Stress field variations in the Swiss Alps and the northern Alpine foreland derived from inversion of fault plane solutions-Reference-Cited by-同舟云学术

Stress field variations in the Swiss Alps and the northern Alpine foreland derived from inversion of fault plane solutions

Published:2004-01 Issue:B1 Volume:109 Page:
ISSN:0148-0227
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res.

Author:

Kastrup Ulrike¹,Zoback Mary Lou²,Deichmann Nicholas¹,Evans Keith F.¹,Giardini Domenico¹,Michael Andrew J.²

Affiliation:

1. Institute of Geophysics, ETH-Hönggerberg; Zürich Switzerland

2. Western Region Earthquake Hazard Team, U.S. Geological Survey; Menlo Park California USA

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference101 articles.

1. Seismotektonische Traverse von der Nordsee bis zum Apennin;Ahorner;Geol. Rundsch.,1972

2. Stresses in the lithosphere caused by crustal thickness inhomogeneities;Artyushkov;J. Geophys. Res.,1973

3. Erosion as a driving mechanism of intracontinental mountain growth;Avouac;J. Geophys. Res.,1996

4. Baer , M. 1990 The seismic station network of the Swiss Seismological Service Workshop on MEDNET, the Broad-Band Seismic Network for the Mediterranean Rome

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