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黄海5.1级地震异常特征
引用本文:李飞,王福才,杨冯威,何培延.黄海5.1级地震异常特征[J].地震地磁观测与研究,2004,25(1):41-47.
作者姓名:李飞  王福才  杨冯威  何培延
作者单位:中国江苏 221400 新沂地震台;中国江苏 225601 高邮地震台
摘    要:结合地震地质构造,利用地震学有关方法,运用各向异性度对新沂台视电阻率进行分析;运用滑动平均对新沂台短水准进行分析;运用加卸载响应比对地磁z分量进行分析。结果表明:在黄海5.1级地震前,存在中短期异常,但临震异常不明显。

关 键 词:黄海地震  异常  各向异性  视电阻率  加卸载响应比
文章编号:1003-3246(2004)01-0041-07
修稿时间:2003年8月10日

Character of anomaly for Huanghai 5.1 earthquake
Li Fei,Wang Fucai,Yang Fengwei and He Peiyan Xinyi Seismic Station,Jiangsu Province ,China Gaoyou Seismic Station,Jiangsu Province ,China.Character of anomaly for Huanghai 5.1 earthquake[J].Seismological and Geomagnetic Observation and Research,2004,25(1):41-47.
Authors:Li Fei  Wang Fucai  Yang Fengwei and He Peiyan Xinyi Seismic Station  Jiangsu Province  China Gaoyou Seismic Station  Jiangsu Province  China
Institution:Li Fei1),Wang Fucai2),Yang Fengwei1) and He Peiyan1) 1) Xinyi Seismic Station,Jiangsu Province 221400,China 2) Gaoyou Seismic Station,Jiangsu Province 221400,China
Abstract:Based upon seismological geology tectonic, some relevant methods of seismology are applied in the paper. The anisotropy of resistivity is analyzed in Xinyi station. At same time, the short leveling is analyzed by the running mean method and the Z component of geomagnetism is also analyzed by the load-unload response ratio. It is revealed that there were obvious mid-short anomalies before Huanghai MS 5.1earthquake at Xinyi station; however, the impending earthqua- ke anomalies weren't obvious.
Keywords:Huanghai earthquake  anomaly  anisotropy  apparent resistivity  load-unload                  response ratio
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