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《Chinese Journal of Geophysics》 2009-02
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The rheological structures of crust and mechanics of high-angle reverse fault slip for Wenchuan M_S8.0 earthquake

ZHOU Yong-Sheng, HE Chang-RongState Key Laboratory of Earthquake Dynamics , Institute of Geology ,China Earthquake Administration,Beijing 100029,China  
The rheological structures of tectonic units related to Wenchuan earthquake is estimated based on geological and geophysical field data, as well as experimental P-velocity and creep data. There are two to three plastic layers in western Sichuan plateau and Longmenshan tectonic zone, but it is almost no any plastic layer in Sichuan basin. It plays a significant role for the complicated rheological structures to accumulate the tectonic stress and forming Wenchuan earthquake. The high temperature and high pressure experiments show that the strength of rocks is very high in earthquake source (mainly granitic rocks, such as adamellite), which could sustain great different stress and accumulate huge energy. This is one of major causes for high-angle reverse fault slip and high intensity of Wenchuan earthquake. However, high fluid pressure is a necessary condition for sliding of high-angle reverse fault and triggering Wenchuan earthquake, and Longmenshan tectonic zone might have provided with the requirement.
【Fund】: 973项目“活动地块边界带的动力过程与强震预测”(2004CB418405-02);; 中国地震局地质研究所基本科研业务费(DF-IGCEA-0607-1-29)资助
【CateGory Index】: P315
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