Abstract
The structure of the Glueckstadt Graben has been investigated by use of 3D gravity backstripping technique and by 2D gravity and magnetic modelling. Subtracting the gravity effects of the Meso-Cenozoic sediments together with Permian salt reveals a positive residual anomaly within the Glueckstadt Graben. This anomaly includes two local maxima over the Westholstein and Eastholstein Troughs. The 2D gravity models point to the presence of a high-density body within the lower crust of the Glueckstadt Graben. In addition, the results of 2D magnetic modelling indicate that the central part of the high-density body is overlain by an area with high susceptibility. Most probable, the formation of this high-density body is a result of complex poly-phase tectonic history of the study area. Finally, the results of gravity modelling indicate that Permian salt is not homogeneous. 3D gravity analysis and, especially, 2D gravity modelling have distinguished the differences in degree of salt saturation in salt-rich bodies, and elucidate the proportion of Rotliegend salt.
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Acknowledgments
The authors gratefully acknowledge the financial support of the German Research Council in the framework of the Priority Programme 1135—DFG-SPP 1135 “Dynamics of sedimentary systems under varying stress conditions by example of the Central European Basin system”. We are grateful to the DGMK as representative of the German Oil and Gas Industry for supporting us with data and allowing us to present industrial data (DGMK project 577). Special thanks go to the E&P-Gesellschaften for data assistance. We would also like to thank Heinz-Jürgen Brink and one anonymous reviewer for providing valuable and constructive reviews, which helped to improve the quality of the manuscript considerably.
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Yegorova, T., Maystrenko, Y., Bayer, U. et al. The Glueckstadt Graben of the North-German Basin: new insights into the structure from 3D and 2D gravity analyses. Int J Earth Sci (Geol Rundsch) 97, 915–930 (2008). https://doi.org/10.1007/s00531-007-0228-5
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DOI: https://doi.org/10.1007/s00531-007-0228-5