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《Acta Seismologica Sinica》 2008-01
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Crustal seismic anisotropy in southeastern Capital area, China

Wu Jing1,2) Gao Yuan1,2), Chen Yuntai1)1) Institute of Geophysics, China Earthquake Administration, Beijing 100081, China 2) Institute of Earthquake Science, China Earthquake Administration, Beijing 100036, China  
Shear-wave splitting parameters of 24 stations in southeastern Capital area (38.5°N--39.85°N, 115.5°E--118.5°E) are obtained with SAM(systematic analysis method of shear-wave splitting) based on the data from 2002 to 2005 of Capital Area Seismic Network (CASN). The results show that the average polarization of fast shear-wave in southeastern Capital area is consistent with regional maximum horizontal principal compressive stress in the area, and is also consistent with maximum horizontal principal compressive strain from GPS in Northern China. The average shear-wave splitting in southeastern Capital area (in basin) is different from that in northwestern Capital area where uplifts and basin exist, illustrating that different tectonics can show different shear-wave splitting results. Research also shows that the distribution of faults around stations can obviously affect the shear-wave splitting results, and complicated distribution of faults can result in much more scattering of shear-wave splitting. It is also shown that in the north and south of the interested area (southeastern Capital area), the polarizations of fast shear-wave are not very consistent, which may be related to differences in tectonic and stress for the two areas.
【Fund】: 地震行业科研专项(200708008);; 中国地震局地震预测研究所基本科研专项(2007-13);; 国家自然科学基金(40674021);; 中国地震局地球物理研究所论著08AC2005
【CateGory Index】: P315.2
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