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新疆新源、和静交界6.6级地震前后波速比异常特征研究
STUDY ON CHARACTERISTICS OF VELOCITY RATIO ANOMALY BEFORE AND AFTER XINYUAN、HEJING EARTHQUAKE WITH M_S6.6
【摘要】 利用天山中段数字化地震观测报告,采用多台和达法,计算了2012年6月30日新疆新源、和静交界6.6级地震前后波速比异常变化情况。结果表明:在该次地震前,波速比在空间上形成一个的低值异常区,其值在1.6左右,地震发生在该异常区的东北缘;地震发生后,震区周围波速比在1.8左右,基本恢复正常。
【Abstract】 Using multi-station method,this paper calculated velocity ratio anomaly before and after Xinyuan,Hejing earthquake with MS6.6 according to digital seismic report in middle section of Tianshan.The result shows: a low value region about 1.6 formed before earthquake and earthquake occured in northeast section of this region;the velocity ratio in seismic area returned to normal about 1.8 after earthquake.
【关键词】 地震观测报告;
多台和达法;
6.6级地震;
波速比异常;
【Key words】 Seismic report; Multi-station method; Earthquake with MS6.6; Velocity ratio anomaly;
【Key words】 Seismic report; Multi-station method; Earthquake with MS6.6; Velocity ratio anomaly;
【基金】 新疆地震科学基金课题(201106)资助
- 【文献出处】 内陆地震 ,Inland Earthquake , 编辑部邮箱 ,2013年02期
- 【分类号】P315.31
- 【被引频次】4
- 【下载频次】23