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2010青海玉树地震同震重力和形变效应模拟

SIMULATION OF COSEISMIC GRACITY CHANGE AND DEFORMATION FOR 2010 QINGHAI YUSHU EARTHQUAKE

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【作者】 赵云峰祝意青梁伟锋徐云马郭树松刘芳刘练

【Author】 Zhao Yunfeng;Zhu Yiqing;Liang Weifeng;Xu Yunma;Guo Shusong;Liu Fang;Liu Lian;Second Crust Monitoring and Application Center,CEA;State Key Laboratory of Geodesy and Earth’s Dynamics,IGGCAS;

【机构】 中国地震局第二监测中心中国科学院测量与地球物理研究所大地测量与地球动力学国家重点实验室

【摘要】 分别以远场地震波形和In SAR数据反演得到的玉树地震断层滑动模型为基础,使用PSGRN/PSCMP程序计算了黏弹分层介质中玉树Ms7.1地震产生的同震重力和形变场。结果表明:1)由远场地震波形数据得到的断层滑动模型计算的同震重力和位移变化与震后野外调查得到的形变场更符合;2)可以监测到的同震重力变化仅分布在断层附近,同震水平位移影响范围明显大于同震重力变化影响范围;3)震前两年和震后一个月,在玉树绝对重力台观测到的绝对重力变化与由两个断层模型计算的结果有明显差别,表明观测到的绝对重力变化蕴含着地震孕育过程、同震重力变化和震后恢复过程产生的重力变化。

【Abstract】 Coseismic gravity change and deformation in layer viscoelastic medium caused by Yushu Ms7. 1were calculated using PSGRN / PSCMP based on different fault slip models. The results show that: 1) Coseismic gravity change and displacement calculated for teleseimic waveform based on the fault slip model are more consistent with results from field survey; 2) Coseismic gravity change only locates near by faults,and the range influenced by coseismic horizon displacements are obvious widely than that by coseimic gravity change; 3) The obsolute gravity change during the period of two years before the earthquake and one month after the earthquake is obvious different from the result calculated,which indicats that observed obsolute gravity change implies earthquake preparation and coseismic change and post-seismic change.

【基金】 中国地震局地震行业科研重点专项(201308004;201308009);国家自然科学基金项目(41274083)
  • 【文献出处】 大地测量与地球动力学 ,Journal of Geodesy and Geodynamics , 编辑部邮箱 ,2014年06期
  • 【分类号】P315
  • 【下载频次】80
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