The paper presents the results of studies of sulfde and fuorite veins of the southern fank of the Saf'yanovka massive sulfde deposit, Central Urals. The sulfde veins include sphalerite-galena and sphalerite-pyrite-chalcopyrite types, in which sulfdes are associated with gypsum, carbonates, barite or quartz. Fluorite in host rocks is closely related to carbonates (dolomite, calcite, and siderite), kaolinite and magnesiocarpholite. The sulfde veins differ in chemical composition and rare minerals. In galena-sphalerite veins, the higher Zn, Pb, Cd and Ag content is associated with the presence of sphalerite, galena and tennantite-(Zn) with Ag (up to 1.09 wt %). In sphalerite-pyrite-chalcopyrite veins, the accumulation of Cu, Sn, In, Se, Te and Bi is explained by the presence of tennantite-(Zn), enargite, stannoidite, sakuraiite (?), wittichenite, hessite and Se-bearing galena. The elevated (ppm) Th (1.69) и U (4.79) and REE + Y (447) content is determined in fuorite veins. The REE minerals include fuorcarbonates (synchisite-(Nd) (predominant), synchisite-(Y), synchisite-(Ce) and bastnasite), which are closely associated with overprinted dolomite and kaolinite. The fuid inclusions study of gypsum from pyrite-chalcopyrite veins showed that the associated Cu mineralization formed from H2O-Na-K chloride fuid at temperatures of 210–150 °С. The fuid, which was responsible for the formation of fuorite veins, contained Na, K, Ca и Mg. The formation temperatures of fuorite range from 190 to 280 °С. New data revealed the peculiarities of mineral composition of rich Cu ores with fuorite and also explain the higher content of some elements, including REEs.
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