The effect of low-temperature oxidation on large multi-domain magnetite
Author:
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://www.agu.org/journals/gl/v021/i009/94GL00639/94GL00639.pdf
Reference20 articles.
1. Alternating field characteristics of pseudo-single-domain (2-14 μm) and multidomain magnetite;Bailey;Earth planet. Sci. Lett.,1983
2. Hysteresis properties of titanomagnetites: grain-size and compositional dependence;Day;Phys. Earth planet. Inter.,1977
3. Determination of domain structure in igneous rocks by alternating field and other methods;Dunlop;Earth planet. Sci. Lett.,1983
4. Hysteresis properties of magnetite and their dependence on particle size: a test of pseudo-single-domain remanence models;Dunlop;J. geophys. Res.,1986
5. Stability of anhysteretic remanent magnetization in fine and coarse magnetite and maghemite particles;Johnson;Geophys. J. R. astron. Soc.,1975
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