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Peculiarities of Ore Formation at the Teploe Ag–Au Deposit, Northeast Russia

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Abstract

The mineralogical–geochemical and thermobarogeochemical features of the Teploe Ag–Au epithermal deposit are considered. The dissolution and redeposition of ore minerals are a result of thermal metamorphism. The redistribution of Ag leads to the formation of lenaite and exsolution structures in minerals of the Cu–Ag–S system; abundant stromeyerite, jalpaite, and mckinstryite compose a significant amount of ores. The atypical physicochemical parameters of the formation of ores include high (for epithermal mineralization) temperatures and low salinity and density of the fluid typical of a dry vapor. The results of fluid inclusion study ascribe the Teploe deposit to an intermediate class of epithermal deposits.

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Correspondence to A. V. Volkov.

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Original Russian Text © A.V. Volkov, N.E. Savva, E.E. Kolova, A.A. Sidorov, 2018, published in Doklady Akademii Nauk, 2018, Vol. 481, No. 3.

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Volkov, A.V., Savva, N.E., Kolova, E.E. et al. Peculiarities of Ore Formation at the Teploe Ag–Au Deposit, Northeast Russia. Dokl. Earth Sc. 481, 869–872 (2018). https://doi.org/10.1134/S1028334X18070310

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  • DOI: https://doi.org/10.1134/S1028334X18070310

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