Platinum-Group minerals as indicator of sulfur fugacity in ophiolitic upper mantle: an example from chromitites of the Ray-Iz ultramafic complex (Polar Urals, Russia)

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Translated title of the contributionPlatinum-Group minerals as indicator of sulfur fugacity in ophiolitic upper mantle: an example from chromitites of the Ray-Iz ultramafic complex (Polar Urals, Russia)
Original languageEnglish
Pages (from-to)1099-1115
JournalThe Canadian Mineralogist
Volume37
Publication statusPublished - 1999