New data on the formation conditions of the Golets Vysochaishiy gold deposit (Bodaibinskiy district, Russia)
https://doi.org/10.33623/0579-9406-2021-6-70-76
Abstract
The Golets Vysochaishy deposit has a sub-tabular orebody hosted by black carbonaceous fine-grained aleuropelitic rocks. We have studied fluid inclusions in quartz samples taken from sulfide-quartz veins in the ore zone of the deposit — performed studies made it possible to establish the parameters of the ore-forming fluid. Thus, the fluids of the deposit are characterized by the typical features of orogenic vein gold deposits’ ore-forming fluids. The process of carbon dioxide degassing from the fluid may have contributed to the deposition of native gold.
About the Authors
M. A. Boguslavskiy
Lomonosov Moscow State University
Russian Federation
Russian Federation
119991, Moscow, GSP-1, Leninskiye Gory, 1
V. D. Sagalevich
Lomonosov Moscow State University
Russian Federation
Russian Federation
119991, Moscow, GSP-1, Leninskiye Gory, 1
V. Yu. Prokofiev
Institut geologii rudnykh mestorozhdeniy, Petrografi i, Mineralogii, Geokhimii RAS
Russian Federation
Russian Federation
119017, Moscow, Staromonetniy pereulok, 35
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Review
For citations:
Boguslavskiy M.A., Sagalevich V.D., Prokofiev V.Yu. New data on the formation conditions of the Golets Vysochaishiy gold deposit (Bodaibinskiy district, Russia). Moscow University Bulletin. Series 4. Geology. 2021;1(6):70-76. (In Russ.) https://doi.org/10.33623/0579-9406-2021-6-70-76
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