Seismicity wedge beneath the Upper Rhine Graben due to backwards Alpine push?-Reference-Cited by-同舟云学术

Seismicity wedge beneath the Upper Rhine Graben due to backwards Alpine push?

Published:2006-12 Issue:1-4 Volume:428 Page:49-64
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Edel Jean-Bernard,Whitechurch Hubert,Diraison Marc

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference44 articles.

1. Present day stress field and seismotectonic block movements along major fault zones in central Europe;Ahorner;Tectonophysics,1975

2. Die Mächtigkeit des Quartärs im Oberrheingraben;Bartz,1972

3. The Jura Mountains — an active foreland fold-and thrust belt?;Becker;Tectonophysics,2000

4. Anatomy and kinematics of oblique continental rifting revealed: a three-dimensional case study of the southeast Upper Rhine Graben (Germany);Behrmann;Am. Assoc. Pet. Geol. Bull.,2003

5. Seismicity pattern and style of seismic faulting at the eastern border fault of the southern Rhine Graben;Bonjer;Tectonophysics,1997

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