Upper Rhine Graben: Role of preexisting structures during rift evolution-Reference-Cited by-同舟云学术

Upper Rhine Graben: Role of preexisting structures during rift evolution

Published:2002-01 Issue:1 Volume:21 Page:6-1-6-17
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Schumacher Markus E.¹

Affiliation:

1. Geological-Palaeontological Institute; University of Basel; Basel Switzerland

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference106 articles.

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

2. General Pattern of Seismotectonic Dislocation and the Earthquake - Generating Stress Field in Central Europe Between the Alps and the North Sea

3. The evolution of the South Hunsrück and Taunus Borderzone;Anderle;Tectonophysics,1987

4. Late Paleozoic strike-slip faulting in southern Europe and northern Africa: Results of a right-lateral shear zone between the Appalachians and the Urals;Arthaud;Geol. Soc. Am. Bull.,1977

5. Kalium-Argon-Altersbestimmungen an tertiären Vulkaniten des Oberrheingraben-Gebietes, II, Die Alterstraverse vom Hegau nach Lothringen;Baranyi;Oberrheinische Geol. Abh.,1976

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