"Invisible" silver in chalcopyrite and bornite from the Mantos Blancos Cu deposit, northern Chile

dc.date.accessioned2020-03-11T20:26:38Z
dc.date.accessioned2022-10-18T22:41:23Z
dc.date.available2020-03-11T20:26:38Z
dc.date.available2022-10-18T22:41:23Z
dc.date.created2020-03-11T20:26:38Z
dc.date.issued2013
dc.identifierhttp://hdl.handle.net/10533/238080
dc.identifier15090013
dc.identifierWOS:000325552100015
dc.identifierno scielo
dc.identifiereid=2-s2.0-84886021560
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4469419
dc.description.abstractRelatively little is known about the mineralogical occurrence and geochemical controls on the incorporation of "invisible" (refractory) silver and gold in hydrothermal sulfide minerals. Secondary ion mass spectrometry (SIMS) analysis reveals that bornite
dc.languageeng
dc.relationhttps://doi.org/10.1127/0935-1221/2013/0025-2287
dc.relation10.1127/0935-1221/2013/0025-2287
dc.rightsinfo:eu-repo/semantics/openAccess
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Chile
dc.rightshttp://creativecommons.org/licenses/by-nc-nd/3.0/cl/
dc.title"Invisible" silver in chalcopyrite and bornite from the Mantos Blancos Cu deposit, northern Chile
dc.typeArticulo


Este ítem pertenece a la siguiente institución