Annotation
The natural magnetic states of rock have been studied and compared with a zero initial state. Rocks are usually in nonequilibrium states. The deviation from equilibrium depends on the temperature at which the natural remnant magnetization was formed and on the time which has elapsed since the rock formation.
© 2016 Publisher M.V.Lomonosov Moscow State University
Authors
V.I. Trukhin
Department of Physics of the Earth
Department of Physics of the Earth
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