吉林地区地电阻率震兆异常对比分析  

Comparative analysis on earthquake precursor anomalies of geoelectrical resisitivity in Jilin region

作　　者：史红军[1,2] 赵卫星[1] 刘立波 李宁[1] 朱伟楠[1] SHI Hong-jun;ZHAO Wei-xing;LI Ning;ZHU Wei-nan;LIU Li-bo(Yushu Seismostation, Yushu 130400, Jilin, China;College o f Geo-exploration Science and Technology, Jilin University, Changchun 130026, China;Siping Seismostation, Siping 136000, Jilin, China)

机构地区：[1]榆树地震台,吉林榆树130400 [2]吉林大学地球探测科学与技术学院,长春130026 [3]四平地震台,吉林四平136000

出　　处：《世界地质》2016年第3期865-872,共8页World Geology

基　　金：中国地震局"地震监测;预报;科研三结合"课题(140701)

摘　　要：对采用形态法、归一化变化速率法和各向异性度法提取到的吉林省内深源地震以及浅源地震前的地电阻率异常变化进行对比分析，结果表明：①震前地电阻率出现1~2年尺度中期异常，甚至短期异常，异常以负异常为主；②震前地电阻率原始月均值异常变化幅度<1%,表明数字地电仪捕捉电信号灵敏度的提高，更与台址构造密不可分；③震前地电阻率出现异常变化，震后恢复到正常变化形态，反映出震前震中区地下应力的变化，震后区域构造应力场重新调整并逐渐恢复的过程。Pre-earthquake geoelectrical resisitivity anomalies of deep source and shallow source earthquakes in Jilin Province have been abstracted by morphological method, normalized rate change method and degree of anisotropy method. The results show that ① pre-earthquake geoelectrical resisitivity displayed 1 ?2 years mid-term a n o m aly,even short-term anomaly with mainly negative anomaly; (2)the original monthly m e a n of anomaly variation a m plitude of pre-earthquake geoelectrical resisitivity less than one percent, showing the increases of captures signal sensitivity by digital geoelectrical instrument, which inextricably links with the sandstone bedrock structure beneath stations; (3)anomalous variation existing in pre-earthquake geoelectrical resisitivity and recovery to normal morphology after earthquakes, reflecting the change of stress in underground epicentral area before earthquakes, and the return and restoration process of regional tectonic stress field after earthquakes.

关 键 词：吉林地区 地电阻率 异常 分析方法 

分 类 号：P631.322[天文地球—地质矿产勘探]