition: NNW-SSE streichende, nach WSW einfallende Abschiebung mit unbekanntem Einfallswinkel. @de
created: 2020-11-23T14:50:43.879Z
definition: NNW-SSE striking normal fault, dipping WSW with unknown angle
notation: DE-BW_242
notation: geola_036
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Albstadt Shear Zone

Trochtelfingen Fault 2
type: Fault
type: Limit
definition: N-S striking normal fault, dipping W with unknown angle
definition: N-S streichende, nach W einfallende Abschiebung mit unbekanntem Einfallswinkel. @de
type: Concept
notation: DE-BW_215
preferred label: Trochtelfinger Verwerfung 2 @de
created: 2020-11-23T14:50:44.185Z
references: https://data.geoscience.earth/ncl/geoera/ref/6382
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Albstadt Shear Zone

Steinhilbe Fault 2
type: Fault
type: Limit
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6382
notation: DE-BW_214
preferred label: Steinhilbener Verwerfung 2 @de
definition: SSW-NNE streichende Blattverschiebung. @de
created: 2020-11-23T14:50:44.158Z
definition: SSW-NNE striking strike-slip fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Albstadt Shear Zone

Teck Fault 3
type: Fault
type: Limit
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6382
definition: N-S striking normal fault, dipping W with unknown angle
definition: N-S streichende, nach W einfallende Abschiebung mit unbekanntem Einfallswinkel. @de
preferred label: Teck-Störung 3 @de
notation: DE-BW_244
created: 2020-11-23T14:50:43.936Z
notation: geola_038
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Albstadt Shear Zone

Teck Fault 2
type: Fault
type: Limit
preferred label: Teck-Störung 2 @de
created: 2020-11-23T14:50:43.907Z
notation: DE-BW_243
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6382
definition: N-S striking normal fault, dipping W with unknown angle
notation: geola_037
definition: N-S streichende, nach W einfallende Abschiebung mit unbekanntem Einfallswinkel. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Albstadt Shear Zone

Hohenzollern Graben
type: Fault
type: Limit
definition: Hohenzollern Graben is a more than 30 km long, on average 1.5 km wide graben structure of the southwestern Swabian Alb. Running in Hercynian (NW-SE) direction, it formed some 15 ma ago as a result of the tectonic tension caused by the Alpine orogeny. Its conjugate, V-shaped marginal faults feature throws of up to 100 m on the Alb Plateau, and up to 40 m in the foreland. Hohenzollern Graben manifests a conspicuous relief inversion with the trough interior jutting out its surround by up to 350 m.
definition: Der Hohenzollern-Graben ist ein über 30 km langer und durchschnittlich 1,5 km breiter geologischer Graben im Bereich der südwestlichen Schwäbischen Alb, der sich in herzynischer Richtung (NW-SE) von der Albhochfläche bis ins Albvorland zieht. Er entstand vor ca. 15 Millionen Jahren als Folge der tektonischen Spannungen durch die Auffaltung der Alpen. Die den Hohenzollerngraben begrenzenden Randverwerfungen haben eine Sprunghöhe von rund 100 m auf der Albhochfläche und bis zu 40 m im Vorland und fallen als konjugierte Störungen V-förmig nach innen, wo sie wahrscheinlich in eine dextrale Scherzone münden, die als antithetische Nebenstörung der Nord-Süd orientierten Albstadt-Scherzone im Untergrund betrachtet wird. Der Hohenzollern-Graben zeigt eine ausgeprägte Reliefumkehr: Obwohl es sich um ein Einbruchgebiet handelt, überragt das grabeninnere Gelände seine Umgebung bis zu 350 m. @de
preferred label: Hohenzollern-Graben @de
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6389
created: 2020-11-23T14:50:44.212Z
narrower: Hohenzollern Graben Fault 1
references: https://data.geoscience.earth/ncl/geoera/ref/6398
narrower: Hohenzollern Graben Fault 2
narrower: Hohenzollern Graben Fault 3
narrower: Hohenzollern Graben Fault 5
narrower: Hohenzollern Graben Fault 4
references: https://data.geoscience.earth/ncl/geoera/ref/6359
notation: DE-BW_909
narrower: Hohenzollern Graben Fault 7
narrower: Hohenzollern Graben Fault 8
narrower: Hohenzollern Graben Fault 9
references: https://data.geoscience.earth/ncl/geoera/ref/6382
narrower: Hohenzollern Graben Fault 11
narrower: Hohenzollern Graben Fault 6
narrower: Hohenzollern Graben Fault 10
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Albstadt Shear Zone

Hohenzollern Graben Fault 8
type: Fault
type: Limit
type: Concept
preferred label: Hohenzollern-Graben Störung 8 @de
definition: WNW-ESE streichende Blattverschiebung; Teil der Nordrandverwerfung des Hohenzollerngrabens. @de
notation: DE-BW_230
notation: geola_028
definition: WNW-ESE striking strike-slip fault; part of the northern boundary of the Hohenzollerngraben.
created: 2020-11-23T14:50:44.437Z
references: https://data.geoscience.earth/ncl/geoera/ref/6382
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Hohenzollern Graben

Hohenzollern Graben Fault 7
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6382
notation: geola_027
notation: DE-BW_229
definition: WNW-ESE streichende Störung, Teil der Südrandverwerfung des Hohenzollerngrabens. Nordwestlicher Abschnitt als Blattverschiebung, südöstlicher Abschnitt als Abschiebung Richtung NNE mit unbekanntem Einfallswinkel ausgeprägt. @de
type: Concept
definition: WNW-ESE striking fault with the northwestern segemt developed as strike-slip and the southeastern part as normal fault dipping NNE with unkown angle; part of the southern boundary of the Hohenzollerngraben.
preferred label: Hohenzollern-Graben Störung 7 @de
created: 2020-11-23T14:50:44.408Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Hohenzollern Graben

Hohenzollern Graben Fault 10
type: Fault
type: Limit
definition: WNW-ESE streichende, nach SSW einfallende Abschiebung mit unbekanntem Einfallswinkel; Teil der Nordrandverwerfung des Hohenzollerngrabens. @de
notation: geola_030
notation: DE-BW_232
preferred label: Hohenzollern-Graben Störung 10 @de
references: https://data.geoscience.earth/ncl/geoera/ref/6382
definition: WNW-ESE striking normal fault, dipping SSW with unknown angle; part of the northern boundary of the Hohenzollerngraben.
created: 2020-11-23T14:50:44.492Z
type: Concept
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Hohenzollern Graben

Hohenzollern Graben Fault 9
type: Fault
type: Limit
preferred label: Hohenzollern-Graben Störung 9 @de
definition: WNW-ESE streichende Blattverschiebung; Teil der Südrandverwerfung des Hohenzollerngrabens. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6382
notation: DE-BW_231
type: Concept
notation: geola_029
definition: WNW-ESE striking strike-slip fault; part of the southern boundary of the Hohenzollerngraben.
created: 2020-11-23T14:50:44.464Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Hohenzollern Graben

Hohenzollern Graben Fault 1
type: Fault
type: Limit
definition: NW-SE striking normal fault, dipping NE with unknown angle, at intersection with DE-BW_227 partly strike-slip; part of the southern boundary of the Hohenzollerngraben.
created: 2020-11-23T14:50:44.241Z
definition: NW-SE streichende, nach NE einfallende Abschiebung mit unbekanntem Einfallswinkel; an der Verschneidung mit DE-BW_227 mit Blattverschiebungskomponente; Teil der Südrandverwerfung des Hohenzollerngrabens. @de
type: Concept
notation: DE-BW_223
references: https://data.geoscience.earth/ncl/geoera/ref/6359
notation: geola_021
preferred label: Hohenzollern-Graben Störung 1 @de
references: https://data.geoscience.earth/ncl/geoera/ref/6382
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Hohenzollern Graben

Hohenzollern Graben Fault 11
type: Fault
type: Limit
definition: SSW-NNE striking strike-slip fault; lateral fault of the Hohenzollerngraben.
references: https://data.geoscience.earth/ncl/geoera/ref/6382
type: Concept
notation: geola_031
notation: DE-BW_233
definition: SSW-NNE streichende Blattverschiebung; Nebenstörung des Hohenzollerngrabens. @de
preferred label: Hohenzollern-Graben Störung 11 @de
created: 2020-11-23T14:50:44.520Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Hohenzollern Graben

Hohenzollern Graben Fault 2
type: Fault
type: Limit
definition: NW-SE striking strike-slip fault; part of the northern boundary of the Hohenzollerngraben.
type: Concept
notation: geola_022
created: 2020-11-23T14:50:44.268Z
preferred label: Hohenzollern-Graben Störung 2 @de
notation: DE-BW_224
references: https://data.geoscience.earth/ncl/geoera/ref/6382
definition: NW-SE streichende Blattverschiebung; Teil der Nordrandverwerfung des Hohenzollerngrabens. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Hohenzollern Graben

Hohenzollern Graben Fault 4
type: Fault
type: Limit
type: Concept
notation: DE-BW_226
definition: NW-SE streichende, nach SW einfallende Abschiebung mit unbekanntem Einfallswinkel; Teil der Nordrandverwerfung des Hohenzollerngrabens. @de
notation: geola_024
preferred label: Hohenzollern-Graben Störung 4 @de
created: 2020-11-23T14:50:44.325Z
references: https://data.geoscience.earth/ncl/geoera/ref/6382
definition: NW-SE striking normal fault, dipping SW with unknown angle; part of the northern boundary of the Hohenzollerngraben.
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Hohenzollern Graben

Hohenzollern Graben Fault 3
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6382
notation: DE-BW_225
notation: geola_023
preferred label: Hohenzollern-Graben Störung 3 @de
definition: WNW-ESE streichende, nach SSW einfallende Abschiebung mit unbekanntem Einfallswinkel; Teil der Nordrandverwerfung des Hohenzollerngrabens. @de
type: Concept
definition: WNW-ESE striking normal fault, dipping SSW with unknown angle; part of the northern boundary of the Hohenzollerngraben.
created: 2020-11-23T14:50:44.297Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Hohenzollern Graben

Hohenzollern Graben Fault 6
type: Fault
type: Limit
created: 2020-11-23T14:50:44.381Z
type: Concept
notation: geola_026
notation: DE-BW_228
definition: WNW-ESE striking fault with the northern segment developed as normal fault dipping SSW with unknown angle and the southern part as strike-slip; part of the northern boundary of the Hohenzollerngraben.
definition: WNW-ESE streichende Störung; nördlicher Abschnitt als Abschiebung Richtung SSW mit unbekanntem Einfallswinkel, südlicher Abschnitt als Blattverschiebung ausgeprägt; Teil der Nordrandverwerfung des Hohenzollerngrabens. @de
preferred label: Hohenzollern-Graben Störung 6 @de
references: https://data.geoscience.earth/ncl/geoera/ref/6382
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Hohenzollern Graben

Hohenzollern Graben Fault 5
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6382
definition: NW-SE streichende Blattverschiebung; an der Verschneidung mit DE-BW_223 mit Abschiebungskomponente; Teil der Südrandverwerfung des Hohenzollerngrabens. @de
created: 2020-11-23T14:50:44.353Z
notation: DE-BW_227
notation: geola_025
type: Concept
preferred label: Hohenzollern-Graben Störung 5 @de
definition: NW-SE striking strike-slip fault, at intersection with DE-BW_223 partly normal faulting; part of the southern boundary of the Hohenzollerngraben.
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Hohenzollern Graben

Teck Fault 4
type: Fault
type: Limit
definition: NW-SE streichende, nach SW einfallende Abschiebung mit unbekanntem Einfallswinkel. @de
preferred label: Teck-Störung 4 @de
notation: geola_039
notation: DE-BW_245
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6382
definition: NW-SE striking normal fault, dipping SW with unknown angle
created: 2020-11-23T14:50:43.965Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Albstadt Shear Zone

Gauingen Fault
type: Fault
type: Limit
definition: N–S streichendes Abschiebungs system mit 2 Hauptstörungen @de
definition: N-S striking normal fault system with two main faults
references: https://data.geoscience.earth/ncl/geoera/ref/6370
preferred label: Gauinger Verwerfung @de
references: https://data.geoscience.earth/ncl/geoera/ref/6390
notation: DE-BW_216
type: Concept
created: 2020-11-23T14:50:44.576Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Albstadt Shear Zone

Pfronstetten-Kettenacker-Ittenhausen Fault
type: Fault
type: Limit
type: Concept
definition: SSW-NNE striking normal fault, dipping ESE with unknown angle
notation: DE-BW_237
definition: SSW-NNE streichende, nach ESE einfallende Abschiebung mit unbekanntem Einfallswinkel. @de
created: 2020-11-23T14:50:44.548Z
notation: geola_076
preferred label: Pfronstetten-Kettenacker-Ittenhausen Verwerfung @de
references: https://data.geoscience.earth/ncl/geoera/ref/6382
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Albstadt Shear Zone

Teck Fault 6
type: Fault
type: Limit
definition: N-S streichende, nach W einfallende Abschiebung mit unbekanntem Einfallswinkel. @de
definition: N-S striking normal fault, dipping W with unknown angle
notation: geola_041
type: Concept
notation: DE-BW_247
preferred label: Teck-Störung 6 @de
created: 2020-11-23T14:50:44.021Z
references: https://data.geoscience.earth/ncl/geoera/ref/6382
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Albstadt Shear Zone

Lautertal Fault
type: Fault
type: Limit
notation: DE-BW_235
definition: SW-NE striking normal fault, downthrow of SE-block about 70 m
notation: geola_074
references: https://data.geoscience.earth/ncl/geoera/ref/6390
references: https://data.geoscience.earth/ncl/geoera/ref/6370
created: 2020-11-23T14:50:44.632Z
preferred label: Lautertal Störung @de
definition: SW-NE streichende Störung, SE-Scholle etwa 70 m abgesunken @de
type: Concept
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Albstadt Shear Zone

Teck Fault 5
type: Fault
type: Limit
created: 2020-11-23T14:50:43.993Z
definition: WSW-ENE streichende, nach WNW einfallende Abschiebung mit unbekanntem Einfallswinkel. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6382
notation: geola_040
preferred label: Teck-Störung 5 @de
notation: DE-BW_246
definition: SSW-NNE striking normal fault, dipping WNW with unknown angle
type: Concept
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Albstadt Shear Zone

Indelhausen-Oberwilzingen Fault
type: Fault
type: Limit
definition: NNW-SSE streichende, nach WSW einfallende Abschiebung mit unbekanntem Einfallswinkel. @de
definition: NNW-SSE striking normal fault, dipping WSW with unknown angle.
notation: geola_073
preferred label: Indelhausen-Oberwilzingen-Störung @de
type: Concept
created: 2020-11-23T14:50:44.604Z
notation: DE-BW_234
references: https://data.geoscience.earth/ncl/geoera/ref/6382
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Albstadt Shear Zone

Achalm-Halfgraben
type: Fault
type: Limit
created: 2020-11-23T14:50:44.076Z
definition: NW-SE streichender Halbgraben, welcher neben abschiebenenden teilweise auch dextral-transtensive Bewegungsindikatoren aufweist. Diese entsprechen konjugierten antithetischen Scherflächen zu den sinistralen Gleitbewegungen des tieferen Gebirges im Bereich der Albstadt-Scherzone; nördliche Begrenzung durch Störung, Südgrenze als Flexur. @de
definition: NW-SE striking single halfgraben, which shows characteristics of normal faulting and right-lateral-transtensive movement. The latter correspont to conjugated antithetical shear surfaces to the left-lateral sliding movement of the basement in the area of the Albstadt Shear Zone; northern boundary as fault, southern boundary as a flexure.
references: https://data.geoscience.earth/ncl/geoera/ref/6389
type: Concept
notation: DE-BW_211
references: https://data.geoscience.earth/ncl/geoera/ref/6359
preferred label: Achalm-Halbgraben @de
references: https://data.geoscience.earth/ncl/geoera/ref/6398
references: https://data.geoscience.earth/ncl/geoera/ref/6382
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Albstadt Shear Zone

Römerstein Fault
type: Fault
type: Limit
preferred label: Römerstein Verwerfung @de
notation: geola_001
references: https://data.geoscience.earth/ncl/geoera/ref/6382
created: 2020-11-23T14:50:44.049Z
notation: DE-BW_197
definition: N-S streichende, nach W einfallende Abschiebung mit unbekanntem Einfallswinkel. @de
definition: N-S striking normal fault, dipping W with unknown angle
type: Concept
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Albstadt Shear Zone

Zwiefalten Faultzone
type: Fault
type: Limit
preferred label: Zwiefaltener Bruchfeld @de
created: 2020-11-23T14:50:44.659Z
type: Concept
notation: DE-BW_251
notation: geola_045
definition: N-S streichende, nach E einfallende Abschiebung mit unbekanntem Einfallswinkel. @de
definition: N-S striking normal fault, dipping E with unknown angle
references: https://data.geoscience.earth/ncl/geoera/ref/6382
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Albstadt Shear Zone

Schlossberg Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:38.012Z
notation: DE-BY_1325
preferred label: Schloßberg Störung @de
definition: SW-NE striking, vertical to steeply NW dipping normal fault running W to NW of Kallmünz across the Vils river valley.
definition: SW-NE streichende, saigere bis steil nach NW einfallende Abschiebung W bis NW von Kallmünz, quer durch das Vilstal. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4124
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1325
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Ursheim Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:36.788Z
notation: DE-BY_1281
preferred label: Ursheim Störung @de
definition: W-E striking normal fault crossing Rohrach river valley south of Schmidsberg-Hahnenberg Fault [N_11].
definition: Das Rohrachtal querende, W-E streichende Abschiebung südlich der Schmidsberg-Hahnenberg Störung [N_11]. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1281
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Sandbreite Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:37.984Z
notation: DE-BY_1324
preferred label: Sandbreite Störung @de
definition: N-S striking, vertical to steeply E dipping normal fault with a minor throw.
definition: N-S streichende, saigere bis steil nach E einfallende Abschiebung mit geringer Sprunghöhe. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4124
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1324
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Krachenhausen-Holzheim Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:37.957Z
notation: DE-BY_1323
preferred label: Krachenhausen-Holzheim Störung @de
definition: W-E striking fault along Holzheimer valley.
definition: W-E streichende Störung entlang des Holzheimer Tals. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4124
sf touches: Krachenhausen-Dornau Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1323
broader: Swabian-Franconian Alb fault domain

Filstal Graben
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/7675
definition: Schwäbisch (SW-NE) streichendes Grabenbruchfeld mit Verwerfungen um 25 m, welches die Krusteneinwölbung (um 100 m auf 10 km Breite) des oberen Filstals überprägt. @de
type: Concept
definition: Swabian (SW-NE) striking rift valley with faults of 25 m offset, overprinting the crustal vaulting (100 m over 10 km width) of the upper Fils valley.
narrower: Mähdlesbühl Fault
narrower: Filstal Graben Fault 1
notation: DE-BW_911
created: 2020-11-23T14:50:44.882Z
preferred label: Filstal-Graben @de
narrower: Filstal Graben Fault 2
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Swabian-Franconian Alb fault domain

Filstal Graben Fault 1
type: Fault
type: Limit
created: 2020-11-23T14:50:44.937Z
definition: SSW-NNE streichende, nach WNW einfallende Abschiebung mit unbekanntem Einfallswinkel. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6382
notation: DE-BW_209
notation: geola_013
definition: SSW-NNE striking normal fault, dipping WNW with unknown angle
type: Concept
preferred label: Filstal-Graben Störung 1 @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Filstal Graben

Mähdlesbühl Fault
type: Fault
type: Limit
type: Concept
definition: SW-NE streichende, nach SE einfallende Abschiebung mit unbekanntem Einfallswinkel. @de
created: 2020-11-23T14:50:44.909Z
notation: DE-BW_236
preferred label: Mähdlesbühl-Verwerfung @de
definition: SW-NE striking normal fault, dipping SE with unkown angle
references: https://data.geoscience.earth/ncl/geoera/ref/6382
notation: geola_077
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Filstal Graben

Filstal Graben Fault 2
type: Fault
type: Limit
created: 2020-11-23T14:50:44.965Z
type: Concept
definition: WSW-ENE streichende, nach SSE einfallende Abschiebung mit unbekanntem Einfallswinkel. @de
definition: WSW-ENE striking normal fault, dipping SSE with unknown angle
notation: geola_014
notation: DE-BW_210
references: https://data.geoscience.earth/ncl/geoera/ref/6382
preferred label: Filstal-Graben Störung 2 @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Filstal Graben

Krachenhausen-Dornau Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:37.929Z
notation: DE-BY_1322
preferred label: Krachenhausen-Dornau Störung @de
definition: NW-SE striking, steeply NE dipping normal fault.
definition: NW-SE streichende, steil nach NE einfallende Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4124
sf touches: Krachenhausen-Holzheim Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1322
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

[geola_008]
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6382
created: 2020-11-23T14:50:43.711Z
definition: SW-NE striking normal fault, dipping SE with unkown angle
type: Concept
notation: DE-BW_204
definition: SW-NE streichende, nach SE einfallende Abschiebung mit unbekanntem Einfallswinkel. @de
notation: geola_008
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Swabian-Franconian Alb fault domain

Arberschlag-Hubhof Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4124
definition: SW-NE streichende, steil nach NE einfallende Abschiebung mit einer Sprunghöhe um 10 m. @de
type: Concept
created: 2020-10-09T11:35:37.901Z
notation: DE-BY_1321
preferred label: Arberschlag-Hubhof Störung @de
definition: SW-NE striking, steeply NE dipping normal fault with an approx. 10 m throw.
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1321
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Sachsenhofen-Vogelhüll Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4118
references: https://data.geoscience.earth/ncl/geoera/ref/4124
sf touches: Duggendorf Fault
type: Concept
created: 2020-10-09T11:35:37.874Z
notation: DE-BY_1320
preferred label: Sachsenhofen-Vogelhüll Störung @de
definition: N-S striking, vertical to steeply E dipping normal fault featuring a throw of up to 15 m.
definition: N-S streichende, saigere bis steil nach E einfallende Abschiebung mit einer Sprunghöhe bis zu 15 m. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1320
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Frieding Fault
type: Fault
type: Limit
definition: SSW-NNE striking normal fault, dipping ESE with unknown angle
references: https://data.geoscience.earth/ncl/geoera/ref/6382
definition: SSW-NNE streichende, nach ESE einfallende Abschiebung mit unbekanntem Einfallswinkel. @de
created: 2020-11-23T14:50:43.767Z
type: Concept
notation: geola_010
notation: DE-BW_206
type: SpatialObject
preferred label: Friedinger Störung @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Swabian-Franconian Alb fault domain

Mindelsee Fault
type: Fault
type: Limit
definition: NW-SE streichende, ca. 80° nach SW einfallende Abschiebung mit um ca. 120 m abgesenkter SW-Scholle; Teil der Bodenseebrüche und NE-Randstörung des Hegau Grabens, damit Grenzlinie zwischen dem eigentlichen Molassebecken und seinem Beckenrand als Teil der Freiburg-Bonndorf-Bodensee Zone [DE-BW_913]. @de
definition: NW-SE striking, approx. 80 ° to SW dipping normal fault with SW downthrow block lowered by approx. 120 m. Part of the Lake Constance fractures and northeastern marginal fault of the Hegau Graben, thus the borderline between the Molasse basin proper and its basin edge as part of the Freiburg-Bonndorf-Lake Constance Zone [DE-BW_913].
references: https://data.geoscience.earth/ncl/geoera/ref/6392
references: https://data.geoscience.earth/ncl/geoera/ref/6390
created: 2020-11-23T14:50:44.993Z
references: https://data.geoscience.earth/ncl/geoera/ref/6359
preferred label: Mindelsee-Verwerfung @de
type: Concept
notation: DE-BW_145
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Swabian-Franconian Alb fault domain

Duggendorf Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4118
references: https://data.geoscience.earth/ncl/geoera/ref/4124
sf touches: Sachsenhofen-Vogelhüll Fault
type: Concept
created: 2020-10-09T11:35:37.846Z
notation: DE-BY_1319
preferred label: Duggendorf Störung @de
definition: WNW-ESE to WSW-ENE trending, steeply SSW to SSE dipping normal fault featuring a throw of up to 40 m.
definition: WNW-ESE bis WSW-ENE verlaufende, steil nach SSW bis SSE einfallende Abschiebung mit einer Sprunghöhe bis zu 40 m. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1319
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

[geola_009]
type: Fault
type: Limit
definition: WSW-ENE streichende, nach SSE einfallende Abschiebung mit unbekanntem Einfallswinkel. @de
type: Concept
definition: WSW-ENE striking normal fault, dipping SSE with unknown angle
created: 2020-11-23T14:50:43.739Z
references: https://data.geoscience.earth/ncl/geoera/ref/6382
notation: DE-BW_205
notation: geola_009
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Swabian-Franconian Alb fault domain

Kühschlag-Nittendorf Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4114
sf touches: Deuerling Fault
type: Concept
created: 2020-10-09T11:35:37.818Z
notation: DE-BY_1318
preferred label: Kühschlag-Nittendorf Störung @de
definition: Kinked S-N to SSW-NNE trending, steeply E to ESE dipping normal fault.
definition: Geknickt S-N bis SSW-NNE verlaufende, steil nach E bis ESE einfallende Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1318
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Kaldorf-Tafelmühle Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4136
references: https://data.geoscience.earth/ncl/geoera/ref/4115
type: Concept
created: 2020-10-09T11:35:36.956Z
notation: DE-BY_1287
preferred label: Kaldorf-Tafelmühle Störung @de
definition: SW-NE striking pair of conjugate normal faults W of Titting, a SE dipping northwestern branch and a NW dipping southeastern branch, forming a local graben structure.
definition: SW-NE streichendes Paar konjugierter Abschiebungen W von Titting, die mit einem nach SE einfallenden Nordwest-Ast und einem nach NE einfallenden Südost-Ast eine lokale Grabenstruktur begrenzen. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1287
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Preith-Walting Lineament
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4085
references: https://data.geoscience.earth/ncl/geoera/ref/4115
type: Concept
created: 2020-10-09T11:35:36.928Z
notation: DE-BY_1286
definition: Predominantly W-E trending, strikingly persistent lineament, turning to a WNW-ESE trend along Affental dry valley. Due to the intense interlock of facies in the Upper Jurassic carbonates vertical and/or lateral movements cannot be verified.
definition: Überwiegend W-E verlaufendes und auffallend langes Lineament, das entlang des Affental auf WNW-ESE umbiegt. Vertikale und/oder laterale Versätze sind aufgrund der intensiven Faziesverzahnung im Weißen Jura nicht nachzuweisen. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Swabian-Franconian Alb fault domain

Mühltal Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:38.068Z
notation: DE-BY_1327
preferred label: Mühltal Störung @de
definition: SW-NE to SSW-NNE trending, steeply SE to ESE dipping normal fault.
definition: SW-NE bis SSW-NNE verlaufende, steil nach SE bis ESE einfallende Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4124
sf touches: Rohrbach Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1327
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Lichtenberg Step Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4154
references: https://data.geoscience.earth/ncl/geoera/ref/4088
references: https://data.geoscience.earth/ncl/geoera/ref/4138
type: Concept
created: 2020-10-09T11:35:36.845Z
notation: DE-BY_1283
preferred label: Lichtenbergsprung @de
definition: WNW-ESE trending, approx. 70° SSE dipping, 2- to 3-stepped step fault featuring a throw of overall up to 30 m.
definition: Südlich von Solnhofen WNW-ESE verlaufende, ca. 70° nach SSE einfallende, 2- bis 3-stufige Bruchstaffel mit einem Verwurf von insgesamt bis zu 30 m. @de
narrower: Schelmenbuck-Maxberg Fault
narrower: Schrandelbuck-Mörnsheim Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1283
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Schrandelbuck-Mörnsheim Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4131
references: https://data.geoscience.earth/ncl/geoera/ref/4088
references: https://data.geoscience.earth/ncl/geoera/ref/4138
type: Concept
created: 2020-10-09T11:35:36.900Z
notation: DE-BY_1285
preferred label: Schrandelbuck-Mörnsheim Störung @de
definition: WNW-ESE trending, approx. 70° SSE dipping normal fault; southern scarp of Lichtenberg Step Fault.
definition: WNW-ESE verlaufende, ca. 70° nach SSE einfallende Abschiebung; südlicher Abbruch des Lichtenbergsprungs. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1285
limit type: normalFault
broader: Lichtenberg Step Fault

Schelmenbuck-Maxberg Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4138
references: https://data.geoscience.earth/ncl/geoera/ref/4154
references: https://data.geoscience.earth/ncl/geoera/ref/4088
type: Concept
created: 2020-10-09T11:35:36.872Z
notation: DE-BY_1284
preferred label: Schelmenbuck-Maxberg Störung @de
definition: WNW-ESE trending, approx. 70° SSE dipping normal fault. Main scarp of Lichtenberg Step Fault, towards the west increasingly covered by Ries Impact ejecta masses.
definition: WNW-ESE verlaufende, ca. 70° nach SSE einfallende Abschiebung. Nach Westen hin zunehmend von Ries-Trümmermassen verdeckter Hauptabbruch des Lichtenbergsprungs. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1284
limit type: normalFault
broader: Lichtenberg Step Fault

Rohrbach Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:38.040Z
notation: DE-BY_1326
preferred label: Rohrbach Störung @de
definition: WSW-ENE striking, steeply NNW dipping normal fault crossing Vils river valley south of Rohrbach.
definition: WSW-ENE streichende, steil nach NNW einfallende Abschiebung; quert das Vilstal südlich von Rohrbach. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4124
sf touches: Mühltal Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1326
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Judenbuck-Pappenheim Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4125
type: Concept
created: 2020-10-09T11:35:36.816Z
notation: DE-BY_1282
preferred label: Judenbuck-Pappenheim Störung @de
definition: Slightly undulate W-E trending, steeply N dipping normal fault with a throw of up to 40 m running sub-parallel to Heunischhof-Treuchtlingen Fault [DE-BY_1262) and Schambach Fault [DE-BY_1261] forming a local graben structure in between.
definition: Leicht gewellt W-E verlaufende, steil nach N einfallende Abschiebung mit einem Vertikalversatz von bis zu 40 m. Bildet mit den nördlich sub-parallel verlaufenden Heunischhof-Treuchtlingen [DE-BY_1262) und Schambach [DE-BY_1261] Störungen eine lokale Grabenstruktur. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1282
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Vils Valley train of faults
type: Fault
type: Limit
created: 2021-01-25T14:46:55.451Z
type: Concept
type: SpatialObject
preferred label: Vilstal Störungszug @de
notation: DE-BY_1546
definition: Running from Vilshofen (with a possible northern extension as far as Ebermanndorf) to Schmidmühlen more or less along Vils river valley, array of NNW-SSE and NNE-SSW striking fault segments, partly in two branches. This overall N-S trending train of normal faults, inferred in most sections, dips steeply to the west with a minor throw of up to 15 m.
definition: Von Vilshofen (möglicherweise bereits von Ebermannsdorf) überwiegend entlang des Vilstales bis nach Schmidmühlen ziehende Abfolge NNW-SSE und NNE-SSW streichender Störungssegmente, abschnittsweise in zwei Ästen. Dieser insgesamt N-S verlaufende, in den meisten Abschnitten vermuteter Störungszug, besteht aus steil W fallenden Abschiebungen mit einer Sprunghöhe von höchstens 15 m. @de
references: https://data.geoscience.earth/ncl/geoera/ref/7322
references: https://data.geoscience.earth/ncl/geoera/ref/7677
references: https://data.geoscience.earth/ncl/geoera/ref/7320
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1546
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Unterödenhart Fault
type: Fault
type: Limit
created: 2021-01-25T14:45:32.872Z
type: Concept
type: SpatialObject
preferred label: Unterödenhart Störung @de
notation: DE-BY_1545
definition: Running from Reisberg to Machendorf deserted hamlet, N-S to WNW-ESE trending, steeply E to NNE dipping normal fault with a minor throw.
definition: Vom Reisberg zur Wüstung Machendorf ziehende, N-S bis WNW-ESE verlaufende, steil nach E bis nach NNE einfallende Abschiebung mit geringer Sprunghöhe. @de
references: https://data.geoscience.earth/ncl/geoera/ref/7677
references: https://data.geoscience.earth/ncl/geoera/ref/7320
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1545
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Hohenfels-Machtelwies Fault
type: Fault
type: Limit
created: 2021-01-25T14:43:36.759Z
type: Concept
type: SpatialObject
preferred label: Hohenfels-Machtelwies Störung @de
notation: DE-BY_1544
definition: Discontinuous, undulate WSW-ESE to W-E trending, steeply ± N dipping normal fault with a minor throw up to 10 m.
definition: Diskontinuierliche, gewellt WSW-ENE bis W-E verlaufende, steil nach ± N einfallende Abschiebung mit einer geringen Sprunghöhe von höchstens 10 m. @de
references: https://data.geoscience.earth/ncl/geoera/ref/7677
references: https://data.geoscience.earth/ncl/geoera/ref/7320
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1544
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Oberbügl-Michelsberg Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:38.095Z
notation: DE-BY_1328
preferred label: Oberbügl-Michelsberg Störung @de
definition: NNW-SSE striking fault of unresolved kinematic.
definition: NNW-SSE streichende Störung unbekannter Kinematic. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4124
sf touches: Mitterbügl Cross Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1328
broader: Swabian-Franconian Alb fault domain

Thannhausen Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:38.317Z
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4075
sf touches: Hattenhausen Fault
sf touches: Schafshill-Neuenhizenhausen Fault
notation: DE-BY_1336
preferred label: Thannhausen Störung @de
definition: W-E striking, steeply N dipping normal fault.
definition: W-E streichende, steil nach N einfallende Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1336
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Schellenburg Horsts Scarps
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:37.095Z
notation: DE-BY_1292
preferred label: Schellenburg Horst-Flanken @de
definition: Altmühl and Anlauter valleys at their confluence with Schwarzach valley at Kinding show relief inversions underneath the Quaternary alluvium, formed by SSW-NNE trending upheavals. Inferred from borehole evidence the confining steeply dipping reverse faults feature a 30 m throw (Altmühl valley) and less than 10 m (Anlauter valley). Due to lack of evidence the continuation of the horst flanks to the south as well as to the north, crossing Schwarzach valley, is uncertain. Virtual extension of the fault’s trend to the north implies a merger into / branching off or truncation by Rumburg-Kinding Fault [DE-BY_1274] and its unexposed continuation along Schwarzwald-Bayerwald Line [DE-BY_1255]. At depth, the Altmühl valley horst flanks margin a geophysically detected Permian Rotliegend trough, implying a Variscan origin and post-Jurassic reactivation of the faults.
definition: Die Täler von Altmühl und Anlauter zeigen an ihrer Einmündung ins Schwarzachtal bei Kinding unter der quartären Talfüllung eine Reliefumkehr, hervorgerufen durch SSW-NNE (rheinisch) streichende, Horst-artige Strukturen. Die begrenzenden, steil einfallenden Aufschiebungen weisen, abgeleitet aus Bohloch-Korrelationen, Sprunghöhen von 30 m (Altmühltal) und weniger als 10 m (Anlautertal) auf. Wegen fehlender Geländenachweise ist die Fortsetzung der Horst-Flanken nach Süden wie Norden (im und jenseits des Schwarzachtals) hin, ungeklärt. Eine virtuelle Verlängerung der Horst-Flanken nach Norden, deutet auf eine Konfluenz mit der oder Kappung durch die Rumburg-Kinding Störung [DE-BY_1274] hin, bzw. ihrer nicht aufgeschlossenen Verlängerung entlang der Schwarzwald-Bayerwald Linie [DE-BY_1255]. Die Flanken des Altmühltal Horstes begrenzen auch den geophysikalisch nachgewiesenen Rotliegend Trog in der Tiefe; eine variskische Anlage und post-jurassische Reaktivierung der Brüche ist daher anzunehmen. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4116
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1292
limit type: reverseFault
broader: Swabian-Franconian Alb fault domain

Hattenhausen Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:38.290Z
notation: DE-BY_1335
definition: NW-SE streichende, steil nach SW einfallende Abschiebung. @de
type: SpatialObject
preferred label: Hattenhausen Störung @de
definition: NW-SE striking, steeply SW dipping normal fault.
references: https://data.geoscience.earth/ncl/geoera/ref/4075
sf touches: Thannhausen Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1335
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Frauenleite Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:37.067Z
notation: DE-BY_1291
preferred label: Frauenleite Störung @de
definition: W-E trending, steeply S dipping two-step normal fault NW of Kinding.
definition: Nordwestlich von Kinding W-E verlaufende, steil nach S einfallende zweistufige Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4135
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1291
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Lautersee Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:38.262Z
notation: DE-BY_1334
preferred label: Lautersee Störung @de
definition: West of Painten NNW-SSE striking, steeply WSW dipping normal fault with a throw of about 10 m.
definition: Westlich von Painten NNW-SSE streichende, steil nach WSW einfallende Abschiebung mit einer Sprunghöhe um 10 m. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4075
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1334
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Euerwang Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:37.039Z
notation: DE-BY_1290
preferred label: Euerwang Störung @de
definition: South of Euerwang WNW-ESE striking, steeply S dipping normal fault featuring a throw of up to 15 m.
definition: Südlich von Euerwang WNW-ESE streichende,steil südfallende Abschiebung mit einer Sprunghöhe von bis zu 15 m. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4136
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1290
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Swabian Lineament
type: Fault
type: Limit
definition: Western Part of the Schwarzwald-Bayerwald Line, a principal fault zone cutting WSW-ENE to W-E through southern Germany. Multi-phase oblique-slip fault system, west of the Ries Impact Crater [DE-BY_1342], in Baden-Württemberg, as the WSW-ENE striking Swabian Lineament traceable in the Upper Jurassic carbonates between Heubach W Aalen and the Ries crater only, in few predominantly steeply S dipping fault segments featuring throws from 20 to 100 m.
definition: Westlicher Abschnitt der Schwarzwald-Bayerwald Linie, einer bedeutenden Störungszone die sich in WSW-ENE bis W-E Richtung quer durch Süddeutschland verfolgen lässt. Mehrphasiges Schrägabschiebungssystem das sich westlich des Rieskraters [DE-BY_1342], in Baden-Württemberg, als WSW-ENE streichendes Schwäbische Lineament nur abschnittsweise als überwiegend steil südfallende Störung mit Vertikalversätzen von 20 bis 100 m manifestiert und von Heubach W Aalen bis zum Ries durch die oberjurassischen Karbonate zieht. Zwischen den Schollen nördlich und südlich des Schwäbischen Lineaments besteht ein nur unbedeutender Höhenversatz, die großen Sprunghöhen liegen zwischen den Teilschollen im Inneren der Störungszone. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6362
narrower: Swabian Lineament 1
narrower: Swabian Lineament 2
created: 2020-11-23T14:50:43.042Z
preferred label: Schwäbisches Lineament @de
narrower: Swabian Lineament 3
references: https://data.geoscience.earth/ncl/geoera/ref/6393
references: https://data.geoscience.earth/ncl/geoera/ref/6361
narrower: Swabian Lineament 4
notation: DE-BW_906
narrower: Hohenstaufen Fault Zone
type: Concept
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Swabian-Franconian Alb fault domain

Hohenstaufen Fault Zone
type: Fault
type: Limit
narrower: Hohenstaufen Fault Zone - Fault 6
narrower: Hohenstaufen Fault Zone - Fault 2
preferred label: Hohenstaufen Störungszone @de
narrower: Hohenstaufen Fault Zone - Fault 3
narrower: Hohenstaufen Fault Zone - Fault 4
narrower: Hohenstaufen Fault Zone - Fault 5
definition: SW-NE streichendes sinistrales Störungssystem zwischen Fildergraben und Ries; vertikale Versatzbeträge wechseln innerhalb kurzer Distanzen stark. Östlicher Abschnitt des Schwäbischen Lineaments. @de
narrower: Hohenstaufen Fault Zone - Fault 1
narrower: Hohenstaufen Fault Zone - Fault 8
narrower: Hohenstaufen Fault Zone - Fault 7
definition: SW-NE striking left-lateral fault system between the Fildergaben and Ries; vertical offset vary greatly within short distances. Eastern section of the Swabian lineament.
created: 2020-11-23T14:50:43.180Z
narrower: Hohenstaufen Fault Zone - Fault 9
references: https://data.geoscience.earth/ncl/geoera/ref/6361
type: Concept
narrower: Hohenstaufen Fault Zone - Fault 10
narrower: Hohenstaufen Fault Zone - Fault 11
notation: DE-BW_907
narrower: Hohenstaufen Fault Zone - Fault 12
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Swabian Lineament

Hohenstaufen Fault Zone - Fault 1
type: Fault
type: Limit
created: 2020-11-23T14:50:43.207Z
preferred label: Hohenstaufen Störungszone Fiederstruktur 1 @de
notation: DE-BW_248
definition: WNW-ESE striking strike-slip fault, as horsetail splay structure part of the swabian lineament
type: Concept
notation: geola_042
references: https://data.geoscience.earth/ncl/geoera/ref/6382
definition: Teil des Schwäbischen Lineaments @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Hohenstaufen Fault Zone

Hohenstaufen Fault Zone - Fault 12
type: Fault
type: Limit
type: Concept
created: 2020-11-23T14:50:43.514Z
definition: W-E streichende Blattverschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6382
notation: geola_054
notation: DE-BW_260
preferred label: Hohenstaufen Störungszone Verwerfung 12 @de
definition: W-E striking strike-slip fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Hohenstaufen Fault Zone

Hohenstaufen Fault Zone - Fault 11
type: Fault
type: Limit
created: 2020-11-23T14:50:43.486Z
definition: WSW-ENE striking strike-slip fault
preferred label: Hohenstaufen Störungszone Verwerfung 11 @de
notation: DE-BW_259
type: Concept
notation: geola_053
definition: WSW-ENE streichende Blattverschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6382
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Hohenstaufen Fault Zone

Hohenstaufen Fault Zone - Fault 3
type: Fault
type: Limit
preferred label: Hohenstaufen Störungszone Fiederstruktur 3 @de
notation: DE-BW_250
created: 2020-11-23T14:50:43.263Z
notation: geola_044
definition: WNW-ESE streichende Blattverschiebung; als Fierderstruktur Teil des Schwäbischen Lineamentes @de
type: Concept
definition: WNW-ESE striking strike-slip fault, as horsetail splay structure part of the swabian lineament
references: https://data.geoscience.earth/ncl/geoera/ref/6382
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Hohenstaufen Fault Zone

Hohenstaufen Fault Zone - Fault 2
type: Fault
type: Limit
definition: WNW-ESE streichende Blattverschiebung; als Fierderstruktur Teil des Schwäbischen Lineamentes @de
notation: DE-BW_249
preferred label: Hohenstaufen Störungszone Fiederstruktur 2 @de
references: https://data.geoscience.earth/ncl/geoera/ref/6382
type: Concept
notation: geola_043
created: 2020-11-23T14:50:43.236Z
definition: WNW-ESE striking strike-slip fault, as horsetail splay structure part of the swabian lineament
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Hohenstaufen Fault Zone

Hohenstaufen Fault Zone - Fault 5
type: Fault
type: Limit
created: 2020-11-23T14:50:43.318Z
notation: DE-BW_253
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6382
preferred label: Hohenstaufen Störungszone Verwerfung 5 @de
definition: WSW-ENE striking strike-slip fault
definition: WSW-ENE streichende Blattverschiebung. @de
notation: geola_047
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Hohenstaufen Fault Zone

Hohenstaufen Fault Zone - Fault 4
type: Fault
type: Limit
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6382
definition: W-E streichende Blattverschiebung. @de
definition: W-E striking strike-slip fault
created: 2020-11-23T14:50:43.291Z
notation: DE-BW_252
preferred label: Hohenstaufen Störungszone Verwerfung 4 @de
notation: geola_046
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Hohenstaufen Fault Zone

Hohenstaufen Fault Zone - Fault 7
type: Fault
type: Limit
created: 2020-11-23T14:50:43.374Z
references: https://data.geoscience.earth/ncl/geoera/ref/6382
definition: WSW-ENE streichende Blattverschiebung. @de
notation: DE-BW_255
preferred label: Hohenstaufen Störungszone Verwerfung 7 @de
type: Concept
definition: WSW-ENE striking strike-slip fault
notation: geola_049
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Hohenstaufen Fault Zone

Hohenstaufen Fault Zone - Fault 6
type: Fault
type: Limit
created: 2020-11-23T14:50:43.346Z
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6382
definition: WSW-ENE striking strike-slip fault
definition: WSW-ENE streichende Blattverschiebung. @de
preferred label: Hohenstaufen Störungszone Verwerfung 6 @de
notation: DE-BW_254
notation: geola_048
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Hohenstaufen Fault Zone

Hohenstaufen Fault Zone - Fault 8
type: Fault
type: Limit
definition: W-E streichende Blattverschiebung. @de
type: Concept
created: 2020-11-23T14:50:43.402Z
definition: W-E striking strike-slip fault
notation: DE-BW_256
notation: geola_050
references: https://data.geoscience.earth/ncl/geoera/ref/6382
preferred label: Hohenstaufen Störungszone Verwerfung 8 @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Hohenstaufen Fault Zone

Hohenstaufen Fault Zone - Fault 10
type: Fault
type: Limit
definition: WNW-ESE streichende Blattverschiebung. @de
preferred label: Hohenstaufen Störungszone Verwerfung 10 @de
references: https://data.geoscience.earth/ncl/geoera/ref/6382
notation: DE-BW_258
notation: geola_052
created: 2020-11-23T14:50:43.458Z
definition: WNW-ESE striking strike-slip fault
type: Concept
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Hohenstaufen Fault Zone

Hohenstaufen Fault Zone - Fault 9
type: Fault
type: Limit
definition: WSW-ENE striking strike-slip fault
created: 2020-11-23T14:50:43.430Z
notation: geola_051
type: Concept
definition: WSW-ENE streichende Blattverschiebung. @de
notation: DE-BW_257
references: https://data.geoscience.earth/ncl/geoera/ref/6382
preferred label: Hohenstaufen Störungszone Verwerfung 9 @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Hohenstaufen Fault Zone

Swabian Lineament 2
type: Fault
type: Limit
notation: DE-BW_239
definition: W-E streichende Blattverschiebung. @de
created: 2020-11-23T14:50:43.097Z
preferred label: Schwäbisches Lineament 2 @de
references: https://data.geoscience.earth/ncl/geoera/ref/6382
definition: W-E striking strike-slip fault
notation: geoLa_033
type: Concept
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Swabian Lineament

Swabian Lineament 1
type: Fault
type: Limit
notation: DE-BW_238
definition: W-E striking strike-slip fault
created: 2020-11-23T14:50:43.069Z
preferred label: Schwäbisches Lineament 1 @de
type: Concept
definition: W-E streichende Blattverschiebung. @de
notation: geoLa_032
references: https://data.geoscience.earth/ncl/geoera/ref/6382
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Swabian Lineament

Swabian Lineament 4
type: Fault
type: Limit
definition: WSW-ENE striking strike-slip fault
notation: DE-BW_241
type: Concept
preferred label: Schwäbisches Lineament 4 @de
notation: geoLa_035
created: 2020-11-23T14:50:43.152Z
references: https://data.geoscience.earth/ncl/geoera/ref/6382
definition: WSW-ENE streichende Blattverschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Swabian Lineament

Swabian Lineament 3
type: Fault
type: Limit
preferred label: Schwäbisches Lineament 3 @de
definition: WSW-ENE striking strike-slip fault
type: Concept
created: 2020-11-23T14:50:43.125Z
definition: WSW-ENE streichende Blattverschiebung. @de
notation: geoLa_034
references: https://data.geoscience.earth/ncl/geoera/ref/6382
notation: DE-BW_240
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Swabian Lineament

Riedenburg Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:38.234Z
notation: DE-BY_1333
preferred label: Riedenburg Störung @de
definition: SSW-NNE striking, steeply WNW dipping normal fault featuring a throw of more than 100 m.
definition: SSW-NNE streichende, steil nach WNW einfallende Abschiebung mit einer Sprunghöhe von über 100 m. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4075
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1333
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Erlinghofen Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:37.011Z
notation: DE-BY_1289
preferred label: Erlinghofen Störung @de
definition: North of Erlinghofen WSW-ENE striking, steeply SSE dipping two-step normal fault with a cumulative throw of about 20 m.
definition: Nördlich von Erlinghofen WSW-ENE streichende, steil nach SSE einfallende zweistufige Abschiebung mit einer Gesamtsprunghöhe von etwa 20 m. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4136
references: https://data.geoscience.earth/ncl/geoera/ref/4115
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1289
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Maierleite-Breitenbrunn Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:38.206Z
notation: DE-BY_1332
preferred label: Maierleite-Breitenbrunn Störung @de
definition: W-E striking, steeply S dipping normal fault featuring a throw of up to 25 m.
definition: W-E streichende, steil nach S einfallende Abschiebung mit einem Vertikalversatz von bis zu 25 m. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4145
references: https://data.geoscience.earth/ncl/geoera/ref/4142
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1332
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Fuchsberg Fault
type: Fault
type: Limit
type: SpatialObject
preferred label: Fuchsberg Störung @de
definition: NNW-SSE striking, steeply ENE dipping normal fault east of Titting.
definition: NNW-SSE streichende, steil nach ENE einfallende Abschiebung östlich von Titting. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4115
type: Concept
created: 2020-10-09T11:35:36.984Z
notation: DE-BY_1288
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1288
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Parsberg Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:38.179Z
notation: DE-BY_1331
preferred label: Parsberg Störung @de
definition: SSW-NNE striking, steeply ESE dipping normal fault featuring a throw up to 25 m.
definition: SSW-NNE streichende, steil nach ESE einfallende Abschiebung mit einer Sprunghöhe bis zu 25 m. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4143
references: https://data.geoscience.earth/ncl/geoera/ref/4118
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1331
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Grünschlag-Neuhof Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:38.151Z
notation: DE-BY_1330
preferred label: Grünschlag-Neuhof Störung @de
definition: NW-SE to NNW-SSE trending, vertical to steeply NE to ENE dipping normal fault featuring a throw of up to 30 m.
definition: NW-SE bis NNW-SSE verlaufende, vertikale bis steil nach NE bis ENE einfallende Abschiebung mit einer Sprunghöhe bis 30 m. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4124
sf touches: Mitterbügl Cross Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1330
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Mitterbügl Cross Fault
limit type: obliqueSlipFault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:38.123Z
notation: DE-BY_1329
preferred label: Mitterbügl Querstörung @de
definition: SW-NE trending oblique-slip fault with a small-scale dextral movement, displacing Grünschlag-Neuhof Fault, and a minor vertical movement of less than 10 m.
definition: SW-NE verlaufende Schrägabschiebung mit einer kleinräumigen dextralen Bewegungsrichtung, die die Grünschlag-Neuhof Störung versetzt, und einem Vertikalversatz von weniger als 10 m. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4124
sf touches: Oberbügl-Michelsberg Fault
sf touches: Grünschlag-Neuhof Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1329
broader: Swabian-Franconian Alb fault domain

Ammerfeld-Rohrbach Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4146
sf touches: Eibichel-Treidelheim Fault
type: Concept
created: 2020-10-09T11:35:37.235Z
notation: DE-BY_1297
preferred label: Ammerfeld-Rohrbach Störung @de
definition: NW-SE trending, steeply NE dipping normal fault, southwestern flank of Asbrunner Graben (Streit 1978).
definition: NW-SE streichende, steil nach NE einfallende Abschiebung; südwestliche Begrenzung des Asbrunner Grabens (Streit 1978). @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1297
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Eibichel-Treidelheim Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4154
references: https://data.geoscience.earth/ncl/geoera/ref/4146
sf touches: Ammerfeld-Rohrbach Fault
type: Concept
created: 2020-10-09T11:35:37.207Z
notation: DE-BY_1296
preferred label: Eibichel-Treidelheim Störung @de
definition: NNW-SSE to NW-SE trending, steeply WSW to SW dipping normal fault; in its western section forming the northeastern flank of Asbrunner Graben (Zeiss 1964, Streit 1978).
definition: NNW-SSE bis NW-SE verlaufende, steil nach WSW bis SW einfallende Abschiebung; bildet im westlichen Abschnitt die nordöstliche Begrenzung des Asbrunner Grabens (Zeiss 1964, Streit 1978). @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1296
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Konstein Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4154
references: https://data.geoscience.earth/ncl/geoera/ref/4139
sf touches: Spindeltal-Gammersfeld Fault
definition: Crossing the Wellheim dry valley NW of Konstein, SW-NE striking, approx. 70° NW dipping normal fault featuring a throw up to 60 m.
type: Concept
created: 2020-10-09T11:35:37.179Z
notation: DE-BY_1295
preferred label: Konstein Störung @de
definition: Das Wellheimer Trockental NW von Konstein kreuzende, SW-NE streichende, ca. 70° nach NW fallende Abschiebung mit einer Sprunghöhe bis zu 60 m. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1295
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Spindeltal-Gammersfeld Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:37.151Z
notation: DE-BY_1294
references: https://data.geoscience.earth/ncl/geoera/ref/6372
references: https://data.geoscience.earth/ncl/geoera/ref/4131
references: https://data.geoscience.earth/ncl/geoera/ref/4154
sf touches: Konstein Fault
alternative label: Gammersfelder Sprung @de
alternative label: Gammersfeld-Eulahof Verwerfung @de
preferred label: Spindeltal-Gammersfeld Störung @de
definition: NNW-SSE trending, steeply (85°-60°) WSW dipping normal fault featuring a throw up to 40 m.
definition: NNW-SSE verlaufende, steil (85°-60°) nach WSW einfallende Abschiebung mit einer Sprunghöhe bis zu 40 m. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1294
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Hagenau Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:37.123Z
notation: DE-BY_1293
preferred label: Hagenausprung @de
definition: Predominantly WSW-ENE trending, at its western limb veering to NNW-SSE, steeply (85°-60°) SSE to WSW dipping normal fault featuring a throw of about 10 m, distributed among two fault scarps in the east.
definition: Überwiegend WSW-ENE verlaufende, an ihrem westlichen Ende auf NNW-SSE abbiegende, steil (85°-60°) nach SSE bis WSW einfallende Abschiebung mit einem Verwurf von insgesamt rund 10 m, im Osten aufgeteilt auf zwei Bruchstaffeln. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4138
references: https://data.geoscience.earth/ncl/geoera/ref/4088
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1293
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Schafshill-Neuenhizenhausen Fault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/4075
type: SpatialObject
sf touches: Thannhausen Fault
type: Concept
created: 2020-10-09T11:35:38.345Z
notation: DE-BY_1337
preferred label: Schafshill-Neuenhizenhausen Störung @de
definition: N-S striking, steeply W dipping normal fault featuring a throw of about 50 m.
definition: N-S streichende, steil nach W einfallende Abschiebung mit einer Sprunghöhe um 50 m. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1337
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Schwarzwald-Bayerwald Line
type: Fault
type: Limit
definition: Principal fault zone cutting WSW-ENE to W-E through southern Germany. Multi-phase oblique-slip fault system, in Bavaria traceable only in few predominantly steeply S dipping fault segments in Upper Jurassic subcrops, featuring a throw rarely exceeding 50 m, or as flexures. The main phase of deformation, mainly a dextral movement with a significant vertical component resulting in throws up to 300 m, is assigned to Late Variscan, as inferred from seismic evidence at the edge of Permo-Carboniferous troughs at depth.
definition: Bedeutende Störungszone die sich in WSW-ENE bis W-E Richtung quer durch Süddeutschland verfolgen lässt. Mehrphasiges Schrägabschiebungssystem das in Bayern nur abschnittsweise als überwiegend steil südfallende Störung der jurassischen Oberfläche mit Versätzen von selten über 50 m oder als Flexur nachweisbar ist. Die am Rand permokarbonischer Tröge in der Tiefe geophysikalisch ermittelten Versätze bis zu 300 m implizieren, dass die spätvariszische Hauptbewegungsphase mit überwiegend dextral seitenverschiebendem Bewegungssinn auch eine deutliche Vertikalkomponente umfasste. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6362
references: https://data.geoscience.earth/ncl/geoera/ref/6361
references: https://data.geoscience.earth/ncl/geoera/ref/6393
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/4083
sf touches: Keilberg Fault
sf touches: Danube Fault System
type: Concept
created: 2020-10-09T11:35:36.175Z
notation: DE-BY_1255
alternative label: Schwäbisch-Fränkisches Lineament @de
preferred label: Schwarzwald-Bayerwald-Linie @de
narrower: Deuerling Fault
narrower: Kneiting-Pfaffenstein Fault
narrower: Kareth Step Fault
narrower: Kumpfhof Fault
narrower: Beilngries-Dietfurt Fault
narrower: Töging Fault
narrower: Rumburg-Kinding Fault
narrower: Wachenzell-Altdorf Lineament
narrower: Antoniholz Cross Fault
narrower: Lohrmannshof Fault
narrower: Schambach Fault
narrower: Heumödern-Treuchtlingen Fault
narrower: Schmidsberg-Hahnenberg Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Swabian-Franconian Alb fault domain

Kareth Step Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4073
type: Concept
created: 2020-10-09T11:35:36.259Z
notation: DE-BY_1258
alternative label: Karether Störungszone @de
preferred label: Kareth Bruchstaffel @de
definition: W-E to WNW-ESE trending steeply (85°-60°) S to SSW dipping step fault crossing the Regen river valley immediately north of its junction with Danube river valley. This 3-stepped fault featuring a cumulative throw of less than 20 m is deemed the northernmost branch of the forking western continuation of the Donaurand Fault Scarp [DE-BY_698] (Bauberger et al. 1969).
definition: W-E bis WNW-ESE verlaufende, steil (85°-60°) nach S bis SSW einfallender Staffelbruch der das Regental unmittelbar nördlich der Regen Mündung in die Donau quert. 3-stufiger Abbruch mit einer Gesamtsprunghöhe von unter 20 m, der als nördlichster Zweig der sich verzweigenden Fortsetzung des Donaurandbruchs [DE-BY_698] angesehen wird (Bauberger et al. 1969). @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1258
limit type: normalFault
broader: Schwarzwald-Bayerwald Line

Kneiting-Pfaffenstein Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4073
sf touches: Deuerling Fault
type: Concept
created: 2020-10-09T11:35:36.231Z
notation: DE-BY_1257
preferred label: Kneiting-Pfaffenstein Störung @de
definition: W-E trending, steeply (85°-60°) S dipping normal fault subcropping between Kneiting and mouth of Regen river. Subordinate (northern) branch of western continuation of Donaurand Fault Scarp [DE-BY_698], assigned to Schwarzwald-Bayerwald-Line.
definition: W-E verlaufende, steil (85°-60°) nach S einfallende Abschiebung zwischen Kneiting und der Regen Mündung. Subordinate (nördlicher) Zweig der westlichen Fortsetzung des Donaurandbruchs [DE-BY_698], die der Schwarzwald-Bayerwald-Linie zugerechnet wird. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1257
limit type: normalFault
broader: Schwarzwald-Bayerwald Line

Deuerling Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/6372
references: https://data.geoscience.earth/ncl/geoera/ref/4073
sf touches: Keilberg Fault
sf touches: Donaurand Fault Scarp
sf touches: Kühschlag-Nittendorf Fault
type: Concept
created: 2020-10-09T11:35:36.203Z
notation: DE-BY_1256
alternative label: Deuerlinger Störung @de
preferred label: Deuerling Störung @de
definition: W-E trending, approx. 70° S dipping normal fault with a throw up to 80 m. Subcropping between Hohenschambach and Tegernheim in parts as a step fault in two subparallel branches. Main (southern) branch of western continuation of Donaurand Fault Scarp [DE-BY_698]. Assigned to Schwarzwald-Bayerwald-Line and part of Regensburg Confluence in the sense of Schwarz (2012).
definition: W-E verlaufende, ca. 70° nach S einfallende Abschiebung, streckenweise als zweistufiger Staffelbruch, mit einer kumulativen Sprunghöhe bis zu 80 m. Nur teilweise aufgeschlossene Störung zwischen Hohenschambach und Tegernheim als Hauptast der westlichen Fortsetzung des Donaurandbruchs [DE-BY_698]. Teil der Regensburger Konfluenz im Sinne von Schwarz (2012), die der Schwarzwald-Bayerwald Linie zugeschrieben wird. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1256
limit type: normalFault
broader: Schwarzwald-Bayerwald Line

Wachenzell-Altdorf Lineament
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/6372
references: https://data.geoscience.earth/ncl/geoera/ref/4085
references: https://data.geoscience.earth/ncl/geoera/ref/4115
sf touches: Antoniholz Cross Fault
type: Concept
created: 2020-10-09T11:35:36.481Z
notation: DE-BY_1275
alternative label: Altdorfer Flexur @de
definition: This striking lineament along "Blaubrunnental" dry valley implies that at least certain segments of the "Altdorfer Flexur" (Freyberg 1969), as inferred from narrowing intervals of Upper Jurassic contour lines, have been deformed by brittle tectonics.
definition: Das auffällige Lineament entlang des Blaubrunnentals impliziert, dass zumindest einige Abschnitte der "Altdorfer Flexur" (Freyberg 1969), abgeleitet aus dem Zusammenrücken der Streichlinien, einer bruchhaften Verformung unterlagen. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Schwarzwald-Bayerwald Line

Rumburg-Kinding Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4135
references: https://data.geoscience.earth/ncl/geoera/ref/4141
sf touches: Schellenburg Horsts Scarps
type: Concept
created: 2020-10-09T11:35:36.453Z
notation: DE-BY_1274
preferred label: Rumburg-Kinding Störung @de
definition: SW-NE trending, steeply SE dipping normal fault with a minor throw passing into a WSW-ENE trending flexure to the west ("Altdorfer Flexur" [DE-BY_1275]).
definition: SW-NE verlaufende, steil nach SE einfallende Abschiebung mit geringer Sprunghöhe, die nach Westen hin in eine WSW-ENE verlaufende Flexur übergeht ("Altdorfer Flexur" [DE-BY_1275]). @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1274
limit type: normalFault
broader: Schwarzwald-Bayerwald Line

Töging Fault
type: Limit
type: Fault
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4142
references: https://data.geoscience.earth/ncl/geoera/ref/4145
type: Concept
created: 2020-10-09T11:35:36.425Z
notation: DE-BY_1273
preferred label: Töging Störung @de
definition: Running southerly parallel to Ottmaring Fault [DE-BY_1270], W-E striking, steeply S dipping normal fault featuring a throw of up to 20 m. Assumedly a section of a suppositious southern offset of Schwarzwald-Bayerwald Line [DE-BY_1255] continuing in Mühlbach Fault [DE-BY_1271] and Kumpfhof Fault [DE-BY_1269] to the east.
definition: Südlich parallel zur Ottmaring Störung [DE-BY_1270] verlaufende, W-E streichende, steil nach S einfallende Abschiebung mit einer Sprunghöhe bis zu 20 m. Vermutlich Teil des hypothetischen Süd-Astes der Schwarzwald-Bayerwald Linie [DE-BY_1255] der sich nach Osten hin in den Mühlbach [DE-BY_1271] and Kumpfhof [DE-BY_1269]] Störungen fortsetzt. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1273
limit type: normalFault
broader: Schwarzwald-Bayerwald Line

Schmidsberg-Hahnenberg Fault
type: Fault
type: Limit
type: SpatialObject
narrower: Stahlmühle Subfault
references: https://data.geoscience.earth/ncl/geoera/ref/4100
references: https://data.geoscience.earth/ncl/geoera/ref/4101
type: Concept
created: 2020-10-09T11:35:36.704Z
notation: DE-BY_1278
preferred label: Schmidsberg-Hahnenberg Störung @de
definition: Crossing Rohrach river valley, W-E trending, steeply S dipping normal fault emerging from the Ries Impact ejecta masses in the west.
definition: Das Rohrachtal querende, W-E verlaufende, steil nach S einfallende Abschiebung, die sich östlich der Ries-Trümmermassen verfolgen lässt. @de
narrower: Schlossberg Subfault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1278
limit type: normalFault
broader: Schwarzwald-Bayerwald Line

Schlossberg Subfault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:36.760Z
notation: DE-BY_1280
preferred label: Schloßberg Nebenstörung @de
definition: W-E striking branch of Schmidsberg-Hahnenberg Fault running parallel north of the main fault.
definition: W-E streichende nördlich parallel zur Schmidsberg-Hahnenberg Störung verlaufender Seitenast. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1280
broader: Schmidsberg-Hahnenberg Fault

Stahlmühle Subfault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:36.732Z
notation: DE-BY_1279
preferred label: Stahlmühle Zweigstörung @de
definition: WSW-ENE striking side branch of Schmidsberg-Hahnenberg Fault.
definition: WSW-ENE streichender Seitenast der Schmidsberg-Hahnenberg Störung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1279
broader: Schmidsberg-Hahnenberg Fault

Beilngries-Dietfurt Fault
type: Fault
type: Limit
definition: Nur selten zu Tage tretender Abschnitt der Schwarzwald-Bayerwald-Linie zwischen Beilngries und östlich von Dietfurt. WNW-ESE verlaufende, ± saigere bis steil SSE oder NNW einfallende Abschiebung mit einer Sprunghöhe von etwa 40 m. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4142
references: https://data.geoscience.earth/ncl/geoera/ref/4145
references: https://data.geoscience.earth/ncl/geoera/ref/4134
sf touches: Hellafelsen Querstörung
type: Concept
created: 2020-10-09T11:35:36.314Z
notation: DE-BY_1259
alternative label: Beilngrieser Verwerfung @de
preferred label: Beilngries-Dietfurt Störung @de
definition: Largely subcropping segment of Schwarzwald-Bayerwald-Line running from Beilngries to the east of Dietfurt. WNW-ESE trending ± vertical to steeply SSE or NNW dipping normal fault featuring a throw of about 40 m.
narrower: Ottmaring Fault
narrower: Mühlbach Störung
narrower: Hellafelsen Querstörung
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1259
limit type: normalFault
broader: Schwarzwald-Bayerwald Line

Hellafelsen Querstörung
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:36.398Z
notation: DE-BY_1272
definition: SW-NE striking, steeply NW dipping link of Ottmaring Fault [DE-BY_1270] and Beilngries-Dietfurt Fault [DE-BY_1259].
definition: SW-NE streichende, steil nach NW einfallende Verbindung von Ottmaring [DE-BY_1270] und Beilngries-Dietfurt [DE-BY_1259] Störung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1272
broader: Beilngries-Dietfurt Fault

Mühlbach Störung
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:36.370Z
notation: DE-BY_1271
definition: NW-SE striking, turning to a W-E strike, steeply NE to N dipping normal fault with a throw of up to 30 m. The fault's southern, W-E striking part assumedly is a section of the suppositious southern offset of Schwarzwald-Bayerwald Line [DE-BY_1255] continuing in Kumpfhof Fault [DE-BY_1269] to the east and Töging Fault [DE-BY_1273] to the west.
definition: NW-SE streichende, im Süden nach W-E umbiegende, steil nach NE bis N einfallende Abschiebung mit einer Sprunghöhe von bis zu 30 m. Der südliche, W-E streichende Abschnitt der Störung ist vermutlich Teil des hypothetischen Süd-Astes der Schwarzwald-Bayerwald Linie [DE-BY_1255] der sich nach Osten hin in der Kumpfhof Störung [DE-BY_1269], nach Westen hin in der Töging Störung [DE-BY_1273] Störungen fortsetzt. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1271
limit type: normalFault
broader: Beilngries-Dietfurt Fault

Ottmaring Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4145
sf touches: Mühlbach Störung
type: Concept
created: 2020-10-09T11:35:36.342Z
notation: DE-BY_1270
preferred label: Ottmaring Störung @de
definition: Southerly subparallel to Beilngries-Dietfurt Fault [DE-BY_1259] WNW-ESE trending, steeply SSE dipping normal fault featuring a throw of less than 20 m.
definition: Südlich subparallel zur Beilngries-Dietfurt Störung [DE-BY_1259] WNW-ESE verlaufende, steil nach SSE einfallende Abschiebung mit einem Vertikalversatz von höchstens 20 m. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1270
limit type: normalFault
broader: Beilngries-Dietfurt Fault

Kumpfhof Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4145
type: Concept
created: 2020-10-09T11:35:36.287Z
notation: DE-BY_1269
preferred label: Kumpfhof Störung @de
definition: W-E trending, steeply N dipping normal fault with a throw of up to 25 m, running southerly parallel to the inferred trend of Schwarzwald-Bayerwald Line [DE-BY_1255]. Assumedly part of a hypothetic southern offset of that suture continuing in Mühlbach Fault [DE-BY_1271] and Töging Fault [DE-BY_1273] to the west.
definition: W-E verlaufende, steil nach N einfallende Abschiebung mit einer Sprunghöhe bis zu 25 m, südlich parallel zum vermuteten Verlauf der Schwarzwald-Bayerwald Line [DE-BY_1255] als mutmaßlicher Abschnitt eines hypothetischen südlichen Seitenasts dieser Sutur, der auch die Mühlbach Störung Fault [DE-BY_1271] und Töging Störung [DE-BY_1273] im Westen umfasst. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1269
limit type: normalFault
broader: Schwarzwald-Bayerwald Line

Heumödern-Treuchtlingen Fault
type: Fault
type: Limit
narrower: Treuchtlingen Subfault
narrower: Heumödern-Dietfurt Fault
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4133
references: https://data.geoscience.earth/ncl/geoera/ref/4125
type: Concept
created: 2020-10-09T11:35:36.620Z
notation: DE-BY_1262
preferred label: Heumödern-Treuchtlingen Störung @de
definition: WSW-ENE to W-E striking, approx. 70° ± S dipping normal fault featuring an approx. 100 m throw in the west and 30 m in the east. Assigned to Schwarzwald-Bayerwald-Line; main-branch of the Treuchtlingen Confluence in the sense of Schwarz (2012), continuing in Schambach Fault [DE-BY_1261] to the east.
definition: Von WSW-ENE auf W-E Streichen abknickende, ca. 70° nach ± S einfallende Abschiebung mit einer Sprunghöhe von etwa 100 m im Westen und ca. 30 m im Osten, die der Schwarzwald-Bayerwald Linie zugerechnet wird. Hauptast der Treuchtlinger Konfluenz im Sinne von Schwarz (2012). Setzt sich jenseits der Treuchtlinger Talspinne in der Schambach Störung [DE-BY_1261] fort. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1262
limit type: normalFault
broader: Schwarzwald-Bayerwald Line

Heumödern-Dietfurt Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4133
type: Concept
created: 2020-10-09T11:35:36.676Z
notation: DE-BY_1264
preferred label: Heumödern-Dietfurt Störung @de
definition: Undulate, NW-SE to WNW-ESE trending normal fault branching off Heumödern-Treuchtlingen Fault to the southeast and in following Heumödern valley in large parts. Side-branch of the Treuchtlingen Confluence in the sense of Schwarz (2012).
definition: Gewellt NW-SE bis WNW-ESE verlaufende Abschiebung mit einer Sprunghöhe bis über 60 m. Von der Heumödern-Treuchtlingen Störung nach SE abzweigender, dem Heumöderntal folgender Nebenast der Treuchtlinger Konfluenz im Sinne von Schwarz (2012). @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1264
limit type: normalFault
broader: Heumödern-Treuchtlingen Fault

Treuchtlingen Subfault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4133
references: https://data.geoscience.earth/ncl/geoera/ref/4125
type: Concept
created: 2020-10-09T11:35:36.648Z
notation: DE-BY_1263
preferred label: Treuchtlingen Zweigstörung @de
definition: NW-SE trending, steeply SW dipping normal fault featuring a throw up to 20 m, southeastwardly branching off Heumödern-Treuchtlingen Fault [DE-BY_1262]. Side-branch of the Treuchtlingen Confluence in the sense of Schwarz (2012).
definition: NW-SE verlaufende, steil nach SW einfallende Abschiebung mit einer Sprunghöhe von bis zu 20 m. Von der Heumödern-Treuchtlingen Störung [DE-BY_1262] südostwärts abzweigender Nebenast der Treuchtlinger Konfluenz im Sinne von Schwarz (2012). @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1263
limit type: normalFault
broader: Heumödern-Treuchtlingen Fault

Schambach Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4133
type: Concept
created: 2020-10-09T11:35:36.592Z
notation: DE-BY_1261
preferred label: Schambach Störung @de
definition: Undulate, overall W-E striking, approx. 70° S dipping normal fault featuring an approx. 30 m throw, assigned to Schwarzwald-Bayerwald-Line. Eastern continuation of Heumödern-Treuchtlingen Fault [DE-BY_1262].
definition: Gewellt, insgesamt W-E streichende, ca. 70° nach S einfallende Abschiebung mit einer Sprunghöhe von etwa 30 m die der Schwarzwald-Bayerwald Linie zugerechnet wird. Östliche Fortsetzung der Heumödern-Treuchtlingen Störung [DE-BY_1262]. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1261
limit type: normalFault
broader: Schwarzwald-Bayerwald Line

Lohrmannshof Fault
type: Fault
type: Limit
narrower: Lohrmannshof Subfault
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/6372
references: https://data.geoscience.earth/ncl/geoera/ref/4137
type: Concept
created: 2020-10-09T11:35:36.537Z
notation: DE-BY_1260
preferred label: Lohrmannshof Störung @de
definition: Largely subcropping, W-E trending fault assigned to Schwarzwald-Bayerwald Line. Inferred from westward adjoining segments, Schmidt-Kaler (1990) assumes an approx. 70° S dipping normal fault with a throw of about 30 m, passing over into a flexure to the east (Schwarz 2012, "Altdorfer Flexur" after Freyberg 1969).
definition: W-E verlaufende, nur selten aufgeschlossene Störungslinie die der Schwarzwald-Bayerwald Linie zugerechnet wird. Aus den Verhältnissen in westlich benachbarten Abschnitten wird eine 70° nach S einfallende Abschiebung mit einer Sprunghöhe um 30 m angenommen (Schmidt-Kaler 1990), die nach Osten hin in eine Flexur übergeht (Schwarz 2012, "Altdorfer Flexur" nach Freyberg 1969). @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1260
limit type: normalFault
broader: Schwarzwald-Bayerwald Line

Lohrmannshof Subfault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4137
type: Concept
created: 2020-10-09T11:35:36.565Z
notation: DE-BY_1277
preferred label: Lohrmannshof Zweigstörung @de
definition: NW-SE striking side branch of Lohrmannshof Fault, formed by a steeply SW dipping normal fault.
definition: NW-SE streichender Abzweig der Lohrmannshof Störung, der eine steil nach SW einfallende Abschiebung bildet. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1277
limit type: normalFault
broader: Lohrmannshof Fault

Antoniholz Cross Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4115
sf touches: Wachenzell-Altdorf Lineament
type: Concept
created: 2020-10-09T11:35:36.509Z
notation: DE-BY_1276
preferred label: Antoniholz Querstörung @de
definition: NW-SE trending, steeply SW dipping normal fault crossing Wachenzell-Altdorf Lineament with a NE dipping side branch branching off SE of that lineament.
definition: Das Wachenzell-Altdorf Lineament kreuzende, NW-SE verlaufende, steil nach SW einfallende Abschiebung mit einem NE fallenden Seitenast südwestlich des Lineaments. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1276
limit type: normalFault
broader: Schwarzwald-Bayerwald Line

Mödingen Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4089
references: https://data.geoscience.earth/ncl/geoera/ref/4105
sf touches: Riedheim-Wittislingen Fault
sf touches: Langenau-Wittislingen Fault
sf touches: Wittislingen-Lutzingen Fault
type: Concept
created: 2020-10-09T11:35:36.148Z
notation: DE-BY_1254
preferred label: Mödinger Abbruch @de
definition: Emerging from Riedheim-Wittislingen Fault [DE-BY_1250], SW-NE trending, steeply (85°-60°) SE dipping normal fault featuring a throw of approx. 50 m.
definition: Fortsetzung der Riedheim-Wittislingen Störung [DE-BY_1250], SW-NW streichende, steil (85°-60°) nach SE einfallende Abschiebung mit einer Sprunghöhe von ca. 50 m. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1254
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Lenting-Hepberg Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/6372
references: https://data.geoscience.earth/ncl/geoera/ref/4141
sf touches: Hepberg Cross Fault
type: Concept
created: 2020-10-09T11:35:37.403Z
notation: DE-BY_1303
preferred label: Lenting-Hepberg Störung @de
definition: Conjugate pair of SSW-NNE striking normal faults, an ESE dipping western branch and a WNW dipping eastern branch, both featuring a throw of up to 12 m, thereby forming a local graben structure truncated by Hepberg Cross Fault [DE-BY_ DE-BY_1304] in the north.
definition: Konjugiertes Paar SSW-NNE streichender Abschiebungen, die mit einem nach ESE einfallenden West-Ast und einem nach WNE einfallenden Ost-Ast, bei einem vertikalen Versatz von bis zu 12 m, eine lokale, von der Hepberg Querstörung [DE-BY_DE-BY_1304] im Norden abgeschnittene Grabenstruktur begrenzen. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1303
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Bittenbrunn-Sehensand Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/4146
type: Concept
created: 2020-10-09T11:35:37.375Z
notation: DE-BY_1302
preferred label: Bittenbrunn-Sehensand Störung @de
definition: Eastward arcuate overall N-S trending, steeply W dipping normal fault transecting the Neuburg Jurassic Spur across the Danube river valley.
definition: Ostwärts gebogen, insgesamt N-S verlaufende, steil nach W einfallende Abschiebung, die den Neuburger Jurasporn über das Donautal hinweg durchschneidet. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1302
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Pfaffengrund Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4146
type: Concept
created: 2020-10-09T11:35:37.347Z
notation: DE-BY_1301
preferred label: Pfaffengrunder Querbruch @de
definition: W-E trending, steeply S dipping normal fault, probably displacing the southern continuation of the Bergen Fault [DE-BY_1300] as Bittenbrunn-Sehensand Fault [DE-BY_1302] to the west.
definition: W-E verlaufende, steil nach S einfallende Abschiebung, die wahrscheinlich die südliche Fortsetzung der Bergener Verwerfung [DE-BY_1300] als Bittenbrunn-Sehensand Störung [DE-BY_1302] nach Westen hin versetzt. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1301
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Bergen Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4146
type: Concept
created: 2020-10-09T11:35:37.319Z
notation: DE-BY_1300
preferred label: Bergener Verwerfung @de
definition: NW-SE to NNW-SSE trending, steeply SW to WSW dipping normal fault, possibly continuing in the Bittenbrunn-Sehensand Fault [DE-BY_1302] displaced to the west by the Pfaffengrund Fault [DE-BY_1301].
definition: NW-SE bis NNW-SSE verlaufende, steil nach SW bis WSW einfallende Abschiebung, die sich nach Süden hin, durch den Pfaffengrunder Querbruch [DE-BY_1301] nach Westen versetzt, möglicherweise in der Bittenbrunn-Sehensand Fault [DE-BY_1302] fortsetzt. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1300
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Hainberg-Gietlhausen Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4146
definition: Arcuate NW-SE to WNW-ESE trending, steeply SW dipping normal fault featuring a throw of up to 50 m.
type: Concept
created: 2020-10-09T11:35:37.291Z
notation: DE-BY_1299
preferred label: Hainberg-Gietlhausen Störung @de
definition: Gebogen NW-SE bis WNW-ESE verlaufende, steil nach SW einfallende Abschiebung mit einer Sprunghöhe von bis zu 50 m. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1299
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Frauenholz-Hainberg Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4146
definition: Slightly undulate NW-SE trending, steeply SW dipping normal fault featuring a throw of up to 80 m.
type: Concept
created: 2020-10-09T11:35:37.263Z
notation: DE-BY_1298
preferred label: Frauenholz-Hainberg Störung @de
definition: Leicht gewellt NW-SE verlaufende, steil nach SW einfallende Abschiebung mit einer Sprunghöhe bis zu 80 m. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1298
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Theissing-Dünzing Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/6372
references: https://data.geoscience.earth/ncl/geoera/ref/4121
type: Concept
created: 2020-10-09T11:35:37.515Z
notation: DE-BY_1307
alternative label: Theißing-Dünzinger Störung @de
preferred label: Theißing-Dünzing Störung @de
definition: NNW-SSE striking, WSW dipping normal fault with a throw of up to 40 m, inferred from Upper Jurassic contour line pattern.
definition: NNW-SSE streichende, nach WSW einfallende Abschiebung mit einer Sprunghöhe bis zu 40 m, abgeleitet aus dem Streichlinienmuster im Malm. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1307
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Demling-Vohburg Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:37.487Z
notation: DE-BY_1306
preferred label: Demling-Vohburg Störung @de
definition: NNW-SSE striking, WSW dipping normal fault subcropping between Demling and Auhöfe; its continuation as a blind fault underneath the Molasse sediments to S of Vohburg is assumed.
definition: NNW-SSE streichende, nach WSW einfallende Abschiebung, die Zwischen Demling und Auhöfe nur selten aufgeschlossen ist und sich unter Molasse-Überdeckung wahrscheinlich bis S Vohburg fortsetzt. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1306
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Kösching-Bettbrunn Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/6372
type: Concept
created: 2020-10-09T11:35:37.458Z
notation: DE-BY_1305
alternative label: Kösching-Bettbrunner Störung @de
preferred label: Kösching-Bettbrunn Störung @de
definition: SSW-NNE striking, steeply WNW dipping normal fault featuring a throw of more than 30 m in its middle segment.
definition: SSW-NNE streichende, steil nach WNW einfallende Abschiebung mit einer Sprunghöhe bis über 30 m im mittleren Abschnitt. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1305
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Hepberg Cross Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/6372
references: https://data.geoscience.earth/ncl/geoera/ref/4141
sf touches: Lenting-Hepberg Fault
type: Concept
created: 2020-10-09T11:35:37.430Z
notation: DE-BY_1304
preferred label: Hepberg Querstörung @de
definition: W-E striking, steeply N dipping normal fault with a throw up to 15 m and truncating the western branch of Lenting-Hepberg Fault [DE-BY_ DE-BY_1303].
definition: W-E streichende, steil nach N einfallende Abschiebung mit einer Sprunghöhe bis zu 15 m. Nördliche Begrenzung der von der Lenting-Hepberg Störung [DE-BY_DE-BY_1303] gebildeten Grabenstruktur. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1304
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Ries Crater Rim
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6363
type: Concept
created: 2020-10-29T14:56:29.204Z
type: SpatialObject
preferred label: Ries Kraterrand @de
notation: DE-BY_1342
alternative label: Struktureller Kraterrand @de
definition: This most striking structural feature of the Swabian-Franconian Alb, overlapping its northern escarpment at the border of Baden-Württemberg and Bavaria, is atectonic: the almost circular outer rim of the Ries crater formed by an asteroid impact about 14.6 million years ago in the Miocene, leaving a rampart crater of 24 km in diameter. The Ries outer rim is formed by a concentric array of blind listric faults (concave curved normal faults) resulting from slumping of mega-blocks when the over-steep impact crater flanks collapsed.
definition: Die auffälligste Struktur der Schwäbisch-Fränkischen Alb, die im Grenzgebiet zwischen Schwäbischer und Fränkischer Alb den Albtrauf großflächig überdeckt, ist atektonisch: der annähernd kreisrunde Kraterrand des Ries Asteroiden-Einschlagskraters, entstanden vor rund 14,6 Millionen Jahren im Miozän mit einem Durchmesser von rund 24 km. Der Ries Kraterrand wird von überdeckten, konzentrischen listrischen (konkav gebogenen) Abschiebungen aufgebaut, die durch Groß-Rutschungen (parautochthone Schollen) beim Kollaps der übersteilten Einschlagskraterwände entstanden. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4810
references: https://data.geoscience.earth/ncl/geoera/ref/4811
references: https://data.geoscience.earth/ncl/geoera/ref/4812
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Swabian-Franconian Alb fault domain

Eger Valley Line 1
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6369
notation: geola_003
created: 2020-11-23T14:50:43.571Z
definition: WNW-ESE striking strike-slip fault
definition: WNW-ESE streichende Blattverschiebung. @de
notation: DE-BW_199
references: https://data.geoscience.earth/ncl/geoera/ref/6382
preferred label: Egertallinie 1 @de
type: Concept
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Swabian-Franconian Alb fault domain

[geola_002]
type: Fault
type: Limit
created: 2020-11-23T14:50:43.543Z
notation: geola_002
definition: W-E striking strike-slip fault
notation: DE-BW_198
type: Concept
definition: W-E streichende Blattverschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6382
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Swabian-Franconian Alb fault domain

Eger Valley Line 3
type: Fault
type: Limit
definition: NW-SE striking strike-slip fault
references: https://data.geoscience.earth/ncl/geoera/ref/6369
notation: geola_005
references: https://data.geoscience.earth/ncl/geoera/ref/6382
preferred label: Egertallinie 3 @de
created: 2020-11-23T14:50:43.627Z
notation: DE-BW_201
definition: NW-SE streichende Blattverschiebung. @de
type: Concept
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Swabian-Franconian Alb fault domain

Eger Valley Line 2
type: Fault
type: Limit
notation: geola_004
created: 2020-11-23T14:50:43.600Z
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6369
definition: WNW-ESE striking strike-slip fault
preferred label: Egertallinie 2 @de
definition: WNW-ESE streichende Blattverschiebung. @de
notation: DE-BW_200
references: https://data.geoscience.earth/ncl/geoera/ref/6382
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Swabian-Franconian Alb fault domain

Ipf North-South Fault
type: Limit
type: Fault
references: https://data.geoscience.earth/ncl/geoera/ref/6382
definition: N-S striking normal fault, dipping W with unknown angle
definition: N-S streichende, nach W einfallende Abschiebung mit unbekanntem Einfallswinkel. @de
notation: DE-BW_203
type: Concept
notation: geola_007
created: 2020-11-23T14:50:43.655Z
narrower: Ipf North-South Subfault
preferred label: Ipf-Nord-Süd-Sprung @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Swabian-Franconian Alb fault domain

Ipf North-South Subfault
type: Fault
type: Limit
definition: NNW-SSE striking normal fault, dipping WSW with unknown angle
definition: NNW-SSE streichende, nach WSW einfallende Abschiebung mit unbekanntem Einfallswinkel. @de
notation: DE-BW_202
references: https://data.geoscience.earth/ncl/geoera/ref/6382
preferred label: Nebenstörung Ipf-Nord-Süd-Sprung @de
notation: geola_006
type: Concept
created: 2020-11-23T14:50:43.683Z
references: https://data.geoscience.earth/ncl/geoera/ref/6361
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Ipf North-South Fault

Viehhausen-Bergmatting Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4129
type: Concept
created: 2020-10-09T11:35:37.708Z
notation: DE-BY_1314
alternative label: Viehausener Verwerfung @de
preferred label: Viehhausen-Bergmatting Störung @de
definition: NW-SE striking, ± vertical normal fault with a throw up to 10 m.
definition: NW-SE streichende, ± vertikale Abschiebung mit einer Sprunghöhe von bis zu 10 m. @de
narrower: Bergmatting-Lohstadt Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1314
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Bergmatting-Lohstadt Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4129
type: Concept
created: 2020-10-09T11:35:37.735Z
notation: DE-BY_1315
preferred label: Bergmatting-Lohstadt Störung @de
definition: N-S striking branch of Viehhausen-Bergmatting Fault. Vertical to steepy E dipping normal fault feauring a throw up to more than 20 m.
definition: N-S streichender Zweig der Viehhausen-Bergmatting Störung. Saigere bis steil ostfallende Abschiebung mit einem Vertikalversatz bis über 20 m. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1315
limit type: normalFault
broader: Viehhausen-Bergmatting Fault

Saxberg-Lohstadt Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4129
sf touches: Palmberg-Dachsberg Fault
type: Concept
created: 2020-10-09T11:35:37.680Z
notation: DE-BY_1313
preferred label: Saxberg-Lohstadt Störung @de
definition: Southwestward arcuate, NNW-SSE to WNW-ESE trending along Kunzwies Valley, vertical to steeply ± SW dipping normal fault with a 20 m throw.
definition: Südwestwärts gebogen NNW-SSE bis WNW-ESE entlang des Kunzwiestals verlaufende, vertikal bis steil südfallende Abschiebung mit einem Vertikalversatz von bis zu 20 m. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1313
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Palmberg-Dachsberg Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4075
references: https://data.geoscience.earth/ncl/geoera/ref/4129
sf touches: Saxberg-Lohstadt Fault
type: Concept
created: 2020-10-09T11:35:37.652Z
notation: DE-BY_1312
alternative label: Palmberger Verwerfung @de
alternative label: Dachsberg-Verwerfung @de
preferred label: Palmberg-Dachsberg Störung @de
definition: Undulate, overall W-E trending, in sections branching out into small-scale faults and/or displaced by lateral faults, vertical to steepy S to SW dipping normal fault running from NE of Essing to NW of Kapfelberg. In the west, "Palmberg Fault" features a throw of up to 40 m, in its eastern leg (Dachsberg Fault), up to 60 m.
definition: Von Riedhof NE Essing bis zum Dachsberg NW Kapfelberg gewellt, insgesamt W-E verlaufende Störung, abschnittweise zu Kleinststörungen aufgefiedert und/oder durch Querstörungen versetzt. Vertikale bis steil süd- bis südwestfallende Abschiebung mit Sprunghöhen im Westen von bis 40 m (Palmberger Verwerfung), im Osten bis 60 m (Dachsberg-Verwerfung). @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1312
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Weltenburg-Mitterfecking Fault Swarm
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4129
type: Concept
created: 2020-10-09T11:35:37.625Z
notation: DE-BY_1311
preferred label: Weltenburg-Mitterfecking Störungsschar @de
definition: Array of WNW-ESE to NW-SE trending small-scale normal faults south to southeast of Kelheim, possibly portions of a branching on-strike continuation of blind Schierling Fault [DE-BY_752].
definition: Abfolge WNW-ESE bis NW-SE verlaufender Kleinabschiebungen südlich bis südöstlich von Kelheim. Möglicherweise Segmente einer aufgefiederten Fortsetzung im Streichen der überdeckten Schierling Störung [DE-BY_752]. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1311
broader: Swabian-Franconian Alb fault domain

Schwabner Berg Fault
type: Limit
type: Fault
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4132
type: Concept
created: 2020-10-09T11:35:37.597Z
notation: DE-BY_1310
preferred label: Schwabner Berg Störung @de
definition: Slightly kinked WNW-ESE trending, steeply (85°-60°) SSW dipping normal fault with a throw up to 20 m, across the Danube River north of Hienheim.
definition: Leicht geknickt WNW-ESE verlaufende, steil (85°-60°) nach SSW einfallende Abschiebung mit einer Sprunghöhe von bis zu 20 m; quert das Donautal nördlich von Hienheim. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1310
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Abusina-Sandharlanden Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4132
type: Concept
created: 2020-10-09T11:35:37.570Z
notation: DE-BY_1309
preferred label: Abusina-Sandharlanden Störung @de
definition: WNW-ESE striking, steeply (85°-60°) SSW dipping normal fault with a throw up to 20 m running from the Roman fort ruins of Abusina S of Eining to Sandharlanden. The (subthermal) water supply of the Roman thermae at Abusina seems to be a manifestation of this fault. The on-strike continuation across the Danube River is inferred from the straight-lined dry valley Hochtal west of the Danube.
definition: WNW-ESE streichende, steil (85°-60°) nach SSW einfallende Abschiebung mit einer Sprunghöhe von bis zu 20 m zwischen dem Römerkastell Abusina S von Eining und Sandharlanden. Die subthermale Wasserversorgung der römischen Therme Abusina steht wahrscheinlich im Zusammenhang mit dieser Störung, deren westliche Verlängerung aus dem im Streichen geradlinigen Verlauf eines Trockentals jenseits der Donau abgeleitet wurde. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1309
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Lauchert Graben
type: Fault
type: Limit
narrower: Lauchertgraben Fault 2
notation: DE-BW_910
definition: The Lauchert Graben, between Veringenstadt and the ruins of Hertenstein, clearly recognizable as a morphological deepening, is a Rhenish striking (N-S), Miocene-Pliocene tectonic graben about eleven kilometers long, with a maximum throw of the visible trench shoulder of 100 m today. Its continuation to the south and north is morphologically not recognizable but evideced by seismic surveys.
created: 2020-11-23T14:50:44.688Z
definition: Der Lauchertgraben ist ein zwischen Veringenstadt und der Ruine Hertenstein als morphologische Eintiefung deutlich erkennbarer, rund elf Kilometer langer rheinisch (N-S) streichender, miozän-pliozäner tektonischer Graben, mit einer maximalen Sprunghöhe der sichtbaren Grabenschulter von heute 100 m. Seine Fortsetzung nach Süden und Norden ist morphologisch nicht erkennbar, aber durch seismische Messungen nachgewiesen. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6382
references: https://data.geoscience.earth/ncl/geoera/ref/6360
preferred label: Lauchertgraben @de
narrower: Lauchertgraben Fault 4
narrower: Lauchertgraben Fault 3
narrower: Lauchertgraben Fault 5
narrower: Lauchertgraben Fault 6
references: https://data.geoscience.earth/ncl/geoera/ref/6389
type: Concept
narrower: Lauchertgraben Fault 1
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Swabian-Franconian Alb fault domain

Lauchertgraben Fault 2
type: Fault
type: Limit
definition: N-S streichende, nach W einfallende Abschiebung mit unbekanntem Einfallswinkel; Südicher Abschnitt der Östlichen Randstörung des Lauchertgrabens @de
definition: N-S striking normal fault, dipping W with unknown angle; southern part of the eastern boundary of the Lauchertgraben.
references: https://data.geoscience.earth/ncl/geoera/ref/6382
notation: geola_016
created: 2020-11-23T14:50:44.743Z
notation: DE-BW_218
type: Concept
preferred label: Lauchertgraben Störung 2 @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lauchert Graben

Lauchertgraben Fault 1
type: Fault
type: Limit
definition: N-S striking normal fault, dipping E with unknown angle; western boundary of the Lauchertgraben.
type: Concept
notation: geola_015
notation: DE-BW_217
definition: N-S streichende, nach E einfallende Abschiebung mit unbekanntem Einfallswinkel, westliche Randstörung des Lauchertgrabens. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6382
created: 2020-11-23T14:50:44.715Z
preferred label: Lauchertgraben Störung 1 @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lauchert Graben

Lauchertgraben Fault 4
type: Fault
type: Limit
created: 2020-11-23T14:50:44.798Z
type: Concept
definition: SSW-NNE striking normal fault, dipping WNW with unknown angle; northern part of the the eastern boundary of the Lauchertgraben.
references: https://data.geoscience.earth/ncl/geoera/ref/6382
notation: geola_018
notation: DE-BW_220
definition: SSW-NNE streichende, nach WNW einfallende Abschiebung mit unbekanntem Einfallswinkel; nördlicher Abschnitt der östlichen Randstörung des Lauchertgrabens. @de
preferred label: Lauchertgraben Störung 4 @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lauchert Graben

Lauchertgraben Fault 3
type: Fault
type: Limit
definition: SSW-NNE streichende, nach WNW einfallende Abschiebung mit unbekanntem Einfallswinkel; östliche Randstörung des Lauchertgrabens. @de
type: Concept
notation: geola_017
notation: DE-BW_219
created: 2020-11-23T14:50:44.770Z
definition: SSW-NNE striking normal fault, dipping WNW with unknown angle; eastern boundary of the Lauchertgraben.
references: https://data.geoscience.earth/ncl/geoera/ref/6382
preferred label: Lauchertgraben Störung 3 @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lauchert Graben

Lauchertgraben Fault 5
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6382
preferred label: Lauchertgraben Störung 5 @de
notation: geola_019
notation: DE-BW_221
type: Concept
definition: WNW-ESE streichende, nach SSW einfallende Abschiebung mit unbekanntem Einfallswinkel; nördliche Querstörung Lauchertgraben. @de
definition: WNW-ESE striking normal fault, dipping SSW with unknown angle; northern lateral fault of the Lauchertgraben.
created: 2020-11-23T14:50:44.826Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lauchert Graben

Lauchertgraben Fault 6
type: Fault
type: Limit
type: Concept
definition: WNW-ESE streichende, nach SSW einfallende Abschiebung mit unbekanntem Einfallswinkel; südliche Querstörung Lauchertgraben. @de
notation: geola_020
notation: DE-BW_222
preferred label: Lauchertgraben Störung 6 @de
references: https://data.geoscience.earth/ncl/geoera/ref/6382
created: 2020-11-23T14:50:44.854Z
definition: WNW-ESE striking normal fault, dipping SSW with unknown angle; southern lateral fault of the Lauchertgraben.
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lauchert Graben

