Massive Iron Oxide-Apatite (IOA) Deposit Formation by Efficient Flotation of Magmatic Magnetite Suspensions: A Genetic Link Between IOA and IOCG Deposits?

dc.date.accessioned2019-03-27T15:55:53Z
dc.date.accessioned2022-10-18T22:03:47Z
dc.date.available2019-03-27T15:55:53Z
dc.date.available2022-10-18T22:03:47Z
dc.date.created2019-03-27T15:55:53Z
dc.date.issued2015
dc.identifierhttp://hdl.handle.net/10533/233189
dc.identifier1140780
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4464546
dc.description.abstractThe link between iron oxide-apatite (IOA, or “Kiruna-type”) and iron oxide-copper-gold (IOCG) deposits remains controversial. Based on geochemical and isotopic data of magnetite from the Los Colorados IOA deposit in northern Chile, we report compelling ev
dc.languageeng
dc.relation14°
dc.relationinfo:eu-repo/grantAgreement/Fondecyt/1140780
dc.relationCongreso Geológico Chileno
dc.rightsinfo:eu-repo/semantics/openAccess
dc.titleMassive Iron Oxide-Apatite (IOA) Deposit Formation by Efficient Flotation of Magmatic Magnetite Suspensions: A Genetic Link Between IOA and IOCG Deposits?
dc.typePonencia


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