Show simple item record

dc.creatorReich, M.
dc.creatorDeditius, A.
dc.creatorChryssoulis, S.
dc.creatorLi, J. W.
dc.creatorMa, C. Q.
dc.creatorParada, M. A.
dc.creatorBarra, F.
dc.creatorMi ttermayr, F.
dc.date.accessioned2020-03-11T20:26:38Z
dc.date.available2020-03-11T20:26:38Z
dc.date.issued2013
dc.identifier.urihttp://hdl.handle.net/10533/238079
dc.description.abstractPorphyry copper deposits are currently the world’s largest source of copper and molybdenum, and are also among the largest reservoirs of gold in the upper crust. Despite the fact that pyrite is a ubiquitous mineral phase in these deposits and secondary Cu
dc.language.isoeng
dc.relation.urihttps://doi.org/10.1016/j.gca.2012.11.006
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Chile
dc.rightshttp://creativecommons.org/licenses/by-nc-nd/3.0/cl/
dc.titlePyrite as a record of hydrothermal fluid evolution in a porphyry copper system: A SIMS/EMPA trace element study.
dc.typeArticulo
dc.identifier.folio15090013
dc.description.conicytprogramFONDAP
dc.rights.driverinfo:eu-repo/semantics/openAccess
dc.title.journalGeochimica et Cosmochimica Acta
dc.type.driverinfo:eu-repo/semantics/article
dc.description.shortconicytprogramFONDAP
dc.type.openaireinfo:eu-repo/semantics/publishedVersion


Files in this item

FilesSizeFormatView

There are no files associated with this item

This item appears in the following Collection(s)

Show simple item record