Features of the Ore Forming Process on the Dvoinoye Epithermal Au–Ag Deposit (Western Chukotka)


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The results of thermobaric geochemical study of ores of the Dvoinoye epithermal Au–Ag deposit are considered. Study of the fluid inclusions has shown that the ores were formed from low-salinity hydrothermal solutions with Na, Ka, and Mg chlorides and CO2, HS, CH4 trace fluxes at the time when the temperature dropped from 370 to 130°C. The results are compared with data obtained from the closely located Kupol and Sentyabr’skoye deposits.

作者简介

E. Kolova

Shilo Northeast Interdisciplinary Scientific Research Institute, Far East Branch

Email: tma2105@mail.ru
俄罗斯联邦, Magadan, 685000

A. Volkov

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

编辑信件的主要联系方式.
Email: tma2105@mail.ru
俄罗斯联邦, Moscow, 119017

N. Savva

Shilo Northeast Interdisciplinary Scientific Research Institute, Far East Branch

Email: tma2105@mail.ru
俄罗斯联邦, Magadan, 685000

V. Prokof’ev

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

Email: tma2105@mail.ru
俄罗斯联邦, Moscow, 119017

A. Sidorov

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

Email: tma2105@mail.ru
俄罗斯联邦, Moscow, 119017

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