The shear-wave splitting study of Sichuan Zipingpu reservoir region

被引:9
|
作者
Zhang Yong-Jiu [1 ]
Gao Yuan [2 ]
Shi Yu-Tao [2 ]
Tai Ling-Xue [2 ]
机构
[1] Earthquake Adm Sichuan Prov, Chengdu 610041, Peoples R China
[2] China Earthquake Adm, Inst Earthquake Sci, Beijing 100036, Peoples R China
来源
CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION | 2010年 / 53卷 / 09期
关键词
Sichuan Zipingpu reservoir; Shear-wave splitting; Polarization of fast shear-wave; Principal compressive stress; Active faults; STRESS-FORECAST EARTHQUAKE; TEMPORAL VARIATIONS; SEISMIC ANISOTROPY; TIME-DELAYS; FIELD; POLARIZATIONS; PROPAGATION; CALIFORNIA; FEATURES; CHINA;
D O I
10.3969/j.issn.0001-5733.2010.09.009
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Using seismic data recorded by Zipingpu reservoir Digital Seismic Network from Aug. 17, 2004 to May 11, 2008, the dominant polarization directions of fast shear-waves are obtained at 8 digital seismic stations in this region by SAM technique. The results show that dominant directions of polarizations of fast shear-waves are mainly in nearly NE or NW direction in Zipingpu reservoir region. The dominant polarization directions of fast shear-waves are consistent with the strikes of active faults, or regional principal compressive stress. The direction variety of polarization of fast shear-wave are related with the enhancement of regional stress and micro-cracking of Longmenshan fault before Wenchuan earthquake, and there are correlation between delay time of slow shear-wave and water level of Zipingpu reservoir.
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页码:2091 / 2101
页数:11
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