Bad Gögging Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:37.542Z
notation: DE-BY_1308
preferred label: Bad Gögging Störung @de
definition: Inferred from the linear array of subthermal sulfurous springs at Bad Gögging and Irnsing, WNW-ESE striking continuation of Abensberg-Rottenburg Fault [DE-BY_812].
definition: Aus der linearen Anordnung subthermaler Schwefelquellen in Bad Gögging und Irnsing geschlossene, WNW-ESE streichende Fortsetzung der Abensberg-Rottenburg Störung [DE-BY_812]. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1308
broader: Swabian-Franconian Alb fault domain

Irading-Kugelgraben Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4120
type: Concept
created: 2020-10-09T11:35:37.790Z
notation: DE-BY_1317
alternative label: Iradinger Bruch @de
preferred label: Irading-Kugelgraben Störung @de
definition: Kinked NW-SE to N-S trending, steeply (85°-60°) NE to E dipping normal fault NW to SE of Grasslfing, featuring a throw of up to 20 m.
definition: Nordwestlich bis südöstlich von Graßlfing geknickt NW-SE bis N-S verlaufende, steil (85°-60°) nach NE bis E einfallende Abschiebung mit einem Vertikalversatz bis zu 20 m. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1317
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Grossberg Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4120
type: Concept
created: 2020-10-09T11:35:37.763Z
notation: DE-BY_1316
alternative label: Großberger Verwerfung @de
preferred label: Großberg Störung @de
definition: Running from the Danube river to Niedergebrachting, kinked NW-SE to NNW-SSE trending, steeply (85°-60°) NE to ENE dipping normal fault featuring a throw of up to 30 m.
definition: Von der Donau bis nach Niedergebraching geknickt NW-SE bis NNW-SSE verlaufende, steil (85°-60°) nach NE bis ENE einfallende Abschiebung mit bis zu 30 m Vertikalversatz. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1316
limit type: normalFault
broader: Swabian-Franconian Alb fault domain

Lower Bavaria - Upper Austria Molasse Basin Eastern Margin Fault Systems
type: Limit
in scheme: GC3D limits
type: Fault
type: Concept
created: 2021-02-10T13:24:29.528Z
type: SpatialObject
preferred label: Niederbayerisch-oberösterreichisches Molassebecken Ostrand-Störungssysteme @de
notation: DE-BY_1518
narrower: Deggendorf-Ried Faultsystem
narrower: Danube Fault System
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1518
broader: 1: Tectonic Boundary Objects in the central part of the North Alpine Molasse Basin and northward adjoining areas

Foreland Molasse Southern Margin Faults
type: Limit
in scheme: GC3D limits
type: Fault
narrower: Loisach Valley Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/6368
references: https://data.geoscience.earth/ncl/geoera/ref/6363
narrower: Iller Valley Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/7684
created: 2021-02-01T13:14:07.793Z
type: Concept
type: SpatialObject
notation: DE-BY_1548
preferred label: Südrand-Störungen der Vorlandmolasse @de
definition: Between Lake Constance in the west and Chiemsee in the east the southern boundary ot the Foreland Molasse is formed by the northern boundary of Subalpine (Folded) Molasse [DE-BY_789]. East of Chiemsee, where the Subalpine Molasse is overthrusted by Alpine units, the Alpine Basal Thrust (Thrust Front of Helvetic, Penninic and Austroalpine Nappes) [DE-BY_753] represents the southern boundary of the Foreland Molasse.
definition: Zwischen dem Bodensee im Westen und dem Chiemsee im Osten wird der Südrand der Vorlandmolasse vom Nordrand der Faltenmolasse (Subalpinen Molasse) [DE-BY_789 gebildet. Östlich des Chiemsees, wo die Subalpine Molasse von den alpinen Einheiten überfahren wurde, bildet die Überschiebungsfront des helvetischen, penninischen und ostalpinen Deckenstapels [DE-BY_753] die Südgrenze der Vorlandmolasse. @de
narrower: Northern Boundary of Subalpine Molasse
narrower: Thrust Front of Helvetic, Penninic and Austroalpine Nappes
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1548
limit type: reverseFault
broader: 1: Tectonic Boundary Objects in the central part of the North Alpine Molasse Basin and northward adjoining areas

Northern Boundary of Subalpine Molasse
type: Fault
type: Limit
alternative label: Nordrand der Aufgerichteten Molasse @de
references: https://data.geoscience.earth/ncl/geoera/ref/6365
references: https://data.geoscience.earth/ncl/geoera/ref/6364
references: https://data.geoscience.earth/ncl/geoera/ref/6363
sf touches: Iller Valley Fault
sf touches: Thrust Front of Helvetic, Penninic and Austroalpine Nappes
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4104
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:38.372Z
notation: DE-BY_789
alternative label: Northern Limit of Tilted Molasse
alternative label: Northern Boundary of Folded Molasse
alternative label: Nordrand der subalpinen Molasse @de
preferred label: Nordrand der Faltenmolasse @de
definition: Southern boundary of the Alpine Foreland Molasse towards the Subalpine (aka Folded or Imbricate) Molasse. Commonly WSW-ENE trending, steeply (85°-60°) S dipping reverse fault, laterally displaced by few sinistral transverse faults [DE-BY_788], [DE-BY_933]. Represents the sheared off northernmost flanks of the synclines formed by compressional stress of the Alpine northward thrust. In the western part (Allgäu), where the Folded or Imbricate Molasse merges into tectonic wedging forming triangle zones, it represents the N dipping leg at the crest of the blind, protruding wedges. In the Alpine foothills of eastern Bavaria and Austria the Subalpine Molasse is completely overthrusted by the Alpine nappes, headed by Helvetic nappes and the Rhenodanubian Flysch, thus does not emerge here.
definition: Südgrenze der alpinen Vorlandmolasse. WSW-ENE verlaufende, steil (85°-60°) südwärts einfallende Aufschiebungen, bereichsweise durch N-S verlaufende sinistrale Blattverschiebung [DE-BY_788], [DE-BY_933] versetzt. Wird von den auf die Vorlandmolasse aufgeschobenen Nordflügeln von Muldenstrukturen gebildet, die aus der Kompressionstektonik des nordwärts gerichteten Alpenschubs resultiert. Im Westen (Allgäu), wo die Faltenmolasse in sog. Triangel Zonen übergeht, wird die Grenze vom nordfallenden Schenkel im Scheitel der überdeckten Orogen-Keile aufgebaut. Im Osten der bayerischen Voralpen und in Österreich wurde die Faltenmolasse komplett von den alpinen Decken, zuvorderst Helvetikum und Rhenodanubischer Flysch, überfahren und tritt daher hier nicht zutage. @de
narrower: Loisach Valley Fault System
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11680
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11681
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11687
notation: LfU-BY_789
limit type: reverseFault
broader: Foreland Molasse Southern Margin Faults

Loisach Valley Fault System
limit type: strikeSlipFault
type: Limit
type: Fault
definition: SW-NE trending fault with left-lateral movement running parallel to the Loisach valley. Displaces the Alpine Basal Thrust [DE-BY_753] and assumedly (not disclosed) the Northern Boundary of Subalpine Molasse [DE-BY_789].
definition: SW-NE verlaufende Störung sub-parallel zum Loisachtal mit sinistral seitenverschiebender Kinematik; versetzt die Alpine Deckenfront [DE-BY_753] und vermutlich (nicht aufgeschlossen) den Nordrand der Faltenmolasse [DE-BY_789]. @de
sf touches: Thrust Front of Helvetic, Penninic and Austroalpine Nappes
references: https://data.geoscience.earth/ncl/geoera/ref/737
references: https://data.geoscience.earth/ncl/geoera/ref/7269
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4111
type: Concept
created: 2020-10-09T11:35:38.428Z
notation: DE-BY_933
alternative label: Penzberg Transfer Fault
alternative label: Penzberger Querstörung @de
alternative label: Loisach Störung @de
preferred label: Loisachtal Störungssystem @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_933
broader: Northern Boundary of Subalpine Molasse
broader: Foreland Molasse Southern Margin Faults

Thrust Front of Helvetic, Penninic and Austroalpine Nappes
limit type: thrustFault
type: Limit
type: Fault
notation: DE-BY_753
alternative label: Southern Boundary of Subalpine Molasse
alternative label: Alpine Basal Thrust
alternative label: Südrand der subalpinen Molasse @de
alternative label: Alpine Deckenfront @de
preferred label: Überschiebungsfront des helvetischen, penninischen und ostalpinen Deckenstapels @de
definition: Nordgrenze des helvetischen, penninischen und ostalpinen Deckenstapels und Südgrenze der gefalteten Molasse. WSW-ENE verlaufende Überschiebung mit steilem (85°-60°) Süd-Fallen, bereichsweise saiger oder überkippt. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6368
references: https://data.geoscience.earth/ncl/geoera/ref/6363
sf touches: Northern Boundary of Subalpine Molasse
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/7269
references: https://data.geoscience.earth/ncl/geoera/ref/4153
sf touches: Loisach Valley Fault System
definition: Northern boundary of the Helvetic, Penninic and Austroalpine nappes and southern boundary of Subalpine Molasse. WSW-ENE trending thrust fault with a steep (85°-60°) southerly to vertical dip, in parts recumbent.
type: Concept
created: 2020-10-09T11:35:38.456Z
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11577
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11583
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11680
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11681
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11687
notation: LfU-BY_753
broader: Foreland Molasse Southern Margin Faults

Molasse Basin Northern Margin Fault System
in scheme: GC3D limits
type: Fault
type: Limit
alternative label: Molasseflexur @de
alternative label: Malm-Abbruch @de
scope note: Due to the lack of prospectivity in terms of hydrocarbon deposits or geothermal potential, very few seismic surveys have been carried out in the shallow parts of the Molasse Basin. Unlike the tectonic boundaries in the deeper parts of the basin, these blind faults are inferred from borehole correlation of the top of Upper Jurassic and the extrapolation of mapped or inferred faults in the respective exposed sequence of the Swabian-Franconian Alb cuesta.
definition: Array of overall SW-NE to W-E trending, steeply SE to S dipping normal faults, in larger sections as step faults or occasionally displaced by lateral faults, running from Ulm / Neu-Ulm to Ingolstadt. The eastward continuation to Neustadt/Donau and Abensberg (Freyberg 1969) is uncertain but, further to the east, seems to be manifested by the Neustadt Flexure between Neustadt/Donau and Bad Gögging (Schmidt-Kaler 1968). To the west of Ulm, a flexure is continuously formed on the northern edge of the Molasse Basin (DE-BW_915], but it does not coincide with the basin edge (the cliff line north of it) (Geyer et al. 2011).
scope note: Von Ulm / Neu-Ulm bis Ingolstadt insgesamt SW-NE bis W-E verlaufendes System steil nach Süd bis Südost einfallender Abschiebungen, abschnittsweise als Staffelbruch oder vereinzelt durch Querbrüche versetzt. Eine Fortsetzung nach Osten hin, bis Neustadt/Donau und Abensberg (Freyberg 1969) ist unsicher, scheint sich aber im Osten in der Neustädter Flexur zwischen Neustadt/Donau und Bad Gögging (Schmidt-Kaler 1968) abzuzeichnen. Westlich von Ulm, ist am Molassebecken-Nordrand durchgehend eine Flexur ausgebildet [DE-BW_915], die jedoch nicht mit dem Beckenrand (der Klifflinie nördlich davon) zusammenfällt (Geyer et al. 2011). @de
narrower: Molasse Flexure
references: https://data.geoscience.earth/ncl/geoera/ref/6372
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4132
references: https://data.geoscience.earth/ncl/geoera/ref/4083
type: Concept
created: 2020-10-09T11:35:35.784Z
notation: DE-BY_1244
preferred label: Molassebecken-Nordrand Störungssystem @de
definition: Von Ulm / Neu-Ulm bis Ingolstadt insgesamt SW-NE bis W-E verlaufendes System steil nach Süd bis Südost einfallender Abschiebungen, abschnittsweise als Staffelbruch oder vereinzelt durch Querbrüche versetzt. Eine Fortsetzung nach Osten hin, bis Neustadt/Donau und Abensberg (Freyberg 1969) ist unsicher, scheint sich aber im Osten in der Neustädter Flexur zwischen Neustadt/Donau und Bad Gögging (Schmidt-Kaler 1968) abzuzeichnen. @de
narrower: Franconian Alb Boundary System
narrower: Riedheim-Wittislingen Fault
narrower: Langenau-Wittislingen Fault
narrower: Wittislingen-Lutzingen Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1244
limit type: normalFault
broader: 1: Tectonic Boundary Objects in the central part of the North Alpine Molasse Basin and northward adjoining areas

Franconian Alb Boundary System
type: Fault
type: Limit
alternative label: Alb-Südrandbruch @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4105
references: https://data.geoscience.earth/ncl/geoera/ref/4106
references: https://data.geoscience.earth/ncl/geoera/ref/4083
type: Concept
created: 2020-10-09T11:35:35.812Z
notation: DE-BY_1245
hidden label: Donaurandbruch @de
preferred label: Jurarandbruch System @de
definition: Array of steeply (85°-60°) S to SE dipping normal faults running from Ulm / Neu-Ulm to Ingolstadt; step fault in the Leipheim-Donauwörth area. The eastward continuation to south of Vohburg is uncertain (Jung et al. 2003).
definition: Von Ulm / Neu-Ulm bis Ingolstadt ziehendes System steil nach Süd bis Südost einfallender Abschiebungen, im Bereich Leipheim-Donauwörth als Staffelbruch. Eine Fortsetzung nach Osten hin, bis südlich von Vohburg, ist unsicher (Jung et al. 2003). @de
narrower: Strass-Nordendorf Fault
narrower: Nersingen-Sinning Fault
narrower: Moos-Sinning Fault
narrower: Elchingen-Neuburg Fault
narrower: Neuburg Fault
narrower: Jurarandbruch
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1245
limit type: normalFault
broader: Molasse Basin Northern Margin Fault System

Elchingen-Neuburg Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4105
references: https://data.geoscience.earth/ncl/geoera/ref/4083
sf touches: Lauingen-Schwennigen Subfault
sf touches: Schambach Fault
sf touches: Riedheim-Wittislingen Fault
type: Concept
created: 2020-10-09T11:35:35.924Z
notation: DE-BY_1247
preferred label: Elchingen-Neuburg Störung @de
definition: WSW-ENE to W-E trending, steeply (85°-60°) SSE to S dipping synthetic normal fault featuring a throw of up tp 50 m; northern and principal subfault of the step fault forming the buried Franconian Alb Boundary System in the Leipheim-Donauwörth area, probably continuing to Ulm / Neu-Ulm in the west and reaching to Neuburg-Fault [DE-BY_1249] in the east.
definition: WSW-ENE bis W-E verlaufende, steil (85°-60°) nach SSE bis S einfallende synthetische Abschiebung; nördliche Teilstörung des überdeckten Jurarand-Staffelbruchs im Bereich Leipheim-Donauwörth, die im Westen wohl bis nach Ulm / Neu-Ulm fortsetzt und im Osten bis zur Neuburg-Störung [DE-BY_1249] reicht. @de
narrower: Lauingen-Schwennigen Subfault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1247
limit type: normalFault
broader: Franconian Alb Boundary System

Lauingen-Schwennigen Subfault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/4105
sf touches: Elchingen-Neuburg Fault
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:35.952Z
notation: DE-BY_1248
preferred label: Lauingen-Schwenningen Nebenstörung @de
definition: WSW-ENE strikng, steeply (85°-60°) SSE dipping synthetic normal fault forming a pre-step of Elchingen-Neuburg Fault.
definition: WSW-ENE streichende, steil (85°-60°) nach SSE einfallende synthetische Abschiebung als Vorstufe der Elchingen-Neuburg Störung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1248
limit type: normalFault
broader: Elchingen-Neuburg Fault

Moos-Sinning Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4105
sf touches: Nersingen-Sinning Fault
type: Concept
created: 2020-10-09T11:35:35.896Z
notation: DE-BY_1268
preferred label: Moos-Sinning Querstörung @de
definition: Southwestern boundary of the Neuburg Jurassic spur truncating Nersingen-Sinning Fault [DE-BY_781].
definition: Südwestliche Begrenzung des Neuburger Jura Sporns und östliches Ende der Nersingen-Sinning Störung [DE-BY_781]. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1268
limit type: normalFault
broader: Franconian Alb Boundary System

Nersingen-Sinning Fault
type: Fault
type: Limit
definition: WSW-ENE trending, steeply (85°-60°) ± SSE dipping synthetic normal fault running probably from Neu-Ulm, evidenced by borehole correlation from Nersingen, in the west to Sinning in the east, featuring a throw of up to 60 m; middle subfault of the step fault forming the blind Franconian Alb Boundary System in the Leipheim-Donauwörth area.
definition: WSW-ENE verlaufende, steil (85°-60°) nach ± SSE einfallende synthetische Abschiebung, wahrscheinlich zwischen Neu-Ulm (mittels Bohrloch-Korrelation nachgewiesen ab Nersingen) und Sinning, mit einer Sprunghöhe bis zu 60 m; mittlere Teilstörung des überdeckten Jurarand-Staffelbruchs im Bereich Leipheim-Donauwörth. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4105
type: Concept
created: 2020-10-09T11:35:35.868Z
notation: DE-BY_781
preferred label: Nersingen-Sinning Störung @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_781
limit type: normalFault
broader: Franconian Alb Boundary System

Strass-Nordendorf Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4105
type: Concept
created: 2020-10-09T11:35:35.840Z
notation: DE-BY_1246
preferred label: Strass-Nordendorf Störung @de
definition: WSW-ENE to W-E trending, steeply (85°-60°) SSE to S dipping synthetic normal fault featuring a throw of up to 50 m; southern subfault of the step fault forming the buried Franconian Alb Boundary System in the Leipheim-Donauwörth area.
definition: WSW-ENE bis W-E verlaufende, steil (85°-60°) nach SSE bis S einfallende synthetische Abschiebung mit einer Sprunghöhe bis zu 50 m; südliche Teilstörung des überdeckten Jurarand-Staffelbruchs im Bereich Leipheim-Donauwörth. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1246
limit type: normalFault
broader: Franconian Alb Boundary System

Jurarandbruch
type: Limit
type: Fault
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4102
references: https://data.geoscience.earth/ncl/geoera/ref/4151
sf touches: Neuburg Fault
type: Concept
created: 2020-10-09T11:35:36.008Z
notation: DE-BY_782
hidden label: Donaurandbruch @de
alternative label: Malm-Abbruch @de
definition: WNW-ESE trending, steeply (85°-60°) SSW dipping normal fault with a throw of up to 80 m between Joshofen NE Neuburg and Hundszell S of Ingolstadt City. Blind fault within the Ingolstadt subbasin, presumably part of the larger, buried section of the Franconian Alb Boundary System continuing to the east (Unger 1999).
definition: Überdeckte WNW-ESE streichende, steil (85°-60°) nach SSW einfallende Abschiebung zwischen Joshofen nordöstlich von Neuburg und Hundszell südlich der Altstadt von Ingolstadt. Die Störung mit einem Versatz von bis zu 80 m verläuft durch das Ingolstädter Becken und ist mutmaßlich Teil eines größeren, überdeckten Abschnitts des Jurarandbruchs der sich nach Osten hin fortsetzt (Unger 1999). @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11682
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11683
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11888
notation: LfU-BY_782
limit type: normalFault
broader: Franconian Alb Boundary System

Neuburg Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4090
references: https://data.geoscience.earth/ncl/geoera/ref/4083
sf touches: Jurarandbruch
sf touches: Elchingen-Neuburg Fault
type: Concept
created: 2020-10-09T11:35:35.980Z
notation: DE-BY_1249
hidden label: Donaurandbruch @de
preferred label: Neuburg Störung @de
definition: SW-NE striking, steeply (85°-60°) SE dipping normal fault subcropping E to NE of Neuburg/Donau. Southwestern boundary of the Neuburg Jurassic protrudion with Ingolstadt subbasin having a throw of more than 250 m at the top of Jurassic as inferred from correlation of marker horizons (Fiebig & Pürner 2003).
definition: Überdeckte, SW-NE streichende, steil (85°-60°) nach SE einfallende Abschiebung östlich bis nordöstlich von Neuburg a.d. Donau; südöstliche Begrenzung des Neuburger Jurasporns. Aus der Korrelation von Leithorizonten lässt sich zwischen der jurassischen Schichtoberfläche des Neuburger Sporns und des Ingolstädter Beckens eine Sprunghöhe von über 250 m ableiten (Fiebig & Pürner 2003). @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11680
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11887
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11888
notation: LfU-BY_1249
limit type: normalFault
broader: Franconian Alb Boundary System

Wittislingen-Lutzingen Fault
type: Limit
type: Fault
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4105
sf touches: Mödingen Fault
type: Concept
created: 2020-10-09T11:35:36.092Z
notation: DE-BY_1252
preferred label: Wittislingen-Lutzingen Störung @de
definition: Southeastward arcuate, overall SW-NE trending, steeply (85°-60°) SSE to SE dipping normal fault branch of Mödingen Fault [DE-BY_1254].
definition: Südostwärts gebogen, insgesamt SW-NE verlaufende, steil (85°-60°) nach SSE bis SE einfallende Abschiebung; Abzweig des Mödinger Abbruchs [DE-BY_1254]. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1252
limit type: normalFault
broader: Molasse Basin Northern Margin Fault System

Langenau-Wittislingen Fault
type: Limit
type: Fault
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4105
sf touches: Riedheim-Wittislingen Fault
sf touches: Mödingen Fault
type: Concept
created: 2020-10-09T11:35:36.064Z
notation: DE-BY_1251
preferred label: Langenau-Wittislingen Störung @de
definition: WSW-ENE trending, steeply (85°-60°) SSE dipping normal fault subcropping northward parallel to Elchingen-Neuburg Fault [DE-BY_1247] and merging into Riedheim-Wittislingen Fault [DE-BY_1250], continuing northeastward as Mödingen Fault [DE-BY_1254].
definition: WSW-ENE verlaufende, steil (85°-60°) nach SSE einfallende Abschiebung nördlich parallel zur Elchingen-Neuburg Störung [DE-BY_1247]. Geht in die Riedheim-Wittislingen Störung [DE-BY_1250] über, die sich nordostwärts als Mödinger Abbruch [DE-BY_1254] fortsetzt. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1251
limit type: normalFault
broader: Molasse Basin Northern Margin Fault System

Riedheim-Wittislingen Fault
type: Limit
type: Fault
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4105
sf touches: Elchingen-Neuburg Fault
sf touches: Langenau-Wittislingen Fault
sf touches: Mödingen Fault
type: Concept
created: 2020-10-09T11:35:36.036Z
notation: DE-BY_1250
preferred label: Riedheim-Wittislingen Störung @de
definition: SW-NE trending, steeply (85°-60°) SE dipping branch of Elchingen-Neuburg Fault [DE-BY_1247]; continuing northeastward as Mödingen Fault [DE-BY_1254].
definition: SW-NE verlaufender, steil (85°-60°) nach SE einfallender Abzweig der Elchingen-Neuburg Störung [DE-BY_1247]; setzt sich nordostwärts im Mödinger Abbruch [DE-BY_1254] fort. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1250
limit type: normalFault
broader: Molasse Basin Northern Margin Fault System

Molasse Flexure
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6360
alternative label: Alb Southern Margin Flexure
references: https://data.geoscience.earth/ncl/geoera/ref/6390
definition: Struktureller Nordrand des Molasse Beckens als tektonische Region, welcher jedoch nicht mit dem Beckenrand (bzw. der Klifflinie nördlich davon) zusammenfällt. Im Anschluss an das „Jurarandbruch Sytem“ [DE-BY_1245] östlich von Ulm, ist am Nordrand des Molassebeckens in Baden-Württemberg durchgehend eine Flexur ausgebildet, an der sich die Schichtlagerung des Tafeldeckgebirges auf kurze Distanz von höchstens ca. 1° im Ostteil des südlichen Schichtstufenlandes auf etwa 5° erhöht. @de
type: SpatialObject
preferred label: Molasseflexur @de
references: https://data.geoscience.earth/ncl/geoera/ref/6396
created: 2020-11-23T14:40:19.969Z
references: https://data.geoscience.earth/ncl/geoera/ref/6359
alternative label: Albsüdrandflexur @de
type: Concept
definition: Structural northern margin of the Molasse Basin as a tectonic region, which does not coincide with the basin edge (or the cliff line north of it). Following the "Franconian Alb Boundary System" [DE-BY_1245] east of Ulm, a flexure is continuously formed on the northern margin of the Molasse Basin in Baden-Württemberg, where the dip of the overburden increase over a short distance from less than 1° southeast to approx. 5° at most.
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Molasse Basin Northern Margin Fault System

Central Foreland Molasse Basin fault domain
alternative label: Central Foreland Molasse Basin limits and internal faults
in scheme: GC3D limits
type: Fault
type: Limit
narrower: Lindau-Hergatz Fault
narrower: Lautrach-Stetten Fault
narrower: Guggenberg-Erisried Fault
narrower: Jettenbach Fault
narrower: Kraiburg-Unterneukirchen Fault
narrower: Waldhausen-Asten Fault
narrower: Kirchweidach Fault
narrower: Tylraching Fault
narrower: Oberfeldkirchen Fault
narrower: Schnaitsee-Trostberg Fault
narrower: Wasserburg-Schnaitsee Fault
narrower: Aham-Stockham Fault
narrower: Obing-Altenmarkt Fault
narrower: Wolnzach Fault
narrower: Unterschweinbach Fault
narrower: Eurishofen-Waal Fault
narrower: Stockheim-Buchloe Fault
narrower: Bad Wörishofen Fault
narrower: Lauchdorf-Bad Wörishofen Fault
narrower: Vöhringen-Roggenburg Fault
narrower: Illertissen-Messhofen Fault
narrower: Kirchberg-Osterberg Fault
narrower: Kellmünz Fault
narrower: Fellheim-Oberschönegg Fault
narrower: Pless-Winterrieden Fault
narrower: Wollmetshofen-Leitershofen Fault
narrower: Langenneufnach-Döpshofen Fault
narrower: Eurasburg-Gartenberg Fault
narrower: Babenstuben-Sachsenkam Fault
narrower: Humbach-Dietenhausen Fault
narrower: Föggenbach Fault
narrower: Thanning Fault
narrower: Frasshausen Fault
narrower: Sauerlach-Schlacht Fault
narrower: Faistenhaar-Egmating Fault
narrower: Kreuzstrasse-Baiern Fault
narrower: Otterfing Fault
narrower: Hofoldinger Forst Fault
narrower: Ebersberg-Steinhöring Fault
narrower: Eichenried-Pretzen Fault
narrower: Eching-Erching Fault
narrower: Dietersheim Fault
narrower: Oberschleissheim-Walpertskirchen Fault
narrower: Ismaning-Zengermoos Cross-fault
narrower: Ismaning-Neufinsing Fault
narrower: Neuching-Wörth Fault
narrower: Kirchasch-Algasing Fault
narrower: Grünbach-Kalling Fault
narrower: Krumbach-Dinkelscherben Fault
narrower: Dinkelscherben-Ried Fault
narrower: Kirchhaslach-Aletshausen Fault
narrower: Aletshausen-Langenneufnach Fault
narrower: Reichau-Hasberg Fault
narrower: Stolzenhofen-Hasberg Fault
narrower: Haselbach-Mickhausen Fault
narrower: Mörgen-Walkershofen Fault
narrower: Trostberg Fault
narrower: Grossbergham-Lochen Fault
narrower: Memmingen Fault
narrower: Benningen-Kammlach Fault
narrower: Frauenzell-Böhen Fault
narrower: Hochzoll-St. Afra Fault
narrower: Schwabmünchen Fault
narrower: Herrsching-Gauting Fault
narrower: Tuntenhausen-Schönstett Fault
narrower: Ilmmünster Step Fault
narrower: Petershausen-Schweitenkirchen Fault
narrower: Vierkirchen-Leonhardsbuch Fault
narrower: Strassbach-Vierkirchen Fault
narrower: Biberbach-Bachhausen Fault
narrower: Arzbach-Fahrenzhausen Fault
narrower: Stetten-Arzbach Fault
narrower: Höslwang Fault
narrower: Seebruck Fault
narrower: Velden Fault
narrower: Taufkirchen-Ampfing Fault

Lauchdorf-Bad Wörishofen Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.250Z
notation: DE-BY_1188
preferred label: Lauchdorf-Bad Wörishofen Störung @de
definition: SSW-NNE striking, approx. 80° WNW dipping antithetic normal fault running subparallel to synthetic Warmisried-Altensteig Fault [DE-BY_1121] forming a local graben structure.
definition: SSW-NNE streichende, ca. 80° nach WNW einfallende antithetische Abschiebung. Bildet mit der subparallel verlaufenden synthetischen Warmisried-Altensteig Störung [DE-BY_1121] eine lokale Grabenstruktur. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
sf touches: Bad Wörishofen Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1188
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

[hl_069]
type: Fault
type: Limit
notation: DE-BW_117
definition: N-S streichende, ca. 80° nach E einfallende Abschiebung. @de
definition: N-S striking, approx. 80° E dipping normal fault
sf touches: [hl_067]
created: 2020-11-23T14:24:51.249Z
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
narrower: [hl_071]
sf touches: [hl_028]
narrower: [hl_068]
narrower: [hl_070]
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_070]
type: Fault
type: Limit
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
definition: W-E streichende, ca. 80° nach S einfallende Abschiebung. @de
sf touches: [hl_071]
created: 2020-11-23T14:24:51.252Z
definition: W-E striking, approx. 80° S dipping normal fault
notation: DE-BW_119
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [hl_069]

[hl_071]
type: Fault
type: Limit
created: 2020-11-23T14:24:51.254Z
definition: W-E streichende, fast saiger stehende Abschiebung. @de
sf touches: [hl_070]
type: Concept
notation: DE-BW_120
references: https://data.geoscience.earth/ncl/geoera/ref/4097
definition: W-E striking, almost vertical normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [hl_069]

[hl_068]
type: Fault
type: Limit
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
notation: DE-BW_118
created: 2020-11-23T14:24:51.251Z
definition: WNW-ESE streichende, ca. 70° nach SSW einfallende Abschiebung. @de
definition: WNW-ESE striking, approx. 70° SSW dipping normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [hl_069]

Pfaffenhofen Step Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.876Z
notation: DE-BY_767
preferred label: Pfaffenhofener Bruchstaffel @de
definition: Staggered array of 4 (sub-)parallel W-E to SW-NE striking, steeply (85°-60°) N to NNW dipping antithetic fault scarps with a minor throw immediate north of synthetic Ilmmünster Step Fault [DE-BY_917]. Beyond the four detected faults featuring throws of more than about 10 m, more subseismic fault scarps are possible.
definition: Bruchstaffel aus vier (sub)parallelen, W-E bis SW-NE verlaufenden, steil (85°-60°) nach N bis NNW einfallenden antithetischen Abschiebungen mit geringer Sprunghöhe, unmittelbar nördlich der synthetischen Ilmmünster Bruchstaffel [DE-BY_917]. Neben den vier identifizierbaren Stufen mit Sprunghöhen von mehr als ca. 10 m sind weitere subseismische Bruchstufen möglich. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_767
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Bad Wörishofen Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.222Z
notation: DE-BY_1187
preferred label: Bad Wörishofen Störung @de
definition: WNW-ESE striking, approx. 85° SSW dipping synthetic normal fault.
definition: WNW-ESE streichende, ca. 85° nach SSW einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
sf touches: Stockheim-Buchloe Fault
sf touches: Lauchdorf-Bad Wörishofen Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1187
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Pless-Winterrieden Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.472Z
notation: DE-BY_874
preferred label: Pleß-Winterrieden Störung @de
definition: SW-NE striking, steeply (85°-60°) SE dipping synthetic normal fault.
definition: SW-NE streichende, steil (85°-60°) nach SE einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_874
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Fellheim-Oberschönegg Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.444Z
notation: DE-BY_1193
preferred label: Fellheim-Oberschönegg Störung @de
definition: WSW-ENE striking, approx. 55° SSE dipping synthetic normal fault.
definition: WSW-ENE streichende, in etwa 55° nach SSE einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1193
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Kellmünz Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.417Z
notation: DE-BY_1192
preferred label: Kellmünz Störung @de
definition: SW-NE striking, approx. 70° SE dipping synthetic normal fault connecting into Baden-Württembergian territory.
definition: SW-NE streichende, in etwa 70° nach SE einfallende synthetische Abschiebung mit Fortsetzung in Baden-Württemberg. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1192
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Ichenhausen-Zusmarshausen Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:29.041Z
notation: DE-BY_785
preferred label: Ichenhausen-Zusmarshausen Störung @de
definition: Mainly WSW-ENE striking, veering to a WNW-ESE trend in its eastern part, steeply (85°-60°) NNW to NNE dipping antithetic normal fault.
definition: Überwiegend WSW-ENE streichende, im Ostteil auf WNW-ESE drehende, steil (85°-60°) nach NNW bis NNE einfallende antithetische Abschiebung. @de
narrower: Ichenhausen Subfault
narrower: Ellzee-Scheppach Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_785
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Ellzee-Scheppach Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:29.097Z
notation: DE-BY_893
preferred label: Ellzee-Scheppach Störung @de
definition: SSW-NNE striking, steeply (85°-60°) NNW dipping antithetic normal fault, branch of Ichenhausen-Zusmarshausen Fault [DE-BY_785].
definition: SSW-NNE streichende, steil (85°-60°) nach NNW einfallende antithetische Abschiebung, Zweig der Ichenhausen-Zusmarshausen Störung [DE-BY_785]. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
sf touches: Ichenhausen-Zusmarshausen Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_893
limit type: normalFault
broader: Ichenhausen-Zusmarshausen Fault

Ichenhausen Subfault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:29.069Z
notation: DE-BY_892
preferred label: Ichenhausen Nebenstörung @de
definition: Branch of Ichenhausen-Zusmarshausen Fault. SSW-NNE striking, steeply (85°-60°) WNW dipping antithetic normal fault.
definition: Zweig der Ichenhausen-Zusmarshausen Störung. SSW-NNE streichende, steil (85°-60°) nach NNW einfallende antithetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
sf touches: Ichenhausen-Zusmarshausen Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_892
limit type: normalFault
broader: Ichenhausen-Zusmarshausen Fault

Kirchberg-Osterberg Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.389Z
notation: DE-BY_1191
preferred label: Kirchberg-Osterberg Störung @de
definition: WSW-ENE striking, approx. 70° SSE dipping synthetic normal fault connecting into Baden-Württembergian territory.
definition: WSW-ENE streichende, in etwa 70° nach SSE einfallende synthetische Abschiebung mit Fortsetzung in Baden-Württemberg. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1191
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Derching-Wollomoos Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.986Z
notation: DE-BY_780
preferred label: Derching-Wollomoos Störung @de
definition: Mainly WSW-ENE trending, veering to an undulate WNW-ESE trend in its eastern part, steeply (85°-60°) NNW to NNE dipping antithetic normal fault.
definition: Überwiegend WSW-ENE verlaufende, im Ostteil wellenförmig auf WNW-ESE drehende, steil (85°-60°) nach NNW bis NNE einfallende antithetische Abschiebung. @de
narrower: Klingen Subfault
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_780
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Klingen Subfault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:29.014Z
notation: DE-BY_1122
preferred label: Klingen Nebenstörung @de
definition: W-E striking, steeply (85°-60°) N dipping antithetic normal fault.
definition: W-E streichende, steil (85°-60°) nach N einfallende antithetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1122
limit type: normalFault
broader: Derching-Wollomoos Fault

Neusäss-Aichach Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.958Z
notation: DE-BY_779
preferred label: Neusäß-Aichach Störung @de
definition: WSW-ENE trending, steeply (85°-60°) S dipping synthetic normal fault.
definition: WSW-ENE verlaufende, steil (85°-60°) nach S einfallende synthetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: Ichenhausen-Zusmarshausen Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_779
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Illertissen-Messhofen Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.306Z
notation: DE-BY_871
preferred label: Illertissen-Meßhofen Störung @de
definition: WSW-ENE to SW-NE striking, steeply (85°-60°) ± NW dipping antithetic normal fault.
definition: WSW-ENE bis SW-NE streichende, steil (85°-60°) nach ± NW einfallende antithetische Abschiebung. @de
narrower: Matzenhofen Cross-fault
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
narrower: Altenstadt-Buch Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_871
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Matzenhofen Cross-fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.362Z
notation: DE-BY_1190
preferred label: Matzenhofen Querstörung @de
definition: NW-SE striking, approx. 80° NE dipping antithetic normal fault, cross-fault to Illertissen-Messhofen Fault [DE-BY_871].
definition: NW-SE streichende, in etwa 80° nach NE einfallende antithetische Abschiebung; Querstörung zur Illertissen-Meßhofen Störung [DE-BY_871] @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1190
limit type: normalFault
broader: Illertissen-Messhofen Fault

Altenstadt-Buch Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.334Z
notation: DE-BY_1189
preferred label: Altenstadt-Buch Störung @de
definition: SW-NE striking, steeply (85°-60°) NW dipping antithetic normal fault, branch of Illertissen-Messhofen Fault [DE-BY_871].
definition: SW-NE streichende, steil (85°-60°) nach NW einfallende antithetische Abschiebung; Zweig der Illertissen-Meßhofen Störung [DE-BY_871]. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1189
limit type: normalFault
broader: Illertissen-Messhofen Fault

Vöhringen-Roggenburg Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.278Z
notation: DE-BY_870
preferred label: Vöhringen-Roggenburg Störung @de
definition: WNW-ESE striking, steeply (85°-60°) NNE dipping antithetic normal fault.
definition: WNW-ESE streichende, steil (85°-60°) nach NNE einfallende antithetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_870
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Zusmarshausen-Gundelsdorf Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.903Z
notation: DE-BY_777
preferred label: Zusmarshausen-Gundelsdorf Störung @de
definition: Undulate, overall WSW-ENE trending, steeply (85°-60°) ± NNW dipping antithetic normal fault.
definition: WSW-ENE verlaufende, steil (85°-60°) nach NNW einfallende antithetische Abschiebung. @de
narrower: Adelsried-Aichach Subfault
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
sf touches: Ichenhausen-Zusmarshausen Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_777
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Adelsried-Aichach Subfault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.931Z
notation: DE-BY_778
preferred label: Adelsried-Aichach Störung @de
definition: Southern branch of Zusmarshausen-Gundelsdorf Fault [DE-BY_777]. Undulate, overall W-E trending, steeply (85°-60°) ± N dipping antithetic normal fault running from Adelsried to Kühbach.
definition: Wellenförmig insgesamt W-E verlaufende, steil (85°-60°) nach ± N einfallende antithetische Abschiebung. Südlicher, von Adelsried bis Kühbach verlaufender Ast der Zusmarshausen-Gundelsdorf Störung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
sf touches: Ichenhausen-Zusmarshausen Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_778
limit type: normalFault
broader: Zusmarshausen-Gundelsdorf Fault

[lca_012]
type: Fault
type: Limit
definition: WSW-ENE streichende, fast saiger stehende Abschiebung. @de
notation: DE-BW_066
type: Concept
definition: WSW-ENE striking, almost vertical normal fault
references: https://data.geoscience.earth/ncl/geoera/ref/6357
created: 2020-11-23T14:24:51.096Z
references: https://data.geoscience.earth/ncl/geoera/ref/6373
sf touches: [lca_002]
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_014]
type: Fault
type: Limit
definition: SW-NE striking, approx. 65° NW dipping normal fault
references: https://data.geoscience.earth/ncl/geoera/ref/6373
references: https://data.geoscience.earth/ncl/geoera/ref/6357
type: Concept
notation: DE-BW_053
created: 2020-11-23T14:24:51.055Z
definition: SW-NE streichende, ca. 65° nach NW einfallende Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_015]
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6373
type: Concept
definition: WNW-ESE streichende, ca. 75° nach NNE einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6357
definition: WNW-ESE striking, approx. 75° NNE dipping normal fault
narrower: [lca_082]
created: 2020-11-23T14:24:51.069Z
notation: DE-BW_058
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_082]
type: Fault
type: Limit
notation: DE-BW_122
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6373
references: https://data.geoscience.earth/ncl/geoera/ref/6357
created: 2020-11-23T14:24:51.071Z
definition: WSW-ENE streichende, ca. 85° nach SSE einfallende Abschiebung. @de
definition: WSW-ENE striking, approx. 85° SSE dipping normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [lca_015]

[lca_010]
type: Fault
type: Limit
definition: WSW-ENE striking, approx. 60° NNW dipping normal fault.
created: 2020-11-23T14:24:51.045Z
type: Concept
notation: DE-BW_049
references: https://data.geoscience.earth/ncl/geoera/ref/6357
references: https://data.geoscience.earth/ncl/geoera/ref/6373
definition: WSW-ENE streichende, ca. 60° nach NNW einfallende Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

Unterbergen-Althegnenberg Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:29.125Z
notation: DE-BY_791
preferred label: Unterbergen-Althegnenberg Störung @de
definition: W-E striking, approx. 75° S dipping synthetic normal fault.
definition: W-E streichende, ca. 75° nach S einfallende synthetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_791
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

[hl_075]
type: Fault
type: Limit
definition: SW-NE trending, approx. 70° NW dipping normal fault
notation: DE-BW_018
sf touches: [lca_002]
sf touches: [hl_081]
references: https://data.geoscience.earth/ncl/geoera/ref/4097
created: 2020-11-23T14:24:50.966Z
definition: SW-NE streichende, ca. 70° nach NW einfallende Abschiebung. @de
type: Concept
sf touches: [hl_076]
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_016]
type: Fault
type: Limit
definition: WSW-ENE striking, approx. 60° SSE dipping normal fault
created: 2020-11-23T14:24:51.213Z
notation: DE-BW_105
references: https://data.geoscience.earth/ncl/geoera/ref/6373
type: Concept
definition: WSW-ENE streichende, ca. 60° nach SSE einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6357
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_017]
type: Fault
type: Limit
type: Concept
definition: WSW-ENE streichende, ca. 65° nach SSE einfallende Abschiebung. @de
sf touches: [hl_072]
references: https://data.geoscience.earth/ncl/geoera/ref/4097
definition: WSW-ENE striking, approx. 65° SSE dipping normal fault
sf touches: [hl_065]
created: 2020-11-23T14:24:50.957Z
sf touches: [hl_009]
notation: DE-BW_014
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_018]
type: Fault
type: Limit
definition: SW-NE bis SSW-NNE streichende, ca. 60° nach SE einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6373
definition: SW-NE to SSW-NNE trending, approx. 60° SE to ESE dipping normal fault
notation: DE-BW_102
type: Concept
created: 2020-11-23T14:24:51.204Z
references: https://data.geoscience.earth/ncl/geoera/ref/6357
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_078]
type: Fault
type: Limit
created: 2020-11-23T14:24:51.261Z
definition: SW-NE striking, approx. 65° SE dipping normal fault
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
notation: DE-BW_123
definition: SW-NE streichende, ca. 65° nach SE einfallende Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_079]
type: Fault
type: Limit
definition: WSW-ENE streichende, ca. 85° nach SSE einfallende Abschiebung. @de
created: 2020-11-23T14:24:51.264Z
definition: WSW-ENE striking, approx. 85° SSE dipping normal fault
notation: DE-BW_124
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_019]
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6373
type: Concept
definition: SSW-NNE streichende, ca. 55° nach ESE einfallende Abschiebung. @de
definition: SSW-NNE striking, approx. 55° ESE dipping normal fault
references: https://data.geoscience.earth/ncl/geoera/ref/6357
notation: DE-BW_104
created: 2020-11-23T14:24:51.210Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

Eurasburg-Gartenberg Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.556Z
notation: DE-BY_881
preferred label: Eurasburg-Gartenberg Störung @de
definition: WSW-ENE striking, approx. 85° NNW dipping antithetic normal fault.
definition: WSW-ENE streichende, ca. 85° nach NNW einfallende antithetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_881
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Puchheim-Feldmoching Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:29.180Z
notation: DE-BY_796
preferred label: Puchheim-Feldmoching Störung @de
definition: SW-NE trending, approx. 75° SE dipping synthetic normal fault west to north of Munich.
definition: SW-NE verlaufende, ca. 75° nach SE einfallende synthetische Abschiebung im Westen bis Norden von München. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_796
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Langenneufnach-Döpshofen Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.528Z
notation: DE-BY_880
preferred label: Langenneufnach-Döpshofen Störung @de
definition: WSW-ENE striking, approx. 65° NNW dipping antithetic normal fault.
definition: WSW-ENE streichende, ca. 65° nach NNW einfallende antithetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_880
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Alling-Lochhausen Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:29.152Z
notation: DE-BY_1123
preferred label: Alling-Lochhausen Störung @de
definition: SW-NE striking, approx. 80° SE dipping synthetic normal fault west to northwest of Munich.
definition: SW-NE streichende, ca. 80° nach SE einfallende synthetische Abschiebung im Westen bis Nordwesten von München. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1123
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Wollmetshofen-Leitershofen Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.500Z
notation: DE-BY_879
preferred label: Wollmetshofen-Leitershofen Störung @de
definition: WSW-ENE striking, approx. 80° NNW dipping antithetic normal fault.
definition: WSW-ENE streichende, ca. 80° nach NNW einfallende antithetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_879
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Erding-Altfraunhofen Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:29.412Z
notation: DE-BY_792
preferred label: Erding-Altfraunhofen Störung @de
definition: SW-NE trending, on av. approx. 65° SE dipping synthetic normal fault. In the area of Erding running subparallel to antithetic Erding Subfault [DE-BY_1134] forming a local graben structure.
definition: SW-NE verlaufende, im Mittel ca. 65° nach SE einfallende synthetische Abschiebung. Bildet im Raum Erding mit der südlich subparallel verlaufenden, antithetischen Erding Nebenstörung [DE-BY_1134] eine lokale Grabenstruktur. @de
narrower: Oberding Subfault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_792
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Oberding Subfault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:29.442Z
notation: DE-BY_1130
preferred label: Oberding Nebenstörung @de
definition: W-E striking approx. 80° S dipping synthetic normal fault.
definition: W-E streichende, ca. 80° nach S einfallende synthetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1130
limit type: normalFault
broader: Erding-Altfraunhofen Fault

Faistenhaar-Egmating Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.750Z
notation: DE-BY_1200
preferred label: Faistenhaar-Egmating Störung @de
definition: WSW-ENE striking, approx. 75° SSE dipping synthetic normal fault running parallel to Sauerlach-Schlacht Fault [DE-BY_1199] in the south.
definition: WSW-ENE streichende, ca. 75° nach SSE einfallende synthetische Abschiebung parallel zur Sauerlach-Schlacht Störung [DE-BY_1199] unmittelbar südlich. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1200
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Argelsried-Planegg Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:29.382Z
notation: DE-BY_1129
preferred label: Argelsried-Planegg Störung @de
definition: W-E striking, approx. 85° N dipping antithethic normal fault forming a local graben structure with synthetic Gilching-Planegg Fault [DE-BY_1128] paralleling to the north.
definition: W-E streichende, ca. 85° nach N einfallende antithetische Abschiebung. Bildet mit der nördlich parallel verlaufenden synthetischen Gilching-Planegg Störungen [DE-BY_1128] eine lokale Grabenstruktur. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1129
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Sauerlach-Schlacht Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.722Z
notation: DE-BY_1199
preferred label: Sauerlach-Schlacht Störung @de
definition: Undulate WSW-ENE trending, averaged approx. 75° SSE dipping synthetic normal fault
definition: Gewellt WSW-ENE verlaufende, ca. 75° nach SSE einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1199
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Gilching-Planegg Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
sf touches: Gilching-Germering Fault
type: Concept
created: 2020-10-09T11:35:29.348Z
notation: DE-BY_1128
preferred label: Gilching-Planegg Störung @de
definition: W-E striking, approx. 70° S dipping synthethic normal fault forming a local graben structure with antithetic Argelsried-Planegg Fault [DE-BY_1129] paralleling to the south.
definition: W-E streichende, ca. 70° nach S einfallende synthetische Abschiebung. Bildet mit der südlich parallel verlaufenden antithetischen Argelsried-Planegg Störungen [DE-BY_1129] eine lokale Grabenstruktur. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1128
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Frasshausen Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.695Z
notation: DE-BY_1198
preferred label: Fraßhausen Störung @de
definition: WNW-ESE striking, approx. 80° SSW dipping synthetic normal fault.
definition: WNW-ESE streichende, ca. 80° nach SSW einfallende synthetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
sf touches: Thanning Fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1198
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Gilching-Germering Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: Gilching-Planegg Fault
type: Concept
created: 2020-10-09T11:35:29.318Z
notation: DE-BY_1127
preferred label: Gilching-Germering Störung @de
definition: WSW-ENE striking, approx. 80° SSE dipping synthethic normal fault.
definition: WSW-ENE streichende, ca. 80° nach SSE einfallende synthetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1127
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Thanning Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.667Z
notation: DE-BY_1197
preferred label: Thanning Störung @de
definition: WSW-ENE striking, approx. 65° SSE dipping synthetic normal fault.
definition: WNW-ESE streichende, ca. 65° nach SSE einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
sf touches: Frasshausen Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1197
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Hadern-Laim Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:29.289Z
notation: DE-BY_1126
preferred label: Hadern-Laim Störung @de
definition: WSW-ENE striking, approx. 75° NNW dipping antithethic normal fault underpassing the western precincts of Munich city center.
definition: WSW-ENE streichende, ca. 75° nach NNW einfallende antithetische Abschiebung im Westen der Münchener Innenstadt. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1126
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Föggenbach Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.639Z
notation: DE-BY_1196
definition: W-E striking, approx. 75° N dipping antithetic normal fault running parallel to Humbach-Dietenhausen Fault [DE-BY_1195] in the south.
definition: W-E streichende, ca. 75° nach N einfallende antithetische Abschiebung parallel zur Humbach-Dietenhausen Störung [DE-BY_1195] unmittelbar südlich. @de
preferred label: Föggenbach Störung @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1196
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Pasing-Daglfing Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:29.262Z
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
notation: DE-BY_1125
preferred label: Pasing-Daglfing Störung @de
definition: W-E trending, approx. 60° ± S dipping synthetic normal fault underpassing the northern precincts of Munich city center.
definition: W-E verlaufende, ca. 60° nach ± S einfallende synthetische Abschiebung im Norden der Münchener Innenstadt. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1125
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Humbach-Dietenhausen Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.611Z
notation: DE-BY_1195
preferred label: Humbach-Dietenhausen Störung @de
definition: W-E striking, approx. 75° N dipping antithetic normal fault running parallel to Föggenbeuren Fault [DE-BY_1196] in the north.
definition: W-E streichende, ca. 75° nach N einfallende antithetische Abschiebung parallel zur Föggenbeuren Störung [DE-BY_1196] unmittelbar nördlich. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1195
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Schwabing Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:29.235Z
notation: DE-BY_1124
preferred label: Schwabing Störung @de
definition: WNW-ESE trending, approx. 70° SSW dipping synthetic normal fault underpassing the north of Munich.
definition: WNW-ESE verlaufende, ca. 70° nach SSW einfallende synthetische Abschiebung im Norden Münchens. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1124
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Babenstuben-Sachsenkam Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.584Z
notation: DE-BY_1194
preferred label: Babenstuben-Sachsenkam Störung @de
definition: WNW-ESE striking, approx. 70° NNE dipping antithetic normal fault.
definition: WNW-ESE streichende, ca. 70° nach NNE einfallende antithetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1194
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Milbertshofen Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:29.207Z
notation: DE-BY_886
preferred label: Milbertshofen Störung @de
definition: WSW-ENE striking, approx. 80° SSE dipping synthetic normal fault in the north of Munich.
definition: WSW-ESE streichende, ca. 80° nach SSE einfallende synthetische Abschiebung im Norden von München. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_886
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

[lca_023]
type: Fault
type: Limit
definition: SSW-NNE streichende, ca. 70° nach ESE einfallende Abschiebung. @de
created: 2020-11-23T14:24:51.207Z
notation: DE-BW_103
definition: SSW-NNE striking, approx. 70° ESE dipping normal fault
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6357
references: https://data.geoscience.earth/ncl/geoera/ref/6373
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_025]
type: Fault
type: Limit
created: 2020-11-23T14:24:51.093Z
definition: SW-NE striking, approx. 75° SE dipping normal fault
references: https://data.geoscience.earth/ncl/geoera/ref/6357
definition: SW-NE streichende, ca. 75° nach SE einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6373
type: Concept
notation: DE-BW_065
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_026]
type: Fault
type: Limit
created: 2020-11-23T14:24:51.197Z
notation: DE-BW_100
references: https://data.geoscience.earth/ncl/geoera/ref/6357
definition: WSW-ENE striking, approx. 80° SSE dipping normal fault
references: https://data.geoscience.earth/ncl/geoera/ref/6373
type: Concept
definition: WSW-ENE streichende, ca. 80° nach SSE einfallende Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_020]
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6357
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6373
definition: NW-SE striking, approx. 60° NE dipping normal fault
definition: NW-SE streichende, ca. 60° nach NE einfallende Abschiebung. @de
notation: DE-BW_064
created: 2020-11-23T14:24:51.090Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_021]
type: Fault
type: Limit
definition: SW-NE streichende, ca. 80° nach SE einfallende Abschiebung. @de
definition: SW-NE striking, approx. 80° SE dipping normal fault
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6357
created: 2020-11-23T14:24:51.174Z
notation: DE-BW_093
references: https://data.geoscience.earth/ncl/geoera/ref/6373
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_082]
type: Fault
type: Limit
created: 2020-11-23T14:24:51.305Z
notation: DE-BW_141
definition: SW-NE striking, approx. 70° NW dipping normal fault
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
definition: SW-NE streichende, ca. 70° nach NW einfallende Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_022]
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6357
sf touches: [lca_060]
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6373
notation: DE-BW_091
definition: WSW-ENE streichende, ca. 70° nach NNW einfallende Abschiebung. @de
definition: WSW-ENE striking, approx. 70° NNW dipping normal fault
created: 2020-11-23T14:24:51.168Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_083]
type: Fault
type: Limit
definition: WSW-ENE striking, approx. 65° SSE dipping normal fault
notation: DE-BW_095
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
definition: WSW-ENE streichende, ca. 65° nach SSE einfallende Abschiebung. @de
created: 2020-11-23T14:24:51.180Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_087]
type: Fault
type: Limit
notation: DE-BW_039
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
definition: SW-NE streichende, ca. 80° nach SE einfallende Abschiebung. @de
created: 2020-11-23T14:24:51.022Z
narrower: [hl_088]
definition: SW-NE trending, approx. 80° SE dipping normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_088]
type: Fault
type: Limit
notation: DE-BW_040
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
definition: SSW-NNE striking, approx. 85° WNW dipping normal fault
definition: SSW-NNE streichende, ca. 85° nach WNW einfallende Abschiebung. @de
created: 2020-11-23T14:24:51.023Z
narrower: [hl_089]
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [hl_087]

[hl_089]
type: Fault
type: Limit
notation: DE-BW_041
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
definition: SSW-NNE striking, approx. 85° WNW dipping normal fault
definition: SSW-NNE streichende, ca. 85° nach WNW einfallende Abschiebung. @de
created: 2020-11-23T14:24:51.025Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [hl_088]

[lca_027]
type: Fault
type: Limit
created: 2020-11-23T14:24:51.200Z
definition: WSW-ENE striking, approx. 70° SSE dipping normal fault
notation: DE-BW_101
definition: WSW-ENE streichende, ca. 70° nach SSE einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6357
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6373
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_047]
type: Fault
type: Limit
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
notation: DE-BW_005
definition: SW-NE striking, approx. 70° SE dipping normal fault
created: 2020-11-23T14:24:50.929Z
definition: SW-NE streichende, ca. 70° nach SE einfallende Abschiebung. @de
sf touches: [lca_063]
sf touches: [hl_043]
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_049]
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
notation: DE-BW_070
created: 2020-11-23T14:24:51.105Z
definition: WSW-ENE striking, approx. 65° SSE dipping normal fault
definition: WSW-ENE streichende, ca. 65° nach SSE einfallende Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

Waldhausen-Asten Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:31.831Z
notation: DE-BY_853
preferred label: Waldhausen-Asten Störung @de
definition: W-E striking, approx. 65° S dipping synthetic normal fault.
definition: W-E streichende, ca. 65° nach S einfallende synthetische Abschiebung. @de
narrower: Halsbach Subfault
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_853
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Halsbach Subfault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:31.859Z
notation: DE-BY_854
preferred label: Halsbach Nebenstörung @de
definition: WSW-ENE striking, approx. 70° SSE dipping synthetic normal fault.
definition: WSW-ENE streichende, ca. 70° nach S einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_854
limit type: normalFault
broader: Waldhausen-Asten Fault

Kraiburg-Unterneukirchen Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:31.803Z
notation: DE-BY_1181
preferred label: Kraiburg-Unterneukirchen Störung @de
definition: W-E trending, approx. 65° N dipping antithetic normal fault.
definition: W-E verlaufende, ca. 65° nach N einfallende antithetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1181
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Jettenbach Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:31.776Z
notation: DE-BY_850
preferred label: Jettenbach Störung @de
definition: Slightly undulate, overall W-E trending, approx. 75° S dipping synthetic normal fault south of Waldkraiburg.
definition: Leicht gewellt, ingesamt W-E verlaufende, ca. 75° nach S einfallene synthetische Abschiebung südlich von Waldkraiburg. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_850
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Guggenberg-Erisried Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:31.748Z
notation: DE-BY_1180
preferred label: Guggenberg-Erisried Störung @de
definition: SW-NE striking, approx. 50° SE dipping synthetic normal fault subparallel to Lautrach-Stetten Fault [DE-BY_849].
definition: SW-NE streichende, ca. 50° nach SE einfallende synthetische Abschiebung subparallel zur Lautrach-Stetten Störung [DE-BY_849], @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1180
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Arlesried Fault System
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.378Z
notation: DE-BY_743
preferred label: Arlesried Störungssystem @de
definition: Structure of northward arcuate antithetic normal faults confining oil & gas field Arlesried.
definition: Das Öl- und Gasfeld Arlesried begrenzende Struktur aus nordwärts bogenförmig verlaufenden antithetischen Abschiebungen. @de
narrower: Arlesried Fault
narrower: Arlesried Subfault
narrower: Hohenschlau Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4109
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_743
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Hohenschlau Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.516Z
notation: DE-BY_1114
preferred label: Hohenschlau Störung @de
definition: Northward arcuate, overall WSW-WNE trending, steeply (85°-60°) ± NNW dipping antithetic normal fault south of Arlesried Subfault.
definition: Nordwärts bogenförmig, insgesamt WSW-WNE verlaufende, steil (85°-60°) nach ± NNW einfallende antithetische Abschiebung südlich der Arlesried Parallelstörung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1114
limit type: normalFault
broader: Arlesried Fault System

Arlesried Subfault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.488Z
notation: DE-BY_744
preferred label: Arlesried Parallelstörung @de
definition: Northward arcuate, undulate SW-NE to NW-SE trending, steeply (85°-60°) NW to NE dipping antithetic normal fault southward subparallel to the middle section of Arlesried Fault.
definition: Nordwärts bogenförmig, gewellt SW-NE bis NW-SE verlaufende, steil (85°-60°) nach NW bis NE einfallende antithetische Abschiebung südlich subparallel zum mittleren Abschnitt der Arlesried Störung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4109
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_744
limit type: normalFault
broader: Arlesried Fault System

Arlesried Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.406Z
notation: DE-BY_1111
preferred label: Arlesried Störung @de
definition: Northern boundary of oil & gas field Arlesried. Northward arcuate SW-NE to NW-SE trending, approx. 75° NW to NE dipping antithetic normal fault running from Egg to Oberrieden.
definition: Nördliche Begrenzung des Öl- und Gasfeldes Arlesried. Nordwärts bogenförmig SW-NE bis NW-SE verlaufende, ca. 75° nach NW bis NE einfallende antithetische Abschiebung mit zwischen Egg und Oberrieden. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
narrower: Oberrieden Lateral Fault
narrower: Weilbach Lateral Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1111
limit type: normalFault
broader: Arlesried Fault System

Oberrieden Lateral Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.461Z
notation: DE-BY_1113
preferred label: Oberrieden Querstörung @de
definition: WSW-ENE trending, steeply (85°-60°) NNW dipping antithetic normal fault merging into the far eastern limp of Arlesried Fault.
definition: WSW-ENE verlaufende, steil (85°-60°) nach NNW einfallende antithetische Abschiebung mit Übergang in den äußeren westlichen Ast der Arlesried Störung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1113
limit type: normalFault
broader: Arlesried Fault

Weilbach Lateral Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.433Z
notation: DE-BY_1112
preferred label: Weilbach Querstörung @de
definition: SSW-NNE trending, steeply (85°-60°) WNW dipping antithetic normal fault merging into the eastern limp of Arlesried Fault.
definition: SSW-NNE verlaufende, steil (85°-60°) nach WNW einfallende antithetische Abschiebung mit Übergang in den West-Ast der Arlesried Störung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1112
limit type: normalFault
broader: Arlesried Fault

Lautrach-Stetten Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:31.720Z
notation: DE-BY_849
preferred label: Lautrach-Stetten Störung @de
definition: Overall SW-NE trending, steeply (85°-60°) SE dipping synthetic normal fault running from Iller river to Mindelheim.
definition: Insgesamt SW-NE verlaufende, steil (85°-60°) nach SE einfallende synthetische Abschiebung von der Iller bis nach Mindelheim. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_849
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Grossaitingen Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.350Z
notation: DE-BY_742
preferred label: Großaitingen Störung @de
definition: Northern boundary of oil & gas fields Schwabmünchen and Aitingen. W-E striking, approx. 55° N dipping antithetic normal fault north of Schwabmünchen.
definition: Nördliche Begrenzung der Öl- und Gasfelder Schwabmünchen und Aitingen. W-E streichende, ca. 55° nach N einfallende antithetische Abschiebung nördlich von Schwabmünchen. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4109
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_742
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Lindau-Hergatz Fault
type: Fault
type: Limit
created: 2020-10-09T11:35:31.693Z
notation: DE-BY_846
preferred label: Lindau-Hergatz Störung @de
definition: SW-NE striking, approx. 65° SE dipping synthetic normal fault.
definition: SW-NE streichende, ca. 65° nach SE einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_846
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Haimhausen Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.323Z
notation: DE-BY_741
preferred label: Haimhausen Störung @de
definition: Northern boundary of oil- and gasfield Haimhausen. Northward arcuate, overall SW-NE trending, steeply (85°-60°) NNW to NE dipping antithetic normal fault of the same structure as Herbertshausen Fault [DE-BY_740] to the SW.
definition: Nördliche Begrenzung des Öl- und Gasfeldes Haimhausen. Nordwärts gebogene, insgesamt SW-NE verlaufende, steil (85°-60°) nach NNW bis NE einfallende antithetische Abschiebung derselben Struktur wie die SW gelegene Herbertshausen Störung [DE-BY_740]. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4109
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_741
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Boos Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.571Z
notation: DE-BY_746
preferred label: Boos Störung @de
definition: Northern boundary of oil- and gasfield Boos. Northward curved overall W-E trending, steeply (85°-60°) NW to NE dipping antithetic normal fault.
definition: Nördliche Begrenzung des Öl- und Gasfeldes Boos. Nordwärts gebogene, übergeordnet W-E verlaufende, steil (85°-60°) nach NW bis NE einfallende antithetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4109
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_746
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Tylraching Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:31.914Z
notation: DE-BY_855
preferred label: Tyrlaching Störung @de
definition: W-E to WNW-ESE trending, approx. 65° S to SSW dipping synthetic normal fault.
definition: W-E bis WNW-ESE verlaufende, ca. 65° nach S bis SSW einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_855
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Lauben-Lauberhart Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.543Z
notation: DE-BY_745
preferred label: Lauben-Lauberhart Störung @de
definition: Northern boundary of oil- and gasfields Lauberhart and Lauben. Arc-shaped SW-NE to NW-SE trending, steeply (85°-60°) NW to NE dipping antithetic normal fault.
definition: Nördliche Begrenzung der Öl- und Gasfelder Lauberhart und Lauben. Bogenförmig SW-NE bis NE-SW verlaufende, steil (85°-60°) nach NW bis NE einfallende antithetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4109
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_745
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Kirchweidach Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:31.887Z
notation: DE-BY_1182
preferred label: Kirchweidach Störung @de
definition: WNW-ESE to NW-SW trending, approx. 70° SSW to SW dipping synthetic normal fault running from Thann to Tittmoning.
definition: WNW-ESE bis NW-SW verlaufende, ca. 70° nach SSW bis SW einfallende synthetische Abschiebung zwischen Thann und Tittmoning. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1182
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

[hl_052]
type: Fault
type: Limit
sf touches: [hl_043]
definition: SW-NE striking, approx. 60° SE dipping normal fault
created: 2020-11-23T14:24:51.283Z
definition: SW-NE streichende, ca. 60° nach SE einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: [lca_001]
type: Concept
notation: DE-BW_132
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_053]
type: Fault
type: Limit
created: 2020-11-23T14:24:51.286Z
references: https://data.geoscience.earth/ncl/geoera/ref/4097
definition: SW-NE striking, approx. 80° NW dipping normal fault
type: Concept
definition: SW-NE streichende, ca. 80° nach NW einfallende Abschiebung. @de
notation: DE-BW_133
sf touches: [lca_001]
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_054]
type: Fault
type: Limit
created: 2020-11-23T14:24:51.107Z
definition: SSW-NNE striking, approx. 75° ESE dipping normal fault
definition: SSW-NNE streichende, ca. 75° nach ESE einfallende Abschiebung. @de
notation: DE-BW_071
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_055]
type: Fault
type: Limit
type: Concept
definition: SW-NE streichende, ca. 70° nach SE einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
notation: DE-BW_069
definition: SW-NE striking, approx. 70° SE dipping normal fault
sf touches: [hl_056]
created: 2020-11-23T14:24:51.102Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_056]
type: Fault
type: Limit
definition: W-E streichende, ca. 75° nach S einfallende Abschiebung. @de
definition: W-E striking, approx. 75° S dipping normal fault
notation: DE-BW_074
sf touches: [hl_055]
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
created: 2020-11-23T14:24:51.116Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_057]
type: Fault
type: Limit
definition: SSW-NNE striking, approx. 70° WNW dipping normal fault
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
created: 2020-11-23T14:24:51.110Z
notation: DE-BW_072
sf touches: [lca_001]
definition: SSW-NNE streichende, ca. 70° nach WNW einfallende Abschiebung. @de
sf touches: [lca_063]
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

Oberfeldkirchen Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:31.942Z
notation: DE-BY_1183
preferred label: Oberfeldkirchen Störung @de
definition: WNW-ESE striking, approx. 80° SSW dipping synthetic normal fault.
definition: WNW-ESE streichende, ca. 80° nach SSW einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1183
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

[hl_058]
type: Fault
type: Limit
definition: SSW-NNE streichende, ca. 75° nach WNW einfallende Abschiebung. @de
created: 2020-11-23T14:24:51.113Z
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: [lca_001]
sf touches: [lca_063]
notation: DE-BW_073
type: Concept
definition: SSW-NNE trending, approx. 75° WNW dipping normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

Eurishofen-Waal Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.167Z
notation: DE-BY_868
preferred label: Eurishofen-Waal Störung @de
definition: WSW-ENE striking, approx. 80° SSE dipping synthetic normal fault.
definition: WSW-ENE streichende, ca. 80° nach SSE einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_868
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Warmisried-Altensteig Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.793Z
notation: DE-BY_1121
preferred label: Warmisried-Altensteig Störung @de
definition: SSW-NNE trending, approx. 80° ESE dipping synthetic normal fault running subparallel to antithetic Lauchdorf-Bad Wörishofen Fault [DE-BY_1188] forming a local graben structure.
definition: SSW-NNE ziehende, ca. 80° nach ESE einfallende synthetische Abschiebung. Bildet mit der subparallel verlaufenden antithetischen Lauchdorf-Bad Wörishofen Störung [DE-BY_1188] eine lokale Grabenstruktur. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1121
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Unterschweinbach Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.138Z
notation: DE-BY_865
preferred label: Unterschweinbach Störung @de
definition: W-E striking, approx. 65° N dipping antithetic normal fault.
definition: W-E streichende, ca. 65 nach N einfallende antithetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_865
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Dirlewang-Scheuring Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.766Z
notation: DE-BY_1120
preferred label: Dirlewang-Scheuring Störung @de
definition: Slightly undulate, overall SW-NE trending, averaged approx. 75° SE dipping synthetic normal fault running from south of Mindelheim to the Lech river.
definition: Leicht gewellt, insgesamt SW-NE verlaufende, im Mittel ca. 75° nach SE einfallende synthetische Abschiebung zwischen S von Mindelheim und dem Lech. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1120
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Wolnzach Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.110Z
notation: DE-BY_859
preferred label: Wolnzach Störung @de
definition: WNW-ESE to NW-SE trending, steeply (85°-60°) NNE to NE dipping antithetic normal fault.
definition: WNW-ESE bis NW-SE verlaufende, steil (85°-60°) nach NNE bis NE einfallende antithetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_859
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Mindelheim-Türkheim Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.738Z
notation: DE-BY_1119
preferred label: Mindelheim-Türkheim Störung @de
definition: E-W trending, approx. 70° N dipping antithetic normal fault.
definition: E-W verlaufende, ca. 70° nach N einfallende antithetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1119
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Obing-Altenmarkt Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.082Z
notation: DE-BY_857
preferred label: Obing-Altenmarkt Störung @de
definition: W-E trending, approx. 60° S dipping synthetic normal fault.
definition: W-E verlaufende, ca. 60° nach S einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_857
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Rammingen-Berg Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.710Z
notation: DE-BY_1118
preferred label: Rammingen-Berg Störung @de
definition: WSW-ENE striking, approx. 65° SSE dipping synthetic normal fault.
definition: WSW-ENE streichende, ca. 65° nach SSE einfallende synthetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1118
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Aham-Stockham Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.054Z
notation: DE-BY_1186
preferred label: Aham-Stockham Störung @de
definition: W-E trending, approx. 60° S dipping synthetic normal fault north of Amerang and Obing.
definition: W-E verlaufende, ca. 60° nach S einfallende synthetische Abschiebung nördlich Amerang und Obing. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1186
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Tussenhausen-Siebnach Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.682Z
notation: DE-BY_1117
preferred label: Tussenhausen-Siebnach Störung @de
definition: WSW-ENE trending, approx. 85° SSE dipping synthetic normal fault.
definition: WSW-ENE streichende, ca. 85° nach SSE einfallende synthetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1117
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Wasserburg-Schnaitsee Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.026Z
notation: DE-BY_1185
preferred label: Wasserburg-Schnaitsee Störung @de
definition: W-E striking, approx. 65° S dipping synthetic normal fault.
definition: W-E streichende, ca. 65° nach S einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: Schnaitsee Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1185
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Erlenberg-Tussenhausen Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.654Z
notation: DE-BY_1116
preferred label: Erlenberg-Tussenhausen Störung @de
definition: WSW-ENE trending, approx. 60° SSE dipping synthetic normal fault.
definition: WSW-ENE streichende, ca. 60° nach SSE einfallende synthetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: Benningen-Kammlach Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1116
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Lauberhart-Daxberg Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.626Z
notation: DE-BY_1115
preferred label: Lauberhart-Daxberg Störung @de
definition: WSW-ENE striking, approx. 65° SSE dipping synthetic normal fault.
definition: WSW-ENE streichende, ca. 65° nach SSE einfallende synthetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1115
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Schnaitsee-Trostberg Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:31.970Z
notation: DE-BY_856
preferred label: Schnaitsee-Trostberg Störung @de
definition: WNW-ESE trending, approx. 65° SSW dipping synthetic normal fault.
definition: WNW-ESE verlaufende, ca. 65° nach SSW einfallende synthetische Abschiebung. @de
narrower: Schmidham Subfault
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: Schnaitsee Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_856
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Schmidham Subfault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:31.998Z
notation: DE-BY_1184
preferred label: Schmidham Nebenstörung @de
definition: WSW-ENE striking, approx. 70° SSE dipping synthetic normal fault. Branch of Schnaitsee-Trostberg Fault [DE-BY_856].
definition: WSW-ENE streichende, ca. 70° nach SSE einfallende synthetische Abschiebung. Zweig der Schnaitsee-Trostberg Störung [DE-BY_856]. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1184
limit type: normalFault
broader: Schnaitsee-Trostberg Fault

Niederrieden Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.599Z
notation: DE-BY_747
preferred label: Niederrieden Störung @de
definition: Northern boundary of oil- and gasfield Niederrieden. NW-SE trending, steeply (85°-60°) NNE to NE dipping antithetic normal fault.
definition: Nördliche Begrenzung des Öl- und Gasfeldes Niederrieden. NW-SE verlaufende, steil (85°-60°) nach NNE bis NE einfallende antithetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4109
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_747
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

[lca_001]
type: Fault
type: Limit
definition: W-E streichende, ca. 65° nach N einfallende Abschiebung. @de
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6357
notation: DE-BW_146
sf touches: [hl_052]
references: https://data.geoscience.earth/ncl/geoera/ref/6373
narrower: [lca_029]
definition: W-E trending, approx. 65° N dipping normal fault
sf touches: [hl_057]
created: 2020-11-23T14:24:51.315Z
narrower: [hl_059]
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_059]
type: Fault
type: Limit
definition: WSW-ENE striking, approx. 85° SSE dipping normal fault
created: 2020-11-23T14:24:51.320Z
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
definition: WSW-ENE streichende, ca. 85° nach SSE einfallende Abschiebung. @de
notation: DE-BW_149
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [lca_001]

[lca_029]
type: Fault
type: Limit
sf touches: [hl_057]
definition: SW-NE striking, approx. 50° SE dipping normal fault
notation: DE-BW_147
created: 2020-11-23T14:24:51.316Z
definition: SW-NE streichende, ca. 50° nach SE einfallende Abschiebung. @de
narrower: [lca_077]
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6357
sf touches: [lca_063]
references: https://data.geoscience.earth/ncl/geoera/ref/6373
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [lca_001]

[lca_077]
type: Fault
type: Limit
definition: WNW-ESE striking, approx. 85° NNE dipping normal fault
created: 2020-11-23T14:24:51.318Z
notation: DE-BW_148
references: https://data.geoscience.earth/ncl/geoera/ref/6373
definition: WNW-ESE streichende, ca. 85° nach NNE einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6357
type: Concept
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [lca_029]

[lca_002]
type: Fault
type: Limit
created: 2020-11-23T14:24:51.099Z
sf touches: [lca_012]
definition: WSW-ENE striking, approx. 60° SSE dipping normal fault
sf touches: [hl_075]
definition: WSW-ENE streichende, ca. 60° nach SSE einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6373
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6357
notation: DE-BW_067
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_004]
type: Fault
type: Limit
definition: SW-NE streichende, ca. 85° nach SE einfallende Abschiebung. @de
created: 2020-11-23T14:24:51.074Z
sf touches: [hl_093]
references: https://data.geoscience.earth/ncl/geoera/ref/6357
definition: SW-NE striking, approx. 85° SE dipping normal fault
notation: DE-BW_059
references: https://data.geoscience.earth/ncl/geoera/ref/6373
type: Concept
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

Reichertshofen Fault Scarp
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.849Z
notation: DE-BY_749
preferred label: Reichertshofener Abbruch @de
definition: WNW-ESE striking, steeply (85°-60°) SSW dipping synthetic normal fault south of Ingolstadt, possibly the southern fault scarp (resp. step fault) of the Jurarandbruch [DE-BY_1245]. Continuation further to the (south)east, merging into the Landshut-Neuötting Step Fault, is inferred (Jerz & Schmidt-Kaler 1999, Doppler et al. 2002) but not evidenced yet.
definition: WNW-ESE streichende, steil (85°-60°) nach SSW einfallende synthetische Abschiebung südlich von Ingolstadt. Möglicherweise südliche Abbruchstufe (bzw. Bruchstaffel) des Jurarandbruchs [DE-BY_1245]; eine Fortsetzung nach (Süd-)Osten hin mit Übergang in den Landshut-Neuöttinger Abbruch, wird vermutet (Jerz & Schmidt-Kaler 1999, Doppler et al. 2002), konnte aber bisher nicht nachgewiesen werden. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4083
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4102
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_749
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Stockheim-Buchloe Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.195Z
notation: DE-BY_869
preferred label: Stockheim-Buchloe Störung @de
definition: SW-NE trending, approx. 75° SE dipping synthetic normal fault.
definition: SW-NO verlaufende, ca. 75° nach SE einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: Buchloe-Landsberg Fault
sf touches: Bad Wörishofen Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_869
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

[hl_060]
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/4097
created: 2020-11-23T14:24:51.118Z
notation: DE-BW_075
type: Concept
definition: SW-NE streichende, ca. 65° nach SE einfallende Abschiebung. @de
definition: SW-NE trending, approx. 65° SE dipping normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

Heimertingen Fault System
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.821Z
notation: DE-BY_748
alternative label: Heimertinger Störungsschar @de
preferred label: Heimertingen Störungssystem @de
definition: Structure confining oil and gas field Heimertingen. WSW-ENE and WNW-ESE striking antithetic normal faults with a steep (85°-60°) dip towards NNW, resp. NNE.
definition: Das Öl- und Gasfeld Heimertingen begrenzende Struktur aus WSW-ENE und WNW-ESE streichenden, antithetischen Abschiebungen mit steilem (85°-60°) Einfallen nach NNW bzw. NNE. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4103
references: https://data.geoscience.earth/ncl/geoera/ref/4109
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_748
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

[lca_009]
type: Fault
type: Limit
notation: DE-BW_011
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
definition: W-E striking, approx. 80° S dipping normal fault
definition: W-E streichende, ca. 80° nach S einfallende Abschiebung. @de
created: 2020-11-23T14:24:50.947Z
sf touches: [lca_017]
sf touches: [hl_065]
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_061]
type: Fault
type: Limit
definition: SW-NE trending, approx. 70° NW dipping normal fault
type: Concept
narrower: [hl_010]
sf touches: Saulgau Main Fault
notation: DE-BW_142
references: https://data.geoscience.earth/ncl/geoera/ref/4097
created: 2020-11-23T14:24:51.308Z
definition: SW-NE streichende, ca. 70° nach NW einfallende Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_010]
type: Fault
type: Limit
notation: DE-BW_143
created: 2020-11-23T14:24:51.309Z
references: https://data.geoscience.earth/ncl/geoera/ref/4097
definition: SSW-NNE striking, approx. 65° WNW dipping normal fault
type: Concept
definition: SSW-NNE streichende, ca. 65° nach WNW einfallende Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [hl_061]

[hl_063]
type: Fault
type: Limit
created: 2020-11-23T14:24:50.944Z
notation: DE-BW_010
definition: WSW-ENE striking, approx. 70° NNW dipping normal fault
type: Concept
definition: WSW-ENE streichende, ca. 70° nach NNW einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_065]
type: Fault
type: Limit
sf touches: [hl_023]
definition: SW-NE streichende, ca. 60° nach NW einfallende Abschiebung. @de
sf touches: [hl_022]
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: [lca_017]
type: Concept
notation: DE-BW_013
created: 2020-11-23T14:24:50.952Z
narrower: [hl_072]
definition: SW-NE striking, approx. 60° NW dipping normal fault
sf touches: [lca_009]
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_072]
type: Fault
type: Limit
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
created: 2020-11-23T14:24:50.954Z
definition: SW-NE striking, approx. 75° NW dipping normal fault
definition: SW-NE streichende, ca. 75° nach NW einfallende Abschiebung. @de
sf touches: [lca_017]
notation: DE-BW_068
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [hl_065]

[lca_007]
type: Fault
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
notation: DE-BW_012
created: 2020-11-23T14:24:50.949Z
definition: SSW-NNE striking, approx. 75° ESE dipping normal fault
definition: SSW-NNE streichende, ca. 75° nach ESE einfallende Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
type: Limit
broader: Central Foreland Molasse Basin fault domain

[hl_067]
type: Fault
type: Limit
definition: WNW-ESE striking, approx. 80° NNE dipping normal fault
sf touches: [hl_069]
definition: WNW-ESE streichende, ca. 80° nach NNE einfallende Abschiebung. @de
sf touches: [hl_076]
created: 2020-11-23T14:24:50.964Z
type: Concept
notation: DE-BW_017
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_025]
type: Fault
type: Limit
definition: W-E striking, approx. 75° S dipping normal fault
definition: W-E streichende, ca. 75° nach S einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
notation: DE-BW_029
sf touches: [hl_026]
created: 2020-11-23T14:24:50.996Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_026]
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-11-23T14:24:50.999Z
definition: WSW-ENE striking, approx. 70° SSE dipping normal fault
notation: DE-BW_030
definition: WSW-ENE streichende, ca. 70° nach SSE einfallende Abschiebung. @de
sf touches: [hl_025]
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_028]
type: Fault
type: Limit
notation: DE-BW_015
created: 2020-11-23T14:24:50.959Z
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
definition: SW-NE striking, approx. 70° SE dipping normal fault
definition: SW-NE streichende, ca. 70° nach SE einfallende Abschiebung. @de
narrower: [hl_024]
sf touches: [hl_069]
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_024]
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
definition: SW-NE streichende, ca. 75° nach SE einfallende Abschiebung. @de
notation: DE-BW_016
created: 2020-11-23T14:24:50.961Z
definition: SW-NE striking, approx. 75° SE dipping normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [hl_028]

Irschenberg Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:31.248Z
notation: DE-BY_901
preferred label: Irschenberg Störung @de
definition: WSW-ENE striking, approx. 80° NNW dipping antithetic normal fault.
definition: WSW-ENE streichenede, ca. 80° nach NNW einfallende antithetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_901
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Utting Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:31.359Z
notation: DE-BY_1174
preferred label: Utting Störung @de
definition: W-E striking, approx. 70° N dipping antithetic normal fault.
definition: W-E streichende, ca. 70° nach N einfallende antithetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1174
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Eberfing-Eurasburg Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: Polling-Eberfing Fault
type: Concept
created: 2020-10-09T11:35:31.304Z
notation: DE-BY_835
preferred label: Eberfing-Eurasburg Störung @de
definition: Undulate SW-NE trending, approx. 80° SE dipping synthetic normal fault.
definition: Wellenförmig SW-NE verlaufende, ca. 80° nach SE einfallende synthetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_835
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Miesbach Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:31.276Z
notation: DE-BY_902
preferred label: Miesbach Störung @de
definition: Slightly northward arcuate W-E trending, approx. 70° N dipping antithetic normal fault north of Miesbach.
definition: Leicht nordwärts gekrümmte, W-E verlaufende, ca. 70° nach N einfallende antithetische Abschiebung nördlich von Miesbach. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_902
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

[hl_033]
type: Fault
type: Limit
notation: DE-BW_125
created: 2020-11-23T14:24:51.267Z
definition: SSW-NNE streichende, ca. 80° nach ESE einfallende Abschiebung. @de
sf touches: Rast Fault
sf touches: Schwackenreut Main Fault
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
definition: SSW-NNE striking, approx. 80° ESE dipping normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_035]
type: Fault
type: Limit
created: 2020-11-23T14:24:51.270Z
definition: SW-NE striking, approx. 65° NW dipping normal fault
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
definition: SW-NE streichende, ca. 65° nach NW einfallende Abschiebung. @de
notation: DE-BW_126
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

Deisenhofen-Wächterhof Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.183Z
notation: DE-BY_1110
preferred label: Deisenhofen-Wächterhof Störung @de
definition: WSW-ENE striking, approx. 80° SSE dipping synthetic normal fault.
definition: WSW-ENE streichende, ca. 80° nach SSE einfallende synthetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1110
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Markt Oberdorf Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:31.553Z
notation: DE-BY_1267
preferred label: Markt Oberdorf Störung @de
definition: Undulating WSW-ENE trending, approx. 75° NNW dipping antithetic normal fault running from Kempter Wald to Schongau.
definition: Gewellt WSW-ENE verlaufende, ca. 75° nach NNW einfallende antithetische Abschiebung zwischen Kempter Wald und Schongau. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1267
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Brunnthal Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.155Z
notation: DE-BY_1109
preferred label: Brunnthal Störung @de
definition: WSW-ENE streichende, ca. 85° nach SSE einfallende synthetische Abschiebung; bildet mit der südlich parallel verlaufenden antithetischen Wolfersberg-Moosach Störung [DE-BY_734] eine lokale Grabenstruktur. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
definition: WSW-ENE striking, approx. 85° SSE dipping synthetic normal fault parallel to antithetic Wolfersberg-Moosach Fault [DE-BY_734] forming a local graben structure.
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1109
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Lengenwang Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:31.526Z
notation: DE-BY_1266
preferred label: Lengenwang Störung @de
definition: WSW-ENE trending, approx. 65° NNW dipping antithetic normal fault.
definition: WSW-ENE verlaufende, ca. 65° nach NNW einfallende antithetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1266
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Wolfersberg-Moosach Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.127Z
notation: DE-BY_734
preferred label: Wolfersberg-Moosach Störung @de
definition: Northern boundary of oil- and gasfields Wolfersberg and Moosach. Undulate WSW-ENE trending, averaged approx. 75° NNW dipping antithetic normal fault running from Sauerlach to Forsting.
definition: Nördliche Begrenzung der Öl- und Gasfelder Wolfersberg und Moosach. Gewellt WSW-ENE verlaufende, im Mittel ca. 75° nach NNW einfallende antithetische Abschiebung zwischen Sauerlach und Forsting. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4109
sf touches: Münsing-Brunnthal Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_734
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Lengenwang-Lech Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:31.498Z
notation: DE-BY_838
preferred label: Lengenwang-Lech Störung @de
definition: WSW-ENE trending, approx. 70° SSE dipping synthetic normal fault.
definition: WSW-ENE verlaufende, ca. 70° nach SSE einfallende synthetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_838
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Waging-Kirchanschöring Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.099Z
notation: DE-BY_1108
preferred label: Waging-Kirchanschöring Störung @de
definition: Undulate W-E trending, approx. 55° N dipping antithetic normal fault.
definition: Wellenförmig W-E verlaufende, ca. 55° nach N einfallende antithetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1108
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Königsdorf South Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:31.470Z
notation: DE-BY_837
preferred label: Königsdorf Süd Störung @de
definition: W-E striking, approx. 85° N dipping antithetic normal fault. Subparallel to synthetic Königsdorf North Fault [DE-BY_836], this probably conjugate pair of faults forms a local graben structure.
definition: W-E streichende, ca. 85° nach N einfallende antithetische Abschiebung. Subparallel zur synthetischen Königsdorf Nord Störung [DE-BY_836] bildet dieses wahrscheinlich konjugierte Störungspaar eine lokale Grabenstruktur. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_837
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Königsdorf North Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:31.442Z
notation: DE-BY_836
preferred label: Königsdorf Nord Störung @de
definition: W-E striking, approx. 85° S dipping synthetic normal fault. Subparallel to antithetic Königsdorf South Fault [DE-BY_837], this probably conjugate pair of faults forms a local graben structure.
definition: W-E streichende, ca. 85° nach S einfallende synthetische Abschiebung. Subparallel zur antithetischen Königsdorf Süd Störung [DE-BY_837] bildet dieses wahrscheinlich konjugierte Störungspaar eine lokale Grabenstruktur. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_836
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Schondorf Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:31.414Z
notation: DE-BY_1176
preferred label: Schondorf Störung @de
definition: W-E striking, approx. 70° N dipping antithetic normal fault.
definition: W-E streichende, ca. 70° nach N einfallende antithetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1176
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Finning Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:31.387Z
notation: DE-BY_1175
preferred label: Finning Störung @de
definition: W-E striking, approx. 75° N dipping antithetic normal fault.
definition: W-E streichende, ca. 75° nach N einfallende antithetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1175
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Hebertshausen Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.295Z
notation: DE-BY_740
preferred label: Hebertshausen Störung @de
definition: Northern boundary of oil- and gasfield Hebertshausen. WSW-ENE trending, steeply (85°-60°) NNW dipping antithetic normal fault of the same structure as Haimhausen Fault [DE-BY_741] to the NE.
definition: Nördliche Begrenzung des Öl- und Gasfeldes Hebertshausen. WSW-ENE verlaufende, steil (85°-60°) nach NNW einfallende antithetische Abschiebung derselben Struktur wie die NE gelegene Haimhausen Störung [DE-BY_741]. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4109
sf touches: Einsbach-Dachau Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_740
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Bad Aibling Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.267Z
notation: DE-BY_738
preferred label: Bad Aibling Störung @de
definition: SW-NE striking, steeply (85°-60°) NW dipping antithetic normal fault.
definition: SW-NE streichende, steil (85°-60°) nach NW einfallende antithetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_738
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Schmidhausen-Inzenham-Zaissberg Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:28.211Z
notation: DE-BY_735
preferred label: Schmidhausen-Inzenham-Zaißberg Störung @de
definition: Northward arcuate structure located nearby oil- and gasfields Schmidhausen and Inzenham-Zaissberg. Overall W-E trending, steeply (85°-60°) NW to NNE dipping antithetic normal fault north of Rosenheim.
definition: Nordwärts gebogene Struktur an den Öl- und Gasfeldern Schmidhausen und Inzenham-Zaissberg. Insgesamt W-E verlaufende, steil (85°-60°) nach NW bis NNE einfallende antithetische Abschiebung nördlich von Rosenheim. @de
narrower: Tattenhausen Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4109
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_735
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Tattenhausen Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.240Z
notation: DE-BY_736
preferred label: Tattenhausen Störung @de
definition: SW-NE striking, ca. 70° NW dipping antithetic normal fault. Branch of Schmidhausen-Inzenham-Zaissberg Fault [DE-BY_735].
definition: SW-NE streichende Zweigstörung zur Schmidhausen-Inzenham-Zaissberg Störung [DE-BY_735]; ca. 70° nach NW einfallende antithetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_736
limit type: normalFault
broader: Schmidhausen-Inzenham-Zaissberg Fault

Weitnau-Burggen Train of Faults
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:31.581Z
notation: DE-BY_842
preferred label: Weitnau-Burggen Störungszug @de
definition: WSW-ENE trending, at Kempten veering to W-E, chain of approx. 75° to 85° SSE to S dipping synthetic normal faults.
definition: WSW-ENE verlaufender, bei Kempten auf W-E drehender, ca. 75° bis 85° nach SSE bis S einfallender Störungszug synthetischer Abschiebungen. @de
narrower: Weitnau-Wertach Fault
narrower: Wertach-Stötten Fault
narrower: Wald-Burggen Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_842
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Wertach-Stötten Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
sf touches: Weitnau-Wertach Fault
type: Concept
created: 2020-10-09T11:35:31.636Z
notation: DE-BY_1178
preferred label: Wertach-Stötten Störung @de
definition: W-E trending, approx. 75° S dipping synthetic normal fault south of Markt Oberdorf. In its eastern part, most likely linked via a relay ramp to Wald-Burggen Fault [DE-BY_1179] running subparallel to the south.
definition: W-E verlaufende, ca. 75° nach S einfallende synthetische Abschiebung südlich von Markt Oberdorf. Im östlichen Teil höchstwahrscheinlich über eine Relay Ramp mit der südlich subparallel verlaufenden Wald-Burggen Fault [DE-BY_1179] verbunden. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1178
limit type: normalFault
broader: Weitnau-Burggen Train of Faults

Weitnau-Wertach Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: Wertach-Stötten Fault
type: Concept
created: 2020-10-09T11:35:31.608Z
notation: DE-BY_1177
preferred label: Weitnau-Wertach Störung @de
definition: Slightly undulating, overall WSW-ENE trending, approx. 80-85° SSE dipping synthetic normal fault; interconnection beneath Kempten inferred.
definition: Leicht gewellt, insgesamt WSW-ENE verlaufende, ca. 80-85° nach SSE einfallende synthetische Abschiebung; Verbindung unter Kempten ist nicht gesichert. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1177
limit type: normalFault
broader: Weitnau-Burggen Train of Faults

Wald-Burggen Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:31.665Z
notation: DE-BY_1179
preferred label: Wald-Burggen Störung @de
definition: WSW-ENE trending, approx. 75° SSE dipping synthetic normal fault. In its westernmost part, most likely connected via a relay ramp to Wertach-Stötten Fault [DE-BY_1178] running subparallel to the north.
definition: WSW-ENE verlaufende, ca. 75° nach SSE einfallende synthetische Abschiebung. Im westlichsten Teil höchstwahrscheinlich über eine Relay Ramp mit der nördlich subparallel verlaufenden Wertach-Stötten Störung [DE-BY_1178] verbunden. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1179
limit type: normalFault
broader: Weitnau-Burggen Train of Faults

[hl_040]
type: Fault
type: Limit
notation: DE-BW_127
definition: SW-NE streichende, ca. 70° nach NW einfallende Abschiebung. @de
definition: SW-NE striking, approx. 70° NW dipping normal fault
narrower: Sentenharter Fault
created: 2020-11-23T14:24:51.272Z
narrower: [hl_037]
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_037]
type: Fault
type: Limit
created: 2020-11-23T14:24:51.275Z
definition: SW-NE streichende, ca. 75° nach SE einfallende Abschiebung. @de
definition: SW-NE trending, approx. 75° SE dipping normal fault
notation: DE-BW_129
sf touches: [hl_039]
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [hl_040]

Sentenharter Fault
type: Fault
type: Limit
preferred label: Sentenharter Verwerfung @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
definition: SSW-NNE streichende, ca. 70° nach WNW einfallende Abschiebung. @de
definition: SSW-NNE striking, approx. 70° WNW dipping normal fault
created: 2020-11-23T14:24:51.274Z
notation: DE-BW_128
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [hl_040]

[hl_042]
type: Fault
type: Limit
type: Concept
notation: DE-BW_130
definition: SW-NE striking, approx. 55° NW dipping normal fault
sf touches: Weiherholz Fault
definition: SW-NE streichende, ca. 55° nach NW einfallende Abschiebung. @de
created: 2020-11-23T14:24:51.278Z
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_043]
type: Fault
type: Limit
notation: DE-BW_003
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
definition: N-S streichende, ca. 85° nach W einfallende Abschiebung. @de
sf touches: [hl_052]
created: 2020-11-23T14:24:50.923Z
sf touches: [hl_045]
sf touches: [hl_047]
definition: N-S trending, approx. 85° W dipping normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_044]
type: Fault
type: Limit
notation: DE-BW_131
created: 2020-11-23T14:24:51.280Z
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
sf touches: Weiherholz Fault
definition: SW-NE striking, approx. 70° NW dipping normal fault
definition: SW-NE streichende, ca. 70° nach NW einfallende Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_045]
type: Fault
type: Limit
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
definition: SW-NE striking, approx. 70° NW dipping normal fault
definition: SW-NE streichende, ca. 70° nach NW einfallende Abschiebung. @de
created: 2020-11-23T14:24:50.926Z
sf touches: [lca_063]
notation: DE-BW_004
sf touches: [hl_043]
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_046]
type: Fault
type: Limit
created: 2020-11-23T14:24:51.312Z
definition: SW-NE striking, approx. 65° NW dipping normal fault
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
notation: DE-BW_144
definition: SW-NE streichende, ca. 65° nach NW einfallende Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_003]
type: Fault
type: Limit
definition: SW-NE streichende, ca. 80° nach NW einfallende Abschiebung. @de
created: 2020-11-23T14:24:50.932Z
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: [hl_004]
notation: DE-BW_006
definition: SW-NE striking, approx. 80° NW dipping normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_004]
type: Fault
type: Limit
notation: DE-BW_007
definition: SW-NE striking, approx. 75° SE dipping normal fault
sf touches: [hl_003]
created: 2020-11-23T14:24:50.935Z
definition: SW-NE streichende, ca. 75° nach SE einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_005]
type: Fault
type: Limit
created: 2020-11-23T14:24:50.938Z
notation: DE-BW_008
type: Concept
definition: SW-NE streichende, ca. 75° nach SE einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
definition: SW-NE striking, approx. 75° SE dipping normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_007]
type: Fault
type: Limit
definition: WSW-ENE striking, approx. 70° NNW dipping normal fault
created: 2020-11-23T14:24:50.988Z
notation: DE-BW_026
definition: WSW-ENE streichende, ca. 70° nach NNW einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_008]
type: Fault
type: Limit
created: 2020-11-23T14:24:50.991Z
notation: DE-BW_027
definition: WSW-ENE striking, approx. 75° SSE dipping normal fault
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: [hl_009]
definition: WNW-ESE streichende, ca. 75° nach SSE einfallende Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_009]
type: Fault
type: Limit
definition: SW-NE streichende, ca. 80° nach NW einfallende Abschiebung. @de
notation: DE-BW_028
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-11-23T14:24:50.993Z
sf touches: [lca_017]
sf touches: [hl_008]
definition: SW-NE striking, approx. 80° NW dipping normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

