The Co-Ni signature of sulfide minerals from the Mantoverde IOCG deposit, northern Chile

dc.creatorJohansson, Cinthia
dc.creatorBarra-Pantoja, Luis Fernando
dc.creatorReich, Martín
dc.creatorDeditius, Artur P
dc.creatorSimon, Adam C
dc.creatorRojas, Paula A
dc.date2019-03-27T15:55:54Z
dc.date2022-06-18T19:22:34Z
dc.date2019-03-27T15:55:54Z
dc.date2022-06-18T19:22:34Z
dc.date2017
dc.date2017
dc.date2017
dc.date.accessioned2023-08-22T09:27:48Z
dc.date.available2023-08-22T09:27:48Z
dc.identifier1140780
dc.identifierhttps://hdl.handle.net/10533/233200
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/8336383
dc.descriptionIron Oxide Copper Gold (IOCG) deposits are an important source of Cu and other elements such as Au, Ag, REE, U, P and Co. Although these deposits are economically important, their modes of origin remain controversial and two main genetic models have been
dc.descriptionFONDECYT
dc.descriptionFONDECYT
dc.languageeng
dc.relationGoldschmidt
dc.relationinfo:eu-repo/grantAgreement/Fondecyt/1140780
dc.rightsinfo:eu-repo/semantics/openAccess
dc.titleThe Co-Ni signature of sulfide minerals from the Mantoverde IOCG deposit, northern Chile
dc.typePonencia
dc.coverageParis


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