Abstract
This study presents a reconstruction of the tectonic history of an Upper Rotliegend tight gas field in Northern Germany. Tectonism of the greater study area was influenced by multiple phases of salt movement, which produced a variety of salt-related structural features such as salt walls, salt diapirs as well as salt glaciers (namakiers). A sequential 2D retro-deformation and stratal backstripping methodology was used to differentiate mechanisms inducing salt movement and to discuss their relation to regional tectonics. The quantitative geometric restoration included sedimentary balancing, decompaction, fault-related deformation, salt movement, thermal subsidence, and isostasy to unravel the post-depositional tectonic overprint of the Rotliegend reservoir rock. The results of this study indicate that reactive salt diapirism started during an Early Triassic interval of thin-skinned extensional tectonics, followed by an active diapirism stage with an overburden salt piercement in the Late Triassic, and finally a period of intensive salt surface extrusion and the formation of salt glaciers (namakiers) in Late Triassic and Jurassic times. Since the Early Cretaceous, salt in the study area has been rising by passive diapirism.
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Acknowledgments
The study is part of the Wintershall and RWTH Aachen University Tight Gas Initiative. We thank Wintershall Holding GmbH and GDF Suez E&P Deutschland GmbH for providing the data and supporting this project. Thanks also to the IJES editorial staff, in particular chief editors Wolf-Christian Dullo and Jürgen Grötsch and the referees Reinhard Gaupp and Jos Okkerman for their constructive comments which greatly improved the manuscript. We are grateful to Schlumberger Ltd. and Midland Valley Ltd. for providing academic Petrel and Move licenses for the use at RWTH Aachen University.
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Vackiner, A.A., Antrett, P., Strozyk, F. et al. Salt kinematics and regional tectonics across a Permian gas field: a case study from East Frisia, NW Germany. Int J Earth Sci (Geol Rundsch) 102, 1701–1716 (2013). https://doi.org/10.1007/s00531-013-0887-3
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DOI: https://doi.org/10.1007/s00531-013-0887-3