Grünwald Graben Fault System
type: Fault
type: Limit
type: Concept
created: 2020-10-29T12:07:22.001Z
type: SpatialObject
preferred label: Grünwalder Grabenbruch System @de
notation: DE-BY_1343
definition: Subparallel array of WSW-ENE trending normal faults between Lake Starnberg and Oberhaching forming the eastern and western Grünwald Graben. The graben structure is target of the Oberhaching / Grünwald geothermal exploration and production drillings.
definition: Subparallele Abfolge WSW-ENE verlaufender Abschiebungen zwischen dem Starnberger See und Oberhaching die den westlichen und östlichen Grünwald Graben bilden. Die Grabenstruktur ist Ziel der Oberhaching/Grünwald Geothermie-Erkundungs- und Erschließungsbohrungen. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
narrower: Kempfenhausen Fault
narrower: Berg-Strasslach Fault
narrower: Oberhaching Fault
narrower: Schorn-Grünwald Fault
narrower: Grünwalder Forst Fault
narrower: Strasslach-Oberhaching Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1343
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Berg-Strasslach Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:29.750Z
notation: DE-BY_806
preferred label: Berg-Straßlach Störung @de
definition: WSW-ENE, approx. 55° SSE dipping synthetic normal fault.
definition: WSW-ENE streichende, ca. 55° nach SSE einfallende synthetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_806
limit type: normalFault
broader: Grünwald Graben Fault System

Grünwalder Forst Fault
type: Fault
type: Limit
created: 2020-10-29T12:13:56.753Z
type: Concept
type: SpatialObject
preferred label: Grünwalder Forst Störung @de
alternative label: Grünwald Störung @de
definition: Undulate WSW-ENE trending, 80° SSE dipping synthetic normal fault featuring a throw up to 200 m. Northern boundary of eastern Grünwald Graben.
definition: Gewellt WSW-ENE verlaufende, ca. 80° nach SSE einfallende synthetische Abschiebung mit einem Vertikalveratz bis zu 200 m; Nordflanke des östlichen Grünwald Grabens. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
notation: DE-BY_1339
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1339
limit type: normalFault
broader: Grünwald Graben Fault System

Strasslach-Oberhaching Fault
type: Fault
type: Limit
sf touches: Oberhaching Fault
created: 2020-10-29T12:15:46.821Z
type: Concept
type: SpatialObject
preferred label: Straßlach-Oberhaching Störung @de
notation: DE-BY_1340
definition: Slightly undulate WSW-ENE trending, approx. 70° NNW dipping antithetic normal fault featuring a throw of about 80 m. Southern boundary of western and eastern Grünwald Graben.
definition: Leicht gewellt WSW-ENE verlaufende, ca. 70° nach NNW einfallende antithetische Abschiebung mit einer Sprunghöhe von rund 80 m. Südflanke des westlichen und östlichen Grünwald Grabens. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1340
limit type: normalFault
broader: Grünwald Graben Fault System

Kempfenhausen Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.136Z
notation: DE-BY_1091
preferred label: Kempfenhausen Störung @de
definition: SW-NE striking, approx. 80° NW dipping antithetic normal fault.
definition: SW-NE streichende, ca. 80° nach NW einfallende antithetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1091
limit type: normalFault
broader: Grünwald Graben Fault System

Oberhaching Fault
type: Fault
type: Limit
sf touches: Strasslach-Oberhaching Fault
definition: WSW-ENE trending, approx. 80° NNW dipping antithetic normal fault with a minor throw running within eastern Grünwald Graben.
definition: Im östlichen Grünwald Graben WSW-ENE verlaufende, ca. 80° nach NNW einfallende antithetische Abschiebung mit geringem Vertikalversatz. @de
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:26.832Z
notation: DE-BY_823
preferred label: Oberhaching Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_823
limit type: normalFault
broader: Grünwald Graben Fault System

Schorn-Grünwald Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.108Z
notation: DE-BY_1090
preferred label: Schorn-Grünwald Störung @de
definition: SW-NE to E-W trending, approx. 70° SE to S dipping synthetic normal fault.
definition: SW-NE bis E-W verlaufende, ca. 70° nach SE bis S einfallende synthetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
sf touches: Berg-Oberhaching Fault
sf touches: Münsing-Brunnthal Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1090
limit type: normalFault
broader: Grünwald Graben Fault System

Altmühldorf-Tüssling Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.918Z
notation: DE-BY_1221
preferred label: Altmühldorf-Tüßling Störung @de
definition: Slightly northeastward arcuate overall NW-SE trending, approx. 65° ± NE dipping antithetic normal fault. In parts inferred segment of the southwestern boundary of Gifthal Trough, a northwestward widening graben-like structure along the southwestern scarp of Landshut-Neuötting crystalline rise. The apparent segmentation of this borderline, emerging from proved Taufkirchen-Ampfing Fault [DE-BY_793], arguably results from subseismic throws related to flexure-like segments, the incremental onlap of the Gifthal Trough onto the lower step of Landshut-Neuötting rise confined by Fault Scarp 3 [DE-BY_703], and the overthrust caused by Grasset-Wechselberg reverse fault [DE-BY_1224].
definition: Leicht nach NE gebogen, insgesamt NW-SW verlaufende, ca. 65° nach NE einfallende antithetische Abschiebung. Südwestliche Grenze des Gifthal Trogs, einer sich nach NW hin aufweitenden Grabenstruktur entlang des südwestlichen Abbruchs des Landshut-Neuötting Hochs. Die augenscheinliche Segmentierung der Trogflanke, als Fortsetzung der seismisch nachgewiesenen Taufkirchen-Ampfing Störung [DE-BY_793], resultiert aus der abschnittsweisen „Unsichtbarkeit“ in seismischen Profilen, wahrscheinlich bedingt durch subseismische, flexurartige Abschnitte in Verbindung mit dem schleifenden Anstieg auf die unterste Staffel des Landshut-Neuötting Abbruchs, begrenzt von der Abbruchstufe 3 [DE-BY_703], sowie die Überfahrung durch die Grasset-Wechselberg Aufschiebung [DE-BY_1224]. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11681
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11689
notation: LfU-BY_1221
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Taufkirchen-Ampfing Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.890Z
notation: DE-BY_793
alternative label: Taufkirchener Abbruch @de
preferred label: Taufkirchen-Ampfing Störung @de
definition: From WSW-ENE to NW-SE veering, averaged approx. 60° NNW to NE dipping antithetic normal fault. Likewise the close-by Velden Fault [DE-BY_711], this fault north of Dorfen veers from the "Central Molasse Basin" characteristic strike to the "Lower Bavaria Molasse Basin" characteristic trend when approaching the Landshut-Neuötting crystalline rise. Continuing as Altmühldorf-Tüssling Fault [DE-BY_1221] along the southwestern flank of Gifthal Trough, finally vanishing at the onlap of Gifthal Trough onto the stepped flank of Landshut-Neuötting crystalline rise [DE-BY_700].
definition: Von WSW-ENE auf NW-SE Verlauf drehend, im Mittel ca. 60° nach NNW bis NE einfallende antithetische Abschiebung nördlich von Dorfen. Gleich wie bei der nordöstlich gelegenen Velden Störung, folgt der Verlauf dieser Störung in ihrem westlichen Teil der für die zentrale Vorlandmolasse typischen Richtung und dreht mit Annäherung an das Landshut-Neuötting Hoch auf herzynische, für das Niederbayerische Molassebecken charakteristische Richtung und zieht sich als Altmühldorf-Tüßling Störung [DE-BY_1221], entlang der südwestlichen Flanke des Gifthal Trogs, der sich schleifend auf den Landshut-Neuötting Abbruch [DE-BY_700] zieht. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4119
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11681
limit to: https://data.geoscience.earth/ncl/geoera/geoconnect3d/units/11689
notation: LfU-BY_793
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Isnerberg-Unterried Fault
type: Fault
type: Limit
created: 2020-10-29T12:22:31.766Z
type: Concept
type: SpatialObject
preferred label: Isnerberg-Unterried Störung @de
notation: DE-BY_1341
definition: N-S striking, approx. 60° E dipping antithetic normal fault.
definition: N-S streichende, ca. 60° nach E einfallenden antithetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1341
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

[hl_133]
type: Fault
type: Limit
definition: NNW-SSE streichende, ca. 85° nach WSW einfallende Abschiebung. @de
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
definition: NNW-SSE striking, approx. 85° WSW dipping normal fault
created: 2020-11-23T14:24:51.043Z
notation: DE-BW_048
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_013]
type: Fault
type: Limit
definition: SW-NE striking, approx. 65° NW dipping normal fault
notation: DE-BW_140
created: 2020-11-23T14:24:51.303Z
definition: SW-NE streichende, ca. 65° nach NW einfallende Abschiebung. @de
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_015]
type: Fault
type: Limit
created: 2020-11-23T14:24:50.941Z
definition: SW-NE streichende, ca. 70° nach SE einfallende Abschiebung. @de
notation: DE-BW_009
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: [hl_019]
definition: SW-NE striking, approx. 70° SE dipping normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_016]
type: Fault
type: Limit
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
notation: DE-BW_024
definition: SW-NE striking, approx. 65° NW dipping normal fault
created: 2020-11-23T14:24:50.982Z
sf touches: [hl_019]
definition: SW-NE streichende, ca. 65° nach NW einfallende Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_017]
type: Fault
type: Limit
definition: SW-NE streichende, ca. 75° nach NW einfallende Abschiebung. @de
created: 2020-11-23T14:24:50.985Z
notation: DE-BW_025
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
definition: SW-NE striking, approx. 75° NW dipping normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_019]
type: Fault
type: Limit
created: 2020-11-23T14:24:50.969Z
sf touches: [hl_015]
definition: W-E streichende, ca. 65° nach S einfallende Abschiebung. @de
definition: W-E striking, approx. 65° S dipping normal fault
sf touches: [hl_061]
sf touches: [hl_023]
notation: DE-BW_019
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
sf touches: [hl_016]
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

Haindlfing-Erlau Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:30.940Z
notation: DE-BY_1165
preferred label: Haindlfing-Erlau Störung @de
definition: W-E to WNW-ESE trending, approx. 75° N to NNE dipping antithetic normal fault north of Freising. Conjugate with synthetic Burghausen-Zolling Fault [DE-BY_827] it forms a wedge-shaped graben structure levelling out to the east.
definition: W-E bis WNW-ESE verlaufende, ca. 75° nach N bis NNE einfallende antithetische Abschiebung nördlich von Freising. Bildet zusammen mit der synthetischen Burghausen-Zolling Störung [DE-BY_827] eine keilförmige, nach Osten auslaufende Grabenstruktur. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1165
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Thalhausen Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:30.913Z
notation: DE-BY_1164
preferred label: Thalhausen Störung @de
definition: WSW-ENE striking, approx. 85° SSE dipping synthetic normal fault NW of Freising.
definition: WSW-ENE streichende, ca. 85° nach SSE einfallende synthetische Abschiebung NW von Freising. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1164
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Giggenhausen Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:30.885Z
notation: DE-BY_1163
preferred label: Giggenhausen Störung @de
definition: W-E trending, approx. 65° S dipping synthetic normal fault SW of Freising
definition: W-E verlaufende, ca. 65° nach S einfallende synthetische Abschiebung SW von Freising. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1163
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Burghausen-Zolling Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:30.857Z
notation: DE-BY_827
preferred label: Burghausen-Zolling Störung @de
definition: WSW-ENE trending, approx. 80° SSE dipping synthetic normal fault north of Freising.
definition: WSW-ENE verlaufende, ca. 80° nach SSE einfallende synthetische Abschiebung nördlich von Freising. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_827
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Grossnöbach-Pulling Fault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:30.830Z
notation: DE-BY_826
preferred label: Großnöbach-Pulling Störung @de
definition: Slightly undulated overall W-E trending, approx. 65° ± S dipping synthetic normal fault southwest of Freising.
definition: Leicht wellenförmig W-E verlaufende, ca. 65° nach ± S einfallende synthetische Abschiebung südwestlich von Freising. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_826
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Nesselwang-Steingaden Fault System
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:31.080Z
notation: DE-BY_1167
preferred label: Nesselwang-Steingaden Störungssystem @de
definition: WSW-ENE trending array of steeply dipping normal faults underneath the Subalpine Molasse. The faults of this array in sections are forming local graben structures with the northward subparallel Rückholz Fault [DE-BY_841].
definition: WSW-ENE verlaufende Gruppe steil einfallender Abschiebungen unter der Faltenmolasse. Südlich subparallel zur Rückholz Störung [DE-BY_841], mit der die Teilstörungen abschnittsweise lokale Grabenstrukturen bilden. @de
narrower: Maria Rain Fault
narrower: Seeg Fault
narrower: Seeg-Steingaden Fault
narrower: Lechbruck Fault
narrower: Rosshaupten-Prem Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1167
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Rosshaupten-Prem Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:31.220Z
notation: DE-BY_1172
preferred label: Roßhaupten-Prem Störung @de
definition: WSW-ENE striking, approx. 85° SSE dipping synthetic normal fault
definition: WSW-ENE streichende, ca. 85° nach SSE einfallende synthetische Abschiebung @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1172
limit type: normalFault
broader: Nesselwang-Steingaden Fault System

Lechbruck Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:31.191Z
notation: DE-BY_1171
preferred label: Lechbruck Störung @de
definition: WSW-ENE striking, approx. 80° SSE dipping synthetic normal fault
definition: WSW-ENE streichende, ca. 80° nach SSE einfallende synthetische Abschiebung @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1171
limit type: normalFault
broader: Nesselwang-Steingaden Fault System

Seeg-Steingaden Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:31.163Z
notation: DE-BY_1170
preferred label: Seeg-Steingaden Störung @de
definition: Undulate WSW-ENE trending, approx. 65° NNW dipping antithetic normal fault.
definition: Gewellt WSW-ENE verlaufende, ca. 65° nach NNW einfallende antithetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1170
limit type: normalFault
broader: Nesselwang-Steingaden Fault System

Seeg Fault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:31.135Z
notation: DE-BY_1169
preferred label: Seeg Störung @de
definition: WSW-ENE striking, approx. 75° SSE dipping synthetic normal fault
definition: WSW-ENE streichende, ca. 75° nach SSE einfallende synthetische Abschiebung @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1169
limit type: normalFault
broader: Nesselwang-Steingaden Fault System

Maria Rain Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:31.107Z
notation: DE-BY_1168
preferred label: Maria Rain Störung @de
definition: WSW-ENE striking, approx. 75° NNE dipping antithetic normal fault.
definition: WSW-ENE streichende, ca. 75° nach NNE einfallende antithetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1168
limit type: normalFault
broader: Nesselwang-Steingaden Fault System

Rückholz Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: Oberreute-Oy-Mittelberg Fault
type: Concept
created: 2020-10-09T11:35:31.052Z
notation: DE-BY_841
preferred label: Rückholz Störung @de
definition: W-E to WSW-ENE trending, approx. 65° S to SSE dipping synthetic normal fault.
definition: W-E bis WSW-ENE verlaufende, ca. 65° nach S bis SSE einfallende synthetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_841
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Waltenhofen-Görisried Faults
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:31.024Z
notation: DE-BY_1166
preferred label: Waltenhofen-Görisried Störungen @de
definition: Group of WSW-ENE to WNW-ESE striking, steeply (85°-60°) dipping syn- and antithetic normal faults southwest of Kempten, in between Weitnau-Wertach Fault [DE-BY_1177] to the north and Oberreute-Oy-Mittelberg Fault [DE-BY_832] to the south.
definition: Gruppe WSW-ENE bis WNW-ESE streichender, steil (85°-60°) einfallender syn- und antithetischer Abschiebungen SW von Kempten zwischen der Weitnau-Wertach Störung [DE-BY_1177] im Norden und der Oberreute-Oy-Mittelberg Störung [DE-BY_832] im Süden. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1166
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Oberreute-Oy-Mittelberg Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
sf touches: Rückholz Fault
type: Concept
created: 2020-10-09T11:35:30.996Z
notation: DE-BY_832
preferred label: Oberreute-Oy-Mittelberg Störung @de
definition: Overall WSW-ENE trending, on average, approx. 75° SSE dipping synthetic normal fault, linked to Rückholz Fault [DE-BY_841] in the east.
definition: Insgesamt WSW-ENE streichende, durchschnittlich ca. 75° nach SSE einfallende synthetische Abschiebung die sich im Osten in der Rückholz Störung [DE-BY_841] fortsetzt. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_832
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Kirchdorf-Thonhausen Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:30.968Z
notation: DE-BY_828
preferred label: Kirchdorf-Thonhausen Störung @de
definition: W-E to WSW-ENE trending, approx. 65° S to SSE dipping synthetic normal fault north of Freising.
definition: W-E bis WSW-ENE verlaufende, ca. 65° nach S bis SSE einfallende synthetische Abschiebung nördlich von Freising. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_828
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

[hl_020]
type: Fault
type: Limit
type: Concept
created: 2020-11-23T14:24:50.972Z
references: https://data.geoscience.earth/ncl/geoera/ref/4097
notation: DE-BW_020
definition: WSW-ENE streichende, ca. 65° nach SSE einfallende Abschiebung. @de
definition: WSW-ENE striking, approx. 65° SSE dipping normal fault
sf touches: [hl_022]
sf touches: [hl_061]
narrower: [hl_021]
sf touches: [hl_023]
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_021]
type: Fault
type: Limit
definition: SW-NE streichende, ca. 85° nach SE einfallende Abschiebung. @de
definition: SW-NE striking, approx. 85° SE dipping normal fault
type: Concept
notation: DE-BW_021
references: https://data.geoscience.earth/ncl/geoera/ref/4097
created: 2020-11-23T14:24:50.973Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [hl_020]

[hl_022]
type: Fault
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
created: 2020-11-23T14:24:50.976Z
definition: SW-NE striking, approx. 70° SE dipping normal fault
sf touches: [hl_020]
notation: DE-BW_022
definition: SW-NE streichende, ca. 70° nach SE einfallende Abschiebung. @de
sf touches: [hl_065]
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
type: Limit
broader: Central Foreland Molasse Basin fault domain

[hl_023]
type: Fault
type: Limit
sf touches: [hl_065]
definition: SW-NE streichende, ca. 70° nach SE einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
notation: DE-BW_023
created: 2020-11-23T14:24:50.979Z
definition: SW-NE striking, approx. 70° SE dipping normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

Schwackenreut Main Fault
type: Fault
type: Limit
sf touches: [hl_033]
notation: DE-BW_157
definition: SW-NE striking, approx. 65° NW dipping normal fault/fault zone, downthrow of SE-block about 40 m.
preferred label: Schwackenreuter Störungszone @de
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6390
definition: SW-NE streichende, ca. 65° nach NW einfallende Abschiebung, NW-Teil etwa 40 m abgesunken @de
created: 2020-11-23T14:24:51.337Z
references: https://data.geoscience.earth/ncl/geoera/ref/6370
narrower: Schwackenreut Subfault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

Schwackenreut Subfault
type: Fault
type: Limit
type: Concept
notation: DE-BW_158
definition: WSW-ENE streichende, ca. 70° nach NNW einfallende Abschiebung. @de
preferred label: Nebenstörung Schwackenreuter Verwerfung @de
created: 2020-11-23T14:24:51.338Z
definition: WSW-ENE striking, approx. 70° NNW dipping normal fault.
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Schwackenreut Main Fault

Saulgau Main Fault
type: Fault
type: Limit
notation: DE-BW_154
references: https://data.geoscience.earth/ncl/geoera/ref/6390
references: https://data.geoscience.earth/ncl/geoera/ref/6370
sf touches: [hl_061]
preferred label: Saulgauer Hauptverwerfung @de
created: 2020-11-23T14:24:51.331Z
definition: WSW-ENE bis SW-NE streichende, ca. 70° nach NNW bis NW einfallende Störungszone, NW-Teil abgesunken, max. 200 m vertikaler Versatzbetrag @de
definition: WSW-ENE to SW-NE trending, approx 70° NNW to NW dipping normal fault system, downthrow of NW-part max 200 m
narrower: [hl_010_b]
narrower: [hl_011]
type: Concept
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_011]
type: Fault
type: Limit
definition: SW-NE streichende, ca. 80° nach NW einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
definition: SW-NE striking, approx. 80° NW dipping normal fault
notation: DE-BW_156
created: 2020-11-23T14:24:51.334Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Saulgau Main Fault

[hl_010_b]
type: Fault
type: Limit
created: 2020-11-23T14:24:51.333Z
notation: DE-BW_155
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
definition: SW-NE striking, approx. 70° NW dipping normal fault
definition: SW-NE streichende, ca. 70° nach NW einfallende Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Saulgau Main Fault

Bad Waldsee Fault Zone
type: Fault
type: Limit
narrower: [lca_006_a]
preferred label: Störungszone Bad Waldsee @de
definition: NE-SW trending fault zone, downthrow of SE-block max. 25 m.
definition: NE-SW streichende Störungszone, SE-Scholle max. 25 m abgesunken. @de
type: Concept
created: 2020-11-23T14:24:51.341Z
narrower: [hl_105]
narrower: [lca_054]
notation: DE-BW_901
references: https://data.geoscience.earth/ncl/geoera/ref/6390
references: https://data.geoscience.earth/ncl/geoera/ref/6370
narrower: [hl_104]
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_104]
type: Fault
type: Limit
type: Concept
notation: DE-BW_164
narrower: [hl_112]
references: https://data.geoscience.earth/ncl/geoera/ref/4097
definition: SSW-NNE streichende, ca. 60° nach ESE einfallende Abschiebung. @de
definition: SSW-NNE striking, approx. 60° ESE dipping normal fault.
created: 2020-11-23T14:24:51.350Z
sf touches: [hl_100]
sf touches: [lca_006_b]
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Bad Waldsee Fault Zone

[hl_112]
type: Fault
type: Limit
definition: NNW-SSE streichende, ca. 70° nach ENE einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-11-23T14:24:51.352Z
definition: NNW-SSE striking, approx. 70° ENE dipping normal fault.
notation: DE-BW_165
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [hl_104]

[hl_105]
type: Fault
type: Limit
sf touches: [hl_100]
definition: SW-NE streichende, ca. 65° nach SE einfallende Abschiebung. @de
definition: SW-NE striking, approx. 65° SE dipping normal fault.
narrower: [hl_111]
type: Concept
created: 2020-11-23T14:24:51.343Z
sf touches: [lca_006_a]
references: https://data.geoscience.earth/ncl/geoera/ref/4097
notation: DE-BW_159
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Bad Waldsee Fault Zone

[hl_111]
type: Fault
type: Limit
definition: SSW-NNE streichende, ca. 85° nach WNW einfallende Abschiebung. @de
definition: SSW-NNE striking, approx. 85° WNW dipping normal fault.
type: Concept
created: 2020-11-23T14:24:51.344Z
notation: DE-BW_160
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [hl_105]

[lca_054]
type: Fault
type: Limit
notation: DE-BW_161
definition: NW-SE streichende, ca. 50° nach NE einfallende Abschiebung. @de
created: 2020-11-23T14:24:51.345Z
references: https://data.geoscience.earth/ncl/geoera/ref/6373
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6357
definition: NW-SE striking, approx. 50° NE dipping normal fault.
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Bad Waldsee Fault Zone

[lca_006_a]
type: Fault
type: Limit
sf touches: [hl_105]
definition: WSW-ENE striking, approx. 55° SSE dipping normal fault.
references: https://data.geoscience.earth/ncl/geoera/ref/6373
created: 2020-11-23T14:24:51.347Z
notation: DE-BW_162
type: Concept
definition: WSW-ENE streichende, ca. 55° nach SSE einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6357
narrower: [lca_006_b]
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Bad Waldsee Fault Zone

[lca_006_b]
type: Fault
type: Limit
notation: DE-BW_163
references: https://data.geoscience.earth/ncl/geoera/ref/6373
created: 2020-11-23T14:24:51.349Z
sf touches: [hl_104]
references: https://data.geoscience.earth/ncl/geoera/ref/6357
definition: WSW-ENE trending, approx. 80° SSE dipping normal fault.
definition: WSW-ENE streichende, ca. 80° nach SSE einfallende Abschiebung. @de
type: Concept
sf touches: [hl_103]
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [lca_006_a]

Traunreut Step Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.878Z
notation: DE-BY_731
preferred label: Traunreut Bruchstaffel @de
definition: Structure located nearby oil- and gasfield Traunreut. Staggered array of roughly W-E trending ± 60° S dipping synthetic normal faults.
definition: Am Öl- und Gasfeld Traunreut gelegene, ungefähr W-E verlaufende Bruchstaffel von ± 60° nach S einfallenden synthetischen Abschiebungen. @de
narrower: Seeon-Traunreut Fault
narrower: Truchtlaching-Traunreut Fault
narrower: Hörpolding Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4109
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_731
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Hörpolding Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.960Z
notation: DE-BY_1106
preferred label: Hörpolding Störung @de
definition: WSW-ENE striking, approx. 60° SSE dipping fault scarp of the Traunreut Step Fault.
definition: WSW-ENE streichende, ca. 60° nach SSE einfallende Bruchstufe der Traunreut Bruchstaffel. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1106
limit type: normalFault
broader: Traunreut Step Fault

Truchtlaching-Traunreut Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.933Z
notation: DE-BY_1105
preferred label: Truchtlaching-Traunreut Störung @de
definition: W-E to WSW-ENE striking, approx. 60° S to SSE dipping fault scarp of the Traunreut Step Fault.
definition: W-E bis WSW-ENE streichende, ca. 60° südfallende Bruchstufe der Traunreut Bruchstaffel. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1105
limit type: normalFault
broader: Traunreut Step Fault

Seeon-Traunreut Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.905Z
notation: DE-BY_1104
preferred label: Seeon-Traunreut Störung @de
definition: W-E striking, approx. 60° S dipping fault scarp of the Traunreut Step Fault.
definition: W-E streichende, ca. 60° südfallende Bruchstufe der Traunreut Bruchstaffel. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1104
limit type: normalFault
broader: Traunreut Step Fault

[hl_106]
type: Fault
type: Limit
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
created: 2020-11-23T14:24:51.005Z
notation: DE-BW_032
definition: WSW-ENE striking, approx. 65° SSE dipping normal fault
definition: WSW-ENE streichende, ca. 65° nach SSE einfallende Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

Ilmensee-Fronhofen-Aulendorf Fault Zone
type: Fault
type: Limit
preferred label: Störungszone Ilmensee-Fronhofen-Aulendorf @de
definition: SW-NE streichende Störungszone, NW-Teil abgesunken, max. 100 m vertikaler Versatzbetrag. @de
type: Concept
created: 2020-11-23T14:24:51.360Z
notation: DE-BW_903
narrower: [hl_084]
narrower: [hl_076]
references: https://data.geoscience.earth/ncl/geoera/ref/6390
definition: SW-NE trending fault zone, downthrown of NW-block max. 100 m
references: https://data.geoscience.earth/ncl/geoera/ref/6370
narrower: [hl_081]
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_081]
type: Fault
type: Limit
definition: SW-NE striking, approx. 70° NW dipping normal fault. Northern boundary of Frohnhofen-Illensee oil and gas fields.
sf touches: [lca_055]
type: Concept
notation: DE-BW_172
references: https://data.geoscience.earth/ncl/geoera/ref/4097
definition: SW-NE streichende, ca. 70° nach NW einfallende Abschiebung. Nordgrenze der Öl- und Gasfelder Frohnhofen-Illmensee. @de
narrower: [lca_065]
references: https://data.geoscience.earth/ncl/geoera/ref/4109
narrower: [hl_097_b]
created: 2020-11-23T14:24:51.366Z
narrower: [hl_085]
narrower: [lca_008]
sf touches: [hl_075]
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Ilmensee-Fronhofen-Aulendorf Fault Zone

[lca_065]
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6373
type: Concept
notation: DE-BW_174
definition: SSW-NNE streichende, ca. 75° nach ESE einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6357
definition: SSW-NNE striking, approx. 75° ESE dipping normal fault.
created: 2020-11-23T14:24:51.370Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [hl_081]

[hl_085]
type: Fault
type: Limit
type: SpatialObject
definition: WNW-ESE streichende, ca. 75° nach NNE einfallende Abschiebung. @de
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
created: 2020-11-23T14:24:51.373Z
notation: DE-BW_175
definition: WNW-ESE striking, approx. 75° NNE dipping normal fault.
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [hl_081]

[hl_097_b]
type: Fault
type: Limit
notation: DE-BW_169
created: 2020-11-23T14:24:51.371Z
definition: WSW-ENE striking, approx. 80° SSE dipping normal fault.
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
definition: WSW-ENE streichende, ca. 80° nach SSE einfallende Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [hl_081]

[lca_008]
type: Fault
type: Limit
notation: DE-BW_173
definition: WSW-ENE striking, approx. 80° SSE dipping normal fault.
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6357
references: https://data.geoscience.earth/ncl/geoera/ref/6373
created: 2020-11-23T14:24:51.368Z
definition: WSW-ENE streichende, ca. 80° nach SSE einfallende Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [hl_081]

[hl_084]
type: Fault
type: Limit
notation: DE-BW_171
created: 2020-11-23T14:24:51.365Z
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
definition: SW-NE striking, approx. 75° SE dipping normal fault.
definition: SW-NE streichende, ca. 75° nach SE einfallende Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Ilmensee-Fronhofen-Aulendorf Fault Zone

[hl_076]
type: Fault
type: Limit
sf touches: [hl_092]
type: Concept
created: 2020-11-23T14:24:51.362Z
references: https://data.geoscience.earth/ncl/geoera/ref/4097
notation: DE-BW_168
narrower: [hl_097]
definition: WSW-ENE trending, approx. 65° NNW dipping normal fault.
definition: WSW-ENE streichende, ca. 65° nach NNW einfallende Abschiebung. @de
sf touches: [hl_075]
sf touches: [hl_067]
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Ilmensee-Fronhofen-Aulendorf Fault Zone

[hl_097]
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/4097
created: 2020-11-23T14:24:51.364Z
type: Concept
notation: DE-BW_193
definition: WSW-ENE striking, approx. 75° SSE dipping normal fault.
definition: WSW-ENE streichende, ca. 75° nach SSE einfallende Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [hl_076]

Innthal-Mauerkirchen Fault
type: Fault
type: Limit
preferred label: Innthal-Mauerkirchen Störung @de
definition: W-E striking, approx. 70° S dipping synthetic normal fault south of Bad Endorf.
definition: W-E streichende, ca. 70° nach S einfallende synthetische Abschiebung südlich von Bad Endorf. @de
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.850Z
notation: DE-BY_1103
references: https://data.geoscience.earth/ncl/geoera/ref/4082
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1103
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Eichberg-Kirchdorf a.d. Iller Fault Zone
type: Fault
type: Limit
definition: Flaches SE-NW verlaufendes Grabensystem. @de
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6390
references: https://data.geoscience.earth/ncl/geoera/ref/6370
created: 2020-11-23T14:24:51.355Z
preferred label: Störungszone Eichberg-Kirchdorf a.d. Iller @de
narrower: [hl_107]
notation: DE-BW_902
definition: Shallow SE-NW trending graben system.
narrower: [hl_113]
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_113]
type: Fault
type: Limit
definition: SW-NE striking, approx. 65° SE dipping normal fault.
notation: DE-BW_167
created: 2020-11-23T14:24:51.358Z
definition: SW-NE streichende, ca. 65° nach SE einfallende Abschiebung. @de
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Eichberg-Kirchdorf a.d. Iller Fault Zone

[hl_107]
type: Fault
type: Limit
created: 2020-11-23T14:24:51.356Z
notation: DE-BW_166
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
definition: WSW-ENE striking, approx. 70° NNW dipping normal fault.
definition: WSW-ENE streichende, ca. 70° nach NNW einfallende Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Eichberg-Kirchdorf a.d. Iller Fault Zone

Bad Endorf Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.823Z
notation: DE-BY_1102
preferred label: Bad Endorf Störung @de
definition: W-E striking, approx. 80° S dipping synthetic normal fault.
definition: W-E streichende, ca. 80° nach S einfallende synthetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1102
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Ochsenhausen-Kirchberg a.d. Iller Fault Zone
type: Fault
type: Limit
preferred label: Störungszone Ochsenhausen-Kirchberg a.d. Iller @de
definition: NE-SW streichende Störungszone, NW-Teil max. 50 m abgesunken. @de
created: 2020-11-23T14:24:51.400Z
type: Concept
definition: NE-SW trending fault zone, downthrown of NW-part max. 50 m.
notation: DE-BW_905
narrower: [hl_092]
references: https://data.geoscience.earth/ncl/geoera/ref/6370
references: https://data.geoscience.earth/ncl/geoera/ref/6390
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_092]
type: Fault
type: Limit
sf touches: [hl_076]
sf touches: [hl_100]
definition: SW-NE streichende, ca. 65° nach NW einfallende Abschiebung. @de
narrower: [hl_091]
type: Concept
narrower: [hl_099]
references: https://data.geoscience.earth/ncl/geoera/ref/4097
notation: DE-BW_190
created: 2020-11-23T14:24:51.401Z
narrower: [hl_095]
definition: SW-NE striking, approx. 65° NW dipping normal fault.
narrower: [hl_103]
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Ochsenhausen-Kirchberg a.d. Iller Fault Zone

[hl_103]
type: Fault
type: Limit
definition: SW-NE striking, approx. 75° NW dipping normal fault.
sf touches: [lca_006_b]
definition: SW-NE streichende, ca. 75° nach NW einfallende Abschiebung. @de
notation: DE-BW_195
created: 2020-11-23T14:24:51.406Z
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [hl_092]

[hl_091]
type: Fault
type: Limit
created: 2020-11-23T14:24:51.403Z
sf touches: [lca_055]
sf touches: [hl_090]
definition: N-S striking, approx. 70° W dipping normal fault.
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
definition: N-S streichende, ca. 70° nach W einfallende Abschiebung. @de
notation: DE-BW_191
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [hl_092]

[hl_095]
type: Fault
type: Limit
type: Concept
created: 2020-11-23T14:24:51.407Z
references: https://data.geoscience.earth/ncl/geoera/ref/4097
definition: SW-NE streichende, ca. 65° nach NW einfallende Abschiebung. @de
notation: DE-BW_192
definition: SW-NE striking, approx. 65° NW dipping normal fault.
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [hl_092]

[hl_099]
type: Fault
type: Limit
created: 2020-11-23T14:24:51.404Z
definition: N-S streichende, ca. 80° nach W einfallende Abschiebung. @de
notation: DE-BW_194
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
definition: N-S striking, approx. 80° W dipping normal fault.
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [hl_092]

Almertsham Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.796Z
notation: DE-BY_730
preferred label: Almertsham Störung @de
definition: Structure located nearby oil- and gasfield Almertsham. Slightly northward arcuate W-E trending, approx. 60° N dipping antithetic normal fault north of Bad Endorf.
definition: Am Öl- und Gasfeld Almertsham gelegene, leicht nordwärts gebogene, W-E verlaufende, ca. 60° nach N einfallende antithetische Abschiebung nördlich von Bad Endorf. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4109
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_730
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

[hl_109]
type: Fault
type: Limit
created: 2020-11-23T14:24:51.030Z
notation: DE-BW_043
definition: SSW-NNE streichende, ca. 60° nach ESE einfallende Abschiebung. @de
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
definition: SSW-NNE striking, approx. 60° ESE dipping normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

Mönchsrot-Ellwangen (Ellbach) Fault Zone
type: Fault
type: Limit
narrower: [hl_126]
narrower: [hl_128]
narrower: [hl_137]
narrower: [hl_114]
narrower: [hl_127]
preferred label: Störungszone Mönchsrot-Ellwangen (Ellbach) @de
references: https://data.geoscience.earth/ncl/geoera/ref/6370
references: https://data.geoscience.earth/ncl/geoera/ref/6390
definition: SW-NE streichende Störungszone, NW -Scholle etwa 50 m abgesunken. @de
definition: SW-NE trending fault zone, downthrow of NW-block about 50 m.
narrower: [hl_129]
type: Concept
narrower: [lca_052]
narrower: [lca_051]
narrower: [lca_049]
created: 2020-11-23T14:24:51.376Z
narrower: [hl_124]
notation: DE-BW_904
narrower: [hl_125]
type: SpatialObject
narrower: [hl_108]
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_124]
type: Fault
type: Limit
definition: Slightly undulate SW-NE striking, approx. 65° NW dipping normal fault.
references: https://data.geoscience.earth/ncl/geoera/ref/4097
notation: DE-BW_184
type: Concept
created: 2020-11-23T14:24:51.389Z
type: SpatialObject
definition: Leicht gewellt SW-NE verlaufende, ca. 65° nach NW einfallende Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Mönchsrot-Ellwangen (Ellbach) Fault Zone

[hl_114]
type: Fault
type: Limit
notation: DE-BW_176
definition: SW-NE streichende, ca. 70° nach NW einfallende Abschiebung. @de
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
narrower: [hl_131]
narrower: [hl_132]
created: 2020-11-23T14:24:51.377Z
definition: SW-NE striking, approx. 70° NW dipping normal fault.
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Mönchsrot-Ellwangen (Ellbach) Fault Zone

[hl_131]
type: Fault
type: Limit
definition: Gewellt WSW-ENE verlaufende, ca. 65° nach NNW einfallende Abschiebung, Seitenast von [DE-BW_176]. @de
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
created: 2020-11-23T14:24:51.379Z
definition: Undulate WSW-ENE trending, approx. 65° NNW dipping normal fault, branch of [hl_114].
notation: DE-BW_177
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [hl_114]

[hl_132]
type: Fault
type: Limit
definition: W-E streichende, ca. 65° nach N einfallende Abschiebung, Seitenast von [DE-BW_177]. @de
created: 2020-11-23T14:24:51.380Z
notation: DE-BW_178
type: Concept
definition: W-E striking, approx. 65° N dipping normal fault, branch of [hl_131].
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [hl_114]

[hl_125]
type: Fault
type: Limit
definition: WNW-ESE striking, approx. 55° NNE dipping normal fault, lateral fault connecting [hl_108] and [hl_129].
definition: WNW-ESE streichende, ca. 55° nach NNE einfallende Abschiebung, Querstörung zwischen [DE-BW_033] und [DE-BW_179]. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-11-23T14:24:51.397Z
notation: DE-BW_189
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Mönchsrot-Ellwangen (Ellbach) Fault Zone

[hl_126]
type: Fault
type: Limit
definition: Arcuate WSW-ENE trending, approx. 85° SSE dipping normal fault, in its NE closely subparallel to [hl_128].
definition: Gebogen WSW-ENE verlaufende, ca. 85° nach SSE einfallende Abschiebung, im NE subparallel zur nahen [DE-BW_188]. @de
created: 2020-11-23T14:24:51.392Z
notation: DE-BW_186
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Mönchsrot-Ellwangen (Ellbach) Fault Zone

[hl_137]
type: Fault
type: Limit
definition: SW-NE streichende, ca. 65° nach NW einfallende Abschiebung. @de
created: 2020-11-23T14:24:51.391Z
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
definition: SW-NE striking, approx. 65° NW dipping normal fault.
notation: DE-BW_185
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Mönchsrot-Ellwangen (Ellbach) Fault Zone

[lca_052]
type: Fault
type: Limit
definition: SSW-NNE striking, approx. 60° ESE dipping normal fault.
notation: DE-BW_181
definition: SSW-NNE streichende, ca. 60° nach ESE einfallende Abschiebung. @de
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6373
created: 2020-11-23T14:24:51.384Z
references: https://data.geoscience.earth/ncl/geoera/ref/6357
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Mönchsrot-Ellwangen (Ellbach) Fault Zone

[hl_129]
type: Fault
type: Limit
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
definition: WSW-ENE streichende, ca. 60° nach NNW einfallende Abschiebung. @de
notation: DE-BW_179
definition: WSW-ENE striking, approx. 60° NNW dipping normal fault.
created: 2020-11-23T14:24:51.382Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Mönchsrot-Ellwangen (Ellbach) Fault Zone

[hl_108]
type: Fault
type: Limit
narrower: [hl_108_b]
notation: DE-BW_033
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
created: 2020-11-23T14:24:51.008Z
narrower: [hl_134]
definition: SW-NE striking, approx. 60° NW dipping normal fault
definition: SW-NE streichende, ca. 60° nach NW einfallende Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Mönchsrot-Ellwangen (Ellbach) Fault Zone

[hl_108_b]
type: Fault
type: Limit
definition: Arcuate SW-NE trending, approx. 75° NW dipping normal fault, link between [hl_108] and [hl_125].
definition: Gebogen SW-NE verlaufende, ca. 75° nach NW einfallende Abschiebung, Verbindung zwischen [DE-BW_033] and [DE-BW_189]. @de
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
created: 2020-11-23T14:24:51.383Z
notation: DE-BW_180
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [hl_108]

[hl_134]
type: Fault
type: Limit
definition: SW-NE striking, approx. 70° SE dipping normal fault
definition: SW-NE streichende, ca. 70° nach SE einfallende Abschiebung. @de
created: 2020-11-23T14:24:51.009Z
notation: DE-BW_034
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [hl_108]

[hl_128]
type: Fault
type: Limit
definition: Undulate SW-NE trending, approx. 75° NW dipping normal fault closely subparallel to [hl_126].
definition: Gewellt SW-NE verlaufende, ca. 75° nach NW einfallende Abschiebung subparallel zur nahen [DE-BW_186]. @de
created: 2020-11-23T14:24:51.395Z
notation: DE-BW_188
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Mönchsrot-Ellwangen (Ellbach) Fault Zone

[hl_127]
type: Fault
type: Limit
definition: Branching off [hl_126], undulate W-E trending, approx. 65° ± S dipping normal fault.
definition: Abzweig von [hl_126], gewellt W-E verlaufende, ca. 65° nach ± S einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-11-23T14:24:51.394Z
notation: DE-BW_187
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Mönchsrot-Ellwangen (Ellbach) Fault Zone

[lca_051]
type: Fault
type: Limit
notation: DE-BW_182
created: 2020-11-23T14:24:51.386Z
references: https://data.geoscience.earth/ncl/geoera/ref/6373
type: Concept
definition: SW-NE streichende, ca. 55° nach SE einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6357
definition: SW-NE striking, approx. 55° SE dipping normal fault.
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Mönchsrot-Ellwangen (Ellbach) Fault Zone

[lca_049]
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6357
created: 2020-11-23T14:24:51.388Z
definition: SSW-NNE striking, approx. 45° ESE dipping normal fault.
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6373
definition: SSW-NNE streichende, ca. 45° nach ESE einfallende Abschiebung. @de
notation: DE-BW_183
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Mönchsrot-Ellwangen (Ellbach) Fault Zone

Rast Fault
type: Fault
type: Limit
sf touches: [hl_033]
definition: SW-NE streichende, ca. 60° nach SE einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
created: 2020-11-23T14:24:51.325Z
type: Concept
definition: SW-NE striking, approx. 60° SE dipping normal fault
narrower: [hl_038]
preferred label: Rast Verwerfung @de
narrower: [hl_039]
notation: DE-BW_151
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_038]
type: Fault
type: Limit
definition: SSW-NNE streichende, ca. 80° nach ESE einfallende Abschiebung. @de
created: 2020-11-23T14:24:51.327Z
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
notation: DE-BW_152
definition: SSW-NNE striking, approx. 80° ESE dipping normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Rast Fault

[hl_039]
type: Fault
type: Limit
definition: SSW-NNE trending, approx. 65° WNW dipping normal fault
notation: DE-BW_153
sf touches: [hl_037]
created: 2020-11-23T14:24:51.328Z
references: https://data.geoscience.earth/ncl/geoera/ref/4097
definition: SSW-NNE streichende, ca. 65° nach WNW einfallende Abschiebung. @de
type: Concept
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Rast Fault

Krumbach Fault
type: Fault
type: Limit
definition: SW-NE striking, approx. 65° NW dipping normal fault/fault zone, downthrow of NW block max. 140 m.
definition: SW-NE streichende Störungszone, NW -Teil abgesunken, max. 140 m Versatzbetrag @de
preferred label: Krumbacher Verwerfung @de
references: https://data.geoscience.earth/ncl/geoera/ref/6370
references: https://data.geoscience.earth/ncl/geoera/ref/6390
created: 2020-11-23T14:24:51.322Z
notation: DE-BW_150
type: Concept
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

Assing-Bromberg Fault System
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.987Z
notation: DE-BY_732
preferred label: Assing-Bromberg Störungssystem @de
definition: Northern boundary of oil- and gasfields Assing and Bromberg. WNW-ESE trending 70°-80° NNE dipping antithetic normal faults running from Palling towards Laufen/Inn.
definition: Nördliche Begrenzung der Öl- und Gasfelder Assing und Bromberg. WNW-ESE von Palling Richtung Laufen/Inn verlaufende, 70°-80° nach NNE einfallende antithetische Abschiebungen. @de
narrower: Palling-Mauerham Fault
narrower: Gessenhausen-Thannsberg Fault
narrower: Tettenhausen-Kirchanschöring Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4109
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_732
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Tettenhausen-Kirchanschöring Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.071Z
notation: DE-BY_1107
preferred label: Tettenhausen-Kirchanschöring Störung @de
definition: WNW-ESE striking, approx. 75° NNE dipping antithetic normal fault.
definition: WNW-ESE verlaufende, ca. 75° nach NNW einfallende antithetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1107
limit type: normalFault
broader: Assing-Bromberg Fault System

Gessenhausen-Thannsberg Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.042Z
notation: DE-BY_831
preferred label: Gessenhausen-Thannsberg Störung @de
definition: WNW-ESE striking, approx. 75° NNE dipping antithetic normal fault.
definition: WNW-ESE verlaufende, ca. 75° nach NNW einfallende antithetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_831
limit type: normalFault
broader: Assing-Bromberg Fault System

Palling-Mauerham Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:28.015Z
notation: DE-BY_830
preferred label: Palling-Mauerham Störung @de
definition: WNW-ESE striking, approx. 80° NNE dipping antithetic normal fault.
definition: WNW-ESE verlaufende, ca. 80° nach NNW einfallende antithetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_830
limit type: normalFault
broader: Assing-Bromberg Fault System

[hl_116]
type: Fault
type: Limit
definition: SSW-NNE striking, approx. 80° ESE dipping normal fault
created: 2020-11-23T14:24:51.012Z
type: Concept
notation: DE-BW_035
definition: SSW-NNE streichende, ca. 80° nach ESE einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
narrower: [hl_117]
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_117]
type: Fault
type: Limit
notation: DE-BW_036
definition: WSW-ENE streichende, ca. 75° nach SSE einfallende Abschiebung. @de
created: 2020-11-23T14:24:51.013Z
definition: WSW-ENE striking, approx. 75° SSE dipping normal fault
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [hl_116]

[hl_118]
type: Fault
type: Limit
definition: WSW-ENE striking, approx. 80° SSE dipping normal fault
created: 2020-11-23T14:24:51.035Z
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
notation: DE-BW_045
definition: WSW-ENE streichende, ca. 80° nach SSE einfallende Abschiebung. @de
narrower: [hl_119]
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_119]
type: Fault
type: Limit
definition: WSW-ENE streichende, fast saiger stehende Abschiebung. @de
notation: DE-BW_046
created: 2020-11-23T14:24:51.037Z
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
definition: WSW-ENE striking, almost vertical normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [hl_118]

Strassbach-Vierkirchen Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.693Z
notation: DE-BY_1216
preferred label: Straßbach-Vierkirchen Störung @de
definition: SW-NE striking, approx. 75° NW dipping antithetic normal fault.
definition: SW-NE streichende, ca. 75° nach NW einfallende antithetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1216
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Vierkirchen-Leonhardsbuch Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.665Z
notation: DE-BY_1215
preferred label: Vierkirchen-Leonhardsbuch Störung @de
definition: SW-NE striking, approx. 55° SE dipping synthetic normal fault.
definition: SW-NE streichende, ca. 55° nach SE einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1215
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Petershausen-Schweitenkirchen Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.637Z
notation: DE-BY_918
preferred label: Petershausen-Schweitenkirchen Störung @de
definition: SW-NE striking, approx. 75° SE dipping synthetic normal fault.
definition: SW-NE streichende, ca. 75° nach SE einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_918
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Ilmmünster Step Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.609Z
notation: DE-BY_917
preferred label: Ilmmünster Bruchstaffel @de
definition: Staggered array of 5 (sub-)parallel W-E to SW-NE striking, steeply (85°-60°) S to SSE dipping synthetic normal faults scarps with minor throws immediate south of Pfaffenhofen Step Fault [DE-BY_767]. Beyond the five detected faults featuring throws of more than about 10 m, more subseismic fault scarps are possible.
definition: Bruchstaffel aus fünf (sub)parallelen, W-E bis SW-NE verlaufenden, steil (85°-60°) nach S bis SSE einfallenden synthetischen Abschiebungen mit geringer Sprunghöhe, unmittelbar südlich der antithetischen Pfaffenhofen Bruchstaffel [DE-BY_767]. Neben den fünf identifizierbaren Stufen mit Sprunghöhen von mehr als ca. 10 m sind weitere subseismische Bruchstufen möglich. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_917
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Weiherholz Fault
type: Fault
type: Limit
definition: N-S striking normal fault dipping W with unknown angle.
preferred label: Weiherholz Verwerfung @de
type: Concept
notation: DE-BW_196
sf touches: [hl_044]
sf touches: [hl_042]
definition: N-S streichende, nach W einfallende Abschiebung mit unbekanntem Einfallswinkel @de
references: https://data.geoscience.earth/ncl/geoera/ref/6362
created: 2020-11-23T14:24:51.412Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

Velden Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.861Z
notation: DE-BY_711
preferred label: Velden Störung @de
definition: From WSW-ENE strike veering to NW-SE trend, averaged approx. 55° NNW to NE dipping antithetic normal fault; northern boundary of oil- and gasfield Velden. This fault runs within the Gifthal Trough from Taufkirchen/Vils to Oberbergkirchen veering from the "Central Molasse Basin" characteristic trend to the "Lower Bavaria Molasse Basin" typical strike when approaching the Landshut-Neuötting crystalline rise and ends, forking into proven horsetail splays, ESE of Oberbergkirchen.
definition: Von Taufkirchen/Vils bis Oberbergkirchen, von WSW-ENE auf NW-SE drehend verlaufende, im Mittel ca. 55° nach NNW bis NE einfallende antithetische Abschiebung; nördliche Begrenzung der Öl- und Gasfelds Velden. Der Verlauf der Störung folgt dem Gifthal Trog, im westlichen Teil in für die zentrale Vorlandmolasse typischer Richtung, dreht mit Annäherung an das Landshut-Neuötting Hoch auf herzynische, für das Niederbayerische Molassebecken charakteristische Richtung und fiedert ESE von Oberbergkirchen in kleine, zunehmend subseismische Störungsäste (horsetail splay) auf. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4109
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_711
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Seebruck Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.833Z
notation: DE-BY_1220
preferred label: Seebruck Störung @de
definition: W-E striking, approx. 65° S dipping synthetic normal fault at the northern shore of Chiemsee.
definition: W-E streichende ca. 65° nach S einfallende synthetische Abschiebung am Nordufer des Chiemsee. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1220
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Höslwang Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.805Z
notation: DE-BY_919
preferred label: Höslwang Störung @de
definition: W-E striking, approx. 70° S dipping synthetic normal fault running from Halfing to Eschenauer See.
definition: W-E streichende, ca. 70° nach S einfallende synthetische Abschiebung zwischen Halfing und Eschenauer See. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_919
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Stetten-Arzbach Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.777Z
notation: DE-BY_1219
preferred label: Stetten-Arzbach Störung @de
definition: SW-NE striking, approx. 60° SE dipping synthetic normal fault NW of Dachau.
definition: SW-NE streichende, ca. 55° nach 60 einfallende synthetische Abschiebung NW von Dachau. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1219
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Arzbach-Fahrenzhausen Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.749Z
notation: DE-BY_1218
preferred label: Arzbach-Fahrenzhausen Störung @de
definition: SW-NE striking, approx. 80° NW dipping antithetic normal fault north of Dachau.
definition: SW-NE streichende, ca. 80° nach NW einfallende antithetische Abschiebung nördlich von Dachau. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1218
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Biberbach-Bachhausen Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.721Z
notation: DE-BY_1217
preferred label: Biberbach-Bachhausen Störung @de
definition: SW-NE striking, approx. 55° SE dipping synthetic normal fault.
definition: SW-NE streichende, ca. 55° nach SE einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1217
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

[hl_120]
type: Fault
type: Limit
notation: DE-BW_135
definition: WSW-ENE streichende, ca. 80° nach SSE einfallende Abschiebung. @de
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
narrower: [hl_122]
created: 2020-11-23T14:24:51.291Z
definition: WSW-ENE striking, approx. 80° SSE dipping normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_122]
type: Fault
type: Limit
definition: SSW-NNE trending, approx. 85° WNW dipping normal fault
notation: DE-BW_136
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
definition: SSW-NNE streichende, ca. 85° nach WNW einfallende Abschiebung. @de
created: 2020-11-23T14:24:51.293Z
narrower: [hl_123]
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [hl_120]

[hl_123]
type: Fault
type: Limit
definition: WSW-ENE striking, approx. 80° NNW dipping normal fault
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
created: 2020-11-23T14:24:51.294Z
notation: DE-BW_137
definition: WSW-ENE streichende, ca. 80° nach NNW einfallende Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [hl_122]

[hl_121]
type: Fault
type: Limit
notation: DE-BW_047
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-11-23T14:24:51.040Z
definition: SW-NE striking, approx. 85° SE dipping normal fault
definition: SW-NE streichende, ca. 85° nach SE einfallende Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_001]
type: Fault
type: Limit
definition: SW-NE striking, approx. 80° NW dipping normal fault
created: 2020-11-23T14:24:50.913Z
definition: SW-NE streichende, ca. 80° nach NW einfallende Abschiebung. @de
notation: DE-BW_001
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_002]
type: Fault
type: Limit
created: 2020-11-23T14:24:50.920Z
notation: DE-BW_002
definition: SW-NE streichende, ca. 70° nach NW einfallende Abschiebung. @de
definition: SW-NE striking, approx. 70° NW dipping normal fault
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

Höhenrain Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.356Z
notation: DE-BY_724
preferred label: Höhenrain Störung @de
definition: Northern boundary of oil- and gasfield Höhenrain. Undulate SW-NE to W-E trending, approx. 70° NW to N dipping antithetic normal fault running from Holzkirchen to Rott am Inn.
definition: Nördliche Begrenzung des Öl- und Gasfeldes Höhenrain. Von Holzkirchen bis Rott am Inn gewellt SW-NE bis W-E verlaufende, ca. 70° nach NW bis N einfallende antithetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4109
sf touches: Holzkirchen Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_724
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Dachau-Inhausen Fault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:30.720Z
notation: DE-BY_1160
preferred label: Dachau-Inhausen Störung @de
definition: SW-NE striking, approx. 60° SE dipping synthetic normal fault.
definition: SW-NE streichende, ca. 60° nach SE einfallende synthetische Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1160
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Gars-Garching Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.328Z
notation: DE-BY_851
preferred label: Gars-Garching Störung @de
definition: W-E trending, approx. 75° S dipping synthetic normal fault running from S of Gars/Inn to N of Garching/Alz.
definition: W-E verlaufende, ca. 75° nach S einfallende synthetische Abschiebung zwischen S von Gars am Inn und N von Garching an der Alz. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: Bierwang Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_851
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Dachau-Unterschleissheim Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:30.693Z
notation: DE-BY_1159
preferred label: Dachau-Unterschleißheim Störung @de
definition: SW-NE striking, >85° SE dipping synthetic normal fault.
definition: SW-NE streichende, >85° nach SE einfallende synthetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1159
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Bierwang Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.301Z
notation: DE-BY_733
preferred label: Bierwang Störung @de
definition: Nördliche Begrenzung des Öl- und Gasfeldes Bierwang. WSW-ENE verlaufende, ca. 50° nach NNW einfallende antithetische Abschiebung zwischen Soyen und Taufkirchen. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4109
sf touches: Gars-Garching Fault
definition: Northern boundary of oil- and gasfield Bierwang. WSW-ENE trending, approx. 50° NNW dipping dipping antithetic normal fault running from Soyen to Taufkirchen.
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_733
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Albaching-Rechtmehring Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.274Z
notation: DE-BY_723
preferred label: Albaching-Rechtmehring Störung @de
definition: Northern boundary of oil- and gasfields Albaching and Rechtmehring. WSW-ENE to W-E trending, on average approx. 75° NNW to N dipping antithetic normal fault running from Kirchseeon to the Inn river SE of Haag. At its western end possibly conected to Wächterhof-Kirchseeon Fault [DE-BY_1094] via a relay ramp.
definition: WSW-ENE bis W-E verlaufende, im Mittel ca. 75° nach NNW bis N einfallende antithetische Abschiebung zwischen Kirchseeon und dem Inn SE von Haag. Nördliche Begrenzung der Öl- und Gasfelder Albaching und Rechtmehring. Am östlichen Ende möglicherweise über eine Relais Rampe (relay ramp) mit der Wächterhof-Kirchseeon Störung [DE-BY_1094] verbunden. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4109
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_723
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Einsbach-Dachau Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
sf touches: Dachau Subfault
type: Concept
created: 2020-10-09T11:35:30.638Z
notation: DE-BY_824
preferred label: Einsbach-Dachau Störung @de
definition: Undulate W-E trending, approx. 60° S dipping synthetic normal fault.
definition: Gewellt W-E verlaufende, ca. 60° nach S einfallende synthetische Abschiebung. @de
narrower: Dachau Subfault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_824
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Dachau Subfault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: Einsbach-Dachau Fault
type: Concept
created: 2020-10-09T11:35:30.665Z
notation: DE-BY_1158
preferred label: Dachau Nebenstörung @de
definition: W-E trending, approx. 50° S dipping synthetic normal fault.
definition: W-E verlaufende, ca. 50° nach S einfallende synthetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1158
limit type: normalFault
broader: Einsbach-Dachau Fault

Wächterhof-Kirchseeon Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.246Z
notation: DE-BY_1094
preferred label: Wächterhof-Kirchseeon Störung @de
definition: WSW-ENE to W-E trending, approx. 70° NNW to N dipping antithetic normal fault. At its eastern end possibly connected to Albaching-Rechtmehring Fault [DE-BY_723] via a relay ramp.
definition: WSW-ENE bis W-E verlaufende, ca. 70° nach NNW bis N einfallende antithetische Abschiebung. Am östlichen Ende möglicherweise über eine Relais Rampe (relay ramp) mit der Albaching-Rechtmehring Fault [DE-BY_723] verbunden. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1094
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Fuchstal Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:30.610Z
notation: DE-BY_822
preferred label: Fuchstal Störung @de
definition: SW-NE striking, approx. 70° SE dipping synthetic normal fault.
definition: SW-NE streichende, ca. 70° nach SE einfallende synthetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_822
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Anzing-Ödgassen-Waldkraiburg Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.219Z
notation: DE-BY_722
preferred label: Anzing-Ödgassen-Waldkraiburg Störung @de
definition: Running from Anzing E of Munich to Polling S of Mühldorf, undulate WSW-ENE trending, on average approx. 55° NNW dipping antithetic normal fault; northern boundary of oil- and gasfields Anzing, Schnaupping, Haag, Ödgassen, Waldkraiburg, and Mühldorf-Süd.
definition: Wellenförmig WSW-ENE verlaufende im Mittel ca. 55° nach NNW einfallende antithetische Abschiebung zwischen Anzing und Polling S von Mühldorf. Nördliche Begrenzung der Öl- und Gasfelder Anzing, Schnaupping, Haag und Ödgassen, Waldkraiburg und Mühldorf-Süd. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4109
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_722
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Hagenheim-Finning Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:30.583Z
notation: DE-BY_821
preferred label: Hagenheim-Finning Störung @de
definition: SW-NE striking, approx. 85° SE dipping synthetic normal fault.
definition: SW-NE streichende, ca. 85° nach SE einfallende synthetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_821
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Stiefenhofen-Weitnau Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:30.555Z
notation: DE-BY_1157
preferred label: Stiefenhofen-Weitnau Störung @de
definition: WSW-ENE striking, approx. 60° SSE dipping synthetic normal fault.
definition: WSW-ENE streichende, ca. 60° nach SSE einfallende synthetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1157
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

[lca_070]
type: Fault
type: Limit
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6357
references: https://data.geoscience.earth/ncl/geoera/ref/6373
definition: WSW-ENE streichende, ca. 50° nach SSE einfallende Abschiebung. @de
created: 2020-11-23T14:24:51.146Z
notation: DE-BW_084
definition: WSW-ENE striking, approx. 50° SSE dipping normal fault
sf touches: [lca_079]
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_071]
type: Fault
type: Limit
definition: SSW-NNE streichende, ca. 75° nach ESE einfallende Abschiebung. @de
created: 2020-11-23T14:24:51.143Z
definition: SSW-NNE striking, approx. 75° ESE dipping normal fault
type: Concept
notation: DE-BW_083
references: https://data.geoscience.earth/ncl/geoera/ref/6373
references: https://data.geoscience.earth/ncl/geoera/ref/6357
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_072]
type: Fault
type: Limit
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6373
references: https://data.geoscience.earth/ncl/geoera/ref/6357
definition: SSW-NNE streichende, ca. 70° nach ESE einfallende Abschiebung. @de
definition: SSW-NNE striking, approx. 70° ESE dipping normal fault
notation: DE-BW_096
created: 2020-11-23T14:24:51.183Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_073]
type: Fault
type: Limit
notation: DE-BW_094
definition: SSW-NNE striking, approx. 50° WNW dipping normal fault
sf touches: [lca_075]
type: Concept
definition: SSW-NNE streichende, ca. 50° nach WNW einfallende Abschiebung. @de
created: 2020-11-23T14:24:51.177Z
references: https://data.geoscience.earth/ncl/geoera/ref/6373
sf touches: [lca_074]
references: https://data.geoscience.earth/ncl/geoera/ref/6357
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

Kinsau Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.465Z
notation: DE-BY_802
preferred label: Kinsau Störung @de
definition: Northern boundary of oilfield Kinsau. W-E trending, approx. 55° N dipping antithetic normal fault running from Kaltental to Reichling.
definition: Nördliche Begrenzung des Öl-Feldes Kinsau. W-E verlaufende, ca. 55° nach N einfallende antithetische Abschiebung zwischen Kaltental und Reichling. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4109
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_802
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Günzach-Pforzen Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.438Z
notation: DE-BY_1097
preferred label: Günzach-Pforzen Störung @de
definition: SW-NE striking, approx. 70° NW dipping antithetic normal fault.
definition: SW-NE streichende, ca. 70° nach NW einfallende antithetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: Mauerstetten Fault Scarp 1
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1097
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Freising Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4123
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:30.802Z
notation: DE-BY_825
preferred label: Freising Störung @de
definition: Slightly undulated overall W-E trending, approx. 55° ± N dipping antithetic normal fault running from Kranzberg to Schmidhausen.
definition: Leicht wellenförmig W-E verlaufende, ca. 55° nach ± N einfallende antithetische Abschiebung zwischen Kranzberg und Schmidhausen. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_825
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Utrasried-Irsee Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.410Z
notation: DE-BY_1096
preferred label: Utrasried-Irsee Störung @de
definition: Slightly undulating SW-NE to SSW-NNE trending, approx. 50° SE to ESE dipping synthetic normal fault.
definition: Leicht gewellt SW-NE bis SSW-NNE verlaufende, ca. 50° nach SE bis ESE einfallende synthetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: Blöcktach-Bad Wörishofen Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1096
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Grossnöbach-Massenhausen Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: Dachau-Grossnöbach Fault
type: Concept
created: 2020-10-09T11:35:30.775Z
notation: DE-BY_1162
preferred label: Großnöbach-Massenhausen Störung @de
definition: W-E striking, approx. 85° N dipping antithetic normal fault.
definition: W-E streichende, ca. 85° N einfallende antithetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1162
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Blöcktach-Bad Wörishofen Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.383Z
notation: DE-BY_1095
preferred label: Blöcktach-Bad Wörishofen Störung @de
definition: SSW-NNE striking, approx. 80° WNW dipping antithetic normal fault.
definition: SSW-NNE streichende, ca. 80° nach WNW einfallende antithetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
sf touches: Frauenzell-Bad Wörishofen Fault
sf touches: Utrasried-Irsee Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1095
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Dachau-Grossnöbach Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
sf touches: Grossnöbach-Massenhausen Fault
type: Concept
created: 2020-10-09T11:35:30.747Z
notation: DE-BY_1161
preferred label: Dachau-Großnöbach Störung @de
definition: Arcuate SW-NE to SSW-NNE trending, approx. 75° ± SE dipping synthetic normal fault.
definition: Bogenförmig SW-NE bis SSW-NNE verlaufende, ca. 75° nach ± SE einfallende synthetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1161
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

[lca_078]
type: Fault
type: Limit
definition: SW-NE trending, approx. 80° SE dipping normal fault
references: https://data.geoscience.earth/ncl/geoera/ref/6373
notation: DE-BW_081
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6357
created: 2020-11-23T14:24:51.137Z
definition: SW-NE streichende, ca. 80° nach SE einfallende Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_079]
type: Fault
type: Limit
notation: DE-BW_080
definition: SSW-NNE streichende, ca. 85° nach WNW einfallende Abschiebung. @de
definition: SSW-NNE striking, approx. 85° WNW dipping normal fault
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6357
sf touches: [lca_070]
references: https://data.geoscience.earth/ncl/geoera/ref/6373
created: 2020-11-23T14:24:51.134Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_074]
type: Fault
type: Limit
definition: WSW-ENE streichende, ca. 80° nach SSE einfallende Abschiebung. @de
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6373
notation: DE-BW_099
references: https://data.geoscience.earth/ncl/geoera/ref/6357
created: 2020-11-23T14:24:51.194Z
definition: WSW-ENE striking, approx. 80° SSE dipping normal fault
sf touches: [lca_073]
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_075]
type: Fault
type: Limit
sf touches: [lca_073]
notation: DE-BW_121
definition: WSW-ENE striking, approx. 50° SSE dipping normal fault
created: 2020-11-23T14:24:51.257Z
definition: WSW-ENE streichende, ca. 50° nach SSE einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6373
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6357
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_076]
type: Fault
type: Limit
definition: NW-SE striking, approx. 50° NE dipping normal fault
definition: NW-SE streichende, ca. 50° nach NE einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6373
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6357
notation: DE-BW_090
created: 2020-11-23T14:24:51.165Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

Mauerstetten-Markt Schwaben Train of Faults
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.492Z
notation: DE-BY_1098
preferred label: Mauerstetten-Markt Schwaben Störungszug @de
definition: Chain of major synthetic normal faults running from Kempten to Markt Schwaben.
definition: Lineare Anordnung größerer synthetischer Abschiebungen zwischen Kempten und Markt Schwaben. @de
narrower: Mauerstetten Step Fault
narrower: Rott Linking Faults
narrower: Munich Fault
narrower: Markt Schwaben Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
narrower: Apfeldorf Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1098
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Rott Linking Faults
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.658Z
notation: DE-BY_1099
preferred label: Rott Störungsschar @de
definition: En Echelon step fault like cluster of subparallel, overall SW-NE trending, steeply (85°-60°) ± SE dipping synthetic normal faults at the transition from Mauerstetten Step Fault [DE-BY_755] to Munich Fault [DE-BY_1100].
definition: Bruchstaffel subparalleler, insgesamt SW-NE verlaufender, steil (85°-60°) nach ± SE einfallender synthetischer Abschiebungen am Übergang des Mauerstetten Abbruchs [DE-BY_755] zum Münchener Verwurf [DE-BY_1100]. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1099
limit type: normalFault
broader: Mauerstetten-Markt Schwaben Train of Faults

Mauerstetten Step Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.520Z
notation: DE-BY_755
alternative label: Mauerstetten Störung @de
preferred label: Mauerstetten Abbruch @de
definition: Overall WSW-ENE oriented step fault system of up to 4 steeply (55°-85°) ± SSE dipping normal fault scarps.
definition: Übergeordnet WSW-ENE verlaufendes System von bis zu 4 Abbruchstufen aus steilstehenden (55°-85°) Abschiebung mit ± SSE-Einfallen. @de
narrower: Mauerstetten Fault Scarp 1
narrower: Mauerstetten Fault Scarp 2
narrower: Mauerstetten Fault Scarp 3
narrower: Mauerstetten Fault Scarp 4
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4117
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_755
limit type: normalFault
broader: Mauerstetten-Markt Schwaben Train of Faults

Mauerstetten Fault Scarp 4
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.631Z
notation: DE-BY_759
preferred label: Mauerstetten Abbruchstufe 4 @de
definition: Mauerstetten Step Fault far southeastern scarp running from Markt Oberdorf to Osterzell. SSW-NNE trending, approx. 85° ESE dipping synthetic normal fault.
definition: Südöstlichste Bruchstufe des Mauerstetten Abbruchs zwischen Markt Oberdorf und Osterzell. SSW-NNE verlaufende, ca. 85° nach ESE einfallende synthetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4117
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_759
limit type: normalFault
broader: Mauerstetten Step Fault

Mauerstetten Fault Scarp 3
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.603Z
notation: DE-BY_758
preferred label: Mauerstetten Abbruchstufe 3 @de
definition: Mauerstetten Step Fault southeastern scarp running from Aitrang to Stöttwang. WSW-ENE to SW-NE trending, approx. 60° ± SE dipping synthetic normal fault.
definition: Südöstliche Bruchstufe des Mauerstetten Abbruchs zwischen Aitrang und Stöttwang. WSW-ENE bis SW-NE verlaufende, ca. 60° nach ± SE einfallende synthetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4117
sf touches: Mauerstetten Fault Scarp 2
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_758
limit type: normalFault
broader: Mauerstetten Step Fault

Mauerstetten Fault Scarp 2
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.575Z
notation: DE-BY_757
preferred label: Mauerstetten Abbruchstufe 2 @de
definition: Mauerstetten Step Fault main scarp running from north of Kempten to Mauerstetten and eastbound on towards the Lech river. WSW-ENE to W-E trending, approx. 55° SSE to S dipping synthetic normal fault.
definition: Mittlere Bruchstufe des Mauerstetten Abbruchs von nördlich Kempten über Mauerstetten ostwärts bis nach Dienhausen. WSW-ENE bis W-E verlaufende, ca. 55° nach SSE bis S einfallende synthetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4117
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_757
limit type: normalFault
broader: Mauerstetten Step Fault

Mauerstetten Fault Scarp 1
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.548Z
notation: DE-BY_756
preferred label: Mauerstetten Abbruchstufe 1 @de
definition: Mauerstetten Step Fault northwestern scarp running from Günzach to Mauerstetten. Southwestward arcuate WSW-ENE trending, approx. 65° SSE dipping synthetic normal fault.
definition: Nordwestliche Bruchstufe des Mauerstetten Abbruchs zwischen Günzach und Mauerstetten. Südwestwärts gebogen WSW-ENE verlaufende, ca. 65° nach SSE einfallende synthetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4117
sf touches: Günzach-Pforzen Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_756
limit type: normalFault
broader: Mauerstetten Step Fault

Apfeldorf Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:31.332Z
notation: DE-BY_1173
preferred label: Apfeldorf Störung @de
definition: WSW-ENE striking, approx. 85° SSE dipping synthetic normal fault at the transition from Mauerstetten Step Fault [DE-BY_755] to Munich Fault [DE-BY_1100].
definition: WSW-ENE streichende, ca. 85° nach SSE einfallende synthetische Abschiebung am Übergang des Mauerstetten Abbruchs [DE-BY_755] zum Münchener Verwurf [DE-BY_1100]. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1173
limit type: normalFault
broader: Mauerstetten-Markt Schwaben Train of Faults

Markt Schwaben Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.714Z
notation: DE-BY_725
alternative label: Markt Schwaben Verwurf @de
preferred label: Markt Schwabener Verwurf @de
definition: Emerging from the horsetail splay at the eastern end of Munich Fault [DE-BY_1100], this WSW-ENE trending major structure featuring a throw up to 200 m (Dussel et al. 2015) consists of two approx. 75° SSE dipping synthetic normal faults, soft-linked by a relay ramp. Principal target of several deep E&P drillings for hydrothermal heat production.
definition: Östliche Fortsetzung des Münchener Verwurfs [DE-BY_1100]. WSW-ENE verlaufende Struktur, bestehend aus zwei ca. 75° nach SSE einfallenden synthetischen Abschiebungen mit einem Versatz bis zu 200 m (Dussel et al. 2015), die über eine Relais Rampe (relay ramp) miteinander in Verbindung stehen. Zielstruktur hydrothermaler Förderbohrungen zur Wärmegewinnung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4084
sf touches: Neuching-Wörth Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_725
limit type: normalFault
broader: Mauerstetten-Markt Schwaben Train of Faults

Munich Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.686Z
notation: DE-BY_1100
preferred label: Münchener Verwurf @de
definition: Overall WSW-ENE trending, on average approx. 70° SSE dipping synthetic normal fault running from west of Lake Ammer (Ammersee) to the eastern districts of Munich. Principal long-range fault of the Molasse Basin featuring a throw up to 350 m in the Munich area where forkings into several horsetail splays are proven.
definition: Von Rott westlich des Ammersees bis zu den östlichen Stadteilen Münchens, insgesamt WSW-ENE verlaufende, im Mittel ca. 70° nach SSE einfallende synthetische Abschiebung. Eine der Hauptstörungen des Molassebeckens mit Versätzen bis zu 350 m im Raum München, wo eine mehrfache Auffiederung (horsetail splays) seismisch nachgewiesen ist. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1100
limit type: normalFault
broader: Mauerstetten-Markt Schwaben Train of Faults

[lca_083]
type: Fault
type: Limit
definition: WNW-ESE streichende, ca. 60° nach NNE einfallende Abschiebung. @de
created: 2020-11-23T14:24:51.216Z
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6373
notation: DE-BW_106
definition: WNW-ESE striking, approx. 60° NNE dipping normal fault
references: https://data.geoscience.earth/ncl/geoera/ref/6357
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_084]
type: Fault
type: Limit
notation: DE-BW_087
references: https://data.geoscience.earth/ncl/geoera/ref/6357
type: Concept
created: 2020-11-23T14:24:51.156Z
references: https://data.geoscience.earth/ncl/geoera/ref/6373
definition: SW-NE streichende, ca. 70° nach SE einfallende Abschiebung. @de
definition: SW-NE striking, approx. 70° SE dipping normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

Darching Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.741Z
notation: DE-BY_729
preferred label: Darching Störung @de
definition: Northern boundary of oil- and gasfield Darching / Holzkirchen. Slightly undulate WNW-ESE trending, approx. 75° NNE dipping antithetic normal fault running from Holzkichen to Götting.
definition: Nördliche Begrenzung des Öl- und Gasfeldes Darching / Holzkirchen. Leicht gewellt WNW-ESE verlaufende, ca. 75° nach NNE einfallende antithetische Abschiebung zwischen Holzkirchen und Götting. @de
narrower: Holzkirchen Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4094
references: https://data.geoscience.earth/ncl/geoera/ref/4109
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_729
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Holzkirchen Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.768Z
notation: DE-BY_1101
preferred label: Holzkirchen Störung @de
definition: NW-SE striking, approx. 80° NE dipping antithetic branch of Darching Fault.
definition: NW-SE streichender, ca. 80° antithetisch nach NE einfallender Zweig der Darching Störung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
sf touches: Höhenrain Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1101
limit type: normalFault
broader: Darching Fault

[lca_080]
type: Fault
type: Limit
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6357
notation: DE-BW_088
references: https://data.geoscience.earth/ncl/geoera/ref/6373
created: 2020-11-23T14:24:51.159Z
definition: W-E striking, approx. 80° S dipping normal fault
definition: W-E streichende, ca. 80° nach S einfallende Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_089]
type: Fault
type: Limit
definition: WSW-ENE streichende, ca. 80° nach SSE einfallende Abschiebung. @de
definition: WSW-ENE striking, approx. 80° SSE dipping normal fault
references: https://data.geoscience.earth/ncl/geoera/ref/6373
created: 2020-11-23T14:24:51.131Z
notation: DE-BW_079
references: https://data.geoscience.earth/ncl/geoera/ref/6357
type: Concept
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_088]
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6373
definition: WNW-ESE streichende, ca. 85° nach NNE einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6357
type: Concept
definition: WNW-ESE striking, approx. 85° NNE dipping normal fault
notation: DE-BW_082
created: 2020-11-23T14:24:51.140Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_100]
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
notation: DE-BW_031
created: 2020-11-23T14:24:51.002Z
sf touches: [hl_105]
sf touches: [hl_092]
definition: WSW-ENE streichende, ca. 70° nach SSE einfallende Abschiebung. @de
definition: WSW-ENE striking, approx. 70° SSE dipping normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_101]
type: Fault
type: Limit
notation: DE-BW_044
created: 2020-11-23T14:24:51.033Z
references: https://data.geoscience.earth/ncl/geoera/ref/4097
definition: N-S streichende, ca. 85° nach W einfallende Abschiebung. @de
type: Concept
definition: N-S striking, approx. 85° W dipping normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

Frauenzell-Böhen Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.468Z
notation: DE-BY_1214
preferred label: Frauenzell-Böhen Störung @de
definition: SW-NE trending, approx. 70° SE dipping synthetic normal fault.
definition: SW-NE verlaufende, in etwa 70° nach SE einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1214
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Berg-Poing Train of Faults
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:26.749Z
notation: DE-BY_720
preferred label: Berg-Poing Störungszug @de
definition: Train of synthetic faults running from Lake Starnberg to Poing east of Munich, partly linked through horsetail splay structures and an inferred (subseismic) relay ramp. Target of several successful geothermal exploitations and featuring some of the most prolific geothermal installations in the Greater Munich Area.
definition: Vom Starnberger See bis Poing östlich von München reichender Störungszug teilweise über Auffiederungen (horsetail splay) und eine vermutete, subseismische Relais Rampe (relay ramp) verbundener Syntheter. Zielstruktur verschiedener erfolgreicher Tiefengeothermie Erschließungsvorhaben im Großraum München. @de
narrower: Berg-Oberhaching Fault
narrower: Unterhaching Fault System
narrower: Poing Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4109
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_720
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Poing Fault
type: Fault
type: Limit
type: SpatialObject
definition: SW-NE striking, approx. 75° SE dipping synthetic normal fault, at its southwestern end presumably soft-linked to Taufkirchen-Parsdorf Fault [DE-BY_1085] via a relay ramp.
definition: SW-NE streichende, ca. 75° nach SE einfallende synthetische Abschiebung. Am südwestlichen Ende vermutlich über eine Relais Rampe (relay ramp) mit der Taufkirchen-Parsdorf Störung [DE-BY_1085] verbunden. @de
type: Concept
created: 2020-10-09T11:35:27.026Z
notation: DE-BY_1087
preferred label: Poing Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1087
limit type: normalFault
broader: Berg-Poing Train of Faults

Unterhaching Fault System
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:26.915Z
notation: DE-BY_1083
preferred label: Unterhachinger Störungssystem @de
definition: Northeastward forking structure consisting of three main faults, in sections split up into or dwindling in horsetail splay structures, forming a northwestern elevated ramp (horst) and a southeastern graben structure. The complex fault network of Unterhaching Faultsystem represents the target structure of several successful geothermal exploitations, featuring some of the most prolific deep geothermal installations in the Greater Munich Area.
definition: Nach NE hin sich erweiternde und auslaufende Struktur aus drei, bereichsweise in mehrere Äste aufgefiederter Hauptstörungen. Die Störungen begrenzen einen rampenartigen Horst im NW und eine Grabenstruktur im SE. Das komplexe Störungsnetz des Unterhaching Störungssystem ist Zielstruktur verschiedener erfolgreicher Tiefengeothermie-Erschließungsvorhaben. @de
narrower: Unterhaching Fault
narrower: Taufkirchen-Parsdorf Fault
narrower: Putzbrunn-Baldham Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1083
limit type: normalFault
broader: Berg-Poing Train of Faults

Putzbrunn-Baldham Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:26.998Z
notation: DE-BY_1086
preferred label: Putzbrunn-Baldham Störung @de
definition: SW-NE to WSW-ENE trending, largely vertical normal fault with a minor offset, forming the southeastern flank of a local graben structure widening toward NE.
definition: SW-NE bis WSW-ENE verlaufende, großteils vertikale Abschiebung. Diese Störung mit relativ geringer Sprunghöhe bildet die südöstliche Verwerfungsebene einer sich nach NE hin verbreiternden lokalen Grabenstruktur. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1086
limit type: normalFault
broader: Unterhaching Fault System

Taufkirchen-Parsdorf Fault
type: Fault
type: Limit
preferred label: Taufkirchen-Parsdorf Störung @de
definition: SW-NE trending, approx. 75° SE dipping synthetic normal fault featuring a throw of up to more than 100 m, separating the southward tapering local horst and graben structures. At its northeastern end presumably soft linked with Poing Fault [DE-BY_1087] via a relay ramp.
definition: SW-NE verlaufende, ca. 75° nach SE einfallende synthetische Abschiebung. Diese Störung mit einer Sprunghöhe von bis über 100 m bildet die Grenze zwischen den sich südwestwärts verengenden Horst (im NW) und Graben (im SE) Strukturen. Am nordöstlichen Ende vermutlich über eine Relais Rampe (relay ramp) mit der Poing Störung [DE-BY_1087] verbunden. @de
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:26.971Z
notation: DE-BY_1085
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1085
limit type: normalFault
broader: Unterhaching Fault System

Unterhaching Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:26.943Z
notation: DE-BY_1084
preferred label: Unterhaching Störung @de
definition: SSW-NNE striking, approx. 75° WNW dipping antithetic normal fault featuring a throw of up to ca. 100 m, dwindling in a horsetail splay towards its north. Northwestern edge of a narrow, ramp-like local horst structure.
definition: SSW-NNE streichende, ca. 75° nach WNW einfallende antithetische Abschiebung; nach N hin auffiedernd (horsetail splay). Nordwestliche Flanke einer schmalen, rampenförmigen Horst-Struktur. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1084
limit type: normalFault
broader: Unterhaching Fault System

Berg-Oberhaching Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:26.776Z
notation: DE-BY_721
preferred label: Berg-Oberhaching Störung @de
definition: W-E to SW-NE trending, averaged approx. 75° S to SE dipping synthetic normal fault transitioning into Unterhaching Fault System in its northeast.
definition: W-E bis SW-NE verlaufende, im Mittel ca. 75° nach S bis SE einfallende synthetische Abschiebung. Im NE Übergang in das Unterhaching Störungssystem. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
narrower: Deining Subfault
narrower: Kirchstockach Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_721
limit type: normalFault
broader: Berg-Poing Train of Faults

Kirchstockach Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:26.859Z
notation: DE-BY_1081
preferred label: Kirchstockach Störung @de
definition: WSW-ENE striking, approx. 85° SSE dipping synthetic normal fault.
definition: WSW-ENE streichende, ca. 85° nach SSE einfallende synthetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1081
limit type: normalFault
broader: Berg-Oberhaching Fault

Deining Subfault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:26.804Z
notation: DE-BY_1080
preferred label: Deining Nebenstörung @de
definition: WNW-ESE striking, approx. 70° SSW dipping synthetic normal fault connecting Berg-Oberhaching [DE-BY_721], Tutzing-Icking [DE-BY_803] and Münsing-Brunnthal [DE-BY_808] synthetic normal faults with unknown kinematics.
definition: WNW-ESE streichende, ca. 70° nach SSW einfallende synthetische Abschiebung. Kinematisch ungeklärte Verbindung der synthetischen Abschiebungen Berg-Oberhaching [DE-BY_721], Tutzing-Icking [DE-BY_803] und Münsing-Brunnthal [DE-BY_808]. @de
sf touches: Tutzing-Icking Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1080
limit type: normalFault
broader: Berg-Oberhaching Fault

Polling-Eberfing Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: Eberfing-Eurasburg Fault
type: Concept
created: 2020-10-09T11:35:30.111Z
notation: DE-BY_1142
preferred label: Polling-Eberfing Störung @de
definition: WNW-ESE striking, approx. 85° SSW dipping synthetic normal fault.
definition: WNW-ESE streichende, ca. 85° nach SSE einfallende synthetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1142
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Benningen-Kammlach Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.441Z
notation: DE-BY_1213
preferred label: Benningen-Kammlach Störung @de
definition: SW-NE striking, approx. 60° SE dipping synthetic normal fault.
definition: SW-NE streichende, in etwa 60° nach SE einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: Erlenberg-Tussenhausen Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1213
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Forst Bayerdiessen-Wielenbach Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:30.083Z
notation: DE-BY_1141
preferred label: Forst Bayerdießen-Wielenbach Störung @de
definition: Southward arcuate, WNW-ESE to W-E trending, approx. 65° NNE to N dipping antithetic normal fault running from Forst Bayerdiessen to Witzhofen.
definition: Südwärts gebogen, WNW-ESE bis W-E verlaufende, ca. 65° nach NNE bis N einfallende antithetische Abschiebung zwischen Forst Bayerdießen und Witzhofen. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1141
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Memmingen Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.413Z
notation: DE-BY_904
preferred label: Memmingen Störung @de
definition: Kinked SW-NE trending, approx. 45° SE dipping synthetic normal fault.
definition: Geknickt SW-NE verlaufende, in etwa 45° nach SE einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_904
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Wessobrunn-Weilheim Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:30.055Z
notation: DE-BY_1140
preferred label: Wessobrunn-Weilheim Störung @de
definition: Southward arcuate, WNW-ESE to W-E trending, approx. 65° NNE to N dipping antithetic normal fault running from Haid to Unterhausen.
definition: Südwärts gebogen, WNW-ESE bis W-E verlaufende, ca. 65° nach NNE bis N einfallende antithetische Abschiebung zwischen Haid und Unterhausen. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1140
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Grossbergham-Lochen Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.386Z
notation: DE-BY_900
preferred label: Großbergham-Lochen Störung @de
definition: WNW-ESE striking, approx. 70° SSW dipping synthetic normal fault north of Seeon; possibly branch of Obing-Altenmarkt Fault [DE-BY_857].
definition: WNW-ESE streichende, ca. 70° nach SSW einfallende synthetische Abschiebung nördlich von Seeon; möglicherweise Zweig der Obing-Altenmarkt Störung [DE-BY_857]. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_900
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Otterfing-Emertsham Train of Faults
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:26.667Z
notation: DE-BY_1079
preferred label: Otterfing-Emertsham Störungszug @de
definition: Train of faults running from Otterfing N of Holzkirchen in the west to Emertsham NW of Trostberg in the east. Undulate overall WSW-ENE trending array of, steeply ± SSE dipping antithetic normal faults forming the structural traps of various oil- and gasfields.
definition: Von Otterfing (nördlich Holzkirchen) im Westen bis nach Emertsham (nordwestlich von Trostberg) im Osten ziehender Störungszug wellenförmig, insgesamt WSW-ENE verlaufender, steil nach ± SSE einfallender antithetischer Abschiebungen als Fallenstrukturen verschiedener Öl- und Gasfelder. @de
narrower: Mattenhofen-Assling Fault
narrower: Schnaitsee Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1079
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Schnaitsee Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:26.722Z
notation: DE-BY_718
preferred label: Schnaitsee Störung @de
definition: WSW-ENE trending, approx. 60° NNW dipping antithethic normal fault running from Eiselfing to Emertsham; northern boundary of oil- and gasfield Schnaitsee.
definition: Von Eiselfing nach Emertsham ziehende, WSW-ENE verlaufende, ca. 60° nach NNW einfallende antithetische Abschiebung; nördliche Begrenzung des Öl- und Gasfeld Schnaitsee. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4109
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_718
limit type: normalFault
broader: Otterfing-Emertsham Train of Faults

Mattenhofen-Assling Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:26.694Z
notation: DE-BY_719
preferred label: Mattenhofen-Aßling Störung @de
definition: Northern boundary of oil- and gasfields Mattenhofen and Assling. Undulate WSW-ENE trending, approx. 80° NNW dipping antithethic normal fault running from Otterfing to Ramerberg.
definition: Von Otterfing nach Ramerberg ziehende, leicht wellig WSW-ENE verlaufende, ca. 80° nach NNW einfallende antithetische Abschiebung; nördliche Begrenzung der Öl- und Gasfelder Mattenhofen und Assling. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4109
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_719
limit type: normalFault
broader: Otterfing-Emertsham Train of Faults

Weilheim Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:30.027Z
notation: DE-BY_809
preferred label: Weilheim Störung @de
definition: W-E striking, steeply (85°-60°) S dipping synthetic normal fault.
definition: W-E streichende, steil (85°-60°) nach S einfallende synthetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_809
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Trostberg Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.358Z
notation: DE-BY_899
preferred label: Trostberg Störung @de
definition: WNW-ESE striking, approx. 60° NNE dipping antithetic normal fault east of Trostberg.
definition: WNW-ESE streichende, ca. 60° nach NNE einfallende antithetische Abschiebung östlich von Trostberg. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_899
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Bernried-Dorfen Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:29.998Z
notation: DE-BY_810
preferred label: Bernried-Dorfen Störung @de
definition: Slightly arcuate overall WSW-ENE trending, approx. 75° SSE dipping synthetic normal fault.
definition: Leicht gebogen, insgesamt WSW-ENE verlaufende, ca. 75° nach SSE einfallende synthetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_810
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Mörgen-Walkershofen Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.330Z
notation: DE-BY_1212
preferred label: Mörgen-Walkershofen Störung @de
definition: SSW-NNE striking, approx. 75° ESE dipping synthetic normal fault.
definition: SSW-NNE streichende, ca. 75° nach ESE einfallende synthetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: Haselbach-Mickhausen Fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1212
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

[lca_050]
type: Fault
type: Limit
definition: W-E striking, approx. 80° N dipping normal fault
notation: DE-BW_056
created: 2020-11-23T14:24:51.065Z
narrower: [hl_102]
definition: W-E streichende, ca. 80° nach N einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6357
references: https://data.geoscience.earth/ncl/geoera/ref/6373
type: Concept
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_102]
type: Fault
type: Limit
notation: DE-BW_057
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
definition: WSW-ENE striking, almost vertical normal fault
created: 2020-11-23T14:24:51.067Z
definition: WSW-ENE streichende, fast saiger stehende Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [lca_050]

Frauenzell-Bad Wörishofen Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: Blöcktach-Bad Wörishofen Fault
type: Concept
created: 2020-10-09T11:35:30.251Z
notation: DE-BY_819
preferred label: Frauenzell-Bad Wörishofen Störung @de
definition: Slightly undulating, overall SW-NE trending, approx. 55° SE dipping synthetic normal fault from Iller river to Bad Wörishofen.
definition: Leicht wellenförmig, insgesamt SW-NE verlaufende, in etwa 55° nach SE einfallende synthetische Abschiebung zwischen Iller und Bad Wörishofen. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_819
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Tuntenhausen-Schönstett Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.581Z
notation: DE-BY_914
preferred label: Tuntenhausen-Schönstett Störung @de
definition: Undulate WSW-ENE trending, approx. 75° NNW dipping antithetic normal fault.
definition: Gewellt WSW-ENE verlaufende, ca. 75° nach NNW einfallende antithetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_914
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Paterzell Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:30.223Z
notation: DE-BY_1146
preferred label: Paterzell Störung @de
definition: WSW-ENE striking, approx. 80° NNW dipping antithetic normal fault.
definition: WSW-ENE streichende, ca. 80° nach NNW einfallende antithetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1146
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Herrsching-Gauting Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.553Z
notation: DE-BY_912
preferred label: Herrsching-Gauting Störung @de
definition: Slightly northwestward arcuate SW-NE trending, approx. 85° SE dipping synthetic normal fault.
definition: Leicht nordwestwärts gebogene, SW-NE verlaufende, ca. 85° nach SE einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_912
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

St. Leonhard Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:30.195Z
notation: DE-BY_1145
preferred label: St. Leonhard Störung @de
definition: WSW-ENE striking, approx. 85° SSE dipping synthetic normal fault.
definition: WSW-ENE streichende, ca. 85° nach SSE einfallende synthetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1145
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Schwabmünchen Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.525Z
notation: DE-BY_911
preferred label: Schwabmünchen Störung @de
definition: W-E striking, > 85° N dipping antithetic normal fault.
definition: W-E verlaufende, > 85° nach N einfallende antithetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_911
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Peiting-Peissenberg Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:30.168Z
notation: DE-BY_1144
preferred label: Peiting-Peißenberg Störung @de
definition: Slightly undulate W-E trending, approx. 80° N dipping antithetic normal fault.
definition: Leicht gewellt W-E verlaufende, ca. 80° nach N einfallende antithetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1144
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Hochzoll-St. Afra Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.497Z
notation: DE-BY_906
preferred label: Hochzoll-St. Afra Störung @de
definition: WNW-ESE striking, approx. 80° NNE dipping antithetic normal fault.
definition: WNW-ESE streichende, ca. 80° nach NNE einfallende antithetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_906
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Hohenpeissenberg Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:30.140Z
notation: DE-BY_1143
preferred label: Hohenpeißenberg Störung @de
definition: WNW-ESE striking, approx. 85° SSW dipping synthetic normal fault.
definition: WNW-ESE streichende, ca. 85° nach SSE einfallende synthetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1143
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

[lca_056]
type: Fault
type: Limit
definition: SSW-NNE streichende, ca. 75° nach ESE einfallende Abschiebung. @de
definition: SSW-NNE striking, approx. 75° ESE dipping normal fault
notation: DE-BW_098
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6373
created: 2020-11-23T14:24:51.190Z
references: https://data.geoscience.earth/ncl/geoera/ref/6357
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_057]
type: Fault
type: Limit
type: Concept
definition: W-E striking, approx. 80° S dipping normal fault
definition: W-E streichende, ca. 80° nach S einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6373
notation: DE-BW_097
references: https://data.geoscience.earth/ncl/geoera/ref/6357
created: 2020-11-23T14:24:51.186Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_058]
type: Fault
type: Limit
notation: DE-BW_062
definition: SW-NE streichende, ca. 70° nach SE einfallende Abschiebung. @de
created: 2020-11-23T14:24:51.083Z
definition: SW-NE striking, approx. 70° SE dipping normal fault
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6373
references: https://data.geoscience.earth/ncl/geoera/ref/6357
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_059]
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6357
type: Concept
notation: DE-BW_061
references: https://data.geoscience.earth/ncl/geoera/ref/6373
created: 2020-11-23T14:24:51.080Z
definition: W-E streichende, ca. 85° nach S einfallende Abschiebung. @de
definition: W-E striking, approx. 85° S dipping normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_055]
type: Fault
type: Limit
definition: W-E streichende, ca. 75° nach S einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
created: 2020-11-23T14:24:51.016Z
type: Concept
notation: DE-BW_037
sf touches: [hl_081]
sf touches: [hl_092]
sf touches: [hl_090]
definition: W-E striking, approx. 75° S dipping normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

