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  • 1
    Call number: 21/STR 05/14
    In: Scientific technical report
    Type of Medium: GFZ publications
    Pages: X, 144 S.
    Series Statement: Scientific technical report / Geoforschungszentrum Potsdam 05/14
    Classification: A.3.16.
    Note: Zugl.: Berlin, Freie Univ., Diss., 2005
    Location: Reading room
    Branch Library: GFZ Library
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  • 2
    Call number: S 97.0506(577-2/1)
    In: Forschungsbericht
    Type of Medium: Series available for loan
    Pages: 139 S. : Ill., graph. Darst.
    ISBN: 9783936418910
    Series Statement: DGMK research report 577-2/1
    Classification: A.3.16.
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 3
    Call number: S 97.0506(577-2/2)
    In: Forschungsbericht
    Type of Medium: Series available for loan
    Pages: 90 S. : Ill., Kt.
    Edition: Als Ms. gedr.
    ISBN: 9783941721081
    Series Statement: DGMK research report 577-2/2
    Classification: A.3.16.
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 4
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    Potsdam : Deutsches GeoForschungsZentrum GFZ
    Associated volumes
    Call number: STR 11/08
    In: Scientific Technical Report STR - Data
    Type of Medium: 12
    Pages: Online-Ressource
    Series Statement: Scientific Technical Report STR - Data 11/08
    Branch Library: GFZ Library
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  • 5
    Publication Date: 2012-02-13
    Description: The Central European Basin System (CEBS) includes the former Northern and Southern Permian Basins together with superimposed Meso-Cenozoic sub-basins and contains a thick layer of Upper Permian (Zechstein) salt. This salt was mobilized in response to several post-Permian tectonic events. In order to analyse the regional relationship between the structural pattern of the Meso-Cenozoic sedimentary cover and the distribution of the Upper Permian salt, a 3D structural model of the CEBS has been constructed. In this model, the Permian salt is resolved as an extra layer for the entire basin system. According to the 3D structural model, the salt layer is strongly deformed as a result of halokinetic activity. The thickest salt is localized within salt walls and diapirs, reaching up to 9 km of thickness. A regional structural 3D analysis of the overburden in relation to underlying ductile salt demonstrates that the geometry of the sedimentary cover is strongly complicated by a variety of salt structures. The withdrawal of the Permian salt appears to have played a key role in both deposition and deformation of Meso-Cenozoic deposits in addition to tectonically forced regional subsidence.
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  • 6
    Publication Date: 2017-10-07
    Description: Abstract
    Description: The data files belong to a 3D structural model which covers the Vøring and Møre basins offshore Norway. In addition, a part of the exposed Fennoscandian Caledonides in the south-east and an oceanic crustal domain are covered by the model. The constructed 3D model is 490 km wide and 660 km long with a horizontal grid spacing of 2500 m, and a vertical resolution corresponding to the number of integrated layers. The lithospheric-scale 3D structural model includes 14 layers: (1) sea water;(2) upper Neogene (post-middle Miocene) sediments;(3) middle-upper Paleogene-lower Neogene (pre-middle Miocene) sediments;(4) lower Paleogene (Paleocene) sediments;(5) oceanic layer 2AB (basalts);(6) Upper Cretaceous (post-Cenomanian) sediments;(7) Lower Cretaceous (preCenomanian) sediments;(8) pre-Cretaceous sediments;(9) continental crystalline crust;(10) oceanic layer 3A;(11) high-density zones within the continental crystalline crust;(12) oceanic layer 3B;(13) high-density bodies within the lower continental crystalline crust;(14) lithospheric mantle. The thicknesses of the layers correspond to apparent thicknesses. In addition, data for earth surface topography is provided in the file: 0_Topography.dat.Model coordinates are based on the UTM 33 Zone (Northern Hemisphere) using the WGS 84 datum. The data format is ASCII and contains three columns (X, Y and Z), where X and Y are geographical coordinates (X = longitude, Y = latitude); Z (in m) is thickness of the layer or structural depth (base of layer) or surface elevation. The grid of each layer consists of 196 cells in W-E direction and 265 cells in S-N direction. The grid limits are the following: Xmin = -222590 and Xmax = 267410; Ymin = 6892200 and Ymax = 7552200. The vertical datum of the 3D model refers to the mean sea level. Organisation of data files: Data are organised in two folders (“Bases” and “Thicknesses”); data for earth surface topography (in case of water: sea level) is in the root folder: 0_Topography.dat. The folder “Bases” contains 14 data files named according to the model layers as outlined above. The folder “Thicknesses” contains 14 data files named according to the model layers as outlined above.
