Regional stress field in the SE margin of the Tibetan Plateau revealed by the focal mechanisms of small and moderate earthquakes
Author:
Funder
National Natural Science Foundation of China
China Earthquake Administration
Publisher
Elsevier BV
Reference54 articles.
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4. Two crustal low-velocity channels beneath SE Tibet revealed by joint inversion of Rayleigh wave dispersion and receiver functions;Bao;Earth Planet. Sci. Lett.,2015
5. The mechanics of oblique slip faulting;Bott;Geol. Mag.,1959
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