Domain structures in single crystal magnetite below the Verwey Transition as observed with a low-temperature magnetic force microscope
Author:
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://www.agu.org/journals/gl/v023/i020/96GL00962/96GL00962.pdf
Reference24 articles.
1. Magnetocrystalline anisotropy of low temperature phase of magnetite;Abe;J. Phys. Soc. Jpn,1976
2. Separation of local signals from the regional paleomonson record of the Chinese loess plateau: a rock-magnetic approach;Banerjee;Geophys. Res. Lett.,1993
3. Domain pattern observations in rock magnetism: progress and problems;Halgedahl;Phys. Earth Planet. Int.,1987
4. Low-temperature behavior of single-domain through multidomain magnetite;Halgedahl;Earth Planet. Sci. Lett.,1995
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