Geologicheskii Vestnik

The main principles of the thermodegassing method, allowing to determine the temperatures of epigenetic heating and metamorphism of rocks and minerals, are given. The advantages and limitations of this method are evaluated. Paleotemperature studies using the method of thermodegassing of the Lower Permian deposits in the region of Yangantau confirm the idea of a genetic relationship between the thermal manifestations in the region under study with tectonics, and the large energy potential of the Juruzan wrench fault. A conclusion is drawn about the ancient, post — Lower Permian age of these phenomena and the inherited nature of the modern thermal anomaly of Yangantau.

method of thermal degassing, Yangantau, paleotemperature, epigenetic heating

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