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 contribution | 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) |
|---|---|
| Original language | English |
| Pages (from-to) | 1099-1115 |
| Journal | The Canadian Mineralogist |
| Volume | 37 |
| Publication status | Published - 1999 |
