Closed-system behaviour of the Re-Os isotope system recorded in primary and secondary platinum-group mineral assemblages: Evidence from a mantle chromitite at Harold's Grave (Shetland Ophiolite s{cyrillic}omplex, Scotland): Closed-system behaviour of the Re–Os isotope system recorded in primary and secondary platinum-group mineral assemblages: Evidence from a mantle chromitite at Harold's Grave (Shetland Ophiolite Сomplex, Scotland)
Research output: Contribution to journal › Article › Research › peer-review
Authors
Organisational units
External Organisational units
- Institute of Geology and Geochemistry Ural Division of Russian Academy of Sciences
- Macquarie University
- University of Strathclyde
Details
| Original language | English |
|---|---|
| Pages (from-to) | 174-185 |
| Number of pages | 12 |
| Journal | Ore geology reviews |
| Volume | 75.2016 |
| Issue number | June |
| DOIs | |
| Publication status | Published - 1 Jun 2016 |
