Features of the Ore Forming Process on the Dvoinoye Epithermal Au–Ag Deposit (Western Chukotka)
- 作者: Kolova E.E.1, Volkov A.V.2, Savva N.E.1, Prokof’ev V.Y.2, Sidorov A.A.2
-
隶属关系:
- Shilo Northeast Interdisciplinary Scientific Research Institute, Far East Branch
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
- 期: 卷 478, 编号 2 (2018)
- 页面: 166-170
- 栏目: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/192150
- DOI: https://doi.org/10.1134/S1028334X18020149
- ID: 192150
如何引用文章
详细
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
补充文件
