More on the low-temperature magnetism of stable single domain magnetite: Reversibility and non-stoichiometry
Author:
Affiliation:
1. Institute for Rock Magnetism, Newton Horace Winchell School of Earth Sciences; University of Minnesota; Minneapolis Minnesota USA
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Reference14 articles.
1. Low-temperature remanence in stable single domain magnetite;Carter-Stiglitz;Geophys. Res. Lett.,2002
2. Correction to “Low-temperature remanence in stable single domain magnetite”;Carter-Stiglitz;Geophys. Res. Lett.,2003
3. Separating multidomain and single-domain-like remanences in pseudo-single-domain magnetites (215-540 nm) by low-temperature demagnetization;Dunlop;J. Geophys. Res.,1991
4. Dunlop , D. J. Ö. Özdemir 1997 Rock Magnetism: Fundamentals and Frontiers Cambridge Univ. Press New York
5. Influence of deviations from ideal stoichiometry on the anisotropy parameters of magnetite Fe3(1-δ)O4;Kakol;Phys. Rev. B,1989
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