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High-frequency seismo-electromagnetic effects

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TLDR
A review of the high-frequency seismo-electromagnetic phenomena already observed, and occurring before, as well as after, the great Alaskan earthquake in 1964 can be found in this paper.
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This article is published in Physics of the Earth and Planetary Interiors.The article was published on 1993-04-01. It has received 121 citations till now.

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Proceedings ArticleDOI

A Study on Using Natural Source Super Low Frequency Electromagnetic wave to Explore Goaf

TL;DR: The theory and exploring method of using natural source super low frequency (SLF) electromagnetic wave to detect goaves was introduced and the effect of exploration was proved by comparing experiment results with well logging.
Journal ArticleDOI

The ESPERIA satellite project for detecting seismo-associated effects in the topside ionosphere. First instrumental tests in space

TL;DR: The ESPERIA space mission project as mentioned in this paper has been designed for the Italian Space Agency (ASI), and a few instruments of its payload have been built and tested in space to investigate seismo-associated phenomena.

The ESPERIA satellite project for detecting seismo-associated effects in the topside ionosphere

TL;DR: The ESPERIA space mission project as mentioned in this paper has been designed for the Italian Space Agency (ASI), and a few instruments of its payload have been built and tested in space to investigate seismo-associated phenomena.
Journal Article

Observation of seismogenic ultra low frequency electric field fluctuations detected as a burst in the ionosphere during tsunamis over the Andaman and Nicobar Islands

TL;DR: From the recorded observations, it is clear that the intensity of the electric fluctuations varies with the number of earthquakes and diminishes as the number decreases, and the pattern of electric field fluctuations recorded could be used for a precursory study of earthquake occurrences.
Journal ArticleDOI

The ultra low frequency electromagnetic radiation observed in the topside ionosphere above boundaries of tectonic plates

TL;DR: In this paper, a comparison between ultra low frequency (ULF) electromagnetic (EM) radiation, recorded by an electric field instrument onboard the satellite detection of electromagnetic emissions transmitted from earthquake regions in the topside ionosphere, and the seismicity of regions with high and low seismic activity is presented.
References
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Journal ArticleDOI

Estimation of the size of earthquake preparation zones

TL;DR: In this article, an approximate solution of the problem for a soft elastic inclusion in an elastic half-space is presented. But the authors assume that the moduli of the inclusion differ slightly from those of the surrounding medium (by no more than 30%).
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Low‐frequency magnetic field measurements near the epicenter of the Ms 7.1 Loma Prieta Earthquake

TL;DR: In this paper, the authors report the results of measurements of low frequency magnetic noise by two independent monitoring systems prior to the occurrence of the M{sub s} 7.1 Loma Prieta earthquake of 17 October 1989.
Journal ArticleDOI

Physical properties of the variations of the electric field of the earth preceding earthquakes, I

TL;DR: In this article, the physical properties of the preseismic transient variations in the electrotelluric field were described and a few points that were not properly emphasized in previous publications were clarified.
Journal ArticleDOI

Latest aspects of earthquake prediction in Greece based on seismic electric signals, II☆

TL;DR: In this article, the authors reviewed the latest developments in seismic electric signals (SES) based earthquake prediction and described the current procedures used to predict the epicenter and magnitude of an impending earthquake.
Journal ArticleDOI

Global propagation of atmospheric gravity waves: A review

TL;DR: The theoretical and observational evidence concerning the global propagation of atmospheric gravity waves is reviewed in this article, with special emphasis on the waves generated in the auroral zones, and it is concluded that the only natural sources of large-scale TIDs are in the ionospheric zones.
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