首页|2024年1月23日乌什MS7.1地震序列重定位研究

2024年1月23日乌什MS7.1地震序列重定位研究

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为深入研究乌什MS7.1地震,采用双差地震定位法对地震序列进行重定位,定位结果显示:①重定位后主震空间位置变化不大,和重定位前的位置相距2 km,深度为25.6 km,比重定位前深度更深.②重定位后,地震序列沿迈丹断裂分布的收敛特征更加明显,同时存在余震向南移动的趋势,与地震烈度图和灾情分布特征一致.③迈丹断裂在受到山前挤压作用时,在主震震中附近受阻,形成明显的地震稀疏带.迈丹断裂乌什段发震构造比阿合奇段发震构造深,活动性比较弱,因此在主震震中SW向余震多而浅,NE向余震少而深.
WUSHI MS7.1 EARTHQUAKE SEQUENCE RELOCATION RESEARCH ON JANUARY 23,2024
In order to further study Wushi MS7.1 earthquake,double-difference seismic position method was used to relocate the seismic sequence,and the positioning results showed that:① after relocation,the spatial position of the mainshock did not change much.It was 2 km away from the position before relocation,and the depth was 25.6 km,which was deeper than that before reloca-tion.② After reposition,earthquake sequence had a tendency to develop southward along the Maid-an fault,which was basically consistent with the distribution characteristics of disasters.③ When the Maidan fault was extruded by the piedmont extrusion,it was stopped near the epicenter of the main-shock,and the seismic structure of the Wushi section of the Maidan fault was deeper than that of the Aheqi section,and the activity was relatively weak,so there were more and shallow aftershocks in the SW direction and fewer and deeper aftershocks in the NE direction in the mainshock epicenter.

Wushi MS7.1 earthquakeDouble difference seismic positioning methodEarthquake sequence

祖力卡尔·艾则孜、南芳芳、徐衍刚

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新疆维吾尔自治区地震局阿克苏地震监测中心站,新疆阿克苏 843000

乌什MS7.1地震 双差地震定位法 地震序列

2024

内陆地震
新疆维吾尔自治区地震局

内陆地震

影响因子:0.495
ISSN:1001-8956
年,卷(期):2024.38(2)