Volume 34 Issue 10
Oct.  2009
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ZHANG Xi, CUI Duxin, ZHANG Sixin, WANG Shuangxu. Coseismic Response and Influence of the Wenchuan Ms8.0 Earthquake Revealed by Crustal Deformation Observation[J]. Geomatics and Information Science of Wuhan University, 2009, 34(10): 1204-1209.
Citation: ZHANG Xi, CUI Duxin, ZHANG Sixin, WANG Shuangxu. Coseismic Response and Influence of the Wenchuan Ms8.0 Earthquake Revealed by Crustal Deformation Observation[J]. Geomatics and Information Science of Wuhan University, 2009, 34(10): 1204-1209.
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Coseismic Response and Influence of the Wenchuan Ms8.0 Earthquake Revealed by Crustal Deformation Observation

  • 1Institute of Earthquake Prediction of CEA,63 Fuxing Road,Beijing 100036,China;2The Second Monitoring and Application Center of CEA,316 Xiying Road,Xi'an 710054,China

Funds: 中国地震局地震预测研究所基本科研业务专项基金资助项目(青藏块体东北部强震孕育-发生动态过程研究)；国家自然科学基金资助项目(40674010)
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  • Received Date: August 15, 2009
  • Revised Date: August 15, 2009
  • Published Date: October 04, 2009
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  • Using crustal deformation observation data with diverse space-time scale,including GPS,long-leveling cross-fault,short-leveling and short-baseline cross-fault,the coseismic response of the Wenchuan Ms8.0 earthquake on 12 May 2008 and its influence on neighborhood are researched.The analysis shows that,the earthquake region displayed remarkable coseismic deformation of thrust and dextral slip,this great earthquake obviously effected the region from eastern segment of boundary between Gansu and Sichuan province to boundary where Gansu,Sichuan and Shaanxi meet,and the southern segment of Xianshuihe fault and the Y-character region where it meet Longmenshan fault and Anninghe fault,mainly reflecting possible enhanced action for strain accumulation,to some degree.
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