Magnetic susceptibility is the ratio of induced magnetization to the strength of the magnetic field causing the magnetization. Magnetic (susceptibility) anisotropy , in minerals with low crystal symmetry or in rocks with planar or linear fabric, refers to magnetic susceptibility that is not perfectly parallel with the inducing magnetic field because it depends on direction and induced magnetization. Ferromagnetism is a type of magnetic order in which all magnetic atoms in a domain have their moments aligned in the same direction. Ferrimagnetism , another type of magnetic order, macroscopically resembles ferromagnetism. Magnetic ions at different crystal sites are opposed, that is, antiferromagnetically coupled. There is nevertheless a net magnetization because of inequality in the number or magnitude of atomic magnetic moments at the two sites. This type of magnetic order occurs in magnetite. ParamagneticMinerals—those having a small positive magnetic susceptibility, for example,...
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El-Ashry, M.T., Nejib, U.R. (1984). Magnetic susceptibility, earth materials . In: Finkl, C. (eds) Applied Geology. Encyclopedia of Earth Sciences Series, vol 3. Springer, Boston, MA. https://doi.org/10.1007/0-387-30842-3_39
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