Influence of fault geometry and fault interaction on strain partitioning within western Sichuan and its adjacent region  

作　　者：WANG Hui LIU Jie SHEN XuHui LIU Mian LI QingSong SHI YaoLin ZHANG GuoMin 

机构地区：[1]Institute of Earthquake Science,China Earthquake Administration,Beijing 100036,China [2]Department of Geological Sciences,University of Missouri,Columbia,MO 65211,USA [3]China Earthquake Network Center,China Earthquake Administration,Beijing 100045,China [4]Lunar and Planetary Institute,Houston,TX 77058,USA [5]Laboratory of Computational Geodynamics,Graduate University of Chinese Academy of Sciences,Beijing 100049,China

出　　处：《Science China Earth Sciences》2010年第7期1056-1070,共15页中国科学（地球科学英文版）

基　　金：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)

摘　　要：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. Its seismicity is also intense. Slip rates on the Longmenshan fault zone are low. However, Wenchuan Ms8.0 earthquake occurred on this fault zone in 2008. Here we study the impact of fault geometry on strain partitioning in the western Sichuan region using a three-dimensional viscoe- lastoplastic model. We conclude that the slip partitioning on the Xianshuihe-Xiaojiang fault presents as segmented, and it is related to fault geometry and fault structure. Slip rate is high on fault segment with simple geometry and structure, and vice versa. Strain rate outside the fault is localized around the fault segment with complex geometry and fault structure. Strain partitioning on the central section of the Xianshuihe-Xiaojiang fault zone is influenced by the interaction between the Anninghe-Zemuhe fault and the Daliangshan fault zone. Striking of the Longmenshan fault zone is nearly orthogonal to the direction of eastward extrusion in the Tibetan Plateau. It leads to low slip rate on the fault zone.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. Its seismicity is also intense. Slip rates on the Longmenshan fault zone are low. However, Wenchuan Ms8.0 earthquake occurred on this fault zone in 2008. Here we study the impact of fault geometry on strain partitioning in the western Sichuan region using a three-dimensional viscoe- lastoplastic model. We conclude that the slip partitioning on the Xianshuihe-Xiaojiang fault presents as segmented, and it is related to fault geometry and fault structure. Slip rate is high on fault segment with simple geometry and structure, and vice versa. Strain rate outside the fault is localized around the fault segment with complex geometry and fault structure. Strain partitioning on the central section of the Xianshuihe-Xiaojiang fault zone is influenced by the interaction between the Anninghe-Zemuhe fault and the Daliangshan fault zone. Striking of the Longmenshan fault zone is nearly orthogonal to the direction of eastward extrusion in the Tibetan Plateau. It leads to low slip rate on the fault zone.

关 键 词：Xianshuihe-Xiaojiang FAULT ZONE LONGMENSHAN FAULT ZONE FAULT geometry strain partitioning 3D viscoelastoplastic model 

分 类 号：N[自然科学总论]