Oxygen fugacity range of subducting crust inferred from fractionation of trace elements during fluid-present slab melting in the presence of anhydrite versus sulfide
Proteek Chowdhury, Rajdeep Dasgupta, Patrick R. Phelps, Gelu Costin, Cin‐Ty A. Lee
Topics & Concepts
GeologyMineral redox bufferGeochemistrySlabSulfideAnhydriteFractionationCrustFugacitySilicicMineralogyPetrologyMantle (geology)GeophysicsChemistryVolcanoMaterials scienceMetallurgyGypsumOrganic chemistryPhysical chemistryPaleontologyGeological and Geochemical AnalysisMetallurgical Processes and ThermodynamicsGeochemistry and Geologic Mapping