Gold Solubility in Reduced Carbon-Bearing Fluid


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The paper presents first experimental data on gold solubility in CO–CO2 and C–O–S fluids with a low H2O concentration under reduced conditions, a pressure of 200 MPa, and a temperature of 950°C. Gold solubility in C–O–S fluid is approximately 27 ppm. The estimate of gold solubility in CO–CO2 fluid with 10–15 mol % CO is less accurate, and the solubility is no lower than 2–3 ppm but may reach 200–300 ppm. The high gold solubility in reduced CO2 fluid determined in the course of this research, and our earlier estimates of high platinum solubility (Simakin et al., 2016), may explain the deposition of mineralization of these noble metals in the Guli intrusion, polar Siberia, as a result of fluid extraction of these metals and their redeposition at a temperature slightly below the solidus. The reduction of the largely oxidized CO2 fluid, which was determined using mineralogical sensors, was likely related to the subsolidus oxidation of olivine.

作者简介

A. Simakin

Korzhinskii Institute of Experimental Mineralogy (IEM), Russian Academy of Sciences; Schmidt Institute of Physics of the Earth, Russian Academy of Sciences

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Email: simakin@iem.ac.ru
俄罗斯联邦, Chernogolovka, Moscow oblast, 142432; Moscow, 123242

T. Salova

Korzhinskii Institute of Experimental Mineralogy (IEM), Russian Academy of Sciences

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Email: salova@iem.ac.ru
俄罗斯联邦, Chernogolovka, Moscow oblast, 142432

R. Gabitov

Department of Geosciences at Mississippi State University

Email: salova@iem.ac.ru
美国, Oktibbeha County, Mississippi State, MS 39762

L. Kogarko

Vernadsky Institute of Geochemistry and Analytical Chemistry (GEOKhI), Russian Academy of Sciences

Email: salova@iem.ac.ru
俄罗斯联邦, Moscow, 119991

O. Tyutyunnik

Vernadsky Institute of Geochemistry and Analytical Chemistry (GEOKhI), Russian Academy of Sciences

Email: salova@iem.ac.ru
俄罗斯联邦, Moscow, 119991

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