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Reactivity of organic-rich sediment in seawater at 350°c, 500 bars: experimental and theoretical constraints and implications for the guaymas basin hydrothermal system

Organic GeochemistryMarine GeologyBiogeochemistryEngineeringHydrothermal GeochemistrySediment-water InteractionTheoretical ConstraintsOrganic-rich Sedimentary RockMarine ChemistryGeochemistrySeafloor Hydrothermal SystemSedimentologyEarth ScienceHydrothermal FluidOrganic-rich Sediment