Trace Element Geochemistry of Magnetite and Accesory Phases from El Romeral Iron Oxide-Apatite Deposit, Northern Chile

dc.date.accessioned2019-03-27T15:55:55Z
dc.date.accessioned2022-10-18T22:03:55Z
dc.date.available2019-03-27T15:55:55Z
dc.date.available2022-10-18T22:03:55Z
dc.date.created2019-03-27T15:55:55Z
dc.date.issued2017
dc.identifierhttp://hdl.handle.net/10533/233206
dc.identifier1140780
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4464563
dc.description.abstractIron oxide-apatite (IOA) or “Kiruna-type” deposits are an important source of Fe, P, REE, among other essential elements for society. Three main hypotheses have been proposed to explain the genesis of these controversial deposits, which invoke liquid immi
dc.languageeng
dc.relationinfo:eu-repo/grantAgreement/Fondecyt/1140780
dc.relationAGU (American Geophysical Union) Fall Meeting
dc.rightsinfo:eu-repo/semantics/openAccess
dc.titleTrace Element Geochemistry of Magnetite and Accesory Phases from El Romeral Iron Oxide-Apatite Deposit, Northern Chile
dc.typePonencia


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