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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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Citations
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Review of electric and magnetic fields accompanying seismic and volcanic activity

TL;DR: In this paper, magnetic, electric and electromagnetic field variations were obtained on Mt. Unzen in Japan, Reunion Island in Indian Ocean, the Long Valley volcanic caldera in California, and for faults in China and Russia, California and several other locations.
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ELF and VLF radio waves

TL;DR: A review of developments in ELF and VLF radio-wave propagation research over the last 50 years of the Journal of Atmospheric and Solar-Terrestrial Physics can be found in this paper.
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Ionospheric Precursors of Earthquakes; Recent Advances in Theory and Practical Applications

TL;DR: In this paper, a physical model was developed to bridge the traditional precursors of earthquakes and ionospheric ones, demonstrating that the latter belong to the same family, and a possible system of ground-based measurements and satellite monitoring was proposed for regional and global monitoring and possible short-term prediction of destructive earthquakes.
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A mechanism for the production of electromagnetic radiation during fracture of brittle materials

TL;DR: In this article, the feasibility of the charge separation model as the source of electromagnetic radiation received from the fracture of brittle materials is demonstrated, and an analytical expression and a finite difference method enable the calculation of currents flowing around the tip of a crack.
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Ionosphere plasma bubbles and density variations induced by pre‐earthquake rock currents and associated surface charges

TL;DR: In this paper, the authors formulated a coupling model for the stressed rock-Earth surface charges-atmosphere ionosphere system, where the stressed-rock acts as the dynamo to provide the currents for the coupling system.
References
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Observation by space-borne detectors of electric fields and hydromagnetic waves in the ionosphere over an earthquake centre

TL;DR: In this article, the Intercosmos-Bulgaria-1300 satellite in the nearequatorial ionosphere over an earthquake center (φ ∗ = 3.39° S and λ ∗= 177.43° E, M = 4.8) on 21 January 1982
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Continuous, traveling coupling between seismic waves and the ionosphere evident in May 1968 Japan earthquake data

TL;DR: In this paper, atmospheric and ionospheric data collected at Japan and Hawaii after the May 16, 1968, Hachinohe, Japan, earthquake have been analyzed and compared, showing that earth-quake-generated seismic waves produced upward-traveling acoustic waves that propagated over a large front and penetrated into the atmosphere to at least 300 km, producing oscillatory disturbances there.
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Electromagnetic ELF radiation from earthquake regions as observed by low‐altitude satellites

TL;DR: In this article, the data of the COSMOS-1809 satellite were analyzed over the earthquake region in Armenia during the period from January 20 to February 17, 1989, and it was shown that during the event the seismic region is permanently radiating; the intensity and the envelope shape of the wave depend on its time relatively to the time of the earthquake.
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A mechanism to explain the generation of earthquake lights

TL;DR: In this paper, a physical model based on frictional heating of the fault was proposed to solve the problem of how large charge densities can be concentrated and sustained in a conductive Earth.
Journal ArticleDOI

Emission of electromagnetic radiation preceding the Ito seismic swarm of 1989

Yukio Fujinawa, +1 more
- 27 Sep 1990 - 
TL;DR: In this paper, anomalous electromagnetic signals were detected several hours before the occurrence of large earthquakes near Ito city, Japan, about 150 km from the location of the electrodes, which indicated that their monitoring could be valuable for the prediction of seismic activity.
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