supported by National Basic Research Program of China (Grant No. 2004CB418406);National Key Technology R & D Program of China (Grant No. 2008BAC35B05);the "Basic Science Research Plan" of the Institute of Earthquake Science, China Earthquake Administration (Grant No. 0207690203)
There are several major active fault zones in the western Sichuan and its vicinity. Slip rates and seismicity vary on different fault zones. For example, slip rates on the Xianshuihe fault zone are higher than 10 mm/a...
supported by the Key Project of Chinese National Programs for Fundamental Research and Development (973 program,No.2008CB425704 and 2004CB418406)
The characteristics of spatio-temporal seismicity evolution before the Wenchuan earthquake are studied. The results mainly involve in the trend abnormal features and its relation to the Wenchuan earthquake. The wester...
National Basic Research Program of China (Grant No. 2004CB418406);National Natural Science Foundation of China (Grant Nos. 40774049 and 40474038);Computer Network Information Center, Chinese Academy of Sciences (Grant No. INF105-SCE-02-12)
The 2008 Wenchuan earthquake occurred in an active earthquake zone, i.e., Longmenshan tectonic zone. Seismic waves triggered by this earthquake can be used to explore the characteristics of the fault rupture process a...