苏门答腊地震对柴达木地方震的触发作用
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摘要
2004年12月26日印度尼西亚苏门答腊西北海域发生40年来最强烈的地震,造成巨大伤亡和财产损失。大地震在4000km外的柴达木盆地西部地区狮子沟地震台阵网上有长达1000多秒的明显记录,也触发柴西地区地方震的发震频率在大地震之后一天内提高了10倍。从大地震触发的地方震活动分布来看,触发地震的发震断裂是英雄岭南侧花土沟断裂和红柳泉断裂。
A magnitude 9.0 earthquake,which was the strongest earthquake in the past four decades,occurred just off the northwest coast of Sumatra,Indonesia,on December 26,2004.It caused serious damage and casualties.This large earthquake left as long as more than 1000 seconds of records at the Shizigou seismograph station in the western part of the Qaidam basin a distance of 4000 km from the epicenter.It has also triggered the local seismic activity in the western Qaidam basin.The frequency of the local earthquakes in the day after the occurrence of the large earthquake was 10 times as high as it had been.From the distribution of the local seismic activity triggered by the large earthquake,the causative faults triggering the local earthquakes in the western Qaidam basin are the Huatugou fault and Hongliuquan fault on the southern side of the Yingxiong Range.
引文
[1]崔秋文,李建一,董军,等.印度洋大地震与海啸灾害综述[J].地震科技情报快讯,2004,(23~24):1~20.
    [2]黄汉纯,黄庆华,马寅生.柴达木盆地地质与油气预测[M].北京:地质出版社,1996.
    [3]黄庆华,黄汉纯,马寅生.柴达木盆地构造、三维应力与聚油模式[J].地球学报,l996,17(增刊):28~35.

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