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Seismic electric signals in seismic prone areas

Seismic electric signals in seismic prone areas
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摘要 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. 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.
出处 《Earthquake Science》 CSCD 2018年第1期44-51,共8页 地震学报(英文版)
关键词 seismic electric signals VAN method earthquake prediction EMSEV-Bishkek RS-RAS cooperation seismic electric signals VAN method earthquake prediction EMSEV-Bishkek RS-RAS cooperation
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