RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 10, ES6003, doi:10.2205/2008ES000305, 2008

2008ES000305-fig06.html
Figure 6. Curves of AF ( H ) demagnetization of various types of remanence created in titanomagnetite samples (initial x = 0.6) under different conditions of their cooling that underwent multiphase oxidation at 500oC in a field of 0.1 mT during 168 h: (2-4) CRM+pTRM, cooling rates of (2) 100, (3) 10, and (4) 1oC/h; (1) pTRM created in sample 4 (after demagnetization of its components CRM+pTRM by the field H ) during its cooling from 500oC at a rate of 1000oC/h in a field of 0.1 mT.

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Citation: Gapeev, A. K., and S. K. Gribov (2008), Self-reversal of chemical remanent magnetization during multiphase oxidation of synthetic titanomagnetites, Russ. J. Earth Sci., 10, ES6003, doi:10.2205/2008ES000305.

Copyright 2008 by the Russian Journal of Earth Sciences
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