Pöring Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.053Z
notation: DE-BY_1088
preferred label: Pöring Störung @de
definition: W-E striking, approx. 80° S dipping synthetic normal fault.
definition: W-E streichende, ca. 80° nach S einfallende synthetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1088
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Stiefenhofen-Betzigau Fault
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:30.418Z
notation: DE-BY_1152
preferred label: Stiefenhofen-Betzigau Störung @de
definition: WSW-ENE trending, on average approx. 65° NNW dipping antithetic normal fault, probably connected to Möstenberg-Unterthingau Fault [DE-BY_1151].
definition: WSW-ENE verlaufende, durchschnittlich ca. 65° nach NNW einfallende antithetische Abschiebung. Wahrscheinlich mit Möstenberg-Unterthingau Störung [DE-BY_1151] verbunden. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1152
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Möstenberg-Unterthingau Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: Binzenried-Unterthingau Fault
type: Concept
created: 2020-10-09T11:35:30.390Z
notation: DE-BY_1151
preferred label: Möstenberg-Unterthingau Störung @de
definition: WSW-ENE striking, approx. 80° NNW dipping antithetic normal fault beneath Kempter Wald.
definition: WSW-ENE streichende, ca. 80° nach NNW einfallende antithetische Abschiebung unter dem Kempter Wald. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1151
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Binzenried-Unterthingau Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: Möstenberg-Unterthingau Fault
type: Concept
created: 2020-10-09T11:35:30.362Z
notation: DE-BY_1150
preferred label: Binzenried-Unterthingau Störung @de
definition: W-E striking, approx. 70° N dipping antithetic normal fault north of Kempter Wald.
definition: W-E streichende, ca. 70° nach N einfallende antithetische Abschiebung nördlich des Kempter Walds. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1150
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Änger-Kempten Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: Änger-Probstried Fault
type: Concept
created: 2020-10-09T11:35:30.335Z
notation: DE-BY_1149
preferred label: Änger-Kempten Störung @de
definition: W-E striking, approx. 55° SE dipping synthetic normal fault west of Kempten.
definition: W-E streichende, ca. 55° nach S einfallende synthetische Abschiebung westlich von Kempten. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1149
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Änger-Probstried Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
sf touches: Unterkürnach-Probstried Fault
sf touches: Änger-Kempten Fault
type: Concept
created: 2020-10-09T11:35:30.307Z
notation: DE-BY_1148
preferred label: Änger-Probstried Störung @de
definition: SSW-NNE to SW-NE trending, approx. 85° ESE to SE dipping synthetic normal fault northwest of Kempten.
definition: SSW-NNE bis SW-NE verlaufende, in etwa 85° nach ESE bis SE einfallende synthetische Abschiebung nordwestlich von Kempten. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1148
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Unterkürnach-Probstried Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: Änger-Probstried Fault
type: Concept
created: 2020-10-09T11:35:30.280Z
notation: DE-BY_1147
preferred label: Unterkürnach-Probstried Störung @de
definition: WSW-ENE striking, approx. 70° SSE dipping synthetic normal fault northwest of Kempten.
definition: WSW-ENE streichende, in etwa 70° nach SSE einfallende synthetische Abschiebung nordwestlich von Kempten. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1147
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

[lca_060]
type: Fault
type: Limit
sf touches: [lca_022]
definition: WNW-ESE striking, approx. 60° SSW dipping normal fault
references: https://data.geoscience.earth/ncl/geoera/ref/6357
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6373
created: 2020-11-23T14:24:51.171Z
definition: WNW-ESE streichende, ca. 60° nach SSW einfallende Abschiebung. @de
notation: DE-BW_092
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

Starnberg Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.191Z
notation: DE-BY_1093
preferred label: Starnberg Störung @de
definition: Running from Maising to Forstenrieder Park southwest of Munich, SW-NE trending, approx. 85° SE dipping synthetic normal fault. subparallel to antithetic Percha Fault [DE-BY_1092] in the southeast, this probably conjugate pair of faults forms a local graben structure.
definition: Von Maising zum Forstenrieder Park südwestlich von München SW-NE verlaufende, ca. 85° nach SE einfallende synthetische Abschiebung. Subparallel zur antithetischen Percha Störung [DE-BY_1092] im Nordwesten bildet dieses wahrscheinlich konjugierte Störungspaar eine lokale Grabenstruktur. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1093
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Percha Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.164Z
notation: DE-BY_1092
preferred label: Percha Störung @de
definition: Running from Neusöcking to Forstenrieder Park southwest of Munich, SW-NE trending, approx. 80° NW dipping antithetic normal fault. subparallel to synthetic Starnberg Fault [DE-BY_1093] in the northwest, this probably conjugate pair of faults forms a local graben structure.
definition: Von Neusöcking zum Forstenrieder Park südwestlich von München SW-NE verlaufende, ca. 80° nach NW einfallende antithetische Abschiebung. Subparallel zur synthetischen Starnberg Störung [DE-BY_1093] im Südosten bildet dieses wahrscheinlich konjugierte Störungspaar eine lokale Grabenstruktur. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1092
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Lindau-Lindenberg Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:30.528Z
notation: DE-BY_1156
preferred label: Lindau-Lindenberg Störung @de
definition: SW-NE striking, approx. 80° SE dipping synthetic normal fault parallel to Lindau-Hergatz Fault [DE-BY-846].
definition: SW-NE streichende, ca. 85° nach NW einfallende synthetische Abschiebung parallel zur Lindau-Hergatz Störung [DE-BY-846]. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1156
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Scheidegg-Gestratz Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:30.501Z
notation: DE-BY_1155
preferred label: Scheidegg-Gestratz Störung @de
definition: SW-NE striking, approx. 85° NW dipping antithetic normal fault.
definition: SW-NE streichende, ca. 85° nach NW einfallende antithetische Abschiebung nördlich des Kempter Walds. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1155
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Maierhöfen-Röthenbach Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:30.473Z
notation: DE-BY_1154
preferred label: Maierhöfen-Röthenbach Störung @de
definition: SW-NE striking, approx. 65° NW dipping antithetic normal fault.
definition: SW-NE streichende, ca. 65° nach NW einfallende antithetische Abschiebung nördlich des Kempter Walds. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1154
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Hohenbrunn-Grasbrunn Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:27.081Z
notation: DE-BY_1089
preferred label: Hohenbrunn-Grasbrunn Störung @de
definition: WSW-ENE trending, approx. 75° SSE dipping synthetic normal fault.
definition: WSW-ENE streichende, ca. 75° nach SSE einfallende synthetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1089
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Maierhöfen-Ellhofen Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:30.446Z
notation: DE-BY_1153
preferred label: Maierhöfen-Ellhofen Störung @de
definition: SW-NE trending, approx. 75° SE dipping synthetic normal fault.
definition: SW-NE verlaufende, ca. 75° nach SE einfallende synthetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1153
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

[lca_067]
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6373
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6357
definition: SW-NE striking, approx. 60° SE dipping normal fault
notation: DE-BW_076
created: 2020-11-23T14:24:51.121Z
definition: SW-NE streichende, ca. 60° nach SE einfallende Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_068]
type: Fault
type: Limit
sf touches: [lca_069]
definition: WSW-ENE streichende, ca. 50° nach NNW einfallende Abschiebung. @de
definition: WSW-ENE striking, approx. 50° NNW dipping normal fault
notation: DE-BW_086
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6373
references: https://data.geoscience.earth/ncl/geoera/ref/6357
created: 2020-11-23T14:24:51.153Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_069]
type: Fault
type: Limit
notation: DE-BW_085
references: https://data.geoscience.earth/ncl/geoera/ref/6373
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6357
sf touches: [lca_068]
definition: WSW-ENE streichende, ca. 65° nach SSE einfallende Abschiebung. @de
definition: WSW-ENE striking, approx. 65° SSE dipping normal fault
created: 2020-11-23T14:24:51.149Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_063]
type: Fault
type: Limit
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6373
notation: DE-BW_134
references: https://data.geoscience.earth/ncl/geoera/ref/6357
created: 2020-11-23T14:24:51.288Z
sf touches: [hl_047]
sf touches: [hl_045]
sf touches: [hl_057]
definition: W-E streichende, ca. 65° nach N einfallende Abschiebung. @de
sf touches: [lca_029]
sf touches: [hl_058]
definition: W-E striking, approx. 65° N dipping normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_064]
type: Fault
type: Limit
created: 2020-11-23T14:24:51.127Z
definition: WSW-ENE streichende, ca. 75° nach SSE einfallende Abschiebung. @de
notation: DE-BW_078
references: https://data.geoscience.earth/ncl/geoera/ref/6373
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6357
definition: WSW-ENE striking, approx. 75° SSE dipping normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

Ebersberg-Steinhöring Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.859Z
notation: DE-BY_885
preferred label: Ebersberg-Steinhöring Störung @de
definition: WSW-ESE striking, approx. 75° NNW dipping antithetic normal fault.
definition: WSW-ENE streichende, ca. 75° nach NNW einfallende antithetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_885
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Achering Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:29.499Z
notation: DE-BY_1132
preferred label: Achering Störung @de
definition: W-E striking, approx. 75° S dipping synthetic normal fault.
definition: SW-NE streichende, ca. 75° nach SE einfallende synthetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1132
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Hofoldinger Forst Fault
type: Limit
type: Fault
type: Concept
created: 2020-10-09T11:35:32.832Z
notation: DE-BY_884
preferred label: Hofoldinger Forst Störung @de
definition: SW-NE striking, approx. 75° NW dipping antithetic normal fault immediate north of and parallel to Otterfing Fault [DE-BY_883].
definition: SW-NE streichende, ca. 75° nach NW einfallende antithetische Abschiebung unmittelbar nördlich parallel zur synthetischen Otterfing Störung [DE-BY_883]. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_884
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Schwaig-Eitting Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:29.472Z
notation: DE-BY_1131
preferred label: Schwaig-Eitting Störung @de
definition: SW-NE striking, approx. 75° SE dipping synthetic normal fault.
definition: W-E streichende, ca. 75° nach S einfallende synthetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1131
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Otterfing Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.804Z
notation: DE-BY_883
preferred label: Otterfing Störung @de
definition: SW-NE striking, approx. 80° SE dipping synthetic normal fault immediate south of and parallel to antithetic Hofoldinger Forst Fault [DE-BY_884].
definition: SW-NE streichende, ca. 80° nach SE einfallende synthetische Abschiebung unmittelbar südlich parallel zur antithetischen Hofoldinger Forst Störung [DE-BY_884]. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_883
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Kreuzstrasse-Baiern Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.777Z
notation: DE-BY_1201
preferred label: Kreuzstraße-Baiern Störung @de
definition: WSW-ENE to SW-NE striking, approx.75° NNW to NW dipping antithetic normal fault.
definition: WSW-ENE bis SW-NE streichende, ca.75° nach NNW bis NW einfallende antithetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1201
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Petting Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:29.694Z
notation: DE-BY_1135
preferred label: Petting Störung @de
definition: Slightly undulate WSW-ENE trending, approx. 70° NNW dipping antithetic normal fault east of Traunstein.
definition: Leicht gewellt WSW-ENE verlaufende, ca. 70° nach NNW einfallende antithetische Abschiebung östlich von Traunstein. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1135
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Ismaning-Neufinsing Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.026Z
notation: DE-BY_887
preferred label: Ismaning-Neufinsing Störung @de
definition: NW-SE striking, approx. 85° SW dipping normal fault.
definition: NW-SE streichende, ca. 85° nach SW einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
sf touches: Ismaning-Zengermoos Cross-fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_887
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Traunstein Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:29.666Z
notation: DE-BY_805
preferred label: Traunstein Störung @de
definition: W-E trending, approx. 50° N dipping antithetic normal fault.
definition: W-E verlaufende, ca. 50° nach N einfallende antithetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_805
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Ismaning-Zengermoos Cross-fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.998Z
notation: DE-BY_1205
preferred label: Ismaning-Zengermoos Querstörung @de
definition: SW-NE striking, approx. 70° NW dipping antithetic normal fault.
definition: SW-NE streichende, ca. 70° nach NW einfallende antithetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: Oberschleissheim-Walpertskirchen Fault
sf touches: Ismaning-Neufinsing Fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1205
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Chieming-Nussdorf Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
preferred label: Chieming-Nußdorf Störung @de
created: 2020-10-09T11:35:29.639Z
notation: DE-BY_804
definition: Northward arcuate W-E striking, approx. 60° S dipping synthetic normal fault south of the Traunreut Step Fault.
definition: Nordwärts gebogene W-E streichende, ca. 60° nach S einfallende synthetische Abschiebung südlich der Traunreut Bruchstaffel. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_804
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Oberschleissheim-Walpertskirchen Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.971Z
notation: DE-BY_1204
preferred label: Oberschleißheim-Walpertskirchen Störung @de
definition: WSW-ENE to WNW-ESE trending, averaged approx. 75° ± S dipping synthetic normal fault.
definition: WSW-ENE bis WNW-ESE verlaufende, im Mittel ca. 75° nach ± S einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: Ismaning-Zengermoos Cross-fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1204
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Penzing-Türkenfeld Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:29.611Z
notation: DE-BY_801
preferred label: Penzing-Türkenfeld Störung @de
definition: Northwestward arcuate WSW-ENE trending, approx. 80° ± NNW dipping antithetic normal fault running from Penzing to south of Geltendorf.
definition: Von Penzing bis südlich Geltendorf ziehende, nordwestwärts gebogen WSW-ENE verlaufende, ca. 80° nach ± NNW einfallende antithetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_801
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Dietersheim Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.943Z
notation: DE-BY_1203
preferred label: Dietersheim Störung @de
definition: WSW-ENE striking, approx. 70° SSE dipping synthetic normal fault.
definition: WSW-ENE streichende, ca. 70° nach SSE einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1203
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Buchloe-Landsberg Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: Stockheim-Buchloe Fault
type: Concept
created: 2020-10-09T11:35:29.583Z
notation: DE-BY_800
preferred label: Buchloe-Landsberg Störung @de
definition: Slightly arcuate W-E to WSW-ENE trending, approx. 70° S to SSE dipping synthetic normal fault running from Buchloe to Thalhofen.
definition: Leicht gebogen von Buchloe bis Thalhofen ziehende, W-E bis WSW-ENE verlaufende, ca. 70° nach S bis SSE einfallende synthetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_800
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Eching-Erching Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.915Z
notation: DE-BY_1202
preferred label: Eching-Erching Störung @de
definition: WNW-ESE striking, approx. 70° SSW dipping synthetic normal fault.
definition: WNW-ESE streichende, ca. 70° nach SSW einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1202
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Eichenried-Pretzen Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:32.887Z
notation: DE-BY_888
preferred label: Eichenried-Pretzen Störung @de
definition: Southward arcuate W-E trending, approx. 65° S dipping synthetic normal fault south of Erding.
definition: Südwärts gebogen W-E verlaufende, ca. 65° nach S einfallende synthetische Abschiebung südlich von Erding. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_888
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Erding-Bockhorn Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:29.527Z
notation: DE-BY_1133
preferred label: Erding-Bockhorn Störung @de
definition: Slightly undulate, overall WSW-ENE trending, approx. 70° NNW dipping antithetic normal fault.
definition: Leicht gewellt, insgesamt WSW-ENE verlaufende, ca. 70° nach NNW einfallende antithetische Abschiebung. @de
narrower: Erding Subfault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1133
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Erding Subfault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:29.555Z
notation: DE-BY_1134
preferred label: Erding Nebenstörung @de
definition: WSW-ENE striking, approx. 70° NNW dipping antithetic normal fault subparallel to synthetic Erding-Altfraunhofen Fault [DE-BY_792], forming a local graben structure.
definition: WSW-ENE streichende, ca. 70° nach NNW einfallende antithetische Abschiebung. Bildet mit der nordwestlich subparallel verlaufenden synthetischen Erding-Altfraunhofen Fault [DE-BY_792] eine lokale Grabenstruktur. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1134
limit type: normalFault
broader: Erding-Bockhorn Fault

[lca_034]
type: Fault
type: Limit
notation: DE-BW_110
references: https://data.geoscience.earth/ncl/geoera/ref/6357
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6373
created: 2020-11-23T14:24:51.228Z
definition: W-E to WSW-ENE trending, approx. 70° N to NNW dipping normal fault
definition: W-E bis WSW-ENE streichende, ca. 70° nach NNW einfallende Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_035]
type: Fault
type: Limit
definition: WNW-ESE striking, approx. 70° SSW dipping normal fault
notation: DE-BW_109
references: https://data.geoscience.earth/ncl/geoera/ref/6357
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6373
definition: WNW-ESE streichende, ca. 70° nach SSW einfallende Abschiebung. @de
created: 2020-11-23T14:24:51.225Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_036]
type: Fault
type: Limit
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6357
definition: WNW-ESE striking, approx. 65° NNE dipping normal fault
references: https://data.geoscience.earth/ncl/geoera/ref/6373
created: 2020-11-23T14:24:51.219Z
definition: WNW-ESE streichende, ca. 65° nach NNE einfallende Abschiebung. @de
notation: DE-BW_107
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_037]
type: Fault
type: Limit
definition: WNW-ESE striking, approx. 70° NNE dipping normal fault
references: https://data.geoscience.earth/ncl/geoera/ref/6373
type: Concept
created: 2020-11-23T14:24:51.222Z
notation: DE-BW_108
references: https://data.geoscience.earth/ncl/geoera/ref/6357
definition: WNW-ESE streichende, ca. 70° nach NNE einfallende Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_090]
type: Fault
type: Limit
notation: DE-BW_038
sf touches: [hl_091]
definition: W-E streichende, ca. 75° nach N einfallende Abschiebung. @de
definition: W-E striking, approx. 75° N dipping normal fault
sf touches: [lca_055]
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-11-23T14:24:51.019Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_030]
type: Fault
type: Limit
notation: DE-BW_089
type: Concept
definition: WSW-ENE striking, approx. 60° SSE dipping normal fault
references: https://data.geoscience.earth/ncl/geoera/ref/6373
references: https://data.geoscience.earth/ncl/geoera/ref/6357
created: 2020-11-23T14:24:51.162Z
definition: WSW-ENE streichende, ca. 60° nach SSE einfallende Abschiebung. @de
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_031]
type: Fault
type: Limit
definition: SW-NE streichende, ca. 75° nach NW einfallende Abschiebung. @de
created: 2020-11-23T14:24:51.124Z
definition: SW-NE striking, approx. 75° NW dipping normal fault
notation: DE-BW_077
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6373
references: https://data.geoscience.earth/ncl/geoera/ref/6357
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_032]
type: Fault
type: Limit
type: Concept
notation: DE-BW_063
definition: NW-SE streichende, ca. 85° nach NE einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6373
references: https://data.geoscience.earth/ncl/geoera/ref/6357
created: 2020-11-23T14:24:51.086Z
definition: NW-SE striking, approx. 85° NE dipping normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_033]
type: Fault
type: Limit
created: 2020-11-23T14:24:51.062Z
definition: W-E streichende, ca. 75° nach N einfallende Abschiebung. @de
definition: W-E striking, approx. 75° N dipping normal fault
type: Concept
notation: DE-BW_055
references: https://data.geoscience.earth/ncl/geoera/ref/6373
references: https://data.geoscience.earth/ncl/geoera/ref/6357
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_093]
type: Fault
type: Limit
sf touches: [lca_004]
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/4097
definition: WNW-ESE streichende, ca. 75° nach NNE einfallende Abschiebung. @de
created: 2020-11-23T14:24:51.078Z
notation: DE-BW_060
definition: WNW-ESE striking, approx. 75° NNE dipping normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_096]
type: Fault
type: Limit
definition: SW-NE striking, approx. 75° SE dipping normal fault
created: 2020-11-23T14:24:51.027Z
notation: DE-BW_042
references: https://data.geoscience.earth/ncl/geoera/ref/4097
definition: SW-NE streichende, ca. 75° nach SE einfallende Abschiebung. @de
type: Concept
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_038]
type: Fault
type: Limit
type: Concept
definition: SSW-NNE streichende, ca. 60° nach ESE einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6373
created: 2020-11-23T14:24:51.246Z
references: https://data.geoscience.earth/ncl/geoera/ref/6357
notation: DE-BW_116
definition: SSW-NNE striking, approx. 60° ESE dipping normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[hl_098]
type: Fault
type: Limit
definition: W-E streichende, ca. 65° nach N einfallende Abschiebung. @de
created: 2020-11-23T14:24:51.410Z
notation: DE-BW_170
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
definition: W-E striking, approx. 65° N dipping normal fault.
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_039]
type: Fault
type: Limit
definition: SW-NE streichende, ca. 70° nach SE einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6373
type: Concept
created: 2020-11-23T14:24:51.240Z
definition: SW-NE trending, approx. 70° SE dipping normal fault
notation: DE-BW_114
references: https://data.geoscience.earth/ncl/geoera/ref/6357
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

Dinkelscherben-Ried Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.164Z
notation: DE-BY_896
preferred label: Dinkelscherben-Ried Störung @de
definition: NW-SE striking, steeply (85°-60°) SW dipping synthetic normal fault.
definition: NW-SE streichende, steil (85°-60°) nach SW einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: Krumbach-Dinkelscherben Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_896
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Moosach-Grafing Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:29.805Z
notation: DE-BY_1138
preferred label: Moosach-Grafing Störung @de
definition: W-E striking, approx. 80° S dipping synthetic normal fault.
definition: W-E streichende, ca. 80° nach S einfallende synthetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1138
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Krumbach-Dinkelscherben Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.136Z
notation: DE-BY_895
preferred label: Krumbach-Dinkelscherben Störung @de
definition: SW-NE trending, steeply (85°-60°) NW dipping antithetic normal fault.
definition: SW-NE verlaufende, steil (85°-60°) nach NW einfallende antithetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
sf touches: Dinkelscherben-Ried Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_895
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Glonn-Bruck Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:29.777Z
notation: DE-BY_1137
preferred label: Glonn-Bruck Störung @de
definition: WSW-ENE striking, approx. 80° NNW dipping antithetic normal fault.
definition: WSW-ENE streichende, ca. 80° nach NNW einfallende antithetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1137
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Grünbach-Kalling Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.108Z
notation: DE-BY_890
preferred label: Grünbach-Kalling Störung @de
definition: W-E to WNW-ENE trending, approx. 60° ± N dipping antithetic normal fault.
definition: W-E bis WNW-ESE verlaufende, ca. 60° nach ± N einfallende antithetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_890
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Kirchasch-Algasing Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.081Z
notation: DE-BY_889
preferred label: Kirchasch-Algasing Störung @de
definition: WSW-ENE to WNW-ESE trending, averaged approx. 80° ± S dipping synthetic normal fault.
definition: WSW-ENE bis WNW-ESE verlaufende, im Mittel ca. 80° nach ± S einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_889
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Wonneberg Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:29.722Z
notation: DE-BY_1136
preferred label: Wonneberg Störung @de
definition: WSW-ENE striking, approx. 70° SSE dipping synthetic normal fault northeast of Traunstein.
definition: WSW-ENE streichende, ca. 70° nach SSE einfallende synthetische Abschiebung nordöstlich von Traunstein. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1136
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Neuching-Wörth Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.054Z
notation: DE-BY_1206
preferred label: Neuching-Wörth Störung @de
definition: W-E trending, approx. 65° S dipping synthetic normal fault. Kinematic relation to contiguous Markt Schwaben Verwurf [DE-BY_725] unresolved.
definition: W-E verlaufende, ca. 65° nach S einfallende synthetisch Abschiebung. Kinematische Beziehung zum angrenzenden Markt Schwaben Verwurf [DE-BY_725] noch ungeklärt. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: Markt Schwaben Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1206
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Lengdorf Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:26.640Z
notation: DE-BY_715
preferred label: Lengdorf Störung @de
definition: Arcuate W-ESE striking, approx. 60° N dipping antithetic normal fault.
definition: Bogenförmig W-ESE verlaufende, ca. 60° nach N einfallende antithetische Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_715
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Karpfenwinkel Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:29.971Z
notation: DE-BY_1139
preferred label: Karpfenwinkel Störung @de
definition: SW-NE striking, approx. 80° SE dipping synthetic normal fault northwest of Bernried.
definition: SW-NE streichende, ca. 80° nach SE einfallende synthetische Abschiebung nordwestlich von Bernried. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1139
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Haselbach-Mickhausen Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.303Z
notation: DE-BY_1211
preferred label: Haselbach-Mickhausen Störung @de
definition: SW-NE striking, approx. 75° SE dipping synthetic normal fault.
definition: SW-NE streichende, ca. 75° nach SE einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
sf touches: Mörgen-Walkershofen Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1211
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

[lca_040]
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6373
type: Concept
definition: SW-NE striking, approx. 80° SE dipping normal fault
notation: DE-BW_112
references: https://data.geoscience.earth/ncl/geoera/ref/6357
definition: SW-NE streichende, ca. 80° nach SE einfallende Abschiebung. @de
created: 2020-11-23T14:24:51.234Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

Isen-Ampfing Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:26.585Z
notation: DE-BY_713
alternative label: Ampfinger Hauptstörung @de
preferred label: Isen-Ampfing Störung @de
definition: Overall W-E trending, averaged approx. 55° N dipping antithetic normal fault running from Pastetten to Altmühldorf; northern boundary of oil- and gasfields Isen, Weitermühle-Steinkirchen, and Ampfing.
definition: Von Pastetten nach Altmühldorf ziehende, insgesamt W-E verlaufende, im Durchschnitt ca. 55° nach N einfallende antithetische Abschiebung; nördliche Begrenzung der Öl- und Gasfelder Isen, Weitermühle-Steinkirchen und Ampfing. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4109
narrower: Ampfing Subfault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_713
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Ampfing Subfault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:26.613Z
notation: DE-BY_714
alternative label: Ampfinger Querstörung @de
preferred label: Ampfing Nebenstörung @de
definition: NW-SE striking, steeply (85°-60°) NE dipping antithetic normal fault close to Ampfing oil- and gasfield.
definition: NW-SE streichende, steil (85°-60°) nach NE einfallende antithesische Abschiebung am Öl- und Gasfeld Ampfing. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_714
limit type: normalFault
broader: Isen-Ampfing Fault

Tutzing-Icking Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
sf touches: Deining Subfault
type: Concept
created: 2020-10-09T11:35:29.943Z
notation: DE-BY_803
preferred label: Tutzing-Icking Störung @de
definition: Slightly undulate WSW-ENE trending, approx. 80° SSE dipping synthetic normal fault.
definition: Leicht gewellt WSW-ENE verlaufende, ca. 80° nach SSE einfallende synthetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_803
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Stolzenhofen-Hasberg Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.275Z
notation: DE-BY_1210
preferred label: Stolzenhofen-Hasberg Störung @de
definition: SW-NE trending, approx. 85° SE dipping synthetic normal fault.
definition: SW-NE verlaufende, ca. 85° nach SE einfallende synthetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1210
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Walpertskirchen-Dorfen Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:26.557Z
notation: DE-BY_932
preferred label: Walpertskirchen-Dorfen Störung @de
definition: W-E trending, approx. 70° S dipping synthetic normal fault. At its eastern end subparallel to antithetic Dorfen Fault.
definition: W-E verlaufende, ca.70° nach S einfallende synthetische Abschiebung, in ihrem östichen Teil subparallel zur antithetischen Dorfen Störung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_932
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Reichau-Hasberg Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.247Z
notation: DE-BY_1209
preferred label: Reichau-Hasberg Störung @de
definition: SW-NE striking, approx.75° SE dipping synthetic normal fault probably linked to Aletshausen-Langenneufnach Fault [DE-BY_1208] via a relay ramp.
definition: SW-NE streichende, ca. 75° nach SE einfallende synthetische Abschiebung; wahrscheinlich über eine Relais Rampe (relay ramp) mit der Aletshausen-Langenneufnach Störung [DE-BY_1208] verbunden. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1209
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Dorfen Fault
type: Fault
type: Limit
type: SpatialObject
type: Concept
created: 2020-10-09T11:35:26.530Z
notation: DE-BY_712
preferred label: Dorfen Störung @de
definition: W-E trending, approx. 55° N dipping antithetic normal fault running from Dorfen to Schwindegg; northern boundary of oil- and gasfields Dorfen und Dorfen-Ost.
definition: Von Dorfen bis Schwindegg W-E verlaufende, ca. 55° nach N einfallende antithetische Abschiebung; nördliche Begrenzung der Öl- und Gasfelder Dorfen und Dorfen-Ost. @de
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4109
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_712
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Aletshausen-Langenneufnach Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.219Z
notation: DE-BY_1208
preferred label: Aletshausen-Langenneufnach Störung @de
definition: SW-NE to WSW-ENE trending, approx. 75° SE to SSE dipping synthetic normal fault probably linked to Reichau-Hasberg Fault [DE-BY_1209] via a relay ramp.
definition: SW-NE bis WSW-ENE verlaufende, ca. 75° nach SE bis SSE einfallende synthetische Abschiebung; wahrscheinlich über eine Relais Rampe (relay ramp) mit der Reichau-Hasberg Störung [DE-BY_1209] verbunden. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1208
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Münsing-Brunnthal Fault
type: Fault
type: Limit
sf touches: Wolfersberg-Moosach Fault
sf touches: Icking-Deining Lateral Fault
type: SpatialObject
sf touches: Deining Subfault
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:29.861Z
notation: DE-BY_808
preferred label: Münsing-Brunnthal Störung @de
definition: Undulate SW-NE to W-E trending, approx. 75° SE to S dipping synthetic normal fault.
definition: Gewellt SW-NE bis W-E verlaufende, ca. 75° nach SE bis S einfallende synthetische Abschiebung. @de
narrower: Dettenhausen-Sauerlach Subfault
narrower: Icking-Deining Lateral Fault
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_808
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Dettenhausen-Sauerlach Subfault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:29.916Z
notation: DE-BY_882
preferred label: Dettenhausen-Sauerlach Nebenstörung @de
definition: SW-NE striking, approx. 75° SE dipping synthetic normal fault. Branch of Münsing-Brunnthal Fault [DE-BY_808].
definition: SW-NE streichende, ca. 75° nach SE einfallende synthetische Abschiebung. Zweig der Münsing-Brunnthal Störung [DE-BY_808]. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_882
limit type: normalFault
broader: Münsing-Brunnthal Fault

Icking-Deining Lateral Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
references: https://data.geoscience.earth/ncl/geoera/ref/4078
type: Concept
created: 2020-10-09T11:35:29.888Z
notation: DE-BY_739
preferred label: Icking-Deining Querstörung @de
definition: W-E striking, approx. 85° S dipping synthetic normal fault obtuse-angled to Münsing-Brunnthal Fault [DE-BY_808].
definition: W-E streichende, ca. 85° nach S einfallende synthetische Abschiebung stumpfwinklig zur Münsing-Brunnthal Störung [DE-BY_808]. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_739
limit type: normalFault
broader: Münsing-Brunnthal Fault

Kirchhaslach-Aletshausen Fault
type: Fault
type: Limit
type: Concept
created: 2020-10-09T11:35:33.191Z
notation: DE-BY_1207
preferred label: Kirchhaslach-Aletshausen Störung @de
definition: SW-NE striking, approx. 60° NW dipping antithetic normal fault.
definition: SW-NE streichende, ca. 60° nach NW einfallende antithetische Abschiebung. @de
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_1207
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

Grafing-Wasserburg Fault
type: Fault
type: Limit
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4078
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-09T11:35:29.833Z
notation: DE-BY_807
preferred label: Grafing-Wasserburg Störung @de
definition: Undulate WSW-ENE trending, approx. 75° NNW dipping antithetic normal fault.
definition: Gewellt WSW-ENE verlaufende, ca. 75° nach NNW einfallende antithetische Abschiebung. @de
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
notation: LfU-BY_807
limit type: normalFault
broader: Central Foreland Molasse Basin fault domain

[lca_046]
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6373
references: https://data.geoscience.earth/ncl/geoera/ref/6357
definition: SW-NE streichende, ca. 60° nach NW einfallende Abschiebung. @de
notation: DE-BW_050
created: 2020-11-23T14:24:51.049Z
narrower: [lca_045]
type: Concept
narrower: [lca_085]
definition: SW-NE striking, approx. 60° NW dipping normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_045]
type: Fault
type: Limit
definition: WSW-ENE striking, approx. 65° SSE dipping normal fault
type: Concept
notation: DE-BW_051
definition: WSW-ENE streichende, ca. 65° nach SSE einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6373
references: https://data.geoscience.earth/ncl/geoera/ref/6357
created: 2020-11-23T14:24:51.050Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [lca_046]

[lca_085]
type: Fault
type: Limit
notation: DE-BW_052
definition: WSW-ENE streichende, ca. 70° nach SSE einfallende Abschiebung. @de
definition: WSW-ENE striking, approx. 70° SSE dipping normal fault
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6357
references: https://data.geoscience.earth/ncl/geoera/ref/6373
created: 2020-11-23T14:24:51.052Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: [lca_046]

[lca_047]
type: Fault
type: Limit
created: 2020-11-23T14:24:51.297Z
notation: DE-BW_138
definition: SSW-NNE striking, approx. 75° ESE dipping normal fault
type: Concept
definition: SSW-NNE streichende, ca. 75° nach ESE einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6373
references: https://data.geoscience.earth/ncl/geoera/ref/6357
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_048]
type: Fault
type: Limit
definition: N-S striking, approx. 80° W dipping normal fault
notation: DE-BW_139
created: 2020-11-23T14:24:51.300Z
definition: N-S streichende, ca. 80° nach W einfallende Abschiebung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/6357
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6373
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_041]
type: Fault
definition: WSW-ENE streichende, ca. 70° nach SSE einfallende Abschiebung. @de
notation: DE-BW_113
created: 2020-11-23T14:24:51.237Z
definition: WSW-ENE striking, approx. 70° SSE dipping normal fault
references: https://data.geoscience.earth/ncl/geoera/ref/6373
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6357
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
type: Limit
broader: Central Foreland Molasse Basin fault domain

[lca_042]
type: Fault
type: Limit
references: https://data.geoscience.earth/ncl/geoera/ref/6373
references: https://data.geoscience.earth/ncl/geoera/ref/6357
definition: W-E streichende, ca. 80° nach N einfallende Abschiebung. @de
definition: W-E striking, approx. 80° N dipping normal fault
notation: DE-BW_111
type: Concept
created: 2020-11-23T14:24:51.231Z
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_043]
type: Fault
type: Limit
definition: WNW-ESE streichende, ca. 80° nach SSW einfallende Abschiebung. @de
type: Concept
references: https://data.geoscience.earth/ncl/geoera/ref/6373
references: https://data.geoscience.earth/ncl/geoera/ref/6357
notation: DE-BW_115
created: 2020-11-23T14:24:51.243Z
definition: WNW-ESE striking, approx. 80° SSW dipping normal fault
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

[lca_044]
type: Fault
type: Limit
created: 2020-11-23T14:24:51.059Z
references: https://data.geoscience.earth/ncl/geoera/ref/6373
references: https://data.geoscience.earth/ncl/geoera/ref/6357
notation: DE-BW_054
definition: WNW-ESE striking, approx. 80° SSW dipping normal fault
definition: WNW-ESE streichende, ca. 80° nach SSW einfallende Abschiebung. @de
type: Concept
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Central Foreland Molasse Basin fault domain

Tectonic Boundary in Iceland
scope note: All named tectonic boundary objects that are located (at least partly) in Austria, are identified by an ID with the prefix „IS“ listed in the notation.
definition: Instance of a fault or a fissure displayed in the HIKE fault database, as they are represented in the Geological Map of Iceland at 1:600 000 scale and selected faults and fissures on Iceland’s Insular Shelf and Adjacent Deep Ocean
type: Concept
top concept of: Tectonic Boundary Objects in Europe
created: 2020-10-14T11:23:03.262Z
notation: IS-0
narrower: Reykjanes Oblique Rift
narrower: Grímsey Oblique Rift
narrower: Western Volcanic Zone
narrower: Snæfellsnes Volcanic Zone
narrower: Central Volcanic Zone
narrower: Eastern Volcanic Zone
narrower: Northern Volcanic Zone
narrower: South-Iceland Seismic Transform Zone
narrower: Húsavík-Flatey Transform Zone
narrower: Borgarfjörður Zone
narrower: Eyjafjarðaráll Rift Zone
references: https://data.geoscience.earth/ncl/geoera/ref/4608
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe

Eyjafjarðaráll Rift Zone
type: Concept
created: 2020-10-14T11:23:05.673Z
notation: IS-11
definition: From western end of the Húsavík-Flatey Fault zone to the Kolbeinsey Ridge
references: https://data.geoscience.earth/ncl/geoera/ref/4608
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Iceland

Húsavík-Flatey Transform Zone
type: Concept
created: 2020-10-14T11:23:05.618Z
notation: IS-9
definition: From Húsavík to the Eyjafjarðaráll Rift
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Iceland

Borgarfjörður Zone
type: Concept
created: 2020-10-14T11:23:05.646Z
notation: IS-10
definition: Between Snæfellsnes Volcanic Zone and the Central Volcanic Zone
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Iceland

Grímsey Oblique Rift
type: Concept
created: 2020-10-14T11:23:03.736Z
notation: IS-2
definition: From Öxarfjörður to the Kolbeinsey Ridge
narrower: Grímsey Earthquake Fault Set
narrower: Mánáreyjar Fissure Set
narrower: Skjálfandi Fault Set
narrower: Nafir Fault Set
narrower: Hóllinn Fault and Fissure Sets
narrower: Stóragrunn Fault and Fissure Sets
references: https://data.geoscience.earth/ncl/geoera/ref/4609
references: https://data.geoscience.earth/ncl/geoera/ref/4608
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Iceland

Grímsey Earthquake Fault Set
type: Concept
created: 2020-10-14T11:23:03.764Z
notation: IS-21
definition: Earthquake faults in the Grímsey Earthquake Fault set
narrower: Grímsey Strike-slip Fault Set
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Grímsey Oblique Rift

Grímsey Strike-slip Fault Set
type: Concept
created: 2020-10-14T11:23:03.792Z
notation: IS-211
definition: Strike-slip faults in the Grímsey earthquake fault set
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Grímsey Earthquake Fault Set

Stóragrunn Fault and Fissure Sets
type: Concept
created: 2020-10-14T11:23:03.989Z
notation: IS-26
definition: Faults and fissures in the Stóragrunn fissure swarm
narrower: Stóragrunn Fault Set
narrower: Stóragrunn Fissure Set
references: https://data.geoscience.earth/ncl/geoera/ref/4608
in scheme: Tectonic Boundary Objects in Europe
broader: Grímsey Oblique Rift

Stóragrunn Fissure Set
type: Concept
created: 2020-10-14T11:23:04.045Z
notation: IS-262
definition: Fissures in the Stóragrunn fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4608
in scheme: Tectonic Boundary Objects in Europe
broader: Stóragrunn Fault and Fissure Sets

Stóragrunn Fault Set
type: Concept
created: 2020-10-14T11:23:04.017Z
notation: IS-261
definition: Faults in the Stóragrunn fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4608
in scheme: Tectonic Boundary Objects in Europe
broader: Stóragrunn Fault and Fissure Sets

Nafir Fault Set
type: Concept
created: 2020-10-14T11:23:03.876Z
notation: IS-241
definition: Faults in the Nafir fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4608
in scheme: Tectonic Boundary Objects in Europe
broader: Grímsey Oblique Rift

Hóllinn Fault and Fissure Sets
type: Concept
created: 2020-10-14T11:23:03.904Z
notation: IS-25
definition: Faults and fissures in the Hóllinn fissure swarm
narrower: Hóllinn Fault Set
narrower: Hóllinn Fissure Set
references: https://data.geoscience.earth/ncl/geoera/ref/4608
in scheme: Tectonic Boundary Objects in Europe
broader: Grímsey Oblique Rift

Hóllinn Fault Set
type: Concept
created: 2020-10-14T11:23:03.932Z
notation: IS-251
definition: Faults in the Hóllinn fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4608
in scheme: Tectonic Boundary Objects in Europe
broader: Hóllinn Fault and Fissure Sets

Hóllinn Fissure Set
type: Concept
created: 2020-10-14T11:23:03.961Z
notation: IS-252
definition: Fissures in the Hóllinn fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4608
in scheme: Tectonic Boundary Objects in Europe
broader: Hóllinn Fault and Fissure Sets

Mánáreyjar Fissure Set
type: Concept
created: 2020-10-14T11:23:03.820Z
notation: IS-221
definition: Fissures in the Mánáreyjar fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4608
in scheme: Tectonic Boundary Objects in Europe
broader: Grímsey Oblique Rift

Skjálfandi Fault Set
type: Concept
created: 2020-10-14T11:23:03.848Z
notation: IS-231
definition: Faults in the Skjálfandi fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4608
in scheme: Tectonic Boundary Objects in Europe
broader: Grímsey Oblique Rift

Western Volcanic Zone
type: Concept
created: 2020-10-14T11:23:04.073Z
notation: IS-3
definition: Reaches from the Reykjanes Oblique Rift northeast to Hofsjökull glacier
narrower: Þingvellir Fault and Fissure Sets
narrower: Prestahnúkur Fault Set
narrower: Hveravellir Fault and Fissure Sets
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Iceland

Þingvellir Fault and Fissure Sets
type: Concept
created: 2020-10-14T11:23:04.100Z
notation: IS-31
definition: Faults and fissures in the Þingvellir fissure swarm
narrower: Þingvellir Fault Set
narrower: Þingvellir Fissure Set
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Western Volcanic Zone

Þingvellir Fault Set
type: Concept
created: 2020-10-14T11:23:04.128Z
notation: IS-311
definition: Faults in the Þingvellir fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Þingvellir Fault and Fissure Sets

Þingvellir Fissure Set
type: Concept
created: 2020-10-14T11:23:04.155Z
notation: IS-312
definition: Fissures in the Þingvellir fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Þingvellir Fault and Fissure Sets

Prestahnúkur Fault Set
type: Concept
created: 2020-10-14T11:23:04.182Z
notation: IS-321
definition: Faults in the Prestahnúkur fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Western Volcanic Zone

Hveravellir Fault and Fissure Sets
type: Concept
created: 2020-10-14T11:23:04.210Z
notation: IS-33
definition: Faults and fissures in the Hveravellir fissure swarm
narrower: Hveravellir Fault Set
narrower: Hveravellir Fissure Set
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Western Volcanic Zone

Hveravellir Fault Set
type: Concept
created: 2020-10-14T11:23:04.238Z
notation: IS-331
definition: Faults in the Hveravellir fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Hveravellir Fault and Fissure Sets

Hveravellir Fissure Set
type: Concept
created: 2020-10-14T11:23:04.265Z
notation: IS-332
definition: Fissures in the Hveravellir fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Hveravellir Fault and Fissure Sets

South-Iceland Seismic Transform Zone
type: Concept
created: 2020-10-14T11:23:05.591Z
notation: IS-8
definition: Between Reykjanes Oblique Rift and the Eastern Volcanic Zone
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Iceland

Snæfellsnes Volcanic Zone
type: Concept
created: 2020-10-14T11:23:04.293Z
notation: IS-4
definition: Located on the Snæfellsnes Peninsula in the west of Iceland
narrower: Snæfellsjökull Fissure Set
narrower: Lýsuhyrna-Helgrindur Fissure Set
narrower: Ljósufjöll Fault and Fissure Sets
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Iceland

Ljósufjöll Fault and Fissure Sets
type: Concept
created: 2020-10-14T11:23:04.375Z
notation: IS-43
definition: Faults and fissures in the Ljósufjöll fissure swarm
narrower: Ljósufjöll Fault Set
narrower: Ljósufjöll Fissure Set
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Snæfellsnes Volcanic Zone

Ljósufjöll Fault Set
type: Concept
created: 2020-10-14T11:23:04.403Z
notation: IS-431
definition: Faults in the Ljósufjöll fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Ljósufjöll Fault and Fissure Sets

Ljósufjöll Fissure Set
type: Concept
created: 2020-10-14T11:23:04.430Z
notation: IS-432
definition: Fissures in the Ljósufjöll fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Ljósufjöll Fault and Fissure Sets

Lýsuhyrna-Helgrindur Fissure Set
type: Concept
created: 2020-10-14T11:23:04.348Z
notation: IS-421
definition: Fissures in the Lýsuhyrna-Helgrindur fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Snæfellsnes Volcanic Zone

Snæfellsjökull Fissure Set
type: Concept
created: 2020-10-14T11:23:04.320Z
notation: IS-411
definition: Fissures in the Snæfellsjökull fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Snæfellsnes Volcanic Zone

Eastern Volcanic Zone
type: Concept
created: 2020-10-14T11:23:04.540Z
notation: IS-6
definition: From Mýrdalsjökull to Askja north of Vatnajökull
narrower: Hekla-Vatnafjöll Fissure Set
narrower: Torfajökull Fissure Set
narrower: Veiðivötn Fault and Fissure Sets
narrower: Katla-Eldgjá Fault and Fissure Sets
narrower: Laki Fault and Fissure Sets
narrower: Rauðhólar Fault and Fissure Sets
narrower: Hamarinn Fissure Set
narrower: Gjálp Fissure Set
narrower: Vonarskarð Fissure Set
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Iceland

Gjálp Fissure Set
type: Concept
created: 2020-10-14T11:23:04.980Z
notation: IS-681
definition: Fissures in the Gjálp fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Eastern Volcanic Zone

Katla-Eldgjá Fault and Fissure Sets
type: Concept
created: 2020-10-14T11:23:04.705Z
notation: IS-64
definition: Faults and fissures in the Katla-Eldgjá fissure swarm
narrower: Katla-Eldgjá Fault Set
narrower: Katla-Eldgjá Fissure Set
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Eastern Volcanic Zone

Katla-Eldgjá Fault Set
type: Concept
created: 2020-10-14T11:23:04.732Z
notation: IS-641
definition: Faults in the Katla-Eldgjá fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Katla-Eldgjá Fault and Fissure Sets

Katla-Eldgjá Fissure Set
type: Concept
created: 2020-10-14T11:23:04.759Z
notation: IS-642
definition: Fissures in the Katla-Eldgjá fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Katla-Eldgjá Fault and Fissure Sets

Vonarskarð Fissure Set
type: Concept
created: 2020-10-14T11:23:05.008Z
notation: IS-691
definition: Fissures in the Vonarskarð fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Eastern Volcanic Zone

Hamarinn Fissure Set
type: Concept
created: 2020-10-14T11:23:04.952Z
notation: IS-671
definition: Fissures in the Hamarinn fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Eastern Volcanic Zone

Torfajökull Fissure Set
type: Concept
created: 2020-10-14T11:23:04.595Z
notation: IS-621
definition: Fissures in the Torfajökull fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Eastern Volcanic Zone

Veiðivötn Fault and Fissure Sets
type: Concept
created: 2020-10-14T11:23:04.622Z
notation: IS-63
definition: Faults and fissures in the Veiðvötn fissure swarm
narrower: Veiðivötn Fault Set
narrower: Veiðivötn Fissure Set
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Eastern Volcanic Zone

Veiðivötn Fissure Set
type: Concept
created: 2020-10-14T11:23:04.677Z
notation: IS-632
definition: Fissures in the Veiðivötn fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Veiðivötn Fault and Fissure Sets

Veiðivötn Fault Set
type: Concept
created: 2020-10-14T11:23:04.650Z
notation: IS-631
definition: Faults in the Veiðivötn fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Veiðivötn Fault and Fissure Sets

Hekla-Vatnafjöll Fissure Set
type: Concept
created: 2020-10-14T11:23:04.568Z
notation: IS-611
definition: Fissures in the Hekla-Vatnafjöll fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Eastern Volcanic Zone

Rauðhólar Fault and Fissure Sets
type: Concept
created: 2020-10-14T11:23:04.870Z
notation: IS-66
definition: Faults and fissures in the Rauðhólar fissure swarm
narrower: Rauðhólar Fault Set
narrower: Rauðhólar Fissure Set
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Eastern Volcanic Zone

Rauðhólar Fissure Set
type: Concept
created: 2020-10-14T11:23:04.924Z
notation: IS-662
definition: Fissures in the Rauðhólar fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Rauðhólar Fault and Fissure Sets

Rauðhólar Fault Set
type: Concept
created: 2020-10-14T11:23:04.897Z
notation: IS-661
definition: Faults in the Rauðhólar fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Rauðhólar Fault and Fissure Sets

Laki Fault and Fissure Sets
type: Concept
created: 2020-10-14T11:23:04.787Z
notation: IS-65
definition: Faults and fissures in the Laki fissure swarm
narrower: Laki Fault Set
narrower: Laki Fissure Set
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Eastern Volcanic Zone

Laki Fissure Set
type: Concept
created: 2020-10-14T11:23:04.842Z
notation: IS-652
definition: Fissures in the Laki fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Laki Fault and Fissure Sets

Laki Fault Set
type: Concept
created: 2020-10-14T11:23:04.814Z
notation: IS-651
definition: Faults in the Laki fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Laki Fault and Fissure Sets

Reykjanes Oblique Rift
type: Concept
created: 2020-10-14T11:23:03.290Z
notation: IS-1
definition: Offshore from Geirfuglasker near the tip of the Reykjanes Peninsula to Bláfjöll where it connects with the Western Volcanic Zone and the South-Iceland Seismic Zone
narrower: Reykjanes-Eldvörp-Svartsengi Fault and Fissure Sets
narrower: Krýsuvík Fault and Fissure Sets
narrower: Brennisteinsfjöll Fault and Fissure Sets
narrower: Reykjanes Earthquake Fault Set
narrower: Eldey Fault and Fissure Sets
narrower: Geirfuglasker Fault Set
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Iceland

Brennisteinsfjöll Fault and Fissure Sets
type: Concept
created: 2020-10-14T11:23:03.483Z
notation: IS-13
definition: Faults and fissures in the Brennisteinsfjöll fissure swarm
narrower: Brennisteinsfjöll Fault Set
narrower: Brennisteinsfjöll Fissure Set
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Reykjanes Oblique Rift

Brennisteinsfjöll Fault Set
type: Concept
created: 2020-10-14T11:23:03.511Z
notation: IS-131
definition: Faults in the Brennisteinsfjöll fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Brennisteinsfjöll Fault and Fissure Sets

Brennisteinsfjöll Fissure Set
type: Concept
created: 2020-10-14T11:23:03.539Z
notation: IS-132
definition: Fissures in the Brennisteinsfjöll fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Brennisteinsfjöll Fault and Fissure Sets

Krýsuvík Fault and Fissure Sets
type: Concept
created: 2020-10-14T11:23:03.400Z
notation: IS-12
definition: Faults and fissures in the Krýsuvík fissure swarm
narrower: Krýsuvík Fault Set
narrower: Krýsuvík Fissure Set
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Reykjanes Oblique Rift

Krýsuvík Fault Set
type: Concept
created: 2020-10-14T11:23:03.428Z
notation: IS-121
definition: Faults in the Krýsuvík fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Krýsuvík Fault and Fissure Sets

Krýsuvík Fissure Set
type: Concept
created: 2020-10-14T11:23:03.455Z
notation: IS-122
definition: Fissures in the Krýsuvík fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Krýsuvík Fault and Fissure Sets

Geirfuglasker Fault Set
type: Concept
created: 2020-10-14T11:23:03.708Z
notation: IS-161
definition: Faults in the Geirfuglasker fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4608
in scheme: Tectonic Boundary Objects in Europe
broader: Reykjanes Oblique Rift

Reykjanes-Eldvörp-Svartsengi Fault and Fissure Sets
type: Concept
created: 2020-10-14T11:23:03.317Z
notation: IS-11
definition: Faults and fissures in the Reykjanes-Eldvörp-Svartsengi fissure swarm
narrower: Reykjanes-Eldvörp-Svartsengi Fault Set
narrower: Reykjanes-Eldvörp-Svartsengi Fissure Set
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Reykjanes Oblique Rift

Reykjanes-Eldvörp-Svartsengi Fissure Set
type: Concept
created: 2020-10-14T11:23:03.372Z
notation: IS-112
definition: Fissures in the Reykjanes-Eldvörp-Svartsengi fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Reykjanes-Eldvörp-Svartsengi Fault and Fissure Sets

Reykjanes-Eldvörp-Svartsengi Fault Set
type: Concept
created: 2020-10-14T11:23:03.345Z
notation: IS-111
definition: Faults in the Reykjanes-Eldvörp-Svartsengi fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Reykjanes-Eldvörp-Svartsengi Fault and Fissure Sets

Eldey Fault and Fissure Sets
type: Concept
created: 2020-10-14T11:23:03.623Z
notation: IS-15
definition: Faults and fissures in the Eldey fissure swarm
narrower: Eldey Fault Set
narrower: Eldey Fissure Set
references: https://data.geoscience.earth/ncl/geoera/ref/4608
in scheme: Tectonic Boundary Objects in Europe
broader: Reykjanes Oblique Rift

Eldey Fissure Set
type: Concept
created: 2020-10-14T11:23:03.681Z
notation: IS-152
definition: Fissures in the Eldey fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4608
in scheme: Tectonic Boundary Objects in Europe
broader: Eldey Fault and Fissure Sets

Eldey Fault Set
type: Concept
created: 2020-10-14T11:23:03.653Z
notation: IS-151
definition: Faults in the Eldey fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4608
in scheme: Tectonic Boundary Objects in Europe
broader: Eldey Fault and Fissure Sets

Reykjanes Earthquake Fault Set
type: Concept
created: 2020-10-14T11:23:03.567Z
notation: IS-14
definition: Earthquake faults in the Reykjanes Earthquake Fault set
narrower: Reykjanes Strike-slip faults
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Reykjanes Oblique Rift

Reykjanes Strike-slip faults
type: Concept
created: 2020-10-14T11:23:03.594Z
notation: IS-141
definition: Strike-slip faults in the Reykjanes earthquake fault set
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Reykjanes Earthquake Fault Set

Northern Volcanic Zone
type: Concept
created: 2020-10-14T11:23:05.035Z
notation: IS-7
definition: From Vatnajökull to the north coast
narrower: Askja Fault and Fissure Sets
narrower: Kverkfjöll Fault and Fissure Sets
narrower: Hrúthálsar Fault and Fissure Sets
narrower: Fremri-Námar Fault and Fissure Sets
narrower: Krafla-Gjástykki Fault and Fissure Sets
narrower: Þeistareykir Fault and Fissure Sets
narrower: Blikalón Fault and Set
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Iceland

Fremri-Námar Fault and Fissure Sets
type: Concept
created: 2020-10-14T11:23:05.314Z
notation: IS-74
definition: Faults and fissures in the Fremri-Námar fissure swarm
narrower: Fremri-Námar Fault Set
narrower: Fremri-Námar Fissure Set
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Northern Volcanic Zone

Fremri-Námar Fault Set
type: Concept
created: 2020-10-14T11:23:05.343Z
notation: IS-741
definition: Faults in the Fremri-Námar fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Fremri-Námar Fault and Fissure Sets

Fremri-Námar Fissure Set
type: Concept
created: 2020-10-14T11:23:05.371Z
notation: IS-742
definition: Fissures in the Fremri-Námar fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Fremri-Námar Fault and Fissure Sets

Hrúthálsar Fault and Fissure Sets
type: Concept
created: 2020-10-14T11:23:05.230Z
notation: IS-73
definition: Faults and fissures in the Hrúthálsar fissure swarm
narrower: Hrúthálsar Fault Set
narrower: Hrúthálsar Fissure Set
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Northern Volcanic Zone

Hrúthálsar Fissure Set
type: Concept
created: 2020-10-14T11:23:05.286Z
notation: IS-732
definition: Fissures in the Hrúthálsar fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Hrúthálsar Fault and Fissure Sets

Hrúthálsar Fault Set
type: Concept
created: 2020-10-14T11:23:05.258Z
notation: IS-731
definition: Faults in the Hrúthálsar fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Hrúthálsar Fault and Fissure Sets

Blikalón Fault and Set
type: Concept
created: 2020-10-14T11:23:05.563Z
notation: IS-771
definition: Faults in the Blikalón fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Northern Volcanic Zone

Kverkfjöll Fault and Fissure Sets
type: Concept
created: 2020-10-14T11:23:05.147Z
notation: IS-72
definition: Faults and fissures in the Kverkfjöll fissure swarm
narrower: Kverkfjöll Fault Set
narrower: Kverkfjöll Fissure Set
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Northern Volcanic Zone

Kverkfjöll Fissure Set
type: Concept
created: 2020-10-14T11:23:05.202Z
notation: IS-722
definition: Fissures in the Kverkfjöll fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Kverkfjöll Fault and Fissure Sets

Kverkfjöll Fault Set
type: Concept
created: 2020-10-14T11:23:05.174Z
notation: IS-721
definition: Faults in the Kverkfjöll fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Kverkfjöll Fault and Fissure Sets

Þeistareykir Fault and Fissure Sets
type: Concept
created: 2020-10-14T11:23:05.481Z
notation: IS-76
definition: Faults and fissures in the Þeistareykir fissure swarm
narrower: Þeistareykir Fault Set
narrower: Þeistareykir Fissure Set
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Northern Volcanic Zone

Þeistareykir Fault Set
type: Concept
created: 2020-10-14T11:23:05.508Z
notation: IS-761
definition: Faults in the Þeistareykir fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Þeistareykir Fault and Fissure Sets

Þeistareykir Fissure Set
type: Concept
created: 2020-10-14T11:23:05.536Z
notation: IS-762
definition: Fissures in the Þeistareykir fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Þeistareykir Fault and Fissure Sets

Krafla-Gjástykki Fault and Fissure Sets
type: Concept
created: 2020-10-14T11:23:05.398Z
notation: IS-75
definition: Faults and fissures in the Krafla-Gjástykki fissure swarm
narrower: Krafla-Gjástykki Fault Set
narrower: Krafla-Gjástykki Fissure Set
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Northern Volcanic Zone

Krafla-Gjástykki Fissure Set
type: Concept
created: 2020-10-14T11:23:05.454Z
notation: IS-752
definition: Fissures in the Krafla-Gjástykki fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Krafla-Gjástykki Fault and Fissure Sets

Krafla-Gjástykki Fault Set
type: Concept
created: 2020-10-14T11:23:05.426Z
notation: IS-751
definition: Faults in the Krafla-Gjástykki fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Krafla-Gjástykki Fault and Fissure Sets

Askja Fault and Fissure Sets
type: Concept
created: 2020-10-14T11:23:05.063Z
notation: IS-71
definition: Faults and fissures in the Askja fissure swarm
narrower: Askja Fault Set
narrower: Askja Fissure Set
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Northern Volcanic Zone

Askja Fault Set
type: Concept
created: 2020-10-14T11:23:05.091Z
notation: IS-711
definition: Faults in the Askja fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Askja Fault and Fissure Sets

Askja Fissure Set
type: Concept
created: 2020-10-14T11:23:05.119Z
notation: IS-712
definition: Fissures in the Askja fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Askja Fault and Fissure Sets

Central Volcanic Zone
type: Concept
created: 2020-10-14T11:23:04.458Z
notation: IS-5
definition: Surrounding Hofsjökull glacier between Western and Eastern Volcanic Zone
narrower: Kerlingarfjöll Fault Set
narrower: Hofsjökull Fault Set
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Iceland

Kerlingarfjöll Fault Set
type: Concept
created: 2020-10-14T11:23:04.485Z
notation: IS-511
definition: Faults in the Kerlingarfjöll fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Central Volcanic Zone

Hofsjökull Fault Set
type: Concept
created: 2020-10-14T11:23:04.513Z
notation: IS-521
definition: Faults in the Hofsjökull fissure swarm
references: https://data.geoscience.earth/ncl/geoera/ref/4609
in scheme: Tectonic Boundary Objects in Europe
broader: Central Volcanic Zone

Tectonic Boundary in Italy
narrower: Pustertal-Gailtal Subfault System
narrower: Giudicarie-Brenner-Silltal Large-scale Fault System
notation: IT-0
scope note: All named tectonic boundary objects that are located (at least partly) in Italy, are identified by an ID with the prefix „IT“ listed in the notation. Fault systems and/or fault domains can cross political borders and are therefore shared by several countries. Therefore, they can contain faults from different countries, indicated by country-specific prefixes to the respective ID.
definition: Fault in Italy as they appear on the HIKE European fault database. They are sorted into fault systems or tectonic domains.
narrower: Po Plain-Adriatic foreland basin Domain
narrower: Adriatic plate passive continental margin Domain
type: Concept
top concept of: Tectonic Boundary Objects in Europe
created: 2020-10-16T07:56:52.268Z
narrower: Helvetic Domain
narrower: Penninic Domain
narrower: Austroalpine Domain
narrower: Insubric Fault System
narrower: Southalpine Domain
narrower: Sestri-Voltaggio Lineament
narrower: Ligurian Fault Domain
narrower: Northern Apennines Domain
narrower: Apennines extensional Domain
narrower: Ortona-Roccamonfina Lineament
narrower: Southern Apennines Domain
narrower: Bradanic Trough Domain
narrower: Apulia foreland Domain
narrower: Sicilian-Maghrebian Domain
narrower: Catania-Gela foredeep Domain
narrower: Hyblean foreland Domain
narrower: Sangineto Line
narrower: Taormina Line
narrower: Calabride-Peloritane Domain
narrower: Sardinia Variscan basement Domain
narrower: Sardinia Graben system Domain
narrower: Campidano Graben Domain
narrower: Etna volcano Domain
in scheme: Tectonic Boundary Objects in Europe

Ortona-Roccamonfina Lineament
references: https://data.geoscience.earth/ncl/geoera/ref/4799
references: https://data.geoscience.earth/ncl/geoera/ref/4792
type: Concept
created: 2020-10-16T07:56:54.290Z
notation: IT-99100
preferred label: Linea Ortona-Roccamonfina @it
definition: The Ortona-Roccamonfina (or Sangro-Volturno) lineament is considered the tectonic separation between the northern Apennines and and Southern Apennines (Patacca & Scandone, 2007 and references therein). The Ortona-Roccamonfina transversal structure can be interpreted as a crustal oblique thrust ramp, trending NNE-SSW, with right-lateral transpressive kinematic involving the Apulian carbonate platform and the slope-to-basin paleodomains. Thrusts and related folds of the Ortona-Roccamonfina oblique ramp also involve the basal thrust and the left-lateral oblique ramp of the Molise Allocthonous Units (Satolli et al., 2014).
definition: La Linea Ortona-Roccamonfina (o Sangro-Volturno) è considerata la separazione tra l'Appennino settentrionale e quello meridionale (Patacca & Scandone, 2007 e bibliografia inclusa). Questa struttura trasversale può essere interpretata come una rampa crostale obliqua, ad andamento NNE-SSO, con cinematica transpressiva destra, che coinvolge la piattaforma carbonatica Apula e i paleodomini di scarpata-bacino. Sovrascorrimenti e pieghe associate con questa rampa obliqua coinvolgono anche il sovrascorrimento basale e la rampa laterale obliqua sinistra delle Unità alloctone molisane (Satolli et al., 2014). @it
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Italy

Adriatic plate passive continental margin Domain
type: Concept
created: 2020-10-09T13:14:14.908Z
notation: IT-9914
preferred label: Dominio del margine continentale passivo della placca Adriatica @it
definition: The Adriatic plate passive continental margin domain is characterized by normal faults, mainly NNW-SSE and N-S oriented, steeply W- and E-dipping. Minor W-E and NE-SW faults are present. These faults are related to the rifting phase affecting the Adriatic/Africa plate margin during Late Triassic and from Early Jurassic to Early Cretaceous (Masetti et al, 2012).
definition: Il dominio del margine continentale passivo della placca Adriatica è caratterizzato da faglie normali, ad andamento prevalente SSE-NNO e N-S, molto inclinate verso E e O. Meno frequentemente sono presenti anche faglie ad andamento E-O e NE-SO. Queste faglie sono legate alla fase di rifting che ha interessato il margine della placca Adriatica nel Triassico superiore e dal Giurassico inferiore fino al Cretacico inferiore (Masetti et al, 2012). @it
narrower: Virgilio Fault
narrower: Asola Fault System
narrower: Bedizzole Fault System
narrower: Castiglione Fault System
narrower: Gaggiano Fault System
narrower: Gambara Fault System
narrower: Garlasco Fault System
narrower: Mantova Fault System
narrower: Nogara Fault System
narrower: Piadena Fault System
narrower: Rodigo Fault System
narrower: Suzzara Fault System
narrower: Viadana Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/4113
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Italy

Bedizzole Fault System
type: Concept
created: 2020-10-09T13:14:15.172Z
notation: IT-99141
preferred label: Sistema di faglie Bedizzole @it
definition: NE-SW trending fault system characterized by NW- and SE-dipping normal faults.
definition: Sistema di faglie normali ad andamento NE-SO con inclinazione verso NO e SE. @it
narrower: Bedizzole 3 Fault
narrower: Bedizzole 2 Fault
narrower: Bedizzole 1 Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Adriatic plate passive continental margin Domain

Bedizzole 3 Fault
type: Concept
created: 2020-10-09T13:14:15.201Z
notation: IT-4557
preferred label: Faglia Bedizzole 3 @it
definition: NNE-SSW trending normal fault with a steep ESE dip.
definition: Faglia normale ad andamento NNE-SSO molto inclinata verso ESE. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Bedizzole Fault System

Bedizzole 2 Fault
type: Concept
created: 2020-10-09T13:14:15.229Z
notation: IT-4559
preferred label: Faglia Bedizzole 2 @it
definition: NE-SW trending normal fault with a steep north-west dip.
definition: Faglia normale ad andamento NE-SO molto inclinata verso NO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Bedizzole Fault System

Bedizzole 1 Fault
type: Concept
created: 2020-10-09T13:14:15.257Z
notation: IT-4561
preferred label: Faglia Bedizzole 1 @it
definition: NE-SW trending normal fault with a steep north-west dip.
definition: Faglia normale ad andamento NE-SO molto inclinata verso NO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Bedizzole Fault System

Nogara Fault System
type: Concept
created: 2020-10-09T13:14:16.133Z
notation: IT-99147
preferred label: Sistema di faglie Nogara @it
definition: SE-NW trending fault system characterized by steeply SW- and NE-dipping normal faults.
definition: Sistema di faglie normali ad andamento da SE-NO con inclinazione verso SO e NE. @it
narrower: Nogara 9 Fault
narrower: Nogara 8 Fault
narrower: Nogara 6 antithetic Fault
narrower: Nogara 6 Fault
narrower: Nogara 5 Fault
narrower: Nogara 7 Fault
narrower: Nogara 1 antithetic Fault
narrower: Nogara Fault
narrower: Nogara 1 Fault
narrower: Nogara 2 antithetic Fault
narrower: Nogara 2 Fault
narrower: Nogara 3 antithetic Fault
narrower: Nogara 3 Fault
narrower: Nogara 4 antithetic Fault
narrower: Nogara 4 Fault
narrower: Nogara 5 antithetic Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4779
references: https://data.geoscience.earth/ncl/geoera/ref/4518
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Adriatic plate passive continental margin Domain

Nogara 2 antithetic Fault
type: Concept
created: 2020-10-09T13:14:16.410Z
notation: IT-4526
preferred label: Faglia Nogara 2 antitetica @it
definition: SE-NW trending normal fault steeply NE-dipping.
definition: Faglia normale ad andamento SE-NO molto inclinata verso NE. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Nogara Fault System

Nogara 2 Fault
type: Concept
created: 2020-10-09T13:14:16.438Z
notation: IT-4529
preferred label: Faglia Nogara 2 @it
definition: ESE-WNW trending normal fault steeply SSW-dipping.
definition: Faglia normale ad andamento ESE-ONO molto inclinata verso SSO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Nogara Fault System

Nogara 9 Fault
type: Concept
created: 2020-10-09T13:14:16.160Z
notation: IT-4468
preferred label: Faglia Nogara 9 @it
definition: SSE-NNW trending normal fault steeply WSW-dipping.
definition: Faglia normale ad andamento SSE-NNO molto inclinata verso OSO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Nogara Fault System

Nogara 3 antithetic Fault
type: SpatialObject
type: Concept
created: 2020-10-09T13:14:16.466Z
notation: IT-4533
preferred label: Faglia Nogara 3 antitetica @it
definition: SE-NW trending normal fault steeply NE-dipping.
definition: Faglia normale ad andamento SE-NO molto inclinata verso NE. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Nogara Fault System

Nogara 8 Fault
type: Concept
created: 2020-10-09T13:14:16.188Z
notation: IT-4471
preferred label: Faglia Nogara 8 @it
definition: SE-NW trending normal fault steeply SW-dipping.
definition: Faglia normale ad andamento SE-NO molto inclinata verso SO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Nogara Fault System

Nogara 3 Fault
type: Concept
created: 2020-10-09T13:14:16.494Z
notation: IT-4537
preferred label: Faglia Nogara 3 @it
definition: SE-NW trending normal fault steeply SW-dipping.
definition: Faglia normale ad andamento SE-NO molto inclinata verso SO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Nogara Fault System

Nogara 6 antithetic Fault
type: Concept
created: 2020-10-09T13:14:16.216Z
notation: IT-4474
preferred label: Faglia Nogara 6 antitetica @it
definition: ESE-WNW trending normal fault steeply NNE-dipping.
definition: Faglia normale ad andamento ESE-ONO molto inclinata verso NNE. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Nogara Fault System

Nogara 4 antithetic Fault
type: Concept
created: 2020-10-09T13:14:16.521Z
notation: IT-4540
preferred label: Faglia Nogara 4 antitetica @it
definition: SE-NW trending normal fault steeply NE-dipping.
definition: Faglia normale ad andamento SE-NO molto inclinata verso NE. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Nogara Fault System

Nogara 6 Fault
type: Concept
created: 2020-10-09T13:14:16.244Z
notation: IT-4486
preferred label: Faglia Nogara 6 @it
definition: SE-NW trending normal fault steeply SW-dipping.
definition: Faglia normale ad andamento SE-NO molto inclinata verso SO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Nogara Fault System

Nogara 4 Fault
type: Concept
created: 2020-10-09T13:14:16.549Z
notation: IT-4545
preferred label: Faglia Nogara 4 @it
definition: SE-NW trending normal fault steeply SW-dipping.
definition: Faglia normale ad andamento SE-NO molto inclinata verso SO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Nogara Fault System

Nogara 5 Fault
type: Concept
created: 2020-10-09T13:14:16.272Z
notation: IT-4490
preferred label: Faglia Nogara 5 @it
definition: SE-NW trending normal fault steeply SW-dipping.
definition: Faglia normale ad andamento SE-NO molto inclinata verso SO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Nogara Fault System

Nogara 5 antithetic Fault
type: Concept
created: 2020-10-09T13:14:16.577Z
notation: IT-4554
preferred label: Faglia Nogara 5 antitetica @it
definition: SE-NW trending normal fault steeply NE-dipping.
definition: Faglia normale ad andamento SE-NO molto inclinata verso NE. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Nogara Fault System

Nogara 7 Fault
type: Concept
created: 2020-10-09T13:14:16.299Z
notation: IT-4491
preferred label: Faglia Nogara 7 @it
definition: SE-NW trending vertical normal fault SW-dipping.
definition: Faglia normale subverticale ad andamento SE-NO inclinata verso SO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Nogara Fault System

Nogara 1 antithetic Fault
type: Concept
created: 2020-10-09T13:14:16.327Z
notation: IT-4513
preferred label: Faglia Nogara 1 antitetica @it
definition: SE-NW trending normal fault steeply NE-dipping.
definition: Faglia normale ad andamento SE-NO molto inclinata verso NE. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Nogara Fault System

Nogara Fault
type: Concept
created: 2020-10-09T13:14:16.355Z
notation: IT-4516
preferred label: Faglia Nogara @it
definition: SE-NW trending vertical normal fault SW-dipping.
definition: Faglia normale subverticale ad andamento SE-NO inclinata verso SO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Nogara Fault System

Nogara 1 Fault
type: Concept
created: 2020-10-09T13:14:16.383Z
notation: IT-4521
preferred label: Faglia Nogara 1 @it
definition: ESE-WNW trending normal fault steeply SSW-dipping.
definition: Faglia normale ad andamento ESE-ONO molto inclinata verso SSO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Nogara Fault System

Virgilio Fault
type: Concept
created: 2020-10-09T13:14:14.936Z
notation: IT-4470
preferred label: Faglia Virgilio @it
definition: N-S trending normal fault with steep west dip.
definition: Faglia normale ad andamento N-S molto inclinata verso ovest. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Adriatic plate passive continental margin Domain

Asola Fault System
type: Concept
created: 2020-10-09T13:14:14.967Z
notation: IT-99140
preferred label: Sistema di faglie Asola @it
definition: SSE-NNW trending fault system characterized by ENE- and WSW-dipping normal faults.
definition: Sistema di faglie normali ad andamento SSE-NNO con inclinazione verso ENE e OSO. @it
narrower: Asola 5 Fault
narrower: Asola 4 Fault
narrower: Asola 3 Fault
narrower: Asola 2 Fault
narrower: Asola 1 Fault
narrower: Asola 1 antithetic Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Adriatic plate passive continental margin Domain

Asola 5 Fault
type: Concept
created: 2020-10-09T13:14:14.995Z
notation: IT-4568
preferred label: Faglia Asola 5 @it
definition: SSE-NNW trending normal fault with a steep WSW dip.
definition: Faglia normale ad andamento SSE-NNO molto inclinata verso OSO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Asola Fault System

Asola 4 Fault
type: Concept
created: 2020-10-09T13:14:15.023Z
notation: IT-4570
preferred label: Faglia Asola 4 @it
definition: SSE-NNW trending normal fault with a steep WSW dip.
definition: Faglia normale ad andamento SSE-NNO molto inclinata verso OSO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Asola Fault System

Asola 3 Fault
type: Concept
created: 2020-10-09T13:14:15.052Z
notation: IT-4572
preferred label: Faglia Asola 3 @it
definition: SE-NW trending normal fault with a steep SW dip.
definition: Faglia normale ad andamento SE-NO molto inclinata verso SO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Asola Fault System

Asola 2 Fault
type: Concept
created: 2020-10-09T13:14:15.081Z
notation: IT-4573
preferred label: Faglia Asola 2 @it
definition: SE-NW trending normal fault with a steep SW dip.
definition: Faglia normale ad andamento SE-NO molto inclinata verso SO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Asola Fault System

Asola 1 Fault
type: Concept
created: 2020-10-09T13:14:15.109Z
notation: IT-4575
preferred label: Faglia Asola 1 @it
definition: SSE-NNW trending normal fault with a steep WSW dip.
definition: Faglia normale ad andamento SSE-NNO molto inclinata verso OSO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Asola Fault System

Asola 1 antithetic Fault
type: Concept
created: 2020-10-09T13:14:15.140Z
notation: IT-4566
preferred label: Faglia Asola 1 antitetica @it
definition: SSE-NNW trending normal fault with a steep ENE dip.
definition: Faglia normale ad andamento SSE-NNO molto inclinata verso ENE. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Asola Fault System

Castiglione Fault System
type: Concept
created: 2020-10-09T13:14:15.286Z
notation: IT-99142
preferred label: Sistema di faglie Castiglione @it
definition: ESE-WNW trending fault system characterized by SSW-dipping normal faults.
definition: Sistema di faglie normali ad andamento ESE-ONO con inclinazione verso SSO. @it
narrower: Castiglione Fault
narrower: Castiglione 3 Fault
narrower: Castiglione 2 Fault
narrower: Castiglione 1 Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Adriatic plate passive continental margin Domain

Castiglione Fault
type: Concept
created: 2020-10-09T13:14:15.314Z
notation: IT-4530
preferred label: Faglia Castiglione @it
definition: ESE-WNW trending normal fault with a steep SSW dip.
definition: Faglia normale ad andamento ESE-ONO molto inclinata verso SSO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Castiglione Fault System

Castiglione 3 Fault
type: Concept
created: 2020-10-09T13:14:15.343Z
notation: IT-4534
preferred label: Faglia Castiglione 3 @it
definition: ESE-WNW trending normal fault with a steep SSW dip.
definition: Faglia normale ad andamento ESE-ONO molto inclinata verso SSO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Castiglione Fault System

Castiglione 2 Fault
type: Concept
created: 2020-10-09T13:14:15.373Z
notation: IT-4536
preferred label: Faglia Castiglione 2 @it
definition: SE-NW trending normal fault with a steep SW dip.
definition: Faglia normale ad andamento SE-NO molto inclinata verso SO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Castiglione Fault System

Castiglione 1 Fault
type: Concept
created: 2020-10-09T13:14:15.401Z
notation: IT-4539
preferred label: Faglia Castiglione 1 @it
definition: SE-NW trending normal fault with a steep SW dip.
definition: Faglia normale ad andamento SE-NO molto inclinata verso SO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Castiglione Fault System

Gambara Fault System
type: Concept
created: 2020-10-09T13:14:15.598Z
notation: IT-99144
preferred label: Sistema di faglie Gambara @it
definition: N-S to NNE-SSW trending fault system characterized by W-and E-dipping normal faults.
definition: Sistema di faglie normali ad andamento da N-S a NNE-SSO con inclinazione verso ovest e verso est. @it
narrower: Gambara 8 Fault
narrower: Gambara 11 Fault
narrower: Gambara 10 Fault
narrower: Gambara 9 Fault
narrower: Gambara 4 Fault
narrower: Gambara 3 Fault
narrower: Gambara 1 Fault
narrower: Gambara 2 Fault
narrower: Gambara 5 Fault
narrower: Gambara 6 Fault
narrower: Gambara 7 Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Adriatic plate passive continental margin Domain

Gambara 1 Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: Concept
created: 2020-10-09T13:14:15.799Z
notation: IT-4515
preferred label: Faglia Gambara 1 @it
definition: N-S trending normal fault with steep west dip.
definition: Faglia normale ad andamento N-S molto inclinata verso ovest. @it
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Gambara Fault System

Gambara 2 Fault
type: Concept
created: 2020-10-09T13:14:15.828Z
notation: IT-4517
preferred label: Faglia Gambara 2 @it
definition: SSE-NNW trending nornal fault with a steep WSW dip.
definition: Faglia normale ad andamento SSE-NNO molto inclinata verso OSO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Gambara Fault System

Gambara 5 Fault
type: Concept
created: 2020-10-09T13:14:15.855Z
notation: IT-4589
preferred label: Faglia Gambara 5 @it
definition: N-S trending normal fault with steep west dip.
definition: Faglia normale ad andamento N-S molto inclinata verso ovest. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Gambara Fault System

Gambara 6 Fault
type: Concept
created: 2020-10-09T13:14:15.883Z
notation: IT-4594
preferred label: Faglia Gambara 6 @it
definition: N-S trending normal fault with steep west dip.
definition: Faglia normale ad andamento N-S molto inclinata verso ovest. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Gambara Fault System

Gambara 7 Fault
type: Concept
created: 2020-10-09T13:14:15.911Z
notation: IT-4600
preferred label: Faglia Gambara 7 @it
definition: NNE-SSW trending normal fault with a steep WNW dip.
definition: Faglia normale ad andamento NNE-SSO molto inclinata verso ONO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Gambara Fault System

Gambara 8 Fault
type: Concept
created: 2020-10-09T13:14:15.626Z
notation: IT-4438
preferred label: Faglia Gambara 8 @it
definition: N-S trending normal fault with steep west dip.
definition: Faglia normale ad andamento N-S molto inclinata verso ovest. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Gambara Fault System

Gambara 11 Fault
type: Concept
created: 2020-10-09T13:14:15.654Z
notation: IT-4499
preferred label: Faglia Gambara 11 @it
definition: ENE-WSW trending normal fault with a steep SSE dip.
definition: Faglia normale ad andamento ENE-OSO molto inclinata verso SSE. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Gambara Fault System

Gambara 10 Fault
type: Concept
created: 2020-10-09T13:14:15.683Z
notation: IT-4502
preferred label: Faglia Gambara 10 @it
definition: NNE-SSW trending normal fault with a steep WNW dip.
definition: Faglia normale ad andamento NNE-SSO molto inclinata verso ONO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Gambara Fault System

Gambara 9 Fault
type: Concept
created: 2020-10-09T13:14:15.714Z
notation: IT-4506
preferred label: Faglia Gambara 9 @it
definition: NNE-SSW trending normal fault with a steep WNW dip.
definition: Faglia normale ad andamento NNE-SSO molto inclinata verso ONO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Gambara Fault System

Gambara 4 Fault
type: Concept
created: 2020-10-09T13:14:15.743Z
notation: IT-4509
preferred label: Faglia Gambara 4 @it
definition: N-S trending normal fault with steep west dip.
definition: Faglia normale ad andamento N-S molto inclinata verso ovest. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Gambara Fault System

Gambara 3 Fault
type: Concept
created: 2020-10-09T13:14:15.770Z
notation: IT-4512
preferred label: Faglia Gambara 3 @it
definition: NNE-SSW trending normal fault with a steep WNW dip.
definition: Faglia normale ad andamento NNE-SSO molto inclinata verso ONO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Gambara Fault System

Viadana Fault System
type: Concept
created: 2020-10-09T13:14:17.163Z
notation: IT-991411
preferred label: Sistema di faglie Viadana @it
definition: SE-NW trending fault system characterized by normal faults steeply SW-dipping.
definition: Sistema di faglie normali ad andamento da SE-NO con inclinazione verso SO. @it
narrower: Viadana 6 Fault
narrower: Viadana 4 Fault
narrower: Viadana Fault
narrower: Viadana 1 Fault
narrower: Viadana 2 Fault
narrower: Viadana 3 Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4779
references: https://data.geoscience.earth/ncl/geoera/ref/4518
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Adriatic plate passive continental margin Domain

Viadana 3 Fault
type: Concept
created: 2020-10-09T13:14:17.334Z
notation: IT-4578
preferred label: Faglia Viadana 3 @it
definition: SE-NW trending normal fault with a steep SW dip.
definition: Faglia normale ad andamento SE-NO molto inclinata verso SO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Viadana Fault System

Viadana 6 Fault
type: Concept
created: 2020-10-09T13:14:17.192Z
notation: IT-4465
preferred label: Faglia Viadana 6 @it
definition: ESE-WNW trending normal fault with a steep SSW dip.
definition: Faglia normale ad andamento ESE-ONO molto inclinata verso SSO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Viadana Fault System

Viadana 4 Fault
type: Concept
created: 2020-10-09T13:14:17.220Z
notation: IT-4469
preferred label: Faglia Viadana 4 @it
definition: ESE-WNW trending normal fault with a steep SSW dip.
definition: Faglia normale ad andamento ESE-ONO molto inclinata verso SSO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Viadana Fault System

Viadana Fault
type: Concept
created: 2020-10-09T13:14:17.248Z
notation: IT-4473
preferred label: Faglia Viadana @it
definition: SE-NW trending normal fault with a steep SW dip.
definition: Faglia normale ad andamento SE-NO molto inclinata verso SO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Viadana Fault System

Viadana 1 Fault
type: Concept
created: 2020-10-09T13:14:17.276Z
notation: IT-4576
preferred label: Faglia Viadana 1 @it
definition: SE-NW trending normal fault with a steep SW dip.
definition: Faglia normale ad andamento SE-NO molto inclinata verso SO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Viadana Fault System

Viadana 2 Fault
type: Concept
created: 2020-10-09T13:14:17.305Z
notation: IT-4577
preferred label: Faglia Viadana 2 @it
definition: SE-NW trending normal fault with a steep SW dip.
definition: Faglia normale ad andamento SE-NO molto inclinata verso SO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Viadana Fault System

Rodigo Fault System
type: Concept
created: 2020-10-09T13:14:16.799Z
notation: IT-99149
preferred label: Sistema di faglie Rodigo @it
definition: SSE-NNW trending fault system characterized by steeply WSW- and ENE-dipping normal faults.
definition: Sistema di faglie normali ad andamento da SSE-NNO con inclinazione verso OSO e ENE. @it
narrower: Rodigo 2 Fault
narrower: Rodigo 1 Fault
narrower: Rodigo Fault
narrower: Rodigo 1 antithetic Fault
narrower: Rodigo 3 Fault
narrower: Rodigo 4 Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Adriatic plate passive continental margin Domain

Rodigo 2 Fault
type: Concept
created: 2020-10-09T13:14:16.827Z
notation: IT-4476
preferred label: Faglia Rodigo 2 @it
definition: SE-NW trending normal fault with a steep south-west dip.
definition: Faglia normale ad andamento SE-NO molto inclinata verso SO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Rodigo Fault System

Rodigo 1 Fault
type: Concept
created: 2020-10-09T13:14:16.855Z
notation: IT-4478
preferred label: Faglia Rodigo 1 @it
definition: N-S trending normal fault with a steep west dip.
definition: Faglia normale ad andamento N-S molto inclinata verso O. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Rodigo Fault System

Rodigo Fault
type: Concept
created: 2020-10-09T13:14:16.884Z
notation: IT-4481
preferred label: Faglia Rodigo @it
definition: SSE-NNW trending normal fault with a steep WSW dip.
definition: Faglia normale ad andamento SSE-NNO molto inclinata verso OSO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Rodigo Fault System

Rodigo 1 antithetic Fault
type: Concept
created: 2020-10-09T13:14:16.912Z
notation: IT-4484
preferred label: Faglia Rodigo 1 antitetica @it
definition: SSE-NNW trending normal fault with a steep ENE dip.
definition: Faglia normale ad andamento SSE-NNO molto inclinata verso ENE. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Rodigo Fault System

Rodigo 3 Fault
type: Concept
created: 2020-10-09T13:14:16.940Z
notation: IT-4485
preferred label: Faglia Rodigo 3 @it
definition: SSE-NNW trending normal fault with a steep WSW dip.
definition: Faglia normale ad andamento SSE-NNO molto inclinata verso OSO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Rodigo Fault System

Rodigo 4 Fault
type: Concept
created: 2020-10-09T13:14:16.968Z
notation: IT-4503
preferred label: Faglia Rodigo 4 @it
definition: SSE-NNW trending vertical normal fault with a WSW dip.
definition: Faglia normale subverticale ad andamento SSE-NNO inclinata verso OSO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Rodigo Fault System

Garlasco Fault System
type: Concept
created: 2020-10-09T13:14:15.939Z
notation: IT-99145
preferred label: Sistema di faglie Garlasco @it
definition: N-S trending fault system characterized by E-dipping normal faults.
definition: Sistema di faglie normali ad andamento da N-S con inclinazione verso est. @it
narrower: Garlasco 1 Fault
narrower: Garlasco 2 Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Adriatic plate passive continental margin Domain

Garlasco 1 Fault
type: Concept
created: 2020-10-09T13:14:15.967Z
notation: IT-4563
preferred label: Faglia Garlasco 1 @it
definition: N-S trending normal fault with an intermediate east dip.
definition: Faglia normale ad andamento N-S molto inclinata verso est. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Garlasco Fault System

Garlasco 2 Fault
type: Concept
created: 2020-10-09T13:14:15.994Z
notation: IT-4582
preferred label: Faglia Garlasco 2 @it
definition: SSE-NNW trending normal fault with an intermediate east dip.
definition: Faglia normale ad andamento SSE-NNO molto inclinata verso est. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Garlasco Fault System

Piadena Fault System
type: Concept
created: 2020-10-09T13:14:16.605Z
notation: IT-99148
preferred label: Sistema di faglie Piadena @it
definition: SE-NW trending fault system characterized by steeply SW- and NE-dipping normal faults.
definition: Sistema di faglie normali ad andamento da SE-NO con inclinazione verso SO e NE. @it
narrower: Piadena Fault
narrower: Piadena 1 antithetic Fault
narrower: Piadena 4 Fault
narrower: Piadena 1 Fault
narrower: Piadena 2 Fault
narrower: Piadena 3 Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Adriatic plate passive continental margin Domain

Piadena 1 Fault
type: Concept
created: 2020-10-09T13:14:16.716Z
notation: IT-4565
preferred label: Faglia Piadena 1 @it
definition: SE-NW trending normal fault with a steep SW dip.
definition: Faglia normale ad andamento SE-NO molto inclinata verso SO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Piadena Fault System

Piadena 2 Fault
type: Concept
created: 2020-10-09T13:14:16.744Z
notation: IT-4567
preferred label: Faglia Piadena 2 @it
definition: SE-NW trending normal fault with a steep SW dip.
definition: Faglia normale ad andamento SE-NO molto inclinata verso SO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Piadena Fault System

Piadena 3 Fault
type: Concept
created: 2020-10-09T13:14:16.771Z
notation: IT-4569
preferred label: Faglia Piadena 3 @it
definition: SE-NW trending normal fault with a steep SW dip.
definition: Faglia normale ad andamento SE-NO molto inclinata verso SO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Piadena Fault System

Piadena Fault
type: Concept
created: 2020-10-09T13:14:16.633Z
notation: IT-4439
preferred label: Faglia Piadena @it
definition: SE-NW trending normal fault with a steep SW dip.
definition: Faglia normale ad andamento SE-NO molto inclinata verso SO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Piadena Fault System

Piadena 1 antithetic Fault
type: Concept
created: 2020-10-09T13:14:16.660Z
notation: IT-4456
preferred label: Faglia Piadena 1 antitetica @it
definition: SE-NW trending normal fault with a steep NE dip.
definition: Faglia normale ad andamento SE-NO molto inclinata verso NE. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Piadena Fault System

Piadena 4 Fault
type: Concept
created: 2020-10-09T13:14:16.688Z
notation: IT-4560
preferred label: Faglia Piadena 4 @it
definition: SSE-NNW trending vertical normal fault with a WSW dip.
definition: Faglia normale subverticale ad andamento SSE-NNO inclinata verso OSO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Piadena Fault System

Mantova Fault System
type: Concept
created: 2020-10-09T13:14:16.022Z
notation: IT-99146
preferred label: Sistema di faglie Mantova @it
definition: NE-SW trending fault system characterized by SE-dipping normal faults.
definition: Sistema di faglie normali ad andamento da NE-SO con inclinazione verso SE. @it
narrower: Mantova 1 Fault
narrower: Mantova 2 Fault
narrower: Mantova Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4779
references: https://data.geoscience.earth/ncl/geoera/ref/4518
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Adriatic plate passive continental margin Domain

Mantova Fault
type: Concept
created: 2020-10-09T13:14:16.105Z
notation: IT-4510
preferred label: Faglia Mantova @it
definition: NE-SW trending vertical normal fault with a south-east dip.
definition: Faglia normale subverticale ad andamento NE-SO inclinata verso SE. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Mantova Fault System

Mantova 1 Fault
type: Concept
created: 2020-10-09T13:14:16.050Z
notation: IT-4497
preferred label: Faglia Mantova 1 @it
definition: ENE-WSW trending normal fault with a steep south dip.
definition: Faglia normale ad andamento ENE-OSO molto inclinata verso sud. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Mantova Fault System

Mantova 2 Fault
type: Concept
created: 2020-10-09T13:14:16.077Z
notation: IT-4505
preferred label: Faglia Mantova 2 @it
definition: ENE-WSW trending normal fault with a steep SSE dip.
definition: Faglia normale ad andamento ENE-OSO molto inclinata verso SSE. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Mantova Fault System

Gaggiano Fault System
type: Concept
created: 2020-10-09T13:14:15.429Z
notation: IT-99143
preferred label: Sistema di faglie Gaggiano @it
definition: N-S trending fault system characterized by W-and E-dipping normal faults.
definition: Sistema di faglie normali ad andamento N-S con inclinazione verso ovest e verso est. @it
narrower: Gaggiano 5 Fault
narrower: Gaggiano 2 Fault
narrower: Gaggiano 1 Fault
narrower: Gaggiano 3 Fault
narrower: Gaggiano 4 Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Adriatic plate passive continental margin Domain

Gaggiano 2 Fault
type: Concept
created: 2020-10-09T13:14:15.485Z
notation: IT-4520
preferred label: Faglia Gaggiano 2 @it
definition: N-S trending normal faults with an intermediate east dip.
definition: Faglia normale ad andamento N-S mediamente inclinata verso est. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Gaggiano Fault System

Gaggiano 1 Fault
type: Concept
created: 2020-10-09T13:14:15.513Z
notation: IT-4523
preferred label: Faglia Gaggiano 1 @it
definition: N-S trending normal faults with an intermediate east dip.
definition: Faglia normale ad andamento N-S mediamente inclinata verso est. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Gaggiano Fault System

Gaggiano 3 Fault
type: Concept
created: 2020-10-09T13:14:15.541Z
notation: IT-4528
preferred label: Faglia Gaggiano 3 @it
definition: N-S trending normal faults with an intermediate east dip.
definition: Faglia normale ad andamento N-S mediamente inclinata verso est. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Gaggiano Fault System

Gaggiano 4 Fault
type: Concept
created: 2020-10-09T13:14:15.570Z
notation: IT-4562
preferred label: Faglia Gaggiano 4 @it
definition: N-S trending nvertical ormal faults with a west dip.
definition: Faglia normale subverticale ad andamento N-S inclinata verso ovest. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Gaggiano Fault System

Gaggiano 5 Fault
type: Concept
created: 2020-10-09T13:14:15.457Z
notation: IT-4477
preferred label: Faglia Gaggiano 5 @it
definition: NNE-SSE trending normal fault with an interemediate ESE dip.
definition: Faglia normale ad andamento SSE-NNO mediamente inclinata verso ESE. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Gaggiano Fault System

Suzzara Fault System
type: Concept
created: 2020-10-09T13:14:16.996Z
notation: IT-991410
preferred label: Sistema di faglie Suzzara @it
definition: SSE-NNW trending fault system characterized by steeply WSW- and ENE-dipping normal faults.
definition: Sistema di faglie normali ad andamento da SSE-NNO con inclinazione verso OSO e ENE. @it
narrower: Suzzara 2 antithetic Fault
narrower: Suzzara Fault
narrower: Suzzara 1 antithetic Fault
narrower: Suzzara 2 Fault
narrower: Suzzara 1 Fault
references: https://data.geoscience.earth/ncl/geoera/ref/4779
references: https://data.geoscience.earth/ncl/geoera/ref/4518
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Adriatic plate passive continental margin Domain

Suzzara 2 antithetic Fault
type: Concept
created: 2020-10-09T13:14:17.024Z
notation: IT-4457
preferred label: Faglia Suzzara 2 antitetica @it
definition: SSE-NNW trending normal fault with a steep WSW dip.
definition: Faglia normale ad andamento SSE-NNO molto inclinata verso OSO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Suzzara Fault System

Suzzara Fault
type: Concept
created: 2020-10-09T13:14:17.051Z
notation: IT-4460
preferred label: Faglia Suzzara @it
definition: SSE-NNW trending normal fault with a steep ENE dip.
definition: Faglia normale ad andamento SSE-NNO molto inclinata verso ENE. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Suzzara Fault System

Suzzara 1 antithetic Fault
type: Concept
created: 2020-10-09T13:14:17.079Z
notation: IT-4463
preferred label: Faglia Suzzara 1 antitetica @it
definition: SSE-NNW trending normal fault with a steep WSW dip.
definition: Faglia normale ad andamento SSE-NNO molto inclinata verso OSO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Suzzara Fault System

Suzzara 2 Fault
type: Concept
created: 2020-10-09T13:14:17.107Z
notation: IT-4494
preferred label: Faglia Suzzara 2 @it
definition: N-S trending normal fault with a steep east dip.
definition: Faglia normale ad andamento N-S molto inclinata verso est. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Suzzara Fault System

Suzzara 1 Fault
type: Concept
created: 2020-10-09T13:14:17.135Z
notation: IT-4496
preferred label: Faglia Suzzara 1 @it
definition: N-S trending normal fault with a steep east dip.
definition: Faglia normale ad andamento N-S molto inclinata verso est. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Suzzara Fault System

Po Plain-Adriatic foreland basin Domain
references: https://data.geoscience.earth/ncl/geoera/ref/4127
definition: Il Dominio del bacino di avampaese Padano-Adriatico è caratterizzato da sovrascorrimenti sepolti e/o ciechi evidenziati unicamente da indagini sismiche e perforazioni profonde. Esso ha rappresentato il bacino di avampaese sia per la catena Alpina (retrovergente) che per quella Appenninica Settentrionale; per questo motivo i sovrascorrimenti hanno immersioni e vergenze opposte: immersione verso N e vergenza a S, per la catena Alpina (Sudalpino), e immersione da S a SO e vergenza da N a NE, per la catena Appenninica. La loro attività è compresa tra il Cattiano e il presente. I principali sovrascorrimenti sono caratterizzati da una forma arcuata con un andamento, spostandosi da ovest a est/sud-est: principalmente O-E (Alpi Occidentali e Sudalpino, Fronte del Monferrato e Arco Emiliano), NO-SE (Arco Ferrara-Romagna) e NNO-SSE i sovrascorrimenti adriatici. Sono anche riconosciuti alcuni sovrasocrrimenti minori e isolati NE-vergenti. @it
definition: The Po Plain-Adriatic foreland basin domain is characterized by buried and/or blind thrusts solely evidenced by seismic surveys and deep drillings. It represented the common foreland basin of both Alps (retroforeland) and Northern Apennines fold-and-thrust belts; for this reason the thrusts are N-dipping S-vergent and S- to SW-dipping N- to NE-vergent, respectively those of the retrobelt of the Alps (Southern Alps) and of the Apennines front. Their activity ranges from Chattian to present. The main thrust fronts are characterized by an arcuated shape with the following trend, moving from west to east and south-east: mainly E-W (Western and Southern Alps, Monferrato Front and Emilia arc), SE-NW (Ferrara-Romagna arc) and SSE-NNW the adriatic thrusts. Some minor isolated thrust NE-vergent are also recognized.
type: Concept
created: 2020-10-09T13:14:12.453Z
notation: IT-9913
preferred label: Dominio del bacino di avampaese padano-adriatico @it
narrower: Lacchiarella Fault System
narrower: Western Alps Back-thrusts subdomain
narrower: Lombardia Arc subdomain
narrower: Monferrato Front subdomain
narrower: Emilia Arc subdomain
narrower: Ferrara - Romagna arc subdomain
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Italy

