Platinum-group minerals within the Ballantrae Complex, SW Scotland

M. R. Power, D Pirrie

    Research output: Contribution to journalArticlepeer-review

    Abstract

    Platinum-group minerals (PGM) are present within the chromitites of the northern serpentinite belt (Pinbain Bridge area) of the ophiolitic Ballantrae Complex. A relatively uncommon but moderately diverse PGM assemblage is dominated by small (

    Original languageEnglish
    Pages (from-to)1-5
    Number of pages5
    JournalScottish Journal of Geology
    Volume40
    DOIs
    Publication statusPublished - 2004

    Keywords

    • OPHIOLITE COMPLEX
    • PGE
    • FRACTIONATION
    • CHROMITITE
    • MANTLE
    • ORIGIN
    • GREECE
    • RICH

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