NDLI: Tertiary tectonics of the Dannemarie Basin, upper Rhine graben, and regional implications

Content Provider	Springer Nature Link
Author	Rotstein, Y. Schaming, M. Rousse, S.
Copyright Year	2005
Abstract	Recently released seismic reflection data, together with previous seismic and well data, are used to describe the development of the Dannemarie basin, in the SW end of the Upper Rhine Graben. The Dannemarie Basin was formed during the main rifting phase of the Upper Rhine Graben as an asymmetrical graben trending NE–SW. Post-rift tectonism shifted the depocenter southward and changed the overall shape of the basin. Miocene Jura compression did not result in the formation of folds, as in the adjacent Mulhouse Horst. Strike slip faulting was dominant in the post-rift period and new faults were created, most notably the north trending and transpressional Belfort Fault. The boundary of the Dannemarie Basin with the Vosges Mountains is part of a restraining bend, which may account for the uplift of the southernmost part of the Vosges Mountains.
Starting Page	669
Ending Page	679
Page Count	11
File Format	PDF
ISSN	14373254
Journal	International Journal of Earth Sciences
Volume Number	94
Issue Number	4
e-ISSN	14373262
Language	English
Publisher	Springer-Verlag
Publisher Date	2005-04-09
Publisher Place	Berlin, Heidelberg
Access Restriction	One Nation One Subscription (ONOS)
Subject Keyword	Rhine Graben Dannemarie Basin Vosges Mountains Seismic reflection
Content Type	Text
Resource Type	Article
Subject	Earth and Planetary Sciences

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Tertiary tectonics of the Dannemarie Basin, upper Rhine graben, and regional implications