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

dc.creatorBarra-Pantoja, Luis Fernando
dc.creatorRojas, Paula A
dc.creatorReich, Martín
dc.creatorDeditius, Artur
dc.creatorSimon, Adam
dc.date2019-03-27T15:55:55Z
dc.date2022-06-18T19:22:54Z
dc.date2019-03-27T15:55:55Z
dc.date2022-06-18T19:22:54Z
dc.date2017
dc.date2017
dc.date2017
dc.date.accessioned2023-08-22T05:14:52Z
dc.date.available2023-08-22T05:14:52Z
dc.identifier1140780
dc.identifierhttps://hdl.handle.net/10533/233206
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/8323345
dc.descriptionIron 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.descriptionFONDECYT
dc.descriptionFONDECYT
dc.languageeng
dc.relationAGU (American Geophysical Union) Fall Meeting
dc.relationinfo:eu-repo/grantAgreement/Fondecyt/1140780
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
dc.coverageParis


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