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Journal ArticleDOI

Basic magnetic properties of rocks under the effects of mechanical stresses

Takesi Nagata
- 01 Mar 1970 - 
- Vol. 9, pp 167-195
TLDR
In this article, the effects of mechanical stresses on the magnetization of the earth's crust can be classified in two categories: (a) the reversible effect which disappears when the stress is removed; and (b) the irreversible effect which causes an irreversible enhancement or an irreversible demagnetization of remanent magnetization.
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This article is published in Tectonophysics.The article was published on 1970-03-01. It has received 103 citations till now. The article focuses on the topics: Remanence & Magnetization.

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Citations
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Numerical Evidences of Unrest Related Electromagnetic Effects in the Campi Flegrei Caldera

TL;DR: In this article, a numerical study performed using the Comsol multiphysics code is presented, carried out to evaluate the effects on the main physically observable fields of an ideal unrest episode of the Campi Flegrei Caldera (Italy).
Journal ArticleDOI

Effect of Mechanical Stresses on the Initial Susceptibility and Hysteresis Characteristics of an Ensemble of Nanoparticles

TL;DR: In this article, the effect of uniaxial mechanical stresses on the initial susceptibility, saturation remanence, and coercive force of materials in which single-domain nanoparticles are carriers of magnetic properties has been studied theoretically.
References
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Journal ArticleDOI

The seismomagnetic effect

TL;DR: In this article, the authors calculate local variations in the geomagnetic field, which are produced by stress changes in crustal rocks, from the stress patterns and the piezomagnetic properties of the rocks down to the Curie point isotherm.
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Earthquake Energy, Earthquake Volume, Aftershock Area, and Strength of the Earth's Crust

TL;DR: In this article, the authors deduced the energy of the largest possible earthquake from the spatial distribution of the stress energy within the earth's crust, which was then combined with the magnitude energy relation due to GUTENBERG and RICHTER, yielding a formulaE=6×102×A1·5.
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Effects of Uniaxial Compression on Remanent Magnetization

TL;DR: In this article, the effect of directional stress on the remanent magnetization of magnetite bearing rocks and nickel polycrystallites was investigated and a nearly reversible change in intensity was found when the direction of compression is perpendicular to that of TRM.
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The effect of stress on the susceptibility and magnetization of a partially magnetized multidomain system

TL;DR: In this article, a model for partial magnetization of an isotropic multidomain magnetic system was proposed and the behavior of the model system in response to applied stress was analyzed.
Journal ArticleDOI

Theory of the magnetic susceptibility of stressed rock

TL;DR: In this paper, the authors calculated the stress dependence of magnetic susceptibility of igneous rock from the multidomain theory of magnetic grains, assuming that the magnetic mineral is pure magnetite whose saturation magnetization, magnetocrystalline anisotropy and saturation magnetostriction are known.
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