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兴海6.6级地震前后地震波的变化
引用本文:都昌庭,徐兰芬,等. 兴海6.6级地震前后地震波的变化[J]. 高原地震, 2001, 13(1): 38-44
作者姓名:都昌庭  徐兰芬  
作者单位:青海省地震局,青海西宁810001
摘    要:2000年9月12日在青海省海南州兴海县西南发生了6.6级地震。震后发现,青海省6个专业台站的地震波速比在震前出现了下降-低值-发震的过程。波速比空间分布在兴海地震前形成了一个椭圆形的异常分布区,异常波速比的地震占总地震的73%。另外,在武台的尾波持续时间在兴海地震前显示出了较为完整的异常过程。

关 键 词:兴海地震 波速比 尾波持续时间 震源机制解

VARIATION OF SEISMIC WAVE BEFORE AND AFTER XINGHAI EARTHQUAKE WITH Ms 6.6
WTHZ]DU Chang-ting,XU Lan-fen,ZHAO Yong-hai [WTBX]. VARIATION OF SEISMIC WAVE BEFORE AND AFTER XINGHAI EARTHQUAKE WITH Ms 6.6[J]. Plateau Earthquake Research, 2001, 13(1): 38-44
Authors:WTHZ]DU Chang-ting  XU Lan-fen  ZHAO Yong-hai [WTBX]
Affiliation:WT5HZ]DU Chang-ting,XU Lan-fen,ZHAO Yong-hai [WT5BX]
Abstract:WT5BZ]There occurred an earthquake with M s6.6 in Xinghai county in Qinghai province on Sept. 12,2000.The authors have found that V P/V S was in a drop-low-occur process in six professional stations before the earthquake.Spatial distribution of V P/V S formed an ellipse area,and the earthquakes of anomaly V P/V S were 73% of the total.The coda wave duration of Dawu was a complete anomaly process before the event.
Keywords:Xinghai earthquake  V P/V S  Coda wave duration
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