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Structure and Evolution of the Glueckstadt Graben in Relation to the Other PostPermian Subbasins of the Central European Basin System

Authors

Maystrenko,  Y. P.
External Organizations;

/persons/resource/bayer

Bayer,  Ulf
3.2 Organic Geochemistry, 3.0 Geochemistry, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

/persons/resource/leni

Scheck-Wenderoth,  Magdalena
6.1 Basin Modelling, 6.0 Geotechnologies, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

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Citation

Maystrenko, Y. P., Bayer, U., Scheck-Wenderoth, M. (2017): Structure and Evolution of the Glueckstadt Graben in Relation to the Other PostPermian Subbasins of the Central European Basin System. - In: Soto, J. I., Flinch, J., Tari, G. (Eds.), Permo-Triassic Salt Provinces of Europe, North Africa and the Atlantic Margins: Tectonics and Hydrocarbon Potential, Amsterdam : Elsevier, 203-220.
https://doi.org/10.1016/B978-0-12-809417-4.00010-0


Cite as: https://gfzpublic.gfz-potsdam.de/pubman/item/item_2344910
Abstract
The Glueckstadt Graben is a key subbasin in terms of salt tectonics within the entire Central European Basin System, representing the most outstanding manifestation of salt movements throughout the basin system. The sedimentary pattern within this basin demonstrates that the Permian salt was a main controlling factor for the evolution of the Glueckstadt Graben, which was partially formed as a “basin-scale rim syncline” during Mesozoic-Cenozoic times. The tectonically induced gradual withdrawal of the Permian salt layer created additional accommodation space for deposition, showing a good correlation between the major phases of salt tectonics and tectonic activity within the Glueckstadt Graben.