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REGULARITIES IN THE DISTRIBUTION OF NONFERROUS AND PRECIOUS METALS IN PRINCIPAL ORE MINERALS AND SILICATES OF THE NORIL'SK DEPOSITS
Abstract:The results of a study of copper, nickel, cobalt, platinum, palladium, gold, and rhodium distribution in basic ore-forming sulfide minerals (chalcopyrite and pyrrhotites) as well as in the silicate portion of the host rocks of the Noril'sk deposit, are given. Interrelations between metals in different sulfide minerals and silicates are characterized. It has been established that palladium, platinum, and gold are concentrated in chalcopyrite while cobalt and rhodium are concentrated in pyrrhotite. The cobalt and precious metal content in sulfides grows with the increase of their nickel content. The relative content, however, of all these elements estimated for 1% of nickel is different in chalcopyrites and pyrrhotites. The former show a high platinum, palladium, and gold content and the latter--cobalt and rhodium. Ratios of these elements in sulfides and silicates are different. The relative platinum content increases in silicates due to a considerably greater content of mineralized platinum. Both nickel and cobalt form silicate compounds the latter to a much greater extent than the former. The relative cobalt content is therefore higher in silicates than in sulfides. In descending order, the element concentrations in sulfides range as follows: copper, nickel, palladium, gold, cobalt, platinum. — Auth. English Summ.
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