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Intracontinental and arc-related hydrothermal systems display distinct δ202Hg and Δ199Hg features: Implication for large-scale mercury recycling and isotopic fractionation in different tectonic settings

EngineeringMercury ChemistryIsotope GeochemistryMercury BiogeochemistryArc-related Hydrothermal SystemsGeologyGeochemistryδ199Hg FeaturesEarth ScienceMagmatic-hydrothermal SystemHydrothermal GeochemistryDistinct δ202HgTectonics