Architecture and Kinematics of the Constance-Frick Trough (Northern Switzerland): Implications for the Formation of Post-Variscan Basins in the Foreland of the Alps and Scenarios of Their Neogene Reactivation-Reference-Cited by-同舟云学术

Architecture and Kinematics of the Constance-Frick Trough (Northern Switzerland): Implications for the Formation of Post-Variscan Basins in the Foreland of the Alps and Scenarios of Their Neogene Reactivation

Published:2018-07 Issue:7 Volume:37 Page:2197-2220
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Madritsch Herfried¹^ORCID,Naef Henry²,Meier Beat³^ORCID,Franzke Hans Joachim⁴,Schreurs Guido⁵^ORCID

Affiliation:

1. Nagra (National Cooperative for the Disposal of Radioactive Waste); Wettingen Switzerland

2. geosfer AG; St. Gallen Switzerland

3. Formerly at Proseis AG; Zurich Switzerland

4. Formerly at TU Clausthal; Clausthal-Zellerfeld Germany

5. Institute of Geological Sciences; University of Bern; Bern Switzerland

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1029/2017TC004945/fullpdf

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3. Late Paleozoic strike-slip faulting in southern Europe and northern Africa: Result of a right-lateral shear zone between the Appalachians and the Urals;Arthaud;Bulletin Geological Society of America,1977

4. Successive post-Variscan stress fields in the French Massif Central and its borders (Western European plate): Comparison with geodynamic data;Blés;Tectonophysics,1989

5. Faziesanalyse im Rotliegenden des Nordschweizer Permokarbon-Trogs (Hochrhein-Region zwischen Basel und Laufenburg);Blüm;Eclogae Geologicae Helvetiae,1989

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