Abstract
New data are obtained on the age of the epithermal gold-silver mineralization of the Kubaka deposit (Omolon Massif, Northeast Russia). Our geological observations in the open-pit mine of the Zokol zone of the deposit allow us to conclude that the mineralization formed between the eruptions of Upper Devonian ore-hosting volcanites of the Kedon series (zircon U-Pb age ~ 370 ± 2.5 Ma, SHRIMP) and Lower-to-Middle Jurassic trachybasalts and picrobasalts of the Omolon Complex (40Ar/39Ar plateau age of 179 ± 8 Ma) without the vein penetrating into the Carboniferous Corba Formation. The 40Ar/39Ar plateau age for a white adularia from the productive quartz vein yielded 299 ± 3.5 Ma (MSWD = 0.91, p = 0.43, 66% of 39Ar released in four steps). Our results contradict a commonly accepted concept of “polychronous” ore formation (during the Carboniferous and Cretaceous) or long-term mineralization at the Kubaka deposit, and likely indicate a high probability of at least an Upper Carboniferous upper age limit of epithermal gold mineralization.
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ACKNOWLEDGMENTS
We would like to thank A.A. Sorokin and A.V. Prokopiev for positive reviews and useful comments.
Funding
The studies were supported by the Program “Far East”, grant 18-2-015, and were performed within the State Assignment for NEISRI FEB RAS using NIR no. AAAA-A17-117022850033-6 theme.
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Recommended for publishing by A.A. Sorokin
Translated by N. Kovriga
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Akinin, V.V., Glukhov, A.N., Polzunenkov, G.O. et al. The Age of the Kubaka Epithermal Gold-Silver Deposit (Omolon Massif, Northeast Russia): Geological and Isotopic-Geochronological Constrains (U-Pb and 40Ar/39Ar Methods). Russ. J. of Pac. Geol. 14, 32–42 (2020). https://doi.org/10.1134/S1819714020010029
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DOI: https://doi.org/10.1134/S1819714020010029