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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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Ionospheric anomalies observed over South Korea preceding the Great Tohoku earthquake of 2011

TL;DR: In this article, the authors investigated the ionospheric anomalies observed before the Tohoku earthquake, which occurred near the northeast coast of Honshu, Japan on 11 March, 2011.
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Seismo-electrical effects: Experiments and field measurements

TL;DR: In this article, the authors report on laboratory and field measurements of electrical effects caused by dislocation of different geomaterials at a shear plane and propose a phenomenological model in four steps: mechanical loading, charge generation in the creep phase, charge separation during dislocation, and mechanical relaxation and electrical discharge.
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Plasma and Fields Evaluation at the Chinese Seismo-Electromagnetic Satellite for Electric Field Detector Measurements

TL;DR: The main objective of this paper is that of improving the accuracy of the electric field detectors (EFDs), which are installed on CSES and will measure the field vector in a wideband from dc up to 3.5 MHz.
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Tropospheric and Ionospheric Anomalies Induced by Volcanic and Saharan Dust Events as Part of Geosphere Interaction Phenomena

TL;DR: In this article, the authors assessed the possible relation of ionospheric perturbations observed by Detection of Electro-Magnetic Emissions Transmitted from Earthquake Regions (DEMETER), Global Positioning System total electron content (GPS TEC), National Oceanic and Atmospheric Administration (NOAA)-derived outgoing longwave-Earth radiation (OLR), and atmospheric chemical potential (ACP) measurements, with volcanic and Saharan dust events identified by ground and satellite-based medium infrared/thermal infrared (MIR/TIR) observations.
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Ionospheric turbulence from ground-based and satellite VLF/LF transmitter signal observations for the Simushir earthquake (November 15, 2006)

TL;DR: In this paper, the ground and satellite data were processed by a method based on the difference between the real signal at night-time and the model signal, and a two-dimensional model of the signal distribution over the selected area was constructed.
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.
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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.
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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.
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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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