利用构造板块应力释放的电磁能量拍摄岩石圈中的贝尼奥夫带

J. Heraud, V. Centa, T. Bleier
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引用次数: 2

摘要

多年来,科学文献报道了电磁现象的不同表现,将它们与地震事件联系起来,从大到3.0毫升的地震。例如震前和同震发光,各种形式的电荷位移和磁场,应力产生的电磁脉冲,不同频率加速电荷产生的无线电波,甚至奇怪的动物行为。在本文中,我们报告了几个与地震事件相关的电磁脉冲事件,并通过磁力计记录了这些事件,并分析了几个电磁现象的案例,这些电磁现象导致了通过被动接收与地震相关的脉冲来确定岩石圈的物理形态和其他物理方面。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Images of the benioff zone in the lithosphere using electromagnetic energy released from stress in tectonic plates
Different manifestations of electromagnetic phenomena have been reported in the scientific literature for many years, linking them with seismic events, from large to even 3.0 Ml earthquakes. Examples are pre-seismic and co-seismic luminescence, various forms of electric charge displacement and magnetic fields, stress generated electromagnetic pulses, radio wave generation by accelerated charges at different frequencies and even strange animal behavior. In this paper, we report several events of electromagnetic pulses associated with seismic events and registered by magnetometers and analyze several cases of EM phenomena leading to the determination of the physical morphology and other physical aspects of the lithosphere from passive reception of pulses associated with earthquakes.
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