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Introduction There are two kinds of methods for the mathematic study on electro-magnetic induction in geo-field: one is analytic method, such as integral equation method; the other is numerical model-ing method, such as finite difference method and finite element method. The analytic method can only be applied to the conductor with very simple shape, such as sphere, circular cylinder, etc. With the increasing of computing speed and popularity of computer, the numerical modeling methods are use… 相似文献
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文章综述了几个地震之前短周期地磁变化参数的时间变化,认为利用它有可能探寻震前地下电导率的异常。为了捕捉该类地震前兆,需要在重点地震监测区建立较密的三分量磁力仪台网。 相似文献
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IntroductionThe history of studying the changes in deep geoelectric conductivity of an earthquake preparation using the parameters of geomagnetic short-period variations has been about 30 years. At first, Japanese calculated the real transfer functions as well as the a and b coefficients of Parkinson vector by taking the measurement of graph and using empirical formula. There are some examples, such as the 1923 Kanto M=7.9 earthquake (Yanagihara, 1972), the 1966 Tashkent M=5.5 earthquake, t… 相似文献
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地磁水平场转换函数在唐山地震前的异常反应 总被引:1,自引:1,他引:1
搜集了昌黎和白家疃1972~1984年的磁变仪资料.19组资料的计算结果表明:① 白家疃的单台垂直场转换函数A,B及昌黎的B没有明显异常,但昌黎的Au,Av有明显异常变化.这一结果与用量图方法求得的a,b基本一致.表明异常局限在余震区及其附近;② 台际转换函数Cu,Cv,Fu,Fv在唐山地震前都有一些变化,但虚部Cv,Fv的变化较为显著.这点与对台湾花莲地震的研究结果一致.但Beamish(1982)对Carlisle 5级地震的研究结果,是实部Fu,Cu的变化较为显著. 相似文献
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广东省地磁台的帕金森矢量及广州台的系数在河源地震前后的时间变化 总被引:1,自引:0,他引:1
本文发现广州、香港、琼中三个台的帕金森矢量垂直于海岸线总的走向并指向海洋,且香港、琼中的矢量比广州大1—1.5倍,有着明显的海岸效应的特点。在河源地震前后|B|出现了两个最低的值,且超过了一倍标准差。这也许不是偶然的巧合,但仍不能说有明显的异常。广州台 A、B 有明显的季节变化,A 是周年变化,B 以半年变化占优势。 相似文献
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TheanomalousreactionsofthegeomagnetichorizontalfieldtransferfunctionsbeforeTangshanearthquakeSHAOJINGGONG(龚绍京)HUARANCHEN(... 相似文献
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