First Find Of Pge Minerals In Sulfide Ores Related To Ultrabasic Rocks Of The Iisk-kuksher Trough, southern Siberia

摘要

PGE minerals are additional indicators of genesis of ultrabasic rocks and conditions of formation of associated sulfide-nickel ores. Their composition and assemblages can be used to estimate the composition of parent magmas, their fluid regime, and stages of ore formation. In addition, the presence of PGE minerals significantly increases the economic significance of the mineralization.