Characteristics of Focal Mechanisms and the Stress Field in the Southeastern Margin of the Tibetan Plateau
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/content/pdf/10.1007/s00024-016-1350-8.pdf
Reference82 articles.
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2. Angelier, J. (1984). Tectonic analysis of fault slip data sets. Journal of Geophysical Research, 89(B7), 5835–5848.
3. Angelier, J. (2002). Inversion of earthquake focal mechanisms to obtain theseismotectonic stress IV—a newmethod free of choice among nodal lines. Geophysical Journal International, 150, 588–609.
4. Arnold, R., & Townend, J. (2007). A Bayesian approach to estimating tectonic stress from seismological data. Geophysical Journal International, 170, 1336–1356.
5. Bai, D., Unsworth, M. J., Meju, M. A., Ma, X., Teng, J., Kong, X., et al. (2010). Crustal deformation of the eastern Tibetan plateau revealed by magnetotelluric imaging. Nature Geoscience, 3(5), 358–362.
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