Sulfide and noble metals mineralization in chromium ores of Lagorta-Kershor area, Voikar-Syninsky massif (Polar Urals)

The results of study sulfide and noble metal mineralization in chrome ores of Lagortia-Kershor area, Voikar-Synya ultrabasic massif are given. Millerite, pentlandite, heazlewoodite, galena, arsenopyrite, cooper sulfides, mineral phases of osmium, ruthenium, iridium and palladium, native metals: gold...

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Bibliographic Details
Main Authors: R. I. Shaybekov, S. K. Kuznetsov, M. M. Gaykovich, S. S. Shevchuk
Format: Article in Journal/Newspaper
Language:English
Russian
Published: A.N. Zavaritsky Institute of Geology and Geochemistry 2015
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Online Access:https://doaj.org/article/9732182b6523488aa3117089460998a0
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Summary:The results of study sulfide and noble metal mineralization in chrome ores of Lagortia-Kershor area, Voikar-Synya ultrabasic massif are given. Millerite, pentlandite, heazlewoodite, galena, arsenopyrite, cooper sulfides, mineral phases of osmium, ruthenium, iridium and palladium, native metals: gold, silver, zinc, copper, iron, nickel are identified and characterized. Formation of sulphide and noble metal mineralization (Au-Pd) occurred mainly in the Late Paleozoic time in connection with hydrothermal-metasomatic (metamorphic) processes. Gold-palladium mineralization superimposed not only on chrome ore, but also on host rocks in faults zones. Voikar-Synya and other ultrabasic massifs of Polar Urals deserve attention and further study of PGE and gold-PGE mineralization.