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《Chinese Journal of Geophysics》 2012-01
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Numerical simulation of 5.12 Wenchuan M_S8.0 earthquake geodynamic background

LIAO Li,ZHANG Dong-Ning,YANG Jian-Si Institute of Geophysics,China Earthquake Administration,Beijing 100081,China  
The Wenchuan MS8.0 earthquake occurred on Longmenshan faults on May 12,2008.This paper is based on previous geology and geophysics research results,high resolution elevation data,and heat flow data.We have built a finite model to study the Longmenshan faults.By using GPS data,stress field and source rupture process as constraint condition,we have studied the geodynamic background of this strong earthquake to confirm whether or not the starting rupture position of the earthquake and the fault dislocation pattern were influenced by the elevation and rheological strength difference between the Sichuan basin and Tibetan plateau,and by the different frictions of Longmenshan faults and fault geometry.The result of our computing model shows that,when considering the deep material of Tibetan plateau flowing toward east,the above factors all actually influence the starting rupture position of the earthquake and the fault dislocation pattern.This paper uses the geodynamic finite element software to simulate the rupture process of Longmenshan faults during the Wenchuan earthquake.
【Fund】: 国家自然科学基金项目(40644021);; 公益性地震行业专项项目(201108002 200708009)资助
【CateGory Index】: P315
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