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Electromagnetic precursors to earthquakes in the Ulf band: A review of observations and mechanisms

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TLDR
In this article, the authors have demonstrated conclusively that self potentials develop owing to fluid flow and that both resistivity and magnetization change when rocks are stressed, however, field experiments have had much less success.
Abstract
Despite over 2 decades of international and national monitoring of electrical signals with the hope of detecting precursors to earthquakes, the scientific community is no closer to understanding why precursors are observed only in some cases. Laboratory measurements have demonstrated conclusively that self potentials develop owing to fluid flow and that both resistivity and magnetization change when rocks are stressed. However, field experiments have had much less success. Many purported observations of low-frequency electrical precursors are much larger than expectations based on laboratory results. In some cases, no precursors occurred prior to earthquakes, or precursory signals were reported with no corresponding coseismic signals. Nonetheless, the field experiments are in approximate agreement with laboratory measurements. Maximum resistivity changes of a few percent have been observed prior to some earthquakes in China, but the mechanism causing those changes is still unknown. Anomalous electric and magnetic fields associated with fluid flow prior to earthquakes may have been observed. Finally, piezomagnetic signals associated with stress release in earthquakes have been documented in measurements of magnetic fields.

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Journal ArticleDOI

Earthquake prediction: a critical review

TL;DR: Theoretical work suggests that faulting is a non-linear process which is highly sensitive to unmeasurably fine details of the state of the Earth in a large volume, not just in the immediate vicinity of the hypocentre.
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Streaming potential in porous media: 1. Theory of the zeta potential

TL;DR: In this paper, the authors derived analytical equations for the ξ potential and specific surface conductance of a binary symmetric 1:1 electrolyte such as NaCl and used them to predict the variations of these parameters with the pore fluid salinity, temperature, and pH (within a /pH range of 6-8).
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OPERATIONAL EARTHQUAKE FORECASTING. State of Knowledge and Guidelines for Utilization

TL;DR: In this article, the authors focus on the short-term prediction and forecasting of tectonic earthquakes and indicate guidelines for utilization of possible forerunners of large earthquakes to drive civil protection actions, including the use of probabilistic seismic hazard analysis in the wake of a large earthquake.
Journal ArticleDOI

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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Taiwan orogeny: thin-skinned or lithospheric collision?

TL;DR: In this paper, the thin-skinned tectonics hypothesis was formulated to explain mainly the geologic and relatively shallow structures in Taiwan orogeny, which can be used continually to test critically hypotheses of the Taiwan Orogeny.
References
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Journal ArticleDOI

The electrical resistivity log as an aid in determining some reservoir characteristics

TL;DR: The usefulness of the electrical resistivity log in determining reservoir characteristics is governed largely by: (1) the accuracy with which the true resistivity of the formation can be determined; (2) the scope of detailed data concerning the relation of resistivity measurements to formation characteristics; (3) the available information concerning the conductivity of connate or formation waters; and (4) the extent of geologic knowledge regarding probable changes in facies within given horizons, both vertically and laterally, particularly in relation to the resultant effect on the electrical properties of the reservoir as mentioned in this paper.
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Magnetotellurics with a remote magnetic reference

TL;DR: In this article, magnetic field measurements were performed simultaneously at two sites 4.8 km apart near Hollister, California, where the data obtained at each site were analyzed using the magnetic fields at the other site as a remote reference.
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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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Pressure solution and the force of crystallization: a phenomenological theory

TL;DR: In this article, the authors assume that this transport takes place by diffusion in a solution film between the grains and predict an increase in pressure solution with decreasing grain size, and they also explain how pre-existing clay films in the sediment may develop into stylolites.
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Experimental and theoretical basis of electrokinetic phenomena in rock‐water systems and its applications to geophysics

TL;DR: In this article, the authors measured the ζ potentials and the streaming potential coefficients of silicate mineral-water and rock-water systems for purposes of estimating the magnitude of electrokinetic effects induced by water diffusion in the earth's interior.
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