The coercive force of fine particles of monoclinic pyrrhotite (Fe7S8) studied at elevated temperature-Reference-Cited by-同舟云学术

The coercive force of fine particles of monoclinic pyrrhotite (Fe7S8) studied at elevated temperature

Published:1995-05 Issue:1-2 Volume:89 Page:51-62
ISSN:0031-9201
Container-title:Physics of the Earth and Planetary Interiors
language:en
Short-container-title:Physics of the Earth and Planetary Interiors

Author:

Menyeh A.,O'Reilly W.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Physics and Astronomy (miscellaneous),Geophysics,Astronomy and Astrophysics

Reference29 articles.

1. Origin of magnetic anisotropy energy of Fe7S8 and Fe7Se8;Adachi;J. Appl. Phys.,1968

2. Magnetic anisotropy in pyrrhotite;Bin;J. Appl. Phys.,1963

3. Dévelopment d'aimantation cristalline et d'auto-inversion dans les roches à pyrrhotite; implications en paléomagnétisme et pour l'interprétation des anomalies magnétiques;Bina;C. R. Acad. Sci. Paris,1993

4. Magnetic properties of minerals;Bleil,1982

5. Hysteresis properties of sized dispersed monoclinic pyrrhotite grains;Clark;Geophys. Res. Lett.,1984

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