地磁垂直分量日变幅逐日比法及其在新疆地区地震预测中的应用

Geomagnetic vertical component daily amplitude ratio method and its application to earthquake prediction in Xinjiang region

  • 摘要: 使用国家地磁台网中心产出的地磁场垂直分量分钟采样序列资料,对2015年1月1日至2025年12月31日期间的地磁逐日比异常与新疆地区MS5.0以上中强地震之间的关系进行了深入分析。结果显示,地磁逐日比异常与新疆地区MS5.0以上中强地震之间存在较好的对应关系,且在逐日比异常发生后三个月内,其异常阈值线内部区域或附近地区发生MS5.0以上强震的概率较高。根据统计分析,2015年1月1日至2025年12月31日期间,新疆地区共记录到32组(次)地磁逐日比异常,这些异常与随后三个月内发生的19组(次)地震有较好的对应关系,其中优势对应期为两个月,异常对应率为59.4%,漏报率为40.6%;地磁逐日比出现两次或多次超阈值异常时,对应发生了13次中强地震。本文提出并验证了地磁逐日比异常阈值线叠加法:将强震前出现的多条地磁逐日比异常的阈值线在空间上叠加到同一底图上,就会形成一个地磁逐日比异常阈值线集中区,中强地震则往往发生于该集中区。通过综合分析历史地震活动特征、活动构造断裂分布、电磁学科多参量异常耦合和配套以及强震预测的中长期潜在危险区、本地区年度中强地震风险区等多源信息,对发震区域进行精细研判,有效缩小了地磁逐日比预测在时空强度方面的误差范围。

     

    Abstract:
    Earthquake prediction is a long-term concerned but unsolved scientific challenge in the global seismological community. Due to the complex seismogenic process and the inaccessibility of underground structures for direct observation, traditional geophysical methods still have considerable uncertainty in the accurate prediction of earthquake occurrence time, location and magnitude. In recent years, geomagnetic methods have gradually become one of the important directions in short-term earthquake prediction research, owing to their advantages such as high sensitivity to changes in underground electrical structures, mature observation techniques and strong data continuity. In this paper, the daily ratio method of the vertical component daily variation amplitude of the geomagnetic field is used to study the relationship between the daily ratio of the geomagnetic field and the earthquake with MS≥5.0 in Xinjiang from January 1, 2015 to December 31, 2025. The results indicate a strong correlation between the daily ratio of the geomagnetic field and MS≥5.0 earthquakes. Within months after the daily ratio of the geomagnetic field exceeds an abnormal threshold line, the probability of an earthquake with MS≥5.0 occurring in the corresponding area is high. The following conclusions are drawn.
    1) Based on the minute-sampled data of the geomagnetic vertical component from the National Geomagnetic Network Center, this study investigates 43 earthquakes of MS≥5.0 in Xinjiang, China from January 1, 2015 to December 31, 2025. A total of 32 groups of geomagnetic daily ratio anomalies are counted, and 19 groups are followed by earthquakes. The anomaly correspondence rate is 59.4%, the false alarm rate is 40.6%, the earthquake missing rate is 44.1%, 21 earthquakes are successfully predicted, and the earthquake prediction accuracy is 48.8%. The dominant corresponding period is 2 months. Among them, only one geomagnetic daily ratio anomaly appeared before seven earthquakes, while two or more anomalies occurred before 13 earthquakes. Multiple anomalies are common before earthquakes, and the false alarm rate of grouped anomalies is much lower than that of single anomaly. Due to the uniqueness of geotectonic and active tectonic conditions in Xinjiang, the geomagnetic daily ratio anomalies before strong earthquakes also show regional characteristics. From January 1, 2015 to December 31, 2025, there were 25 days with geomagnetic storms characterized by the daily mean index Dst>−70 nT in the global geomagnetic environment, and consecutive storm days were counted as one event (Dst indices are obtained from https://wdc.kugi.kyoto-u.ac.jp/). Among them, six storms triggered over-threshold geomagnetic daily ratio anomalies. Only three of these storm-induced anomalies were followed by three earthquakes with MS5.0−5.9 within three months, and no earthquakes with MS≥6.0 occurred. The remaining three storm-induced anomalies were not followed by any earthquake of MS≥5.0. Statistics show that there is no one-to-one correspondence between moderate-strong geomagnetic storms and geomagnetic daily ratio anomalies, and most anomalies occur on geomagnetically quiet days. The monthly frequency of geomagnetic daily ratio anomalies is generally higher in winter and summer and lower in spring and autumn, without an obvious dominant distribution.
    2) This paper also studies three strong earthquakes with MS≥6.0: the MS6.1 Shaya earthquake on January 30, 2023, the MS7.1 Wushi earthquake on January 23, 2024, and the MS6.0 Akqi earthquake on December 4, 2025. It is found that the frequency and spatiotemporal evolution of geomagnetic daily ratio anomalies before these three earthquakes show certain similarity and repeatability. That is, two or more over-threshold geomagnetic daily ratio anomalies appeared within three months before these three earthquakes. This feature may indicate multiple micro-fractures in deep structures shortly before the mainshock, which can be regarded as a precursor of the sub-instability state before earthquakes. Before the mainshocks, geomagnetic daily ratio anomalies migrated from distant areas to the epicenter, with anomaly areas shrinking from large to small or moving toward the locked seismogenic zone. Epicenters are mainly located at the intersections, concentrated zones and high-curvature sections of anomaly threshold lines, which is helpful for predicting the location of future earthquakes.
    3) By superimposing multiple daily geomagnetic ratio anomalies threshold lines on the same base map, an abnormal intersection area or a concentration area can be formed.
    Earthquakes frequently occur in these areas where daily geomagnetic ratio threshold lines are concentrated or intersect. Combined with the distribution of active tectonic faults, historical seismicity, multi-parameter anomaly coupling, and the long-term and short-term predictions for the potential strong earthquake risk zones and annual seismic hazard zones in Xinjiang, comprehensive judgment on seismically risky areas can effectively reduce the errors in location, time and magnitude predicted by the geomagnetic daily ratio method. This provides a reference for determining the location and time of subsequent strong earthquakes, and is of practical significance for the application of earthquake prediction techniques.

     

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