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应城MS4.9地震前第二类地脉动信号异常分析
引用本文:韦进,吕品姬,郝洪涛,王建伟,栗宁,胡敏章.应城MS4.9地震前第二类地脉动信号异常分析[J].大地测量与地球动力学,2022,42(1):88-95.
作者姓名:韦进  吕品姬  郝洪涛  王建伟  栗宁  胡敏章
作者单位:中国地震局地震大地测量重点实验室;武汉引力与固体潮国家野外科学观测研究站
基金项目:国家自然科学基金(41204058);武汉引力与固体潮国家野外科学观测研究站开放基金(WHYWZ202106)。
摘    要:2019-12-26应城MS4.9地震前,襄阳重力台记录到第二类(double frequency, DF)地脉动信号持续增强异常。对比全球能量辐射模型(ASSM)及西太平洋台风数据发现,震前10 h左右的DF地脉动增强及优势频率增大的异常与西太平洋Phanfone台风靠近中国大陆这一远场信号源关系较弱,与本地未知近场同源同频信号有关。结合恩施重力台观测分析认为,该异常信号不属于应城地震前的慢地震事件。此外研究发现,长江中游巴东-秭归段和襄樊-广济断裂及其邻近区域5次MS4.0以上地震中的4次都与七曜山-金佛山断裂附近发生的MS4.5~5.0地震呈成组活动,时间间隔为0.5~1 a,且发震时间都在DF地脉动信号的高噪声水平时段内(10月~次年3月)。当恩施-襄阳DF地脉动信号基线的月中位数和众数值的差异持续4个月增加或处于高值时,研究区发生MS4.0以上地震的可能性增加。对震前DF地脉动信号异常特征的总结可为预测未来长江中游巴东-秭归段和襄樊-广济断裂及其邻近区域MS4.0以上地震的发生时段提供经验指标。

关 键 词:gPhone重力仪  DF地脉动信号异常  ASSM  应城MS4.9地震  

Study on the Anomalies of the Double Frequency Microseisms before Yingcheng Ms4.9 Earthquake
WEI Jin,L Pinji,HAO Hongtao,WANG Jianwei,LI Ning,HU Minzhang.Study on the Anomalies of the Double Frequency Microseisms before Yingcheng Ms4.9 Earthquake[J].Journal of Geodesy and Geodynamics,2022,42(1):88-95.
Authors:WEI Jin  L Pinji  HAO Hongtao  WANG Jianwei  LI Ning  HU Minzhang
Institution:(Key Laboratory of Earthquake Geodesy,CEA,40 Hongshance Road,Wuhan 430071,China;Wuhan Gravitation and Solid Earth Tides,National Observation and Research Station,40 Hongshance Road,Wuhan 430071,China)
Abstract:It is found that the anomalies of the double frequency (DF) microseisms in Xiangyang gravity station (XYS) before the Yingcheng MS4.9 earthquake on December 26, 2019 is continuously enhanced. By comparing the Ardhuin seismic spectra model(ASSM) and the western Pacific typhoon data, we find that the relationship between the enhancement anomalies of DF microseisms and the dominant frequency in the 10 hours before the earthquake and the western Pacific Phanfone are weaker than that of the local unknown near field homologous frequency signal. Combined with the observation and analysis of Enshi gravity station (ENS), we consider that the anomalies signal is not a slow earthquake event before the Yingcheng earthquake. 4 of the 5 earthquakes larger thanMS4.0 in Badong-Zigui areas and Xiangyang-Guangji fault areas have the regularity of group activity with the earthquakes withMS4.5-5.0 near Qiyaoshan-Jinfoshan fault areas about 0.5-1 year ago. Further, their occurrence time are in the period of high noise level of DF microseisms from October to March in the next year. If the difference between the median and majority values of ENS-XYS DF microseisms baseline increases continuesly for 4 months or at a high level, it is possible to occurMS≥4.0 earthquake in the studied area. The conclusion of the anomalies before the earthquake can provide experience and reference for the occurrence period of earthquakes greater thanMS4.0 near Badong-Zigui areas and Xiangfan-Guangji fault areas in the future.
Keywords:gPhone gravimeter  the anomalies of the DF microseisms  ASSM  Yingcheng Ms4  9 earthquake
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