Geochemistry and iron isotope systematics of coexisting Fe-bearing minerals in magmatic Fe Ti deposits: A case study of the Damiao titanomagnetite ore deposit, North China Craton

Volume: 81, Pages: 240 - 251
Published: May 1, 2020
Abstract
Geochemical and iron isotopic compositions of magnetite, ilmenite and pyrite separates from the FeTi oxide ores hosted in the Damiao anorthosite-type FeTi ore deposit were analyzed to investigate sub-solidus cooling history of the titanomagnetite. The FeTi oxides form two series of solid solutions, namely, ulvöspinel-magnetite (Usp-Mtss) and hematite-ilmenite (Hem-Ilmss) solid solutions. The magnetite separates have 14–27 mol% ulvöspinel, while...
Paper Details
Title
Geochemistry and iron isotope systematics of coexisting Fe-bearing minerals in magmatic Fe Ti deposits: A case study of the Damiao titanomagnetite ore deposit, North China Craton
Published Date
May 1, 2020
Volume
81
Pages
240 - 251
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