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《Chinese Journal of Geophysics》 2012-01
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Tectonic stress analysis based on the crustal seismic anisotropy in the northeastern margin of Tibetan plateau

ZHANG Hui1,3,GAO Yuan2*,SHI Yu-Tao2,LIU Xiao-Feng1,WANG Yi-Xi1 1 Lanzhou Institute of Seismology,China Earthquake Administration,Lanzhou 730000,China 2 Earthquake Science Institute,China Earthquake Administration,Beijing 100036,China 3 Lanzhou National Observatory of Geophysics,Lanzhou 730000,China  
The northeastern margin of Tibetan plateau is controlled jointly by several tectonic blocks and shows complicated geophysical and geological characters.In the paper,the data from Gansu Seismological Network(2001—2008) are analyzed with the seismic anisotropy analysis method in crust(SAM).1005 shear-wave splitting parameters from 18 stations are obtained.The results show that the crustal seismic anisotropy in the northeastern margin of Tibetan plateau varies in space.The delay times of slow shear-waves show the variation characteristics of the strength of crustal seismic anisotropy and the average polarizations of fast shear-waves reflect the spacial variation characteristics of regional tectonic stress.It is shown that the interaction of Tibetan plateau block and Alxa block controls the region of Qilianshan-Hexi corridor active structures,where the direction of tectonic stress is the same as in Tibetan plateau block.In the southeast of Gansu active structure region,it is regarded that active faults are influential on the stress field,which shows local tectonic stress characteristics.
【Fund】: 国家自然科学基金(41040034);; 地震行业科研专项(201008001);; 南北地震带北段大震危险性强化跟踪项目资助
【CateGory Index】: P315.2
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