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
Authors:
- Mathieu RospabéMRMathieu Rospabé
- Georges CeuleneerGCGeorges Ceuleneer
- Nicolas GranierNGNicolas Granier
- Shoji AraiSAShoji Arai
- Anastassia Y. BorisovaAnastassia Y. Borisova
Abstract
No abstract availableKeywords
Funding Information
- Centre National de la Recherche Scientifique
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