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《Seismology and Geology》 2008-02
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RUPTURE OF THE M_S 8.0 WENCHUAN EARTHQUAKE

HE Hong-lin1)SUN Zhao-min2)WANG Shi-yuan3)WANG Ji-qiang2)DONG Shao-peng1)1)Institute of Geology,China Earthquake Administration,Beijing 100029,China2)Earthquake Administration of Shandong Province,Jinan 250014,China3)Earthquake Administration of Sichuan Province,Chengdu 100717,China  
On the 12th of May,2008,a devastating MS 8.0 earthquake struck Wenchuan County,Sichuan Province.The earthquake rupture extends about 200km,and the maximum co-seismic strike-slip displacement and vertical displacement are(4.8±0.2)m and(5±0.2)m,respectively.Only one fault plane(N32°E/NW∠76°)has been found on the southern section of the rupture.The high dip of the fault plane and high angle stria on the fault plane show that the fault is dominated by reverse motion,with a small amount of right-lateral strike-slip component in this segment.
【CateGory Index】: P315
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