The St. Gallen Fault Zone: a long-lived, multiphase structure in the North Alpine Foreland Basin revealed by 3D seismic data-Reference-Cited by-同舟云学术

The St. Gallen Fault Zone: a long-lived, multiphase structure in the North Alpine Foreland Basin revealed by 3D seismic data

Published:2016-02-08 Issue:1 Volume:109 Page:83-102
ISSN:1661-8726
Container-title:Swiss Journal of Geosciences
language:en
Short-container-title:Swiss J Geosci

Author:

Heuberger Stefan,Roth Philippe,Zingg Olivier,Naef Henry,Meier Beat P.

Publisher

Springer Science and Business Media LLC

Subject

Geology

Link

http://link.springer.com/content/pdf/10.1007/s00015-016-0208-5.pdf

Reference73 articles.

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2. Allenbach, R. P., & Wetzel, A. (2006). Spatial patterns of Mesozoic facies relationships and the age of the Rhenish Lineament: A compilation. International Journal of Earth Sciences, 95, 803–813.

3. Bachmann, G. H., Dohr, G., & Müller, M. (1982). Exploration in a classic thrust belt and its foreland: Bavarian Alps, Germany. American Association of Petroleum Geologists Bulletin, 66, 2529–2542.

4. Berge, T. B., & Veal, S. L. (2005). Structure of the Alpine foreland. Tectonics, 24, TC5011.

5. Birkhäuser, P., Roth, P., Meier, B., & Naef, H. (2001). 3D-Seismik: Räumliche Erkundung der mesozoischen Sedimentschichten im Zürcher Weinland. Nagra Technischer Bericht (NTB 00-03). Wettingen: Nagra.

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