Abstract
The article presents the results of a comparative analysis of fluorite from various mineralization types of the Saf’yanovka massive sulfide deposit in the Central Urals. The predominant green fluorite is intergrown with barite, quartz, and carbonates in hydrothermal colloform and massive pyrite, veinlet–disseminated chalcopyrite–pyrite–sphalerite and pyrite–chalcopyrite ores, as well as in hydrothermally altered rhyolite. In colloform pyrite ore, fluorite together with galena, sphalerite, chalcopyrite, fahlore, and barite fills interstices between crystals. In altered rhyolite, yellow-green fluorite occurs as veins of 1 cm thick, 2–3 cm pockets, and intergrowths with quartz, carbonate, and barite. The rare-earth element (REE) and yttrium concentrations have been determined by ICP-MS. The highest Y content (160 ppm) is measured in fluorite from metasomatic rock; the intermediate Y content (40–130 ppm) is determined in fluorite from pyrite ore, and the lowest one (4–9 ppm) is typical of fluorite from chalcopyrite–pyrite–sphalerite and chalcopyrite ore. The total REE content in fluorite is 70–150 ppm (chalcopyrite–pyrite–sphalerite and chalcopyrite ore), 100–280 ppm in pyrite ore, and reaches 180 ppm in altered rhyolites. The highest REE concentration is caused by the presence of xenotime, goyazite, monazite, barite or apatite inclusions in fluorite. The Tb/La and Tb/Ca ratios suggest that fluorite resulted from hydrothermal processes. The REE distribution patterns with an evident Eu anomaly (Eu/Eu* > 1) show enrichment in LREE. Positive Eu anomalies reflect the high-temperature conditions (≥250°C) during fluorite crystallization. The pressure-corrected (~100–150 bar) temperature of fluorite formation is 190–260°С.
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Report on prospecting work to assess the economic significance of the Kamenskaya Safyanovskaya copper ore zone of the East Ural basin OJSC SUGRE.
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ACKNOWLEDGMENTS
We thank N.V. Leshchev, chief geologist of OAO Saf’yanmed for his assistance in field work; E.V. Belogub and M.E. Pritchin for the samples kindly placed at our disposal; L.V. Leonova for analytical study; and I.Yu Melekestseva for discussion of the results obtained.
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This study was supported under a state task (state registration no. AAAA-A19-119061790049-3).
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Safina, N.P., Soroka, E.I., Ankusheva, N.N. et al. Fluorite in Ores of the Saf’yanovka Massive Sulfide Deposit, Central Urals: Assemblages, Composition, and Genesis. Geol. Ore Deposits 63, 118–137 (2021). https://doi.org/10.1134/S1075701521020057
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DOI: https://doi.org/10.1134/S1075701521020057