Analysis reveals magnetic heterogeneity and mineral composition in Blagodatnoye deposit, indicating hydrothermal evolution patterns.
The history of the geodynamic development of the Yenisei Ridge from the perspective of the supercontinental cycles is briefly illuminated. The geological structure of the Blagodatnoye gold-sulfide deposit, and the stages of its hydrothermal-metasomatic evolution are described. The magnetic structure of the mineralized zone is characterized in detail. The relationship of pyrite and pyrrhotite compositions with the magnetic heterogeneity of pyrite-pyrrhotite paragenesis and the distribution of gold mineralization in the ore zone has been established.
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Fedorov et al. (2025) studied this question.
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