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Fe–Mg diffusion in olivine I: experimental determination between 700 and 1,200°C as a function of composition, crystal orientation and oxygen fugacity

Materials ScienceInorganic ChemistryMagnetic PropertiesEngineeringOxygen FugacityMineral-fluid InteractionCrystal OrientationGeochemistryChemistryFe–mg DiffusionMineral Geochemistry