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 language | English |
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Pages (from-to) | 1-5 |
Number of pages | 5 |
Journal | Scottish Journal of Geology |
Volume | 40 |
DOIs | |
Publication status | Published - 2004 |
Keywords
- OPHIOLITE COMPLEX
- PGE
- FRACTIONATION
- CHROMITITE
- MANTLE
- ORIGIN
- GREECE
- RICH