supported by the National Natural Science Foundation of China (Grant Nos. 41174042, 41040034);the China National Special Fund for Earthquake Scientific Research in Public Interest (Grant No. 201008001)
On April 20, 2013, the Lushan M^7.0 earthquake struck at the southern part of the Longmenshan fault in the eastern Tibetan Plateau, China. The shear-wave splitting in the crust indicates a connection between the direc...
supported by basic research project of Institute of Earthquake Science of China Earthquake Science(No.2009-21);National Natural Science Foundation of China(No.41040034)
The 2010 Yushu MsT.1 earthquake occurred in Ganzi-Yushu fault, which is the south boundary of Bayan Har block. In this study, by using double difference algorithm, the locations of mainshock (33.13°N, 96.59°E, foca...
supported by International Science and Technology Cooperation Program of China(2010DFB20190);National Natural Science Foundation of China(41040034 and 41174042);the support by basic research project of Institute of Earthquake Science,China Earthquake Administration(2009IES0211)
When propagating through anisotropic rocks in the crust, shear-waves split into faster and slower components with almost orthogonal polarizations. For nearly vertical propagation the polarization of fast shear- wave ...