    Keywords: continental margin ; structural model ; Vøring Basin ; Møre Basin ; Norway
    Language: English
    Type: Dataset , Dataset
    Format: 11377451 Bytes
    Format: 1 Files
    Format: application/x-zip-compressed
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  • 7
    Publication Date: 2017-10-09
    Description: Abstract
    Description: The data files belong to a 3D structural model which covers the Glueckstadt Graben, NW Germany. The constructed 3D model is 170 km wide and 166 km long with a horizontal grid spacing of 2000 m, and a vertical resolution corresponding to the number of integrated layers. The 3D structural model includes 10 layers: (1) sea water; (2) Quaternary-Neogene; (3) Paleogene; (4) Upper Cretaceous; (5) Lower Cretaceous; (6) Jurassic; (7) uppermost part of the Middle Triassic and the Upper Triassic (Keuper); (8) Middle Triassic without uppermost and lowermost parts (Muschelkalk); (9) Lower Triassic and lowermost part of the Middle Triassic (Buntsandstein); (10) upper part of the Lower Permian and the Upper Permian (undivided Zechstein plus salt-rich Rotliegend). The thicknesses of the layers correspond to apparent thicknesses. In addition, data for earth surface topography is provided in the file: 0_Topography.dat. Model coordinates are based on the Gauss-Krueger DHDN (zone 3) system. The data format is ASCII and contains three columns (X, Y and Z), where X and Y are geographical coordinates (X = longitude, Y = latitude); Z (in m) is thickness of the layer or structural depth (base of layer) or surface elevation. The grid of each layer consists of 86 cells in W-E direction and 84 cells in S-N direction. The grid limits are the following: Xmin = 3450000 and Xmax = 3620000; Ymin = 5915100 and Ymax = 6081100. The vertical datum of the 3D model refers to the mean sea level. Organisation of data files: Data are organized in two folders (“Bases” and “Thicknesses”); data for earth surface topography (in case of water: sea level) is in the root folder ( 0_Topography.dat).The folder “Bases” contains 10 data files named according to the model layers as outlined above. The folder “Thicknesses” contains 10 data files named according to the model layers as outlined above.
    Keywords: structural model ; Glueckstadt Graben
    Language: English
    Type: Dataset , Dataset
    Format: 1362622 Bytes
    Format: 1 Files
    Format: application/x-zip-compressed
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  • 8
    Publication Date: 2018-07-30
    Description: thesis
    Keywords: VAE 830 ; VBL 500 ; TQC 220 ; TQG 000 ; VEB 110 ; TSB 110 ; Bruchschollenstrukturen {Geologie} ; Geologische Bohrungen in einzelnen Regionen ; Reflexionsseismik {Geophysik} ; Geophysikalische Bohrlochmessungen ; Norddeutsche Senke {Geologie} ; Norddeutsche Senke {Geophysik}
    Language: English
    Type: monograph , publishedVersion
    Format: 144 S.
