首页|2024年1月23日乌什MS7.1地震前新疆地电优势方位角变化特征分析

2024年1月23日乌什MS7.1地震前新疆地电优势方位角变化特征分析

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通过对2024年1月23日乌什MS7.1地震前新疆境内5个地电台站观测数据的回溯性分析,计算地震前各台站地电优势方位角,总结数据变化特征,发现地震前各台站地电优势方位角均出现了不同程度的异常变化,异常表现为分散、集中、偏转和跃变的特征.其中震中附近的乌什台、温泉台地电优势方位角异常在时间上具有准同步变化.地震前震中500 km范围内的乌什、温泉、和田台不仅存在不同方位间相关系数的准同步下降变化,而且极化方位也出现了相似的线性极化增强现象,且乌什、和田台优势方位角的异常变化均呈现出向主压应力集中现象,说明在乌什MS7.1地震前乌什、温泉、和田台观测到的地电数据变化,同此次地震具有一定机理上的联系.
CHARACTERISTICS ANALYSIS OF GEOELECTRIC DOMINANT AZIMUTH CHANGES IN XINJIANG BEFORE WUSHI MS7.1 EARTHQUAKE ON JANUARY 23,2024
Based on the retrospective analysis of the observation data of five geoelectric stations in Xinjiang before the Wushi MS7.1 earthquake on January 23,2024,the geoelectric dominant azimuth of each station before the earthquake is calculated,and the data variation characteristics are summa-rized.It is found that the geoelectric dominant azimuth of each station before the earthquake has dif-ferent degrees of abnormal changes,and the anomalies are characterized by dispersion,concentra-tion,deflection and jump.The geoelectric dominant azimuth anomalies of Wushi and Wenquan sta-tions near the epicenter have quasi-synchronous changes in time.Before the earthquake,the Wushi,Wenquan and Hetian stations within 500 km of the epicenter not only had quasi-synchronous decline in the correlation coefficient between different azimuths,but also had similar linear polarization en-hancement in the polarization azimuth,and the abnormal changes of the dominant azimuth of Wushi and Hetian stations showed the phenomenon of concentration to the principal compressive stress P,indicating that the changes of geoelectric data observed by Wushi,Wenquan and Hetian stations be-fore the Wushi MS7.1 earthquake had a certain mechanism connection with the earthquake.

Wushi MS7.1 earthquakeGeoelectric fieldDominant azimuthChange characteris-ticsFocal mechanism

刘海洋、饶文、徐衍刚、艾萨·伊斯马伊力

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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

新疆维吾尔自治区地震局,新疆乌鲁木齐 830011

乌什MS7.1地震 地电场 优势方位角 变化特性 震源机制

中国地震局监测、预报、科研三结合课题中国地震局地震预测开放基金项目

3JH-202401055XH24008D

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)