Email this article Energy Parameters of Ore-Forming Deep Fluid Systems
- Authors: Letnikov F.A.1, Danilov B.S.1, Letnikova A.F.2
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Affiliations:
- Institute of the Earth’s Crust, Siberian Branch
- Irkutsk State University
- Issue: Vol 481, No 1 (2018)
- Pages: 877-878
- Section: Geology
- URL: https://journals.rcsi.science/1028-334X/article/view/193582
- DOI: https://doi.org/10.1134/S1028334X18070255
- ID: 193582
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Abstract
The energy parameters of ore-forming deep fluid systems (enthalpy and Gibbs free energy) for compounds of S, Cl, and B have been estimated by thermodynamic methods at a lithosphere depth of 1000–20 km. At a depth of 1000 km, ore-forming fluids are dominated by BF3. With a decrease in a depth to 100–20 km, the range of fluid ore-forming systems becomes wider due to the B, F, Cl, and S compounds providing a real basis for development of the voluminous ore-forming fluid systems at the top of the lithosphere.
About the authors
F. A. Letnikov
Institute of the Earth’s Crust, Siberian Branch
Email: let_an@mail.ru
Russian Federation, Irkutsk, 664033
B. S. Danilov
Institute of the Earth’s Crust, Siberian Branch
Email: let_an@mail.ru
Russian Federation, Irkutsk, 664033
A. F. Letnikova
Irkutsk State University
Author for correspondence.
Email: let_an@mail.ru
Russian Federation, Irkutsk, 664003
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