Remanent magnetization of a “paramagnetic” composition in the ilmenite-hematite solid solution series
Author:
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://www.agu.org/journals/gl/v011/i003/GL011i003p00197/GL011i003p00197.pdf
Reference17 articles.
1. Alternating field characteristics of pseudo-single-domain (2-14 um) and multidomain magnetite;Bailey;Earth Planet. Sci. Lett.,1983
2. Theoretical single-domain grain size range in magnetite and titanomagnetite;Butler;J. Geophys. Res.,1975
3. Single domain magnetite and high coercivitis in a gabbroic instrusion;Evans;Earth Planet. Sci. Lett.,1968
4. Cation diffusion processes and self-reversal of thermoremanent magnetization in the ilmenitehematite solid solution series;Hoffman;Geophys. J.,1975
5. On the kinetics of cation ordering in the hemoilmenites and reexamination of the self-reversal process;Hoffman;EOS,1975
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