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Ultra Low-Frequency Electromagnetic Disturbances Appearing before Strong Seismic Events

机译:在强烈地震事件发生之前出现超低频电磁干扰

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摘要

Analysis of experimental observations of variations in the magnetic field of the Earth recorded by instrumental complexes of the North Caucasus Geophysical Observatory is performed. It is shown that it is possible to distinguish characteristic ultra-low-frequency (ULF) wave forms in the structure of the recorded electromagnetic signals preceding strong teleseismic events.
机译:对北高加索地球物理天文台的仪器配合物记录的地球磁场变化的实验观察结果进行了分析。结果表明,有可能在强地震事件发生之前,在记录的电磁信号的结构中区分特征性的超低频(ULF)波形。

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  • 来源
    《Doklady Earth Sciences》 |2009年第9期|1549-1552|共4页
  • 作者单位

    Schmidt Institute of Physics of the Earth, Russian Academy of Sciences,ul. Bol'shaya Gruzinskaya 10, Moscow, 123995 Russia;

    Pushkov Institute of Terrestrial Magnetism, the Ionosphere, and Radiowave Propagation, Russian Academy of Sciences,Troitsk, Moscow oblast, 142190 Russia;

    Schmidt Institute of Physics of the Earth, Russian Academy of Sciences,ul. Bol'shaya Gruzinskaya 10, Moscow, 123995 Russia;

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