汶川中强余震震源深度的确定及其意义
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摘要
首次尝试用滑动时窗相关法识别sPn震相,并通过sPn与Pn震相之间的到时差约束区域地震事件的震源深度.利用陕西、青海、甘肃、云南和四川等区域地震台网记录,给出了汶川MS8.0级地震后,17个中强(MS≥5.0)余震的震源深度.研究结果显示,震源深度主要分布在8~20km深,且以32.5°N为界,由南到北,平均分布在两个不同的深度,分别为11和17km,表明这些余震的震源位于中上地壳.结合其他研究结果,我们认为龙门山断裂可能没有穿透整个地壳,且平武-青川断裂可能不是龙门山断裂的北向延伸.
引文
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