Lombardia Arc subdomain
type: Concept
created: 2020-10-09T13:14:12.732Z
notation: IT-99132
preferred label: Arco Lombardo @it
definition: The Lombardia Arc subdomain is characterized by thrusts connected to the south-verging retrobelt of the Alps (i.e. Southern Alps). The thrusts and back-thrusts have a mainly E-W trend. Two different décollement levels characterize these thrusts: the deeper in correspondence of Triassic evaporites (L1), the shallower in correspondence of the Eocene-Oligocene marly units (L2). The southward propagation of these structures occurred during Late Cretaceous, with major shortening occurring during Oligocene and Miocene.
definition: Il sottodominio dell'Arco Lombardo è caratterizzato da sovrascorrimenti legati alla catena Alpina sud-vergente (Sudalpino). I sovrascorrimenti e i retroscorrimenti hanno prevalentemente direzione E-O. I sovrascorrimenti sono caratterizzati da due diversi livelli di scollamento: il più profondo in corrispondenza delle evaporiti triassiche (L1), il più superficiale in corrispondenza delle unità marnose di età variabile tra l'Eocene e l'Oligocene (L2). La migrazione verso sud delle strutture è avvenuta durante il Cretacico superiore, con i maggiori raccorciamenti durante l'Oligocene e il Miocene. @it
narrower: San Gervasio Thrust Splay
narrower: Crema 1 Trust
narrower: Crema Thrust
narrower: Solferino Thrust
narrower: San Gervasio Thrust
narrower: Malpaga Thrust
narrower: Borgosatollo Thrust
narrower: Maclodio 1 Thrust
narrower: Maclodio 2 Thrust
narrower: Brescia Thrust splay
narrower: San Gervasio back-thrust
narrower: Ponterosso Thrust
narrower: Manerbio Thrust
narrower: Brescia Thrust
narrower: Ghedi Thrust
narrower: Castenedolo Thrust
narrower: Capriano del Colle Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4127
references: https://data.geoscience.earth/ncl/geoera/ref/4087
type: SpatialObject
narrower: Bagnolo Mella Thrust
narrower: Verolanuova Thrust
narrower: San Bartolomeo Thrust
narrower: Crema 2 Thrust
narrower: Crema 3 Thrust
narrower: Sirmione Thrust
narrower: Campazzo Thrust
narrower: Soncino Thrust
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Po Plain-Adriatic foreland basin Domain

Malpaga Thrust
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: Concept
created: 2020-10-16T07:56:54.598Z
notation: IT-4427
preferred label: Sovrascorrimento Malpaga @it
definition: E-W trending thrust fault with an intermediate north dip. The décollement level is L1.
definition: Sovrascorrimento ad andamento E-O mediamente inclinato verso nord. Il livello di scollamento è L1. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lombardia Arc subdomain

San Gervasio Thrust Splay
type: Concept
created: 2020-10-09T13:14:12.761Z
notation: IT-4441
preferred label: Sovrascorrimento secondario San Gervasio @it
definition: E-W trending thrust fault with a gentle north dip. The décollement level is L2.
definition: Sovrascorrimento ad andamento E-O debolmente inclinato verso nord. Il livello di scollamento è L2. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lombardia Arc subdomain

Crema 1 Trust
type: Concept
created: 2020-10-09T13:14:12.789Z
notation: IT-4555
preferred label: Sovrascorrimento Crema 1 @it
definition: E-W to N-S trending thrust fault, gentle dipping toward NE. The décollement level is L2.
definition: Sovrascorrimento ad andamento da E-O a N-S debolmente inclinato verso NE. Il livello di scollamento è L2. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lombardia Arc subdomain

Crema 3 Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:55.104Z
notation: IT-4606
preferred label: Sovrascorrimento Crema 3 @it
definition: SSE-NNW trending thrust fault with a gentle ENE dip. The décollement level is L2.
definition: Sovrascorrimento ad andamento SSE-NNO debolmente inclinato verso ENE. Il livello di scollamento è L2. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lombardia Arc subdomain

Soncino Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:55.131Z
notation: IT-4607
preferred label: Sovrascorrimento Soncino @it
definition: ESE-WNW trending fault with a gentle NNE dip. The décollement level is L1.
definition: Sovrascorrimento ad andamento ESE-ONO debolmente inclinato verso NNE. Il livello di scollamento è L1. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lombardia Arc subdomain

San Gervasio back-thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:54.739Z
notation: IT-4445
preferred label: Retroscorrimento San Gervasio @it
definition: E-W trending thrust fault with an intermediate south dip. It is a back-thrust associated with the San Gervasio thrust.The décollement level is L2.
definition: Sovrascorrimento ad andamento E-O mediamente inclinato verso sud. È un retroscorrimento associato al Sovrascorrimento San Gervasio. Il livello di scollamento è L2. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lombardia Arc subdomain

Ponterosso Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:54.766Z
notation: IT-4447
preferred label: Sovrascorrimento Ponterosso @it
definition: ENE-WSW trending thrust fault with a gentle NNW dip. The décollement level is L2.
definition: Sovrascorrimento ad andamento ENE-OSO debolmente inclinato verso NNO. Il livello di scollamento è L2. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lombardia Arc subdomain

Sirmione Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:55.076Z
notation: IT-4581
preferred label: Sovrascorrimento Sirmione @it
definition: E-W trending thrust fault with an intermediate north dip. The décollement level is L1.
definition: Sovrascorrimento ad andamento E-O mediamente inclinato verso nord. Il livello di scollamento è L1. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lombardia Arc subdomain

Maclodio 2 Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:54.682Z
notation: IT-4431
preferred label: Sovrascorrimento Maclodio 2 @it
definition: ESE-WNW trending thrust fault with an intermediate NNE dip. The décollement level is L2.
definition: Sovrascorrimento ad andamento ESE-ONO mediamente inclinato verso NNE. Il livello di scollamento è L2. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lombardia Arc subdomain

Brescia Thrust splay
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:54.711Z
notation: IT-4433
preferred label: Sovrascorrimento secondario Brescia @it
definition: ESE-WNW trending thrust fault with an intermediate NNE dip. The décollement level is L1.
definition: Sovrascorrimento ad andamento ESE-ONO mediamente inclinato verso NNE. Il livello di scollamento è L1. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lombardia Arc subdomain

Borgosatollo Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:54.626Z
notation: IT-4428
preferred label: Sovrascorrimento Borgosatollo @it
definition: ENE-WSW trending thrust fault with an intermediate NNW dip. The décollement level is L2.
definition: Sovrascorrimento ad andamento ENE-OSO mediamente inclinato verso NNO. Il livello di scollamento è L2. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lombardia Arc subdomain

Maclodio 1 Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:54.654Z
notation: IT-4429
preferred label: Sovrascorrimento Maclodio 1 @it
definition: E-W trending thrust fault with an intermediate north dip. The décollement level is L2.
definition: Sovrascorrimento ad andamento E-O mediamente inclinato verso nord. Il livello di scollamento è L2. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lombardia Arc subdomain

Crema Thrust
type: Concept
created: 2020-10-09T13:14:12.817Z
notation: IT-4599
preferred label: Sovrascorrimento Crema @it
definition: E-W trending thrust fault with an intermediate north dip. The décollement level is L2.
definition: Sovrascorrimento ad andamento E-O mediamente inclinato verso nord. Il livello di scollamento è L2. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lombardia Arc subdomain

Solferino Thrust
type: Concept
created: 2020-10-09T13:14:12.844Z
notation: IT-4564
preferred label: Sovrascorrimento Solferino @it
definition: E-W trending thrust fault with a intermediate north dip. The décollement level is L1.
definition: Sovrascorrimento ad andamento E-O mediamente inclinato verso nord. Il livello di scollamento è L1. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lombardia Arc subdomain

San Gervasio Thrust
type: Concept
created: 2020-10-09T13:14:12.872Z
notation: IT-4443
preferred label: Sovrascorrimento San Gervasio @it
definition: E-W to N-S trending thrust fault gentle NNW dipping. The décollement level is L2.
definition: Sovrascorrimento ad andamento da E-O a N-S debolmente inclinato verso NNO. Il livello di scollamento è L2. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lombardia Arc subdomain

San Bartolomeo Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:55.021Z
notation: IT-4541
preferred label: Sovrascorrimento San Bartolomeo @it
definition: E-W trending thrust fault with a gentle north dip. The décollement level is L1.
definition: Sovrascorrimento ad andamento E-O debolmente inclinato verso nord. Il livello di scollamento è L1. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lombardia Arc subdomain

Crema 2 Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:55.048Z
notation: IT-4546
preferred label: Sovrascorrimento Crema 2 @it
definition: E-W trending thrust fault with an intermediate north dip. The décollement level is L2.
definition: Sovrascorrimento ad andamento E-O mediamente inclinato verso nord. Il livello di scollamento è L2. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lombardia Arc subdomain

Campazzo Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:54.965Z
notation: IT-4464
preferred label: Sovrascorrimento Campazzo @it
definition: ENE-WSW trending thrust fault with a gentle NNW dip. The décollement level is L2.
definition: Sovrascorrimento ad andamento ENE-OSO debolmente inclinato verso NNO. Il livello di scollamento è L2. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lombardia Arc subdomain

Verolanuova Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:54.993Z
notation: IT-4467
preferred label: Sovrascorrimento Verolanuova @it
definition: ENE-WSW trending thrust fault with a gentle NNW dip. The décollement level is L2.
definition: Sovrascorrimento ad andamento ENE-OSO debolmente inclinato verso NNO. Il livello di scollamento è L2. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lombardia Arc subdomain

Capriano del Colle Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:54.907Z
notation: IT-4458
preferred label: Sovrascorrimento Capriano del Colle @it
definition: ESE-WNW trending thrust fault with an intermediate SSW dip. The décollement level is L2.
definition: Sovrascorrimento ad andamento ESE-ONO mediamente inclinato verso SSO. Il livello di scollamento è L2. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lombardia Arc subdomain

Bagnolo Mella Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:54.934Z
notation: IT-4461
preferred label: Sovrascorrimento Bagnolo Mella @it
definition: ESE-WNW trending thrust fault with a gentle NNE dip. The décollement level is L2.
definition: Sovrascorrimento ad andamento ESE-ONO debolmente inclinato verso NNE. Il livello di scollamento è L2. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lombardia Arc subdomain

Ghedi Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:54.849Z
notation: IT-4453
preferred label: Sovrascorrimento Ghedi @it
definition: ENE-WSW trending thrust fault with a gentle NNW dip. The décollement level is L2.
definition: Sovrascorrimento ad andamento ENE-OSO debolmente inclinato verso NNO. Il livello di scollamento è L2. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lombardia Arc subdomain

Castenedolo Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:54.879Z
notation: IT-4454
preferred label: Sovrascorrimento Castenedolo @it
definition: ESE-WNW trending thrust fault with a gentle SSW dip. The décollement level is L2.
definition: Sovrascorrimento ad andamento ESE-ONO debolmente inclinato verso SSO. Il livello di scollamento è L2. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lombardia Arc subdomain

Manerbio Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:54.794Z
notation: IT-4449
preferred label: Sovrascorrimento Manerbio @it
definition: NE-SW trending thrust fault with a gentle NW dip. The décollement level is L2.
definition: Sovrascorrimento ad andamento NE-SO debolmente inclinato verso NO. Il livello di scollamento è L2. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lombardia Arc subdomain

Brescia Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:54.822Z
notation: IT-4451
preferred label: Sovrascorrimento Brescia @it
definition: E-W trending thrust fault with an intermediate north dip. The décollement level is L1.
definition: Sovrascorrimento ad andamento E-O mediamente inclinato verso nord. Il livello di scollamento è L1. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lombardia Arc subdomain

Emilia Arc subdomain
type: Concept
created: 2020-10-09T13:14:13.042Z
notation: IT-99134
preferred label: Sottodominio Arco Emiliano @it
definition: The Emilia Arc subdomain is the central arc of the Northern Apennines. It is a mainly north-verging system of thrust faults with related back-thrusts. Two different décollement levels characterize these thrust faults: the deeper in correspondence of Triassic evaporites (L1), the shallower in correspondence of the Eocene-Oligocene to Miocene marly units (L2). The Emilia arc started deforming in the Tortonian, reached its present-day configuration in the Zanclean, and experienced maximum activity in Piacenzian–Gelasian times.
definition: Il sottodominio dell'Arco Emiliano rappresenta la porzione centrale del fronte dell'Appennino Settentrionale. È costituito da sistemi di faglie con sovrascorrimenti e associati retroscorrimenti. Sono riconoscibili due livelli di scollamento: il più profondo in corrispondenza delle evaporiti triassiche (L1), il più superficiale in corrispondenza delle unità marnose di età variabile dall'Eocene-Oligocene al Miocene (L2). La deformazione ha avuto inizio nel Tortoniano; l'Arco ha raggiunto la sua attuale configurazione nello Zancleano, e ha subito la massima deformazione nell'intervallo Piacenziano-Gelasiano. @it
narrower: Castelnovo thrust
narrower: Voghera - San Colombano Fault System
narrower: Cremona - Reggio nell'Emilia Fault System
narrower: Caviaga - Pontevico Fault System
narrower: Solarolo Fault System
narrower: Cortemaggiore - Cavriago Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/4112
references: https://data.geoscience.earth/ncl/geoera/ref/4127
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Po Plain-Adriatic foreland basin Domain

Caviaga - Pontevico Fault System
type: Concept
created: 2020-10-09T13:14:13.321Z
notation: IT-991342
preferred label: Sistema di faglie Caviaga - Pontevico @it
definition: E-W trending fault system characterized by thrust and back-thrust. The décollement level is L2.
definition: Sistema di faglie caratterizzato da sovrascorrimenti e associati retroscorrrimenti ad andamento E-O. Il livello di scollamento è L2. @it
narrower: Caviaga - Pontevico Thrust
narrower: Caviaga - Pontevico back-thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Emilia Arc subdomain

Caviaga - Pontevico Thrust
type: Concept
created: 2020-10-09T13:14:13.350Z
notation: IT-4550
preferred label: Sovrascorrimento Caviaga - Pontevico @it
definition: E-W trending thrust fault with a gentle south dip.
definition: Sovrascorrimento ad andamento E-O debolmente inclinato verso sud. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Caviaga - Pontevico Fault System

Caviaga - Pontevico back-thrust
type: Concept
created: 2020-10-09T13:14:13.378Z
notation: IT-4542
preferred label: Retroscorrimento Caviaga - Pontevico @it
definition: E-W trending thrust fault with an intermediate north dip. It is a back-thrust associated with the Cornegliano Thrust.
definition: Sovrascorrimento ad andamento E-O mediamente inclinato verso nord. È un retroscorrimento associato al Sovrascorrimento Caviaga - Pontevico. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Caviaga - Pontevico Fault System

Cortemaggiore - Cavriago Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:55.273Z
notation: IT-991344
preferred label: Sistema di faglie Cortemaggiore - Cavriago @it
definition: ESE-WNW trending fault system characterized by thrust and back-thrust. The décollement level is L2.
definition: Sistema di faglie caratterizzato da sovrascorrimenti e associati retroscorrrimenti ad andamento ESE-ONO. Il livello di scollamento è L2. @it
narrower: Cavriago Thrust
narrower: Parma Thrust
narrower: Cortemaggiore Thrust
narrower: Cortemaggiore back-thrust
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Emilia Arc subdomain

Parma Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:55.328Z
notation: IT-4595
preferred label: Sovrascorrimento Parma @it
definition: SE-NW trending thrust fault with an intermediate SW dip.
definition: Sovrascorrimento ad andamento SE-NO mediamente inclinato verso SO. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cortemaggiore - Cavriago Fault System

Cavriago Thrust
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: Concept
created: 2020-10-16T07:56:55.301Z
notation: IT-4586
preferred label: Sovrascorrimento Cavriago @it
definition: ESE-WNW trending thrust fault with a steep SSW dip.
definition: Sovrascorrimento ad andamento ESE-ONO molto inclinato verso SSO. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cortemaggiore - Cavriago Fault System

Cortemaggiore Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:55.356Z
notation: IT-4596
preferred label: Sovrascorrimento Cortemaggiore @it
definition: ESE-WNW trending thrust fault with an intermediate SSW dip.
definition: Sovrascorrimento ad andamento ESE-ONO mediamente inclinato verso SSO. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cortemaggiore - Cavriago Fault System

Cortemaggiore back-thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:55.384Z
notation: IT-4558
preferred label: Retroscorrimento Cortemaggiore @it
definition: ESE-WNW trending thrust fault with an intermediate NNE dip. It is a back-thrust associated with the Cortemaggiore Thrust.
definition: Sovrascorrimento ad andamento ESE-ONO mediamente inclinato verso NNE. È un retroscorrimento associato al Sovrascorrimento Cortemaggiore. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cortemaggiore - Cavriago Fault System

Castelnovo thrust
type: Concept
created: 2020-10-09T13:14:13.070Z
notation: IT-4580
preferred label: Sovrascorrimento Castelnovo @it
definition: ESE-WNW trending thrust fault gentle SSW-dipping. The décollement level is L2.
definition: Sovrascorrimento ad andamento ESE-ONO debolmente inclinato verso SSO. Il livello di scollamento è L2. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Emilia Arc subdomain

Voghera - San Colombano Fault System
type: Concept
created: 2020-10-09T13:14:13.098Z
notation: IT-991340
preferred label: Sistema di faglie Voghera - San Colombano @it
definition: NE-SW to E-W trending fault system constituted by thrust faults with intermediate mostly south dip. The décollement level is L2.
definition: Sistema di faglie caratterizzato da sovrascorrimenti ad andamento da NE-SO a E-O, mediamente inclinati prevalentemente verso sud. Il livello di scollamento è L2. @it
narrower: San Colombano Thrust
narrower: Voghera - Villanterio Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Emilia Arc subdomain

San Colombano Thrust
type: Concept
created: 2020-10-09T13:14:13.126Z
notation: IT-4603
preferred label: Sovrascorrimento San Colombano @it
definition: E-W trending thrust fault with an internediate south dip.
definition: Sovrascorrimento ad andamento E-O mediamente inclinato verso sud. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Voghera - San Colombano Fault System

Voghera - Villanterio Thrust
type: Concept
created: 2020-10-09T13:14:13.154Z
notation: IT-4604
preferred label: Sovrascorrimento Voghera - Villanterio @it
definition: NE-SW thrust fault with intermediate south-east dip.
definition: Sovrascorrimento ad andamento NE-SO mediamente inclinato verso SE. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Voghera - San Colombano Fault System

Solarolo Fault System
type: Concept
created: 2020-10-09T13:14:13.406Z
notation: IT-991343
preferred label: Sistema di faglie Solarolo @it
definition: ESE-WNW trending fault system characterized by thrust faults SSW-dipping. The décollement level is L2.
definition: Sistema di faglie caratterizzato da sovrascorrimenti ad andamento ESE-ONO. Il livello di scollamento è L2. @it
narrower: Solarolo 1 Thrust
narrower: Solarolo Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Emilia Arc subdomain

Solarolo 1 Thrust
type: Concept
created: 2020-10-09T13:14:13.434Z
notation: IT-4571
preferred label: Sovrascorrimento Solarolo 1 @it
definition: ESE-WNW thrust fault with a gentle SSW-dipping.
definition: Sovrascorrimento ad andamento ESE-ONO debolmente inclinato verso SSO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Solarolo Fault System

Solarolo Thrust
type: Concept
created: 2020-10-09T13:14:13.462Z
notation: IT-4574
preferred label: Sovrascorrimento Solarolo @it
definition: ESE-WNW thrust fault with a gentle SSW-dipping.
definition: Sovrascorrimento ad andamento ESE-ONO debolmente inclinato verso SSO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Solarolo Fault System

Cremona - Reggio nell'Emilia Fault System
type: Concept
created: 2020-10-09T13:14:13.182Z
notation: IT-991341
preferred label: Sistema di faglie Cremona - Reggio nell'Emilia @it
definition: SE-NW trending fault system characterized by thrust faults with gentle to intermediate south-west dip and associated back-thrusts. The décollement level is L2.
definition: Sistema di faglie caratterizzato da sovrascorrimenti ad andamento SE-NO, da debolmente a mediamente inclinati verso SO, con associati retroscorrimenti. Il livello di scollamento è L2. @it
narrower: Cremona Thrust
narrower: Parma - Reggio nell'Emilia 1 Thrust
narrower: Parma - Reggio nell'Emilia 1 Back-Thrust
narrower: Cremona Back-Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Emilia Arc subdomain

Cremona Back-Thrust
type: Concept
created: 2020-10-09T13:14:13.293Z
notation: IT-4556
preferred label: Retroscorrimento Cremona @it
definition: ESE-WNW trending thrust fault, intermediate NNE-dipping. It is a back-thrust associated with the Cremona Thrust.
definition: Sovrascorrimento ad andamento ESE-ONO mediamente inclinato verso NNE. È un retroscorrimento associato al Sovrascorrimento Cremona. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cremona - Reggio nell'Emilia Fault System

Cremona Thrust
type: SpatialObject
type: Concept
created: 2020-10-09T13:14:13.210Z
notation: IT-4538
preferred label: Sovrascorrimento Cremona @it
definition: ESE-WNW trending thrust fault, gentle SSW-dipping.
definition: Sovrascorrimento ad andamento ESE-ONO debolmente inclinato verso SSO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4097
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cremona - Reggio nell'Emilia Fault System

Parma - Reggio nell'Emilia 1 Thrust
type: Concept
created: 2020-10-09T13:14:13.238Z
notation: IT-4544
preferred label: Sovrascorrimento Parma - Reggio nell'Emilia 1 @it
definition: SE-NW trending thrust fault with intermediate south-west dip.
definition: Sovrascorrimento ad andamento SE-NO mediamente inclinato verso SO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cremona - Reggio nell'Emilia Fault System

Parma - Reggio nell'Emilia 1 Back-Thrust
type: Concept
created: 2020-10-09T13:14:13.266Z
notation: IT-4548
preferred label: Retroscorrimento Parma - Reggio nell'Emilia 1 @it
definition: SE-NW trending thrust fault with steep north-east dip. It is a back-thrust associated with the Parma - Reggio nell'Emilia Thrust 1.
definition: Sovrascorrimento ad andamento SE-NO molto inclinato verso NE. È un retroscorrimento associato al Sovrascorrimento Parma - Reggio nell'Emilia 1. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cremona - Reggio nell'Emilia Fault System

Lacchiarella Fault System
type: Concept
created: 2020-10-09T13:14:12.481Z
notation: IT-99130
preferred label: Sistema di faglie Lacchiarella @it
definition: N-S trending fault system characterized by thrusts and back-thrusts related to the reactivation and tectonic inversion of former syn-rift Mesozoic (Liassic) normal faults (i.e. Gaggiano Fault System). Reactivation activity spans from Chattian to Tortonian.
definition: Sistema di faglie ad andamento N-S connesso alla riattivazione e all'inversione di faglie normali preesistenti (Sistema di faglie di Gaggiano) legate al rifting mesozoico. La riattivazione è compresa tra il Cattiano e il Tortoniano. @it
narrower: Lacchiarella 2 Thrust
narrower: Lacchiarella 1 Thrust
narrower: Lacchiarella back-thrust
narrower: Lacchiarella Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4087
references: https://data.geoscience.earth/ncl/geoera/ref/4784
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Po Plain-Adriatic foreland basin Domain

Lacchiarella 2 Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4784
type: Concept
created: 2020-10-09T13:14:12.508Z
notation: IT-4480
preferred label: Sovrascorrimento di Lacchiarella 2 @it
definition: N-S trending thrust fault with a gentle eastern dip.
definition: Sovrascorrimento ad andamento N-S debolmente inclinato verso est. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4087
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lacchiarella Fault System

Lacchiarella 1 Thrust
type: Concept
created: 2020-10-09T13:14:12.536Z
notation: IT-4482
preferred label: Sovrascorrimento di Lacchiarella 1 @it
definition: NNE-SSW trending thrust fault with a gentle eastern dip.
definition: Sovrascorrimento ad andamento NNE-SSO debolmente inclinato verso est. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4087
references: https://data.geoscience.earth/ncl/geoera/ref/4784
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lacchiarella Fault System

Lacchiarella back-thrust
type: Concept
created: 2020-10-09T13:14:12.564Z
notation: IT-4551
preferred label: Retroscorrimento di Lacchiarella @it
definition: N-S trending thrust fault with a gentle western dip. It is a back-thrust associated with Lacchiarella Thrust.
definition: Sovrascorrimento ad andamento N-S debolmente inclinato verso ovest. Si tratta di un retroscorrimento associato al Sovrascorrimento Lacchiarella. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4087
references: https://data.geoscience.earth/ncl/geoera/ref/4784
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lacchiarella Fault System

Lacchiarella Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4784
type: Concept
created: 2020-10-09T13:14:12.593Z
notation: IT-4597
preferred label: Sovrascorrimento di Lacchiarella @it
definition: N-S trending thrust fault with an intermediate eastern dip.
definition: Sovrascorrimento ad andamento N-S mediamente inclinato verso est. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4087
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Lacchiarella Fault System

Ferrara - Romagna arc subdomain
type: Concept
created: 2020-10-09T13:14:13.490Z
notation: IT-99135
preferred label: Arco Ferrara - Romagna @it
definition: The Ferrara-Romagna Arc subdomain is the eastern arc of the Northern Apennines. It is a mainly SE-dipping fault system of thrusts, related back-thrusts, and oblique slip faults. The thrusts have a ENE-WSW, in the western sector, and ESE-WNW trend, in the eastern sector. Two different décollement levels characterize these thrust faults: the deeper in correspondence of Triassic evaporites (L1), the shallower in correspondence of the Eocene-Oligocene to Miocene marly units (L2). The fault system activity started in the Late Messinian-Early Pliocene; the outward propagation of the thrust fronts continued until the Zanclean–Piacenzian and the Gelasian, moving from the inner to the outer fronts, and is still active.
definition: Il sottodominio dell'Arco Ferrara-Romagna è la porzione più orientale del fronte dell'Appennino Settentrionale. È costiutito da sovrascorrimenti prevalentemente inclinati verso SE, con associati retroscorrimenti e faglie oblique. I sovrascorrimenti hanno andamento ENE-OSO nel settore occidentale, e ESE-ONO nel settore orientale. Sono riconoscibili due livelli di scollamento: il più profondo in corrispondenza delle evaporiti triassiche (L1), il più superficiale in corrispondenza delle unità marnose di età variabile dall'Eocene-Oligocene al Miocene (L2). L'attività è iniziata nel Messiniano superiore - Pliocene inferiore; la migrazione verso l'esterno del fronte è proseguita fino allo Zancleano-Piacenziano e al Gelasiano, spostandosi dai settori più interni verso quelli esterni, ed è tuttora attiva. @it
narrower: Cavone Fault System
narrower: Novellara Fault System
narrower: Mirandola - Consandolo Fault System
narrower: Poggio Rusco - Ferrara Fault System
narrower: Sermide - Copparo Fault System
narrower: Bagnolo Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/4127
type: SpatialObject
narrower: Correggio back-thrust
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Po Plain-Adriatic foreland basin Domain

Sermide - Copparo Fault System
type: Concept
created: 2020-10-09T13:14:14.851Z
notation: IT-991355
preferred label: Sistema di faglie Sermide - Copparo @it
definition: E-W trending fault system characterized by south-dipping thrust faults.
definition: Sistema di faglie caratterizzato da sovrascorrimenti ad andamento E-O inclinati verso sud. @it
narrower: Sermide - Copparo Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Ferrara - Romagna arc subdomain

Sermide - Copparo Thrust
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2020-10-09T13:14:14.879Z
notation: IT-4605
preferred label: Sovrascorrimento Sermide - Copparo @it
definition: E-W trending thrust fault with a gentle south dip. The décollement level is L1.
definition: Sovrascorrimento ad andamento E-O debolmente inclinato verso sud. Il livello di scollamento è L1. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Sermide - Copparo Fault System

Mirandola - Consandolo Fault System
type: Concept
created: 2020-10-09T13:14:14.337Z
notation: IT-991353
preferred label: Sistema di faglie Mirandola - Consandolo @it
definition: ESE-WNW trending fault system characterized by thrust, back-thrust and associated oblique slip faults. The décollement level is L1.
definition: Sistema di faglie caratterizzato da sovrascorrimenti e retroscorrrimenti ad andamento ESE-ONO, e associate faglie oblique. Il livello di scollamento è L1. @it
narrower: Mirandola - Consandolo thrust
narrower: San Felice 1 inner thrust
narrower: San Felice 2 inner thrust
narrower: San Felice 3 inner thrust
narrower: San Felice 4 inner thrust
narrower: San Felice minor 1 back-thrust
narrower: San Felice minor 2 back-thrust
narrower: San Felice minor 3 back-thrust
narrower: San Felice minor 4 back-thrust
narrower: San Felice 1 oblique slip fault
narrower: San Felice 2 oblique slip fault
narrower: San Felice 3 oblique slip fault
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Ferrara - Romagna arc subdomain

San Felice minor 2 back-thrust
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2020-10-09T13:14:14.541Z
notation: IT-4432
preferred label: Retroscorrimento San Felice minore 2 @it
definition: SE-NW trending thrust fault with a steep NE dip. It is a back-thrust associated with the S. Felice inner 2 thrust.
definition: Sovrascorrimento ad andamento SE-NO molto inclinato verso NE. È un retroscorrimento associato con il Sovrascorrimento San Felice interno 2. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Mirandola - Consandolo Fault System

San Felice minor 3 back-thrust
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2020-10-09T13:14:14.570Z
notation: IT-4430
preferred label: Retroscorrimento San Felice minore 3 @it
definition: ESE-WNW trending thrust fault with a steep NNE dip. It is a back-thrust associated with the Mirandola - Consandolo thrust.
definition: Sovrascorrimento ad andamento ESE-ONO molto inclinato verso NNE. È un retroscorrimento associato con il Sovrascorrimento Mirandola - Consandolo. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Mirandola - Consandolo Fault System

San Felice minor 4 back-thrust
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2020-10-09T13:14:14.599Z
notation: IT-4435
preferred label: Retroscorrimento San Felice minore 4 @it
definition: ESE-WNW trending thrust fault with a steep NNE dip. It is a back-thrust associated with the Mirandola - Consandolo thrust.
definition: Sovrascorrimento ad andamento ESE-ONO molto inclinato verso NNE. È un retroscorrimento associato con il Sovrascorrimento Mirandola - Consandolo. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Mirandola - Consandolo Fault System

San Felice 1 oblique slip fault
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2020-10-09T13:14:14.627Z
notation: IT-4436
preferred label: Faglia obliqua San Felice 1 @it
definition: NE-SW trending oblique slip fault with a steep SE dip.
definition: Faglia obliqua ad andamento NE-SO molto inclinata verso SE. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Mirandola - Consandolo Fault System

San Felice 2 oblique slip fault
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2020-10-09T13:14:14.655Z
notation: IT-4434
preferred label: Faglia obliqua San Felice 2 @it
definition: NNE-SSW trending oblique slip vertical fault with a ESE dip.
definition: Faglia obliqua subverticale ad andamento NNE-SSO inclinata verso ESE. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Mirandola - Consandolo Fault System

Mirandola - Consandolo thrust
type: Concept
created: 2020-10-09T13:14:14.366Z
notation: IT-4475
preferred label: Sovrascorrimento Mirandola - Consandolo @it
definition: ESE-WNW trending thrust fault with an intermediate SSW dip.
definition: Sovrascorrimento ad andamento ESE-ONO mediamente inclinato verso SSO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Mirandola - Consandolo Fault System

San Felice 3 oblique slip fault
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2020-10-09T13:14:14.683Z
notation: IT-4601
preferred label: Faglia obliqua San Felice 3 @it
definition: NE-SW trending oblique slip vertical fault with a SE dip.
definition: Faglia obliqua subverticale ad andamento NE-SO inclinata verso SE. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Mirandola - Consandolo Fault System

San Felice 1 inner thrust
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2020-10-09T13:14:14.400Z
notation: IT-4444
preferred label: Sovrascorrimento San Felice interno 1 @it
definition: E-W trending thrust fault with an intermediate south dip.
definition: Sovrascorrimento ad andamento E-O mediamente inclinato verso sud. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Mirandola - Consandolo Fault System

San Felice 2 inner thrust
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2020-10-09T13:14:14.428Z
notation: IT-4442
preferred label: Sovrascorrimento San Felice interno 2 @it
definition: ESE-WNW trending thrust fault with an intermediate SSW dip.
definition: Sovrascorrimento ad andamento ESE-ONO mediamente inclinato verso SSO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Mirandola - Consandolo Fault System

San Felice 3 inner thrust
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2020-10-09T13:14:14.456Z
notation: IT-4440
preferred label: Sovrascorrimento San Felice interno 3 @it
definition: SSE-NNW trending thrust fault with an intermediate WSW dip.
definition: Sovrascorrimento ad andamento SSE-NNO mediamente inclinato verso OSO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Mirandola - Consandolo Fault System

San Felice 4 inner thrust
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2020-10-09T13:14:14.485Z
notation: IT-4437
preferred label: Sovrascorrimento San Felice interno 4 @it
definition: SSE-NNW trending thrust fault with an intermediate WSW dip.
definition: Sovrascorrimento ad andamento SSE-NNO mediamente inclinato verso OSO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Mirandola - Consandolo Fault System

San Felice minor 1 back-thrust
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2020-10-09T13:14:14.513Z
notation: IT-4598
preferred label: Retroscorrimento San Felice minore 1 @it
definition: ESE-WNW trending thrust fault with a steep NNE dip. It is a back-thrust associated with the S. Felice inner 1 thrust.
definition: Sovrascorrimento ad andamento ESE-ONO molto inclinato verso NNE. È un retroscorrimento associato con il Sovrascorrimento San Felice interno 1. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Mirandola - Consandolo Fault System

Poggio Rusco - Ferrara Fault System
type: Concept
created: 2020-10-09T13:14:14.711Z
notation: IT-991354
preferred label: Sistema di faglie Poggio Rusco -Ferrara @it
definition: E-W trending fault system characterized by south-dipping thrust faults. The décollement level is L1, occasionally L2.
definition: Sistema di faglie caratterizzato da sovrascorrimenti ad andamento E-O inclinati verso sud. Il livello di scollamento è L1, più raramente L2. @it
narrower: Poggio Rusco - Ferrara thrust
narrower: Poggio Rusco 2 thrust
narrower: Poggio Rusco 3 thrust
narrower: Poggio Rusco 4 thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Ferrara - Romagna arc subdomain

Poggio Rusco - Ferrara thrust
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2020-10-09T13:14:14.739Z
notation: IT-4495
preferred label: Sovrascorrrimento Poggio Rusco - Ferrara @it
definition: E-W trending thrust fault with a gentle south dip. The décollement level is L1.
definition: Sovrascorrimento ad andamento E-O debolmente inclinato verso sud. Il livello di scollamento è L1. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Poggio Rusco - Ferrara Fault System

Poggio Rusco 2 thrust
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2020-10-09T13:14:14.766Z
notation: IT-4479
preferred label: Sovrascorrrimento Poggio Rusco 2 @it
definition: E-W trending thrust fault with a gentle south dip. The décollement level is L1.
definition: Sovrascorrimento ad andamento E-O debolmente inclinato verso sud. Il livello di scollamento è L1. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Poggio Rusco - Ferrara Fault System

Poggio Rusco 3 thrust
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2020-10-09T13:14:14.794Z
notation: IT-4488
preferred label: Sovrascorrrimento Poggio Rusco 3 @it
definition: E-W trending thrust fault with an intermediate south dip. The décollement level is L1.
definition: Sovrascorrimento ad andamento E-O mediamente inclinato verso sud. Il livello di scollamento è L1. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Poggio Rusco - Ferrara Fault System

Poggio Rusco 4 thrust
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2020-10-09T13:14:14.823Z
notation: IT-4492
preferred label: Sovrascorrrimento Poggio Rusco 4 @it
definition: E-W trending thrust fault with an intermediate south dip. The décollement level is L2.
definition: Sovrascorrimento ad andamento E-O mediamente inclinato verso sud. Il livello di scollamento è L2. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Poggio Rusco - Ferrara Fault System

Correggio back-thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:55.412Z
notation: IT-4462
preferred label: Retroscorrimento Correggio @it
definition: NNE-SSW trending thrust fault with an intermediate WNW dip. The décollement level is L1.
definition: Sovrascorrimento ad andamento NNE-SSO mediamente inclinato verso ONO. Il livello di scollamento è L1. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Ferrara - Romagna arc subdomain

Bagnolo Fault System
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: Concept
created: 2020-10-16T07:56:55.440Z
notation: IT-991350
preferred label: Sistema di faglie Bagnolo @it
definition: E-W trending fault system characterized by thrust and back-thrust. The décollement level is L1.
definition: Sistema di faglie caratterizzato da sovrascorrimenti e retroscorrimenti ad andamento E-O. Il livello di scollamento è L1. @it
narrower: Bagnolo Thrust
narrower: Bagnolo back-thrust
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Ferrara - Romagna arc subdomain

Bagnolo Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4779
in scheme: Tectonic Boundary Objects in Europe
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:55.468Z
notation: IT-4584
preferred label: Sovrascorrimento Bagnolo @it
definition: E-W trending thrust fault with a steep south dip.
definition: Sovrascorrimento ad andamento E-O molto inclinato verso sud. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Bagnolo Fault System

Bagnolo back-thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4779
in scheme: Tectonic Boundary Objects in Europe
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:55.496Z
notation: IT-4553
preferred label: Retroscorrimento Bagnolo @it
definition: E-W trending thrust fault with a steep north dip. It is a back-thrust asscociated with the Bagnolo Thrust.
definition: Sovrascorrimento ad andamento E-O molto inclinato verso nord. È un retroscorrimento associato al Sovrascorrimento Bagnolo. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Bagnolo Fault System

Cavone Fault System
type: Concept
created: 2020-10-09T13:14:13.518Z
notation: IT-991351
preferred label: Sistema di faglie Cavone @it
definition: E-W trending fault system characterized by thrust and back-thrust, and associated oblique slip faults. The décollement level is L1, occasionally L2.
definition: Sistema di faglie caratterizzato da sovrascorrimenti e retroscorrimenti ad andamento E-O, e associate faglie oblique. Il livello di scollamento è L1, più rararmente L2. @it
narrower: Cavone outer 1 Thrust
narrower: Cavone outer 2 Thrust
narrower: Cavone outer splay Thrust
narrower: Cavone inner 1 Thrust
narrower: Cavone inner 2 Thrust
narrower: Cavone inner 3 Thrust
narrower: Cavone inner 4 Thrust
narrower: Cavone inner 5 Thrust
narrower: Cavone East minor outer Thrust
narrower: Cavone East minor inner Thrust
narrower: Cavone East minor Back-thrust
narrower: Cavone West minor 1 Back-thrust
narrower: Cavone West minor 2 Back-thrust
narrower: Cavone West minor 3 Back-thrust
narrower: Cavone minor 1 Back-thrust
narrower: Cavone minor 2 Back-thrust
narrower: Cavone minor 3 Back-thrust
narrower: Cavone minor 4 Back-thrust
narrower: Cavone 1 Oblique slip fault
narrower: Cavone 2 Oblique slip fault
narrower: Cavone 3 Oblique slip fault
narrower: Cavone 4 Oblique slip fault
narrower: Cavone 5 Oblique slip fault
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Ferrara - Romagna arc subdomain

Cavone outer splay Thrust
type: Concept
created: 2020-10-09T13:14:13.603Z
notation: IT-4446
preferred label: Sovrascorrimento secondario Cavone esterno @it
definition: ESE-WNW trending thrust fault gentle SSW-dipping. The décollement level is L2.
definition: Sovrascorrimento ad andamento ESE-ONO debolmente inclinato verso SSO. Il livello di scollamento è L2. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cavone Fault System

Cavone West minor 3 Back-thrust
type: Concept
created: 2020-10-09T13:14:13.914Z
notation: IT-4500
preferred label: Retroscorrimento Cavone minore ovest 3 @it
definition: E-W trending thrust fault with an intermediate north dip. The décollement level is L1. It is a back-thrust associated with the Cavone inner 1 Thrust.
definition: Sovrascorrimento ad andamento E-O mediamente inclinato verso nord. Il livello di scollamento è L1. È un retroscorrimento associato con il Sovrascorrimento Cavone interno 1. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cavone Fault System

Cavone inner 1 Thrust
type: Concept
created: 2020-10-09T13:14:13.631Z
notation: IT-4508
preferred label: Sovrascorrimento Cavone interno 1 @it
definition: ENE-WSW trending thrust fault intermediate SSE-dipping. The décollement level is L1.
definition: Sovrascorrimento ad andamento ENE-OSO mediamente inclinato verso SSE. Il livello di scollamento è L1. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cavone Fault System

Cavone inner 3 Thrust
type: Concept
created: 2020-10-09T13:14:13.688Z
notation: IT-4543
preferred label: Sovrascorrimento Cavone interno 3 @it
definition: E-W trending thrust fault with an intermediate south dip. The décollement level is L1.
definition: Sovrascorrimento ad andamento E-O mediamente inclinato verso sud. Il livello di scollamento è L1. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cavone Fault System

Cavone minor 3 Back-thrust
type: Concept
created: 2020-10-09T13:14:13.999Z
notation: IT-4547
preferred label: Retroscorrimento Cavone minore 3 @it
definition: ENE-WSW trending thrust fault with a steep NNW dip. The décollement level is L1. It is a back-thrust associated with the Cavone inner 3 Thrust.
definition: Sovrascorrimento ad andamento ENE-OSO molto inclinato verso NNO. Il livello di scollamento è L1. È un retroscorrimento associato con il Sovrascorrimento Cavone interno 3. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cavone Fault System

Cavone inner 4 Thrust
type: Concept
created: 2020-10-09T13:14:13.717Z
notation: IT-4587
preferred label: Sovrascorrimento Cavone interno 4 @it
definition: E-W trending thrust fault with an intermediate south dip. The décollement level is L1.
definition: Sovrascorrimento ad andamento E-O mediamente inclinato verso sud. Il livello di scollamento è L1. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cavone Fault System

Cavone minor 4 Back-thrust
type: Concept
created: 2020-10-09T13:14:14.027Z
notation: IT-4583
preferred label: Retroscorrimento Cavone minore 4 @it
definition: E-W trending thrust fault with a steep north dip. The décollement level is L1. It is a back-thrust associated with the Cavone inner 4 Thrust.
definition: Sovrascorrimento ad andamento E-O molto inclinato verso nord. Il livello di scollamento è L1. È un retroscorrimento associato con il Sovrascorrimento Cavone interno 4. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cavone Fault System

Cavone inner 5 Thrust
type: Concept
created: 2020-10-09T13:14:13.745Z
notation: IT-4590
preferred label: Sovrascorrimento Cavone interno 5 @it
definition: SE-NW trending thrust fault with an intermediate south-west dip. The décollement level is L1.
definition: Sovrascorrimento ad andamento SE-NO mediamente inclinato verso SO. Il livello di scollamento è L1. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cavone Fault System

Cavone 1 Oblique slip fault
type: Concept
created: 2020-10-09T13:14:14.055Z
notation: IT-4588
preferred label: Faglia obliqua Cavone 1 @it
definition: NNE-SSW trending oblique slip vertical fault with WNW dip.
definition: Faglia obliqua subverticale ad andamento NNE-SSO inclinata verso ONO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cavone Fault System

Cavone East minor outer Thrust
type: Concept
created: 2020-10-09T13:14:13.773Z
notation: IT-4591
preferred label: Sovrascorrimento Cavone esterno minore est @it
definition: SE-NW trending thrust fault with a steep south-west dip. The décollement level is L1.
definition: Sovrascorrimento ad andamento SE-NO molto inclinato verso SO. Il livello di scollamento è L1. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cavone Fault System

Cavone 2 Oblique slip fault
type: Concept
created: 2020-10-09T13:14:14.083Z
notation: IT-4579
preferred label: Faglia obliqua Cavone 2 @it
definition: SSE-NNW trending oblique slip vertical fault with a ENE dip.
definition: Faglia obliqua subverticale ad andamento SSE-NNO inclinata verso ENE. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cavone Fault System

Cavone East minor inner Thrust
type: Concept
created: 2020-10-09T13:14:13.802Z
notation: IT-4592
preferred label: Sovrascorrimento Cavone interno minore est @it
definition: SE-NW trending thrust fault with a steep south-west dip. The décollement level is L1.
definition: Sovrascorrimento ad andamento SE-NO molto inclinato verso SO. Il livello di scollamento è L1. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cavone Fault System

Cavone 3 Oblique slip fault
type: Concept
created: 2020-10-09T13:14:14.111Z
notation: IT-4525
preferred label: Faglia obliqua Cavone 3 @it
definition: SSE-NNW trending oblique slip fault with a steep WSW dip.
definition: Faglia obliqua ad andamento SSE-NNO molto inclinata verso OSO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cavone Fault System

Cavone East minor Back-thrust
type: Concept
created: 2020-10-09T13:14:13.830Z
notation: IT-4593
preferred label: Retroscorrimento Cavone minore est @it
definition: ESE-WNW trending thrust fault with a steep NNE dip. The décollement level is L1. It is a back-thrust associated with the Cavone inner 5 Thrust.
definition: Sovrascorrimento ad andamento ESE-ONO molto inclinato verso NNE. Il livello di scollamento è L1. È un retroscorrimento associato con il Sovrascorrimento Cavone interno 5. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cavone Fault System

Cavone 4 Oblique slip fault
type: Concept
created: 2020-10-09T13:14:14.139Z
notation: IT-4552
preferred label: Faglia obliqua Cavone 4 @it
definition: SE-NW trending oblique slip fault with a steep SW dip.
definition: Faglia obliqua ad andamento SE-NO molto inclinata verso SO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cavone Fault System

Cavone outer 1 Thrust
type: Concept
created: 2020-10-09T13:14:13.546Z
notation: IT-4448
preferred label: Sovrascorrimento Cavone esterno 1 @it
definition: E-W trending thrust fault with an intermediate south dip. The décollement level is L1.
definition: Sovrascorrimento ad andamento E-O debolmente inclinato verso sud. Il livello di scollamento è L1. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cavone Fault System

Cavone West minor 1 Back-thrust
type: Concept
created: 2020-10-09T13:14:13.858Z
notation: IT-4514
preferred label: Retroscorrimento Cavone minore ovest 1 @it
definition: E-W trending thrust fault with an intermediate north dip. The décollement level is L1. It is a back-thrust associated with the Cavone inner 1 Thrust.
definition: Sovrascorrimento ad andamento E-O mediamente inclinato verso nord. Il livello di scollamento è L1. È un retroscorrimento associato con il Sovrascorrimento Cavone interno 1. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cavone Fault System

Cavone 5 Oblique slip fault
type: Concept
created: 2020-10-09T13:14:14.168Z
notation: IT-4504
preferred label: Faglia obliqua Cavone 5 @it
definition: SE-NW trending oblique slip fault with a steep SW dip.
definition: Faglia obliqua ad andamento SE-NO molto inclinata verso SO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cavone Fault System

Cavone outer 2 Thrust
type: Concept
created: 2020-10-09T13:14:13.575Z
notation: IT-4455
preferred label: Sovrascorrimento Cavone esterno 2 @it
definition: NE-SW trending thrust fault with an intermediate south-east dip. The décollement level is L1.
definition: Sovrascorrimento ad andamento NE-SO mediamente inclinato verso SE. Il livello di scollamento è L1. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cavone Fault System

Cavone West minor 2 Back-thrust
type: Concept
created: 2020-10-09T13:14:13.886Z
notation: IT-4518
preferred label: Retroscorrimento Cavone minore ovest 2 @it
definition: E-W trending thrust fault with an intermediate north dip. The décollement level is L1. It is a back-thrust associated with the Cavone inner 1 Thrust.
definition: Sovrascorrimento ad andamento E-O mediamente inclinato verso nord. Il livello di scollamento è L1. È un retroscorrimento associato con il Sovrascorrimento Cavone interno 1. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cavone Fault System

Cavone minor 1 Back-thrust
type: Concept
created: 2020-10-09T13:14:13.942Z
notation: IT-4532
preferred label: Retroscorrimento Cavone minore 1 @it
definition: E-W trending thrust fault with a steep north dip. The décollement level is L1. It is a back-thrust associated with the Cavone inner 2 Thrust.
definition: Sovrascorrimento ad andamento E-O molto inclinato verso nord. Il livello di scollamento è L1. È un retroscorrimento associato con il Sovrascorrimento Cavone interno 2. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cavone Fault System

Cavone inner 2 Thrust
type: Concept
created: 2020-10-09T13:14:13.660Z
notation: IT-4535
preferred label: Sovrascorrimento Cavone interno 2 @it
definition: ENE-WSW trending thrust fault intermediate SSE-dipping. The décollement level is L1.
definition: Sovrascorrimento ad andamento ENE-OSO mediamente inclinato verso SSE. Il livello di scollamento è L1. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cavone Fault System

Cavone minor 2 Back-thrust
type: Concept
created: 2020-10-09T13:14:13.970Z
notation: IT-4524
preferred label: Retroscorrimento Cavone minore 2 @it
definition: ENE-WSW trending thrust fault with a steep NNW dip. The décollement level is L1. It is a back-thrust associated with the Cavone inner 2 Thrust.
definition: Sovrascorrimento ad andamento ENE-OSO molto inclinato verso NNO. Il livello di scollamento è L1. È un retroscorrimento associato con il Sovrascorrimento Cavone interno 2. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Cavone Fault System

Novellara Fault System
type: Concept
created: 2020-10-09T13:14:14.196Z
notation: IT-991352
preferred label: Sistema di faglie Novellara @it
definition: NE-SW trending fault system characterized by thrust and associated oblique slip faults. The décollement level is L1.
definition: Sistema di faglie caratterizzato da sovrascorrimento ad andamento NE-SO e associate faglie oblique. Il livello di scollamento è L1. @it
narrower: Novellara Thrust
narrower: Novellara 2 oblique slip fault
narrower: Novellara 1 oblique slip fault
narrower: Novellara 3 oblique slip fault
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Ferrara - Romagna arc subdomain

Novellara Thrust
type: Concept
created: 2020-10-09T13:14:14.225Z
notation: IT-4466
preferred label: Sovrascorrimento Novellara @it
definition: NE-SW trending thrust fault with an intermediate south-east dip.
definition: Sovrascorrimento ad andamento NE-SO mediamente inclinato verso SE. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Novellara Fault System

Novellara 2 oblique slip fault
type: SpatialObject
type: Concept
created: 2020-10-09T13:14:14.253Z
notation: IT-4450
preferred label: Faglia obliqua Novellara 2 @it
definition: SSE-NNW trending oblique slip vertical fault with a ENE dip.
definition: Faglia obliqua subverticale ad andamento SSE-NNO inclinata verso ENE. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Novellara Fault System

Novellara 1 oblique slip fault
type: Concept
created: 2020-10-09T13:14:14.281Z
notation: IT-4452
preferred label: Faglia obliqua Novellara 1 @it
definition: SE-NW trending oblique slip fault with a steep SW dip.
definition: Faglia obliqua ad andamento SE-NO molto inclinata verso SO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Novellara Fault System

Novellara 3 oblique slip fault
references: https://data.geoscience.earth/ncl/geoera/ref/4779
type: Concept
created: 2020-10-09T13:14:14.309Z
notation: IT-4459
preferred label: Faglia obliqua Novellara 3 @it
definition: SSE-NNW trending oblique slip fault with a steep ENE dip.
definition: Faglia obliqua ad andamento SSE-NNO molto inclinata verso ENE. @it
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Novellara Fault System

Monferrato Front subdomain
type: Concept
created: 2020-10-09T13:14:12.900Z
notation: IT-99133
preferred label: Sottodominio Arco del Monferrato @it
definition: The Monferrato front subdomain, one of the three parts composing the Northern Apennines thrust front, is characterized by thrust faults distributed in an arc-shaped geometry, with a mean E-W trend, mainly S-dipping. The activitiy ranges from Late Oligocene to Pleistocene
definition: Il sottodominio del Fronte del Monferrato, uno dei tre settori che compongono il fronte dell'Appennino settentrionale,è caratterizzato da sovrascorrimenti disposti ad arco, con un andamento mediamente E-O, prevalentemente immergenti a sud. La loro attività è comresa tra l'Oligocene superiore e il Pleistocene. @it
narrower: Inner Monferrato Thrust front
narrower: Tricerro Thrust
narrower: Sali Vercellese Thrust
narrower: Outer Monferrato thrust front
narrower: Montecastello Thrust
narrower: Montecastello back- thrust
narrower: Montechiaro d'Asti Thrust
type: SpatialObject
narrower: Chivasso thrust
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Po Plain-Adriatic foreland basin Domain

Sali Vercellese Thrust
type: Concept
created: 2020-10-09T13:14:12.985Z
notation: IT-4511
preferred label: Sovrascorrimento Sali Vercellese @it
definition: SE-NW trending thrust fault with an intermediate south-west dip.
definition: Sovrascorrimento ad andamento SE-NO mediamente inclinato verso SO. @it
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Monferrato Front subdomain

Outer Monferrato thrust front
type: Concept
created: 2020-10-09T13:14:13.013Z
notation: IT-4531
preferred label: Fronte esterno dei sovrascorrimenti del Monferrato @it
definition: ESE-WNW trending thrust fault with an intermediate SSW-dipping.
definition: Sovrascorrimento ad andamento ESE-ONO mediamente inclinato verso SSO. @it
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Monferrato Front subdomain

Montechiaro d'Asti Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4784
references: https://data.geoscience.earth/ncl/geoera/ref/4789
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:55.217Z
notation: IT-4472
preferred label: Sovrascorrimento Montechiaro d'Asti @it
definition: ESE-WNW trending thrust fault with an intermediate SSW-dipping.
definition: Sovrascorrimento ad andamento ESE-ONO mediamente inclinato verso SSO. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Monferrato Front subdomain

Chivasso thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4784
references: https://data.geoscience.earth/ncl/geoera/ref/4789
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:55.244Z
notation: IT-4493
preferred label: Sovrascorimmento Chivasso @it
definition: E-W trending thrust fault with an intermediate south dip.
definition: Sovrascorrimento ad andamento E-O mediamente inclinato verso sud. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Monferrato Front subdomain

Montecastello back- thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:55.161Z
notation: IT-4519
preferred label: Retroscorrimento Montecastello @it
definition: SE-NW trending thrust fault with a steep NE dip. It is a back-thrust associated with the Montecastello thrust.
definition: Sovrascorrimento ad andamento SE-NO molto inclinato verso NE. È un retroscorrimento associato al Sovrascorrimento Montecastello. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Monferrato Front subdomain

Montecastello Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4784
references: https://data.geoscience.earth/ncl/geoera/ref/4789
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:55.189Z
notation: IT-4522
preferred label: Sovrascorrimento Montecastello @it
definition: SE-NW trending thrust fault with an intermediate SW dip.
definition: Sovrascorrimento ad andamento SE-NO mediamente inclinato verso SO. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Monferrato Front subdomain

Inner Monferrato Thrust front
type: Concept
created: 2020-10-09T13:14:12.928Z
notation: IT-4527
preferred label: Fronte interno dei sovrascorrimenti del Monferrato @it
definition: SE-NW trending thrust fault with an intermediate SW dip.
definition: Sovrascorrimento ad andamento SE-NO mediamente inclinato verso SO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4789
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Monferrato Front subdomain

Tricerro Thrust
type: Concept
created: 2020-10-09T13:14:12.957Z
notation: IT-4602
preferred label: Sovrascorrimento Tricerro @it
definition: E-W trending thrust fault with an internediate south dip.
definition: Sovrascorrimento ad andamento E-O mediamente inclinato verso sud. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4789
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Monferrato Front subdomain

Western Alps Back-thrusts subdomain
type: Concept
created: 2020-10-09T13:14:12.620Z
notation: IT-99131
preferred label: Sottodominio dei retroscorrimenti delle Alpi Occidentali @it
definition: The Western Alps back-thrust subdomain is characterized by thrusts connected to the south-verging retrobelt of the Alps, active during Oligocene and Miocene. The thrusts and backthrusts have a ENE-WSW trend. They involve generally both the metamorphic basement and the Meso-Cenozoic sedimentary succession.
definition: Il sottodominio dei retroscorrimenti delle Alpi Occidentali è caratterizzato da sovrascorrimenti connessi alla porzione di catena Alpina con vergenza verso sud, attiva durante l'Oligocene e il Miocene. I sovrascorrimenti e retroscorrimenti hanno un andamento ENE-OSO. Essi coinvolgono generalmente sia il basamento metamorfico che la successione sedimentaria meso-cenozoica. @it
narrower: Romentino Fault System
narrower: Ghemme - Borgoticino Fault System
narrower: Salussola Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/4127
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Po Plain-Adriatic foreland basin Domain

Salussola Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/4784
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:54.514Z
notation: IT-991313
preferred label: Sistema di faglie Salussola @it
definition: ENE-WSW trending fault system characterized by NNW-dipping thrust faults. They involve both the metamorphic basement and the Mesozoic sedimentary succession. The activity is dated Upper Eocene-Upper Oligocene.
definition: Sistema di faglie caratterizzato da sovrascorrimenti ad andamento ENE-OSO e immersione verso NNO. I sovrascorrimenti coinvolgono sia il basamento metamorfico che la successione sedimentaria mesozoica. L'attività è riferibile all'Eocene superiore-Oligocene superiore. @it
narrower: Salussola Thrust
narrower: Salussola 1 Thrust
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Western Alps Back-thrusts subdomain

Salussola 1 Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4784
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:54.570Z
notation: IT-4489
preferred label: Sovrascorrimento Salussola 1 @it
definition: ENE-WSW trending thrust fault with a gentle NNW dip.
definition: Sovrascorrimento ad andamento ENE-OSO debolmente inclinato verso NNO. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Salussola Fault System

Salussola Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4784
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:54.542Z
notation: IT-4487
preferred label: Sovrascorrimento Salussola @it
definition: ENE-WSW trending thrust fault with a gentle NNW dip.
definition: Sovrascorrimento ad andamento ENE-OSO debolmente inclinato verso NNO. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Salussola Fault System

Ghemme - Borgoticino Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/4784
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:54.431Z
notation: IT-991312
preferred label: Sistema di faglie Ghemme - Borgoticino @it
definition: NE-SW trending fault system characterized by thrusts and back-thrusts, active in the Lower-Middle Miocene. They involve basement and sedimentary succession up to Middle Miocene.
definition: Sistema di faglie ad andamento NE-SO caratterizzato da sovrascorrimenti e retroscorrimenti attivi nel Miocene inferiore-medio. Essi coinvolgono sia il basamento metamorfico che la successione sedimentaria fino al Miocene medio. @it
narrower: Sesia Back-thrust
narrower: Sesia Thrust
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Western Alps Back-thrusts subdomain

Sesia Thrust
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/4784
references: https://data.geoscience.earth/ncl/geoera/ref/4789
type: Concept
created: 2020-10-16T07:56:54.486Z
notation: IT-4498
preferred label: Sovrascorrimento Sesia @it
definition: NE-SW trending thrust fault with a steep NW dip.
definition: Sovrascorrimento ad andamento NE-SO molto inclinato verso NO. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Ghemme - Borgoticino Fault System

Sesia Back-thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
type: Concept
created: 2020-10-16T07:56:54.459Z
notation: IT-4483
preferred label: Retroscorrimento Sesia @it
definition: ENE-WSW trending thrust fault with a gentle SSE dip. It is a back-thrust associated with Sesia Thrust.
definition: Sovrascorrimento ad andamento ENE-OSO debolmente inclinato verso SSE; è un retroscorrimento associato con il Sovrascorrimento Sesia. @it
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Ghemme - Borgoticino Fault System

Romentino Fault System
type: Concept
created: 2020-10-09T13:14:12.649Z
notation: IT-991311
preferred label: Sistema di faglie Romentino @it
definition: ENE-WSW trending thrust faults, NNW dipping, with décollement at the level of the Eocene terrigenous succession. The activity is dated Lower-Middle Miocene.
definition: Sistema di faglie caratterizzato da sovrascorrimenti ad andamento ENE-OSO e immersione verso NNO, con livello di scollamento nella successione terrigena eocenica. L'attività è riferibile al Miocene inferiore-medio. @it
narrower: Turbigo Thrust
narrower: Romentino Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/4784
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Western Alps Back-thrusts subdomain

Turbigo Thrust
type: Concept
created: 2020-10-09T13:14:12.677Z
notation: IT-4501
preferred label: Sovrascorrimento Turbigo @it
definition: ENE-WSW trending thrust fault with intermediate NNW dip.
definition: Sovrascorrimento ad andamento ENE-OSO mediamente inclinato verso NNO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4097
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Romentino Fault System

Romentino Thrust
type: Concept
created: 2020-10-09T13:14:12.704Z
notation: IT-4507
preferred label: Sovrascorrimento Romentino Sud @it
definition: ENE-WSW trending thrust fault with intermediate NNW dip.
definition: Sovrascorrimento ad andamento ENE-OSO mediamente inclinato verso NNO. @it
references: https://data.geoscience.earth/ncl/geoera/ref/4784
type: SpatialObject
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
in scheme: Tectonic Boundary Objects in Europe
broader: Romentino Fault System

Campidano Graben Domain
references: https://data.geoscience.earth/ncl/geoera/ref/4769
references: https://data.geoscience.earth/ncl/geoera/ref/4774
type: Concept
created: 2020-10-16T07:56:55.886Z
notation: IT-9921
preferred label: Dominio del Graben del Campidano @it
definition: The Campidano Graben domain corresponds to a NW-SE elongated Plio-Quaternary depression lies on the SW sector of the Sardinia block and extends from the Gulf of Oristano to the NW and the Gulf of Cagliari to the South. The graben is probably related to the coeval extension in the Tyrrhenian Sea; it is in part superimposed on the Oligo-Miocene rift system and involves mostly reactivated normal faults (Casula et al., 2001; Carmignani et al., 2001; 2015). This domain is characterized by prevalently NW-SE striking normal faults organized in half-graben geometry. In the central and southern sectors of the basin two main longitudinal master faults (i.e.: Isili fault, and Monastir fault) are along the eastern side. Several associated second order synthetic and antithetic structures are present in the subsurface of the Campidano basin. In the same way, minor extensional tectonic features related to the Plio-Quaternary extensional phase have been also mapped affecting the Variscan basement out of the borders of the Campidano valley.
definition: Il dominio del Graben del Campidano corrisponde con una depressione plio-quaternaria allungata NO-SE, ubicata nel settore SO del blocco sardo, e si estende dal Golfo di Oristano, a nord-ovest, fino al Golfo di Cagliari, a sud. Il graben è probabilmente legato alla coeva estensione nel Mar Tirreno, è sovraimposto in parte al sistema di rift dell'Oligo-Miocene e coinvolge prevalentemente faglie normali riattivate (Casula et al., 2001; Carmignani et al., 2001; 2015). Il dominio è caratterizzato da faglie normali prevalentemente a direzione NO-SE organizzate con geometria ad half-graben. Nei settori centrale e meridionale del bacino, due faglie principali longitudinali (faglia di Isili e la faglia di Monastir) bordano il lato orientale. Diverse strutture di secondo ordine associate, sintetiche e antitetiche, sono presenti nel sottosuolo del bacino. Inoltre, elementi estensionali minori, connessi con la fase estensionale plio-quaternaria, sono stati mappati fuori dal bacino del Campidano, a coinvolgere il basamento varisico. @it
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Italy

Sicilian-Maghrebian Domain
references: https://data.geoscience.earth/ncl/geoera/ref/4800
references: https://data.geoscience.earth/ncl/geoera/ref/4777
type: Concept
created: 2020-10-16T07:56:55.607Z
notation: IT-9915
preferred label: Dominio Sicilide-Magrebide @it
definition: The Sicilian-Maghrebian domain extends in the whole Sicily west of the Etna volcano and the Calabro- Peloritane Units and north of the Catania-Gela Foredeep. This structural domain is related to the complex Sicilian Fold and Thrust Belt system deriving from the Miocene-Pliocene deformation of the Northern African Continental Margin. On the whole, the domain is characterized by prevalently E-W trending, S- and locally SE-verging thrust tectonic related structures that show variable shortening and rotational rates. Compressive structures are locally dislocated by strike-slip faults mainly related to the rotational Plio-Pleistocene phase. High-angle normal fault systems related to early Pliocene-Present extensional tectonics are also present.
definition: Il Dominio Sicilide-Magrebide si estende su tutta la Sicilia, a ovest dell'Etna e delle unità Calabro-Peloritane, e a nord dell'avanfossa Gela-Catania. Questo dominio strutturale è connesso al complesso sistema a pieghe e sovrascorrimenti (Sicilian Fold and Thrust Belt system) derivante dalle deformazioni mio-plioceniche del margine continentale africano. Nell'insieme, il dominio è caratterizzato da sovrascorrimenti ad andamento prevalentemente E-O vergenti a S e, localmente, a SE con tassi di raccorciamento e rotazione variabili. Le strutture compressive sono localmente dislocate da faglie trascorrenti prevalentemente connesse a rotazione durante il Plio-Pleistocene. Sono presenti anche sistemi di faglie normali ad alto angolo connesse alla tettonica estensionale del Pliocene inferiore-attuale. @it
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Italy

Northern Apennines Domain
references: https://data.geoscience.earth/ncl/geoera/ref/4795
references: https://data.geoscience.earth/ncl/geoera/ref/4778
type: Concept
created: 2020-10-16T07:56:52.745Z
notation: IT-9908
preferred label: Dominio Appennino Settentrionale @it
definition: The Northern Apennines domain is characterized by thrust fault imbricated structures, mainly E-vergent, related to the Apenninic orogenic phase (post-collisional neoalpine) active from Chattian. Several decollemenet low-competence levels are recognized (the deeper at the top of the Triassic Anidriti di Burano, the shallower located on Lower Jurassic Rosso Ammonitico, Lower Cretaceous Marne a Fucoidi, Eocene-Lower Miocene Scaglia cinerea or Messinian Evaporites). Back-thrusts are associated to the main structures. The boundary between Northern and Southern Apennines domains is the Ortona-Roccamonfina lineament.
definition: Il dominio dell'Appennino Settentrionale è caratterizzato da sovrascorrimenti, prevalentemente vergenti a est, legati alla fase orogenica Appenninica (post-collisionale, neoalpina) attiva dal Cattiano. Sono riconosciuti diversi livelli di scollamento a bassa competenza (il più profondo al tetto delle Anidriti di Burano triassiche, i più superficiali posti variabilmente al Rosso Ammonitico del Giurassico inferiore, alle Marne a Fucoidi del Cretacico inferiore, alla Scaglia cinerea dell'Eocene-Miocene inferiore o alle evaporiti del Messiniano). Retroscorrimenti sono associati alle strutture principali. Il limite tra i domini dell'Appennino Settentrionale e Meridionale è posto in corrispondenza della linea Ortona-Roccamonfina. @it
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Italy

Sardinia Variscan basement Domain
references: https://data.geoscience.earth/ncl/geoera/ref/4767
references: https://data.geoscience.earth/ncl/geoera/ref/4768
type: Concept
created: 2020-10-16T07:56:55.830Z
notation: IT-9919
preferred label: Dominio del basamento Ercinico della Sardegna @it
definition: The largest part of Sardinia consists of a Variscan basement, composed by different tectonic units deformed and emplaced with a tectonic transport direction toward SW during the Early Carboniferous and of a Permo-Carboniferous batholith emplaced between 340 and 280 Ma (Carmignani et al., 2001). The main tectonic features are ductile and brittle-ductile overthrusts developed during the continental collision between Gondwana and the Armorica Terranes Assemblage. Low- to high-angle normal faults developed during collapse of the thickened crust in the final stages of the Variscan orogeny, in part during emplacement of the plutonic complex, the dyke complex and development of a volcano-sedimentary complex of Upper Carboniferous–Lower Triassic age (Carmignani et al., 2015). The External zone, cropping out in the SW sector (Iglesiente and Sulcis), is the less metamorphosed and deformed portion of the Sardinia Variscan chain allowing to distinguish fold and thrust (Carmignani et al., 2004). The Variscan tectonic structures are locally cut or reactivated by the most recent normal faults related to the extensional phase responsible for the Oligocene-Miocene Sardinia Rifting System.
definition: La maggior parte della sardegna è costituita da basamento varisico, composto da differenti unità tettoniche, deformate e messe in posto, con una direzione di trasporto verso SO, durante il Carbonifero inferiore. A queste unità si aggiunge un batolite permo-carbonifero messo in posso tra 340 e 280 Ma (Carmignani et al., 2001). I principali elementi tettonici sono overthrust duttili e fragili-duttili sviluppatisi durante la collisione tra terranes di provenienza gondwanica e armoricana. Faglie normali, da basso ad alto angolo, si sono sviluppate durante il collasso di crosta inspessita, nelle fasi finali dell'orogenesi varisica, e in parte durante la messa in posto del complesso plutonico, dei dicchi e lo sviluppo del complesso vulcano-sedimentario (Carbonifero superiore–Triassico inferiore) (Carmignani et al., 2015). La Zona Esterna, affiorante nel settore SO (Iglesiente e Sulcis), è la meno metamorfosata e deformata della catena varisica, consentendo di distinguere pieghe e sovrascorrimenti (Carmignani et al., 2004). Le strutture tettoniche varisiche sono localmente tagliate o riattivate da faglie normali più recenti connesse con la fase estensionale responsabile della formazione del sistema di rifting della Sardegna (Oligocene-Miocene). @it
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Italy

Apennines extensional Domain
references: https://data.geoscience.earth/ncl/geoera/ref/4796
type: Concept
created: 2020-10-16T07:56:52.774Z
notation: IT-9909
preferred label: Dominio estensionale appenninico @it
definition: The domain is characterized by normal faults, mainly NW-SE and NNW-SSE oriented, related to the extensional regime active from the Middle-Upper Miocene due to the counter-clockwise rotation of the Corsica-Sardinia block, the opening of Tyrrhenian Sea, the foreland flexural process, and the fast overall uplift of the Apennines chain. The age of inception rejuvenates from west to east superimposing on the compressional phases. In the Northern Apennines extensional kinematic is associated with minor transtensional, with master faults are often E-dipping with antithetic W-dipping faults; in the Southern Apennines both right- and left-strike-slip faults are observed, related to counter- and clockwise rotation respectively.
definition: Il dominio estensionale appenninico è caratterizzato da faglie normali, ad andamento prevalente NO-SE e NNO-SSE, connesse al regime estensionale attivo dal Miocene medio-superiore connesso alla rotazione antioraria del blocco sardo-corso, all'apertura del mar Tirreno, ai processi di flessurazione dell'avampaese, e al generale sollevamento della catena appenninica. L'età di inizio del regime estensionale ringiovanisce da ovest verso est sovraimponendosi alle fasi compressive. Nell'Appennino Settenrionale la cinematica estensionale è associata a transtensione secondaria, con faglie principali generalmente immergenti a E e faglie antitetiche immergenti a O. Nell'Appennino Meridionale sono riconosciute sia faglie trascorrenti sinistre che destre, connesse, a rotazione oraria e antioraria, rispettivamente. @it
narrower: Acciano fault
narrower: Barisciano fault
narrower: Bazzano fault
narrower: Civitaretenga fault
narrower: Colle Cicogna fault
narrower: Colle Cocurello fault
narrower: Colle Praticciolo fault
narrower: Costa Castello fault
narrower: Fontechio fault
narrower: Fossa fault
narrower: Molina Aterno fault
narrower: Monticchio fault
narrower: Paganica fault
narrower: Poggio Picenze fault
narrower: Ripa fault
narrower: San Demetrio 3 fault
narrower: San Demetrio fault
narrower: San Martino fault
narrower: San Pio delle Camere fault
narrower: San Rocco fault
narrower: Valle Bovacchio fault
narrower: Vallecupa fault
narrower: Vigne Basse fault
narrower: Villa S.Angelo fault
narrower: Base Monte Vettore 2 fault
narrower: Base Monte Vettore 3 fault
narrower: Base Monte Vettore fault
narrower: Colle Infante - Monte Rotondo fault
narrower: Colle Infante fault
narrower: Cordone del Vettore fault
narrower: Forca di Presta fault
narrower: Monte Abuzzago 1 fault
narrower: Frontignano fault
narrower: Monte Argentella fault
narrower: Monte Bicco fault
narrower: Monte Cornaccione - Le Pianelle
narrower: Monte Cornaccione fault
narrower: Monte Porche fault
narrower: Palazzo Borghese fault
narrower: Passo Cattivo 3 fault
narrower: Passo Cattivo fault
narrower: Quarto San Lorenzo fault
narrower: Scoglio della Volpe - Colle Abieri fault
narrower: Strada Frontignano - Cornaccione 2 fault
narrower: Strada Frontignano - M Cornaccione fault
narrower: Valle delle Fonti fault
narrower: Vettore 1
narrower: Vettore 3 fault
narrower: Vettore 5 fault
narrower: Vettoretto 2
narrower: Vettoretto 3
narrower: Vettoretto fault
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Italy

Passo Cattivo fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.954Z
notation: IT-6127
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Quarto San Lorenzo fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.982Z
notation: IT-6128
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Fossa fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.054Z
notation: IT-6096
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Molina Aterno fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.082Z
notation: IT-6097
notation: IT-6098
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Costa Castello fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:52.998Z
notation: IT-6094
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Fontechio fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.026Z
notation: IT-6095
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Colle Cocurello fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:52.942Z
notation: IT-6092
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Vettore 5 fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:54.178Z
notation: IT-6135
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Colle Praticciolo fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:52.970Z
notation: IT-6093
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Vettoretto 2
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:54.206Z
notation: IT-6136
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Civitaretenga fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:52.886Z
notation: IT-6090
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Vettore 1
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:54.123Z
notation: IT-6133
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Colle Cicogna fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:52.914Z
notation: IT-6091
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Vettore 3 fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:54.150Z
notation: IT-6134
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Barisciano fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:52.830Z
notation: IT-6088
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Strada Frontignano - M Cornaccione fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:54.067Z
notation: IT-6131
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Bazzano fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:52.858Z
notation: IT-6089
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Valle delle Fonti fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:54.095Z
notation: IT-6132
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Scoglio della Volpe - Colle Abieri fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:54.010Z
notation: IT-6129
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Strada Frontignano - Cornaccione 2 fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:54.038Z
notation: IT-6130
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Forca di Presta fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.674Z
notation: IT-6118
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Acciano fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:52.802Z
notation: IT-6087
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Passo Cattivo 3 fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.926Z
notation: IT-6126
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Monte Porche fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.870Z
notation: IT-6124
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Palazzo Borghese fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.898Z
notation: IT-6125
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Monte Cornaccione - Le Pianelle
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.814Z
notation: IT-6122
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Monte Cornaccione fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.842Z
notation: IT-6123
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Monte Argentella fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.758Z
notation: IT-6120
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Monte Bicco fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.786Z
notation: IT-6121
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Monte Abuzzago 1 fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.701Z
notation: IT-6119a
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Frontignano fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.730Z
notation: IT-6119b
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Colle Infante fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.617Z
notation: IT-6116
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Cordone del Vettore fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.646Z
notation: IT-6117
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Base Monte Vettore fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.559Z
notation: IT-6114
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Colle Infante - Monte Rotondo fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.588Z
notation: IT-6115
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Base Monte Vettore 2 fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.503Z
notation: IT-6112
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Base Monte Vettore 3 fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.531Z
notation: IT-6113
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Vigne Basse fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.447Z
notation: IT-6110
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Villa S.Angelo fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.475Z
notation: IT-6111
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Valle Bovacchio fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.391Z
notation: IT-6108
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Vallecupa fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.419Z
notation: IT-6109
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Vettoretto fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:54.262Z
notation: IT-6138
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Vettoretto 3
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:54.234Z
notation: IT-6137
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

San Rocco fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.363Z
notation: IT-6107
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

San Martino fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.308Z
notation: IT-6105
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

San Pio delle Camere fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.335Z
notation: IT-6106
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

San Demetrio 3 fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.252Z
notation: IT-6103
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

San Demetrio fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.280Z
notation: IT-6104
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Poggio Picenze fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.195Z
notation: IT-6101
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Ripa fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.224Z
notation: IT-6102
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Monticchio fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.138Z
notation: IT-6099
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Paganica fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:53.166Z
notation: IT-6100
in scheme: Tectonic Boundary Objects in Europe
broader: Apennines extensional Domain

Sardinia Graben system Domain
references: https://data.geoscience.earth/ncl/geoera/ref/4769
references: https://data.geoscience.earth/ncl/geoera/ref/4774
type: Concept
created: 2020-10-16T07:56:55.858Z
notation: IT-9920
preferred label: Dominio del sistema dei graben della Sardegna @it
definition: The Sardinia Graben System characterizes the western sector of the Sardinia block with a roughly N-S elongated depression running from the Gulf of Asinara to the North and the Gulf of Cagliari to the south (Carmignani et al., 2001; 2015). The system started developing since the Oligocene up to Miocene upon the Variscan metamorphic and plutonic basement as a result of the extensional regime that affected the Iberian-Europe Region at about 34 Ma (Casula et al., 2001). The present-day structure of the Sardinia Graben System consists of large graben whose margins are well exposed and bordered by major N-S striking normal faults with associated minor parallel and transverse structures (Casula et al., 2001; Carmignani et al., 2015).
definition: Il sistema dei graben della Sardegna, che caratterizza la porzione occidentale del blocco sardo, si presenta come una depressione con un andamento allungato circa N-S, dal Golfo dell'Asinara, a nord, al Golfo di Cagliari, a sud (Carmignani et al., 2001; 2015). I graben hanno iniziato a svilupparsi a partire dall'Oligocenefino al Miocene, sul basamento metamorfico e plutonico varisico, come risultato del regime estensionale che ha coinvolto la regione iberico-europea a partire da 34 Ma (Casula et al., 2001). L'attuale assetto del sistema dei graben della Sardegna consiste in ampi graben i cui margini, ben esposti, sono bordati da faglie normali principali ad andamento N-S, con associate faglie minori parallele e strutture trasversali (Casula et al., 2001; Carmignani et al., 2015). @it
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Italy

Sestri-Voltaggio Lineament
references: https://data.geoscience.earth/ncl/geoera/ref/4772
type: Concept
created: 2020-10-16T07:56:52.689Z
notation: IT-9906
preferred label: Linea Sestri-Voltaggio @it
definition: The Sestri-Voltaggio lineament is a N-S lineament acting as boundary between Alps and Apennines chains with opposite vergence, it was active, as transform fault (Scholle, 1970), during the eo- and meso-alpine tectonic phases
definition: La linea Sestri-Voltaggio, lineamento ad andamento N-S che ha agito come limite tra le catene alpina e appenninica caratterizzate da opposte vergenze, è stato attivo come faglia trasforme (Scholle, 1970) durante le fasi tettoniche eo- e meso-alpina. @it
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Italy

Taormina Line
references: https://data.geoscience.earth/ncl/geoera/ref/4765
type: Concept
created: 2020-10-16T07:56:55.774Z
notation: IT-99181
preferred label: Linea di Taormina @it
definition: The Taormina Line identifies the southern border of the Calabride-Peloritane domain. This Tectonic Line is interpreted to be a NNE dipping thrust fault (Bonardi et al., 2001).
definition: La Linea di Taormina identifica il bordo meridioanle del Dominio Calabro-Peloritano. Questa linea è interpretata come un sovrascorrimento immergente a NNE (Bonardi et al., 2001). @it
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Italy

Ligurian Fault Domain
references: https://data.geoscience.earth/ncl/geoera/ref/4795
references: https://data.geoscience.earth/ncl/geoera/ref/4778
type: Concept
created: 2020-10-16T07:56:52.717Z
notation: IT-9907
preferred label: Dominio Ligure @it
definition: The Ligurian domain is characterized by thrusts active during the collisional mesoalpine underthrusting and underplating (Late Cretaceous-Middle Eocene); furtherly active during post-collisional neoalpine eastward overthrusting (Oligocene-early Pliocene or Pleistocene - Sillaro e Marecchia). Both ductile and fragile deformations are recorded.
definition: Il Dominio Ligure è caratterizzato da sovrascorrimenti attivi durante la fase collisionale mesoalpina (underthrusting e underplating; Cretacico superiore-Eocene medio); successivamente attivi durante la migrazione verso est connessa alla fase post-collisionale neoalpina (Oligocene-Pliocene inferiore e Pleistocene - zona del Sillaro e Marecchia). Sono registrate sia deformazioni duttili che fragili. @it
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Italy

Calabride-Peloritane Domain
references: https://data.geoscience.earth/ncl/geoera/ref/4765
type: Concept
created: 2020-10-16T07:56:55.802Z
notation: IT-9918
preferred label: Dominio Calabro-Peloritano @it
definition: The Calabride-Peloritane domain is a fault-bounded exotic terrane located at the intersection between the NW-SE-trending Southern Apennines and the E-W-trending Sicilian Maghrebides, characterized by: i) pre-Mesozoic crystalline basement with ductile deformations (Hercynian Orogeny), ii) Alpine (Apennines) Oligo-Miocene reverse faults (Bonardi et al., 2001) associated with shear zones, and iii) post-orogenic extensional, sub-vertical and sub-parallel N-S, NE-SW, and NW-SE, with minor NNE-SSW and E-W, normal faults (upper Miocene and upper Pleistocene-Holocene). At its N and S margins, the Calabride-Peloritane domain is bounded by the Sangineto and Taormina lines.
definition: Il dominio Calabro-Peloritano è un terrane esotico bordato da faglie e posizionato all'intersezione tra l'Appennino Meridionale, ad andamento NO-SE, e quello Sicilide-Magrebide ad andamento E-O. Il dominio è caratterizzato da: i) un basamento cristallino pre-mesozoico con deformazioni duttili (Orogenesi Ercinica), ii) faglie inverse appenniniche dell'Oligo-Miocene (Bonardi et al., 2001) con associate zone di taglio, e iii) faglie normali post-orogeniche, sub-verticali e sub-parallele, ad andamento N-S, NE-SO, e NO-SE, e secondariamente NNE-SSO e E-O (Miocene superiore e Pleistocene superiore-Olocene). Il Dominio Calabro-Peloritano è bordato a nord e sud, rispettivamente, dalla Linea di Sangineto e dalla Linea Taormina. @it
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Italy

Penninic Domain
narrower: Greiner Shear Zone
narrower: Base of the Glockner Nappe System
references: https://data.geoscience.earth/ncl/geoera/ref/4783
type: Concept
created: 2020-10-16T07:56:52.324Z
notation: IT-9902
preferred label: Dominio Pennidico @it
definition: The Penninic domain, part of the Alpine chain, groups the continental and oceanic nappes which issued from the distal European continental margin and Mesozoic ocean, characterized by ductile deformations and Europe-vergent thrust faults, bounding the tectonic windows or separating units, mainly stacked during Paleogene. The domain is marked by a severe Alpine metamorphic overprint with the exception of pre-Alpine klippen.
definition: Il dominio Pennidico, parte della catena alpina, raggruppa falde costituite da unità delle porzioni distali del margine continentale europeo e dell'oceano antistante. Le falde sono caratterizzate da deformazioni duttili e da sovrascorrimenti con vergenza europea, che costituiscono i limiti di finestre tettoniche o di unità tettoniche, prevalentemente impilate durante il Paleogene. Il dominio, con l'eccezione di klippen pre-alpini, è marcato da una forte sovraimpronta metamorfica. @it
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Italy

Austroalpine Domain
narrower: Base of the Ötztal-Bundschuh Nappe System
narrower: Base of the Matrei Nordrahmen Zone Nappe System
references: https://data.geoscience.earth/ncl/geoera/ref/4783
type: Concept
created: 2020-10-16T07:56:52.352Z
notation: IT-9903
preferred label: Dominio Austroalpino @it
definition: The Austroalpine domain, descending from the Africa ocean-facing continental margin, overlies the Penninic domain, as part of the Alpine chain. The faults are boundaries of the main nappes and tectonic windows showing the Penninic domain units. The activity is dated to pre-Late Cretaceous (pre-collisional phase, eoalpine) for the eastern part and to Late Cretaceous-Eocene (collisional, mesoalpine) for the western part.
definition: Il dominio Austroalpino, parte della catena alpina e derivante dal margine continentale africano prossimo all'oceano, ricopre il dominio Pennidico. Le faglie sono i limite delle falde principali e delle finestre tettoniche che mostrano le unità del dominio Pennidico sottostante. L'attività è riferibile alla parte iniziale del Cretacico superiore (fase pre-collisionale, eoalpina) nel settore orientale, e al Cretacico superiore-eocene (fase collisionale, mesoalpina) nel settore occidentale. @it
narrower: fault (IT-0030)
narrower: Gallo Fault
narrower: fault (IT-0048)
narrower: fault (IT-0049)
narrower: fault (IT-0051)
narrower: fault (IT-4189)
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Italy

fault (IT-0049)
alternative label: Jaufen-Passeier Fault System
type: Concept
created: 2020-10-16T07:56:52.464Z
notation: IT-0049
in scheme: Tectonic Boundary Objects in Europe
broader: Austroalpine Domain

Southalpine Domain
references: https://data.geoscience.earth/ncl/geoera/ref/4771
type: Concept
created: 2020-10-16T07:56:52.660Z
notation: IT-9905
preferred label: Dominio Sudalpino @it
definition: The Southalpine domain, as part of the Alpine chain, is characterized by large scale thrusting and folding, mainly E-W and NE-SW trending, with dominant vergence toward south. In addition, extensional faults, antithetic and syntethic mainly NW-SE trending, related to Upper Triassic-Middle Jurassic rifting are preserved within large inverted compressional structures. Some areas still preserve the record of Variscan/Hercynian deformations with limited metamorphic overprint. The compressional activity (post-collisional, neoalpine) started during the Tertiary (Oligocene) and progressively propagated towards the foreland; in the western sector evidences of Cretaceous compressional phases are known. The northern boundary of this domain is represented by the Insubric Fault System.
definition: Il dominio Sudalpino, parte della catena alpina, è caratterizzato da sovrascorrimenti e piegamenti a scala regionale, prevalentemente ad andamento E-O e NE-SO, con vergenza dominante verso sud. Sono inoltre preservate faglie dirette, sintetiche e antitetiche, prevalentemente ad andamento NO-SE, connesse al rifting del Triassico superiore-Giurassico medio, preservate dalle strutture compressive. In alcune aree sono ancora presenti elementi delle deformazioni Varisiche (erciniche) con limitata sovraimpronta metamorfica. L'attività compressiva (post-collisionale, neoalpina) è iniziata durante il Terziario (Oligocene) e progressivamente si è propagata verso l'avampaese; nel settore occidentale sono note evidenze di attività compressiva cretacica. Il limite settentrionale del dominio è rappresentato dal sistema di faglie della Linea Insubrica. @it
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Italy

Sangineto Line
references: https://data.geoscience.earth/ncl/geoera/ref/4765
type: Concept
created: 2020-10-16T07:56:55.747Z
notation: IT-99180
preferred label: Linea di Sangineto @it
definition: The Sangineto Line marks the northern border of the Calabride-Peloritane domain. T the Sangineto line seems to be a complex fault system with a left-lateral strike-slip component (Bonardi et al., 2001).
definition: La Linea di Sangineto marca il bordo settentrionale del Dominio Calabro-Peloritano. Essa si presenta come un complesso sistema di faglie con una componente trascorrente sinistra (Bonardi et al., 2001). @it
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Italy

Hyblean foreland Domain
type: Concept
created: 2020-10-16T07:56:55.663Z
notation: IT-9917
preferred label: Avampaese Ibleo @it
definition: The Hyblean foreland is characterized by sub-parallel normal faults, mainly NE-SW oriented and NW dipping, related to the Mesozoic extensional phase (Patacca et al., 1979; Lentini et al., 1987) and to a Plio-Quaternary collapse as response to the migration of the thrust front. In addition, Plio-Pleistocene NW-SE oriented normal faults and NNE-SSW strike-slip faults, with dextral movement, occur (Ghisetti & Vezzani, 1981; Lentini et al., 1984).
definition: L'avampaese Ibleo è caratterizzato da faglie normali sub-parallele, prevalentemente orientate NE-SO e immergenti a NO, connesse alla fase estensionale mesozoica (Patacca et al., 1979; Lentini et al., 1987) e al collasso plio-quaternario, come risposta alla migrazione del fronte dei sovrascorrimenti. Inoltre, sono presenti faglie normali plio-pleistoceniche orientate NO-SE e faglie trascorrenti destre a orientazione NNE-SSO (Ghisetti & Vezzani, 1981; Lentini et al., 1984). @it
narrower: ﻿Hyblean - Malta Escarpment_02
narrower: ﻿Hyblean - Malta Escarpment_09
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Italy

﻿Hyblean - Malta Escarpment_09
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:55.718Z
notation: IT-6061
preferred label: Scarpata di Malta_09 @it
in scheme: Tectonic Boundary Objects in Europe
broader: Hyblean foreland Domain

﻿Hyblean - Malta Escarpment_02
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:55.691Z
notation: IT-6060
preferred label: Scarpata di Malta_02 @it
in scheme: Tectonic Boundary Objects in Europe
broader: Hyblean foreland Domain

Helvetic Domain
references: https://data.geoscience.earth/ncl/geoera/ref/4783
type: Concept
created: 2020-10-16T07:56:52.296Z
notation: IT-9901
preferred label: Dominio Elvetico @it
definition: The Helvetic domain, part of the Alpine chain, is characterized by Europe-vergent (N and NW) nappes derived from the proximal part of the European continental margin, imbricated from the Oligocene onwards.
definition: Il dominio Elvetico, parte della catena alpina, è caratterizzato da una vergenza europea (N e NO) delle falde derivanti dalle porzioni prossimali del margine continentale europeo, impilate a partire dall'Oligocene. @it
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Italy

Apulia foreland Domain
references: https://data.geoscience.earth/ncl/geoera/ref/4797
references: https://data.geoscience.earth/ncl/geoera/ref/4780
type: Concept
created: 2020-10-16T07:56:54.375Z
notation: IT-9912
preferred label: Avampaese Apulo @it
definition: The Apulia foreland domain represents the outcropping portion of the Southern Apennines foreland. This structural domain is characterized by NW-SE striking normal faults linked to the early Middle Pleistocene flexural tectonics and to the following Middle–Upper Pleistocene extensional tectonics. These faults affected mainly the foreland buried below the front of the chain and below the foredeep deposits. The outcropping Apulia sector (Apulia foreland) exhibits a regional pattern of large scale deformation which is manifested through a system of NW-SE extensional structures affecting both its smoothly flexure along the contact with the Bradanic foredeep and its eastern sector; locally minor striking NE-SW normal faults are also present. The northern border of this structural Domain is marked by the E-W trending Mattinata fault and in general by the Gargano Fault System.
definition: Il dominio dell'Avampaese Apulo rappresenta la porzione affiorante dell'avampaese dell'Appennino Meridionale. Questo dominio strutturale è caratterizzato da faglie normali a direzione NO-SE connesse alla flessurazione dell'inizio del Pleistocene medio e alla seguente tettonica estensionale del Pleistocene medio-superiore. Queste faglie coinvolgono prevalentemente l'avampaese sepolto sotto il fronte della catena e dai depositi di avanfossa. Il settore affiorante mostra un reticolo di deformazioni a larga scala manifestate da un sistema di strutture estensionali NO-SE che coinvolgono sia la zona interna, al margine della Fossa Bradanica, sia il settore orientale; localmente sono presenti faglie normali minori a direzione NE-SO. Il bordo settentrionale di questo dominio strutturale è marcato dalla faglia di Mattinata, ad andamento E-O, e in generale dal Sistema di faglie Gargano. @it
narrower: Gargano Fault System
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Italy

Gargano Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/4798
references: https://data.geoscience.earth/ncl/geoera/ref/4790
type: Concept
created: 2020-10-16T07:56:54.402Z
notation: IT-99120
preferred label: Sistema di faglie del Gargano @it
definition: The Gargano Fault System characterizes the Gargano Promontory, that represents the northern portion of the Apulian foreland emerging from the Adriatic Sea. The promontory shows E-W elongated anticline morphology and it is affected by NW-SE and E-W trending main faults and by NE-SW trending minor faults. The major structure is the E-W trending, south dipping, Mattinata Fault cutting cross the southern border of the Gargano Promontory (Funiciello et al., 1988). Many Authors suggest that the Gargano faults might have experienced different activity and different sense of motion in different tectonic regimes and they propose a multi-phase kinematics (Patacca & Sacandone, 2004 and references therein). Major evidences are in favour for a dextral strike slip kinematics along the Mattinata Fault from Late Pliocene to the present (Piccardi, et al., 2004).
definition: Il sistema di faglie del Gargano caratterzza il promontorio del Gargano, che rappresenta la porzione settentrionale dell'avampaese Apulo. Il promontorio è caratterizzato da un'anticlinale allungata in direzione E-O, interessata da faglie principali ad andamento NO-SE ed E-O, e da faglie minori NE-SO. La struttura maggiore, denominata faglia di Mattinata, ha andamento E-O immergente verso sud, e taglia il borso meridionale del promontorio del Gargano (Funiciello et al., 1988). Diversi autori hanno ipotizzato che le faglie del sistema siano state interessate da diverse fasi di attività e da differente tipo di movimento, in diversi regimi tettonici; essi hanno proposto una cinematica multifase (Patacca & Sacandone, 2004 e bibliografia associata). Le maggiori eveidenze sono a favore di cinematica trascorrente destra per la faglia di Mattinata a partire dal Pliocene superiore fino ad oggi (Piccardi, et al., 2004). @it
in scheme: Tectonic Boundary Objects in Europe
broader: Apulia foreland Domain

Etna volcano Domain
references: https://data.geoscience.earth/ncl/geoera/ref/4766
references: https://data.geoscience.earth/ncl/geoera/ref/4787
type: Concept
created: 2020-10-16T07:56:55.914Z
notation: IT-9922
preferred label: Dominio dell'Etna @it
definition: The Etna volcano, in eastern Sicily, is the largest and most active stratovolcano in Europe. Its eruptive activity started during the middle Pleistocene on the structural domain of the Gela– Catania Foredeep in the front of the the Apennine–-Maghrebian thrust belt at the intersection of two active regional master faults, the Hyblean–Malta Escarpment and the Messina–Fiumefreddo line (Branca et al., 2011). The Etna structural setting represents the result of the interaction of regional tectonics, volcano-tectonic processes and local scale volcano-related and gravitative processes (Lo Giudice et al., 1982). The northern termination of the Malta Escarpment dissects the base of the eastern flank of Etna volcano through a set of NNW–SSE normal faults called Timpe fault system (Lo Giudice et al. 1982). The most active faults in this system are the Moscarello, San Leonardello and Acireale faults. The E-W trending Pernicana-Fiumefreddo fault system and the NW-SE trending Tremestieri and Trecastagni faults represent the northern and the southern border of a sliding sector. Both these faults systems are characterized by seismic and aseismic (creep) activity.
definition: L'Etna, nella Sicilia orientale, è il più grande e attivo strato-vulcano in Europa. La sua attività eruttiva è iniziata durante il Pleistocene medio sul dominio dell'Avanfossa Gela-Catania, di fronte alla catena Appenninico-Magrebide e all'intersezione di due faglie attive di importanza regionale, la Scarpata Ibleo-Maltese e la linea Messina-Fiumefreddo (Branca et al., 2011). L'assetto strutturale dell'Etna è il risultato dell'interazione della tettonica regionale, dei processi vulcano-tettonici e di processi locali connessi al vulcano e alla gravità (Lo Giudice et al., 1982). La terminazione settentrionale della Scarpata Ibleo-Maltese taglia la base del fianco orientale del vulcano attraverso una serie di faglie normali, ad andamento NNO-SSE, chiamate Sistema delle Timpe (Lo Giudice et al. 1982). La faglie più attive del sistema sono Moscarello, San Leonardello e Acireale. Il Sistema Pernicana-Fiumefreddo, ad andamento E-O, e le faglie Tremestieri eTrecastagni, ad andamento NO-SE, rappresentano i bordi settentrionale e meridionale di un settore in scivolamento. Entrambi questi sistemi sono caratterizzati da attività sismica e asismica (creep). @it
narrower: Acireale fault
narrower: Guardia fault
narrower: Gurna fault
narrower: Guzzi fault
narrower: Macchia - Stazzo fault
narrower: Massa Annunziata fault
narrower: Moscarello fault
narrower: Nicolosi fault
narrower: Pernicana fault
narrower: Pernicana_05 fault
narrower: Pernicana_16 fault
narrower: Provenzana fault
narrower: San Giovanni Bosco fault
narrower: San Leonardello fault
narrower: Sant'Alfio fault
narrower: Santa Maria la Scala fault
narrower: Santa Tecla - Linera fault
narrower: Santa Tecla - Santa Venerina fault
narrower: Santa Tecla fault
narrower: Santa Venera fault
narrower: Santa Venera_01 fault
narrower: Santa Venera_02 fault
narrower: Trecastagni fault
narrower: Tremestieri fault
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Italy

