首页> 外国专利> METHOD FOR FORETELLING EARTHQUAKE BY TOMOGRAPHY OR GENERATION REGION OF LONG WAVE EARTH CURRENT BEING PREMONITORY SYMPTOMS OF EARTHQUAKE

METHOD FOR FORETELLING EARTHQUAKE BY TOMOGRAPHY OR GENERATION REGION OF LONG WAVE EARTH CURRENT BEING PREMONITORY SYMPTOMS OF EARTHQUAKE

机译:地震前兆的长波层析成像或发电区域预兆地震的方法

摘要

PURPOSE:To foretell the occurring date, magnitude and centrum of an earthquake, by observing a radio wave or earth current generated as the omen phenomenon of an earthquake. CONSTITUTION:The long wave earth current being one of the premonitory symptoms of an earthquake is simultaneously observed at least at four points in the earth or the sea bottom. A wave source can calculate a relative error of about 1km from a received/detected signal and can draw the fault chart of a wave source region. The local small destruction of rock occurs on a fault plane becoming a centrum region prior to the generation of an earthquake and a radio wave is generated at this time. Therefore, the centrum region can be foretold from the centrum region. Since the relation between the magnitude of an earthquake, the expanse of the centrum region and the shift of the fault plane as well as the relation between the magnitude of shift and the generation intensity of a long wave are known, the magnitude of the earthquake can be foretold. Since the generation intensity and frequency of a long wave of 3kHz or less and the magnitude of the wave source region become max. immediately before the generation of an earthquake, the timewise change of these values are extrapolated by the continuous tomography of the wave source region and the data when the calculated magnitude of an earthquake (in the case of our country) becomes 7-8.4 is set to a data when an earthquake of magnitude of 7 or more occurs.
机译:目的:通过观察作为地震预兆现象而产生的无线电波或土流,来预测地震的发生日期,强度和中心。组成:长波地电流是地震的先兆之一,至少在地球或海底的四个位置同时被观测到。波形源可以从接收/检测到的信号中计算出大约1km的相对误差,并且可以绘制波形源区域的故障图。岩石的局部小破坏发生在断层平面上,该断层平面在地震发生之前成为中心区域,并且此时产生了无线电波。因此,可以从中心区域预知中心区域。由于已知地震的强度,中心区域的扩大与断层平面的位移之间的关系以及位移的大小与长波的产生强度之间的关系,因此地震的强度可以预言。 3kHz以下的长波的产生强度和频率以及波源区域的大小成为最大。紧接地震发生之前,通过震源区域的连续层析成像推断这些值的时间变化,并将计算出的地震烈度(在我国为例)为7-8.4时的数据设置为发生7级以上地震时的数据。

著录项

  • 公开/公告号JPH0536000B2

    专利类型

  • 公开/公告日1993-05-27

    原文格式PDF

  • 申请/专利权人 JUSEISHO TSUSHIN SOGO KENKYUSHOCHO;

    申请/专利号JP19870251470

  • 发明设计人 TAKAHASHI KOZO;

    申请日1987-10-07

  • 分类号G01V1/00;G01V3/12;

  • 国家 JP

  • 入库时间 2022-08-22 05:19:39

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