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《Chinese Journal of Geophysics》 2005-03
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Relocation of small earthquakes in western Sichuan, China and its implications for active tectonics

ZHU Ai-Lan 1, XU Xi-Wei 1, ZHOU Yong-Sheng 1, YIN Jing-Yuan 2, GAN Wei-Jun 1, CHEN Gui-Hua 1 1 Institute of Geology, China Earthquake Administration, Beijing 100029, China 2 Seismological Bureau of Shanghai, Shanghai 200062, China  
We relocated 13367 small earthquakes that occurred in western Sichuan from 1992 to 2002 using the double-difference (DD) earthquake location algorithm to improve relative location accuracy. The relocated seismicity forms highly organized structures that correlate well with the surface faulting, showing the flower-shaped structure across the simple strike-slip fault, and the organized but dispersed structure across the pull-apart basin and thrust fault. Beneath the thrust fault, there exists an aseismic layer. The seismicity also shows segmentation characteristics along the active faults. Other new findings, which were previously obscured by routine location errors, are also revealed by the relocated seismicity. Some blind faults are revealed by lineages of seismicity that are suggestive of faulting structures. Large seismic gaps appear with dimensions of tens of kilometers on the Xianshuihe-Anninghe-Zemuhe fault zone, which have been aseismic over a time interval of 10-year, suggesting that these segments are either locked or retarded and are storing strain energy for release in future large earthquakes. An aseismic layer with the thickness of 5km exists in most places beneath western Sichuan plateau at depths of 15 to 20km. Basing on the results from high-temperature and high-pressure experiments, we calculated the crustal strength envelopes for the western Sichuan. The result shows that the granite in upper crust at depths of 14 to 19km appears to be ductile, which is in good agreement with the thickness and depth range of the aseismic layer, suggesting that the aseismic layer may be the result of the ductile deformation of the granite in the upper crust.
【Fund】: 国家重点基础发展规划项目 (2 0 0 4CB41840 1);; 国家科技基础条件平台重点项目 (2 0 0 3DIA6N0 0 5 );; 国家自然科学基金 (4 0 4740 67);; 科技部重大基础研究前期研究专项 (2 0 0 3CCB0 0 60 0 )联合资助
【CateGory Index】: P315.2
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