Nicolosi fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:56.139Z
notation: IT-6070
in scheme: Tectonic Boundary Objects in Europe
broader: Etna volcano Domain

Santa Tecla fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:56.445Z
notation: IT-6081
in scheme: Tectonic Boundary Objects in Europe
broader: Etna volcano Domain

Pernicana fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:56.166Z
notation: IT-6071
in scheme: Tectonic Boundary Objects in Europe
broader: Etna volcano Domain

Massa Annunziata fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:56.082Z
notation: IT-6068
in scheme: Tectonic Boundary Objects in Europe
broader: Etna volcano Domain

Santa Tecla - Linera fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:56.389Z
notation: IT-6079
in scheme: Tectonic Boundary Objects in Europe
broader: Etna volcano Domain

Moscarello fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:56.111Z
notation: IT-6069
in scheme: Tectonic Boundary Objects in Europe
broader: Etna volcano Domain

Santa Tecla - Santa Venerina fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:56.417Z
notation: IT-6080
in scheme: Tectonic Boundary Objects in Europe
broader: Etna volcano Domain

Guzzi fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:56.026Z
notation: IT-6066
in scheme: Tectonic Boundary Objects in Europe
broader: Etna volcano Domain

Sant'Alfio fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:56.334Z
notation: IT-6077
in scheme: Tectonic Boundary Objects in Europe
broader: Etna volcano Domain

Macchia - Stazzo fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:56.054Z
notation: IT-6067
in scheme: Tectonic Boundary Objects in Europe
broader: Etna volcano Domain

Santa Maria la Scala fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:56.361Z
notation: IT-6078
in scheme: Tectonic Boundary Objects in Europe
broader: Etna volcano Domain

Guardia fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:55.970Z
notation: IT-6064
in scheme: Tectonic Boundary Objects in Europe
broader: Etna volcano Domain

San Giovanni Bosco fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:56.279Z
notation: IT-6075
in scheme: Tectonic Boundary Objects in Europe
broader: Etna volcano Domain

Tremestieri fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:56.584Z
notation: IT-6086
in scheme: Tectonic Boundary Objects in Europe
broader: Etna volcano Domain

Gurna fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:55.998Z
notation: IT-6065
in scheme: Tectonic Boundary Objects in Europe
broader: Etna volcano Domain

San Leonardello fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:56.306Z
notation: IT-6076
in scheme: Tectonic Boundary Objects in Europe
broader: Etna volcano Domain

Pernicana_16 fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:56.223Z
notation: IT-6073
in scheme: Tectonic Boundary Objects in Europe
broader: Etna volcano Domain

Santa Venera_02 fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:56.528Z
notation: IT-6084
in scheme: Tectonic Boundary Objects in Europe
broader: Etna volcano Domain

Acireale fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:55.941Z
notation: IT-6063
in scheme: Tectonic Boundary Objects in Europe
broader: Etna volcano Domain

Provenzana fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:56.250Z
notation: IT-6074
in scheme: Tectonic Boundary Objects in Europe
broader: Etna volcano Domain

Trecastagni fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:56.556Z
notation: IT-6085
in scheme: Tectonic Boundary Objects in Europe
broader: Etna volcano Domain

Santa Venera fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:56.473Z
notation: IT-6082
in scheme: Tectonic Boundary Objects in Europe
broader: Etna volcano Domain

Pernicana_05 fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:56.194Z
notation: IT-6072
in scheme: Tectonic Boundary Objects in Europe
broader: Etna volcano Domain

Santa Venera_01 fault
references: https://data.geoscience.earth/ncl/geoera/ref/4801
type: Concept
created: 2020-10-16T07:56:56.500Z
notation: IT-6083
in scheme: Tectonic Boundary Objects in Europe
broader: Etna volcano Domain

Catania-Gela foredeep Domain
references: https://data.geoscience.earth/ncl/geoera/ref/4775
references: https://data.geoscience.earth/ncl/geoera/ref/4776
type: Concept
created: 2020-10-16T07:56:55.635Z
notation: IT-9916
preferred label: Avanfossa Catania-Gela @it
definition: The Catania-Gela Foredeep domain extends between the front of the Apenninic-Maghrebides Belt and the Hyblean Plateau (foreland). The depression starts developing in the Late Pliocene from the inflection of the carbonate substrate related also to the frontal nappe loading (Catalano et al., 1993). The north-western sector the Catania-Gela Foredeep is fully occupied by the allochthonous units of the frontal wedge of the chain, the Gela Nappe, of which the S and SE verging front represents the main structural feature. A system of NE-SW trending normal faults identifies its south-eastern border and the separation with the Hyblean Foreland domain, partially flexured below the foredeep. Minor extensional elements mainly NE-SW striking locally deform the Upper Pliocene-Pleistocene sedimentary succession.
definition: Il Dominio di avanfossa Catania-Gela si estende tra il fronte della catena Appenninico-Magrebide e il Plateau Ibleo (avampaese). Lo sviluppo della depressione è iniziato nel Pliocene superiore, a partire dall'inflessione del substrato carbonatico connessa anche al carico delle falde frontali (Catalano et al., 1993). Il settore nord-occidentale dell'avanfossa Catania-Gela è completamente occupato da unità alloctone del cuneo frontale della catena (Falda di Gela) le cui strutture principali sono S- e SE-vergenti. Un sistema di faglie normali a direzione NE-SO identifica il suo bordo sudorientale e la separazione con il dominio dell'Avampaese Ibleo, parzialmente flessurato sotto l'avanfossa. Elementi estensionali minori, prevalentemente a direzione NE-SO, deformano la successione sedimentaria del Pliocene superiore-Pleistocene. @it
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Italy

Southern Apennines Domain
references: https://data.geoscience.earth/ncl/geoera/ref/4799
references: https://data.geoscience.earth/ncl/geoera/ref/4794
type: Concept
created: 2020-10-16T07:56:54.319Z
notation: IT-9910
preferred label: Dominio Appennino meridionale @it
definition: The Southern Apennines Domain developed through the deformation of the thinned oceanic-transitional to continental crust of the Liguria-Piedmont Ocean and the Africa continental passive margin, starting in the Late Cretaceous. The accretion of the fold-and-thrust belt is strictly linked to the continental collision and post-collisional activity, ranging from late Oligocene to early Pleistocene, with eastward migration of the deformation and piling and out-of-sequence thrusting. The Southern Apennine mountain chain is formed by a deep-seated carbonate duplex system tectonically overlain by a thick pile of NE-verging rootless nappes derived from basin and platform domains (Patacca & Scandone, 2007). Each tectonic-sedimentary unit (nappe) is bordered by major thrusts or, more frequently, by a group of thrusts. The internal nappe geometry is complicated by second order of folds and thrusts mainly NE-verging. In addition, some allochthonous unit, locally placed up as gravitative flows, constitute the easternmost and more advanced thrust sheets outcropping in the Southern Apennines.This complex NE-verging thrust belt developed during Neogene and Quaternary times along the eastward-retreating west-directed subduction of the Apulo-Adriatic lithosphere (Scrocca, 2010 ).
definition: Il Dominio Appennino Meridionale si è sviluppato attraverso la deformazione di crosta assottigliata oceanica e di transizione dell'Oceano Ligure-Piemontese e del margine continentale passivo africano, a partire dal Cretacico superiore. L'accrezione della catena a pieghe e sovrascorrimenti è strettamente connessa alla collisione continentale e alle fasi post-collisionali, nell'intervallo Oligocene superiore - Pleistocene inferiore, con migrazione verso est della deformazione e dell'impilamento, con sovrascorrimenti fuori sequenza. La catena dell'Appennino Meridionale è formata da un sistema radicato nei carbonati e raddoppiato, tettonicamente sovrascorso da una potente pila di falde scollate, NE vergenti, derivate da domini di bacino e piattaforma (Patacca & Scandone, 2007). Ciascuna unità tettono-sedimentaria (falda) è bordata da sovrascorrimenti principali o, più frequentemente, da più sovrascorrimenti. La geometria interna delle falde è complicata da pieghe e sovrascorrimenti di secondo ordine, prevalentemente vergenti a NE. Inoltre, alcune unità alloctone, localemente messe in posto come colate gravitative, costituiscono gli elementi più orientali ed esterni affiornati nell'Appennino Meridionale. Questa complessa catena NE vergente si è sviluppata durante il Neogene e il Quaternario lungo la zona di subduzione della litosfera Apulo-Adriatica in arretramento verso est (Scrocca, 2010 ). @it
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Italy

Bradanic Trough Domain
references: https://data.geoscience.earth/ncl/geoera/ref/4770
references: https://data.geoscience.earth/ncl/geoera/ref/4788
type: Concept
created: 2020-10-16T07:56:54.347Z
notation: IT-9911
preferred label: Fossa Bradanica @it
definition: The Bradanic Trough represents the Pliocene-present-day southern Apennines foredeep. It is a NW-SE elongated foreland basin separating the Apennine chain from the Apulia foreland. This flexural depression developed at the front of the Apennine thrust belt and have been filled by Pliocene-Pleistocene deposits. This domain is mainly characterized by the presence of NW-SE trending E-verging thrusts due to the involvement in the Apennines thrust front deformation or to the Apennine blind thrust propagation. At same time, syn-depositional extensional structures are present as a results of the propagation of the deep extensional tectonic pattern affecting the buried foreland
definition: La Fossa Bradanica rappresenta l'avanfossa dell'Appennino Meridionale a partire dal Pliocene fino a oggi. Si tratta di un bacino allungato NO-SE, che separa la catena appenninica dall'avampaese Apulo. Questa depressione flessurale si è sviluppata al fronte della catena ed è stata colmata da sedimenti plio-pleistocenici. Il dominio è caratterizzato prevalentemente da sovrascorrimenti ad andamento NO-SE, E vergenti, connessi all'avanzata del fronte della catena o alla propagazione di sovrascorrimenti ciechi. Allo stesso tempo, sono presenti strutture estensionali sindeposizionali risultato della propagazione di strutture estensionali profonde e sepolte che coinvolgono l'avampaese. @it
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Italy

Tectonic Boundary in Poland
narrower: Southern segment of the Trans-European Suture Zone
narrower: Upper Sileasian fault zones
narrower: Lower Silesian fault systems and zones
narrower: Inner Carpathians
scope note: All named tectonic boundary objects that are located (at least partly) in Poland, are identified by an ID with the prefix „PL“ listed in the notation. Fault systems and/or fault domains can cross political borders and are therefore shared by several countries. Therefore, they can contain faults from different countries, indicated by country-specific prefixes to the respective ID.
definition: Fault in Poland displayed on the European HIKE fault database.
narrower: Northern segment of the Trans-European suture zone
type: Concept
top concept of: Tectonic Boundary Objects in Europe
created: 2021-03-03T16:08:15.409Z
preferred label: Granice tektoniczne w Polsce @pl
narrower: East European Craton (tectonic megadomain)
in scheme: Tectonic Boundary Objects in Europe
notation: PL-0

Inner Carpathians
type: Concept
created: 2021-03-03T16:08:15.888Z
definition: Inner Carpathians are constituted by the cristalline basement and overthrusted sedimentary nappes of the Tatras, Podhale flysh basin and the Pieniny Klippen Belt.
definition: Karpaty wewnętrze obejmują krystaliczne podłoże I fałdowo-płaszczowinową pokrywę osadową Tatr, fliszowe Podhale oraz Pieniński Pas Skałkowy. @pl
preferred label: Karpaty wewnętrzne @pl
narrower: Pieniny Klippen Belt
narrower: Podhale synclinorium
references: https://data.geoscience.earth/ncl/geoera/ref/8125
in scheme: Tectonic Boundary Objects in Europe
notation: PL-60000000
broader: Tectonic Boundary in Poland

Podhale synclinorium
type: Concept
created: 2021-03-03T16:08:15.896Z
definition: Palaeogene flysh basin in front of the Tatra Mountains, overlying ALCAPA basement.
definition: Fliszowy basen przedgórski Tatr, rozwinięty na mikropłycie ALCAPA. @pl
preferred label: Synklinorium podhalańskie @pl
narrower: Biały Dunajec fault zone
narrower: Białka fault
references: https://data.geoscience.earth/ncl/geoera/ref/8073
in scheme: Tectonic Boundary Objects in Europe
notation: PL-62000000
broader: Inner Carpathians

Białka fault
type: Concept
created: 2021-03-03T16:08:15.903Z
definition: The system of discrete faults in the dextral strike-slip fault zone. Probably deeply rooted and reactivated in the Miocene. In morphology forming the Białka river valley. Method of observation: surface observation, geological mapping. (Country Report fault code: F-3)
definition: System uskoków w strefie uskoku prawoprzesuwczego. Prawdopodobnie zakorzeniony głęboko i reaktywowany w miocenie. W morfologii wykorzystany przez dolinę Białki. Metody obserwacji: odsłonięcia, kartowanie geologiczne. (Kod uskoku w Raporcie krajowym projektu HIKE: F-3) @pl
preferred label: Uskok Białki @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8072
in scheme: Tectonic Boundary Objects in Europe
notation: PL-62020000
broader: Podhale synclinorium

Biały Dunajec fault zone
type: Concept
created: 2021-03-03T16:08:15.900Z
definition: The system of discrete faults in the sinistral strike-slip fault zone. Probably deeply rooted and reactivated in the Miocene. In morphology forming the Biały Dunajec river valley. Method of observation: surface observation, geological mapping. (Country Report fault code: F-2)
definition: System uskoków w strefie uskoku lewoprzesuwczego. Prawdopodobnie zakorzeniony głęboko w podłożu i reaktywowany w miocenie. W morfologii wykorzystany przez dolinę Białego Dunajca. Metody obserwacji: odsłonięcia, kartowanie geologiczne. (Kod uskoku w Raporcie krajowym projektu HIKE: F-2) @pl
preferred label: Strefa uskokowa Białego Dunajca @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8073
in scheme: Tectonic Boundary Objects in Europe
notation: PL-62010000
broader: Podhale synclinorium

Pieniny Klippen Belt
type: Concept
created: 2021-03-03T16:08:15.891Z
definition: A major suture zone coming from the Alps all along the Carpathian chain, forming the boundary between ALCAPA, to the S, and the Eurasian plate, to the N. Created during ALCAPA accretion in the Neogene. Perfectly recognized by geological mapping and recorded by geophysical methods. Recent seismic activity is marked by the strike-slip kinematics. Described structure is a border of Inner and Outer Carpathians. Method of observation: surface observation, geological mapping, geophysics. Strike: W–E in the study area. (Country Report fault code: F-1)
definition: Strefa szwu tektonicznego, ciągnąca się od Alp wzdłuż całego łańcucha karpackiego, tworząca granicę między mikropłytą ALCAPA na południu i płytą euroazjatycką na północy. Powstała w neogenie podczas akrecji mikropłyty ALCAPA. Doskonale rozpoznana w trakcie kartowania geologicznego i rejestrowana metodami geofizycznymi. Współczesna aktywność sejsmiczna ma kinematykę przesuwczą. Opisana struktura wyznacza granicę Karpat Wewnętrznych i Zewnętrznych. Metody obserwacji: odsłoniecia, kartowanie geologiczne, geofizyka. Bieg: W–E w badanym obszarze. (Kod uskoku w Raporcie krajowym projektu HIKE: F-1) @pl
preferred label: Pieniński Pas Skałkowy @pl
references: https://data.geoscience.earth/ncl/geoera/ref/7997
references: https://data.geoscience.earth/ncl/geoera/ref/8046
references: https://data.geoscience.earth/ncl/geoera/ref/8056
in scheme: Tectonic Boundary Objects in Europe
notation: PL-61000000
broader: Inner Carpathians

East European Craton (tectonic megadomain)
references: https://data.geoscience.earth/ncl/geoera/ref/8125
references: https://data.geoscience.earth/ncl/geoera/ref/8024
narrower: Mazowsze tectonic domain
narrower: Podlasie–Bielarus Granulite Belt
narrower: Mazury Complex
narrower: Lublin Basin
narrower: Płock Trough
type: Concept
created: 2021-03-03T16:08:15.412Z
definition: Megadomena tektoniczna zajmująca północno-wschodnią część Polski (i północno-wschodnią Europę), czyli polski fragment kratonu wschodnioeuropejskiego, składający się z podłoża krystalicznego (skał paleo- i mezoproterozoicznych), pokrywy osadowej skał neoproterozoicznych, paleozoicznych i mezozoicznych oraz uskoków przecinających tę domenę. @pl
preferred label: Kraton wschodnioeuropejski @pl
alternative label: East European Craton
narrower: Pomorze–Blekinge Belt
definition: Tectonic megadomain occupying the NE half of Poland (and the NE half of Europe), i.e. the Polish fragment of the East European Craton, consisting of Paleo- and Mezoproterozoic crystalline basement and Neoproterozoic, Palaeozoic and Mezozoic cover and faults cross-cutting this domain.
in scheme: Tectonic Boundary Objects in Europe
notation: PL-10000000
broader: Tectonic Boundary in Poland

Mazowsze tectonic domain
references: https://data.geoscience.earth/ncl/geoera/ref/8058
type: Concept
created: 2021-03-03T16:08:15.466Z
definition: Tectonic boundary defined on the basis of regional magnetic and gravimetric anomalies pattern.
definition: Granica tektoniczna wyznaczona na podstawie regionalnych anomalii magnetycznych i grawimetrycznych. @pl
preferred label: Domena mazowiecka @pl
narrower: Mazowsze fault zone
in scheme: Tectonic Boundary Objects in Europe
notation: PL-12000000
broader: East European Craton (tectonic megadomain)

Mazowsze fault zone
references: https://data.geoscience.earth/ncl/geoera/ref/8121
references: https://data.geoscience.earth/ncl/geoera/ref/8036
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-03-03T16:08:15.470Z
definition: Y-shaped magnetic and gravimetric anomalies north of the TTZ, central Poland, close to Mława syenite intrusion. Method of observation: magnetic anomaly map, seismic profiles. Strike: NW–SE. (Country Report fault code: A-8)
definition: Anomalie magnetyczne i grawimetryczne w kształcie litery Y na północ od TTZ, środkowa Polska, w pobliżu intruzji sjenitowej Mławy. Metoda obserwacji: mapa anomalii magnetycznej, profile sejsmiczne. Bieg: NW–SE. (Kod uskoku w Raporcie krajowym projektu HIKE: A-8) @pl
preferred label: Strefa uskokowa Mazowsza @pl
notation: PL-12010000
broader: Mazowsze tectonic domain

Pomorze–Blekinge Belt
references: https://data.geoscience.earth/ncl/geoera/ref/8058
narrower: Kuźnica fault zone
narrower: Sambia fault zone
narrower: Żarnowiec fault zone
type: Concept
created: 2021-03-03T16:08:15.418Z
definition: Nasunięcie / granica tektoniczna określona na podstawie regionalnych anomalii magnetycznych i grawimetrycznych. @pl
preferred label: Pasmo Pomorze–Blekinge @pl
alternative label: Pomorze–Blekinge border
narrower: Darłowo fault zone
narrower: Ustka fault zone
narrower: Smołdzino fault zone
narrower: Łeba fault zone
definition: Nappe / tectonic boundary defined on the basis of regional magnetic and gravimetric anomalies pattern.
narrower: Karwia fault zone
in scheme: Tectonic Boundary Objects in Europe
notation: PL-11000000
broader: East European Craton (tectonic megadomain)

Żarnowiec fault zone
references: https://data.geoscience.earth/ncl/geoera/ref/8010
references: https://data.geoscience.earth/ncl/geoera/ref/8008
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-03-03T16:08:15.462Z
definition: System uskoków definiowany na podstawie segmentacji bloków podłoża i przekroju sejsmicznego. @pl
preferred label: Strefa uskokowa Żarnowca @pl
definition: Fault system defined on the basis segmentation of basement blocks and seismic cross section.
notation: PL-11080000
broader: Pomorze–Blekinge Belt

Sambia fault zone
references: https://data.geoscience.earth/ncl/geoera/ref/8013
references: https://data.geoscience.earth/ncl/geoera/ref/7999
references: https://data.geoscience.earth/ncl/geoera/ref/8010
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-03-03T16:08:15.458Z
definition: Basement fault zone reactivated during Early Palaeozoic and recently seismically active (2004 earthquakes with max. mag. M5.3) Method of observation: seismic profiles, borehole data, seismic events. (Country Report fault code: A-7)
definition: Strefa uskokowa podłoża reaktywowana we wczesnym paleozoiku, ostatnio aktywna sejsmicznie (trzęsienia ziemi w 2004 r. maksymalna Mag. M5.3) Metoda obserwacji: profile sejsmiczne, dane z otworów wiertniczych, zdarzenia sejsmiczne. (Kod uskoku w Raporcie krajowym projektu HIKE: A-7) @pl
preferred label: Strefa uskokowa Sambii @pl
notation: PL-11070000
broader: Pomorze–Blekinge Belt

Kuźnica fault zone
references: https://data.geoscience.earth/ncl/geoera/ref/8010
references: https://data.geoscience.earth/ncl/geoera/ref/8013
references: https://data.geoscience.earth/ncl/geoera/ref/8093
references: https://data.geoscience.earth/ncl/geoera/ref/8106
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-03-03T16:08:15.453Z
definition: This fault is deeply rooted in the Proterozoic basement and reactivated after Devonian. Method of observation: seismic profiles, magneto telluric. Strike: N–S. (Country Report fault code: A-6)
definition: Uskok głęboko zakorzeniony w podłożu proterozoicznym, reaktywowany po dewonie. Metody obserwacji: profile sejsmiczne, magnetotelluryka. Bieg: N–S. (Kod uskoku w Raporcie krajowym projektu HIKE: A-6) @pl
preferred label: Strefa uskokowa Kuźnicy @pl
notation: PL-11060000
broader: Pomorze–Blekinge Belt

Karwia fault zone
references: https://data.geoscience.earth/ncl/geoera/ref/8013
references: https://data.geoscience.earth/ncl/geoera/ref/7999
in scheme: Tectonic Boundary Objects in Europe
created: 2021-03-03T16:08:15.449Z
definition: Uskok w podłożu (?) reaktywowany po dewonie, prawdopodobnie w okresie waryscyjskim. W podkenozoicznym pietrze strukturalnym obserwuje się znaczącą zmienność po przeciwnych stronach tej strefiy uskokowej. Metody obserwacji: profile sejsmiczne, dane z otworów wiertniczych. Bieg: N–S. (Kod uskoku w Raporcie krajowym projektu HIKE: A-5) @pl
preferred label: Strefa uskokowa Karwii @pl
type: Concept
definition: Basement(?) fault reactivated after Devonian, probably during Variscan stage. Significant changes in sub-Cenozoic structural level is observed across this fault zone. Method of observation: seismic profiles, borehole data. Strike: N–S. (Country Report fault code: A-5)
notation: PL-11050000
broader: Pomorze–Blekinge Belt

Łeba fault zone
references: https://data.geoscience.earth/ncl/geoera/ref/8010
references: https://data.geoscience.earth/ncl/geoera/ref/8013
references: https://data.geoscience.earth/ncl/geoera/ref/8093
references: https://data.geoscience.earth/ncl/geoera/ref/8106
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-03-03T16:08:15.437Z
definition: Fault zone parallels the TTZ, deeply rooted in the Proterozoic basement, and reactivated in the Palaeozoic and end Creataceous times. Method of observation: seismic profiles, magneto telluric. Strike: NW-SE. (Country Report fault code: A-4)
definition: Strefa uskokowa równoległa do TTZ, głęboko zakorzeniona w podłożu proterozoicznym, reaktywowana w paleozoiku i późnej kredzie. Metody obserwacji: profile sejsmiczne, magnetotelluryka. Bieg: NW–SE. (Kod uskoku w Raporcie krajowym projektu HIKE: A-4) @pl
preferred label: Strefa uskokowa Łeby @pl
narrower: Łeba fault zone 1
narrower: Łeba fault zone 2
notation: PL-11040000
broader: Pomorze–Blekinge Belt

Łeba fault zone 2
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-03-03T16:08:15.446Z
notation: PL-11040002
broader: Łeba fault zone

Łeba fault zone 1
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-03-03T16:08:15.442Z
notation: PL-11040001
broader: Łeba fault zone

Smołdzino fault zone
references: https://data.geoscience.earth/ncl/geoera/ref/8010
references: https://data.geoscience.earth/ncl/geoera/ref/8013
references: https://data.geoscience.earth/ncl/geoera/ref/8093
references: https://data.geoscience.earth/ncl/geoera/ref/8106
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-03-03T16:08:15.431Z
definition: Fault zone parallels the TTZ, deeply rooted in the Proterozoic basement and reactivated in Palaeozoic. Method of observation: seismic profiles, magneto telluric. Strike: N–S. (Country Report fault code: A-3)
definition: Strefa uskokowa równoległa do TTZ, głęboko zakorzeniona w podłożu proterozoicznym, reaktywowana w paleozoiku. Metody obserwacji: profile sejsmiczne, magnetotelluryka. Bieg: N–S. (Kod uskoku w Raporcie krajowym projektu HIKE: A-3) @pl
preferred label: Strefa uskokowa Smołdzina @pl
notation: PL-11030000
broader: Pomorze–Blekinge Belt

Ustka fault zone
references: https://data.geoscience.earth/ncl/geoera/ref/8010
references: https://data.geoscience.earth/ncl/geoera/ref/8013
references: https://data.geoscience.earth/ncl/geoera/ref/8093
references: https://data.geoscience.earth/ncl/geoera/ref/8106
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-03-03T16:08:15.426Z
definition: Fault zone parallels the TTZ, deeply rooted in the Proterozoic basement and reactivated in Palaeozoic and, slightly, later. Method of observation: seismic profiles, magneto telluric. Strike: NW–SE. (Country Report fault code: A-2)
definition: Strefa uskokowa równoległa do TTZ, głęboko zakorzeniona w podłożu proterozoicznym, reaktywowana w paleozoiku, a także później. Metody obserwacji: profile sejsmiczne, magnetotelluryka. Bieg: NW–SE. (Kod uskoku w Raporcie krajowym projektu HIKE: A-2) @pl
preferred label: Strefa uskokowa Ustki @pl
notation: PL-11020000
broader: Pomorze–Blekinge Belt

Darłowo fault zone
references: https://data.geoscience.earth/ncl/geoera/ref/8010
references: https://data.geoscience.earth/ncl/geoera/ref/8013
references: https://data.geoscience.earth/ncl/geoera/ref/8093
references: https://data.geoscience.earth/ncl/geoera/ref/8106
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-03-03T16:08:15.421Z
definition: Fault zone parallels the TTZ, deeply rooted in the Proterozoic basement and reactivated in the Palaeozoic and end Creataceous times. Method of observation: seismic profiles, magneto telluric. Strike: NW–SE. (Country Report fault code: A-1)
definition: Strefa uskokowa równoległa do TTZ, głęboko zakorzeniona w podłożu proterozoicznym, reaktywowana w paleozoiku i późnej kredzie. Metody obserwacji: profile sejsmiczne, magnetotelluryka. Bieg: NW–SE. (Kod uskoku w Raporcie krajowym projektu HIKE: A-1) @pl
preferred label: Strefa uskokowa Darłowa @pl
notation: PL-11010000
broader: Pomorze–Blekinge Belt

Mazury Complex
references: https://data.geoscience.earth/ncl/geoera/ref/8024
type: Concept
created: 2021-03-03T16:08:15.497Z
definition: Tectono-metamorphic unit of the East European Craton forming a 200 km long and 40 km wide zone of of granitoids and anorthosite /norite massifs and associated faults, that crosscuts the granulite and amphibolite facies domains in NE Poland.
definition: Jednostka tektoniczno-metamorficzna kratonu wschodnioeuropejskiego tworząca strefę granitoidów i masywy anortozytowe / norytowe o długości 200 km i szerokości 40 km przecinającą domeny facji granulitowych I amfibolitowych w północno-wschodniej Polsce. @pl
preferred label: Kompleks mazurski @pl
narrower: Mazury fault zone
in scheme: Tectonic Boundary Objects in Europe
notation: PL-14000000
broader: East European Craton (tectonic megadomain)

Mazury fault zone
references: https://data.geoscience.earth/ncl/geoera/ref/8059
references: https://data.geoscience.earth/ncl/geoera/ref/8121
references: https://data.geoscience.earth/ncl/geoera/ref/7998
references: https://data.geoscience.earth/ncl/geoera/ref/8036
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-03-03T16:08:15.501Z
definition: A regional E–W trending lineament in northern Poland and southern Lithuania detected by magnetic and gravimetric mapping. Method of observation: magnetic anomaly map, seismic profiles. Strike: WNW–ESE. (Country Report fault code: A-10)
definition: Reginalny lineament E–W w północnej Polsce i południowej Litwie wykryty za pomocą badań magnetycznych i grawimetrycznych. Metoda obserwacji: mapa anomalii magnetycznej, profile sejsmiczne. Bieg: WNW – ESE. (Kod uskoku w Raporcie krajowym projektu HIKE: A-10) @pl
preferred label: Mazurska strefa uskokowa @pl
narrower: Mazury fault 1
narrower: Mazury fault 2
narrower: Mazury fault 3
notation: PL-14010000
broader: Mazury Complex

Mazury fault 1
type: Concept
created: 2021-03-03T16:08:15.506Z
in scheme: Tectonic Boundary Objects in Europe
notation: PL-14010001
broader: Mazury fault zone

Mazury fault 3
type: Concept
created: 2021-03-03T16:08:15.512Z
in scheme: Tectonic Boundary Objects in Europe
notation: PL-14010003
broader: Mazury fault zone

Mazury fault 2
type: Concept
created: 2021-03-03T16:08:15.509Z
in scheme: Tectonic Boundary Objects in Europe
notation: PL-14010002
broader: Mazury fault zone

Płock Trough
references: https://data.geoscience.earth/ncl/geoera/ref/8069
type: Concept
created: 2021-03-03T16:08:15.561Z
definition: The Płock trough is located over the slope of the pre-Vendian East European Platform and the Teisseyre-Tornquist tectonic zone. It developed in its present form at the turn of the Cretaceous and Tertiary but its basement, especially the segmentation of underlying platform sediments, reveal older roots.
definition: Niecka Płocka położona na skłonie przedwendyjskiej platformy wschodnioeuropejskiej i strefy tektonicznej Teisseyre-Tornquista. Obecny kształt niecki powstał na przełomie kredy i trzeciorzędu. Podłoże niecki, zwłaszcza tektoniczna segmentacja niżej leżących osadów pokrywy platformowej, ujawnia starsze korzenie. @pl
preferred label: Niecka płocka @pl
narrower: Żuromin–Płońsk fault zone
in scheme: Tectonic Boundary Objects in Europe
notation: PL-16000000
broader: East European Craton (tectonic megadomain)

Żuromin–Płońsk fault zone
references: https://data.geoscience.earth/ncl/geoera/ref/8014
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-03-03T16:08:15.565Z
definition: Probably basement fault reactivated in Late Cretaceous in a form of narrow anticlines bounded with reverse faults accommodated in the Zechstein salt. Method of observation: seismic profiles, borehole data. Strike: NW–SE to WNW–ESE. (Country Report fault code: A-18)
definition: Prawdopodobny uskok podłoża reaktywowany w późnej kredzie w postaci wąskich antyklin ograniczonych uskokami odwróconymi, powiązanymi z solami cechsztyńskimi. Metody obserwacji: profile sejsmiczne, dane z otworów wiertniczych. Bieg: NW–SE do WNW–ESE. (Kod uskoku w Raporcie krajowym projektu HIKE: A-18) @pl
preferred label: Strefa uskokowa Żuromin–Płońsk @pl
notation: PL-16010000
broader: Płock Trough

Lublin Basin
references: https://data.geoscience.earth/ncl/geoera/ref/8084
type: Concept
created: 2021-03-03T16:08:15.515Z
definition: Devonian–Carboniferous fault-controlled basin developed within the Variscan foreland over the SW limit of the east European Craton [the Teisseyre-Tornquist Zone (TTZ)] and then inverted at the end of the Variscan orogeny.
definition: Dewońsko–karboński basen lubelski, który rozwinął się na przedpolu waryscyjskim na granicy z kratonem wschodnioeuropejskim [strefa Teisseyre-Tornquista (TTZ)], a następnie uległ inwersji pod koniec orogenezy waryscyjskiej. @pl
preferred label: Basen lubelski @pl
narrower: Kock fault zone
narrower: Ursynów–Kazimierz fault set
narrower: Wilczopole–Marynin–Radawiec fault zone
narrower: Izbica–Zamość fault zone
narrower: Ciecierzyn fault system
narrower: Niedrzwica–Bełżce fault system
narrower: Grójec fault
narrower: Hanna fault
narrower: Narol fault
in scheme: Tectonic Boundary Objects in Europe
notation: PL-15000000
broader: East European Craton (tectonic megadomain)

Grójec fault
references: https://data.geoscience.earth/ncl/geoera/ref/8064
references: https://data.geoscience.earth/ncl/geoera/ref/8076
references: https://data.geoscience.earth/ncl/geoera/ref/8127
references: https://data.geoscience.earth/ncl/geoera/ref/8111
references: https://data.geoscience.earth/ncl/geoera/ref/8009
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-03-03T16:08:15.542Z
definition: Deeply-rooted basement fault zone reactivated during Late Paleozoic subsidence and inversion of the Lublin Basin. The kinematics is unknown. Representation in the magnetic and gravimetric anomaly fields points to its trans-crustal range. Method of observation: seismic profiles, potential fields data. Strike: NE–SW. (Country Report fault code: A-17)
definition: Głęboko zakorzeniona strefa uskoków podłoża reaktywowana podczas późno-paleozoicznej subsydencji a następnie inwersji niecki lubelskiej. Kinematyka jest nieznana. Obraz anomalii magnetycznych i grawimetrycznych wskazuje na strefę o zasięgu skorupowym. Metoda obserwacji: profile sejsmiczne, dane dotyczące pól potencjalnych. Bieg: NE–SW. (Kod uskoku w Raporcie krajowym projektu HIKE: A-17) @pl
preferred label: Uskok Grójca @pl
narrower: Grójec fault 1
narrower: Grójec fault 2
notation: PL-15070000
broader: Lublin Basin

Grójec fault 1
references: https://data.geoscience.earth/ncl/geoera/ref/8127
type: Concept
created: 2021-03-03T16:08:15.547Z
in scheme: Tectonic Boundary Objects in Europe
notation: PL-15070001
broader: Grójec fault

Grójec fault 2
references: https://data.geoscience.earth/ncl/geoera/ref/8127
type: Concept
created: 2021-03-03T16:08:15.550Z
in scheme: Tectonic Boundary Objects in Europe
notation: PL-15070002
broader: Grójec fault

Niedrzwica–Bełżce fault system
references: https://data.geoscience.earth/ncl/geoera/ref/8127
references: https://data.geoscience.earth/ncl/geoera/ref/8111
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-03-03T16:08:15.538Z
definition: Minor reverse faults developed on both sides of the thin-skinned anticlinal structure due to the basin inversion in Late Carboniferous. Basement faults control on the thrust location is possible. Method of observation: seismic profiles, borehole data. Strike: WNW–ESE. (Country Report fault code: A-16)
definition: Niewielkie uskoki odwrócone powstałe po obu stronach naskórkowej struktury antyklinalnej w wyniku inwersji basenu w późnym karbonie. Możliwa jest korelacja z uskokami podłoża. Metody obserwacji: profile sejsmiczne, dane z otworów wiertniczych. Bieg: WNW–ESE. (Kod uskoku w Raporcie krajowym projektu HIKE: A-16) @pl
preferred label: System uskokowy Niedrzwica–Bełżce @pl
notation: PL-15060000
broader: Lublin Basin

Ciecierzyn fault system
references: https://data.geoscience.earth/ncl/geoera/ref/8127
references: https://data.geoscience.earth/ncl/geoera/ref/8111
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-03-03T16:08:15.535Z
definition: Minor reverse faults developed on both sides of the thin-skinned anticlinal structure due to the basin inversion in Late Carboniferous. Basement faults control on the thrust location is possible. Method of observation: seismic profiles, borehole data. Strike: WNW–ESE. (Country Report fault code: A-15)
definition: Niewielkie uskoki odwrócone powstałe po obu stronach naskórkowej struktury antyklinalnej w wyniku inwersji basenu w późnym karbonie. Możliwa jest korelacja z uskokami podłoża. Metody obserwacji: profile sejsmiczne, dane z otworów wiertniczych. Bieg: WNW–ESE. (Kod uskoku w Raporcie krajowym projektu HIKE: A-15) @pl
preferred label: System uskokowy Ciecierzyn @pl
notation: PL-15050000
broader: Lublin Basin

Izbica–Zamość fault zone
references: https://data.geoscience.earth/ncl/geoera/ref/8127
references: https://data.geoscience.earth/ncl/geoera/ref/8111
references: https://data.geoscience.earth/ncl/geoera/ref/8079
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-03-03T16:08:15.531Z
definition: Thrust faults with the NE vergence with secondary back-thrusts. Thin-skinned structures developed during the Late Carboniferous basin inversion. Basement faults control on the thrust location is possible. Method of observation: seismic profiles, borehole data. Strike: NW–SE to WNW–ESE. (Country Report fault code: A-14)
definition: Nasunięcia o wergencji NE oraz nasunięcia wsteczne niższego rzędu. Powstały na etapie inwersji basenu w późnym karbonie jako struktury tektoniki naskórkowej. Struktura prawdopodobnie rozwinięta ponad uskokami podłoża. Metody obserwacji: profile sejsmiczne, dane z otworów wiertniczych. Bieg: NW–SE do WNW–ESE. (Kod uskoku w Raporcie krajowym projektu HIKE: A-14) @pl
preferred label: Strefa uskokowa Izbica–Zamość @pl
alternative label: Janów fault zone
notation: PL-15040000
broader: Lublin Basin

Wilczopole–Marynin–Radawiec fault zone
references: https://data.geoscience.earth/ncl/geoera/ref/8127
references: https://data.geoscience.earth/ncl/geoera/ref/8111
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-03-03T16:08:15.527Z
definition: Main thrust faults with NE vergence with secondary back-thrusts. Thin-skinned structures developed during the Late Carboniferous basin inversion. Basement faults control on the thrust location is possible. Method of observation: seismic profiles, borehole data. Strike: WNW–ESE. (Country Report fault code: A-13)
definition: Nasunięcie główne o wergencji NE oraz nasunięcia wsteczne niższego rzędu. Powstały na etapie inwersji basenu w późnym karbonie jako struktury tektoniki naskórkowej. Struktura prawdopodobnie rozwinięta ponad uskokami podłoża. Metody obserwacji: profile sejsmiczne, dane z otworów wiertniczych. Bieg: WNW–ESE. (Kod uskoku w Raporcie krajowym projektu HIKE: A-13) @pl
preferred label: Strefa uskokowa Wilczopole-Marynin-Radawiec @pl
notation: PL-15030000
broader: Lublin Basin

Ursynów–Kazimierz fault set
references: https://data.geoscience.earth/ncl/geoera/ref/8127
references: https://data.geoscience.earth/ncl/geoera/ref/8111
references: https://data.geoscience.earth/ncl/geoera/ref/8079
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-03-03T16:08:15.523Z
definition: Set of parallel faults composed of the basement-involved faults active during basin subsidence stage and thin-skinned thrusts of the Carboniferous age related to basin inversion. Minor back thrusts are present. Method of observation: seismic profiles, borehole data. Strike: WNW–ESE. (Country Report fault code: A-12)
definition: Zespół równoległych uskoków zakorzenionych w podłożu, aktywny w tracie subsydencji basenu, a następnie na etapie inwersji basenu w karbonie jako nasunięcia tektoniki naskórkowej. Metody obserwacji: profile sejsmiczne, dane z otworów wiertniczych. Bieg: WNW–ESE. (Kod uskoku w Raporcie krajowym projektu HIKE: A-12) @pl
preferred label: Uskoki Ursynów-Kazimierz @pl
alternative label: Kazimierz–Ursynów fault
notation: PL-15020000
broader: Lublin Basin

Kock fault zone
references: https://data.geoscience.earth/ncl/geoera/ref/8127
references: https://data.geoscience.earth/ncl/geoera/ref/8112
references: https://data.geoscience.earth/ncl/geoera/ref/8083
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-03-03T16:08:15.519Z
definition: Fault zone composed of the basement-involved Early Paleozoic fault downthrowing the NE wall, inverted during the Late Fammenian and then cut and displaced to the NE by a thin-skinned thrust, decoupled in the Silurian shales, during the Late Westphalian phase of the Variscan orogeny. The secondary back-thrusts are also present. Method of observation: seismic profiles, borehole data. Strike: NW–SE to WNW–ESE. (Country Report fault code: A-11)
definition: Strefa uskokowa podłoża rozwinięta we wczesnym paleozoiku, o zrzutowym skrzydle NE, odwrócona w późnym famenie, a następnie przecięta i przesunięta ku NE nasunięciem naskórkowym, odkłutym w łupkach syluru podczas późnej westfalskiej fazy orogenezy waryscyjskiej. Występują tu również nasunięcia wsteczne niższego rzędu. Metody obserwacji: profile sejsmiczne, dane z otworów wiertniczych. Bieg: NW–SE do WNW–ESE. (Kod uskoku w Raporcie krajowym projektu HIKE: A-11) @pl
preferred label: Strefa uskokowa Kocka @pl
alternative label: Kock fault
notation: PL-15010000
broader: Lublin Basin

Narol fault
references: https://data.geoscience.earth/ncl/geoera/ref/8079
references: https://data.geoscience.earth/ncl/geoera/ref/8080
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-03-03T16:08:15.557Z
definition: Major fault system, observed on the basis of deep reflection seismic profile Polcrust 01.
definition: Regionalny system uskokowy obserwowany w głębokim profilu refleksyjnym Polcrust 01. @pl
preferred label: Uskok Narola @pl
alternative label: Biłgoraj Narol zone
notation: PL-15090000
broader: Lublin Basin

Hanna fault
references: https://data.geoscience.earth/ncl/geoera/ref/8059
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-03-03T16:08:15.554Z
definition: Tectonic boundary defined on the basis of regional magnetic and gravimetric anomalies pattern and differences of the crystalline basement depth.
definition: Granica tektoniczna zdefiniowana na podstawie ukladu regionalnych anomalii magnetycznych i grawimetrycznych i różnicy głębokości podłoża. @pl
preferred label: Uskok Hanny @pl
notation: PL-15080000
broader: Lublin Basin

Podlasie–Bielarus Granulite Belt
references: https://data.geoscience.earth/ncl/geoera/ref/8058
references: https://data.geoscience.earth/ncl/geoera/ref/7998
type: Concept
created: 2021-03-03T16:08:15.473Z
definition: Crustal domain trending NE–SW between western Bielarus and TTZ, displaying arcuate, high-positive magnetic anomalies in its eastern part. In Poland it includes a greater part of the Podlasie fold zone and the metamorphic Kampinos complex. A belt of positive magnetic anomalies, interpreted as Białystok fault, defines its NW border.
definition: Domena skorupowa z łukowatymi silnie dodatnimi anomaliami magnetycznymi we wschodniej części, o przebiegu NE–SW od zachodniej Białorusi do TTZ. Na obszarze Polski obejmuje większą część podlaskiej strefy fałdowej i metamorficznego kompleksu kampinoskiego. NW granicę jednostki wyznacza pasmo wyżów magnetycznych interpretowane jako uskok Białegostoku. @pl
preferred label: Podlasko–Białoruski pas granulitowy @pl
narrower: Białystok fault zone
in scheme: Tectonic Boundary Objects in Europe
notation: PL-13000000
broader: East European Craton (tectonic megadomain)

Białystok fault zone
references: https://data.geoscience.earth/ncl/geoera/ref/8121
references: https://data.geoscience.earth/ncl/geoera/ref/7998
references: https://data.geoscience.earth/ncl/geoera/ref/8059
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-03-03T16:08:15.477Z
definition: The border of Palaeoproterozoic structure known as the Belarus Podlasie Granulite belt. SW–NE trending zone of the prominent regional magnetic anomaly interpreted as major shear zones, related to the 1.82 Ga – 1.80 Ga Fennoscandia-Sarmatia collision. Method of observation: magnetic anomaly map, seismic profiles. Strike: WNW–ESE. (Country Report fault code: A-9)
definition: Granica struktury paleeoproterozoicznej zwanej pasem granulitowym Białoruś–Podlasie. Strefa z trendem SW–NE widoczna w regionalnej anomalii magnetycznej, zinterpretowana została jako główne strefy ścinania, związana z kolizją 1,82 Ga - 1,80 Ga Fennoskandia-Sarmcja. Metoda obserwacji: mapa anomalii magnetycznej, profile sejsmiczne. Bieg: WNW – ESE. (Kod uskoku w Raporcie krajowym projektu HIKE: A-9) @pl
preferred label: Strefa uskokowa Białegostoku @pl
narrower: Białystok fault 1
narrower: Białystok fault 2
narrower: Białystok fault 3
narrower: Białystok fault 4
narrower: Białystok fault 5
notation: PL-13010000
broader: Podlasie–Bielarus Granulite Belt

Białystok fault 5
type: Concept
created: 2021-03-03T16:08:15.494Z
in scheme: Tectonic Boundary Objects in Europe
notation: PL-13010005
broader: Białystok fault zone

Białystok fault 4
type: Concept
created: 2021-03-03T16:08:15.491Z
in scheme: Tectonic Boundary Objects in Europe
notation: PL-13010004
broader: Białystok fault zone

Białystok fault 3
type: Concept
created: 2021-03-03T16:08:15.487Z
in scheme: Tectonic Boundary Objects in Europe
notation: PL-13010003
broader: Białystok fault zone

Białystok fault 2
type: Concept
created: 2021-03-03T16:08:15.484Z
in scheme: Tectonic Boundary Objects in Europe
notation: PL-13010002
broader: Białystok fault zone

Białystok fault 1
type: Concept
created: 2021-03-03T16:08:15.481Z
in scheme: Tectonic Boundary Objects in Europe
notation: PL-13010001
broader: Białystok fault zone

Upper Sileasian fault zones
type: Concept
created: 2021-03-03T16:08:15.793Z
definition: Faults cross-cutting the Upper Silesian Block (see below).
definition: Uskoki przecinające blok górnośląski. @pl
preferred label: Strefy uskokowe bloku górnośląskiego @pl
narrower: Upper Silesian Block
references: https://data.geoscience.earth/ncl/geoera/ref/8000
in scheme: Tectonic Boundary Objects in Europe
notation: PL-40000000
broader: Tectonic Boundary in Poland

Upper Silesian Block
type: Concept
created: 2021-03-03T16:08:15.796Z
definition: Upper Silesian block is the Northern part of a complex Brunovistulicum terrane. Within Polish borders, its western limit is the Moldanubian thrust belt, its northern and eastern border is the Kraków–Lubliniec fault zone and its southern limit is the peri-Pieniny fault zone.
definition: Blok górnośląski stanowi północną część złożonego terranu Brunovistulicum. W granicach Polski zachodnią granicę tej jednostki wyznacza strefa nasunięć moldanubskich, północą i wschodnią strefa uskokowa Kraków–Lubliniec, południową perypienińska strefa uskokowa. @pl
preferred label: Blok górnośląski @pl
narrower: Kraków–Lubliniec fault zone
narrower: Krzeszowice–Charsznica fault
narrower: Tworóg–Zawiercie fault set
narrower: Rzeszotary fault set
narrower: Andrychów–Chyżne fault set
narrower: Moravian–Silesian Fold and Thrust Belt
narrower: Ruptawa and Jawiszowice fault set
narrower: Żywiec – Nowy Sącz fault set
references: https://data.geoscience.earth/ncl/geoera/ref/8000
references: https://data.geoscience.earth/ncl/geoera/ref/8025
references: https://data.geoscience.earth/ncl/geoera/ref/8125
in scheme: Tectonic Boundary Objects in Europe
notation: PL-41000000
broader: Upper Sileasian fault zones

Kraków–Lubliniec fault zone
type: Concept
created: 2021-03-03T16:08:15.800Z
definition: Shear zone, active from the Neoproterozoic to the Mesozoic, with multiple strike-slip deformations, with the dominant phases at the turn of the Silurian/Devonian and in the Late Variscan time. Described structure is an edge of Upper Silesian and Małoposka Block. Additionally it’s a part of Hamburg–Kraków Tectonic Zone. Method of observation: gravimetry, borehole data, geological mapping. Strike: NW–SE. (Country Report fault code: D-1)
definition: Strefa ścinania, aktywna od neoproterozoiku do mezozoiku, z licznymi deformacjami przesuwczymi, z dominującymi fazami na przełomie syluru / dewonu i późnych ruchów waryscyjskich. Opisywana struktura stanowi skraj bloku górnośląskiego i małoposkiego. Dodatkowo jest częścią strefy tektonicznej Hamburg–Kraków. Metody obserwacji: grawimetria, dane z otworów wiertniczych, kartografia geologiczna. Bieg: NW–SE. (Kod uskoku w Raporcie krajowym projektu HIKE: D-1) @pl
preferred label: Strefa uskokowa Kraków–Lubliniec @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8122
references: https://data.geoscience.earth/ncl/geoera/ref/8001
references: https://data.geoscience.earth/ncl/geoera/ref/8003
in scheme: Tectonic Boundary Objects in Europe
notation: PL-41010000
broader: Upper Silesian Block

Żywiec – Nowy Sącz fault set
type: Concept
created: 2021-03-03T16:08:15.832Z
definition: Subparallel normal faults of the Late Variscan origin, reactivated until Cenozoic, systematically downthrowing the southern walls by 400–600 m. They form the southern edge of the Bielsko-Biała elevation. Described structure is a border of Upper Silesian Block and Bielsko-Biała dome. Method of observation: geological mapping. Strike: W–E. (Country Report fault code: D-8)
definition: Późnowaryscyjskie równoległe uskoki normalne, aktywne aż do kenozoiku, systematycznie zrzucające południowe skrzydła o o 400–600 m. Tworzą południowy kraniec elewacji Bielska-Białej. Opisywana struktura stanowi granicę bloku górnośląskiego i kopuły Bielska-Białej. Metoda obserwacji: kartowanie geologiczne. Bieg: W–E. (Kod uskoku w Raporcie krajowym projektu HIKE: D-8) @pl
preferred label: Zespół uskoków Żywiec – Nowy Sącz @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8000
in scheme: Tectonic Boundary Objects in Europe
notation: PL-41080000
broader: Upper Silesian Block

Ruptawa and Jawiszowice fault set
type: Concept
created: 2021-03-03T16:08:15.828Z
definition: Subparallel normal faults of the Late Variscan origin, reactivated until Cenozoic, systematically downthrowing theis southern walls by 400–700 m. They form the northern boundary of the Neogene Carpathian Foredeep Basin. Described structure is a border of Upper Silesian Block and the Carpathian Foredeep. Method of observation: borehole data, mining and geological mapping. Strike: W–E. (Country Report fault code: D-7)
definition: Późnowaryscyjskie równoległe uskoki normalne, aktywne aż do kenozoiku, systematycznie zrzucające południowe skrzydła o 400–700 m. Tworzą północną granicę neogeńskiego zapadliska przedkarpackiego. Opisywana struktura stanowi granicę bloku górnośląskiego i zapadliska przedkarpackiego. Metody obserwacji: dane otworowe, mapy górnicze i geologiczne. Bieg: W–E. (Kod uskoku w Raporcie krajowym projektu HIKE: D-7) @pl
preferred label: Zespół uskoków Ruptawy i Jawiszowic @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8045
in scheme: Tectonic Boundary Objects in Europe
notation: PL-41070000
broader: Upper Silesian Block

Moravian–Silesian Fold and Thrust Belt
type: Concept
created: 2021-03-03T16:08:15.821Z
definition: Moravian–Silesian fold and thrust belt formed due to the Late Variscan collision of the Brunovistulicum terrane with the Czechia Massif. It is made of deformed Proterozoic and and Devonian cristalline rocks, Carboniferous flysh and Carboniferous coal-bearing rocks, occuring between Moldanubian thrusts in the west and the Orlova–Boguszowice thrust in the east. Structural style is a fold-and-thrust belt with roughly N–S trending folds showing predominantly eastern vergence.
definition: Morawsko-śląskie pasmo fałdowo-nasuwcze, utworzyło się w wyniku późnowaryscyjskiej kolizji Brunovistulicum z masywem czeskim. Obejmuje zdeformowane proterozoiczne i dewońskie skały krystaliczne, karbońskie utwory fliszowe i karbońskie utwory węglonośne położone między strefą nasunięć moldanubskich na zachodzie a nasunięciem orłowsko–boguszowickim na wschodzie. Obszar cechuje się fałdowo-nasunięciowym stylem budowy, struktury fałdowe wykazują subpołudnikowy przebieg oraz przeważnie wschodnią wergencję. @pl
preferred label: Morawsko–śląski pas fałdowo-nasunięciowy @pl
narrower: Orlova–Boguszowice Thrust
references: https://data.geoscience.earth/ncl/geoera/ref/8000
references: https://data.geoscience.earth/ncl/geoera/ref/8115
references: https://data.geoscience.earth/ncl/geoera/ref/8125
in scheme: Tectonic Boundary Objects in Europe
notation: PL-41060000
broader: Upper Silesian Block

Orlova–Boguszowice Thrust
type: Concept
created: 2021-03-03T16:08:15.825Z
definition: A set of thrust faults of the eastern vergence, forming Variscan deformation front, overthrusted on the Upper Silesian foredeep basin. Method of observation: borehole data, mining and geological mapping. Strike: NNE–SSW. (Country Report fault code: D-6)
definition: Zespół nasunięć o wschodniej wergencji tworzących front deformacji waryscyjskich, nasuniętych na (przedgórski) basen górnośląski. Metody obserwacji: dane otworowe, mapy górnicze i geologiczne. Bieg: NNE–SSW. (Kod uskoku w Raporcie krajowym projektu HIKE: D-6) @pl
preferred label: Nasunięcie Orlowej–Boguszowic @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8005
in scheme: Tectonic Boundary Objects in Europe
notation: PL-41061000
broader: Moravian–Silesian Fold and Thrust Belt

Andrychów–Chyżne fault set
type: Concept
created: 2021-03-03T16:08:15.816Z
definition: Contact zone between Precambrian terranes, reactivated after the Permian. Method of observation: magnetotellurics, borehole data, geological mapping. Strike: NNW–SSE. (Country Report fault code: D-5)
definition: Strefa kontaktu między terranami prekambryjskimi, reaktywowana po permie. Metoda obserwacji: magnetotelluryka, dane otworowe, kartowanie geologiczne. Bieg: NNW–SSE. (Kod uskoku w Raporcie krajowym projektu HIKE: D-5) @pl
preferred label: Zespół uskoków Andrychów–Chyżne @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8095
references: https://data.geoscience.earth/ncl/geoera/ref/8003
references: https://data.geoscience.earth/ncl/geoera/ref/8126
in scheme: Tectonic Boundary Objects in Europe
notation: PL-41050000
broader: Upper Silesian Block

Rzeszotary fault set
type: Concept
created: 2021-03-03T16:08:15.813Z
definition: Tectonic horst with elevated Archaic–Proterozoic basement of the Upper Silesia Block bounded by steep faults showing vertical displacement > 1500 m, active in the Neoproterozoic and Late Variscan times. Method of observation: gravimetry borehole data, geological mapping. Strike: NNW–SSE. (Country Report fault code: D-4)
definition: Zrąb tektoniczny z wyniesionym archaiczno-proterozoicznym podłożem bloku górnośląskiego, ograniczonym stromymi uskokami o przemieszczeniach pionowych > 1500 m, czynny w okresie neoproterozoiku i późnych ruchów waryscyjskich. Metoda obserwacji: dane grawimetryczne z otworów wiertniczych, kartowanie geologiczne. Bieg: NNW–SSE. (Kod uskoku w Raporcie krajowym projektu HIKE: D-4) @pl
preferred label: Zespół uskoków Rzeszotar @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8000
in scheme: Tectonic Boundary Objects in Europe
notation: PL-41040000
broader: Upper Silesian Block

Tworóg–Zawiercie fault set
type: Concept
created: 2021-03-03T16:08:15.809Z
definition: Fault zone founded in Cadomian time and repeatedly reactivated until the Cenozoic; creates the boundary between the elevated Brudzowice (Siewierza) Block and the Permian Sławków Graben. The final vertical offset is >1000 m. Method of observation: gravimetry, borehole data, geological mapping. Strike: WNW–ESE. (Country Report fault code: D-3)
definition: Strefa uskokowa założona w trakcie orogenezy kadomskiej i wielokrotnie reaktywowana aż do kenozoiku; tworzy granicę pomiędzy wyniesionym blokiem Brudzowic (Siewierza) a permskim rowem Sławkowa. Całkowity pionowy zrzut wynosi> 1000 m. Metody obserwacji: grawimetria, dane z otworów wiertniczych, kartografia geologiczna. Bieg: WNW–ESE. (Kod uskoku w Raporcie krajowym projektu HIKE: D-3) @pl
preferred label: Zespół uskoków Tworóg–Zawiercie @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8070
in scheme: Tectonic Boundary Objects in Europe
notation: PL-41030000
broader: Upper Silesian Block

Krzeszowice–Charsznica fault
type: Concept
created: 2021-03-03T16:08:15.804Z
definition: Strike-slip fault, which accomodated 12 km transversal sinistral offset of the Kraków–Lubliniec Fault Zone at the end of the Variscan orogeny. Described structure is the limit between the Upper Silesia and Małoposka blocks. Method of observation: geological mapping. Strike: NNE–SSW. (Country Report fault code: D-2)
definition: Uskok lewo-przesuwczy, który pod koniec orogenezy waryscyjskiej zaabsorbował 12 kilometrów przesunięcia wzdłuż strefy uskokowej Kraków–Lubliniec. Opisana struktura stanowi granicę między blokiem Górnego Śląska i Małoposki. Metoda obserwacji: kartowanie geologiczne. Bieg: NNE–SSW. (Kod uskoku w Raporcie krajowym projektu HIKE: D-2) @pl
preferred label: Uskok Krzeszowice–Charsznica @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8004
references: https://data.geoscience.earth/ncl/geoera/ref/8122
references: https://data.geoscience.earth/ncl/geoera/ref/8002
in scheme: Tectonic Boundary Objects in Europe
notation: PL-41020000
broader: Upper Silesian Block

Lower Silesian fault systems and zones
type: Concept
created: 2021-03-03T16:08:15.835Z
definition: Set of polygenetic and multidirectional fault systems and zones, mostly originating from Variscan orogeny (Carboniferous) or Permian to Mesozoic mainly extensional events, partly inverted by Late Cretaceous–Palaeogene compressional episode and reactivated by Late Cenozoic tectonic activity at the distant foreland of Alps and Carpathians.
definition: Zbiór poligenetycznych i wielokierunkowych systemów i stref uskoków, powstałych głównie podczas orogenezy waryscyjskiej (karbońskiej) lub permo-mezozoicznych epizodów ekstensyjnych. Uskoki te częściowo uległy inwersji w trakcie późnokredowej i paleogeńskiej kompresji a także zostały reaktywowane przez późnokenozoiczną aktywność tektoniczną na dalekim przedpolu Alp i Karpat. @pl
preferred label: Systemy i strefy uskokowe Dolnego Śląska @pl
narrower: Fore-Sudetic homocline faults
narrower: Sudetic block
narrower: Opole Trough
references: https://data.geoscience.earth/ncl/geoera/ref/8094
references: https://data.geoscience.earth/ncl/geoera/ref/8085
in scheme: Tectonic Boundary Objects in Europe
notation: PL-50000000
broader: Tectonic Boundary in Poland

Fore-Sudetic homocline faults
type: Concept
created: 2021-03-03T16:08:15.838Z
definition: Multi-stage faults, often decoupled across Permian salts, cross-cutting shallow NNE- to NE-dipping Permo–Mesozoic succession, defining the SW limb of the Szczecin–Miechów trough (synclinorium), NE of the Middle Odra fault system.
definition: Wielokrotnie odmładzane uskoki, często odspojone w solach permskich, przecinające łagodnie zapadającą na NNE do NE serię permo-mezozoiczną, wyznaczającą SW skrzydło niecki szczecińsko-miechowskiej (synklinorium) na północny-wschód od systemu uskoków Środkowej Odry. @pl
preferred label: Uskoki monokliny przedsudeckiej @pl
narrower: Dolsk fault zone
narrower: Poznań–Oleśnica fault system
references: https://data.geoscience.earth/ncl/geoera/ref/8094
references: https://data.geoscience.earth/ncl/geoera/ref/8123
in scheme: Tectonic Boundary Objects in Europe
notation: PL-51000000
broader: Lower Silesian fault systems and zones

Dolsk fault zone
type: Concept
created: 2021-03-03T16:08:15.842Z
definition: Blind fault zone buried below thick Permo–Mesozoic succession. Originally a Variscan, Carboniferous dextral strike-slip, possibly reactivated in later times. On deep seismic profiles separates different crust types: 3-layer one typical of Baltica and Palaeozoic Platform to the NE and a low-velocity 2-layer one to the SW – typical of the Variscan belt. Method of observation: industrial seismic profiles, borehole data. Strike: WNW–ESE. (Country Report fault code: E-1)
definition: Strefa uskokowa w podłożu miąższej sukcesji skał permo-mezozoicznych. Pierwotnie karboński, prawoprzesuwczy uskok waryscyjski, prawdopodobnie później reaktywowany. Na głębokich profilach sejsmicznych rozdziela różne typy skorupy: 3-warstwową typową dla Baltiki i platformy paleozoicznej na NE i 2-warstwową o niskich prędkościach na SW – typową dla pasa waryscyjskiego. Metoda obserwacji: profile sejsmiczne, dane z otworów wiertniczych. Bieg: WNW–ESE. (Kod uskoku w Raporcie krajowym projektu HIKE: E-1) @pl
preferred label: Strefa uskokowa Dolska @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8074
references: https://data.geoscience.earth/ncl/geoera/ref/8037
references: https://data.geoscience.earth/ncl/geoera/ref/8012
references: https://data.geoscience.earth/ncl/geoera/ref/8053
in scheme: Tectonic Boundary Objects in Europe
notation: PL-51010000
broader: Fore-Sudetic homocline faults

Poznań–Oleśnica fault system
type: Concept
created: 2021-03-03T16:08:15.846Z
definition: Large-scale complex graben system, following the originally Triassic fault train, of possible Variscan antecedence, evolved through Mesozoic extensional events to, eventually, form a system of branching tectonic grabens with Late Cenozoic lignite deposits. Includes grabens of: (1) Poznań–Oleśnica, (2) Chruścina, (3) Chobienia–Rawicz. Method of observation: potential field and drilling record. Strike: NW–SE to ENE–WSW for branches. (Country Report fault code: E-2)
definition: System rowów, przebiegający zgodnie z ciągiem uskoków triasowych, o możliwym założeniu waryscyjskim, ewoluował w wyniku epizodów ekstensji w mezozoiku, ostatecznie tworząc system rozgałęzionych rowów tektonicznych ze złożami późnokenozoicznego węgla brunatnego. Zawiera rowy: (1) Poznań–Oleśnica, (2) Chruścina, (3) Chobienia–Rawicz. Metoda obserwacji: pola potencjalne i wiercenia. Bieg: od NW–SE do ENE–WSW. (Kod uskoku w Raporcie krajowym projektu HIKE: E-2) @pl
preferred label: System uskokowy Poznań–Oleśnica @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8050
references: https://data.geoscience.earth/ncl/geoera/ref/8116
references: https://data.geoscience.earth/ncl/geoera/ref/8048
references: https://data.geoscience.earth/ncl/geoera/ref/8049
references: https://data.geoscience.earth/ncl/geoera/ref/8047
in scheme: Tectonic Boundary Objects in Europe
notation: PL-51020000
broader: Fore-Sudetic homocline faults

Opole Trough
type: Concept
created: 2021-03-03T16:08:15.881Z
definition: Fragment of Upper Cretaceous sedimentary cover erosionally separated from that of the Szczecin–Miechów trough, preserved in a tectonic depression resting on top of older Permo–Mesozoic and Carboniferous strata and Varisan crystalline basement.
definition: Fragment górnokredowej pokrywy osadowej, oddzielonej erozyjnie od niecki szczecińsko-miechowskiej, zachowany w obniżeniu tektonicznym, na warstwach permo–mezozoicznych i karbońskich oraz krystalicznym podłożu waryscyjskim. @pl
preferred label: Niecka opolska @pl
narrower: Paczków and Kędzierzyn graben system
references: https://data.geoscience.earth/ncl/geoera/ref/8088
references: https://data.geoscience.earth/ncl/geoera/ref/8081
in scheme: Tectonic Boundary Objects in Europe
notation: PL-53000000
broader: Lower Silesian fault systems and zones

Paczków and Kędzierzyn graben system
type: Concept
created: 2021-03-03T16:08:15.884Z
definition: A chain of the Late Cenozoic grabens, developed mostly in the Miocene, probably due to extension in the foreland plate of the folded Carpathians. Method of observation: borehole data, seismic profiles. Strike: W–E. (Country Report fault code: E-9)
definition: Łańcuch późno kenozoicznych rowów, rozwinął się głównie w miocenie, prawdopodobnie w wyniku ekstensji na przedpolu Karpat. Metody obserwacji: dane z otworów wiertniczych, profile sejsmiczne. Bieg: W–E. (Kod uskoku w Raporcie krajowym projektu HIKE: E-9) @pl
preferred label: System rowów Paczkowa i Kędzierzyna @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8050
references: https://data.geoscience.earth/ncl/geoera/ref/8027
references: https://data.geoscience.earth/ncl/geoera/ref/8026
in scheme: Tectonic Boundary Objects in Europe
notation: PL-53010000
broader: Opole Trough

Sudetic block
type: Concept
created: 2021-03-03T16:08:15.851Z
definition: Late Miocene-uplifted SW part of the Lower Silesia block, limited by the Sudetic Boundary fault in the NW and extending to Czechia to the SW.
definition: Południowo-zachodnia część bloku dolnośląskiego wyniesiona w późnym miocenie, ograniczona uskokiem brzeżnym sudeckim na NW i sięgająca na SW do Czech. @pl
preferred label: Blok sudecki @pl
narrower: Middle Odra fault system
narrower: Sudetic Boundary (Marginal) fault system
narrower: Intra-Sudetic fault zone
narrower: Turoszów–Żytawa fault system
narrower: North Karkonosze fault system
narrower: Upper Nysa Kłodzka River graben system
references: https://data.geoscience.earth/ncl/geoera/ref/8124
in scheme: Tectonic Boundary Objects in Europe
notation: PL-52000000
broader: Lower Silesian fault systems and zones

Upper Nysa Kłodzka River graben system
type: Concept
created: 2021-03-03T16:08:15.876Z
definition: A system developed from the end of Cretaceous through Late Cenozoic, initially some of its faults originated as reverse, subsequently turned into normal faults downthrowing the Upper Nysa Graben and adjacent smaller depressions. These faults are part of a larger system that continues into Czechia as the Pořiči–Hronov Fault Zone. Described structure is a border of Sudetic Nysa Graben and Kłodzko–Orlica Dome. Includes faults of: Chocieszów, Pstrążna–Gorzanów, Zieleniec, Jagodna–Młoty. Method of observation: topographic expression, geological mapping. Strike: N–S to NW–SE. (Country Report fault code: E-8)
definition: System rozwijał się od końca kredy do późnego kenozoiku, początkowo niektóre jego uskoki były uskokami odwróconymi, a następnie przekształciły się w uskoki normalne zrzucające rów Górnej Nysy i przyległe mniejsze obniżenia. Uskoki te są częścią większego systemu, który ciągnie się do Czech jako strefa uskoku Pořiči–Hronov. Opisywany system stanowi granicę sudeckiego rowu Nysy i wyniesienia kopuły Kłodzko–Orlickiej. W skład systemu wchodzą uskoki: Chocieszów, Pstrążna–Gorzanów, Zieleniec, Jagodna–Młoty. Metody obserwacji: analiza topografii, kartowanie geologiczne. Bieg: z N–S do NW–SE. (Kod uskoku w Raporcie krajowym projektu HIKE: E-8) @pl
preferred label: System rowów górnej Nysy Kłodzkiej @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8118
references: https://data.geoscience.earth/ncl/geoera/ref/7990
references: https://data.geoscience.earth/ncl/geoera/ref/8020
references: https://data.geoscience.earth/ncl/geoera/ref/8021
references: https://data.geoscience.earth/ncl/geoera/ref/8113
in scheme: Tectonic Boundary Objects in Europe
notation: PL-52060000
broader: Sudetic block

North Karkonosze fault system
type: Concept
created: 2021-03-03T16:08:15.872Z
definition: A system of Cenozoic normal faults responsible for downthrowing the Jelenia Góra Basin with respect to the Karkonosze, Rudawy Janowickie, Izera and Kaczawa Mts. Described structure is a border of Sudetic Block and Izera–Karkonosze Massif. Method of observation: topographic expression, surface observations. Strike: WNW—ESE and NE-SW. (Country Report fault code: E-7)
definition: System kenozoicznych uskoków normalnych odpowiedzialnych za obniżenie Kotliny Jeleniogórskiej w stosunku do Karkonoszy, Rudaw Janowickich, Izery i Kaczaw. System wyznacza granicę Bloku Sudeckiego i Masywu Izersko–Karkonoskiego. Metody obserwacji: analiza topografii, obserwacje powierzchniowe. Bieg: WNW–ESE i NE–SW. (Kod uskoku w Raporcie krajowym projektu HIKE: E-7) @pl
preferred label: Północno karkonoski system uskokowy @pl
references: https://data.geoscience.earth/ncl/geoera/ref/7988
references: https://data.geoscience.earth/ncl/geoera/ref/8102
references: https://data.geoscience.earth/ncl/geoera/ref/8075
references: https://data.geoscience.earth/ncl/geoera/ref/8051
in scheme: Tectonic Boundary Objects in Europe
notation: PL-52050000
broader: Sudetic block

Turoszów–Żytawa fault system
type: Concept
created: 2021-03-03T16:08:15.869Z
definition: Faults delineating the Siekierczyn and Zittau Troughs (grabens) filled with lignite formation at the NE termination of the extensive Ohře (Eger) Graben of NW Czechia, related to Late Cenozoic abundant basaltoid volcanism. Described structure is a border of Sudetic Block, Turoszów–Żytawa Trough (synclinorium) and Izera–Karkonosze Massif. Method of observation: surface observations, topographic expression, mining data. Strike: NNE–SSW and WNW–ESE. (Country Report fault code: E-6)
definition: Uskoki wyznaczające niecki siekierczyńską j i żytawską. Niecki wypełnione węglem brunatnym, położone w NE części rozległego rowu Ohře (Eger) północno-zachodnich Czech, związane z wulkanizmem bazaltoidowym późnego kenozoiku. Opisywane struktury stanowią granicę bloku sudeckiego, niecki Turoszów–Żytawa i Masywu Izersko–Karkonoskiego. Metody obserwacji: obserwacje powierzchniowe, analiza topografii, dane górnicze. Bieg: NNE–SSW i WNW–ESE. (Kod uskoku w Raporcie krajowym projektu HIKE: E-6) @pl
preferred label: System uskokowy Turoszów–Żytawa @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8049
references: https://data.geoscience.earth/ncl/geoera/ref/8047
in scheme: Tectonic Boundary Objects in Europe
notation: PL-52040000
broader: Sudetic block

Intra-Sudetic fault zone
type: Concept
created: 2021-03-03T16:08:15.864Z
definition: A major, NW–SE trending ductile shear zone/semi-brittle to brittle fault zone, in most parts exposed on the surface. The main activity occurred in Carboniferous times, with estimated dextral displacement of at least 50 km, but possibly reaching as much as ~300 km. This was followed by Late Carboniferous reversal with a sinistral displacement of ~25 km and Permian to Neogene dip-slip. Method of observation: field observations, potential field record. Strike: NNW–SSE. (Country Report fault code: E-5)
definition: Duża strefa ścinania o kierunku NW–SE przechodząca w strefę uskoków półkruchych do kruchych, w znacznej części widoczna w odsłonięciach. Główna aktywność miała miejsce w karbonie, szacowane przemieszczenie (prawoskrętne) to co najmniej 50 km, ale może sięgać nawet ~ 300 km. W późnym karbonie nastąpiło odwrócenie kierunku ruchu (przesunięcie lewoskrętne), szacowana wielkość tego przemieszczenia to ~ 25 km, następnie deformacje zrzutowe od permu do neogenu. Metoda obserwacji: obserwacje terenowe, pomiary pól potencjalnych. Bieg: NNW–SSE. (Kod uskoku w Raporcie krajowym projektu HIKE: E-5) @pl
preferred label: Strefa uskoku śródsudeckiego @pl
references: https://data.geoscience.earth/ncl/geoera/ref/7987
references: https://data.geoscience.earth/ncl/geoera/ref/8089
references: https://data.geoscience.earth/ncl/geoera/ref/8090
references: https://data.geoscience.earth/ncl/geoera/ref/7986
in scheme: Tectonic Boundary Objects in Europe
notation: PL-52030000
broader: Sudetic block

Sudetic Boundary (Marginal) fault system
type: Concept
created: 2021-03-03T16:08:15.860Z
definition: Fault zone prominently expressed in the Sudetic topography. Originally, a probable large-scale Riedel shear accompanying the Carboniferous displacement on the Intra-Sudetic Fault Zone. Subsequently reactivated with a dip-slip kinematics: (1) at the Cretaceous/Palaeogene turn, uplifting the Fore-Sudetic block with respect to the Sudetic one; (2) in the Late Miocene, reversing the position of the Sudetic vs Fore-Sudetic blocks. Additionally, described structure is a part of Elbe Fault Zone. Method of observation: field observations, potential field record, magnetotelluric data. Strike: NW–SE to NNW–SSE. (Country Report fault code: E-4)
definition: Strefa uskokowa wyraźnie zaznaczona w topografii Sudetów. Pierwotnie prawdopodobnie wielkoskalowe ścięcie Riedla, towarzyszące karbońskiemu przemieszczeniu na uskoku śródsudeckim. Następnie reaktywowana w reżimie zrzutowym: (1) na przełomie kredy / paleogenu, wynosząc blok przedsudecki względem sudeckiego; (2) w późnym miocenie, odwracając położenie bloku sudeckiego względem przedsudeckiego. Opisywana struktura jest częścią strefy uskokowej Łaby. Metoda obserwacji: obserwacje terenowe, pomiary pól potencjalnych, dane magnetotelluryczne. Bieg: NW–SE do NNW–SSE. (Kod uskoku w Raporcie krajowym projektu HIKE: E-4) @pl
preferred label: System uskokowy uskoku brzeżnego sudeckiego @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8055
references: https://data.geoscience.earth/ncl/geoera/ref/7991
references: https://data.geoscience.earth/ncl/geoera/ref/8091
references: https://data.geoscience.earth/ncl/geoera/ref/8027
references: https://data.geoscience.earth/ncl/geoera/ref/8026
in scheme: Tectonic Boundary Objects in Europe
notation: PL-52020000
broader: Sudetic block

Middle Odra fault system
type: Concept
created: 2021-03-03T16:08:15.855Z
definition: Originally a Variscan, Carboniferous dextral strike-slip major fault zone injected with Carboniferous granitoids, recurrently reactivated in the Permo–Mesozoic cover, mostly in dip-slip regime in times between Permian and Neogene. At present, does not show clear topographic effects of its youngest possible activity, except for its trace being followed by the Odra river. Described structure is a border of Sudetic Block and Fore-Sudetic Block. It’s also presumably a part of Hamburg–Kraków Fault Zone. Method of observation: borehole data, potential field, sparse seismic profiles, copper mines data. Strike: NW–SE to WNW–ESE. (Country Report fault code: E-3)
definition: Pierwotnie waryscyjska, karbońska, prawoskrętna strefa uskoku przesuwczego, z karbońskimi intruzjami granitoidów, z widoczną w pokrywie permo-mezozoicznej reaktywacją, głównie w reżimie zrzutowym, w okresie między permem a neogenem. Obecnie w topografii przejawia się jedynie w przebiegu doliny Odry. Opisana struktura wyznacza granicę bloku sudeckiego i przedsudeckiego. Przypuszczalnie jest też częścią strefy uskokowej Hamburg–Kraków. Metody obserwacji: dane z otworów wiertniczych, pola potencjalne, skąpe profile sejsmiczne, dane z kopalni miedzi. Bieg: NW–SE do WNW–ESE. (Kod uskoku w Raporcie krajowym projektu HIKE: E-3) @pl
preferred label: System uskokowy środkowej Odry @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8074
references: https://data.geoscience.earth/ncl/geoera/ref/7986
references: https://data.geoscience.earth/ncl/geoera/ref/8023
references: https://data.geoscience.earth/ncl/geoera/ref/8038
in scheme: Tectonic Boundary Objects in Europe
notation: PL-52010000
broader: Sudetic block

Northern segment of the Trans-European suture zone
narrower: Pomeranian Swell
narrower: Szczecin Trough
narrower: Kujavian Swell
narrower: Łódź Trough
references: https://data.geoscience.earth/ncl/geoera/ref/8086
type: Concept
created: 2021-03-03T16:08:15.568Z
definition: Trans-European suture zone (TESZ) is a litospheric-scale tectonic suture between the East European Craton and the Palaeozoic West European Platform.
definition: TESZ to szew tektoniczny stanowiący granicę między kratonem wschodnioeuropejskim a platformą paleozoiczną Europy Zachodniej. @pl
preferred label: Północna część strefy szwu transeuropejskiego @pl
narrower: Sorgenfrei-Tornquist fault zone
narrower: Teisseyre-Tornquist fault zone
in scheme: Tectonic Boundary Objects in Europe
notation: PL-20000000
broader: Tectonic Boundary in Poland

Łódź Trough
type: Concept
created: 2021-03-03T16:08:15.663Z
definition: Łódź Trough is a middle part of the Szczecin–Miechów synclinorium, bordering the Mid-Polish Swell/anticlinorium from the SW.
definition: Niecka łódzka jest częścią synklinorium szczecińsko-miechowskiego, przylegającego od południowej strony do antyklinorium środkowopolskiego. @pl
preferred label: Niecka łódzka @pl
narrower: Sompolno–Kcynia–Szubin fault zone
narrower: Damasławek–Mogilno fault zone
narrower: Konin–Bełchatów fault zone
narrower: Opatówek–Szczerców fault zone
narrower: Wieluń–Szczerców fault zone
narrower: Poznań–Kalisz–Wieruszów fault zone
references: https://data.geoscience.earth/ncl/geoera/ref/8081
in scheme: Tectonic Boundary Objects in Europe
notation: PL-26000000
broader: Northern segment of the Trans-European suture zone

Poznań–Kalisz–Wieruszów fault zone
type: Concept
created: 2021-03-03T16:08:15.687Z
definition: Sigmoidal and branched basement fault system partially reactivated in the T3–J1. Method of observation: seismic profiles. Strike: NW–SE. (Country Report fault code: B-19)
definition: Sigmoidalny i rozgałęziony system uskoków podłoża, częściowo reaktywowany w T3–J1. Metoda obserwacji: profile sejsmiczne. Bieg: NW–SE. (Kod uskoku w Raporcie krajowym projektu HIKE: B-19) @pl
preferred label: Strefa uskokowa Poznań–Kalisz–Wieruszów @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8022
in scheme: Tectonic Boundary Objects in Europe
notation: PL-26060000
broader: Łódź Trough

Wieluń–Szczerców fault zone
type: Concept
created: 2021-03-03T16:08:15.683Z
definition: Mezozoiczna strefa uskokokowa, częściowo reaktywowana jako rów mioceński. Strefa ta stanowi granicę niecki łódzkiej i monokliny przedsudeckiej. Metoda obserwacji: profile sejsmiczne. Bieg: W–E. (Kod uskoku w Raporcie krajowym projektu HIKE: B-20) @pl
preferred label: Strefa uskokowa Wieluń–Szczerców @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8014
references: https://data.geoscience.earth/ncl/geoera/ref/8022
in scheme: Tectonic Boundary Objects in Europe
definition: Mesozoic fault zone partially reactivated as the Miocene graben. Described structure is a border of Łódź Trough (synclinorium) and Fore-Sudetic Monocline. Method of observation: seismic profiles. Strike: W–E. (Country Report fault code: B-20)
notation: PL-26050000
broader: Łódź Trough

Opatówek–Szczerców fault zone
type: Concept
created: 2021-03-03T16:08:15.679Z
definition: Basement fault zone partially reactivated in the Mesozoic. Described structure is a border of Łódź Trough (synclinorium) and Fore-Sudetic Monocline. Strike: NW–SE. (Country Report fault code: B-18)
definition: Strefa uskokowa podłoża częściowo reaktywowana w mezozoiku. Struktura ta wyznacza granicę niecki łódzkiej i monokliny przedsudeckiej. Bieg: NW–SE. (Kod uskoku w Raporcie krajowym projektu HIKE: B-18) @pl
preferred label: Strefa uskokowa Opatówek–Szczerców @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8022
in scheme: Tectonic Boundary Objects in Europe
notation: PL-26040000
broader: Łódź Trough

Konin–Bełchatów fault zone
type: Concept
created: 2021-03-03T16:08:15.675Z
definition: Rooted in the basement, sigmoidal fault zone, partially reactivated in the Mesozoic. Method of observation: seismic profiles. Strike: NW–SE. (Country Report fault code: B-17)
definition: Sigmoidalna strefa uskokowa mająca swoje korzenie w podłożu, częściowo reaktywowana w mezozoiku. Metoda obserwacji: profile sejsmiczne. Bieg: NW–SE. (Kod uskoku w Raporcie krajowym projektu HIKE: B-17) @pl
preferred label: Strefa uskokowa Konin–Bełchatów @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8022
in scheme: Tectonic Boundary Objects in Europe
notation: PL-26030000
broader: Łódź Trough

Damasławek–Mogilno fault zone
type: Concept
created: 2021-03-03T16:08:15.671Z
definition: Probably basement fault zone documented in the Mesozoic cover with two salt diapirs activated in the Cenozoic. Method of observation: seismic profiles. Strike: NW–SE. (Country Report fault code: B-16)
definition: Prawdopodobnie strefa uskoku podłoża udokumentowana w pokrywie mezozoicznej z dwoma wysadami solnymi aktywnymi w kenozoiku. Metoda obserwacji: profile sejsmiczne. Bieg: NW–SE. (Kod uskoku w Raporcie krajowym projektu HIKE: B-16) @pl
preferred label: Strefa uskokowa Damasławek–Mogilno @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8022
in scheme: Tectonic Boundary Objects in Europe
notation: PL-26020000
broader: Łódź Trough

Sompolno–Kcynia–Szubin fault zone
type: Concept
created: 2021-03-03T16:08:15.667Z
definition: Branched basement fault system reactivated in the Mesozoic with an array of salt diapirs created in the T3–J1. Method of observation: seismic profiles. Strike: NW–SE. (Country Report fault code: B-15)
definition: Rozgałęziony system uskoków podłoża reaktywowany w mezozoiku z szeregiem wysadów solnych powstałych na przełomie T3 – J1. Metoda obserwacji: profile sejsmiczne. Bieg: NW–SE. (Kod uskoku w Raporcie krajowym projektu HIKE: B-15) @pl
preferred label: Strefa uskokowa Sompolno–Kcynia–Szubin @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8022
in scheme: Tectonic Boundary Objects in Europe
notation: PL-26010000
broader: Łódź Trough

Teisseyre-Tornquist fault zone
narrower: T-T fault zone 1
narrower: T-T fault zone 2
narrower: T-T fault zone 3
narrower: T-T fault zone 4
narrower: Miastko–Świecie fault zone
narrower: Koszalin–Toruń fault zone
narrower: Toruń–Radom fault zone
references: https://data.geoscience.earth/ncl/geoera/ref/8086
references: https://data.geoscience.earth/ncl/geoera/ref/8035
references: https://data.geoscience.earth/ncl/geoera/ref/8039
type: Concept
created: 2021-03-03T16:08:15.581Z
definition: A zone of deep, crustal-scale faults delineating the eastern border of the TESZ: a great tectonic boundary defined in regional scale confirmed by deep seismic experiments, regional magnetic and grawimetric mapping.
definition: Strefa głębokich rozłamów stanowiąca wschodnią granicę TESZ, zdefiniowana na podstawie głębokich profilowań sejsmicznych oraz regionalnych map anomalii magnetycznych i grawimetrycznych. @pl
preferred label: Strefa uskokowa Teisseyre-Tornquista @pl
alternative label: Teisseyre-Tornquist zone
in scheme: Tectonic Boundary Objects in Europe
notation: PL-22000000
broader: Northern segment of the Trans-European suture zone

T-T fault zone 1
created: 2021-03-03T16:08:15.585Z
type: Concept
in scheme: Tectonic Boundary Objects in Europe
notation: PL-22000001
broader: Teisseyre-Tornquist fault zone

Toruń–Radom fault zone
type: Concept
created: 2021-03-03T16:08:15.604Z
definition: Basement fault zone being the margin of the East European Craton, reactivated in T3–J1 and Late Cretaceous. Method of observation: seismic profiles. (Country Report fault code: B-12)
definition: Strefa uskoku podłoża stanowiąca krawędź kratonu wschodnioeuropejskiego, reaktywowanego w T3–J1 i późnej kredzie. Metoda obserwacji: profile sejsmiczne. (Kod uskoku w Raporcie krajowym projektu HIKE: B-12) @pl
preferred label: Strefa uskokowa Toruń–Radom @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8014
in scheme: Tectonic Boundary Objects in Europe
notation: PL-22030000
broader: Teisseyre-Tornquist fault zone

Koszalin–Toruń fault zone
type: Concept
created: 2021-03-03T16:08:15.600Z
definition: Northernmost segment of the TTZ being the edge of the EEC. Created in Early Paleozoic and reactivated in Cr2 and later(?). Method of observation: seismic profiles. Strike: NW–SE. (Country Report fault code: B- 2)
definition: Najbardziej na N wysunięty segment TTZ będący krawędzią kratonu wschonioeuropejskiego. Utworzony we wczesnym paleozoiku i reaktywowany w górnej kredzie lub później (?). Metoda obserwacji: profile sejsmiczne. Bieg: NW–SE. (Kod uskoku w Raporcie krajowym projektu HIKE: B- 2) @pl
preferred label: Strefa uskokowa Koszalin–Toruń @pl
references: https://data.geoscience.earth/ncl/geoera/ref/7999
references: https://data.geoscience.earth/ncl/geoera/ref/8017
in scheme: Tectonic Boundary Objects in Europe
notation: PL-22020000
broader: Teisseyre-Tornquist fault zone

Miastko–Świecie fault zone
type: Concept
created: 2021-03-03T16:08:15.597Z
definition: Faulted part of the EEC margin, with the heavily deformed Lower Paleozoic complex, regarded as the front of the Caledonides. Method of observation: seismic profiles, gravimetry. Strike: NW–SE. (Country Report fault code: B-1)
definition: Zuskokowane obrzeże kratonu wschodnioeuropejskiego, z silnie zdeformowanym kompleksem dolnego paleozoiku, uważane za przedpole kaledonidów. Metoda obserwacji: profile sejsmiczne, grawimetria. Bieg: NW–SE. (Kod uskoku w Raporcie krajowym projektu HIKE: B-1) @pl
preferred label: Strefa uskokowa Miastko–Świecie @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8017
in scheme: Tectonic Boundary Objects in Europe
notation: PL-22010000
broader: Teisseyre-Tornquist fault zone

T-T fault zone 4
type: Concept
created: 2021-03-03T16:08:15.594Z
in scheme: Tectonic Boundary Objects in Europe
notation: PL-22000004
broader: Teisseyre-Tornquist fault zone

T-T fault zone 3
type: Concept
created: 2021-03-03T16:08:15.591Z
in scheme: Tectonic Boundary Objects in Europe
notation: PL-22000003
broader: Teisseyre-Tornquist fault zone

T-T fault zone 2
type: Concept
created: 2021-03-03T16:08:15.588Z
in scheme: Tectonic Boundary Objects in Europe
notation: PL-22000002
broader: Teisseyre-Tornquist fault zone

Pomeranian Swell
type: Concept
created: 2021-03-03T16:08:15.608Z
definition: Uplifted and elongated tectonic domain (anticlinorium) about 14000 sq. km in area, forming the NW segment of the Mid-Polish Swell/anticlinorium. Its NW part is characterized by multidirectional faults, occurrence of Late Triassic – Early Jurassic synsedimentary grabens and half-grabens incorporated into the overall anticlinorium architecture, the lack of regional salt tectonics, and reduced sequences of the Zechstein and Mesozoic strata. The SE part is marked by well developed non-piercement salt domes of WNW–ESE to NW–SE trends, separated by the extensive zones out of which the Zechstein salts have been completely or almost completely squeezed. The intensity of salt tectonics increases towards SE, where isolated salt pillows merge into elongated salt swells in which the thickness of tectonically accumulated salts exceeds 2000 m.
definition: Wypiętrzona i wydłużona jednostka tektoniczna o powierzchni ok. 14 000 km2, tworząca północno-zachodni odcinek wyniesienia środkowopolskiego. Jej północno-zachodnia część charakteryzuje się wielokierunkowymi uskokami, występowaniem rowów i półrowów synsedymentacyjnych w późnym triasie i wczesnej jurze, brakiem regionalnej tektoniki solnej oraz zredukowanymi sekwencjami warstw cechsztyńskich i mezozoicznych. Część południowo-wschodnia charakteryzuje się dobrze rozwiniętymi nie-przebijającymi wysadami solnymi o kierunkach od WNW–ESE do NW–SE, oddzielonymi rozległymi strefami, z których całkowicie lub prawie całkowicie wyciśnięte zostały sole cechsztyńskie. Intensywność tektoniki solnej rośnie w kierunku południowo-wschodnim, gdzie izolowane poduszki solne łączą się w wydłużone wały solne, w których miąższość soli spiętrzonych tektonicznie przekracza 2000 m. @pl
preferred label: Wyniesienie Pomorza @pl
narrower: Kołobrzeg fault zone
narrower: Trzebiatów fault zone
narrower: Wysoka Kamieńska fault
narrower: Gryfice–Więcbork fault zone
narrower: Drawsko Pomorskie–Szubin fault zone
narrower: Nowogard–Adler fault zone
references: https://data.geoscience.earth/ncl/geoera/ref/8016
in scheme: Tectonic Boundary Objects in Europe
notation: PL-23000000
broader: Northern segment of the Trans-European suture zone

Wysoka Kamieńska fault
type: Concept
created: 2021-03-03T16:08:15.619Z
definition: T3–J1 graben reactivated in Cr2 related to the slip accommodation of the Kamień–Adler basement strike-slip fault zone. Method of observation: seismic profiles. Strike: WNW–ESE. (Country Report fault code: B-5)
definition: Rów T3 – J1 reaktywowany w Cr2 związany z lokalizacją przesuwczej strefy uskokowej podłoża Kamień–Adler. Metoda obserwacji: profile sejsmiczne. Bieg: WNW–ESE. (Kod uskoku w Raporcie krajowym projektu HIKE: B-5) @pl
preferred label: Uskok Wysoka Kamieńska @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8011
references: https://data.geoscience.earth/ncl/geoera/ref/8014
in scheme: Tectonic Boundary Objects in Europe
notation: PL-23030000
broader: Pomeranian Swell

Trzebiatów fault zone
type: Concept
created: 2021-03-03T16:08:15.615Z
definition: Uskoki ograniczające zachowane fragmenty kompleksu kredowego pośrodku wału środkowopolskiego (wał pomorski). Metoda obserwacji: profile sejsmiczne. Bieg: NW–SE. (Kod uskoku w Raporcie krajowym projektu HIKE: B-4) @pl
preferred label: Strefa uskokowa Trzebiatowa @pl
references: https://data.geoscience.earth/ncl/geoera/ref/7999
references: https://data.geoscience.earth/ncl/geoera/ref/8013
in scheme: Tectonic Boundary Objects in Europe
definition: Bounding remnants of the Cretaceous complex in the middle of the Mid-Polish Swell/anticlinorium (Pomeranian Swell segment). Method of observation: seismic profiles. Strike: NW–SE. (Country Report fault code: B-4)
notation: PL-23020000
broader: Pomeranian Swell

Kołobrzeg fault zone
type: Concept
created: 2021-03-03T16:08:15.612Z
definition: Basement fault zone reactivated in the Mesozoic, linking two larger fault zones. Method of observation: seismic profiles. Strike: N–S. (Country Report fault code: B-3)
definition: Strefa uskokowa podłoża, reaktywowana w mezozoiku, łącząca dwie większe strefy uskokowe. Metoda obserwacji: profile sejsmiczne. Bieg: N–S. (Kod uskoku w Raporcie krajowym projektu HIKE: B-3) @pl
preferred label: Strefa uskokowa Kołobrzegu @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8014
references: https://data.geoscience.earth/ncl/geoera/ref/8022
in scheme: Tectonic Boundary Objects in Europe
notation: PL-23010000
broader: Pomeranian Swell

Nowogard–Adler fault zone
type: Concept
created: 2021-03-03T16:08:15.629Z
definition: Uskok podłoża ograniczający od strony południowo-zachodniej wał środkowopolski (wał pomorski) . W T3–J1 uskok ten kontrolował rozwój rowów typu en echelon. Niewielka reaktywacja w późnej kredzie. Opisywany obiekt stanowi granicę wału pomorskiego i niecki szczecińskiej. Metoda obserwacji: profile sejsmiczne. Bieg: NW–SE. (Kod uskoku w Raporcie krajowym projektu HIKE: B-8) @pl
preferred label: Strefa uskokowa Nowogard–Adler @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8013
references: https://data.geoscience.earth/ncl/geoera/ref/8022
in scheme: Tectonic Boundary Objects in Europe
definition: Basement fault bounding Mid-Polish Swell/anticlinorium (Pomeranian Swell segment) from the SW. In the T3–J1 this fault controlled development of en echelon horse-tail grabens. Minor reactivation in the Late Cretaceous. Described structure is a border of Pomeranian Swell (anticlinorium) and Szczecin Trough (synclinorium). Method of observation: seismic profiles. Strike: NW–SE. (Country Report fault code: B-8)
notation: PL-23060000
broader: Pomeranian Swell

Drawsko Pomorskie–Szubin fault zone
type: Concept
created: 2021-03-03T16:08:15.626Z
definition: Basement fault zone with traces of reactivation in Mesozoic. (Country Report fault code: B-7)
definition: Strefa uskoku podłoża ze śladami reaktywacji w mezozoiku. (Kod uskoku w Raporcie krajowym projektu HIKE: B-7) @pl
preferred label: Strefa uskokowa Rawsko Pomorskie–Szubin @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8014
in scheme: Tectonic Boundary Objects in Europe
notation: PL-23050000
broader: Pomeranian Swell

Gryfice–Więcbork fault zone
type: Concept
created: 2021-03-03T16:08:15.622Z
definition: Presumed basement fault controlling the extent of the Carboniferous and location of salt pillows. Method of observation: seismic profiles, gravimetry. Strike: WNW–ESE. (Country Report fault code: B-6)
definition: Przypuszczalny uskok podłoża kontrolujący zasięg karbonu i usytuowanie poduszek solnych. Metoda obserwacji: profile sejsmiczne, grawimetria. Bieg: WNW–ESE. (Kod uskoku w Raporcie krajowym projektu HIKE: B-6) @pl
preferred label: Strefa uskokowa Gryfice–Więcbork @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8060
in scheme: Tectonic Boundary Objects in Europe
notation: PL-23040000
broader: Pomeranian Swell

