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2014年新疆于田MS7.3级地震序列重定位

DOI: 10.6038/cjg20150310, PP. 802-808

Keywords: 于田地震,余震序列,地震定位,阿尔金断裂,双差定位

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Abstract:

2014年新疆于田发生MS7.3地震,这一地区6年来连续发生2次强烈地震,震中相距不到110km.由于初始定位误差较大,于田地震的发震断层仍不清楚.本研究的主要目标是利用地震精定位方法对于田地震序列及其背景地震活动进行重新定位,确定于田地震的发震断层.本研究使用双差定位方法对于田地震序列进行重新定位.这一方法假设两个地震的震源距小于事件到台站的距离,两个事件到同一台站的走时差主要归因于其空间位置的偏移,因此可消除由于速度模型不准确引起的定位误差.重定位后得到了435个地震的位置参数.结果表明,2014年于田MS7.3级地震发生在阿尔金断裂带的西端,余震分布的优势方向为北东向,展布长度约33km,震源深度主要集中在4~12km,多数余震位于主震的西南侧.NS,EW和UD方向的定位误差分别为0.5km,1.1km和1.7km.于田地震余震序列总体衰减较慢.根据余震分布特征和震源机制解,认为此次地震的断层面为北东向的节面,阿尔金断裂的西南延伸分支断层是这次地震的主要发震构造.于田地震的发生与巴颜喀拉块体的东南向运动有关.

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