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- W2783287152 abstract "In the paper, there are adduced the data of a thermobarogeochemistry investigation of fluid inclusions in apatite of magnetite-chlorite-carbonates rocks from ultrabasite Karabash massife. The rocks are carrying copper-bearing aurum (1.3-2.6 wt % Cu) and was formed at temperature in the range of 480-280°C and a pressure of about 2-3 kbar. The content of the inclusions corresponds to the salt system of H 2 O-NaCl and the salt concentration in the solution 3.7-8.8 wt % eq. NaCl. Fluids gas components, extraction by pirolysis up to temperature 450°C, are described by a system C-H-O with an insignificantly amount of nitrogen. In fluid composition presents a small amount of the reduced gasses - CO, H 2 , CH 4 , hard carbon-hydrates (C 2 H 4 , C 2 H 6 , C 3 H 6 , C 3 H 8 etc.). Adduced comparative analysis of fluid composition and the degree of oxidation fluid gas component (O fl = CO 2 /(CO 2 + CO + H 2 + CH 4 ) during the forming magnetite-chlorite-carbonate rocks, the rodingites and the listwenites. It is established, that carbon acid part of mole in fluid (X CO2 ) grown from extremely low value by the forming of rodingites with copper-bearing aurum ( CO2 . In the same time, reduction regime of the forming rodingites (O fl = 0.14-0.35) is replaced on oxidation one by the forming of magnetite-chlorite-carbonate rocks (O fl = 0.73-0.92), calcite veinlets, in the rodingites (O fl = 0.83) and also the listwenites (O fl = 0.77)." @default.
- W2783287152 created "2018-01-26" @default.
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- W2783287152 date "2017-01-01" @default.
- W2783287152 modified "2023-09-25" @default.
- W2783287152 title "Physic-chemical conditions of gold-bearing magnetite-chlorite-carbonate roks' formation of the Karabash ultramafic massif (the Southern Urals)" @default.
- W2783287152 doi "https://doi.org/10.24930/1681-9004-2017-6-110-117" @default.
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