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The Cenozoic Lower Rhine Basin – rifting, sedimentation, and cyclic stratigraphy

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Abstract

In the Cenozoic, the Lower Rhine Basin formed as a rift at the southeastern terminus of the Dutch German Central Graben, while the Rhenish Massif was uplifted. The study focusses on the marginal marine and fluvial fill of the Lower Rhine Basin. A basin model is developed. Support for this study was given by extensive industry outcrop and well data, by new stratigraphical and sedimentological observations. The ingression and subsequent regression of the Cenozoic North Sea is analysed using the concept of base level cyclicity. As the geohistory of the basin was complex, a subsidence curve is constructed. Furthermore, an attempt is made to trace the simultaneous uplift of the Rhenish Massif.

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Acknowledgements

Rheinbraun AG (today RWE Power) (Köln), Erftverband (Bergheim), and Staatliches Umweltamt (Bonn) are kindly appreciated for the gratitude to use their well data, also thanks are due to Rheinbraun for their generous permission and help to enter their brown coal open-cast mines, where Gerhard Gross, Bertram Wutzler, and especially Fritz von der Hocht were altruistic guides for many years. The Deutsche Forschungsgemeinschaft (DFG) granted splendid financial support for all of us (SFB 350 – Bonn), for which we are deeply grateful. The paper benefitted from a DFG supported travel of A.S. to Tim A. Cross (Golden, Col., USA) some years ago, and from discussions with Tom Aigner, Volker Mosbrugger and Rahman Ashraf (Tübingen), with Agemar Siehl and Niko Froitzheim (Bonn), also and especially from many improvements suggested by the reviewers, who were Noel Vandenberghe (Leuven, Belgium) and Adam Vecsei (Leipzig). The late Hans Hager (Krefeld) initiated early steps into our research work. Tom McCann (Bonn) did the final reading; he not only corrected the English writing, but also suggested numerous valuable improvements to the manuscript. We thank all much for their help.

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Schäfer, A., Utescher, T., Klett, M. et al. The Cenozoic Lower Rhine Basin – rifting, sedimentation, and cyclic stratigraphy. Int J Earth Sci (Geol Rundsch) 94, 621–639 (2005). https://doi.org/10.1007/s00531-005-0499-7

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