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Disequilibrium iron isotopic fractionation during the high-temperature magmatic differentiation of the Baima Fe–Ti oxide-bearing mafic intrusion, SW China

Magmatic ProcessVolcanologyEarth ScienceEngineeringSw ChinaMagmatismIgneous PetrogenesisGeologyGeochemistryHigh Temperature GeochemistryPetrologyMagmatic-hydrothermal SystemHigh-temperature Magmatic DifferentiationTectonics