Speciation of noble metals and conditions of their concentration in massive sulfide ores of the Urals

• Published in: Geology of ore deposits 2006-03, Vol.48 (2), p.77-107, Article 77
• Main Authors: Vikent’ev, I. V., Moloshag, V. P., Yudovskaya, M. A.
• Format: Article
• Language: English
• Subjects: Admixtures; Argentite; Chalcopyrite; Chemical separation; Chromatography; Concentrates (ores); Copper; Dispersion; Epigenetics; Fluid inclusions; Gold; Heavy metals; Hydrothermal alteration; Intermetallic compounds; Metal concentrations; Metals; Minerals; Noble metals; Ores; Pyrite; Recrystallization; Speciation; Sphalerite; Sulfide; Sulfides; Sulfur; Sulphides; Sulphur; Tellurides; Tellurium; X rays; Zincblende
• ISSN: 1555-6476; 1075-7015; 1555-6476
• DOI: 10.1134/s1075701506020012

The distribution of noble metals has been studied in ores and sulfide concentrates from the Gai, Uchaly, Uzel’ga, Aleksandrinsky, Degtyarsk, and Saf’yanovka deposits. The ores, technological products, and hand-picked monofractions were analyzed with INAA; PGE were determined with kinetic and chromatographic methods after their preliminary chemical separation. The ultraheavy fractions from Au-rich samples were used for examining minerals of noble metals. Phase relations and compositions of ore minerals were studied with an X-ray microprobe and electron microscope equipped with an energy dispersive X-ray analyzer. Gold is associated largely with Fe and Cu minerals (pyrite, chalcopyrite, fahlore) and has been detected as an admixture in Pb, Bi, and Ag tellurides. Pyrite—the major mineral of massive sulfide ores—is the main gold concentrator (up to 20 ppm, ∼1 ppm on average). As follows from the results of rational analysis, the concentration of finely dispersed gold in sulfide ores from the studied deposits ranges from 0.8 to 5.0 ppm, i.e., is less than the bulk Au content in the respective samples (0.93–21.2 ppm). Formation conditions of Au-enriched massive sulfide ores were estimated from the homogenization temperature of fluid inclusions in minerals and on the basis of the electrum-argentite-pyrite-sphalerite and electrum-hessite geothermometers, taking into account the sulfur and tellurium fugacities. The appearance of visible gold and tellurides in ores is caused by recrystallization of their fine-grained intergrowths with ore-forming minerals and, likely, by release of isomorphic admixtures contained in sulfides during epigenetic hydrothermal alteration.