Multi-scale development of a stratiform chromite ore body at the base of the dunitic mantle-crust transition zone (Maqsad diapir, Oman ophiolite): The role of repeated melt and fluid influxes
| Autor: | Rospabé, Mathieu, Ceuleneer, Georges, Granier, Nicolas, Arai, Shoji, Borisova, Anastassia Y. |
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| Zdroj: | In LITHOS 15 December 2019 350-351 |
| Databáze: | ScienceDirect |
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