Mesozoic Resource Potential in the Southern Permian Basin
CONTAINS OPEN ACCESS

The Southern Permian Basin, as its name suggests, is a historical heartland for hydrocarbon production from the Palaeozoic Rotliegend interval. However, in this mature basin the Mesozoic presents further possibilities to offer resource security to NW Europe. Such opportunities include increasing efficiency in the production of discovered hydrocarbons, exploration for further hydrocarbons (both conventional and unconventional) and efficient exploration for, and production of, geothermal energy. All these potential resources require a grounding in technically sound geoscience, via traditional scientific observation and the application of new technologies, to unlock their value.
The main aim of this volume is to bring together the work of academics and industry workers to consider cross-border geoscience including contributions on Poland, Germany, The Netherlands, the United Kingdom and adjacent areas. The work presented intends to contribute to the development and discovery of further Mesozoic energy resources across the basin.
The Wiek Fault System east of Rügen Island: origin, tectonic phases and its relationship to the Trans-European Suture Zone
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Published:January 01, 2018
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CiteCitation
Elisabeth Seidel, Martin Meschede, Karsten Obst, 2018. "The Wiek Fault System east of Rügen Island: origin, tectonic phases and its relationship to the Trans-European Suture Zone", Mesozoic Resource Potential in the Southern Permian Basin, B. Kilhams, P. A. Kukla, S. Mazur, T. McKie, H. F. Mijnlieff, K. van Ojik
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Abstract
The Tornquist Fan, reflecting the northern part of the Trans-European Suture Zone, comprises a series of fault zones and major single faults, striking mainly subparallel to the SW margin of the Fennoscandian Shield. The deep-seated faults of Wiek, Nord Jasmund and Schaabe, which cross the northern part of Rügen Island and areas of the adjacent Baltic Sea from NW to SE, originated in the late Paleozoic. They are accompanied by younger faults, especially in the Pomeranian Bay, that were formed by Mesozoic tectonic processes. Based on reprocessed offshore seismic lines east of Rügen, a polyphase evolution for the Wiek...
- Atlantic Ocean
- Baltic region
- Baltic Sea
- block structures
- Caledonian Orogeny
- Carboniferous
- Central Europe
- compression tectonics
- Cretaceous
- data bases
- data processing
- Devonian
- en echelon faults
- Europe
- extension tectonics
- fault zones
- faults
- Fennoscandian Shield
- geophysical methods
- geophysical profiles
- geophysical surveys
- Germany
- Laurussia
- mapping
- Mecklenburg-Western Pomerania Germany
- Mesozoic
- Middle Devonian
- normal faults
- North Atlantic
- orogeny
- Paleozoic
- reconstruction
- reverse faults
- Rugen Island
- segmentation
- seismic methods
- seismic profiles
- seismic stratigraphy
- stress
- stress fields
- succession
- surveys
- suture zones
- systems
- tectonic elements
- tectonics
- Tornquist-Teisseyre Zone
- Upper Carboniferous
- Upper Cretaceous
- Variscan Orogeny
- Monchgut Peninsula
- Tornquist Fan
- Jasmund Peninsula
- Western Pomeranian fault system
- Wiek fault system