    Format: application/pdf
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  • 9
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    GeoForschungsZentrum
    In:  Scientific Technical Report STR ; ISSN: 1610-0956 ; Year: 2005 ; Volume: 05/14 ; Pages: 1-144
    Publication Date: 2017-07-07
    Description: The Central European Basin System is one of the basins where the sedimentary cover is strongly affected by salt tectonics. The most significant stage of salt movement occurred during the Triassic. The largest Triassic subsidence occurred in the different sub-basins surrounding the Ringkoebing-Fyn High such as the Horn Graben, the Danish Basin and the Glueckstadt Graben. Furthermore, the thickest Triassic succession is observed in the Glueckstadt Graben where it reaches more than 9000 m. In the present study, the structure and the Permian to recent evolution of the Glueckstadt Graben are investigated by use of borehole data, seismic lines and 3D structural modelling. The evaluation of the diverse deformation patterns of the sedimentary cover and their relations to salt structures show that the strongest salt movements occurred at the beginning of the Keuper when the Gluckstadt Graben was affected by extension. The onlap patterns of the Jurassic sediments onto the top of the Keuper succession indicate essential changes of the sedimentation style during the Jurassic. Thick Jurassic sediments are only observed around salt structures and are thinning away from salt walls or salt stocks. The Upper Cretaceous strata have an approximately constant thickness and the parallel reflections patterns indicate a quiet tectonic setting with very minor salt movements in the Late Cretaceous. Renewed salt flow during the Paleogene-Neogene caused rapid subsidence along the marginal parts of the Central Triassic Graben in the Westholstein, the Eastholstein and the Hamburger troughs. The thick Paleogene-Neogene strata within the marginal troughs may also be related to a regional component of tectonic subsidence in the area, contemporary with rapid subsidence in the North Sea. The 3D modelling approach has been used to determine salt distribution at certain paleo-levels in response to unloading due to sequential removing of the stratigraphic layers. The modelling approach was also aimed to reconstruct the original Permian salt distribution immediately after deposition. The initial salt thickness varies from 1300 m at the flanks of the basin up to 3000 m within the central part and demonstrates a clear NNE-SSW trend of the basin. The regional trend of the restored salt distribution points to a westward continuation of the Permian salt basin. The formation of the deep Central Triassic Graben and the subsequent Jurassic- Cenozoic marginal troughs was strongly controlled by the development of salt structures through time. It is shown that the depocentre of sedimentation was moving away from the central part of the of the original Graben structure towards its margins. The evaluation of the available data and results of the 3D reverse modelling demonstrate that a greater amount of subsidence occurred close to the active salt structures, and may have resulted in gradual depletion of Permian salt. Thus, this study indicates that the source of such long-term subsidence is derived from gradual depletion of the Permian salt, which started within the axial part of the basin and moved towards the basin flanks with time. In this sense, the Glueckstadt Graben was formed at least partially as a “basin-scale rim syncline” during post-Permian times. Therefore, the results show that salt withdrawal may have played an important role during the Meso-Cenozoic evolution and that the effects of salt-driven subsidence during the Meso-Cenozoic can be considered the main reason for the formation of the deep Central Triassic Graben and the subsequent Jurassic-Cenozoic marginal troughs.
    Keywords: ddc:550
    Language: English
    Type: http://purl.org/eprint/type/Thesis
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  • 10
    Publication Date: 2017-11-10
    Description: The data files belong to a 3D structural model which covers the Glueckstadt Graben, NW Germany. The constructed 3D model is 170 km wide and 166 km long with a horizontal grid spacing of 2000 m, and a vertical resolution corresponding to the number of integrated layers. The 3D structural model includes 10 layers: (1) sea water; (2) Quaternary-Neogene; (3) Paleogene; (4) Upper Cretaceous; (5) Lower Cretaceous; (6) Jurassic; (7) uppermost part of the Middle Triassic and the Upper Triassic (Keuper); (8) Middle Triassic without uppermost and lowermost parts (Muschelkalk); (9) Lower Triassic and lowermost part of the Middle Triassic (Buntsandstein); (10) upper part of the Lower Permian and the Upper Permian (undivided Zechstein plus salt-rich Rotliegend). The thicknesses of the layers correspond to apparent thicknesses. In addition, data for earth surface topography is provided in the file- 0_Topography.dat. Model coordinates are based on the Gauss-Krueger DHDN (zone 3) system. The data format is ASCII and contains three columns (X, Y and Z), where X and Y are geographical coordinates (X = longitude, Y = latitude); Z (in m) is thickness of the layer or structural depth (base of layer) or surface elevation. The grid of each layer consists of 86 cells in W-E direction and 84 cells in S-N direction. The grid limits are the following: Xmin = 3450000 and Xmax = 3620000; Ymin = 5915100 and Ymax = 6081100. The vertical datum of the 3D model refers to the mean sea level. Organisation of data files: Data are organized in two folders (“Bases” and “Thicknesses”); data for earth surface topography (in case of water: sea level) is in the root folder ( 0_Topography.dat). The folder “Bases” contains 10 data files named according to the model layers as outlined above. The folder “Thicknesses” contains 10 data files named according to the model layers as outlined above.
    Keywords: ddc:550
    Language: English
    Type: http://purl.org/escidoc/metadata/ves/publication-types/paper
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