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四川紫坪铺水库库区地震剪切波分裂研究
引用本文:张永久, 高 原, 石玉涛, 太龄雪. 四川紫坪铺水库库区地震剪切波分裂研究[J]. 地球物理学报, 2010, 53(9): 2091-2101, doi: 10.3969/j.issn.0001-5733.2010.09.009
作者姓名:张永久  高原  石玉涛  太龄雪
作者单位:四川省地震局,成都,610041;中国地震局地震预测研究所,北京,100036
基金项目:中国地震局地震预测研究所基本科研专项,国家科技支撑计划水库地震监测与预测技术研究 
摘    要:本研究利用四川紫坪铺水库数字地震台网2004年8月17日~2008年5月11日的地震观测波形资料,使用剪切波分裂SAM系统分析方法,获得了四川紫坪铺水库库区8个数字地震台站的快剪切波偏振结果.结果表明,紫坪铺库区台站的快剪切波偏振优势方向主要为NE或NW方向;台站的快剪切波偏振优势方向与区域主压应力方向或活动断裂走向一致;快剪切波偏振方向变化可能与汶川大地震前区域应力场的增加和龙门山断裂带微破裂增加有关,慢剪切波时间延迟的变化与四川紫坪铺水库水位升降变化相关.

关 键 词:四川紫坪铺水库  剪切波分裂  快剪切波偏振  主压应力  活动断裂
收稿时间:2009-11-25
修稿时间:2010-06-01

The shear-wave splitting study of Sichuan Zipingpu reservoir region
ZHANG Yong-Jiu, GAO Yuan, SHI Yu-Tao, TAI Ling-Xue. The shear-wave splitting study of Sichuan Zipingpu reservoir region[J]. Chinese Journal of Geophysics (in Chinese), 2010, 53(9): 2091-2101, doi: 10.3969/j.issn.0001-5733.2010.09.009
Authors:ZHANG Yong-Jiu  GAO Yuan  SHI Yu-Tao  TAI Ling-Xue
Affiliation:1. Earthquake Administration of Sichuan Province, Chengdu 610041, China; 2. Institute of Earthquake Science, China Earthquake Administration, Beijing 100036, China
Abstract: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.
Keywords:Sichuan Zipingpu reservoir  Shear-wave splitting  Polarization of fast shear-wave  Principal compressive stress  Active faults
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