Kujavian Swell
type: Concept
created: 2021-03-03T16:08:15.648Z
definition: Kujavian Swell (anticlinorium) is the middle part of the (NW-SE oriented) Mid-Polish Swell/anticlinorium, structurally deeper than its immediate NW (Pomeranian Swell segment) and SE counterparts.
definition: Wyniesienie kujawskie jest częścią antyklinorium śródpolskiego, strukturalnie głębszą od przyległych od NW I SE. @pl
preferred label: Wyniesienie kujawskie @pl
narrower: Brześć Kujawski–Kutno–Rawa Mazowiecka fault zone
narrower: Piotrków Trybunalski–Kłodawa–Bydgoszcz fault zone
narrower: Zgierz–Końskie fault zone
references: https://data.geoscience.earth/ncl/geoera/ref/8125
in scheme: Tectonic Boundary Objects in Europe
notation: PL-25000000
broader: Northern segment of the Trans-European suture zone

Zgierz–Końskie fault zone
type: Concept
created: 2021-03-03T16:08:15.660Z
definition: Probably Palaeozoic basement fault zone reactivated in the Mesozoic. Method of observation: seismic profiles. Strike: NW–SE. (Country Report fault code: B-21)
definition: Strefa uskokowa prawdopodobnie powstała w podłożu paleozoicznym, reaktywowana w mezozoiku. Metoda obserwacji: profile sejsmiczne. Bieg: NW–SE. (Kod uskoku w Raporcie krajowym projektu HIKE: B-21) @pl
preferred label: Strefa uskokowa Zgierz–Końskie @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8014
references: https://data.geoscience.earth/ncl/geoera/ref/8022
in scheme: Tectonic Boundary Objects in Europe
notation: PL-25030000
broader: Kujavian Swell

Piotrków Trybunalski–Kłodawa–Bydgoszcz fault zone
type: Concept
created: 2021-03-03T16:08:15.656Z
definition: Sigmoidalna strefa uskokowa mająca swoje korzenie w podłożu, reaktywowana w T3 – J1 jako strefa przesuwcza i w trakcie inwersji późnokredowej. Opisana struktura stanowi granicę wału kujawskiego i niecki łódzkiej. Metoda obserwacji: profile sejsmiczne. Bieg: NW–SE, N–S. (Kod uskoku w Raporcie krajowym projektu HIKE: B-14) @pl
preferred label: Strefa uskokowa Piotrków Trybunalski–Kłodawa–Bydgoszcz @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8014
references: https://data.geoscience.earth/ncl/geoera/ref/8022
in scheme: Tectonic Boundary Objects in Europe
definition: Sigmoidal fault zone rooted in the basement, reactivated in the T3–J1 wrenching phase and during the Cr2 inversion phase. Described structure is a border of Kujavian Swell (anticlinorium) and Łódź Trough (synclinorium). Method of observation: seismic profiles. Strike: NW–SE, N–S. (Country Report fault code: B-14)
notation: PL-25020000
broader: Kujavian Swell

Brześć Kujawski–Kutno–Rawa Mazowiecka fault zone
type: Concept
created: 2021-03-03T16:08:15.652Z
definition: Basement fault zone reactivated in the Mesozoic complex marked by the array of salt pillows and brachyanticlines partially teared out by faults. Method of observation: seismic profiles. Strike: NW–SE. (Country Report fault code: B-13)
definition: Strefa uskoków podłoża, reaktywowana w mezozoiku, gdzie wyznacza szereg poduszek solnych i brachyantyklin, częściowo poprzecinanych uskokami. Metoda obserwacji: profile sejsmiczne. Bieg: NW–SE. (Kod uskoku w Raporcie krajowym projektu HIKE: B-13) @pl
preferred label: Strefa uskokowa Brześć Kujawski–Kutno–Rawa Mazowiecka @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8014
references: https://data.geoscience.earth/ncl/geoera/ref/8022
in scheme: Tectonic Boundary Objects in Europe
notation: PL-25010000
broader: Kujavian Swell

Sorgenfrei-Tornquist fault zone
references: https://data.geoscience.earth/ncl/geoera/ref/8110
references: https://data.geoscience.earth/ncl/geoera/ref/8063
type: Concept
created: 2021-03-03T16:08:15.572Z
definition: Tectonic boundary interpreted from BABEL deep seismic experiment usually described as NW part of the TTZ (in Denmark and/or Sweden).
definition: Granica tektoniczna interpretowana na podstawie głębokiego eksperymentu sejsmicznego BABEL, zwykle opisywana jako północno-zachodnia część TTZ (w Danii i / lub Szwecji). @pl
preferred label: Strefa Sorgenfrei'a-Tornquista @pl
alternative label: Sorgenfrei-Tornquist Zone
narrower: S-T fault zone 1
narrower: S-T fault zone 2
in scheme: Tectonic Boundary Objects in Europe
notation: PL-21000000
broader: Northern segment of the Trans-European suture zone

S-T fault zone 2
type: Concept
created: 2021-03-03T16:08:15.578Z
in scheme: Tectonic Boundary Objects in Europe
notation: PL-21000002
broader: Sorgenfrei-Tornquist fault zone

S-T fault zone 1
type: Concept
created: 2021-03-03T16:08:15.575Z
in scheme: Tectonic Boundary Objects in Europe
notation: PL-21000001
broader: Sorgenfrei-Tornquist fault zone

Szczecin Trough
type: Concept
created: 2021-03-03T16:08:15.633Z
definition: Szczecin Trough is an assymetric synclinorium bordering on the Fore-Sudetic homocline to the SW and the Mid-Polish Swell/anticlinorium (Pomeranian Swell) to the NE. Upper Palaeozoic and Mesozoic rocks form the backbone of this structure.
definition: Niecka szczecińska od SW graniczy z monokliną przedsudecką, a od NE z antyklinorium środkowopolskim. Jest to struktura asymetryczna, zbudowana ze skał młodszego paleozoiku i mezozoiku. @pl
preferred label: Niecka szczecińska @pl
narrower: Stralsund–Wolin fault zone
narrower: Rostock–Szczecin fault zone
narrower: Drawno–Poznań fault zone
references: https://data.geoscience.earth/ncl/geoera/ref/8125
in scheme: Tectonic Boundary Objects in Europe
notation: PL-24000000
broader: Northern segment of the Trans-European suture zone

Drawno–Poznań fault zone
type: Concept
created: 2021-03-03T16:08:15.644Z
definition: Reaktywowany na przełomie T3–J1 duży uskok podłoża, uruchamiający ciąg wysadów solnych ułożonych w ciąg typu en echelon (Szamotuły–Człopa); nieznacznie reaktywowany w Cr2. Opisywana struktura wyznacza granicę niecki szczecińskiej i łódzkiej. Metoda obserwacji: profile sejsmiczne. Bieg: NW–SE. (Kod uskoku w Raporcie krajowym projektu HIKE: B-11) @pl
preferred label: Strefa uskokowa Drawno–Poznań @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8014
in scheme: Tectonic Boundary Objects in Europe
definition: Major basement fault reactivated in T3–J1, creating en echelon array of salt diapirs (Szamotuły–Człopa), with minor reactivation in the Cr2. Described structure is a border of Szczecin Trough (synclinorium) and Łódź Trough (synclinorium). Method of observation: seismic profiles. Strike: NW–SE. (Country Report fault code: B-11)
notation: PL-24030000
broader: Szczecin Trough

Rostock–Szczecin fault zone
type: Concept
created: 2021-03-03T16:08:15.641Z
definition: Limit of the zone of intense faulting in the Baltic region and a relatively more stable Gorzów Block to the SW, i.e. the border of Szczecin Trough (synclinorium) and Gorzów block. Method of observation: seismic profiles. Strike: WNW–ESE. (Country Report fault code: B-10)
definition: Granica strefy pomiędzy intensywnie zuskokowanym rejonem bałtyckim i relatywnie stabilniejszym blokiem Gorzowa na SW, czyli granica niecki szczecińskiej i bloku Gorzowa. Metoda obserwacji: profile sejsmiczne. Bieg: WNW–ESE. (Kod uskoku w Raporcie krajowym projektu HIKE: B-10) @pl
preferred label: Strefa uskokowa Rostock–Szczecin @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8022
in scheme: Tectonic Boundary Objects in Europe
notation: PL-24020000
broader: Szczecin Trough

Stralsund–Wolin fault zone
type: Concept
created: 2021-03-03T16:08:15.637Z
definition: An array of en echelon faults in the Paleozoic basement and the Mesozoic cover. Method of observation: seismic profiles. Strike: WNW–ESE. (Country Report fault code: B-9)
definition: Zespół uskoków typu en echelon, rozwinięty w podłożu paleozoicznym i pokrywie mezozoicznej. Metoda obserwacji: profile sejsmiczne. Bieg: WNW–ESE. (Kod uskoku w Raporcie krajowym projektu HIKE: B-9) @pl
preferred label: Strefa uskokowa Stralsund–Wolin @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8022
in scheme: Tectonic Boundary Objects in Europe
notation: PL-24010000
broader: Szczecin Trough

Southern segment of the Trans-European Suture Zone
type: Concept
created: 2021-03-03T16:08:15.691Z
definition: Southern part of the Trans-European suture zone (TESZ). TESZ is a litospheric-scale tectonic suture between the East European Craton and the Palaeozoic West European Platform.
definition: Południowa część TESZ. TESZ to szew tektoniczny stanowiący granicę między kratonem wschodnioeuropejskim a platformą paleozoiczną Europy Zachodniej. @pl
preferred label: Południowa część strefy szwu transeuropejskiego @pl
narrower: Kielce tectonic domain
narrower: Łysogóry tectonic domain
narrower: Puławy Trough
narrower: Małopolska Massif
narrower: Nida Trough
references: https://data.geoscience.earth/ncl/geoera/ref/8086
in scheme: Tectonic Boundary Objects in Europe
notation: PL-30000000
broader: Tectonic Boundary in Poland

Puławy Trough
type: Concept
created: 2021-03-03T16:08:15.754Z
definition: Niecka puławska należy do synklinoruym kościerzyńsko-puławskiego, leżącego po NE stronie wału środkowopolskiego. @pl
preferred label: Niecka puławska @pl
narrower: Iłża–Biłgoraj fault zone
references: https://data.geoscience.earth/ncl/geoera/ref/8081
definition: Puławy Trough is the SE part of the Kościerzyna–Puławy synclinorium, bounding the Mid-Polish Swell/anticlinorium on the NE.
in scheme: Tectonic Boundary Objects in Europe
notation: PL-33000000
broader: Southern segment of the Trans-European Suture Zone

Iłża–Biłgoraj fault zone
type: Concept
created: 2021-03-03T16:08:15.758Z
definition: The multi-stage fault zone at the boundary between two local domains: Radom–Kraśnik and Biłgoraj–Narol Blocks. It belongs to the TTZ (thus the edge of the EEC). The last significant phase of reactivation was in the end of the Cretaceous. Described structure is a border of Puławy Trough (synclinorium) and the Mid-Polish Swell (anticlinorium). Method of observation: seismic profiles, borehole data. Strike: NW–SE to WNW–ESE. (Country Report fault code: C-8)
definition: Wielostopniowa strefa uskokowa na pograniczu dwóch jednostek lokalnych: bloków Radom–Kraśnik i Biłgoraj–Narol. Należy do strefy TTZ (a więc skraju kratonu wschodnioeuropejskiego). Ostatnia znacząca faza reaktywacji miała miejsce w końcu kredy. Strefa uskokowa Iłża–Biłgoraj stanowi granicę niecki puławskiej i wału środkowopolskiego. Metody obserwacji: profile sejsmiczne, dane z otworów wiertniczych. Bieg: NW–SE do WNW–ESE. (Kod uskoku w Raporcie krajowym projektu HIKE: C-8) @pl
preferred label: Strefa uskokowa Iłża–Biłgoraj @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8003
in scheme: Tectonic Boundary Objects in Europe
notation: PL-33010000
broader: Puławy Trough

Kielce tectonic domain
type: Concept
created: 2021-03-03T16:08:15.695Z
definition: Southern region of the palaeozoic core of the Holy Cross Mountains, to the north limited by the Łysogóry thrust, to the south probably limited by the Lasocin–Strzelce fault zone that includes also the Chmielnik fault. Its northern sub-region, composed primarily of Devonian and Carboniferous rocks, is called the Kielce–Łagów synclinorium and its southern sub-region the Chęciny–Klimontów anticlinorium. The whole region is composed of Palaeozoic rocks of Lower Cambrian to Lower Carboniferous, deformed during the Caledonian and Variscan orogenies. Dense network of faults striking predominantly WNW–ESE, N–S and NNE–SSW cross-cuts it entirely. Caledonian deformation produced diabase and lamprophyre intrusions, Variscan deformations produced lamprophyres. Methods of observation: boreholes, geophysical data, geological maps, NMT, outcrops.
definition: Południowy region w obrębie trzonu paleozoicznego Gór Świętokrzyskich, od północy ograniczony nasunięciem łysogórskim, a od południa najprawdopodobniej strefą uskokową Lasocin–Strzelce, w której skład wchodzi także uskok Chmielnika. Północna część regionu, zbudowana głównie ze skał dewońskich i karbońskich, określana jest jako subregion synklinorium kielecko-łagowskie, a południowa część jako subregion antyklinorium chęcińsko-klimontowskie. Region zbudowany jest ze zdeformowanych w trakcie orogenezy kaledońskiej i waryscyjskiej skał paleozoicznych od kambru starszego po karbon dolny. Region pocięty jest gęstą siecią uskoków o dominujących kierunkach WNW–ESE oraz N–S i NNE–SSE. Z ruchami kaledońskimi związane są intruzje diabazów i lamprofirów, a z ruchami waryscyjskimi związane są intrucje lamprofirów. Metody obserwacji: wiercenia, dane geofizyczne, mapy geologiczne, NMT, odsłonięcia. @pl
preferred label: Jednostka kielecka @pl
narrower: Lasocin–Strzelce fault zone
narrower: Dyminy fault zone
narrower: Szydłówek fault zone
narrower: Bardo fault zone
references: https://data.geoscience.earth/ncl/geoera/ref/8006
references: https://data.geoscience.earth/ncl/geoera/ref/8108
in scheme: Tectonic Boundary Objects in Europe
notation: PL-31000000
broader: Southern segment of the Trans-European Suture Zone

Dyminy fault zone
type: Concept
created: 2021-03-03T16:08:15.710Z
definition: Fault zone overlapping a fold built of the Cambrian, Ordovician and Silurian rocks. It was subject to the main Caledonian activation phase and most likely Variscan reactivation of faults framing the structure from the N and the S. Method of observation: geological mapping, NMT, outcrops. Strike: E–W. (Country Report fault code: C-2)
definition: Strefa uskokowa nasuwająca się na fałd zbudowany ze skał kambru, ordowiku i syluru. Główna faza aktywacji strefy uskokowej – kaledońska i, najprawdopodobniej, reaktywacja w czasie ruchów waryscyjskich uskoków otaczających strukturę od strony północnej i południowej. Metoda obserwacji: kartowanie geologiczne, NMT, odsłonięcia. Bieg: E–W. (Kod uskoku w Raporcie krajowym projektu HIKE: C-2) @pl
preferred label: Strefa uskokowa Dymin @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8006
references: https://data.geoscience.earth/ncl/geoera/ref/7993
in scheme: Tectonic Boundary Objects in Europe
notation: PL-31020000
broader: Kielce tectonic domain

Lasocin–Strzelce fault zone
type: Concept
created: 2021-03-03T16:08:15.700Z
definition: Strefa uskokowa aktywna od dolnego paleozoiku do neogenu. Najbardziej intensywne deformacje miały miejsce w okresie waryscyjskim i alpejskim. Kinematyka uskoków była zmienna – od transtensji do transpresji. Opisywana struktura stanowi granicę między jednostką kielecką a blokiem małopolskim. Metody obserwacji: grawimetria, dane otworowe, kartowanie geologiczne, NMT, odsłonięcia. Bieg: NW–SE. (Kod uskoku w Raporcie krajowym projektu HIKE: C-1) @pl
preferred label: Strefa uskokowa Lasocin–Strzelce @pl
narrower: Zbrza fault
references: https://data.geoscience.earth/ncl/geoera/ref/8077
definition: Multiple faults reactivated starting from the Lower Palaeozoic up to the Neogene. The most intense deformations during the Variscan and Alpine stages. Variable kinematics – from transtension to transpression. Described structure is a border of Kielce tectonic domain [pl: Jednostka Kielecka] and Małopolska Block. Method of observation: gravimetry, borehole data, geological Mapping, NMT, outcrops. Strike: NW–SE. (Country Report fault code: C-1)
in scheme: Tectonic Boundary Objects in Europe
notation: PL-31010000
broader: Kielce tectonic domain

Zbrza fault
type: Concept
created: 2021-03-03T16:08:15.704Z
definition: High-angle reverse fault dipping to the SSW. Along it, the Palaeozoic and (partly) Mesozoic rocks are thrusted towards the NNE and the NE over the Mesozoic strata filling the Piotrkowice syncline. This fault is most probably a Variscan structure, intensly rejuvenated during the Alpine orogeny. Method of observation: gravimetry, borehole data, geological Mapping, NMT, outcrops. Strike: NW–SE. (Country Report fault code: C-1)
definition: Wysokokątowy uskok odwrócony zapadający w kierunku SSW. Wzdłuż uskoku skały paleozoiczne i (częściowo) mezozoiczne przesuwane są w kierunku NNE i NE na warstwy mezozoiczne wypełniające synklinę Piotrkowicką. Uskok ten jest najprawdopodobniej strukturą waryscyjską, intensywnie odmładzaną podczas orogenezy alpejskiej. Metody obserwacji: grawimetria, dane otworowe, kartowanie geologiczne, NMT, odsłonięcia. Bieg: NW–SE. (Kod uskoku w Raporcie krajowym projektu HIKE: C-1) @pl
preferred label: Uskok Zbrzy @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8077
references: https://data.geoscience.earth/ncl/geoera/ref/8029
references: https://data.geoscience.earth/ncl/geoera/ref/8030
in scheme: Tectonic Boundary Objects in Europe
notation: PL-31011000
broader: Lasocin–Strzelce fault zone

Bardo fault zone
type: Concept
created: 2021-03-03T16:08:15.725Z
definition: A zone of subparallel strike-slip faults with complex kinematics: from transtension (with igneous rocks intrusions) to transpression. The zone was formed during the Caledonian compressive stage. Described structure is a border of Kielce tectonic domain [pl: Jednostka Kielecka] and Carpathian Foredeep. Method of observation: gravimetry, borehole data, geological mapping, outcrops. Strike: WNW–ESE. (Country Report fault code: C-7)
definition: Strefa równoległych uskoków przesuwczych o złożonej kinematyce: od transtensji (z intruzjami skał magmowych) do transpresji. Strefa powstała podczas kaledońskich ruchów kompresyjnych. Opisywana struktura stanowi granicę jednostki kieleckiej i zapadliska przedkarpackiego. Metody obserwacji: grawimetria, dane z otworów wiertniczych, kartografia geologiczna, wychodnie. Bieg: WNW–ESE. (Kod uskoku w Raporcie krajowym projektu HIKE: C-7) @pl
preferred label: Strefa uskokowa Barda @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8109
in scheme: Tectonic Boundary Objects in Europe
notation: PL-31040000
broader: Kielce tectonic domain

Szydłówek fault zone
type: Concept
created: 2021-03-03T16:08:15.715Z
definition: A series of thrusts directed towards the SSW and back-thrusts directed towards the NNE. Formed in the Variscan Late Carboniferous compressive stage. Along the frontal thrust, tectonically deformed Silurian and Lower Devonian rocks overlap the Upper Devonian rocks. Method of observation: gravimetry, borehole data, geological mapping, outcrops, NMT. Strike: E–W. (Country Report fault code: C-3)
definition: Seria nasunięć w kierunku SSW i nasunięć wstecznych skierowanych ku NNE. Powstały w fazie kompresji waryscyjskiej, późnokarbońskiej. Wzdłuż czoła na skały górnego dewonu zachodzą tektonicznie zdeformowane skały syluru i dolnego dewonu. Metody obserwacji: grawimetria, dane z otworów wiertniczych, kartografia geologiczna, odsłonięcia, NMT. Bieg: E–W. (Kod uskoku w Raporcie krajowym projektu HIKE: C-3) @pl
preferred label: Strefa uskokowa Szydłówka @pl
narrower: Szydłówek fault
references: https://data.geoscience.earth/ncl/geoera/ref/8006
references: https://data.geoscience.earth/ncl/geoera/ref/8007
in scheme: Tectonic Boundary Objects in Europe
notation: PL-31030000
broader: Kielce tectonic domain

Szydłówek fault
type: Concept
created: 2021-03-03T16:08:15.721Z
definition: Thrust to transpressive fault limiting the Szydłówek fault zone from the south. Along it Lower Palaeozoic (Silurian) and Lower Devonian rocks are thrusted over the Upper Devonian and Carboniferous rocks of Kielce syncline. The fault is a medium-angle structure dippig towards the N and NNE. Methods of observation: outcrops, boreholes, geologic map interpretation, NMT.
definition: Uskok nasuwczy do transpresyjnego, ograniczjący od południa strefę uskokową Szydłówka. Wzdłuż jego powierzchni skały starszego paleozoiku (syluru) i starszego dewonu nasunięte są na skały dewonu młodszego i karbonu synkliny kieleckiej. Powierzchnia uskokowa zapada pod średnimi kątami w kierunku N i NNE. Metody obserwacji: odsłonięcia, wiercenia, interpretacja mapy geologicznej, NMT. @pl
preferred label: Uskok Szydłówka @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8006
in scheme: Tectonic Boundary Objects in Europe
notation: PL-31031000
broader: Szydłówek fault zone

Nida Trough
type: Concept
created: 2021-03-03T16:08:15.778Z
definition: Niecka Nidy to południowo-wschodnia część synclinorium szczecińsko-miechowskiego, graniczącego z wałem środkowopolskim od SW. @pl
preferred label: Niecka nidziańska @pl
narrower: Jędrzejów-Rzeszów fault set
narrower: Bębica fault zone
narrower: Tarnów fault zone
references: https://data.geoscience.earth/ncl/geoera/ref/8081
definition: Nida Trough (synclinorium) is the SE part of the Szczecin–Miechów synclinorium, bordering the Mid-Polish Swell (anticlinorium) on the SW.
in scheme: Tectonic Boundary Objects in Europe
notation: PL-35000000
broader: Southern segment of the Trans-European Suture Zone

Tarnów fault zone
type: Concept
created: 2021-03-03T16:08:15.789Z
definition: A set of basement faults, reactivated in the Mesozoic and only slightly in the Miocene. It sets the trend of the large paleo-valley in the basement of the foredeep basin in front of the Carpathians. Method of observation: seismic profiles, borehole data. Strike: WNW–ESE. (Country Report fault code: C-13)
definition: Zespół uskoków podłoża reaktywowanych w mezozoiku i tylko nieznacznie w miocenie. Wyznacza trend dużej paleo-doliny w podłożu głębokiego basenu na przedpolu Karpat. Metody obserwacji: profile sejsmiczne, dane z otworów wiertniczych. Bieg: WNW–ESE. (Kod uskoku w Raporcie krajowym projektu HIKE: C-13) @pl
preferred label: Strefa uskokowa Tarnowa @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8003
references: https://data.geoscience.earth/ncl/geoera/ref/8062
in scheme: Tectonic Boundary Objects in Europe
notation: PL-35030000
broader: Nida Trough

Bębica fault zone
type: Concept
created: 2021-03-03T16:08:15.785Z
definition: A set of basement faults, reactivated in the Mesozoic and only slightly in the Miocene. It sets the trend of the large Pilsno paleo-valley in the basement of the foredeep basin in front of the Carpathians. Method of observation: seismic profiles, borehole data. Strike: WNW–ESE. (Country Report fault code: C-13)
definition: Zespół uskoków podłoża reaktywowanych w mezozoiku i tylko nieznacznie w miocenie. Wyznacza trend dużej paleo-doliny Pilzna w podłożu głębokiego basenu na przedpolu Karpat. Metody obserwacji: profile sejsmiczne, dane z otworów wiertniczych. Bieg: WNW–ESE. (Kod uskoku w Raporcie krajowym projektu HIKE: C-13) @pl
preferred label: Strefa uskokowa Bębicy @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8003
references: https://data.geoscience.earth/ncl/geoera/ref/8062
in scheme: Tectonic Boundary Objects in Europe
notation: PL-35020000
broader: Nida Trough

Jędrzejów-Rzeszów fault set
type: Concept
created: 2021-03-03T16:08:15.781Z
definition: A set of basement faults, reactivated in Mesozoic and only slightly in the Miocene. Method of observation: seismic profiles, borehole data. Strike: WNW–ESE. (Country Report fault code: C-12)
definition: Zespół uskoków podłoża reaktywowanych w mezozoiku i tylko nieznacznie w miocenie. Metody obserwacji: profile sejsmiczne, dane z otworów wiertniczych. Bieg: WNW–ESE. (Kod uskoku w Raporcie krajowym projektu HIKE: C-12) @pl
preferred label: Strefa uskokowa Jędrzejów–Rzeszów @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8003
in scheme: Tectonic Boundary Objects in Europe
notation: PL-35010000
broader: Nida Trough

Łysogóry tectonic domain
type: Concept
definition: Northern region of the Palaeozoic core of the Holy Cross Mountains, limited on the south by the Łysogóry thrust and on the north by the Skrzynna fault, composed of deformed Palaeozoic rocks of the Middle Cambrian to the Lower Carboniferous age. Structural style or this region is mostly due to the Variscan orogeny, but also arise, to some extent, from the Caledonian orogeny. The domain trends WNW–ESE and so do smaller sub-domains within it. Thrusts and transpression faults are located at the fronts of main folds whose limbs are thus displaced towards the SSW. This fold and thrust belt is criss-crossed by a dense network of high-angle, transverse (roughly N–S trending), strike-slip faults. Diabase intrusions into walls of tensional strike-slip faults are also related to Variscan displacements. Methods of observation: boreholes, geophysical data, geological maps, NMT, outcrops.
created: 2021-03-03T16:08:15.728Z
definition: Północny region trzonu paleozoicznego Gór Świętokrzyskich. Od południa ograniczony nasunięciem łysogórskim, a od północy uskokiem Skrzynna. Budują go zdeformowane tektonicznie skały paleozoiczne od kambru środkowego po karbon dolny. Styl strukturalny zawdzięczją w głównej mierze orogenezie waryscyjskiej, a w mniejszym stopniu także orogenezie kaledońskiej. Przebieg jednostki to WNW–ESE, jednostki niższego rzędu posiadają taką samą orientację przestrzenną. U czoła głównych elementów fałdowych ulokowane są uskoki nasuwcze i transpresyjne, przemieszczające skrzydła nasuwane ku SSW. Całość przecięta jest gęstą siecią stromych, subpołudnikowych uskoków przesuwczych, poprzecznych do przebiegu jednostki. Z ruchami waryscyjskimi związane były intruzje diabazów ulokowane w skrzydłach tensyjnych uskoków przesuwczych. Metody obserwacji: wiercenia, dane geofizyczne, mapy geologiczne, NMT, odsłonięcia. @pl
preferred label: Jednostka Łysogórska @pl
narrower: Łysogóry fault zone
narrower: Rudki fault set
narrower: Odrzywół–Jastrząb–Ćmielów Graben
references: https://data.geoscience.earth/ncl/geoera/ref/8006
references: https://data.geoscience.earth/ncl/geoera/ref/8087
in scheme: Tectonic Boundary Objects in Europe
notation: PL-32000000
broader: Southern segment of the Trans-European Suture Zone

Odrzywół–Jastrząb–Ćmielów Graben
type: Concept
created: 2021-03-03T16:08:15.747Z
definition: Rów tektoniczny, odpowiednik rowu lubelskiego, ograniczający od N region świętokrzyski. Rów wypełniony jest osadami młodszego dewonu i karbonu. Od północy ogranicza go, równoległy do uskoku Skrzynna, uskok Nowe Miasto–Iłża–Bałtów. Rów powstał w wyniku ruchów waryscyjskich, a odmłodzony został w trakcie ruchów alpejskich. Metody obserwacji: geofizyka, wiercenia. @pl
preferred label: Rów Odrzywół–Jastrząb–Ćmielów @pl
narrower: Skrzynna fault
references: https://data.geoscience.earth/ncl/geoera/ref/8057
definition: Tectonic graben which is a counterpart to the Lublin Trough (basin). It limits the Holy Cross region on the north and is filled with Late Devonian to Carboniferous sediments. Nowe Miasto–Iłża–Bałtów fault, parallel to the Skrzynna fault, limits it to the north. The Trough was formed during the Variscan orogeny and rejuvenated during the Alpine orogeny. Methods of observation: geophysics, borehole data.
in scheme: Tectonic Boundary Objects in Europe
notation: PL-32030000
broader: Łysogóry tectonic domain

Skrzynna fault
type: Concept
created: 2021-03-03T16:08:15.750Z
definition: The northern border of the Łysogóry tectonic domain [pl: Jednostka Łysogórska] and the Holy Cross Mountains. The Skrzynna fault shows circa 1300 m of vertical displacement in the Palaeozoic rocks. The hypothetical SE continuation of this zone is the NE boundary of the Małopolska Massif. Methods of observation: gravimetry, seismic profiles, borehole data, geological mapping. Strike: WNW–ESE. (Country Report fault code: C-6)
definition: Północna granica jednostki łysogórskiej i Gór Świętokrzyskich. Uskok Skrzynna wykazuje w skałach paleozoicznych około 1300 m przemieszczenia pionowego. Hipotetyczną kontynuacją tej strefy na SE jest północno-wschodnia granica bloku Małopolski. Metody obserwacji: grawimetria, profile sejsmiczne, dane otworowe, kartowanie geologiczne. Bieg: WNW–ESE. (Kod uskoku w Raporcie krajowym projektu HIKE: C-6) @pl
preferred label: Uskok Skrzynnej @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8057
in scheme: Tectonic Boundary Objects in Europe
notation: PL-32031000
broader: Odrzywół–Jastrząb–Ćmielów Graben

Rudki fault set
type: Concept
created: 2021-03-03T16:08:15.738Z
definition: Horse-tail fault set formed due to the Variscan dextral strike slip. The eastern wall of this zone is displaced over 3 km towards the south. Pyrite and uranium deposits in Rudki are located in the tensive NE wing of the structure. Method of observation: borehole data, geological interpretation, NMT, outcrops. Strike: N–S. (Country Report fault code: SE part of C-5)
definition: Zestaw uskoków o typie „końskiego ogona" utworzony w wyniku waryscyjskiego przesunięcia prawoskrętnego. Wschodnia część tej strefy jest przesunięta o ponad 3 km w kierunku południowym. Złoża pirytu i uranu w Rudkach znajdują się w NE skrzydle uskoku. Metody obserwacji: dane otworowe, interpretacja geologiczna, NMT, odsłonięcia. Bieg: N–S. (Kod uskoku w Raporcie krajowym projektu HIKE: SE część C-5) @pl
preferred label: Zespół uskoków Rudek @pl
narrower: Rudki fault
references: https://data.geoscience.earth/ncl/geoera/ref/8006
in scheme: Tectonic Boundary Objects in Europe
notation: PL-32020000
broader: Łysogóry tectonic domain

Rudki fault
type: Concept
created: 2021-03-03T16:08:15.742Z
definition: Main fault of the Rudki fault set. It limits the horse-tail set from the west in its northern part and from the east in its southern part. The structure is a high-angle, ca. N–S oriented, right-lateral fault, transverse to the Łysogóry tectonic domain [pl: Jednostka Łysogórska] trend. This fault was formed during the Variscan orogeny, its northern region was probably rejuvenated during the Alpine orogeny. Methods of observation: boreholes, geologic map interpretation, NMT, outcrops.
definition: Główny uskok w zespole uskoków Rudek. Ogranicza od zachodu strukturę typu koński ogon w jej północnej części, a od wschodu tą samą strukturę ale w jej południowej części. Jest to stromy, o południkowym przebiegu, prawoprzesuwczy uskok poprzeczny do przebiegu regionu łysogórskiego. Powstał w trakcie orogenezy waryscyjskiej. Prawdopodobnie jego N część odmłodzona w trakcie ruchów alpejskich. Metody obserwacji: otwory wiertnicze, interpretacja map geologicznych, NMT, odsłonięcia. @pl
preferred label: Uskok Rudek @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8006
references: https://data.geoscience.earth/ncl/geoera/ref/8007
in scheme: Tectonic Boundary Objects in Europe
notation: PL-32021000
broader: Rudki fault set

Łysogóry fault zone
type: Concept
created: 2021-03-03T16:08:15.732Z
definition: The overthrust of the folded Cambrian rocks of the Łysogóry tectonic domain [pl: Jednostka Łysogórska] onto the Lower Palaeozoic rocks of the Kielce tectonic domain [pl: Jednostka Kielecka]. Characterized by very low and low degree metamorphism. Multiple reactivation from the Lower Palaeozoic up to the Neogene. Its present trace at the surface is mostly due to the Variscan movements. Described structure is a border of Łysogóry and Kielce tectonic domains. Method of observation: gravimetry, geological mapping, NMT. Strike: WNW–ESE. (Country Report fault code: C-4)
definition: Nasunięcie pofałdowanych skał kambru jednostki łysogórskiej na skały dolnego paleozoiku jednostki kieleckiej. Charakteryzuje się bardzo niskim i niskim stopniem metamorfizmu. Wielokrotna reaktywacja od dolnego paleozoiku do neogenu. Obecny ślad strefy uskoku łysogórskiego na powierzchni jest głównie wynikiem ruchów waryscyjskich. Opisana strefa stanowi rozdziela jednostkę łysogórską i kielecką. Metody obserwacji: grawimetria, kartografia geologiczna, NMT. Bieg: WNW–ESE. (Kod uskoku w Raporcie krajowym projektu HIKE: C-4) @pl
preferred label: Strefa uskoku łysogórskiego @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8096
references: https://data.geoscience.earth/ncl/geoera/ref/8006
references: https://data.geoscience.earth/ncl/geoera/ref/8007
references: https://data.geoscience.earth/ncl/geoera/ref/8015
in scheme: Tectonic Boundary Objects in Europe
notation: PL-32010000
broader: Łysogóry tectonic domain

Małopolska Massif
type: Concept
created: 2021-03-03T16:08:15.762Z
definition: Małopolska Massif (block) is composed of magmatic and metamorphic rocks of the Precambrian basement and the Palaeozoic sedimentary cover. The latter show hiatuses and angular discontinuities. The tectonic fabric of the block is a basin-and-range type of structure. It is located between the Upper Silesia block to the SW and the fold-and-thrust belt of the Holy Cross Mountains to the NE.
definition: Masyw małopolski (blok małopolski) zbudowany jest z magmowych i metamorficznych skał podłoża prekambryjskiego I osadowych skał paleozoiku. W profilach utworów paleozoiku występują luki stratygraficzne (erozyjne) i niezgodności tektoniczne. Blok małopolski charakteryzuje się obecnością struktur zrębowych. Od SW sąsiaduje z blokiem górnośląskim, a od NE z pasmem fałdowym Gór Świętokrzyskich. @pl
preferred label: Masyw małopolski @pl
narrower: Sandomierz–Lubaczów fault zone
narrower: Ryszkowa–Wola fault zone
narrower: Przedbórz–Przemyśl fault system
references: https://data.geoscience.earth/ncl/geoera/ref/8125
in scheme: Tectonic Boundary Objects in Europe
notation: PL-34000000
broader: Southern segment of the Trans-European Suture Zone

Przedbórz–Przemyśl fault system
type: Concept
created: 2021-03-03T16:08:15.774Z
definition: Its NW segment bounds heavily deformed Mesozoic surroundings of the Holy Cross Mts. from the SW. Its middle segment creates the SW edge of Precambrian core of the Małopolska Massif. Described structure is a border of the Małopolska Massif and the Miechów Trough (synclinorium). Method of observation: seismic profiles, borehole data. Strike: WNW–ESE. (Country Report fault code: C-11)
definition: W NW części system uskoków ogranicza mocno zdeformowane SW mezozoiczne obrzeżenie Gór Świętokrzyskich. W środkowym odcinku tworzy południowo-zachodnią krawędź prekambryjskiego podłoża masywu małopolskiego. Opisana struktura stanowi granicę masywu małopolskiego i niecki miechowskiej. Metody obserwacji: profile sejsmiczne, dane z otworów wiertniczych. Bieg: WNW–ESE. (Kod uskoku w Raporcie krajowym projektu HIKE: C-11) @pl
preferred label: System uskoków Przedbórz–Przemyśl @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8003
in scheme: Tectonic Boundary Objects in Europe
notation: PL-34030000
broader: Małopolska Massif

Ryszkowa–Wola fault zone
type: Concept
created: 2021-03-03T16:08:15.770Z
definition: Old fault zone reactivated in the Miocene as a transpressive dextral zone rather than the transtensive sinistral one with minor displacement. Method of observation: seismic profiles, borehole data. Strike: NW–SE to WNW–ESE. (Country Report fault code: C-10)
definition: Stara strefa uskokowa reaktywowana w miocenie bardziej jako transpresyjna strefa prawoprzesuwcza niż transtensyjna, z niewielkim przemieszczeniem. Metody obserwacji: profile sejsmiczne, dane z otworów wiertniczych. Bieg: NW – SE do WNW – ESE. (Kod uskoku w Raporcie krajowym projektu HIKE: C-10) @pl
preferred label: Strefa uskokowa Ryszkowa–Wola @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8003
references: https://data.geoscience.earth/ncl/geoera/ref/8061
in scheme: Tectonic Boundary Objects in Europe
notation: PL-34020000
broader: Małopolska Massif

Sandomierz–Lubaczów fault zone
type: Concept
created: 2021-03-03T16:08:15.766Z
definition: Close to the Polish/Ukrainian border it is known as the Wielkie Oczy Graben which in fact is a half-graben downthrowing the SW wall by almost 1 km, in the Miocene. Method of observation: seismic profiles, borehole data. Strike: NW–SE to WNE–ESE. (Country Report fault code: C-9)
definition: Niedaleko granicy polsko-ukraińskiej znany jest jako rów Wielkie Oczy, który w istocie jest pół-rowem zrzucającym w miocenie swoje południowo-zachodnie skrzydło o prawie 1 km. Metody obserwacji: profile sejsmiczne, dane z otworów wiertniczych. Bieg: NW–SE do WNE–ESE. (Kod uskoku w Raporcie krajowym projektu HIKE: C-9) @pl
preferred label: Strefa uskokowa Sandomierz–Lubaczów @pl
references: https://data.geoscience.earth/ncl/geoera/ref/8003
in scheme: Tectonic Boundary Objects in Europe
notation: PL-34010000
broader: Małopolska Massif

Tectonic Boundary in Brandenburg
narrower: Fault Zones of the southern border of the North German Basin and Lausatian Block
narrower: Fault Zones in the central part of the North German Basin
narrower: Fracture Zones of the Northeastern border of the North German Basin
top concept of: Tectonic Boundary Objects in Europe
notation: DE-BB-0
scope note: All named tectonic boundary objects that are located (at least partly) in Brandenburg, are identified by an ID with the prefix „DE-BB“ listed in the notation. Fault systems and/or fault domains can cross political borders and are therefore shared by several countries. Therefore, they can contain faults from different countries, indicated by country-specific prefixes to the respective ID. In addition, as the concepts are also located in Germany, they may have an additional ID in form of „DE“ referring to a national Germany-wide dataset.
definition: Fault in Brandenburg displayed in the HIKE European fault database.
type: Concept
created: 2021-05-03T08:56:16.270Z
in scheme: Tectonic Boundary Objects in Europe

Fault Zones in the central part of the North German Basin
type: Concept
created: 2021-09-06T15:30:07.255Z
creator: schmar
notation: DE-BB-2
preferred label: Störungszonen im Zentralteil des Norddeutschen Beckens @de
definition: Fault zones in the central eastern part of the North German Basin (NGB) and the underlying basement. NGB : Intra-continental european basin, part of the Southern Permian Basin. Subsidence starting in Carboniferous. Inversion phases in Upper Cretaceous.
definition: Störungszonen des zentralen östlichen Teiles des Norddeutschen Beckens und dessen basement. Norddeutsches Becken: Teil der Mitteleuropäischen Senke. Intrakontinentale Senkungsstruktur ab dem Karbon. Inversionsphasen in der Oberkreide. @de
narrower: Fault Zones of the central eastern North German Basin striking NNE-SSW
narrower: Fault Zones of the central eastern North German Basin striking WNW-ESE
narrower: Fault Zones of the central eastern North German Basin striking E-W
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Brandenburg

Fault Zones of the central eastern North German Basin striking NNE-SSW
type: Concept
created: 2021-09-06T15:30:07.258Z
creator: schmar
notation: DE-BB-21
preferred label: Störungszonen des zentralen östlichen Beckens, Streichen NNE-SSW @de
definition: Fault zones and structure zones in the central eastern part of the North German Basin striking NNE-SSW.
definition: Störungs- und Strukturzonen im östlichen Zentralbereich des Norddeutschen Beckens. Streichen NNE-SSW. @de
narrower: Buckow-Oderhaff Fault Zone
narrower: Rheinsberg Deep Fracture System
narrower: Dannenwalde Fault
narrower: Wredenhagen Fault
narrower: Arendsee Lineament
narrower: Liebenwalde-Torgelow Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7996
in scheme: Tectonic Boundary Objects in Europe
broader: Fault Zones in the central part of the North German Basin

Rheinsberg Deep Fracture System
type: Concept
created: 2021-09-06T15:30:07.278Z
creator: schmar
notation: DE-BB-2102
preferred label: Rheinsberger Tiefenbruchsystem @de
definition: Broad fault system striking NNE-SSW striking consisting of several parallel basement faults and related structures in the sedimentary cover. Reaching from the German Main Escarpments in the South (DE-BB-01a) to the Northern border of the NEGB. Postulated basing on geophysical data (gravimetrics, magnetics, deep seismics) and structures in the sedimentary cover (connected salt structures and related faults). Activation of Permian salt especially following the Kotzen-Zechlin structure zone.
definition: NNE-SSW streichendes, breites Störungssystem im basement bestehend aus mehreren parallelen Störungszonen. Von den Mitteldeutschen Abbrüchen im Süden bis zur Nordgrenze der Norddeutschen Senke verlaufend. Postuliert basierend auf geophysikalischen Daten (Gravimetrie, Magnetik, tiefe Seismik) und Sekundärstrukturen im Deckgebirge. Aktivierung von Salztektonik insbesondere entlang der Kotzen-Zechliner Strukturzone. @de
narrower: Rheinsberg Fault
narrower: Mirow Fault
narrower: Kotzen-Zechlin Structural Zone
narrower: Neuruppin Fault
references: https://data.geoscience.earth/ncl/geoera/ref/12266
references: https://data.geoscience.earth/ncl/geoera/ref/12274
references: https://data.geoscience.earth/ncl/geoera/ref/7996
in scheme: Tectonic Boundary Objects in Europe
broader: Fault Zones of the central eastern North German Basin striking NNE-SSW

Mirow Fault
type: Concept
created: 2021-09-06T15:30:07.289Z
creator: schmar
notation: DE-BB-210202
preferred label: Mirower Störung @de
definition: NNE-SSW striking basement fault. Postulated basing on geophysical data (gravimetrics, magnetics, deep seismics).
definition: NNE-SSE streichende Störung im basement. Postuliert nach geophysikalischen Befunden (Gravimetrie, Magnetik, Tiefe Seismik). @de
references: https://data.geoscience.earth/ncl/geoera/ref/12271
references: https://data.geoscience.earth/ncl/geoera/ref/12264
in scheme: Tectonic Boundary Objects in Europe
broader: Rheinsberg Deep Fracture System

Kotzen-Zechlin Structural Zone
type: Concept
created: 2021-09-06T15:30:07.294Z
creator: schmar
notation: DE-BB-210203
preferred label: Kotzen-Zechliner Strukturzone @de
definition: NNE-SSW and N-S striking structural zone in the sedimentary cover of the Rheinsberg Deep Fracture system. NNE-SSW and N-E elongted faults and salt anticlinals with several diapirs.
definition: NNE-SSE und N-S streichende Strukturzone in jungpaläozoisch-mesozoischen Deckgebirge des Rheinsberger Tiefenbruchsystems. NNE-SSW und N-S orientierte Störungen und halokinetische Antiklinalstrukturen mit mehreren Diapiren. @de
references: https://data.geoscience.earth/ncl/geoera/ref/12274
references: https://data.geoscience.earth/ncl/geoera/ref/12272
in scheme: Tectonic Boundary Objects in Europe
broader: Rheinsberg Deep Fracture System

Rheinsberg Fault
type: Concept
created: 2021-09-06T15:30:07.284Z
creator: schmar
notation: DE-BB-210201
preferred label: Rheinsberger Störung @de
definition: NNE-SSW striking basement fault. Postulated basing on geophysical data (gravimetrics, magnetics, deep seismics).
definition: NNE-SSE streichende Störung im basement . Postuliert nach geophysikalischen Befunden (Gravimetrie, Magnetik, Tiefe Seismik). @de
references: https://data.geoscience.earth/ncl/geoera/ref/12271
references: https://data.geoscience.earth/ncl/geoera/ref/12264
references: https://data.geoscience.earth/ncl/geoera/ref/12272
in scheme: Tectonic Boundary Objects in Europe
broader: Rheinsberg Deep Fracture System

Neuruppin Fault
type: Concept
created: 2021-09-06T15:30:07.299Z
creator: schmar
notation: DE-BB-210204
preferred label: Neuruppiner Störung @de
definition: NNE-SSE striking basement fault. Postulated basing on geophysical data (gravimetrics, magnetics, deep seismics).
definition: NNE-SSE streichende Störung im basement. Postuliert nach geophysikalischen Befunden (Gravimetrie, Magnetik, Tiefe Seismik). @de
references: https://data.geoscience.earth/ncl/geoera/ref/12271
references: https://data.geoscience.earth/ncl/geoera/ref/12272
in scheme: Tectonic Boundary Objects in Europe
broader: Rheinsberg Deep Fracture System

Wredenhagen Fault
type: Concept
created: 2021-09-06T15:30:07.308Z
creator: schmar
notation: DE-BB-2104
preferred label: Wredenhagener Störung @de
definition: NNE-SSW striking fault zone in the basement. Postulated. Activation of salt tectonics (salt structures Wredenhagen and Königsberg).
definition: NNE-SSW streichende Störungszone im basement. Postuliert basierend auf geophysikalischen Daten und der Aktivierung von Salztektonik im Deckgebirge. @de
references: https://data.geoscience.earth/ncl/geoera/ref/7996
in scheme: Tectonic Boundary Objects in Europe
broader: Fault Zones of the central eastern North German Basin striking NNE-SSW

Arendsee Lineament
type: Concept
created: 2021-09-06T15:30:07.312Z
creator: schmar
notation: DE-BB-2105
preferred label: Arendsee Tiefenbruch @de
definition: NNE-SSW striking basement fault zone. Postulated basing on geophysical data (gravimetrics, magnetics, deep seismics).
definition: NNE-SSW streichende Störungszone im basement. Postuliert basierend auf geophysikalischen Daten (Gravimetrie, Magnetik, tiefe Seismik). @de
references: https://data.geoscience.earth/ncl/geoera/ref/12264
references: https://data.geoscience.earth/ncl/geoera/ref/12271
references: https://data.geoscience.earth/ncl/geoera/ref/7996
references: https://data.geoscience.earth/ncl/geoera/ref/8031
in scheme: Tectonic Boundary Objects in Europe
related: Arendsee Fault Zone
broader: Fault Zones of the central eastern North German Basin striking NNE-SSW

Dannenwalde Fault
type: Concept
created: 2021-09-06T15:30:07.303Z
creator: schmar
notation: DE-BB-2103
preferred label: Dannenwalder Störung @de
definition: NNE-SSW striking basement fault. Postulated basing on geophysical data (gravimetrics, magnetics, deep seismics). In the Lower Permian Southeastern border of the Graben structure Zehdenick-Gransee-Graben.
definition: NNE-SSW streichende Störungszone im basement. Postuliert basierend auf geophysikalischen Daten (Gravimetrie, Magnetik, tiefe Seismik). Im Rotliegend Südostgrenze der Grabenstruktur Zehdenick-Gransee. @de
references: https://data.geoscience.earth/ncl/geoera/ref/12271
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/12264
in scheme: Tectonic Boundary Objects in Europe
broader: Fault Zones of the central eastern North German Basin striking NNE-SSW

Buckow-Oderhaff Fault Zone
type: Concept
created: 2021-09-06T15:30:07.263Z
creator: schmar
notation: DE-BB-2101
preferred label: Buckow-Oderhaff-Störungszone @de
definition: NNE-SSW striking fault zone at the Eastern border of the NEGB. In the southern part (Buckow falt zone) reaching from the basement to the Cenozoic. In the Northern part (Oderhaff fault zone) only in the basement (postulated basing on geophysical data). Activation of salt tectonics along the fault zone.
definition: NNE-SSW streichende Störungszone an der Östlichen Grenze der Norddeutschen Senke. Im südlichen Teil (Buckower Störungszone) vom basement bis in Känozoikum verfolgbar. Im nördlichen Teil (Oderhaff Störungszone) im basement (postuliert auf der Basis geophysikalischer Daten). Aktivierung von permischen Salz entlang der Störungszone. @de
narrower: Buckow Fault Zone
narrower: Buckow-Oderhaff Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/12266
references: https://data.geoscience.earth/ncl/geoera/ref/12265
references: https://data.geoscience.earth/ncl/geoera/ref/7996
in scheme: Tectonic Boundary Objects in Europe
broader: Fault Zones of the central eastern North German Basin striking NNE-SSW

Buckow Fault Zone
type: Concept
created: 2021-09-06T15:30:07.268Z
creator: schmar
notation: DE-BB-210101
preferred label: Buckower Störung @de
definition: NNW-SSW striking fault zone reaching from the basement to the Cenozoic. Activation of salt tectonics along the fault zone (salt structures Buckow, Bad Freienwalde) . Sometimes interpreted as a extension of the Potsdam fault zone (DE-BB-02c-01).
definition: NNW-SSE streichende Störungszone. Nachgewiesen vom basement bis ins Känozoikum. Aktivierung von Salztektonik entlang der Störungszone (Salzstrukturen Buckow, Bad Freienwalde). Teilweise interpretiert als östliche Verlängerung der Potsdamer Störungszone (DE-BB-02c-01). @de
references: https://data.geoscience.earth/ncl/geoera/ref/12274
references: https://data.geoscience.earth/ncl/geoera/ref/12264
references: https://data.geoscience.earth/ncl/geoera/ref/12272
in scheme: Tectonic Boundary Objects in Europe
broader: Buckow-Oderhaff Fault Zone

Buckow-Oderhaff Fault Zone
type: Concept
created: 2021-09-06T15:30:07.272Z
creator: schmar
notation: DE-BB-210102
preferred label: Oderhaff Störungszone @de
definition: NNE-SSW striking basement falt zone. Postulated basing on geophysical data. Postulated border between the Northeast German Basin and the Polish Trough.
definition: NNE-SSE streichende Störung im basement. Postuliert nach geophysikalischen Befunden (Gravimetrie, Magnetik, Tiefe Seismik). Postulierte Grenze zwischen dem Norddeutschen Becken im Westen und dem Polnischen Becken im Osten. @de
references: https://data.geoscience.earth/ncl/geoera/ref/12264
references: https://data.geoscience.earth/ncl/geoera/ref/12274
references: https://data.geoscience.earth/ncl/geoera/ref/12271
in scheme: Tectonic Boundary Objects in Europe
broader: Buckow-Oderhaff Fault Zone

Liebenwalde-Torgelow Fault
type: Concept
created: 2021-09-06T15:30:07.317Z
creator: schmar
notation: DE-BB-3102
preferred label: Liebenwalde-Torgelower Störung @de
definition: NNE-SSW striking basement fault zone. Postulated basing on geophysical data (gravimetrics, magnetics, deep seismics).
definition: NNE-SSW streichende Störungszone im basement. Postuliert basierend auf geophysikalischen Daten (Gravimetrie, Magnetik, tiefe Seismik). @de
narrower: Liebenwalde Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7996
references: https://data.geoscience.earth/ncl/geoera/ref/12271
references: https://data.geoscience.earth/ncl/geoera/ref/12272
references: https://data.geoscience.earth/ncl/geoera/ref/8031
in scheme: Tectonic Boundary Objects in Europe
broader: Fault Zones of the central eastern North German Basin striking NNE-SSW

Liebenwalde Fault
type: Concept
created: 2021-09-06T15:30:07.322Z
creator: schmar
notation: DE-BB-310201
preferred label: Liebenwalder Störung @de
definition: Southwestern part of the Liebenwalde-Torgelow fault
definition: Südlicher Teil der Liebenwalde-Torgelow-Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/7996
references: https://data.geoscience.earth/ncl/geoera/ref/12271
references: https://data.geoscience.earth/ncl/geoera/ref/12272
in scheme: Tectonic Boundary Objects in Europe
broader: Liebenwalde-Torgelow Fault

Fault Zones of the central eastern North German Basin striking WNW-ESE
type: Concept
created: 2021-09-06T15:30:07.328Z
creator: schmar
notation: DE-BB-22
preferred label: Störungszonen des zentralen östlichen Beckens, Streichen WNW-ESE @de
definition: Fault zones in the central eastern part of the North German Basin striking NW-SE and related fault sets especially in the Permocarboniferous.
definition: Störungszonen im östlichen Zentralbereich des Norddeutschen Beckens und parallele Störungenscharen insbesondere im Permokarbon. Streichen NW-SE. @de
narrower: Teltow-Kotzen Fault
narrower: Falkensee Fault
narrower: Eberswalde Fault
narrower: Templin Fault
narrower: Gramzow Fault
narrower: Arneburg Fault
narrower: Havelberg Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7996
in scheme: Tectonic Boundary Objects in Europe
broader: Fault Zones in the central part of the North German Basin

Templin Fault
type: Concept
created: 2021-09-06T15:30:07.356Z
creator: schmar
notation: DE-BB-2204
preferred label: Templiner Störung @de
definition: NW-SE striking basement fault. Postulated basing on geophysical data (gravimetrics, magnetics, deep seismics). Active fault zone in the Carboniferous and Lower Permian (Rotliegend).
definition: WNW-ESE streichende Störung im basement. Postuliert auf der Basis geophysikalischer Befunde (Gravimetrie, Magnetik, Tiefe Seismik). Aktive Störung im Karbon und Rotliegend. @de
references: https://data.geoscience.earth/ncl/geoera/ref/12271
references: https://data.geoscience.earth/ncl/geoera/ref/12263
references: https://data.geoscience.earth/ncl/geoera/ref/12274
references: https://data.geoscience.earth/ncl/geoera/ref/12268
in scheme: Tectonic Boundary Objects in Europe
broader: Fault Zones of the central eastern North German Basin striking WNW-ESE

Gramzow Fault
type: Concept
created: 2021-09-06T15:30:07.361Z
creator: schmar
notation: DE-BB-2205
preferred label: Gramzower Störung @de
definition: WNW-ESE striking basement fault. Postulated basing on geophysical data (gravimetrics, magnetics, deep seismics).
definition: WNW-ESE streichende Störung im basement. Postuliert auf der Basis geophysikalischer Befunde (Gravimetrie, Magnetik, Tiefe Seismik). @de
narrower: Schollene Fault
narrower: Wittenburg Fault
references: https://data.geoscience.earth/ncl/geoera/ref/12267
references: https://data.geoscience.earth/ncl/geoera/ref/12271
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/12263
in scheme: Tectonic Boundary Objects in Europe
broader: Fault Zones of the central eastern North German Basin striking WNW-ESE

Schollene Fault
type: Concept
created: 2021-09-06T15:30:07.366Z
creator: schmar
notation: DE-BB-220601
preferred label: Schollene Störung @de
definition: NW-SE striking fault in the Permocarboniferous.
definition: NW-SE streichende Störung im Permokarbonen Deckgebirge. @de
references: https://data.geoscience.earth/ncl/geoera/ref/12229
references: https://data.geoscience.earth/ncl/geoera/ref/8068
in scheme: Tectonic Boundary Objects in Europe
related: Schollene Fault Zone
broader: Gramzow Fault

Wittenburg Fault
type: Concept
created: 2021-09-06T15:30:07.370Z
creator: schmar
notation: DE-BB-220604
preferred label: Wittenburger Störung @de
definition: NW-SE striking fault in the basement and the sedimentary cover. Defined basing on geophysical data (gravimetrics, magnetics, deep seismics) and faults in the Permocarboniferous.
definition: NW-SE streichende Störung im basement und sedimentären Deckgebirge. Definiert nach geophysikalischen Befunden (Gravimetrie, Magnetik, Seismik) und Störungen im Permokarbon. @de
references: https://data.geoscience.earth/ncl/geoera/ref/12272
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/12229
in scheme: Tectonic Boundary Objects in Europe
broader: Gramzow Fault

Havelberg Fault
type: Concept
created: 2021-09-06T15:30:07.380Z
creator: schmar
notation: DE-BB-2210
preferred label: Havelberger Störung @de
definition: NW-SE striking basement fault with related structures in the sedimentary cover. Defined basing on geophysical data (gravimetrics, magnetics, deep seismics), faults in the Permocarboniferous.
definition: NW-SE streichende Störung im basement und sedimentären Deckgebirge. Definiert auf der Basis geophysikalischer Befunde (Gravimetrie, Magnetik, Tiefe Seismik), Störungen im Permokarbon. @de
references: https://data.geoscience.earth/ncl/geoera/ref/12264
references: https://data.geoscience.earth/ncl/geoera/ref/12229
references: https://data.geoscience.earth/ncl/geoera/ref/12272
references: https://data.geoscience.earth/ncl/geoera/ref/8031
in scheme: Tectonic Boundary Objects in Europe
broader: Fault Zones of the central eastern North German Basin striking WNW-ESE

Teltow-Kotzen Fault
type: Concept
created: 2021-09-06T15:30:07.332Z
creator: schmar
notation: DE-BB-2201
preferred label: Teltow-Kotzener Störung @de
definition: NW-ESE striking fault in the basement. Postulated basing on geophysical data (gravimetrics, magnetics, deep seismics). Active from Carboniferous to Triassic.
definition: WNW-ESE streichende Störung im basement. Postuliert auf der Basis geophysikalischer Befunde (Gravimetrie, Magnetik, Tiefe Seismik). Aktive Störung von Karbon bis Trias. @de
narrower: Kotzen Fault
narrower: Teltow Fault
references: https://data.geoscience.earth/ncl/geoera/ref/12267
references: https://data.geoscience.earth/ncl/geoera/ref/12271
references: https://data.geoscience.earth/ncl/geoera/ref/12266
references: https://data.geoscience.earth/ncl/geoera/ref/8031
in scheme: Tectonic Boundary Objects in Europe
broader: Fault Zones of the central eastern North German Basin striking WNW-ESE

Kotzen Fault
type: Concept
created: 2021-09-06T15:30:07.337Z
creator: schmar
notation: DE-BB-220101
preferred label: Kotzener Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/12267
in scheme: Tectonic Boundary Objects in Europe
broader: Teltow-Kotzen Fault

Teltow Fault
type: Concept
created: 2021-09-06T15:30:07.341Z
creator: schmar
notation: DE-BB-220102
preferred label: Teltower Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/12267
in scheme: Tectonic Boundary Objects in Europe
broader: Teltow-Kotzen Fault

Arneburg Fault
type: Concept
created: 2021-09-06T15:30:07.375Z
creator: schmar
notation: DE-BB-2209
preferred label: Arneburg Störung @de
definition: NW-SE striking basement fault with related structures in the sedimentary cover. Defined basing on geophysical data (gravimetrics, magnetics, deep seismics), faults in the Permocarboniferous and salt structures.
definition: NW-SE streichende Störung im basement und sedimentären Deckgebirge. Definiert auf der Basis geophysikalischer Befunde (Gravimetrie, Magnetik, Tiefe Seismik), Störungen im Permokarbon und halokinetischen Strukturen. @de
references: https://data.geoscience.earth/ncl/geoera/ref/12229
references: https://data.geoscience.earth/ncl/geoera/ref/12272
references: https://data.geoscience.earth/ncl/geoera/ref/12271
references: https://data.geoscience.earth/ncl/geoera/ref/8031
in scheme: Tectonic Boundary Objects in Europe
broader: Fault Zones of the central eastern North German Basin striking WNW-ESE

Falkensee Fault
type: Concept
created: 2021-09-06T15:30:07.346Z
creator: schmar
notation: DE-BB-2202
preferred label: Falkensee Störung @de
definition: NW-SE striking basement fault. Postulated basing on geophysical data (gravimetrics, magnetics, deep seismics). Active from Carboniferous to Triassic.
definition: WNW-ESE streichende Störung im basement. Postuliert auf der Basis geophysikalischer Befunde (Gravimetrie, Magnetik, Tiefe Seismik). Aktive Störung von Karbon bis Trias. @de
references: https://data.geoscience.earth/ncl/geoera/ref/12271
references: https://data.geoscience.earth/ncl/geoera/ref/12263
references: https://data.geoscience.earth/ncl/geoera/ref/12264
references: https://data.geoscience.earth/ncl/geoera/ref/12268
in scheme: Tectonic Boundary Objects in Europe
broader: Fault Zones of the central eastern North German Basin striking WNW-ESE

Eberswalde Fault
type: Concept
created: 2021-09-06T15:30:07.351Z
creator: schmar
notation: DE-BB-2203
preferred label: Eberswalder Störung @de
definition: NW-SE striking basement fault. Postulated basing on geophysical data (gravimetrics, magnetics, deep seismics).
definition: WNW-ESE streichende Störung im basement. Postuliert auf der Basis geophysikalischer Befunde (Gravimetrie, Magnetik, Tiefe Seismik). @de
references: https://data.geoscience.earth/ncl/geoera/ref/12271
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/12264
references: https://data.geoscience.earth/ncl/geoera/ref/12274
in scheme: Tectonic Boundary Objects in Europe
broader: Fault Zones of the central eastern North German Basin striking WNW-ESE

Fault Zones of the central eastern North German Basin striking E-W
type: Concept
created: 2021-09-06T15:30:07.385Z
creator: schmar
notation: DE-BB-23
preferred label: Störungszonen des zentralen östlichen Beckens, Streichen E-W @de
definition: Complex fault zones in the central eastern part of the North German Basin striking approximately E-W.
definition: Komplexe Störungszonen im östlichen Zentralbereich des Norddeutschen Beckens. Streichen in etwa E-W. @de
narrower: Potsdam Fault Zone
narrower: Lower Elbe Lineament - Barenthin Fault
references: https://data.geoscience.earth/ncl/geoera/ref/7996
in scheme: Tectonic Boundary Objects in Europe
broader: Fault Zones in the central part of the North German Basin

Potsdam Fault Zone
type: Concept
created: 2021-09-06T15:30:07.389Z
creator: schmar
notation: DE-BB-2301
preferred label: Potsdamer Störungszone @de
definition: E-W striking, complex fault zone in the Permian and Mesozoic strata containing several faults and salt-cored anticlines. In some parts not exactly definable basing on the existing geophysical data (exploration gaps).
definition: Komplexe, E-W streichende Strukturzone aus Störungen und halokinetischen Antiklinalstrukturen im Permischen und Mesozoischen Deckgebirge. Abschnittsweise bisher nicht exakt definierbar im geophysikalischen Bild (Erkundungslücken). @de
references: https://data.geoscience.earth/ncl/geoera/ref/12274
references: https://data.geoscience.earth/ncl/geoera/ref/12272
references: https://data.geoscience.earth/ncl/geoera/ref/7996
references: https://data.geoscience.earth/ncl/geoera/ref/8031
in scheme: Tectonic Boundary Objects in Europe
related: Potsdam fault
broader: Fault Zones of the central eastern North German Basin striking E-W

Lower Elbe Lineament - Barenthin Fault
type: Concept
created: 2021-09-06T15:30:07.394Z
creator: schmar
notation: DE-BB-2302
preferred label: Unterelbe Lineament - Barenthin fault @de
definition: E-W striking basement structure (Lower Elbe Lineament). In the Permian to Mesozoic normal faulting and activation of several salt structures along the fault (Barenthin fault zone).
definition: E-W streichende basement Struktur (Elbe Lineament). In der "Saxonischen" Tekonik im Perm und Mesozoikum normal faulting und Aktivierung von Salzstrukturen entland der Störung (Barenthin-Störungszone). @de
references: https://data.geoscience.earth/ncl/geoera/ref/8068
references: https://data.geoscience.earth/ncl/geoera/ref/7996
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/12266
in scheme: Tectonic Boundary Objects in Europe
related: Lower Elbe fault
broader: Fault Zones of the central eastern North German Basin striking E-W

Fault Zones of the southern border of the North German Basin and Lausatian Block
type: Concept
created: 2021-09-06T15:30:07.054Z
creator: schmar
notation: DE-BB-1
preferred label: Störungszonen des Südrandes des Norddeutschen Beckens und des Lausitzer Blockes @de
definition: Fault zones of the Southeastern border of the North German Basin (NGB) and of the Variscian Lusatian Block. NGB : Intra-continental basin, part of the Southern Permian Basin. Subsidence starting in Carboniferous. Inversion phases in Upper Cretaceous. Lusatian Block: Variscian massif (consisting of Variscian and Cadomian intrusions, folded and low grade metamorphized sediments of the Rhenohercynian and Saxothuringian Zone), uplifted in Upper Cretaceous. Southern border of the NGB in Brandenburg.
definition: Störungszonen der südöstlichen Grenze des Norddeutschen Beckens und des Variszischen Lausitzer Blocks. Norddeutsches Beckens: Teil der Mitteleuropäischen Senke. Intrakontinentale Senkungsstruktur ab den Karbon. Inversionsphasen in der Oberen Kreide. Lausitzer Block: in der Oberen Kreide angehobenes variszisches Massiv (cadomische und variszische Intrusionen, gefaltete und schwach metamorphisierte Sedimente der Rhenoherzynischen und Saxothuringischen Zone). Südliche Begrenzung des Norddeutschen Beckens in Brandenburg. @de
narrower: Central German Main Escarpments and parallel structures (Striking NW-SE)
narrower: Cross-directional structures of the Central German Main Escarpments (Striking NE-SW)
narrower: Variscian structures of the Lusatian Massif (Lusatian Anticline and the Torgau-Doberlug Syncline)
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Brandenburg

Variscian structures of the Lusatian Massif (Lusatian Anticline and the Torgau-Doberlug Syncline)
type: Concept
created: 2021-09-06T15:30:07.231Z
creator: schmar
notation: DE-BB-13
preferred label: Variszische Strukturen des Lausitzer Massivs (Lausitzer Antiklinorium und Torgau-Doberlog-Synklinorium) @de
definition: Variscian structure zones of the Lusatian Massif. Striking NE/ENE-SW/WSW. Partially re-activated during the different phases of the post-variscian development under varying stress regimes ("Saxonian" Tectonics from Permian to Tertiary).
definition: Variszische Strukturzonen des Lausitzer Blockes. Streichen NE/ENE-SW/WSW. Teilweise reaktiviert in verschiedenen Phasen der post-variszischen Entwicklung ("Saxonische" Tektonik von Perm bis Tertiär) unter wechselnden Spannungsregimen. @de
narrower: South Doberlug Fracture Zone
narrower: North Doberlug Fracture Zone
references: https://data.geoscience.earth/ncl/geoera/ref/7996
references: https://data.geoscience.earth/ncl/geoera/ref/12270
in scheme: Tectonic Boundary Objects in Europe
broader: Fault Zones of the southern border of the North German Basin and Lausatian Block

South Doberlug Fracture Zone
type: Concept
created: 2021-09-06T15:30:07.236Z
creator: schmar
notation: DE-BB-1301
preferred label: Süd-Doberluger Bruchzone @de
definition: Fault system at the southern border of the variscian Torgau-Doberlug Syncline, Variscian age. Striking NE-SW (Variscian).
definition: Südliche Grenze der Variszischen Torgau-Doberlug-Synklinale. ENE-WSW streichende Störungszone. @de
narrower: Southern Doberlug Fracture Zone
narrower: Finsterwalde Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/12265
references: https://data.geoscience.earth/ncl/geoera/ref/12270
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/12272
in scheme: Tectonic Boundary Objects in Europe
broader: Variscian structures of the Lusatian Massif (Lusatian Anticline and the Torgau-Doberlug Syncline)

Southern Doberlug Fracture Zone
type: Concept
created: 2021-09-06T15:30:07.241Z
creator: schmar
notation: DE-BB-130101
preferred label: Süd Doberluger Bruchzone @de
references: https://data.geoscience.earth/ncl/geoera/ref/12272
references: https://data.geoscience.earth/ncl/geoera/ref/12232
in scheme: Tectonic Boundary Objects in Europe
broader: South Doberlug Fracture Zone

Finsterwalde Fault Zone
type: Concept
created: 2021-09-06T15:30:07.245Z
creator: schmar
notation: DE-BB-130102
preferred label: Finsterwalder Störungszone @de
definition: Southern border of the Variscian Torgau-Doberlug Syncline, Variscian age. Striking ESE-WSW .
definition: Südliche Grenze der variszischen Torgau-Doberlug-Senke. ESE-WSW streichende variszische Störung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/12272
references: https://data.geoscience.earth/ncl/geoera/ref/12232
in scheme: Tectonic Boundary Objects in Europe
broader: South Doberlug Fracture Zone

North Doberlug Fracture Zone
type: Concept
created: 2021-09-06T15:30:07.250Z
creator: schmar
notation: DE-BB-1302
preferred label: Nord-Doberluger Bruchzone @de
definition: Northern border of Lusatian Massif to the Northeast German Basin (NEGB). Northern border of the Variscian Torgau-Doberlug Syncline. Striking ENE-WSW.
definition: Nördliche Grenze des Lausitzer Blockes zur Norddeutschen Senke. Nördliche Grenze der Variszischen Torgau-Doberlug-Synklinale. ENE-WSW streichende Störingszone. @de
references: https://data.geoscience.earth/ncl/geoera/ref/12232
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/12270
references: https://data.geoscience.earth/ncl/geoera/ref/12272
in scheme: Tectonic Boundary Objects in Europe
broader: Variscian structures of the Lusatian Massif (Lusatian Anticline and the Torgau-Doberlug Syncline)

Central German Main Escarpments and parallel structures (Striking NW-SE)
type: Concept
created: 2021-09-06T15:30:07.057Z
creator: schmar
notation: DE-BB-11
preferred label: Mitteldeutsche Abbrüche und Paralellstrukturen (Streichen NW-SE) @de
definition: Faults zones at the Southeastern border of the North German Basin and related parallel structures striking NW-SE. Formed after the Variscian Orogeny as dextral strike-slip faults in a crustal wrench-system. Re-activated in different phases of the tectonic development of the NGB under varying stress regimes ("Saxonian" Tectonics from Permian to Tertiary). Extensional regimes with normal faulting from Jurassic to Early Cretaceous. Inversion in the Upper Cretaceous (forming of compression structures: thrusts, anticlines).
definition: Störungszonen an der südöstlichen Grenze des Norddeutschen Beckens und Parallelstrukturen mit Streichen NW-SE. Bildung nach der Variszischen Orogenese als dextrale Scherzonen eines krustalen Wrench-Systems. Aktiviert in mehreren Phasen der tektonischen Entwicklung des Norddeutschen Beckens unter wechselnden Spannungsregimen ("Saxonische" Tektonik). Extensionsregime von Jura bis Unterer Kreide. Inversion in der Oberen Kreide (Bildung von Kompressionsstrukturen: Auf-/Überschiebungen, Antiklinalstrukturen). @de
narrower: Lusatian Main Escarpment
narrower: Wünsdorf-Cottbus Fault
narrower: Groß Köris-Dissen-Merzdorf Fault Zone
narrower: Vetschau Fault
narrower: Kausche Graben
narrower: Inter-Lusatian Fault
narrower: West Lusatian Fault
narrower: Schönewalde Fault Zone
narrower: Zahna Fault Zone
narrower: Fürstenwalde-Guben Structural Zone
narrower: Zerben-Belzig Structural Zone
narrower: Setzsteig Structural Zone
narrower: Schweinitz Fault
references: https://data.geoscience.earth/ncl/geoera/ref/12268
references: https://data.geoscience.earth/ncl/geoera/ref/7996
references: https://data.geoscience.earth/ncl/geoera/ref/12270
references: https://data.geoscience.earth/ncl/geoera/ref/8031
in scheme: Tectonic Boundary Objects in Europe
broader: Fault Zones of the southern border of the North German Basin and Lausatian Block

Schönewalde Fault Zone
type: Concept
created: 2021-09-06T15:30:07.104Z
creator: schmar
notation: DE-BB-1108
preferred label: Schönewalde Störung @de
definition: NW-SE striking basement thrust of Variscian age. Reactivation during the Mesozoic "Saxonian" Tectonics. Vertical displacements up to 100m.
definition: NW-SE streichende, variszische Krustenstörung. Reaktivierung in der in der mesozoischen "Saxonischen" Tektonik. Vertikale Versätze bis 100 m. @de
references: https://data.geoscience.earth/ncl/geoera/ref/12265
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/7996
references: https://data.geoscience.earth/ncl/geoera/ref/12271
in scheme: Tectonic Boundary Objects in Europe
related: Schönewalde Fault Zone
broader: Central German Main Escarpments and parallel structures (Striking NW-SE)

Zahna Fault Zone
type: Concept
created: 2021-09-06T15:30:07.109Z
creator: schmar
notation: DE-BB-1109
preferred label: Zahna Störung @de
definition: NW-SE striking fault in the foreland of the West Lusatian fault.
definition: NW-SE streichende Störung im Vorland der Westlausitz-Störung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/7996
in scheme: Tectonic Boundary Objects in Europe
related: Zahna Fault Zone
broader: Central German Main Escarpments and parallel structures (Striking NW-SE)

Inter-Lusatian Fault
type: Concept
created: 2021-09-06T15:30:07.095Z
creator: schmar
notation: DE-BB-1106
preferred label: Innerlausitzer Störungszone @de
definition: NW-SE striking fault zone of Variscian age. Reactivation during the Mesozoic "Saxonian" Tectonics.
definition: NW-SE streichende variszische Störungszone. Reaktiviert in der in der "Saxonischen" Tektonik. @de
references: https://data.geoscience.earth/ncl/geoera/ref/12268
references: https://data.geoscience.earth/ncl/geoera/ref/8031
in scheme: Tectonic Boundary Objects in Europe
broader: Central German Main Escarpments and parallel structures (Striking NW-SE)

West Lusatian Fault
type: Concept
created: 2021-09-06T15:30:07.100Z
creator: schmar
notation: DE-BB-1107
preferred label: Westlausitzer Störungszone @de
definition: NW-SE striking basement thrust of Variscian age. South-western border of the Lausation block. Reactivation during the Mesozoic "Saxonian" Tectonics.
definition: NW-SE streichende variszische Krustenstörung. Südwest-Grenze des Lausitzer Blockes. Reaktivierung in der mesozoischen "Saxonischen" Tektonik. @de
references: https://data.geoscience.earth/ncl/geoera/ref/7996
references: https://data.geoscience.earth/ncl/geoera/ref/8031
in scheme: Tectonic Boundary Objects in Europe
broader: Central German Main Escarpments and parallel structures (Striking NW-SE)

Lusatian Main Escarpment
type: Concept
created: 2021-09-06T15:30:07.063Z
creator: schmar
notation: DE-BB-1101
preferred label: Lausitzer Hauptabbruch @de
definition: The Lusatian Main Escarpment is one of the important basement thrusts at the Southeastern border of the North German Basin and forms the northeastern border of the Lusatian block to the NGB. Dextral strike-slip fault zone, striking NW-SE. Normal faulting in the Permian and Mesozoic with a vertical displacement up to more than 1.000m (decreasing from Southeast to Northwest). In the inversion phase in Upper Cretaceous with reverse faulting.
definition: Der Lausitzer Haupptabbruch ist eine der wichtigen Krustenstörungen am Südrand der Norddeutschen Senke und bildet die nordöstliche Grenze des Lausitzer Blockes zur Norddeutschen Senke. Dextrale strike-slip-Störung mit Abschiebungsbewegungen im Perm und Mesozoikum mit vertikalen Versätzen bis zu 1000m (von Südost nach Nordwest abnehmend). Während der Inversion in der Oberen Kreide mit Rücküberschiebungen. @de
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/12268
references: https://data.geoscience.earth/ncl/geoera/ref/12269
in scheme: Tectonic Boundary Objects in Europe
broader: Central German Main Escarpments and parallel structures (Striking NW-SE)

Wünsdorf-Cottbus Fault
type: Concept
created: 2021-09-06T15:30:07.067Z
creator: schmar
notation: DE-BB-1102
preferred label: Wünsdorf-Cottbus Störung @de
definition: NW-SE striking fault zone in the basement and sedimentary cover. In the sedimentary cover partially as a flexure. Especially in the northern part characteristic strong gradients of the Bouguer anomaly ("Wünsdorf-Cottbusser gravity flank").
definition: NW-SE streichend Störungszone im basement und Deckgebirge. Im Deckgebirge teilweise als Flexur ausgebildet. Insbesondere im nördlichen Teil markante Anomalien der Bouguerschwere ("Wünsdorf-Cottbusser Schwereflanke"). @de
references: https://data.geoscience.earth/ncl/geoera/ref/12274
references: https://data.geoscience.earth/ncl/geoera/ref/12269
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/12265
in scheme: Tectonic Boundary Objects in Europe
broader: Central German Main Escarpments and parallel structures (Striking NW-SE)

Groß Köris-Dissen-Merzdorf Fault Zone
type: Concept
created: 2021-09-06T15:30:07.072Z
creator: schmar
notation: DE-BB-1103
preferred label: Groß-Köris - Dissen - Merzdorfer Störungszone @de
definition: NW-SE striking fault zone in the basement and overburden. Dextral strike-slipe fault. Formation of elongated salt-cored anticlines during the compression phases in Upper Cretaceous.
definition: NW-SE streichend Störungszone im basement und Deckgebirge. Dextrale strike-slip-Störung. Durch Kompressionsphasen in der Oberen Kreide Bildung von Antiklinal-Strukturen im permo-triassichen Deckgebirge, mit langestreckten Salzstrukturen im Kern. @de
narrower: Groß Köris-Merzdorf Structural Zone
narrower: Dissen-Merzdorf Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/12268
references: https://data.geoscience.earth/ncl/geoera/ref/12269
in scheme: Tectonic Boundary Objects in Europe
broader: Central German Main Escarpments and parallel structures (Striking NW-SE)

Groß Köris-Merzdorf Structural Zone
type: Concept
created: 2021-09-06T15:30:07.077Z
creator: schmar
notation: DE-BB-110301
preferred label: Groß Köris-Merzdorfer Strukturzone @de
references: https://data.geoscience.earth/ncl/geoera/ref/12268
references: https://data.geoscience.earth/ncl/geoera/ref/12272
references: https://data.geoscience.earth/ncl/geoera/ref/12232
in scheme: Tectonic Boundary Objects in Europe
broader: Groß Köris-Dissen-Merzdorf Fault Zone

Dissen-Merzdorf Fault Zone
type: Concept
created: 2021-09-06T15:30:07.081Z
creator: schmar
notation: DE-BB-110302
preferred label: Dissen-Derzdorfer Störungszone @de
references: https://data.geoscience.earth/ncl/geoera/ref/12272
references: https://data.geoscience.earth/ncl/geoera/ref/12232
references: https://data.geoscience.earth/ncl/geoera/ref/12273
in scheme: Tectonic Boundary Objects in Europe
broader: Groß Köris-Dissen-Merzdorf Fault Zone

Fürstenwalde-Guben Structural Zone
type: Concept
created: 2021-09-06T15:30:07.113Z
creator: schmar
notation: DE-BB-1110
preferred label: Guben-Fürstenwalder-Störungszone @de
definition: NW/NNW-SE/SSE striking fault zone in the basement and sedimentary cover. Complex system of fracture zones, Graben structures and salt-cored anticlines.
definition: NW-SE bis NNW-SSE streichende Störungszone im Deckgebirge und basement. Komplexes Störungsbild aus Bruchstrukturen, antiklinalen Elementen und Salzstrukturen. @de
narrower: Fürstenwalde Fault Zone
narrower: Guben Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/12268
references: https://data.geoscience.earth/ncl/geoera/ref/7996
references: https://data.geoscience.earth/ncl/geoera/ref/12274
references: https://data.geoscience.earth/ncl/geoera/ref/8031
in scheme: Tectonic Boundary Objects in Europe
broader: Central German Main Escarpments and parallel structures (Striking NW-SE)

Fürstenwalde Fault Zone
type: Concept
created: 2021-09-06T15:30:07.118Z
creator: schmar
notation: DE-BB-111001
preferred label: Fürstenwalder Störungszone @de
references: https://data.geoscience.earth/ncl/geoera/ref/12273
references: https://data.geoscience.earth/ncl/geoera/ref/12272
in scheme: Tectonic Boundary Objects in Europe
broader: Fürstenwalde-Guben Structural Zone

Guben Fault Zone
type: Concept
created: 2021-09-06T15:30:07.123Z
creator: schmar
notation: DE-BB-111002
preferred label: Gubener Störungszone @de
references: https://data.geoscience.earth/ncl/geoera/ref/12272
references: https://data.geoscience.earth/ncl/geoera/ref/12229
in scheme: Tectonic Boundary Objects in Europe
broader: Fürstenwalde-Guben Structural Zone

Vetschau Fault
type: Concept
created: 2021-09-06T15:30:07.086Z
creator: schmar
notation: DE-BB-1104
preferred label: Vetschauer Störung @de
definition: NW-SE striking fault zone in the sedimentary cover between Lusatian Main Escarpmenmt and Wünsdorf-Cottbus fault.
definition: NW-SE streichende Störungszone im Deckgebirge zwischen Lausitzer Abbruch und Wünsdorf-Cottbuser Störungszone. @de
references: https://data.geoscience.earth/ncl/geoera/ref/12269
references: https://data.geoscience.earth/ncl/geoera/ref/8031
in scheme: Tectonic Boundary Objects in Europe
broader: Central German Main Escarpments and parallel structures (Striking NW-SE)

Kausche Graben
type: Concept
created: 2021-09-06T15:30:07.090Z
creator: schmar
notation: DE-BB-1105
preferred label: Kauscher Graben @de
definition: Cenozoic Graben structure in the forland of the Lusatian Main Escarpment. Vertical displacement some decameter.
definition: Känozoische Grabenstruktur im Vorland des Lausitzer Hauptabbruches. Vertikale Versätze von einigen 10er Metern. @de
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/12269
in scheme: Tectonic Boundary Objects in Europe
broader: Central German Main Escarpments and parallel structures (Striking NW-SE)

Schweinitz Fault
type: Concept
created: 2021-09-06T15:30:07.142Z
creator: schmar
notation: DE-BB-1114
preferred label: Schweinitz Störung @de
definition: NW-SE striking fault in the foreland of the West Lusatian fault.
definition: NW-SE streichende Störung im Vorland der Westlausitz-Störung. @de
references: https://data.geoscience.earth/ncl/geoera/ref/12272
references: https://data.geoscience.earth/ncl/geoera/ref/8068
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/12270
in scheme: Tectonic Boundary Objects in Europe
related: Schweinitz Fault Zone
broader: Central German Main Escarpments and parallel structures (Striking NW-SE)

Zerben-Belzig Structural Zone
type: Concept
created: 2021-09-06T15:30:07.128Z
creator: schmar
notation: DE-BB-1111
preferred label: Zerben-Belzig Strukturzone @de
definition: NW-SE striking structural zone. Elongated faulted anticlinale with accumulation of Zechstein salt in the core (thicknes > 1000m).
definition: NW-SE streichende Strukturzone. Langestreckte gestörte Antiklinalkstruktur mit Akkumulation von Zechstein-Salz im Kern (bis 1500 m Mächtigkeit). @de
references: https://data.geoscience.earth/ncl/geoera/ref/8068
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/12272
in scheme: Tectonic Boundary Objects in Europe
related: Zerben Fault Zone
broader: Central German Main Escarpments and parallel structures (Striking NW-SE)

Setzsteig Structural Zone
type: Concept
created: 2021-09-06T15:30:07.133Z
creator: schmar
notation: DE-BB-1113
preferred label: Setzsteiger Strukturzone @de
definition: NW-SE striking fault zone. Reverse fault in the basement (vertical displacement up to 1000 m) and a salt-cored anticline in the sedimentary cover (Reuden-Setzsteig).
definition: NW-SE streichende Störungszone. Aufschiebung im basement mit vertikalem Versatz bis 1000m. Aufsitzende Salzstruktur Reuden-Setzsteig im Deckgebirge. @de
narrower: Burg-Reuden Fault
references: https://data.geoscience.earth/ncl/geoera/ref/12265
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/8068
references: https://data.geoscience.earth/ncl/geoera/ref/12272
in scheme: Tectonic Boundary Objects in Europe
broader: Central German Main Escarpments and parallel structures (Striking NW-SE)

Burg-Reuden Fault
type: Concept
created: 2021-09-06T15:30:07.138Z
creator: schmar
notation: DE-BB-111301
preferred label: Burg-Reuden Störung @de
definition: Part of the Setzsteig structural zone.
definition: Teil der Setzsteiger Strukturzone @de
references: https://data.geoscience.earth/ncl/geoera/ref/12272
references: https://data.geoscience.earth/ncl/geoera/ref/8068
in scheme: Tectonic Boundary Objects in Europe
related: Burg-Reuden Fault Zone
broader: Setzsteig Structural Zone

Cross-directional structures of the Central German Main Escarpments (Striking NE-SW)
type: Concept
created: 2021-09-06T15:30:07.147Z
creator: schmar
notation: DE-BB-12
preferred label: Querstrukturen der Mitteldeutschen Abbrüche (Streichen SW-NE) @de
definition: Fault and fracture zones at the Southern border of the North German Basin striking cross-directional to the Central German main escarpments (SW/WSW-NE/ENE). Post-variscian origin ("Saxonian" Tectonics from Permian to Tertiary). Partially re-activation of Variscian structures.
definition: Saxonische Störungs- und Bruchzonen an der südöstlichen Grenze des Norddeutschen Beckens. Streichen quer zu den Mitteldeutschen Abbrüchen (SW/WSW-NE/ENE). Bildung post-variszisch ("Saxonische" Tektonik). Teilweise Reaktivierung variszischer Strukturen. @de
narrower: Bronkow-Tauer Fault Zone
narrower: Hoyerswerda Fault
narrower: Calau-Plieskendorf-Buchwäldchen Fault Zone
narrower: Herzberg Fault Zone
narrower: Heinersbrück-Guben Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/12269
references: https://data.geoscience.earth/ncl/geoera/ref/7996
in scheme: Tectonic Boundary Objects in Europe
broader: Fault Zones of the southern border of the North German Basin and Lausatian Block

Hoyerswerda Fault
type: Concept
created: 2021-09-06T15:30:07.173Z
creator: schmar
notation: DE-BB-1202
preferred label: Hoyerswerdaer Querstörung @de
definition: NE-SW striking fault zone of the "Saxonian" Tectonics.
definition: NE-SW streichende Störungszone der "Saxonischen" Tektonik. @de
narrower: Hoyerswerda Fault
narrower: Stradow-Buckow Fault
references: https://data.geoscience.earth/ncl/geoera/ref/12268
references: https://data.geoscience.earth/ncl/geoera/ref/7996
references: https://data.geoscience.earth/ncl/geoera/ref/8031
in scheme: Tectonic Boundary Objects in Europe
broader: Cross-directional structures of the Central German Main Escarpments (Striking NE-SW)

Hoyerswerda Fault
type: Concept
created: 2021-09-06T15:30:07.180Z
creator: schmar
notation: DE-BB-120201
preferred label: Hoyerwerdaer Querstörung @de
references: https://data.geoscience.earth/ncl/geoera/ref/12268
in scheme: Tectonic Boundary Objects in Europe
broader: Hoyerswerda Fault

Stradow-Buckow Fault
type: Concept
created: 2021-09-06T15:30:07.186Z
creator: schmar
notation: DE-BB-120202
preferred label: Stradow-Buckower Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/12232
references: https://data.geoscience.earth/ncl/geoera/ref/12229
in scheme: Tectonic Boundary Objects in Europe
broader: Hoyerswerda Fault

Herzberg Fault Zone
type: Concept
created: 2021-09-06T15:30:07.209Z
creator: schmar
notation: DE-BB-1205
preferred label: Herzberger Störung @de
definition: NE-SW striking fault zone of the "Saxonian" Tectonics.
definition: NE-SW streichende Störungszone der "Saxonischen" Tektonik. @de
references: https://data.geoscience.earth/ncl/geoera/ref/7996
references: https://data.geoscience.earth/ncl/geoera/ref/8031
references: https://data.geoscience.earth/ncl/geoera/ref/12270
in scheme: Tectonic Boundary Objects in Europe
broader: Cross-directional structures of the Central German Main Escarpments (Striking NE-SW)

Calau-Plieskendorf-Buchwäldchen Fault Zone
type: Concept
created: 2021-09-06T15:30:07.191Z
creator: schmar
notation: DE-BB-1204
preferred label: Calau-Plieskendorfer Störungszone @de
definition: NE-SW striking fault zone of the "Saxonian" Tectonics. Vertical displacement influenced by fault-controlled subrosion of Permian salt.
definition: NE-SW streichende Störungszone der "Saxonischen" Tektonik. Vertikale Bewegungen durch störungskontrollierte Subrosion von Permischen Salz beeinflusst. @de
narrower: Plieskendorf Fault
narrower: Calau Fault
references: https://data.geoscience.earth/ncl/geoera/ref/12269
references: https://data.geoscience.earth/ncl/geoera/ref/7996
references: https://data.geoscience.earth/ncl/geoera/ref/8031
in scheme: Tectonic Boundary Objects in Europe
broader: Cross-directional structures of the Central German Main Escarpments (Striking NE-SW)

Calau Fault
type: Concept
created: 2021-09-06T15:30:07.203Z
creator: schmar
notation: DE-BB-120402
preferred label: Calauer Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/12269
references: https://data.geoscience.earth/ncl/geoera/ref/12232
in scheme: Tectonic Boundary Objects in Europe
broader: Calau-Plieskendorf-Buchwäldchen Fault Zone

Plieskendorf Fault
type: Concept
created: 2021-09-06T15:30:07.197Z
creator: schmar
notation: DE-BB-120401
preferred label: Plieskendorfer Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/12269
references: https://data.geoscience.earth/ncl/geoera/ref/12232
in scheme: Tectonic Boundary Objects in Europe
broader: Calau-Plieskendorf-Buchwäldchen Fault Zone

Heinersbrück-Guben Fault Zone
type: Concept
created: 2021-09-06T15:30:07.214Z
creator: schmar
notation: DE-BB-1206
preferred label: Heinersbrück-Gubener Störungszone @de
definition: NE-SW striking fault zone of the "Saxonian" Tectonics.
definition: NE-SW streichende Störungszone der "Saxonischen" Tektonik. @de
narrower: Senftenberg Fault
narrower: Heinersbrück-Guben Fault
narrower: Heinersbrück Fault
references: https://data.geoscience.earth/ncl/geoera/ref/12269
references: https://data.geoscience.earth/ncl/geoera/ref/8031
in scheme: Tectonic Boundary Objects in Europe
broader: Cross-directional structures of the Central German Main Escarpments (Striking NE-SW)

Heinersbrück Fault
type: Concept
created: 2021-09-06T15:30:07.226Z
creator: schmar
notation: DE-BB-120605
preferred label: Heinersbrücker Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/12269
references: https://data.geoscience.earth/ncl/geoera/ref/8031
in scheme: Tectonic Boundary Objects in Europe
broader: Heinersbrück-Guben Fault Zone

Senftenberg Fault
type: Concept
created: 2021-09-06T15:30:07.218Z
creator: schmar
notation: DE-BB-120601
preferred label: Senftenberger Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/12272
references: https://data.geoscience.earth/ncl/geoera/ref/12232
in scheme: Tectonic Boundary Objects in Europe
broader: Heinersbrück-Guben Fault Zone

Heinersbrück-Guben Fault
type: Concept
created: 2021-09-06T15:30:07.223Z
creator: schmar
notation: DE-BB-120602
preferred label: Heinersbrück-Gubener Querstörung @de
references: https://data.geoscience.earth/ncl/geoera/ref/12269
in scheme: Tectonic Boundary Objects in Europe
broader: Heinersbrück-Guben Fault Zone

Bronkow-Tauer Fault Zone
type: Concept
created: 2021-09-06T15:30:07.153Z
creator: schmar
notation: DE-BB-1201
preferred label: Bruchzone Bronkow-Tauer @de
definition: NE-SW striking fault zone of the "Saxonian" Tectonics.
definition: NE-SW streichende Störungszone der "Saxonischen" Tektonik. @de
narrower: Tauer-Pinnow Fault
narrower: Bronkow Fault
references: https://data.geoscience.earth/ncl/geoera/ref/12268
references: https://data.geoscience.earth/ncl/geoera/ref/12269
references: https://data.geoscience.earth/ncl/geoera/ref/8031
in scheme: Tectonic Boundary Objects in Europe
broader: Cross-directional structures of the Central German Main Escarpments (Striking NE-SW)

Bronkow Fault
type: Concept
created: 2021-09-06T15:30:07.167Z
creator: schmar
notation: DE-BB-120102
preferred label: Bronkower Störung @de
references: https://data.geoscience.earth/ncl/geoera/ref/12272
references: https://data.geoscience.earth/ncl/geoera/ref/12269
references: https://data.geoscience.earth/ncl/geoera/ref/12268
in scheme: Tectonic Boundary Objects in Europe
broader: Bronkow-Tauer Fault Zone

Tauer-Pinnow Fault
type: Concept
created: 2021-09-06T15:30:07.160Z
creator: schmar
notation: DE-BB-120101
preferred label: Tauer-Pinnow Störungszone @de
references: https://data.geoscience.earth/ncl/geoera/ref/12229
references: https://data.geoscience.earth/ncl/geoera/ref/12269
references: https://data.geoscience.earth/ncl/geoera/ref/12268
in scheme: Tectonic Boundary Objects in Europe
broader: Bronkow-Tauer Fault Zone

Fracture Zones of the Northeastern border of the North German Basin
type: Concept
created: 2021-09-06T15:30:07.401Z
creator: schmar
notation: DE-BB-3
preferred label: Störungszonen des Nordrandes des Norddeutschen Beckens @de
definition: Fault zones of the Eastern/Northeastern border of the North German Basin (NGB). NGB : Intra-continental european basin, part of the Southern Permian Basin. Subsidence starting in Carboniferous. Inversion phases in Upper Cretaceous.
definition: Störungszonen des östlichen/nordöstlichen Randes des Norddeutschen Beckens. Norddeutsches Becken: Teil der Mitteleuropäischen Senke. Intrakontinentale Senkungsstruktur ab den Karbon. Inversionsphasen in der Oberkreide. @de
narrower: Fault Zones Zones of the Northeastern border of the North German Basin striking NNW-SSE
in scheme: Tectonic Boundary Objects in Europe
broader: Tectonic Boundary in Brandenburg

Fault Zones Zones of the Northeastern border of the North German Basin striking NNW-SSE
type: Concept
created: 2021-09-06T15:30:07.404Z
creator: schmar
notation: DE-BB-31
preferred label: Störungszonen des nordöstlichen Randes des Norddeutschen Beckens, Streichen NNW-SSE @de
definition: NNW-SSE striking fault zones at the Northeastern border of the North German Basin. Southern extension of the Western Pommerania Fault system.
definition: NNW-SSE streichende Störungszonen am Nordrand des Norddeutschen Beckens. Südliche Ausläufer des Vorpommern-Störungssystem. @de
references: https://data.geoscience.earth/ncl/geoera/ref/7996
in scheme: Tectonic Boundary Objects in Europe
broader: Fracture Zones of the Northeastern border of the North German Basin

