Geochemistry and iron isotope systematics of coexisting Fe
nbsp 0183 32 Geochemical and iron isotopic compositions of magnetite ilmenite and pyrite separates from the Fe Ti oxide ores hosted in the Damiao anorthosite type Fe Ti ore deposit were analyzed to investigate sub solidus cooling history of the titanomagnetite The Fe Ti oxides form two series of solid solutions namely ulv 246 spinel magnetite Usp Mt ss and hematite ilmenite Hem Ilm ss solid solutions
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