Abstract
Basaltic rocks contain magnetic grains oriented randomly in a nonmagnetic matrix. Experimental studies of low-field hysteresis of such rocks have shown partially and totally constricted hysteresis loops for some specimens. A possible origin of these constricted loops on the basis of interacting single domain behaviour is suggested.
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Communicated by Prof. D. Lal,f.a.sc.
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Radhakrishnamurty, C., Sastry, N.P. A single domain grain model for the low-field constricted hysteresis loops of some basaltic rocks. Proc. Indian Acad. Sci. 72, 94–102 (1970). https://doi.org/10.1007/BF03050410
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DOI: https://doi.org/10.1007/BF03050410