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Authordc.contributor.authorSapiains, Pía
Authordc.contributor.authorFigueroa, Valentina
Authordc.contributor.authorHayashida, Frances
Authordc.contributor.authorSalazar Sutil, Diego Rodrigo
Authordc.contributor.authorMenzies, Andrew
Authordc.contributor.authorGonzález, Cristián
Authordc.contributor.authorLoyola, Rodrigo
Authordc.contributor.authorMurphy, Beau
Authordc.contributor.authorGonzález, Juan
Authordc.contributor.authorParcero Oubiña, César
Authordc.contributor.authorTroncoso Meléndez, Andrés Rolando
Admission datedc.date.accessioned2022-05-09T19:42:18Z
Available datedc.date.available2022-05-09T19:42:18Z
Publication datedc.date.issued2021
Cita de ítemdc.identifier.citationMinerals 2021, 11, 1402es_ES
Identifierdc.identifier.other10.3390/min11121402
Identifierdc.identifier.urihttps://repositorio.uchile.cl/handle/2250/185359
Abstractdc.description.abstractNorthern Chile is home to the world’s largest copper ore deposits, which have been exploited for thousands of years by different groups, at varying scales and for different purposes. In this context, it is important to develop new protocols to characterise the mineralogical variability of archaeological copper ores. A comprehensive and representative methodology in the analysis of minerals, the application of non-destructive analytical techniques, and the combination of insights from geological, archaeological and local knowledge are key to developing a copper mineral repository of the Atacama Desert area. Geochemical analyses were applied to the study of 568 samples from the archaeological site Pukara de Turi, with different techniques such as micro-XRF, XRD, QEMSCAN, Raman spectroscopy and technological studies. This exhaustive analysis allowed for the recognition of two mineralogical associations: atacamite/brochantite (99%) and azurite/chrysocolla (1%). The study of various minerals allows data to be interpreted more reliably and to trace the likely geological sources of these minerals. The azurite/chrysocolla samples appear to belong to the same mineral association found in the Cerro Verde district, which is probably the source of these samples. The atacamite/brochantite samples appear to come from more than one geological source, including, but not limited to, Chuquicamata-Radomiro Tomic and El Abra-Conchi.es_ES
Patrocinadordc.description.sponsorshipIIE Fulbright award University of New Mexico Snead-Wertheim Endowed Lectureship in Anthropology and History Agencia Nacional de Investigacion y Desarrollo (ANID)/BECA DOCTORADO NACIONAL/2018 21181070 Comision Nacional de Investigacion Cientifica y Tecnologica (CONICYT) CONICYT FONDECYT 1201603 Aparece en contenido como:FONDECYT CONICYT-USA 2013/0012es_ES
Lenguagedc.language.isoenes_ES
Publisherdc.publisherMDPIes_ES
Type of licensedc.rightsAttribution-NonCommercial-NoDerivs 3.0 United States*
Link to Licensedc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/us/*
Sourcedc.sourceMineralses_ES
Keywordsdc.subjectCopper mineralses_ES
Keywordsdc.subjectMicro-XRFes_ES
Keywordsdc.subjectArchaeometryes_ES
Títulodc.titleSupergene copper and the ancient mining landscapes of the Atacama desert: Refining the protocol for the study of archaeological copper minerals through the case study of pukara de turies_ES
Document typedc.typeArtículo de revistaes_ES
dc.description.versiondc.description.versionVersión publicada - versión final del editores_ES
dcterms.accessRightsdcterms.accessRightsAcceso abiertoes_ES
Catalogueruchile.catalogadorcfres_ES
Indexationuchile.indexArtículo de publícación WoSes_ES
Indexationuchile.indexArtículo de publicación SCOPUSes_ES


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Attribution-NonCommercial-NoDerivs 3.0 United States
Except where otherwise noted, this item's license is described as Attribution-NonCommercial-NoDerivs 3.0 United States