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Sulfur dissolution capacity of highly hydrated and fluid-saturated dacitic magmas at the lower crust and implications for porphyry deposit formation

Magmatic ProcessVolcanologyEarth ScienceSulfur Dissolution CapacityEngineeringMagmatismIgneous PetrogenesisFluid-saturated Dacitic MagmasGeologyGeochemistryIgneous ProcessPorphyry Deposit FormationPetrologyMagmatic-hydrothermal SystemTectonics