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地震 ›› 2024, Vol. 44 ›› Issue (4): 82-96.doi: 10.12196/j.issn.1000-3274.2024.04.006

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2023年12月18日甘肃积石山6.2级地震前地电阻率变化分析

张宇1,2, 柯浩楠3, 娄晓宇4, 胡颢迪2   

  1. 1.中国地震局地球物理研究所, 北京 100081;
    2.中国地震局地震预测研究所, 北京 100036;
    3.首都师范大学, 北京 100089;
    4.中国地震局地质研究所, 北京 100029
  • 收稿日期:2024-08-01 修回日期:2024-09-18 出版日期:2024-10-31 发布日期:2024-12-16
  • 作者简介:张宇(1984-), 女, 北京人, 在读博士研究生, 高级工程师, 主要从事地震地电观测方法和技术研究。
  • 基金资助:
    中国地震局地震预测研究所基本科研业务费专项(CEAIEF20240901)

Analysis of Changes in Geo-electrical Resistivity before the Jishishan MS6.2 Earthquake in Gansu Province on December 18, 2023

ZHANG Yu1,2, KE Hao-nan3, LOU Xiao-yu4, HU Hao-di2   

  1. 1. Institute of Geophysics, China Earthquake Administration, Beijing 100081, China;
    2. Institute of Earthquake Forecasting, China Earthquake Administration, Beijing 100036, China;
    3. Capital Normal University, Beijing 100089, China;
    4. Institute of Geology, China Earthquake Administration, Beijing 100029, China
  • Received:2024-08-01 Revised:2024-09-18 Online:2024-10-31 Published:2024-12-16

摘要: 2023年12月18日, 甘肃积石山发生了6.2级地震, 震中300 km范围内有9个地电阻率固定观测站。 本研究梳理了震前2~4年地电阻率观测资料, 在扣除年变化和趋势变化基础上, 分析震前异常变化情况。 震前临夏、 定西和通渭的地电阻率值均呈现趋势性下降和年变幅减小的形态, 下降幅度分别为4.9% (距震中44 km)、 1.2% (距震中164 km)和0.6% (距震中232 km), 且地震均发生在下降回转时段内。 异常形态与大量震例统计结果一致, 且距离震中越近, 异常变化幅度越大。 表明这3个台站的地电阻率变化与此次积石山6.2级地震的孕育存在关联。 研究还发现, 距离震中219 km的金银滩地震观测台没有明显震前异常现象, 后续将结合台站实际电性结构和断层分布进一步分析。

关键词: 2023年积石山6.2级地震, 地电阻率, 年变化, 异常变化

Abstract: The MS6.2 earthquake occurred in Jishishan County, Gansu Province, on December 18, 2023. Within a 300 km radius of the epicenter, there were 9 fixed geo-electrical resistivity observation stations. This study preprocessed the geo-electric resistivity observation data from 2 to 4 years before the earthquake, then analyzed the anomalous changes before the earthquake after eliminating annual and trend changes. It showed a declining trend in ground resistivity and a reduction in the annual variation amplitude before the earthquake at Linxia Station, Dingxi Station, and Tongwei Station, with decreasing magnitudes of 4.9% (44 km), 1.2% (164 km), and 0.6% (232 km) respectively. Earthquakes occurred during the declining reversal period. These anomaly patterns are consistent with statistical results from a large number of earthquake cases. Moreover, the closer the distance to the epicenter, the greater the magnitude of the anomaly change. This indicates that the changes in geo-electrical resistivity at these three stations are related to the MS6.2 earthquake in Jishishan. It was also found that there was no obvious pre-seismic anomaly at the Jinyintan seismic station, which is 219 km away from the epicenter of the earthquake. Further analysis will be conducted in conjunction with the station’s actual electricity structure and fault distribution.

Key words: The 2023 Jishishan MS6.2 earthquake, Geo-electrical resistivity, Annual variation, Anomalous variations

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