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- W3206147376 abstract "The Late Jurassic orogenic volcanogenic–plutonogenic gold deposit Darasun (the Eastern Transbaikal segment of Mongolo-Okhotsk folded zone) includes postgold ore antimony mineralization. Aggregates of rice-like quartz, minerals of jordanite–geocronite–schultzite, sphalerite, galena, arsenopyrite, tennantite-tetrahedrite, calcite and Mn-Mg siderite are its earlier formations; aggregates of rice-like quartz, low-iron sphalerite, Pb-Sb sulphosalts, antimonite and berthierite are its late formations. The Darasun trend of Pb-Sb sulphosalts sequence from bulangerite to fülöppite is typical for post-magmatic hydrothermal gold deposits and differs from telethermal ones. The are two fülöppite types in Darasun ores: fülöppite enriched in arsenic (up to 7,5 %wt), which is probably the product of replacement of geocronite and fahl ore row minerals and fülöppite without arsenic associating with antimonite and calcite. The arsenic-bearing fülöppite composition is (Pb 2.90 Ag 0.06 Cu 0.05 ) 3.01 (Sb 7.05 As 0.91 Bi 0.04 ) 8.00 S 14.99 and the composition of fülöppite without arsenic is (Pb 2.83 Cu 0.18 ) 3.01 Sb 7.98 S 15.01 , which are close to stoichiometry. Darasun fülöppite is characterized by positive correlation of As, Bi and Ag; füloppite without arsenic is enriched in copper." @default.
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- W3206147376 date "2020-10-28" @default.
- W3206147376 modified "2023-10-18" @default.
- W3206147376 title "Fülöppite Pb<sub>3</sub>Sb<sub>8</sub>S<sub>15</sub> of volcanogenic plutonogenic Darasun gold deposit, Eastern Transbaikal" @default.
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- W3206147376 doi "https://doi.org/10.33623/0579-9406-2020-5-71-76" @default.
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