Remanent magnetization and coercivity of rocks under hydrostatic pressure up to 1.4 GPa-Reference-Cited by-同舟云学术

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Remanent magnetization and coercivity of rocks under hydrostatic pressure up to 1.4 GPa

Published:2013-08-06 Issue:15 Volume:40 Page:3858-3862
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Demory F.¹,Rochette P.¹,Gattacceca J.¹²,Gabriel T.¹,Bezaeva N. S.³

Affiliation:

1. Aix-Marseille Université, CNRS, IRD, CEREGE UM34; 13545 Aix en Provence France

2. Department of Earth, Atmospheric, and Planetary Sciences; Massachusetts Institute of Technology; Cambridge Massachusetts USA

3. Earth Physics Department, Faculty of Physics; M.V. Lomonosov Moscow State University Leninskie Gory; Moscow Russia

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference26 articles.

1. An interpretation of magnetic signatures of subduction zones detected by MAGSAT;Arkani-Hamed;Tectonophysics,1987

2. Demagnetization of terrestrial and extraterrestrial rocks under hydrostatic pressure up to 1.2 GPa;Bezaeva;Phys. Earth Planet. In.,2010

3. Deformation and paleomagnetism;Borradaile;Surv. Geophys.,1997

4. Magnetic properties of natural pyrrhotite, part 1: Behaviour of initial susceptibility and saturation-magnetization related rock magnetic parameters in a grain-size dependent framework;Dekkers;Phys. Earth Planet. In.,1988

5. Magnetic minerals in the Martian crust;Dunlop;J. Geophys. Res.,2005

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3. Magnetic characterization of non-ideal single-domain monoclinic pyrrhotite and its demagnetization under hydrostatic pressure up to 2 GPa with implications for impact demagnetization;Physics of the Earth and Planetary Interiors;2016-08

4. The effect of hydrostatic pressure up to 1.61 GPa on the Morin transition of hematite‐bearing rocks: Implications for planetary crustal magnetization;Geophysical Research Letters;2015-12-12

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