Articles | Volume 12, issue 6
https://doi.org/10.5194/se-12-1443-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/se-12-1443-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Dawn and dusk of Late Cretaceous basin inversion in central Europe
Thomas Voigt
CORRESPONDING AUTHOR
Institut für Geowissenschaften,
Friedrich-Schiller-Universität Jena, Burgweg 11, 07749 Jena, Germany
Jonas Kley
Georg-August-Universität Göttingen, Geowissenschaftliches
Zentrum, Goldschmidtstraße 3, 37077 Göttingen
Silke Voigt
Goethe-Universität Frankfurt, Institut für Geowissenschaften,
Altenhöferallee 1, 60438 Frankfurt
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31 citations as recorded by crossref.
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- Calcareous dinoflagellate blooms during the Late Cretaceous ‘greenhouse’ world—a case study from western Ukraine A. Ciurej et al. 10.7717/peerj.16201
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- The benthic foraminiferal response to the mid-Maastrichtian event in the NW-European chalk sea of the Maastrichtian type area I. Vancoppenolle et al. 10.1017/njg.2022.10
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- Reconstruction of cyclic Mesozoic–Cenozoic stress development in SE Germany using fault-slip and stylolite inversion S. Köhler et al. 10.1017/S0016756822000656
- Petrophysical characterization, BIB-SEM imaging, and permeability models of tight carbonates from the Upper Jurassic (Malm ß), SE Germany S. Freitag et al. 10.1186/s40517-022-00239-x
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- Inversion tectonics in the Sorgenfrei–Tornquist Zone: insight from new marine seismic data at the Bornholm Gat, SW Baltic Sea Y. Pan et al. 10.1080/11035897.2022.2071335
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Latest update: 13 Dec 2024
Short summary
Basin inversion in central Europe is believed to have started during Late Cretaceous (middle Turonian) and probably proceeded until the Paleogene. Data from different marginal troughs in central Europe point to an earlier start of basin inversion (in the Cenomanian). The end of inversion is overprinted by general uplift but had probably already occurred in the late Campanian to Maastrichtian. Both the start and end of inversion occurred with low rates of uplift and subsidence.
Basin inversion in central Europe is believed to have started during Late Cretaceous (middle...
Special issue