Ore Geology Reviews

dc.creatorDeditius, A.
dc.creatorUtsunomiya-Reich, M.
dc.creatorKesler, S. E.
dc.creatorEwing, R. C.
dc.creatorHough, R.
dc.creatorWalshe, J.
dc.date2020-03-11T20:26:27Z
dc.date2022-07-07T23:43:59Z
dc.date2020-03-11T20:26:27Z
dc.date2022-07-07T23:43:59Z
dc.date2011
dc.date.accessioned2023-08-23T00:38:21Z
dc.date.available2023-08-23T00:38:21Z
dc.identifier15090013
dc.identifier15090013
dc.identifierhttps://hdl.handle.net/10533/238017
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/8355896
dc.descriptionHydrothermal pyrite contains significant amounts of minor and trace elements including As, Pb, Sb, Bi, Cu, Co, Ni, Zn, Au, Ag, Se and Te, which can be incorporated into nanoparticles (NPs). NP-bearing pyrite is most common in hydrothermal ore deposits tha
dc.descriptionFONDAP
dc.descriptionFONDAP
dc.languageeng
dc.relationhttps://doi.org/10.1016/j.oregeorev.2011.03.003
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Chile
dc.rightshttp://creativecommons.org/licenses/by-nc-nd/3.0/cl/
dc.rightsinfo:eu-repo/semantics/openAccess
dc.titleTrace metal nanoparticles in pyrite
dc.titleOre Geology Reviews
dc.typeArticulo
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/publishedVersion


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