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This study reports elemental and iron isotopic compositions of feldspar and its coexisting minerals from four Dabie I-type granitoids to evaluate the factors that control inter-mineral Fe isotopic fractionation in granitoids. The order of heavy iron isotope enrichment is feldspar>pyrite>magnetite>biotite≈hornblende. Feldspar has heavier iron isotopic compositions than its co-existing magnetite...
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