Crustal seismic anisotropy in southeastern Capital area, ChinaOA
Crustal seismic anisotropy in southeastern Capital area, China
Shear-wave splitting parameters of 24 stations in southeastern Capital area of North China (38.5°N-39.85°N,115.5°E～118.5°E) are obtained with systematic analysis method of shear-wave splitting (SAM) based on the data recorded…查看全部>>
Shear-wave splitting parameters of 24 stations in southeastern Capital area of North China (38.5°N-39.85°N,115.5°E～118.5°E) are obtained with systematic analysis method of shear-wave splitting (SAM) based on the data recorded by Capital Area Seismograph Network (CASN) from 2002 to 2005. 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 …查看全部>>
WU Jing;GAO Yuan;CHEN Yun-tai
Institute of Geophysics, China Earthquake Administration, Beijing 100081, ChinaInstitute of Earthquake Science, China Earthquake Administration, Beijing 100036,ChinaInstitute of Geophysics, China Earthquake Administration, Beijing 100081, China
天文与地球科学
southeastern Capital areaseismic anisotropyshear-wave splittingcruststress
southeastern Capital areaseismic anisotropyshear-wave splittingcruststress
《地震学报（英文版）》 2008 (1)
首都圈地区地震各向异性特征及其尺度
1-10,10
Seismic Professional Science Fund (200708008), Basic and Special Research Foundation, Institute of Earthquake Science, China Earthquake Administration (2007-13) and National Natural Science Foundation of China (40674021 ).
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