| Abstract: |
Abstract: Mineral composition of chromitites and host serpentinites from a quarry at Mt. Poklonnaya of the Karabash serpentinite massif is studied using optical and electron microscopy. Along with previously known native osmium and laurite, eight minerals of platinum group elements (MPG) are found. Among them are isoferroplatinum, irarsite, iridium, naldrettite, cuproiridsite, sperrylite, tolovkite, and erlichmannite. It is found that magnesioalumochromite is an early magmatic Cr-spinel, while magnesiochromite and ferrichromite are late magmatic. The earliest native iridium and native osmium are replaced by platinum-group-elements sulfides, arsenides and stibnides. Magnesiochromite is associated with native gold, Ni chalcohenides (gersdorffite, millerite, pentlandite, heaslewoodite) and chalcopyrite. The formation of Cr-magnetite, magnetite, native iron, native nickel, galena, and barite is related to serpentinization. Carbonates (calcite and dolomite), brucite, andradite, sepiolite and an unidentified Ca-silicate formed at the latest stage of serpentinization. Secondary Ni minerals (gaspeite, nepuite, “garnierite”) are most likely products of the latest mineral-forming process. |
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