Abstract
Igneous rocks are shown to possess a magnetic fabric that admits the occurrence of giant Barkhausen jumps. It is also demonstrated that magnetic minerals of rocks can preserve information on a few magnetic fields (differing even in origin) and a few thermal magnetization temperatures.
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Original Russian Text © V.S. Vechfinskii, S.S. Solov’eva, O.V. Gusev, 2008, published in Fizika Zemli, 2008, No. 3, pp. 92–96.
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Vechfinskii, V.S., Solov’eva, S.S. & Gusev, O.V. Giant Barkhausen jumps in Kamchatka basaltic lavas. Izv., Phys. Solid Earth 44, 256–259 (2008). https://doi.org/10.1134/S1069351308030099
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DOI: https://doi.org/10.1134/S1069351308030099