Fahlore and Sphalerite from the Darasun Gold Deposit in the Eastern Transbaikal Region, Russia: II. Fe and Zn Partitioning, Fluid Inclusions, and Formation Conditions
- 作者: Lyubimtseva N.G.1, Bortnikov N.S.1, Borisovsky S.E.1, Prokofiev V.Y.1, Vikent’eva O.V.1
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隶属关系:
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
- 期: 卷 60, 编号 3 (2018)
- 页面: 220-240
- 栏目: Article
- URL: https://journals.rcsi.science/1075-7015/article/view/215329
- DOI: https://doi.org/10.1134/S1075701518030054
- ID: 215329
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详细
The partitioning of Fe and Zn between coexisting fahlore and sphalerite and fluid inclusions in sphalerite from the Darasun gold deposit have been studied. These data were used to estimate the formation temperature of the minerals by the sphalerite–fahlore geothermometer. The calculated crystallization temperature of 175–355°С is close to the homogenization temperature of fluid inclusions in sphalerite of 225–385°С.The estimated pressure for fluid inclusion trapping ranged from 340 to 1420 bar. The sulfur fugacity obtained from the FeS content in sphalerite associated with pyrite and the calculated temperature ranges from 10–5.5 to 10–11 bar.
作者简介
N. Lyubimtseva
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
编辑信件的主要联系方式.
Email: luy-natalia@yandex.ru
俄罗斯联邦, Moscow, 119017
N. Bortnikov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: luy-natalia@yandex.ru
俄罗斯联邦, Moscow, 119017
S. Borisovsky
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: luy-natalia@yandex.ru
俄罗斯联邦, Moscow, 119017
V. Prokofiev
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: luy-natalia@yandex.ru
俄罗斯联邦, Moscow, 119017
O. Vikent’eva
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: luy-natalia@yandex.ru
俄罗斯联邦, Moscow, 119017
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