Russian Journal of Earth Sciences Russian Journal of Earth Sciences Russian Journal of Earth Sciences 1681-1208 47167 ОРИГИНАЛЬНЫЕ СТАТЬИ ORIGINAL ARTICLES ОРИГИНАЛЬНЫЕ СТАТЬИ Temperature benchmarks in the lithosphere, marking the phase transformations of the matter, and the possibilities of estimating their depths Temperature benchmarks in the lithosphere, marking the phase transformations of the matter, and the possibilities of estimating their depths Yakupov V S Yakupov V S Yakupov S V Yakupov S V Mining Research Institute for the Northern Territories, Siberian Division, Russian Academy of Sciences, Yakutsk, Russia ru Mining Research Institute for the Northern Territories, Siberian Division, Russian Academy of Sciences, Yakutsk, Russia ru Mining Research Institute for the Northern Territories, Siberian Division, Russian Academy of Sciences, Yakutsk, Russia ru Mining Research Institute for the Northern Territories, Siberian Division, Russian Academy of Sciences, Yakutsk, Russia ru 3 4 311 315 11 11 2021 https://rjes.ru/en/nauka/article/47167/view

Extensive research into temperature distribution in the lithosphere and upper mantle revealed it to be highly ambiguous. Of great interest in this context is the distribution of temperature benchmarks in the lithosphere, which mark phase transitions in the individual components of rocks and in the fluids filling their pores. As follows from the percolation theory, the physical properties of the rocks change jumpwise at the discontinuities produced by their phase transformations. This simplifies the interpretation of magnetotelluric and other electrical measurements, enhances the reliability of its results, and facilitates the use of radiolocation, especially in the case of relatively shallow discontinuities. The discontinuities may not coincide in terms of percolation and mechanical conpling, this explaining differences in the results of electrical and seismic measurements.

Extensive research into temperature distribution in the lithosphere and upper mantle revealed it to be highly ambiguous. Of great interest in this context is the distribution of temperature benchmarks in the lithosphere, which mark phase transitions in the individual components of rocks and in the fluids filling their pores. As follows from the percolation theory, the physical properties of the rocks change jumpwise at the discontinuities produced by their phase transformations. This simplifies the interpretation of magnetotelluric and other electrical measurements, enhances the reliability of its results, and facilitates the use of radiolocation, especially in the case of relatively shallow discontinuities. The discontinuities may not coincide in terms of percolation and mechanical conpling, this explaining differences in the results of electrical and seismic measurements.

 lithosphere phase transformations temperature benchmarks magnetotelluric measurements. lithosphere phase transformations temperature benchmarks magnetotelluric measurements.

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