地震易发地区的地震电信号

IF 1.9 4区地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS

Earthquake Science Pub Date : 2018-01-01 DOI:10.29382/EQS-2018-0005-5

N. Sarlis, P. Varotsos, E. Skordas, S. Uyeda, J. Zlotnicki, T. Nagao, A. Rybin, Mary S. Lazaridou-Varotsos, K. Papadopoulou, Emsev, Emsev

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引用次数: 19

摘要

Varotsos-Alexopoulos-Nomicos (VAN)方法是20世纪80年代提出的短期地震预报方法。VAN方法通过观察地球电场的瞬态变化，即地震电信号(SES)，可以估计即将发生地震的震中、震级和发生时间。在这里，我们给出了几个在世界各地地震易发地区观测到的SES的例子。

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Seismic electric signals in seismic prone areas

The Varotsos-Alexopoulos-Nomicos (VAN) method of short-term earthquake prediction was introduced in the 1980s. The VAN method enables estimation of the epicenter, magnitude and occurrence time of an impending earthquake by observing transient changes of the electric field of the Earth termed seismic electric signals (SES). Here, we present a few examples of SES observed in various earthquake prone areas worldwide.

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