Abstract
The mineral composition of rock samples of the Zarechenskaya and Nikolskaya magnetic anomalies was determined. The mineral composition was compared with the magnetic properties of rocks, such as inductive and remanent magnetization, Curie temperature, anisotropy of magnetic susceptibility, and the Koenigsberg factor. The influence of the mineral composition on the magnetic properties of rocks is considered. This, in turn, will further increase the reliability of the interpretation of the results of tectonomagnetic monitoring performed here.
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