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2020年伽师MS6.4地震前柯坪台地电阻率数据变化分析

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2020年1月19日位于新疆南天山西的柯坪推覆体附近发生了伽师MS6.4地震,通过对距离震中169 km的柯坪地电阻率观测数据分析显示:自2017年10月开始柯坪台两分量地电阻率观测值出现明显速率异常变化,NS向异常变化幅度为-2.33%,EW向为-0.72%;同时两分量表现出各向异性变化,异性度S出现快速下降变化.为了探讨柯坪地电阻率异常同伽师MS6.4地震是否存在力学机理上的联系,本文中通过断层虚位错模型计算了地震前观测点区域内应力应变的分布,并结合震源机制解计算的P轴方向,发现在地震前柯坪地电阻率的异常变化同此次地震具有相关性.
ANALYSIS ON APPARENT RESISTIVITY VARIATIONS OF KEPING STATION BEFORE 2020 JIASHI MS6.4 EARTHQUAKE
On January 19,2020,the Jiashi MS 6.4 earthquake occurred near the Keping nappe in the west of the southern Tianshan Mountains in Xinjiang.The analysis of the Keping ground resistivi-ty observation data at 169 km from the epicenter shows that since October 2017,the two-component ground resistivity observation values of the Keping station have shown obvious abnormal rate chan-ges.The NS-direction abnormal change range is-2.33%,and the EW-direction is-0.72%.At the same time,the two components showed anisotropic changes,and the anisotropy S decreased rap-idly.In order to explore whether there is a mechanical mechanism between the Keping ground resis-tivity anomaly and the Jiashi MS 6.4 earthquake,this paper calculates the distribution of stress and strain in the observation point area before the earthquake by the fault virtual dislocation model,and combines the P-axis direction calculated by the focal mechanism solution.It is found that the ab-normal change of Keping ground resistivity before the earthquake is related to the earthquake.

Jiashi MS6.4 earthquakeKeping station apparent resistivityAnomaly variationFault virtual dislocation model

刘海洋、艾萨·伊斯马伊力、徐衍刚、韩时雨

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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

伽师MS6.4地震 柯坪台地电阻率 异常变化 断层虚位错模式

中国地震局震情跟踪青年项目中国地震局监测、预报、科研三结合课题新疆维吾尔自治区自然基金特培项目

20230104153JH-2024010552022D03031

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(3)
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