Publication | Open Access

Fluids in the peridotite–water system up to 6 GPa and 800°C: new experimental constrains on dehydration reactions

Dehydration ReactionsChemical EngineeringFluid PropertiesEngineeringMineral-fluid InteractionNew Experimental ConstrainsPeridotite–water SystemGeochemistryThermodynamicsChemistryHigh Temperature GeochemistryWater-rock InteractionChemical KineticsFluid Geochemistry