Publication | Open Access

Melt hybridization and metasomatism triggered by syn-magmatic faults within the Oman ophiolite: A clue to understand the genesis of the dunitic mantle-crust transition zone

Magmatic ProcessVolcanologyEarth ScienceEngineeringMagmatismIgneous PetrogenesisMelt HybridizationOman OphioliteSyn-magmatic FaultsGeologyCrustal MeltingGeochemistryCrust-mantle InteractionPetrologyTectonics