江苏地区渗流方位角变化特征分析  

About seepage azimuth characteristics in Jiangsu area

作　　者：鲍海英[1] 李飞 蒋延龄 卜玉菲[1] 韩丽 Bao Haiying;Li Fei;Jiang Yanling;Bu Yufei;Han Li(Jiangsu Earthquake Agency,Nanjing 210014,China;Xinyi Seismic Station of Jiangsu Province,Jiangsu Province 221400,China;Gaoyou Seismic Station,Jiangsu Province 225600,China;Guangzhou Automobile Group Co.,LTD,Guangdong Province 510000,China)

机构地区：[1]江苏省地震局,中国南京210014 [2]江苏省新沂地震台,中国江苏221400 [3]江苏省高邮地震台,中国江苏225600 [4]广州汽车集团股份有限公司,中国广东510000

出　　处：《地震地磁观测与研究》2018年第6期114-119,共6页Seismological and Geomagnetic Observation and Research

基　　金：江苏省地震局青年科学基金(项目编号:201603);地震监测专项任务(项目编号:17J11ZX037)

摘　　要：利用谐波振幅和峰谷值2种方法,计算江苏地电台站渗流方位角,并尝试利用渗流方位角进行映震分析,结果表明:(1)使用2种方法计算的渗流方位角相差不大,由此所得地震对应关系应基本可靠;(2)高邮地电台渗流方位角与高邮—宝应M_S 4.9地震对应关系较好。因此,对江苏地区开展渗流方位角变化特征分析具有一定意义。Two methods,harmonic amplitude and peak-valley value,are used to calculate the seepage azimuth of Jiangsu stations.Then the results are compared and analyzed.Finally,we study the response of the seepage azimuth to the earthquakes before.The result shows that:①The difference is very small between the seepage azimuth calculated by the peak-valley value method and the harmonic amplitude method.Therefore,it is reliable to try to carry out the seismic stress relationship with this result.②The relationship between the seepage azimuth of Gaoyou station and the Gaoyou-Baoying MS 4.9 earthquake is very good.Therefore,it is of certain significance to carry out the research on the characteristics of seepage azimuth in Jiangsu area.

关 键 词：地电场 渗流方位角 映震 

分 类 号：P315.722[天文地球—地震学]