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Mineral-aqueous fluid partitioning of trace elements at 900°C and 2.0 GPa: Constraints on the trace element chemistry of mantle and deep crustal fluids

Mantle GeochemistryEngineeringTrace Element GeochemistryMineral-aqueous Fluid PartitioningTrace Element ChemistryGeologyGeochemistryChemistryCrust-mantle InteractionEarth ScienceTrace Elements