Tectonic Boundary in the Netherlands
in scheme: Tectonic Boundary Objects in Europe
scope note: All named tectonic boundary objects that are located (at least partly) in the Netherlands, are identified by an ID with the prefix „NL“ listed in the notation. Fault systems and/or fault domains can cross political borders and are therefore shared by several countries. Therefore, they can contain faults from different countries, indicated by country-specific prefixes to the respective ID.
definition: Fault in the Netherlands displayed in the HIKE European fault database. They are sorted into fault systems and tectonic terranes (Fault Domains) represented in the Geological Map of the Netherlands and Dutch subsurface geological models DGM (v2.2) and DGm diep (v5).
notation: NL-0
top concept of: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-02-10T09:29:57.412Z
narrower: Elbe Line
narrower: Caledonian Accretionary Terrane Fault Domain
narrower: Southern North Sea Lüneberg Fault Domain
narrower: Dowsing-South Hewett Large Scale Fault System
narrower: Wales-Brabant Massive Fault Domain

Caledonian Accretionary Terrane Fault Domain
notation: NL-990001
definition: The exact position of this terrane depends on its definition. In the most recent views it corresponds to a Low Velocity Zone in the crust that is attributed to the Caledonian accretionary wedge inbetween Avalonia and Baltica that formed due to Thornquist ocean subduction and is attached to non-subducting Avalonia plate. This definition places the Tor suture south of this accretionary terrane, wheras the deeper seated plate contact might be represented by the Elbe-Line. However, it would be unfortunate to reposition the Thor suture which is positioned further north and likely represents the northern suture of the accretionary prism
in scheme: Tectonic Boundary Objects in Europe
alternative label: Caledonian Accretionary complex
alternative label: collapsed Caledonian accretionary Complex
alternative label: Thor accretionary wedge
type: Concept
created: 2021-02-10T09:33:09.493Z
alternative label: CAT-FD
narrower: Northern Dutch Offshore Graben Large Scale Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/7714
broader: Tectonic Boundary in the Netherlands

Northern Dutch Offshore Graben Large Scale Fault System
notation: NL-990002
definition: Group of faults associated with the approximately N-S trending part of the Dutch Central Graben and its surroundings in the northernmost Dutch offshore
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-02-10T09:33:09.497Z
alternative label: NDOG-LSFS
narrower: Elbow Spit Platform Margin Fault System
narrower: Intra Elbow Spit Platform Fault Domain
narrower: Step Graben Boundary Fault System
narrower: Intra Step Graben Fault Domain
narrower: Dutch Central Graben Fault System
broader: Caledonian Accretionary Terrane Fault Domain

Dutch Central Graben Fault System
notation: NL-990010
definition: Faults associated with the N-S trending Dutch Central Graben system
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-02-10T09:33:09.530Z
alternative label: DCG-FS
narrower: Western Dutch Central Graben Boundary sub Fault System
narrower: Eastern Dutch Central Graben Boundary sub Fault System
narrower: Intra Dutch Central Graben Fault Domain
references: https://data.geoscience.earth/ncl/geoera/ref/7705
broader: Northern Dutch Offshore Graben Large Scale Fault System

Eastern Dutch Central Graben Boundary sub Fault System
notation: NL-990012
definition: N-S trending fault system acting as the eastern margin fault system of the Dutch Central Graben
type: Concept
created: 2021-02-10T09:33:09.538Z
alternative label: E-DCGB-sFS
in scheme: Tectonic Boundary Objects in Europe
broader: Dutch Central Graben Fault System

Western Dutch Central Graben Boundary sub Fault System
notation: NL-990011
definition: N-S trending fault system acting as the western margin fault system of the Dutch Central Graben
type: Concept
created: 2021-02-10T09:33:09.534Z
alternative label: W-DCGB-sFS
in scheme: Tectonic Boundary Objects in Europe
broader: Dutch Central Graben Fault System

Intra Dutch Central Graben Fault Domain
notation: NL-990013
definition: Undifferentiated faults within the Dutch Central Graben
type: Concept
created: 2021-02-10T09:33:09.542Z
alternative label: DCG-FD
narrower: Dutch Central Graben sub-salt Fault Domain
narrower: Dutch Central Graben supra-salt Fault Domain
in scheme: Tectonic Boundary Objects in Europe
broader: Dutch Central Graben Fault System

Dutch Central Graben supra-salt Fault Domain
notation: NL-990015
definition: Undifferentiated faults above the Zechstein Group within the Dutch Central Graben
type: Concept
created: 2021-02-10T09:33:09.549Z
alternative label: DCG-SUPRA-FD
in scheme: Tectonic Boundary Objects in Europe
broader: Intra Dutch Central Graben Fault Domain

Dutch Central Graben sub-salt Fault Domain
notation: NL-990014
definition: Undifferentiated faults below the Zechstein Group within the Dutch Central Graben
type: Concept
created: 2021-02-10T09:33:09.546Z
alternative label: DCG-SUB-FD
in scheme: Tectonic Boundary Objects in Europe
broader: Intra Dutch Central Graben Fault Domain

Intra Step Graben Fault Domain
notation: NL-990006
definition: Undifferentiated faults within the Step Graben. Predominantly N-S oriented faults have been observed, but interpretation density is limited in this area
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-02-10T09:33:09.513Z
alternative label: SG-FD
narrower: Outer Rough Basin sub Fault System
narrower: Step Graben sub-salt Fault Domain
narrower: Step Graben supra-salt Fault Domain
references: https://data.geoscience.earth/ncl/geoera/ref/7697
broader: Northern Dutch Offshore Graben Large Scale Fault System

Step Graben supra-salt Fault Domain
notation: NL-990009
definition: Undifferentiated faults above the Zechstein Group within the Step Graben
type: Concept
created: 2021-02-10T09:33:09.526Z
alternative label: SG-SUPRA-FD
in scheme: Tectonic Boundary Objects in Europe
broader: Intra Step Graben Fault Domain

Step Graben sub-salt Fault Domain
notation: NL-990008
definition: Undifferentiated faults below the Zechstein Group within the Step Graben
type: Concept
created: 2021-02-10T09:33:09.522Z
alternative label: SG-SUB-FD
in scheme: Tectonic Boundary Objects in Europe
broader: Intra Step Graben Fault Domain

Outer Rough Basin sub Fault System
notation: NL-990007
definition: Aligned system of N-S faults defining the northernmost narrowing part of the Step Graben, i.e. at the transition to the Outer Rough Basin in Germany and Denmark
type: Concept
created: 2021-02-10T09:33:09.517Z
alternative label: ORB-sFS
in scheme: Tectonic Boundary Objects in Europe
references: https://data.geoscience.earth/ncl/geoera/ref/7697
broader: Intra Step Graben Fault Domain

Step Graben Boundary Fault System
notation: NL-990005
definition: This fault system separates the Step Graben from the Elbow Spit Platform and Elbow Spit High
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-02-10T09:33:09.508Z
alternative label: SGB-FS
references: https://data.geoscience.earth/ncl/geoera/ref/7697
broader: Northern Dutch Offshore Graben Large Scale Fault System

Intra Elbow Spit Platform Fault Domain
notation: NL-990004
definition: Undifferentiated faults within the Elbow Spit Platform
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-02-10T09:33:09.504Z
alternative label: ESP-FD
broader: Northern Dutch Offshore Graben Large Scale Fault System

Elbow Spit Platform Margin Fault System
notation: NL-990003
definition: NNW-SSE trending fault system in between the Step Graben and the Elbow Spit Platform
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-02-10T09:33:09.501Z
alternative label: ESPM-FS
broader: Northern Dutch Offshore Graben Large Scale Fault System

Elbe Line
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-02-10T09:33:09.483Z
definition: Deep-seated plate contact betwen Avalonia and Baltica underneath the Thor accretionary wedge, situated close to the northern offshore border with Germany. The line is rather hypothetical in the sense that it cannot be seen at shallow levels where most faults are normally interpreted
references: https://data.geoscience.earth/ncl/geoera/ref/7712
broader: Tectonic Boundary in the Netherlands

Wales-Brabant Massive Fault Domain
definition: The Brabant Massif is currently considered to be situated above the boundary of two lithospheric blocks, the Midlands Microcraton to the SW and the Southern North Sea - Lüneberg Terrane to the NE and formed during final closure of the Rheic ocean between Laurentia and Gondwana. the Welsh basin - London-Brabant massif forms a stable block together with the Midlands micro-craton (UK). Two distinct fault directions occur in this domain, i.e.,WNW-ESE and NNW-SSE trending. The latter group is less developed in the Netherlands.
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990119
type: Concept
created: 2021-02-10T09:33:09.978Z
preferred label: London-Brabant Massief @nl
alternative label: WBM-FD
alternative label: Brabant Massief @nl
narrower: Zeeland High Fault Domain
narrower: Limburg High Fault Domain
narrower: Campine Block Fault Domain
references: https://data.geoscience.earth/ncl/geoera/ref/7706
references: https://data.geoscience.earth/ncl/geoera/ref/7712
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Tectonic Boundary in the Netherlands

Campine Block Fault Domain
definition: Group of predominantly WNW-ESE faults in the Northeastern flank of the Brabant Massif that is covered by Paleozoic to Triassic strata, which in turn are unconformably overlain by Upper Cretaceous strata. The southern boundary of the Campine Basin is defined as the area where Carboniferous rocks pinch out or are locally delimited by faults (e.g. the Hoogstraten syn-depositional fault). Faults part of the Campine block have common activity during the Kimmerian and/or Cenozoic tectonic phases.
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/7705
references: https://data.geoscience.earth/ncl/geoera/ref/7707
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990122
type: Concept
created: 2021-02-10T09:33:09.994Z
preferred label: Campine Basin @nl
alternative label: CAM-FD
alternative label: Kempen Blok @nl
narrower: Hoogstraten Fault System
narrower: Oosterhout Platform Fault Domain
narrower: Northern Zeeland Fault System
narrower: Voorne trog Fault Domain
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Wales-Brabant Massive Fault Domain

Voorne trog Fault Domain
definition: A relatively unfaulted area in the Campine Block that acted as depocenter (subsidence area) and was formed due to flexural downwarping in response to Paleogene inversion of the West Netherlands Basin to the north
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990126
type: Concept
created: 2021-02-10T09:33:10.011Z
alternative label: VT-FD
references: https://data.geoscience.earth/ncl/geoera/ref/7715
references: https://data.geoscience.earth/ncl/geoera/ref/7705
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Campine Block Fault Domain

Northern Zeeland Fault System
definition: Boundary fault between the Oosterhout Platform and the Campine basin
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/7705
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990125
type: Concept
created: 2021-02-10T09:33:10.006Z
alternative label: N-ZL-FS
references: https://data.geoscience.earth/ncl/geoera/ref/7707
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Campine Block Fault Domain

Oosterhout Platform Fault Domain
definition: Faults in the area south of the Southern West Netherlands Basin sub Fault System that form a transitional area between the Roer Valley Graben in the north and the Zeeland High (or Campine Block) in the south. Here, Triassic rocks are preserved and unconformably overlain by Upper Cretaceous. The southern boundary of the Oosterhout Platform is defined as the area where Triassic rocks pinch out and is only locally defined by faults
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/7705
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990124
type: Concept
created: 2021-02-10T09:33:10.002Z
alternative label: OP-FD
references: https://data.geoscience.earth/ncl/geoera/ref/7707
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Campine Block Fault Domain

Hoogstraten Fault System
definition: WNW-ESE trending major normal, listric fault within the Campine block probably active during the Carboniferous based as is based on roll-over anticlines in Namurian and Westphalian strata that are unconformably overlain by Cretaceous deposts. It defines the southern extent of Upper Carboniferous rocks. It is only mapped just south of the Netherlands-Belgium border.
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990123
type: Concept
created: 2021-02-10T09:33:09.998Z
alternative label: HS-FS
references: https://data.geoscience.earth/ncl/geoera/ref/7701
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Campine Block Fault Domain

Limburg High Fault Domain
definition: Group of predominantly WNW-ESE faults normal/oblique faults in the Limburg High, which is the southeasternmost extension of the Zeeland-Kempen-Limburg Fault Domain. In this area, Upper Cretaceous deposits directly overlie Carboniferous rocks. In the south, east and west, the Limburg High gives way to the adjacent fault blocks in Germany and Belgium.
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990121
type: Concept
created: 2021-02-10T09:33:09.989Z
alternative label: LH-FD
references: https://data.geoscience.earth/ncl/geoera/ref/7707
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Wales-Brabant Massive Fault Domain

Zeeland High Fault Domain
definition: Group of predominantly WNW-ESE faults normal/oblique faults in the Zeeland Province part of the Wales Brabant massive that is characterized by Upper Cretaceous rocks directly overlying Carboniferous rocks. It is bounded in the north by the Oosterhout Platform, where Triassic rocks are found.
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990120
type: Concept
created: 2021-02-10T09:33:09.985Z
alternative label: ZH-FD
references: https://data.geoscience.earth/ncl/geoera/ref/7707
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Wales-Brabant Massive Fault Domain

Southern North Sea Lüneberg Fault Domain
notation: NL-990016
definition: Faults formed in that part of the Avalonia micro plate that was extended and collapsed in latest Devonian-earliest Carboinferous time at the onset of the Variscan orogeny and that were reactivated during younger deformation phases . The fault domain is separated form the southern part of Avalonia through the Dowsing-South Hewett fault zone
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-02-10T09:33:09.554Z
alternative label: SNSL-FD
narrower: Western Dutch Platform Fault Domain
narrower: Eastern Dutch Platform Fault Domain
narrower: Mid Netherlands Basins Fault Domain
references: https://data.geoscience.earth/ncl/geoera/ref/7712
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Tectonic Boundary in the Netherlands

Mid Netherlands Basins Fault Domain
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
definition: A structural domain defined by the area south of the Dutch Central Graben and Platform fault domains in the north and delimited by the Dowsing-South Hewett Fault System to the south. It consists of several NW-SE and WNW-ESE basin systems that are separated by major normal and reverse faults
notation: NL-990090
type: Concept
created: 2021-02-10T09:33:09.862Z
alternative label: CNB-LFS
narrower: Roer-Valley Graben - West Netherlands Basin Fault Domain
narrower: Peel - Indefatigable Large Scale Fault System
narrower: Peel - Maasbommel_Zandvoort Fault Domain
narrower: Central Netherlands - Broad Fourteens Fault Domain
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Southern North Sea Lüneberg Fault Domain

Roer-Valley Graben - West Netherlands Basin Fault Domain
definition: Basin system with multiple internal faults that were active during Kimmerian, Subhercynian and/or Cenozoïc tectonic phases. The characteristics of the Jurassic subsidence pattern reveal that the Roer-Valley Graben and West Netherlands Basin formed a single tectonic unity during the Mesozoic, but it probably already existed as a structural feature in Paleozoic times that was formed due to wrench movements after the Late Carboniferous–Early Permian Variscan orogeny
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990091
type: Concept
created: 2021-02-10T09:33:09.866Z
alternative label: RVG-WNB-FD
narrower: Roer-Valley Graben Fault Domain
narrower: Rijen Fault System
narrower: West Netherlands Basin Fault Domain
narrower: Indefetigable Platform Fault Domain
references: https://data.geoscience.earth/ncl/geoera/ref/7715
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Mid Netherlands Basins Fault Domain

Roer-Valley Graben Fault Domain
definition: The Roer Valley Graben (RVG) is a distinct fault-bounded graben with multiple internal faults of predominantly NNW-SSE orientations and some NW-SE orientations. Faults were active during Kimmerian, subhercynian and/or Cenozoïc tectonic phases, but it is since the Jurassic that differential subsidence clearly started. Since the Early Cretaceous rocks are missing in the RVG, it is not clear which tectonic regime the RVG experienced in those times. subsidence recommenced in Oligocene times and continues to the present day. Apart from the northwest, where the RVG passes into the West Netherlands Basin (WNB), it is surrounded by platform areas. The boundary to the WNB has been taken at the pinch-out line of Upper Cretaceous sediments. Paleogene uplift of the RVG was less severe than in the WNB, and pre-inversion Chalk has been preserved in the RVG. The northeastern boundary of the basin isformed by the Peel Boundary Fault System
type: SpatialObject
notation: NL-990092
type: Concept
created: 2021-02-10T09:33:09.871Z
alternative label: RVG-FD
references: https://data.geoscience.earth/ncl/geoera/ref/7707
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Roer-Valley Graben - West Netherlands Basin Fault Domain

Indefetigable Platform Fault Domain
definition: Indefetigable Platform formes the domain west of the West Netherlands Basin and BFB. The southern part is also referred to as Winterton Platform
type: SpatialObject
notation: NL-990095
type: Concept
created: 2021-02-10T09:33:09.884Z
alternative label: IDP-FD
alternative label: Indefetigable Shelf
narrower: Winterton High sub Fault Domain
references: https://data.geoscience.earth/ncl/geoera/ref/7712
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Roer-Valley Graben - West Netherlands Basin Fault Domain

Winterton High sub Fault Domain
definition: The Winterton High is part of the Indefetigable Platform Fault Domain and is charaterized by the absence of Permian and Mezozoic strata
type: SpatialObject
notation: NL-990096
type: Concept
created: 2021-02-10T09:33:09.888Z
alternative label: WH-sFD
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Indefetigable Platform Fault Domain

West Netherlands Basin Fault Domain
definition: The West Netherlands Basin (WNB) is a Mesozoic distinct fault-bounded graben with multiple internal faults of predominantly NNW-SSE and NW-SE orientations that toghether make up an anastomosing fault mosaic. The basin which was mildly- to strongly inverted in Late Cretaceous and Paleogene times. The southeastern transition toward the Roer Valley Graben (RVG) corresponds to the area where the Chalk has been completely eroded due to inversion. In the southwest, the Sout West Netherlands Fault System marks the boundary to the Campine Block or Oosterhout Platform. The transition towards the Indefatigable Platform is irregular and runs across different fault blocks. In the northeast, the boundary with the Broad Fourteens- and Central Netherlands basins is formed by the North West Netherlands Fault System, which more or less coincides with the narrow Zandvoort Ridge and IJmuiden Platform
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/7705
notation: NL-990094
type: Concept
created: 2021-02-10T09:33:09.880Z
alternative label: WNB_FD
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Roer-Valley Graben - West Netherlands Basin Fault Domain

Rijen Fault System
definition: NNW oriented fault system active during Paleocene -(sub)Recent times and that has acted as the local boundary to the RVG since Cenozoic times. During the Mesozoic the main step fault was at the Southern West Netherlands Basin Fault System
type: SpatialObject
notation: NL-990093
type: Concept
created: 2021-02-10T09:33:09.875Z
alternative label: RIJN-FS
alternative label: Gilze-Rijen Breuk @nl
references: https://data.geoscience.earth/ncl/geoera/ref/7715
references: https://data.geoscience.earth/ncl/geoera/ref/7710
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Roer-Valley Graben - West Netherlands Basin Fault Domain

Peel - Maasbommel_Zandvoort Fault Domain
definition: Group of faults transecting the WNW-ESE elongated structural High delimited to the south by the Peel - Indefatigable Large Scale Fault System
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/8485
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990101
type: Concept
created: 2021-02-10T09:33:09.907Z
alternative label: PMZ-FD
narrower: Peel Maas Bommel Complex Fault Domain
narrower: IJmuiden Platform Fault Domain
narrower: Zandvoort Ridge Fault Set
narrower: Tegelen Fault System
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Mid Netherlands Basins Fault Domain

Peel Maas Bommel Complex Fault Domain
definition: Undifferentiated faults within the Peel Maas Bommel Complex
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/7705
notation: NL-990102
type: Concept
created: 2021-02-10T09:33:09.911Z
alternative label: PMBC-FD
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Peel - Maasbommel_Zandvoort Fault Domain

Tegelen Fault System
definition: The northern margin fault of the Peel Maas Bommel High
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/8486
notation: NL-990105
type: Concept
created: 2021-02-10T09:33:09.923Z
alternative label: TEG-FS
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Peel - Maasbommel_Zandvoort Fault Domain

Zandvoort Ridge Fault Set
definition: Fault block between Central Netherlands Basin and West Netherlands Basin defined by severe faulting along WNW-ESE faults. This structure is an important inversion ridge, locally accompanied by southvergent reverse- and thrust faults
type: SpatialObject
notation: NL-990104
type: Concept
created: 2021-02-10T09:33:09.919Z
alternative label: ZR-FSET
references: https://data.geoscience.earth/ncl/geoera/ref/7705
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Peel - Maasbommel_Zandvoort Fault Domain

IJmuiden Platform Fault Domain
definition: Fault within the a mild inversion structure just offshore IJmuiden dilimited to the south by the Indefatigable Fault System
type: SpatialObject
notation: NL-990103
type: Concept
created: 2021-02-10T09:33:09.914Z
alternative label: IJP-FD
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Peel - Maasbommel_Zandvoort Fault Domain

Peel - Indefatigable Large Scale Fault System
definition: NW-SE alignment of the Peel Boundary, Mid-Netherlands and Indefatigable Fault system that make up the northern boundary of the Roer-Valley Graben - West Netherlands Basin Fault Domain
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/7710
references: https://data.geoscience.earth/ncl/geoera/ref/7705
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990097
type: Concept
created: 2021-02-10T09:33:09.892Z
alternative label: P-ID-LFS
narrower: Indefatigable Fault System
narrower: Mid Netherland Fault System
narrower: Peel Boundary Fault System
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Mid Netherlands Basins Fault Domain

Peel Boundary Fault System
definition: Alignment of NW-SE faults that form the transition between the Peel Maasbommel High in the north and the Roer Valley Graben in the south
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/8484
references: https://data.geoscience.earth/ncl/geoera/ref/7705
notation: NL-990100
type: Concept
created: 2021-02-10T09:33:09.903Z
alternative label: PB-FS
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Peel - Indefatigable Large Scale Fault System

Mid Netherland Fault System
definition: Alignment of NW-SE faults that form the transition between the Zandvoort Ridge to the north and the West Netherlands Basin to the south. The Mid Netherland Fault System acted as reverse faults during inversion
type: SpatialObject
notation: NL-990099
type: Concept
created: 2021-02-10T09:33:09.900Z
alternative label: MN-FS
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Peel - Indefatigable Large Scale Fault System

Indefatigable Fault System
definition: Alignment of NW-SE faults that form the transition between the Broad Fourteens Basin to the north and the West Netherlands Basin to the south. Locally, the Mid Netherland Fault System acted as reverse faults during inversion
type: SpatialObject
notation: NL-990098
type: Concept
created: 2021-02-10T09:33:09.896Z
alternative label: ID-FS
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Peel - Indefatigable Large Scale Fault System

Central Netherlands - Broad Fourteens Fault Domain
definition: Faults associated with the NW-SE aligned basin system in the central Netherlands
type: SpatialObject
narrower: North Holland Platform Fault System
narrower: Northern Central Netherlands Basin Fault System
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990106
type: Concept
created: 2021-02-10T09:33:09.927Z
alternative label: CNB-BFB-FD
narrower: Central Netherlands Basin Fault Domain
narrower: Broad Fourteens Basin Fault Domain
narrower: Eastern Broad Fourteens Basin Fault System
narrower: Western Broad Fourteens Basin Fault System
narrower: Internal Broad Fourteens Basin Fault System
narrower: North Holland Platform Fault Domain
narrower: Southern Central Netherlands Basin Fault System
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Mid Netherlands Basins Fault Domain

North Holland Platform Fault Domain
definition: Undifferentiated faults within Central Netherlands Basin
type: SpatialObject
notation: NL-990112
type: Concept
created: 2021-02-10T09:33:09.949Z
alternative label: NHP_FD
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Central Netherlands - Broad Fourteens Fault Domain

North Holland Platform Fault System
type: SpatialObject
notation: NL-999132
definition: Complex Fault patterns forming the eastern Boundary of the North Holland platform
created: 2021-03-17T08:25:25.011Z
type: Concept
alternative label: NHP-FS
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Central Netherlands - Broad Fourteens Fault Domain

Internal Broad Fourteens Basin Fault System
definition: Undifferentiated faults within Central Netherlands Basin
type: SpatialObject
notation: NL-990111
type: Concept
created: 2021-02-10T09:33:09.945Z
alternative label: I-BFB-FS
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Central Netherlands - Broad Fourteens Fault Domain

Northern Central Netherlands Basin Fault System
type: SpatialObject
notation: NL-990131
created: 2021-03-17T08:24:25.450Z
definition: Complex Fault patterns forming the Boundary between the Central Netherlands Basin and the Peel Maas Bommel Complex in the west and bifurcating from the Southern Central Netherlands Fault System towards the Northeast
type: Concept
alternative label: N-CNB-FS
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Central Netherlands - Broad Fourteens Fault Domain

Western Broad Fourteens Basin Fault System
definition: Complex Fault patterns forming the western Boundary of the Broad Fourteens Basin
type: SpatialObject
notation: NL-990110
type: Concept
created: 2021-02-10T09:33:09.941Z
alternative label: W-BFB-FS
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Central Netherlands - Broad Fourteens Fault Domain

Eastern Broad Fourteens Basin Fault System
definition: Complex Fault patterns forming the eastern Boundary of the Broad Fourteens Basin
type: SpatialObject
notation: NL-990109
type: Concept
created: 2021-02-10T09:33:09.938Z
alternative label: E-BFS-FS
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Central Netherlands - Broad Fourteens Fault Domain

Southern Central Netherlands Basin Fault System
type: SpatialObject
definition: Complex Fault patterns forming the Boundary between the Central Netherlands Basin and the Peel Maas Bommel Complex
alternative label: S-CNB-FS
type: Concept
notation: NL-990130
created: 2021-03-17T08:23:10.064Z
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Central Netherlands - Broad Fourteens Fault Domain

Broad Fourteens Basin Fault Domain
definition: Undifferentiated faults within Broad Fourteens Basin
type: SpatialObject
notation: NL-990108
type: Concept
created: 2021-02-10T09:33:09.934Z
alternative label: BFB-FD
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Central Netherlands - Broad Fourteens Fault Domain

Central Netherlands Basin Fault Domain
definition: Undifferentiated faults within Central Netherlands Basin
type: SpatialObject
notation: NL-990107
type: Concept
created: 2021-02-10T09:33:09.930Z
alternative label: CNB-FD
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Central Netherlands - Broad Fourteens Fault Domain

Western Dutch Platform Fault Domain
notation: NL-990017
definition: A structural domain largely defined by the area southwest of the Dutch Central Graben
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-02-10T09:33:09.559Z
alternative label: WDP-FD
narrower: Northern Cleaver Bank Margin Fault System
narrower: Eastern Cleaver Bank Margin Fault System
narrower: Intra Cleaver Bank Fault Domain
narrower: Intra Anglo-Dutch Basin Fault Domain
narrower: Central Offshore Platform Margin Fault System
narrower: Intra Central Offshore Platform Fault Domain
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Southern North Sea Lüneberg Fault Domain

Intra Central Offshore Platform Fault Domain
definition: Group of faults within the Central offshore Platform that is seen as the transitional zone between the Dutch Central Graben and the Broad Fourteen Basin
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990033
type: Concept
created: 2021-02-10T09:33:09.620Z
alternative label: COP-FD
narrower: Central Offshore Platform sub-salt NNW-SSE Fault Set
narrower: Central Offshore Platform sub-salt WNW-ESE Fault Set
narrower: Central Offshore Platform sub-salt WSW-ENE Fault Set
narrower: Central Offshore Platform sub-salt NNE-SSW Fault Set
narrower: Central Offshore Platform Supra-salt Fault Domain
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Western Dutch Platform Fault Domain

Central Offshore Platform sub-salt NNW-SSE Fault Set
definition: Faults with a NNW-SSE orietation below the Zechstein Group within the Central Offshore Platform
type: SpatialObject
notation: NL-990034
type: Concept
created: 2021-02-10T09:33:09.624Z
alternative label: COP-SUB-NNW-SSE-FSET
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Intra Central Offshore Platform Fault Domain

Central Offshore Platform Supra-salt Fault Domain
definition: Undifferentiated faults above the Zechstein Group within the Central Offshore Platform
type: SpatialObject
notation: NL-990038
type: Concept
created: 2021-02-10T09:33:09.639Z
alternative label: COP-SUPRA-FD
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Intra Central Offshore Platform Fault Domain

Central Offshore Platform sub-salt NNE-SSW Fault Set
definition: Faults with a NNE-SSW orietation below the Zechstein Group within the Central Offshore Platform
type: SpatialObject
notation: NL-990037
type: Concept
created: 2021-02-10T09:33:09.635Z
alternative label: COP-SUB-NNE-SSW-FSET
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Intra Central Offshore Platform Fault Domain

Central Offshore Platform sub-salt WSW-ENE Fault Set
definition: Faults with a WSW-ENE orietation below the Zechstein Group within the Central Offshore Platform
type: SpatialObject
notation: NL-990036
type: Concept
created: 2021-02-10T09:33:09.631Z
alternative label: COP-SUB-WSW-ENE-FSET
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Intra Central Offshore Platform Fault Domain

Central Offshore Platform sub-salt WNW-ESE Fault Set
definition: Faults with a WNW-ESE orietation below the Zechstein Group within the Central Offshore Platform
type: SpatialObject
notation: NL-990035
type: Concept
created: 2021-02-10T09:33:09.628Z
alternative label: COP-SUB-WNW-ESE-FSET
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Intra Central Offshore Platform Fault Domain

Central Offshore Platform Margin Fault System
definition: NNE-SSW oriended fault system acting as the transition zone between Texel-IJsselmeer High in the east and the Central Offshore Platform in the west
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990032
type: Concept
created: 2021-02-10T09:33:09.616Z
alternative label: COPM-FS
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Western Dutch Platform Fault Domain

Intra Cleaver Bank Fault Domain
definition: Group of faults with various orientations within the Cleaver Bank
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990020
type: Concept
created: 2021-02-10T09:33:09.570Z
alternative label: CB-FD
narrower: Cleaver Bank sub-salt NNW-SSE Fault Set
narrower: Cleaver Bank sub-salt WNW-ESE Fault Set
narrower: Cleaver Bank sub-salt WSW-ENE Fault Set
narrower: Cleaver Bank sub-salt NNE-SSW Fault Set
narrower: Cleaver Bank Supra-salt Fault Domain
references: https://data.geoscience.earth/ncl/geoera/ref/7713
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Western Dutch Platform Fault Domain

Cleaver Bank sub-salt WSW-ENE Fault Set
definition: Faults with a WSW-ENE orietation below the Zechstein Group within the Cleaver Bank
type: SpatialObject
notation: NL-990023
type: Concept
created: 2021-02-10T09:33:09.581Z
alternative label: CB-SUB-WSW-ENE-FSET
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Intra Cleaver Bank Fault Domain

Cleaver Bank sub-salt WNW-ESE Fault Set
definition: Faults with a WNW-ESE orietation below the Zechstein Group within the Cleaver Bank
type: SpatialObject
notation: NL-990022
type: Concept
created: 2021-02-10T09:33:09.578Z
alternative label: CB-SUB-WNW-ESE-FSET
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Intra Cleaver Bank Fault Domain

Cleaver Bank sub-salt NNW-SSE Fault Set
definition: Faults with a NNW-SSE orietation below the Zechstein Group within the Cleaver Bank
type: SpatialObject
notation: NL-990021
type: Concept
created: 2021-02-10T09:33:09.574Z
alternative label: CB-SUB-NNW-SSE-FSET
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Intra Cleaver Bank Fault Domain

Cleaver Bank Supra-salt Fault Domain
definition: Undifferentiated faults above the Zechstein Group within the Cleaver Bank
type: SpatialObject
notation: NL-990025
type: Concept
created: 2021-02-10T09:33:09.589Z
alternative label: CB-SUPRA-FD
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Intra Cleaver Bank Fault Domain

Cleaver Bank sub-salt NNE-SSW Fault Set
definition: Faults with a NNE-SSW orietation below the Zechstein Group within the Cleaver Bank
type: SpatialObject
notation: NL-990024
type: Concept
created: 2021-02-10T09:33:09.585Z
alternative label: CB-SUB-NNE-SSW-FSET
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Intra Cleaver Bank Fault Domain

Eastern Cleaver Bank Margin Fault System
notation: NL-990019
definition: Fault system defining the eastern margin of the Cleaver Bank
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-02-10T09:33:09.566Z
alternative label: E-CBM-FS
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Western Dutch Platform Fault Domain

Northern Cleaver Bank Margin Fault System
notation: NL-990018
definition: Fault system defining the northern margin of the Cleaver Bank
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
type: Concept
created: 2021-02-10T09:33:09.563Z
alternative label: N-CBM-FS
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Western Dutch Platform Fault Domain

Intra Anglo-Dutch Basin Fault Domain
definition: Group of faults with various orientations within Anglo-Dutch Basin
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990026
type: Concept
created: 2021-02-10T09:33:09.593Z
alternative label: ADB-FD
narrower: ADB sub-salt NNW-SSE Fault Set
narrower: ADB sub-salt WNW-ESE Fault Set
narrower: ADB sub-salt WSW-ENE Fault Set
narrower: ADB sub-salt NNE-SSW Fault Set
narrower: ADB Supra-salt Fault Domain
references: https://data.geoscience.earth/ncl/geoera/ref/7698
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Western Dutch Platform Fault Domain

ADB Supra-salt Fault Domain
definition: Undifferentiated faults above the Zechstein Group within the Anglo-Dutch Basin
type: SpatialObject
notation: NL-990031
type: Concept
created: 2021-02-10T09:33:09.613Z
alternative label: ADB-SUPRA-FD
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Intra Anglo-Dutch Basin Fault Domain

ADB sub-salt NNE-SSW Fault Set
definition: Faults with a NNE-SSW orietation below the Zechstein Group within the Anglo-Dutch Basin
type: SpatialObject
notation: NL-990030
type: Concept
created: 2021-02-10T09:33:09.609Z
alternative label: ADB-SUB-NNE-SSW-FSET
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Intra Anglo-Dutch Basin Fault Domain

ADB sub-salt WSW-ENE Fault Set
definition: Faults with a WSW-ENE orietation below the Zechstein Group within the Anglo-Dutch Basin
type: SpatialObject
notation: NL-990029
type: Concept
created: 2021-02-10T09:33:09.605Z
alternative label: ADB-SUB-WSW-ENE-FSET
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Intra Anglo-Dutch Basin Fault Domain

ADB sub-salt WNW-ESE Fault Set
definition: Faults with a WNW-ESE orietation below the Zechstein Group within the Anglo-Dutch Basin
type: SpatialObject
notation: NL-990028
type: Concept
created: 2021-02-10T09:33:09.601Z
alternative label: ADB-SUB-WNW-ESE-FSET
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Intra Anglo-Dutch Basin Fault Domain

ADB sub-salt NNW-SSE Fault Set
definition: Faults with a NNW-SSE orietation below the Zechstein Group within the Anglo-Dutch Basin
type: SpatialObject
notation: NL-990027
type: Concept
created: 2021-02-10T09:33:09.598Z
alternative label: ADB-SUB-NNW-SSE-FSET
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Intra Anglo-Dutch Basin Fault Domain

Eastern Dutch Platform Fault Domain
definition: A structural domain largely defined by the area east of the Dutch Central Graben
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990039
type: Concept
created: 2021-02-10T09:33:09.642Z
alternative label: EDP-FD
narrower: Rif Gronden Fault System
narrower: Intra Schill Grund Platform Fault Domain
narrower: Intra Ameland Platform Fault Domain
narrower: G and L Platform Fault Set
narrower: Intra Terschelling Basin Fault Domain
narrower: Hantum Fault System
narrower: Gronau Fault System
narrower: Holsloot Fault System
narrower: Lower Saxony basin Fault Domain
narrower: Vlieland Basin Fault Domain
narrower: Friesland Platform Fault Domain
narrower: Texel-Ijsselmeer High Fault System
narrower: Raalte Boundary Fault System
narrower: Lauwerzee Trough Fault Domain
narrower: Western Lauwerzee Trough Fault System
narrower: Eastern Lauwerzee Trough Fault System
narrower: Groningen Platform Fault Domain
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Southern North Sea Lüneberg Fault Domain

Intra Terschelling Basin Fault Domain
definition: Faults within the Terschelling Basin
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990056
type: Concept
created: 2021-02-10T09:33:09.709Z
alternative label: TB-FD
narrower: Terschelling Basin sub-salt Fault Domain
narrower: Terschelling Basin supra-salt Fault Domain
references: https://data.geoscience.earth/ncl/geoera/ref/7705
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Eastern Dutch Platform Fault Domain

Terschelling Basin supra-salt Fault Domain
definition: Undifferentiated faults above the Zechstein Group within the Terschelling Basin
type: SpatialObject
notation: NL-990058
type: Concept
created: 2021-02-10T09:33:09.717Z
alternative label: TB-SUPRA-FD
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Intra Terschelling Basin Fault Domain

Terschelling Basin sub-salt Fault Domain
definition: Undifferentiated faults below the Zechstein Group within the Terschelling Basin
type: SpatialObject
notation: NL-990057
type: Concept
created: 2021-02-10T09:33:09.713Z
alternative label: TB-SUB-FD
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Intra Terschelling Basin Fault Domain

Intra Ameland Platform Fault Domain
definition: Group of fault within the Ameland Platform that is partly delimited to the east by the Western Lauwerszee Trough Fault System
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990044
type: Concept
created: 2021-02-10T09:33:09.662Z
alternative label: AP-FD
narrower: Ameland Platform sub-salt NNW-SSE Fault Set
narrower: Ameland Platform sub-salt WNW-ESE Fault Set
narrower: Ameland Platform Platform sub-salt WSW-ENE Fault Set
narrower: Ameland Platform Platform sub-salt NNE-SSW Fault Set
narrower: Ameland Platform supra-salt Fault Domain
references: https://data.geoscience.earth/ncl/geoera/ref/7705
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Eastern Dutch Platform Fault Domain

Ameland Platform sub-salt NNW-SSE Fault Set
definition: Faults with a N-S W orietation below the Zechstein Group within the Ameland Platform
type: SpatialObject
notation: NL-990045
type: Concept
created: 2021-02-10T09:33:09.666Z
alternative label: AP-SUB-NNW-SSE-FSET
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Intra Ameland Platform Fault Domain

Ameland Platform supra-salt Fault Domain
definition: Faults above the Zechstein Group with predominantly NW-SE and WNW-ESE orientation within the Ameland Platform
type: SpatialObject
notation: NL-990049
type: Concept
created: 2021-02-10T09:33:09.682Z
alternative label: AP-SUPRA-FD
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Intra Ameland Platform Fault Domain

Ameland Platform Platform sub-salt NNE-SSW Fault Set
definition: Faults with a NNE-SSW orietation below the Zechstein Group within the Ameland Platform
type: SpatialObject
notation: NL-990048
type: Concept
created: 2021-02-10T09:33:09.678Z
alternative label: APP-SUB-NNE-SSW-FSET
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Intra Ameland Platform Fault Domain

Ameland Platform Platform sub-salt WSW-ENE Fault Set
definition: Faults with a WSW-ENE orietation below the Zechstein Group within the Ameland Platform
type: SpatialObject
notation: NL-990047
type: Concept
created: 2021-02-10T09:33:09.675Z
alternative label: AP-SUB-WSW-ENE-FSET
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Intra Ameland Platform Fault Domain

Ameland Platform sub-salt WNW-ESE Fault Set
definition: Faults with a WNW-ESE orietation below the Zechstein Group within the Ameland Platform
type: SpatialObject
notation: NL-990046
type: Concept
created: 2021-02-10T09:33:09.671Z
alternative label: AP-SUB-WNW-ESE-FSET
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Intra Ameland Platform Fault Domain

Texel-Ijsselmeer High Fault System
definition: Alignment of NW-SE faults and structural blocks defining the
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990077
type: Concept
created: 2021-02-10T09:33:09.794Z
alternative label: TIJH-FS
narrower: Northern Texel-Ijsselmeer High sub Fault System
narrower: Southern Texel-Ijsselmeer High sub Fault System
narrower: Intra Texel IJsselmeer Fault Domain
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Eastern Dutch Platform Fault Domain

Northern Texel-Ijsselmeer High sub Fault System
definition: In the western part of the Netherlands, the Texel-IJsselmeer Fault System is the northernmost marginal fault of the Texel-IJsselmeer High
type: SpatialObject
notation: NL-990078
type: Concept
created: 2021-02-10T09:33:09.798Z
alternative label: N-TIJHM-SFS
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Texel-Ijsselmeer High Fault System

Intra Texel IJsselmeer Fault Domain
definition: Undifferentiated faults within the Texel-IJsselmeer High
type: SpatialObject
notation: NL-990080
type: Concept
created: 2021-02-10T09:33:09.806Z
alternative label: TIJM-FD
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Texel-Ijsselmeer High Fault System

Southern Texel-Ijsselmeer High sub Fault System
definition: In the western part of the Netherlands, the Texel-IJsselmeer Fault System is the southernmost marginal fault of the Texel-IJsselmeer High
type: SpatialObject
notation: NL-990079
type: Concept
created: 2021-02-10T09:33:09.802Z
alternative label: S-TIJHM-SFS
references: https://data.geoscience.earth/ncl/geoera/ref/7707
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Texel-Ijsselmeer High Fault System

Vlieland Basin Fault Domain
definition: A group of faults within the Friesland Platform that define the Vlieland Basin
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990063
type: Concept
created: 2021-02-10T09:33:09.738Z
alternative label: VB-FS
narrower: Southern Vlieland Basin Boundary Fault System
narrower: Intra Vlieland Basin Fault Domain
references: https://data.geoscience.earth/ncl/geoera/ref/7705
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Eastern Dutch Platform Fault Domain

Intra Vlieland Basin Fault Domain
definition: Faults within the Vlieland Basin
type: SpatialObject
notation: NL-990065
type: Concept
created: 2021-02-10T09:33:09.746Z
alternative label: VB-FD
narrower: Vlieland Basin sub-salt Fault Domain
narrower: Vlieland Basin supra-salt Fault Domain
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Vlieland Basin Fault Domain

Vlieland Basin supra-salt Fault Domain
definition: Undifferentiated faults above the Zechstein Group within the Vlieland Basin
type: SpatialObject
notation: NL-990067
type: Concept
created: 2021-02-10T09:33:09.754Z
alternative label: VB-SUPRA-FD
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Intra Vlieland Basin Fault Domain

Vlieland Basin sub-salt Fault Domain
definition: Undifferentiated faults below the Zechstein Group within the Vlieland Basin
type: SpatialObject
notation: NL-990066
type: Concept
created: 2021-02-10T09:33:09.750Z
alternative label: VB-SUB-FD
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Intra Vlieland Basin Fault Domain

Southern Vlieland Basin Boundary Fault System
definition: The southern marginal fault system of the Vlieland Basin that together with the Texel-IJsselmeer High Fault System forms a step-like transition to the Texel-IJsselmeer High
type: SpatialObject
notation: NL-990064
type: Concept
created: 2021-02-10T09:33:09.743Z
alternative label: S-VB-SFS
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Vlieland Basin Fault Domain

Groningen Platform Fault Domain
definition: Undifferentiated faults within the Groningen Platform that forms the eastern block to the east of the Lauwerzee Trough and delimits the Lower Saxony Basin to the North. It continues offshore into the area defined as Dutch-German G&L Platform Fault Set
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990087
type: Concept
created: 2021-02-10T09:33:09.849Z
alternative label: GP-FD
narrower: Groningen Platform sub-salt Fault Domain
narrower: Groningen Platform supra-salt Fault Domain
references: https://data.geoscience.earth/ncl/geoera/ref/7705
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Eastern Dutch Platform Fault Domain

Groningen Platform supra-salt Fault Domain
definition: Undifferentiated faults above the Zechstein Group within Groningen Platform
type: SpatialObject
notation: NL-990089
type: Concept
created: 2021-02-10T09:33:09.858Z
alternative label: GP-SUPRA-FD
references: https://data.geoscience.earth/ncl/geoera/ref/7705
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Groningen Platform Fault Domain

Groningen Platform sub-salt Fault Domain
definition: A complex fault pattern with 4 main fault groups at Rotliegend- and deeper stratigraphic levels that can related to at least three phases of deformtation since Paleozoic times. Early Carbinferous carbonate platforms are generally bounded by NE-SE faults supporing the notion that these are lon-leved Paleozoic structures. The lack of similarly faulted Rotliegend outcrop analogues and the fact that these strain features can thus only be studied in seismic data leaves room for multiple interpretations
type: SpatialObject
notation: NL-990088
type: Concept
created: 2021-02-10T09:33:09.853Z
alternative label: GP-SUB-FD
references: https://data.geoscience.earth/ncl/geoera/ref/7709
references: https://data.geoscience.earth/ncl/geoera/ref/7700
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Groningen Platform Fault Domain

Eastern Lauwerzee Trough Fault System
definition: A complex amalgamation of differently oriented faults making up the transistion between the Groningen Platform and the Lauwerzee Trough. This fault system post dates the NW-SE faults in the area and is of Mesozoic age.
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990086
type: Concept
created: 2021-02-10T09:33:09.844Z
alternative label: ELZT_FS
references: https://data.geoscience.earth/ncl/geoera/ref/7700
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Eastern Dutch Platform Fault Domain

Intra Schill Grund Platform Fault Domain
definition: Group of faults with various orientations within the Schilgrund Platform
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990041
type: Concept
created: 2021-02-10T09:33:09.650Z
alternative label: SGP-FD
narrower: Schill Grund Platform sub-salt Fault Domain
narrower: Schill Grund Platform supra-salt FaultDomain
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Eastern Dutch Platform Fault Domain

Schill Grund Platform supra-salt FaultDomain
definition: Undifferentiated faults above the Zechstein Group within the Schilgrund Platform
type: SpatialObject
notation: NL-990043
type: Concept
created: 2021-02-10T09:33:09.658Z
alternative label: SGP-SUPRA-FD
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Intra Schill Grund Platform Fault Domain

Schill Grund Platform sub-salt Fault Domain
definition: Undifferentiated faults below the Zechstein Group within the Schilgrund Platform
type: SpatialObject
notation: NL-990042
type: Concept
created: 2021-02-10T09:33:09.654Z
alternative label: SGP-SUB-FD
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Intra Schill Grund Platform Fault Domain

Western Lauwerzee Trough Fault System
definition: A complex amalgamation of differently oriented faults making up the transistion between the Groningen Platform and the Lauwerzee Trough. This fault system post dates the NW-SE faults in the area and is of Mesozoic age.
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990085
type: Concept
created: 2021-02-10T09:33:09.826Z
alternative label: WLZT-FS
references: https://data.geoscience.earth/ncl/geoera/ref/7700
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Eastern Dutch Platform Fault Domain

Rif Gronden Fault System
definition: Southern boundary fault zone to the Schilgrund Platform
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990040
type: Concept
created: 2021-02-10T09:33:09.646Z
alternative label: RG-FS
references: https://data.geoscience.earth/ncl/geoera/ref/7705
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Eastern Dutch Platform Fault Domain

Lower Saxony basin Fault Domain
definition: Undifferentiated faults within the Lower Saxony Basin
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990062
type: Concept
created: 2021-02-10T09:33:09.734Z
alternative label: LSB_FD
references: https://data.geoscience.earth/ncl/geoera/ref/7705
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Eastern Dutch Platform Fault Domain

G and L Platform Fault Set
definition: Aligned NNW-SSE faults in the offshore blocks G and L north of (and part of) the Groningen Platform that continues accros the border with Germany
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990050
type: Concept
created: 2021-02-10T09:33:09.686Z
alternative label: GLP-FSET
narrower: G en L Platform sub-salt NNW-SSE Fault Set
narrower: G en L Platform sub-salt WNW-ESE Fault Set
narrower: G en L Platform sub-salt WSW-ENE Fault Set
narrower: G en L Platform sub-salt NNE-SSW Fault Set
narrower: G en L Platform Supra-salt Fault Domain
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Eastern Dutch Platform Fault Domain

G en L Platform Supra-salt Fault Domain
definition: Faults above the Zechstein Group with predominantly NW-SE and WNW-ESE orientation within the G&L Platform
type: SpatialObject
notation: NL-990055
type: Concept
created: 2021-02-10T09:33:09.705Z
alternative label: GLP-SUPRA-FD
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: G and L Platform Fault Set

G en L Platform sub-salt NNE-SSW Fault Set
definition: Faults with a NNE-SSW orietation below the Zechstein Group within the G&L Platform
type: SpatialObject
notation: NL-990054
type: Concept
created: 2021-02-10T09:33:09.701Z
alternative label: GLP-SUB-NNE-SSW-FSET
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: G and L Platform Fault Set

G en L Platform sub-salt WSW-ENE Fault Set
definition: Faults with a WSW-ENE orietation below the Zechstein Group within the G&L Platform
type: SpatialObject
notation: NL-990053
type: Concept
created: 2021-02-10T09:33:09.697Z
alternative label: GLP-SUB-WSW-ENE-FSET
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: G and L Platform Fault Set

G en L Platform sub-salt WNW-ESE Fault Set
definition: Faults with a WNW-ESE orietation below the Zechstein Group within the G&L Platform
type: SpatialObject
notation: NL-990052
type: Concept
created: 2021-02-10T09:33:09.694Z
alternative label: GLP-SUB-WNW-ESE-FSET
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: G and L Platform Fault Set

G en L Platform sub-salt NNW-SSE Fault Set
definition: Faults with a N-S W orietation below the Zechstein Group within the G&L Platform
type: SpatialObject
notation: NL-990051
type: Concept
created: 2021-02-10T09:33:09.690Z
alternative label: GLP-SUB-NNW-SSE-FSET
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: G and L Platform Fault Set

Holsloot Fault System
definition: The Holsloot Fautl System transects the Lower Saxony Basin in its western part and divides a structurally deeper basin in the east from a shallower basin in the west. Plausibly the Holsloot Fault System forms the connection between the Western Lauwerzee Trough Fault System and the Gronau Fault System
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990061
type: Concept
created: 2021-02-10T09:33:09.730Z
alternative label: HS-FS
references: https://data.geoscience.earth/ncl/geoera/ref/7703
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Eastern Dutch Platform Fault Domain

Gronau Fault System
definition: NNW-SSE oriented fault zone active during the Paleozoic (Westphalian C and -D), also referred to as Osning-Gronau Fault System
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990060
type: Concept
created: 2021-02-10T09:33:09.726Z
alternative label: GR-FS
references: https://data.geoscience.earth/ncl/geoera/ref/7708
references: https://data.geoscience.earth/ncl/geoera/ref/7704
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Eastern Dutch Platform Fault Domain

Lauwerzee Trough Fault Domain
definition: Undifferentiated faults within the Lauwerzee Through. The domain extents northward in the offshore where it merges with the Ameland Platform
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990082
type: Concept
created: 2021-02-10T09:33:09.813Z
alternative label: LZT-FD
narrower: Lauwerzee Trough sub-salt Fault Domain
narrower: Lauwerzee Trough supra-salt Fault Domain
references: https://data.geoscience.earth/ncl/geoera/ref/7705
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Eastern Dutch Platform Fault Domain

Lauwerzee Trough supra-salt Fault Domain
definition: The fault pattern above the salt is relatively simple and contains several long regional fault zones as well as smaller-scale faults associated with salt structures (diapirs and ridges). The salt structures, however, have a genetic and to some extent locational relationship to large offset faults below the salt (the sub-salt faults)
type: SpatialObject
notation: NL-990084
type: Concept
created: 2021-02-10T09:33:09.822Z
alternative label: LZT-SUPRA-FD
references: https://data.geoscience.earth/ncl/geoera/ref/7705
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Lauwerzee Trough Fault Domain

Lauwerzee Trough sub-salt Fault Domain
definition: A complex fault pattern at Rotliegend and deeper stratigraphic levels that cannot be easily related to one single phase of faulting with one single stress orientation. More likely, the faults and fault zones evolved through multiple phases of fault activity. Early Carboniferous carbonate platforms are generally bounded by NW-SE faults supporing the notion that these are long-lived Paleozoic structures. The lack of similarly faulted Rotliegend outcrop analogues and the fact that these strain features can thus only be studied in seismic data leaves room for multiple interpretations
type: SpatialObject
notation: NL-990083
type: Concept
created: 2021-02-10T09:33:09.818Z
alternative label: LZT-SUB-FD
references: https://data.geoscience.earth/ncl/geoera/ref/7700
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Lauwerzee Trough Fault Domain

Hantum Fault System
definition: In origin the Hantum Fault System is a Variscan structure that separates the Friesland PLatform from the Terschelling Basin to the North. It was likely instrumental in defining the northern limit of the Lower Carboniferous carbonate platform on the Friesland Platform. The fault system extents to the northwest, probably across the Dutch Central Graben where it may form (or merges) with the Northern Cleaver Bank Margin Fault System. To the southeast it is thought to cross the Lauwerzee Trough where it becomes overprinten by multiple younger faults with various orientations
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990059
type: Concept
created: 2021-02-10T09:33:09.721Z
alternative label: H-FS
references: https://data.geoscience.earth/ncl/geoera/ref/7700
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Eastern Dutch Platform Fault Domain

Raalte Boundary Fault System
definition: In the eastern part of the Netherlands, the Raalte Boundary Fault System is the southermost marginal fault of the Friesland Platform s.l.
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990081
type: Concept
created: 2021-02-10T09:33:09.809Z
alternative label: RB-FS
references: https://data.geoscience.earth/ncl/geoera/ref/7705
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Eastern Dutch Platform Fault Domain

Friesland Platform Fault Domain
definition: The Friesland Platform represents a large and geologically diverse area and is characterised by multiple fault orientations both below and above the Zechstein salt. Early Carbinferous carbonate platforms are generally bounded by NE-SE faults supporing the notion that these are long-lived Paleozoic structures. The platform experienced Middle to Late Jurassic erosion (Mid and Late Kimmerian unconformity). In the north -eastern and southern part of the Friesland Platform, the Triassic can reach a thickness up to 800 m. In the northeast, the Friesland Platform is fault-bounded by the Lauwerszee Trough. Towards the southwest, the Texel-IJsselmeer High forms the boundary. In the northwest, the Friesland Platform passes into the Late Jurassic - Early Cretaceous Vlieland Basin and in the southeast towards the Lower Saxony Basin.
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990068
type: Concept
created: 2021-02-10T09:33:09.758Z
alternative label: FP-FD
narrower: Friesland Platform sub-salt NNW-SSE Fault Set
narrower: Friesland Platform sub-salt WNW-ESE Fault Set
narrower: Friesland Platform sub-salt WSW-ENE Fault Set
narrower: Friesland Platform sub-salt NNE-SSW Fault Set
narrower: Friesland Platfrom supra-salt Fault Domain
narrower: Eastern Friesland Platform Fault Domain
narrower: Dalfsen High Fault Domain
narrower: Northern Dalfsen Faults Set
references: https://data.geoscience.earth/ncl/geoera/ref/7707
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Eastern Dutch Platform Fault Domain

Northern Dalfsen Faults Set
definition: A series of WNW-ESE trending step faults forming the northern margin of the Dalfsen High
type: SpatialObject
notation: NL-990076
type: Concept
created: 2021-02-10T09:33:09.791Z
alternative label: ND-FSET
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Friesland Platform Fault Domain

Dalfsen High Fault Domain
definition: The Dalfsen High (DH) is a relatively small isolated high on the Friesland Platform on strike with the Texel-IJsselmeer High, bounded to te south by the Raalt Boundary Fault System and transected by WNW-ESE fauts. It is characterised by Cretaceous sediments on top Carboniferous rocks. In the area surrounding the DH, the Triassic has been eroded, which points to a Jurassic or more recent phase of uplift. The northern margin is defined by the Northern Dalfsen Fault Set
type: SpatialObject
notation: NL-990075
type: Concept
created: 2021-02-10T09:33:09.786Z
alternative label: DH-FD
references: https://data.geoscience.earth/ncl/geoera/ref/7705
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Friesland Platform Fault Domain

Eastern Friesland Platform Fault Domain
definition: En-echelon pattern of NNE-SSW trending faults forming the transition to the Dalfsen sub Domain
type: SpatialObject
notation: NL-990074
type: Concept
created: 2021-02-10T09:33:09.782Z
alternative label: E-FP-FD
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Friesland Platform Fault Domain

Friesland Platfrom supra-salt Fault Domain
definition: Undifferentiated faults above the Zechstein Group within the Friesland Platform
type: SpatialObject
notation: NL-990073
type: Concept
created: 2021-02-10T09:33:09.779Z
alternative label: FP-SUPRA-FD
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Friesland Platform Fault Domain

Friesland Platform sub-salt NNE-SSW Fault Set
definition: Faults with a NNE-SSW orietation below the Zechstein Group within the Friesland Platform
type: SpatialObject
notation: NL-990072
type: Concept
created: 2021-02-10T09:33:09.775Z
alternative label: FP-SUB-NNE-SSW-FSET
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Friesland Platform Fault Domain

Friesland Platform sub-salt WSW-ENE Fault Set
definition: Faults with a WSW-ENE orietation below the Zechstein Group within the Friesland Platform
type: SpatialObject
notation: NL-990071
type: Concept
created: 2021-02-10T09:33:09.771Z
alternative label: FP-SUB-WSW-ENE-FSET
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Friesland Platform Fault Domain

Friesland Platform sub-salt WNW-ESE Fault Set
definition: Faults with a ESE-WNW orietation below the Zechstein Group within the Friesland Platform
type: SpatialObject
notation: NL-990070
type: Concept
created: 2021-02-10T09:33:09.767Z
alternative label: FP-SUB-WNW-ESE-FSET
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Friesland Platform Fault Domain

Friesland Platform sub-salt NNW-SSE Fault Set
definition: Faults with a NNE-SSW orietation below the Zechstein Group within the Friesland Platform
type: SpatialObject
notation: NL-990069
type: Concept
created: 2021-02-10T09:33:09.763Z
alternative label: FP-SUB-NNW-SSE-FSET
in scheme: Tectonic Boundary Objects in Europe
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Friesland Platform Fault Domain

Dowsing-South Hewett Large Scale Fault System
definition: In the Dutch territory, the Dowsing-South Hewett Large Scale Fault System marks a strong and long-lived contrast between the Wales-Brabant massif and Southern North Sea Basin that was repeatedly reactivated since at least the Carboniferous. The Dowsing-South Hewett Fault Zone, was active during the Carboniferous and possibly earlier times. However, The northwestward continuation as southern boundary of the Calledonian Southern North Sea Lüneberg Terrane is unclear as it does not cross the Southern Uplands/Mid North Sea high.
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990113
type: Concept
created: 2021-02-10T09:33:09.953Z
alternative label: DSH-LFS
narrower: Dowsing-South Hewett Fault System
narrower: Southern West Netherlands Basin - Ruhr Valley Graben Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/7714
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Tectonic Boundary in the Netherlands

Southern West Netherlands Basin - Ruhr Valley Graben Fault System
definition: Eastern part of the Dowsing-South Hewett Large Scale Fault System that defines the southern boundary of the West Netherland Basin - Ruhr Valley Graben Basin basin system
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990115
type: Concept
created: 2021-02-10T09:33:09.962Z
alternative label: S-WNB-RVG-FS
narrower: Southern West Netherlands Basin sub Fault System
narrower: Veldhoven sub Fault System
narrower: FeldBiss sub Fault System
references: https://data.geoscience.earth/ncl/geoera/ref/7707
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Dowsing-South Hewett Large Scale Fault System

FeldBiss sub Fault System
definition: Aligned group of normal faults forming the southwestern border zone of the RVG that were active mainly during the Cenozoic extension but might originate from older faults
type: SpatialObject
references: https://data.geoscience.earth/ncl/geoera/ref/7707
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990118
type: Concept
created: 2021-02-10T09:33:09.974Z
alternative label: FBS-sFS
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Southern West Netherlands Basin - Ruhr Valley Graben Fault System

Veldhoven sub Fault System
definition: Aligned group of normal faults forming the southwestern border zone of the RVG that were active mainly during the Cenozoic extension but might originate from older faults
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990117
type: Concept
created: 2021-02-10T09:33:09.970Z
alternative label: VEH-sFS
references: https://data.geoscience.earth/ncl/geoera/ref/7702
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Southern West Netherlands Basin - Ruhr Valley Graben Fault System

Southern West Netherlands Basin sub Fault System
definition: Group of normal faults in the southwestern border zone of the West Netherland Basin that were active during the Mesozoic and - to a lesser extent- Cenozoic extension and inversion phases . They might originate from older faults
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990116
type: Concept
created: 2021-02-10T09:33:09.966Z
alternative label: S-WNB-sFS
references: https://data.geoscience.earth/ncl/geoera/ref/7707
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Southern West Netherlands Basin - Ruhr Valley Graben Fault System

Dowsing-South Hewett Fault System
definition: A fault system defined by 1) the South Hewett Fault zoney that forms the southern boundary of the Late Permian-Mesozoic Sole Pit trough and 2) its westward continuations into the Dowsing Fault zone that forms the southern margin faults zone of the the Late Permian-Mesozoic Silverpit basin in the UK sector
type: SpatialObject
in scheme: Tectonic Boundary Objects in Europe
notation: NL-990114
type: Concept
created: 2021-02-10T09:33:09.957Z
alternative label: DSH-FS
references: https://data.geoscience.earth/ncl/geoera/ref/7699
references: https://data.geoscience.earth/ncl/geoera/ref/7711
in scheme: Tectonic Boundary Objects in carbonate geothermal reservoirs of Europe
broader: Dowsing-South Hewett Large Scale Fault System

Fault classification terms and parameters
hierarchy root: true
hierarchy root type: ConceptScheme
description: This vocabulary describes a) the hierarchical classification of shear displacement structures and b) parameters used in the attribute list of the HIKE fault data base that extend existing INSPIRE and/or GeoSciML code lists
title: Klassifikation Tektonischer Grenzflächen @de
definition: A formal classification scheme for the elements of the HIKE fault data base that allows a hierarchical ranking of mostly shear displacement structures like e.g. faults, shear zones. It is mainly base on Hintersberger et al. (2017), but has been extended to include further concepts from other countries.
type: ConceptScheme
created: 2020-05-08T14:19:40.180Z
has top concept: Fault classification term
has top concept: Attribute parameters of the HIKE fault data base

Fault classification term
narrower: Tectonic Boundary
top concept of: Fault classification terms and parameters
created: 2021-02-16T07:03:58.771Z
type: Concept
definition: A formal classification scheme for the elements of the HIKE fault data base that allows a hierarchical ranking of mostly shear displacement structures like e.g. faults, shear zones and fissures. It is mainly base on Hintersberger et al. (2017), but has been extended to further concepts in order to describe the tectonic frame work of other countries.
in scheme: Fault classification terms and parameters

Tectonic Boundary
type: Concept
created: 2020-05-08T14:19:40.221Z
preferred label: Tektonische Grenzfläche @de
definition: A Tectonic Boundary is a shear displacement structure separating tectonic units and includes all brittle to ductile style structures along which displacement has occurred, from a simple, single 'planar' brittle or ductile surface to a fault system comprised of tens of strands of both brittle and ductile nature (after GeoSciML Modeling Team, 2017).
definition: Eine Tektonische Grenzfläche ist eine Scherfläche, die tektonische Einheiten trennt und alle spröden bis duktilen Strukturen einschließt, entlang denen die Verschiebung stattgefunden hat, von einer einfachen, einzelnen „planaren“ spröden oder duktilen Fläche bis zu einem Störungssystem bestehend aus mehreren spröden und/oder duktilen Anteilen (nach GeoSciML Modeling Team, 2017). @de
narrower: Fault Set
narrower: Nappe Boundary
narrower: Step fault
narrower: Large-scale Fault System
narrower: Fault Domain
narrower: Volcanic system
references: https://data.geoscience.earth/ncl/geoera/ref/875
in scheme: Fault classification terms and parameters
broader: Fault classification term

Step fault
type: Concept
created: 2020-05-08T14:19:40.330Z
in scheme: Fault classification terms and parameters
broader: Tectonic Boundary

Large-scale Fault System
type: Concept
created: 2020-05-08T14:19:40.358Z
scope note: In the hierarchical ranking, fault systems are merged into a Large-scale Fault System (LFS) if their extent and impact on the orogenic evolution are of transregional importance (i.e. the Periadraric-Mid-Hungarian Large-scale Fault system for the Alpine Orogen).
preferred label: Großstörungssystem @de
definition: A Large-scale Fault System (LFS) corresponds to the highest level of the Tectonic Boundaries Classification Scheme and describes an alignment of connected and kinematically related fault systems that extend transregionally, typically over hundreds of kilometers. (Hintersberger et al. 2017:197).
definition: Ein Großstörungssystem entspricht der höchsten Stufe in der Klassifikation zu Tektonischen Grenzflächen und beschreibt eine Anordnung von verbundenen und kinematisch in Beziehung stehenden Störungssystemen, die sich überregional und typischerweise über Hunderte von Kilometern erstrecken (Hintersberger et al. 2017:197). @de
narrower: Fault System
narrower: Subfault System
references: https://data.geoscience.earth/ncl/geoera/ref/88
in scheme: Fault classification terms and parameters
broader: Tectonic Boundary

Fault System
type: Concept
created: 2020-05-08T14:19:40.386Z
preferred label: Störungssystem @de
example: For example, the Salzach-Ennstal-Mariazell-Puchberg (SEMP) Fault System (Ratschbacher et al., 1991a, b; Decker et al., 1994; Linzer et al., 2002) is a 400 km long ENE–WSW trending fault system consisting of several faults.
definition: A Fault System corresponds to an alignment of connected and kinematically related faults and/or shear zones active during at least one or potentially several geological events and that may contain different deformation styles (modified after Neuendorf et al., 2005). The faults within a fault system must be related spatially and kinematically at least during one main deformation event (Hintersberger et al., 2017:198).
definition: Eine Anordnung von (miteinander) verbundenen und kinematisch in Beziehung stehenden Störungen und/oder Scherzonen, welche über einen längeren geologischen Zeitraum (mehrere Perioden/Stufen/Events) aktiv sind und mehrere Deformationsarten beinhalten können (verändert nach Neuendorf et al., 2005). Die Störungen innerhalb eines Störungssystems müssen räumlich und kinematisch, zumindest während eines Haupt-Deformationsereignisses, mitneinander in Beziehung stehen (Hintersberger et al., 2017:198). @de
narrower: Fault
narrower: Shear zone
references: https://data.geoscience.earth/ncl/geoera/ref/88
in scheme: Fault classification terms and parameters
broader: Large-scale Fault System

Fault
type: Concept
created: 2020-05-08T14:19:40.414Z
scope note: In the German the terms 'Verwerfung', 'Verwurf', 'Bruch' and 'Abbruch' are used as synonyms for faults. The terms 'Bruch' and 'Abbruch' are associated with normal faulting kinematics.
preferred label: Störung @de
definition: The term fault is used here in the sense of a discrete deforming interface separating two rock masses along which one mass has slid past the other (Neuendorf et al., 2005). Deformation in faults is dominated by brittle deformation mechanisms (Schultz & Fossen, 2008). (Hintersberger et al., 2017:198)
definition: Eine diskrete tektonische Grenzfläche oder Zone diskreter Flächen, welche zwei Gesteinskörper/massen trennt und an derer parallel Bewegung stattgefunden hat (Neudendorf et al., 2005). Im allgemeinen Verständnis dominieren spröde Deformationsmechanismen (Schultz & Fossen, 2008). (Hintersberger et al., 2017:198) @de
narrower: Subfault
references: https://data.geoscience.earth/ncl/geoera/ref/88
alternative label: Verwurf @de
alternative label: Bruch @de
alternative label: Abbruch @de
alternative label: Verwerfung @de
in scheme: Fault classification terms and parameters
broader: Fault System

Subfault
type: Concept
created: 2020-05-08T14:19:40.442Z
preferred label: Teilstörung @de
definition: A subfault is a subordinated discrete interface separating two rock masses along which one mass has slid past the other, belonging to an ordinated fault (Neuendorf et al., 2005). (Hintersberger et al., 2017:199)
definition: Eine Teilstörung ist, eine der Störung untergeordnete, diskrete Grenzfläche, die zwei Gesteinsmassen trennt und an der Bewegung stattgefunden hat (Neuendorf et al., 2005). (Hintersberger et al., 2017:199) @de
references: https://data.geoscience.earth/ncl/geoera/ref/88
in scheme: Fault classification terms and parameters
broader: Fault

Shear zone
type: Concept
created: 2020-05-08T14:19:40.471Z
scope note: Shear zones may contain either brittle or ductile fault rocks. Here, deformation in shear zones is dominated by ductile deformation mechanisms (Schultz & Fossen, 2008, and references therein) involving dynamic recrystallization, diffusive mass transfer, dislocation creep and/or grain-boundary sliding. It also includes the term “Mylonite Zone” describing relatively thick zones of intensive ductile shearing (Mawer, 1986).
preferred label: Scherzone @de
definition: A broad planar zone of relatively intense localised deformation (shearing) in which progressive deformation is non-coaxial (Passchier & Trouw, 1996; Hintersberger et al., 2017:198).
definition: Breite planare Zone lokalisierter und relativ intensiver Deformation, in der die progressive Deformation nicht-koaxial (scherend) ist (Passchier & Trouw, 1996; Hintersberger et al., 2017:198). @de
references: https://data.geoscience.earth/ncl/geoera/ref/88
in scheme: Fault classification terms and parameters
broader: Fault System

Subfault System
type: Concept
created: 2020-05-08T14:19:40.499Z
scope note: Shear displacement structures containing at least a ductile and a brittle part are hierarchically considered as a Subfault System. For example, the Brenner SFS consists of the ductile lowangle Brenner Shear Zone and the steeper brittle Brenner Fault.
preferred label: Teilstörungssystem @de
definition: A Subfault System is a part of a fault system defined by spatial, temporal or kinematic characteristics that are different from the overall deformation of the related fault system during at least one main deformation event (Hintersberger et al., 2017:198).
definition: Teil eines Störungssystems, welcher sich aus Störungen und/oder Scherzonen zusammensetzt und einen räumlich, zeitlich, beziehungsweise kinematisch in Beziehung stehenden Teilabschnitt definiert, welcher sich durch mindestens einen Hauptdeformations-Event vom zugehörigen Störungssystem unterscheiden lässt (Hintersberger et al. 2017:198). @de
alternative label: Störungszone @de
alternative label: Fault Zone
references: https://data.geoscience.earth/ncl/geoera/ref/88
in scheme: Fault classification terms and parameters
broader: Large-scale Fault System

Volcanic system
type: Concept
created: 2020-05-08T14:19:40.613Z
narrower: Fissure Set
in scheme: Fault classification terms and parameters
broader: Tectonic Boundary

Fissure Set
type: Concept
created: 2020-05-08T14:19:40.641Z
narrower: Fissure
in scheme: Fault classification terms and parameters
broader: Volcanic system

Fissure
type: Concept
created: 2020-05-08T14:19:40.670Z
in scheme: Fault classification terms and parameters
references: https://data.geoscience.earth/ncl/geoera/ref/8763
definition: Fissures are volcanic vents. They present as linear features on the surface and are created by the non-explosive eruption of lava. In some cases the fissures make rows of craters.
broader: Fissure Set
broader: Fault type

Fault Set
type: Concept
created: 2020-05-08T14:19:40.244Z
scope note: The category 'Fault Set' is mostly used for (sub-)parallel oriented faults in orogens, e.g. the Northern Calcareous Alps, which are subdivided into five groups striking NNE–SSW, NE–SW, ENE–WSW, E–W, NW–SE, respectively.
preferred label: Störungsset @de
definition: A Fault Set describes an alignment of parallel trending faults that are kinematically and temporally linked, but where the spacing between the single fault zones exceeds the displacement observed along the fault. It does not correspond to the term “fault zone” (Hintersberger et al., 2017:198).
definition: Der Begriff Störungsset definiert eine Anordnung von parallel verlaufenden (Teil-)Störungen, welche kinematisch und zeitlich in Verbindung stehen, wobei aber die Abstände zwischen den einzelnen Störungen (im Gegensatz zu Störungszonen) den beobachteten Versatz entlang der Störungen übertrifft (Hintersberger et al., 2017:198). @de
references: https://data.geoscience.earth/ncl/geoera/ref/88
in scheme: Fault classification terms and parameters
broader: Tectonic Boundary

Nappe Boundary
type: Concept
created: 2020-05-08T14:19:40.274Z
definition: The term describes a discrete, brittle or ductile, shearing horizon between tectonic units (e.g. nappes, nappe systems). In this definition, „discrete“ refers to map scale, since in the field a nappe boundary can correspond to a diffuse tectonic mélange zone with elements of both units that it separates (Hintersberger et al. 2017:199).
alternative label: Base of Nappe
references: https://data.geoscience.earth/ncl/geoera/ref/88
in scheme: Fault classification terms and parameters
broader: Tectonic Boundary

Fault Domain
type: Concept
created: 2020-05-08T14:19:40.527Z
scope note: In contrast to Large-scale Fault Systems (LFS) which are more or less linear alignment of (sub-)parallel faults or fault systems, the term 'Fault Domain' applies for areal (non-linear) terrains of similar fault pattern. If any confusion with geological domains would arise, the term 'fault realm' could be used for clarification purposes.
preferred label: Domäne @de
definition: Fault domain describes an area/terrain of similar pattern of fault array implying a similar tectonic regime. Direct subsets can be Subdomains, Fault Systems and/or Faults
definition: Domäne bezeichnet ein Gebiet mit ähnlichen Störungsmustern, die ein vergleichbares tektonisches Regime implizieren. Untereinheiten können Subdomänen, Störungssysteme und/oder Störungen sein. @de
narrower: Fault Subdomain
source: Structural domains
alternative label: Fault Realm
alternative label: structural domain
in scheme: Fault classification terms and parameters
broader: Tectonic Boundary

Fault Subdomain
type: Concept
created: 2020-05-08T14:19:40.556Z
scope note: Fault Subdomain is a subset of Fault domain. This category can be used to distinguish between areas of (subordinate) differenes of fault pattern within a Fault domain. If linear arrays of faults are distinguished the term 'Fault System' applies.
preferred label: Subdomäne @de
definition: Fault subdomains describes distinguishable areas of closely similar pattern of fault array within a Fault domain.
definition: Subdomänen bezeichen unterscheidbare Gebiete sehr ähnlicher Störungsmuster innerhalb einer Domäne. @de
narrower: Fault Chain
in scheme: Fault classification terms and parameters
narrower: Fault Swarm
broader: Fault Domain

Fault Swarm
type: Concept
created: 2020-05-08T14:19:40.302Z
in scheme: Fault classification terms and parameters
definition: A fault swarm is an array of discrete faults with small offsets of same type and formed during the same deformation episode, most probably resulting from distortion caused by movment of blocks along faults with curved profiles (Laubach et al., 1992, 1995).
alternative label: Fault Cluster
preferred label: Störungsschwarm @de
scope note: A Fault Swarm is not necessarily linearly arranged, whereas the fault chain describes a linear array of faults.
references: https://data.geoscience.earth/ncl/geoera/ref/8762
broader: Fault Subdomain

Fault Chain
type: Concept
created: 2020-05-08T14:19:40.585Z
preferred label: Störungszug @de
definition: A string (linear array) of faults (including minor subfaults) inferred to represent one single supraregional fault. Faults of the same type and formed during the same deformation episode.
alternative label: Fault Train
in scheme: Fault classification terms and parameters
broader: Fault Subdomain

Attribute parameters of the HIKE fault data base
top concept of: Fault classification terms and parameters
created: 2021-02-16T07:09:12.027Z
type: Concept
narrower: Offset determination
narrower: Related subsurface activity
narrower: Movement sense
narrower: Dip direction
narrower: Strike
narrower: Fault type
narrower: Evaluation method
narrower: Observation method
narrower: Maximum displacement
in scheme: Fault classification terms and parameters
definition: Here, parameters describing the fault attributes of the HIKE European Fault Database are listet. In general, attribute parameters were choosen to be as close as possible in accordance with INSPIRE and GeoSciML codelists, but mostly do not exactly match the description nor its purpose in the INSPIRE or GeoSciML data model. Additional fault attribute parameters that do not appear in the INSPIRE registry are defined in this Project Vocabulary.

Maximum displacement
created: 2021-02-16T12:23:00.424Z
type: Concept
definition: Displacement in meters as measurement in map view. The default displacement is measured perpendicular to the fault line/trace. If the sense of movement is either (normal/reverse_)dextral or (normal/reverse_)sinistral, the displacement is measured parallel to the fault trace.
in scheme: Fault classification terms and parameters
broader: Attribute parameters of the HIKE fault data base

Fault type
created: 2021-02-16T07:24:00.919Z
type: Concept
definition: The fault type is defined exactly as proposed in the INSPIRE registry. Additional fault types that do not appear in the INSPIRE registry are defined in this Project Vocabulary
narrower: Fissure
narrower: ring fault
narrower: fault (INSPIRE)
in scheme: Fault classification terms and parameters
broader: Attribute parameters of the HIKE fault data base

fault (INSPIRE)
narrower: high angle fault
narrower: low angle fault
type: Concept
definition: A discrete surface, or zone of discrete surfaces, with some thickness, separating two rock masses across which one mass has slid past the other.
in scheme: Fault classification terms and parameters
in scheme: INSPIRE codelists
broader: Fault type

INSPIRE codelists
created: 2020-07-14T06:24:42.126Z
type: ConceptScheme

high angle fault
type: Concept
definition: Fault that dips at least 45 degrees over more than half of its recognized extent, for which slip or separation is not explicitly specified.
in scheme: Fault classification terms and parameters
in scheme: INSPIRE codelists
broader: fault (INSPIRE)

low angle fault
type: Concept
definition: Fault that dips less than 45 degrees over more than half of the recognized extent of the fault.
in scheme: Fault classification terms and parameters
in scheme: INSPIRE codelists
broader: fault (INSPIRE)

ring fault
created: 2021-02-16T07:25:51.115Z
type: Concept
alternative label: caldera fault
definition: A ring fault, also known as caldera fault, is a fault that occur within a collapsed volcanic caldera and the site of bolide strikes, such as the Chesapeake Bay impact crater. Ring faults are result of a series of overlapping normal faults, forming a circular outline.
in scheme: Fault classification terms and parameters
broader: Fault type

Related subsurface activity
created: 2021-02-16T07:15:23.084Z
type: Concept
definition: Known human subsurface activities in relation to the fault. The definition of the attribute parameters is related to the INSPIRE code list BoreholePurposeValue, but do not exactly match the description.
narrower: Exploration of minerals
narrower: Exploration of oil & gas
narrower: Exploration of geothermal energy
narrower: Exploration of groundwater
in scheme: Fault classification terms and parameters
broader: Attribute parameters of the HIKE fault data base

Exploration of groundwater
type: Concept
created: 2021-02-16T07:17:31.051Z
definition: Activity for examination of the subsurface with regard to the extraction of groundwater from an aquifer for various purposes (domestic, industrial, water supply intake and other)
definition: Entnahme von Grundwasser aus einem Grundwasserleiter zu verschiedenen Zwecken (Haushalte, Industrie, Wasserversorgung und andere) @de
in scheme: Fault classification terms and parameters
broader: Related subsurface activity

Exploration of minerals
created: 2021-02-16T07:17:00.737Z
type: Concept
definition: Activity for examination of the subsurface with regard to the locating and/or extracting mineral resources from the subsurface.
in scheme: Fault classification terms and parameters
broader: Related subsurface activity

Exploration of geothermal energy
created: 2021-02-16T07:17:21.882Z
type: Concept
definition: Activity for examination of the subsurface with regard to the utilization of geothermal energy resources and design of geothermal heat pumps.
in scheme: Fault classification terms and parameters
broader: Related subsurface activity

Exploration of oil & gas
type: Concept
created: 2021-02-16T07:17:10.175Z
definition: Activity for examination of the subsurface with regard to the availability of fossil energy resources and planning the extraction thereof.
in scheme: Fault classification terms and parameters
broader: Related subsurface activity

Offset determination
type: Concept
created: 2021-02-16T07:12:42.564Z
definition: Method how the displacement at a fault has been determined.
narrower: crosscutting relationships
narrower: displacement on maps
narrower: field observation
narrower: microfabrics
narrower: palaeogeography
narrower: paleoseismicity
narrower: paleostress measurements
narrower: sediment structures
narrower: seismicity
narrower: well/seismic interpretation
in scheme: Fault classification terms and parameters
broader: Attribute parameters of the HIKE fault data base

well/seismic interpretation
created: 2021-02-15T15:42:34.754Z
type: Concept
top concept of: Fault offset determination
definition: This term refers to the determination of displacement across a (mostly buried) fault based on interpretation of well and/or seismic information
notation: 3
in scheme: Fault offset determination
in scheme: Fault classification terms and parameters
broader: Offset determination

Fault offset determination
description: .. here should be a short, 3-line text - describing the relevant scheme and allow the user to get started with the topic via the listed top concepts ..
type: ConceptScheme
created: 2021-02-15T15:39:04.374Z
hierarchy root: true
hierarchy root type: ConceptScheme
has top concept: palaeogeography
has top concept: crosscutting relationships
has top concept: well/seismic interpretation
has top concept: paleoseismicity
has top concept: displacement on maps
has top concept: seismicity
has top concept: sediment structures
has top concept: paleostress measurements
has top concept: field observation
has top concept: microfabrics

crosscutting relationships
top concept of: Fault offset determination
type: Concept
created: 2021-02-15T15:42:34.751Z
notation: 2
definition: This term refers to the principle of cross-cutting relationships for the determination of displacement across a fault. Cross-cutting relationships is a principle of geology that states that the geologic feature which cuts another is the younger of the two features. It is a relative dating technique in geology.
in scheme: Fault offset determination
in scheme: Fault classification terms and parameters
broader: Offset determination

displacement on maps
type: Concept
created: 2021-02-15T15:42:34.767Z
top concept of: Fault offset determination
notation: 5
definition: This term refers to the determination of displacement across a fault based on information shown on geological maps
in scheme: Fault offset determination
in scheme: Fault classification terms and parameters
broader: Offset determination

paleoseismicity
top concept of: Fault offset determination
type: Concept
created: 2021-02-15T15:42:34.757Z
notation: 4
definition: This term Paleoseismicity refers to geologically recorded earthquakes, most of them unknown from human descriptions or seismograms. Geologic records of past earthquakes can include faulted layers of sediment and rock, injections of liquefied sand, landslides, abruptly raised or lowered shorelines, and tsunami deposits
in scheme: Fault offset determination
in scheme: Fault classification terms and parameters
broader: Offset determination

palaeogeography
type: Concept
top concept of: Fault offset determination
created: 2021-02-15T15:42:34.748Z
notation: 1
definition: This term describes the usage of paleogeographic reconstructions for the determination of the amount of displacement across a fault.
in scheme: Fault offset determination
in scheme: Fault classification terms and parameters
broader: Offset determination

sediment structures
created: 2021-02-15T15:42:34.777Z
type: Concept
top concept of: Fault offset determination
notation: 7
definition: This term refers to the determination of displacement across a fault based on sediment structures
in scheme: Fault offset determination
in scheme: Fault classification terms and parameters
broader: Offset determination

seismicity
top concept of: Fault offset determination
created: 2021-02-15T15:42:34.773Z
type: Concept
notation: 6
definition: This term refers to the determination of displacement across a fault based on seismological information shown on geological maps
in scheme: Fault offset determination
in scheme: Fault classification terms and parameters
broader: Offset determination

field observation
type: Concept
top concept of: Fault offset determination
created: 2021-02-15T15:42:34.784Z
notation: 9
definition: This term refers to the determination of displacement across a fault based on geological field observations such as shear sense indicators or offset observed at outcrop scale.
in scheme: Fault offset determination
in scheme: Fault classification terms and parameters
broader: Offset determination

microfabrics
created: 2021-02-15T15:42:34.787Z
top concept of: Fault offset determination
type: Concept
notation: 10
definition: This term refers to the usage of microfabric analysis to determine the characteristics of displacement across a fault. The microstructural characterization of a crystalline material includes the determination of grain number and size distribution, chemical composition, spatial distribution of phases, crystallographic and structural relationships between grains as well as intragranular misorientation.
in scheme: Fault offset determination
in scheme: Fault classification terms and parameters
broader: Offset determination

paleostress measurements
top concept of: Fault offset determination
created: 2021-02-15T15:42:34.780Z
type: Concept
notation: 8
definition: This term refers to the determination of displacement across a fault based on paleostress analyses.
in scheme: Fault offset determination
in scheme: Fault classification terms and parameters
broader: Offset determination

Evaluation method
created: 2021-02-16T07:26:55.848Z
type: Concept
narrower: observed at depth
narrower: direct observation
in scheme: Fault classification terms and parameters
narrower: inferred
definition: The information given for the “evaluation method” is used as a rough quality measure for the following fault attribute set. It should give a qualitative statement how reliable the observations and the derived fault attributes are. The definition of the attribute parameters is partly related to the GeoSciML classifier code list MappedFeatureObservationMethod , but do not exactly match the description and does not include all options.
broader: Attribute parameters of the HIKE fault data base

direct observation
in scheme: Fault classification terms and parameters
type: Concept
definition: This evaluation method describes the highest evaluation quality, which related to a "direct visual observation", e.g. at an outcrop at the surface.
broader: Evaluation method

observed at depth
type: Concept
created: 2021-02-16T07:27:42.545Z
definition: this evaluation method describes the fact that the respective tectonic boundary has been observed at depth and the fault is generelly assumed to be buried.
in scheme: Fault classification terms and parameters
broader: Evaluation method

inferred
type: Concept
in scheme: Fault classification terms and parameters
definition: The evaluation method “inferred” describes that the fault is neither directly observed at the surface nor observed at depth by reliable methods, but its location and specification are based on inference from available evidence.
broader: Evaluation method

Movement sense
created: 2021-02-16T07:20:02.243Z
type: Concept
definition: Movement sense describes the relative direction of movement of bodies of rock across a fault surface, as defined by the IUGS Commission for Geoscience Information (CGI) Geoscience Terminology Working Group.
narrower: detachment
narrower: dextral
narrower: generic decollement
narrower: normal
narrower: normal dextral
narrower: normal sinistral
narrower: reverse
narrower: reverse dextral
narrower: reverse sinistral
narrower: sinistral
narrower: thrust
narrower: thrust decollement
narrower: no movement sense
in scheme: Fault classification terms and parameters
broader: Attribute parameters of the HIKE fault data base

normal sinistral
type: Concept
in scheme: Fault classification terms and parameters
broader: Movement sense

detachment
type: Concept
in scheme: Fault classification terms and parameters
broader: Movement sense

dextral
type: Concept
in scheme: Fault classification terms and parameters
broader: Movement sense

sinistral
type: Concept
in scheme: Fault classification terms and parameters
broader: Movement sense

reverse sinistral
type: Concept
in scheme: Fault classification terms and parameters
broader: Movement sense

thrust
type: Concept
in scheme: Fault classification terms and parameters
broader: Movement sense

generic decollement
type: Concept
in scheme: Fault classification terms and parameters
broader: Movement sense

normal dextral
type: Concept
in scheme: Fault classification terms and parameters
broader: Movement sense

reverse
type: Concept
in scheme: Fault classification terms and parameters
broader: Movement sense

no movement sense
type: Concept
in scheme: Fault classification terms and parameters
broader: Movement sense

normal
type: Concept
in scheme: Fault classification terms and parameters
broader: Movement sense

reverse dextral
type: Concept
in scheme: Fault classification terms and parameters
broader: Movement sense

thrust decollement
type: Concept
in scheme: Fault classification terms and parameters
broader: Movement sense

Strike
type: Concept
created: 2021-02-16T07:22:23.020Z
alternative label: trend
scope note: For the purpose of the HIKE fault database, the faults are sorted into strike categories. Directions are classified in 8 classes of each 22,5 degrees (WNW-ESE, NW-SE, NNW-SSE, N-S, NNE-SSW, NE-SW, ENE-WSW, E-W).
definition: Strike is defined as the compass direction, relative to north, of the line formed by the intersection of a rock layer or other planar feature with an imaginary horizontal plane. The intersection of two flat planes is a straight line, and in this instance, the line is geologic strike.
in scheme: Fault classification terms and parameters
broader: Attribute parameters of the HIKE fault data base

Dip direction
type: Concept
created: 2021-02-16T07:21:00.937Z
scope note: For the purpose of the HIKE European fault database, the faults are sorted into dip direction categories. Directions are classified in 16 classes of each 22,5 degrees (N, NNE, NE, ENE, E, ESE, SE, SSE, S, SSW, SW, WSW, W, WNW, NW, NNW).
definition: Dip direction is the azimuth perpendicular to the strike of the structure.
in scheme: Fault classification terms and parameters
broader: Attribute parameters of the HIKE fault data base

Observation method
type: Concept
created: 2021-02-16T07:28:41.100Z
narrower: airborne Geophysical Survey
narrower: ground Magnetic Survey
narrower: seismological Survey
narrower: georadar survey
narrower: time-domain EM Survey
narrower: ground Gravity Survey
narrower: borehole Logging Survey
narrower: 1D Resistivity Survey
narrower: 2D Seismic Survey
narrower: frequency Domain EM Survey
narrower: magnetotelluric Survey
narrower: sonar Survey
narrower: observed borehole material
narrower: observed outcrop
narrower: inferred projection between observed locations
narrower: CPT Survey
in scheme: Fault classification terms and parameters
narrower: 3D Seismic Survey
narrower: VSP Survey
narrower: 2D Resistivity Survey
narrower: 3D Resistivity Survey
definition: Observation method gives an overview of the most important methods how the location and the characteristics of a fault objects were obtained. The list of possible methods is based on the INSPIRE codelist entries of “SurveyTypeValue” and includes some definitions of the GeoSciML vocabulary entry “MappedFeature ObservationMethod”, but do not exactly match the description nor its purpose in the INSPIRE or GeoSciML data model.
broader: Attribute parameters of the HIKE fault data base

airborne Geophysical Survey
in scheme: Fault classification terms and parameters
in scheme: INSPIRE codelists
type: Concept
definition: The fault and its characteristics have been observed during a campaign of airborne geophysical measurements, where the geophysical data is obtained by an apparatus fixed to a helicopter, fixed wing, or ultra light aircraft, depending on location and topographic relief.
broader: Observation method

seismological Survey
in scheme: INSPIRE codelists
type: Concept
in scheme: Fault classification terms and parameters
definition: The fault and its characteristics have been observed during a campaign of seismological measurements, where vibrations from natural earthquakes or rupture processes (due to hydraulic stimulation) are used as a source for structural imaging of the subsurface.
broader: Observation method

2D Seismic Survey
type: Concept
in scheme: INSPIRE codelists
in scheme: Fault classification terms and parameters
definition: The fault and its characteristics have been observed during a campaign of 2D seismic measurements, where the behavior of artificially-generated seismic waves in the subsurface is recorded. A seismic wave or pulse is generated at the surface by an active seismic source which can be a vibration, mechanical impact, or near-surface explosion.
broader: Observation method

observed borehole material
created: 2021-02-16T09:30:10.259Z
type: Concept
in scheme: Fault classification terms and parameters
definition: The fault and its characteristics have been directly observed in material obtained from a borehole (e.g., borehole core). If the observation method is “observed borehole material”, the evaluation method (see section 4.4.1.1) should be given as “direct observation”.
broader: Observation method

magnetotelluric Survey
type: Concept
in scheme: Fault classification terms and parameters
in scheme: INSPIRE codelists
definition: The fault and its characteristics have been observed during a campaign of magnetotelluric measurements where the electrical resistivity structure of the subsurface is measured through the measurement of electrical and magnetic fields at the earth's surface.
broader: Observation method

2D Resistivity Survey
type: Concept
in scheme: INSPIRE codelists
in scheme: Fault classification terms and parameters
definition: The fault and its characteristics have been observed during a campaign of 2D multi-electrode direct current measurements, in which current is applied to the ground using electrodes and the earth response (voltage or potential difference) is recorded and presented as a 2D geoelectric section showing apparent resistivity distribution.
broader: Observation method

time-domain EM Survey
in scheme: INSPIRE codelists
type: Concept
in scheme: Fault classification terms and parameters
definition: The fault and its characteristics have been observed during a campaign of The option “observed at depth” refers to the fact that the respective fault information has been observed at depth and the fault is generally assumed to be buried.
broader: Observation method

inferred projection between observed locations
type: Concept
created: 2021-02-16T09:30:42.311Z
in scheme: Fault classification terms and parameters
definition: The determination of the location of the fault, its existence or/and its characteristics is based on inferred continuity with observed locations, and assumption of continuity of the feature. If “inferred projection between observed locations” is given, the evaluation method (see section 4.4.1.1) should be set as “inferred”.
broader: Observation method

3D Seismic Survey
in scheme: Fault classification terms and parameters
in scheme: INSPIRE codelists
type: Concept
definition: The fault and its characteristics have been observed during a campaign of 3D seismic measurements, where the behavior of artificially-generated seismic waves in the subsurface is recorded. A seismic wave or pulse is generated at the surface by an active seismic source which can be a vibration, mechanical impact, or near-surface explosion.
broader: Observation method

sonar Survey
in scheme: Fault classification terms and parameters
type: Concept
in scheme: INSPIRE codelists
definition: The fault and its characteristics have been observed during a campaign of sonar (sound navigation and ranging) measurements, where underwater sound propagation is used, among other applications, for bathymetric mapping, sub-bottom profiling, and gas leak detection.
broader: Observation method

observed outcrop
created: 2021-02-16T09:30:29.341Z
type: Concept
in scheme: Fault classification terms and parameters
definition: The fault and its characteristics have been observed and located directly in outcrop(s), where geologist(s) occupied location of phenomenon, and traced it explicitly over mapped extent. If the observation method is “observed at outcrop”, the evaluation method (see section 4.4.1.1) should be given as “direct observation”.
broader: Observation method

3D Resistivity Survey
type: Concept
in scheme: INSPIRE codelists
in scheme: Fault classification terms and parameters
definition: The fault and its characteristics have been observed during a campaign of 3D multi-electrode direct current measurements, in which current is applied to the ground using electrodes and the earth response (voltage or potential difference) is recorded and presented as a 3D block showing apparent resistivity distribution.
broader: Observation method

georadar survey
type: Concept
in scheme: INSPIRE codelists
in scheme: Fault classification terms and parameters
definition: The fault and its characteristics have been observed during a campaign of ground penetrating radar (GPR) or georadar, where high-frequency electromagnetic waves are used to map below-ground lithology or buried objects.
broader: Observation method

frequency Domain EM Survey
in scheme: Fault classification terms and parameters
type: Concept
in scheme: INSPIRE codelists
definition: The fault and its characteristics have been observed during a campaign of frequency-domain electromagnetic (EM) measurements, where the electrical conductivity of the subsurface through electromagnetic induction is mapped by using continuous wave field methods.
broader: Observation method

ground Magnetic Survey
type: Concept
in scheme: INSPIRE codelists
in scheme: Fault classification terms and parameters
definition: The fault and its characteristics have been observed during a campaign of surface magnetic measurements, recorded at an observation point on the earth's surface.
broader: Observation method

1D Resistivity Survey
type: Concept
in scheme: INSPIRE codelists
in scheme: Fault classification terms and parameters
definition: The fault and its characteristics have been observed during a campaign of vertical electric sounding measurements, which provides information regarding the change in apparent resistivity of the subsurface with depth.
broader: Observation method

ground Gravity Survey
type: Concept
in scheme: Fault classification terms and parameters
in scheme: INSPIRE codelists
definition: The fault and its characteristics have been observed during a campaign of surface gravity measurements, recorded at an observation point on the earth's surface.
broader: Observation method

VSP Survey
type: Concept
in scheme: INSPIRE codelists
in scheme: Fault classification terms and parameters
definition: The fault and its characteristics have been observed during a campaign of Vertical Seismic Profiling (VSP), where the detectors for seismic measurements are in a borehole.
broader: Observation method

CPT Survey
in scheme: INSPIRE codelists
in scheme: Fault classification terms and parameters
type: Concept
definition: The fault and its characteristics have been observed during a campaign of cone penetration test (CPT) sounding measurements, where the geotechnical engineering properties of soils are determined by pushing an instrumented cone into the ground at a controlled rate.
broader: Observation method

borehole Logging Survey
in scheme: INSPIRE codelists
in scheme: Fault classification terms and parameters
type: Concept
definition: The fault and its characteristics have been observed during a campaign of borehole logging, where physical, chemical, and structural properties of penetrated geological formations are measured using tools that are lowered into a borehole on a wireline cables.
broader: Observation method