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汶川8.0级地震后龙门山断裂地震波速异常的讨论
引用本文:田洁,朱振家,朱宗德,姚玉霞,王燕.汶川8.0级地震后龙门山断裂地震波速异常的讨论[J].高原地震,2009,21(4):21-24.
作者姓名:田洁  朱振家  朱宗德  姚玉霞  王燕
作者单位:1. 甘肃省天水中心地震台,甘肃,天水741020
2. 甘肃省高台基准地震台,甘肃,高台734300
摘    要:通过对2008年四川省汶川8.0级特大地震时天水台记录到的地震波形进行分析,结果发现:龙门山断裂带在汶川特大地震后,天水台记录到的余震出现了3—4秒的地震波速异常,认为与此次特大地震后龙门山断裂带的破碎有关。

关 键 词:汶川8.0级地震  龙门山断裂带  波速异常

DISCUSSION ON SEISMIC VELOCITY ANOMALIES OF LONGMENSHAN FAULT ZONE AFTER WENCHUAN 8.0 EARTHQUAKE
TIAN Jie,ZHU Zhenjia,ZHU Zongde,YAO Yuxia,WANG Yan.DISCUSSION ON SEISMIC VELOCITY ANOMALIES OF LONGMENSHAN FAULT ZONE AFTER WENCHUAN 8.0 EARTHQUAKE[J].Plateau Earthquake Research,2009,21(4):21-24.
Authors:TIAN Jie  ZHU Zhenjia  ZHU Zongde  YAO Yuxia  WANG Yan
Institution:1. Tianshui Seismic Station, Gansu Province, Tianshui 741020, China; 2. Gaotai Seismic Station, Gansu Province, Gaotai 734300, China)
Abstract:The seismic waves of Wenchuan 8.0 earthquake in 2008 recorded by Tianshui station were analyzed, and the results show that 7 -8 seconds seismic velocity anomalies appeared in Longmenshan fault zone after the event, and this may be related with the fragmentation of the Longmenshan fault zone.
Keywords:Wenchuan 8  0 earthquake  Longmenshan fault zone  Velocity anomaly
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