Origen de la alunita y la natroalunita del depósito de caolín de Mina Equivocada (Prov. de Río Negro, Argentina)

cic.isFulltexttruees
cic.isPeerReviewedtruees
cic.lugarDesarrolloUniversidad Nacional del Sur es
cic.versioninfo:eu-repo/semantics/publishedVersiones
dc.date.accessioned2016-12-14T13:34:33Z
dc.date.available2016-12-14T13:34:33Z
dc.identifier.urihttps://digital.cic.gba.gob.ar/handle/11746/4990
dc.titleOrigen de la alunita y la natroalunita del depósito de caolín de Mina Equivocada (Prov. de Río Negro, Argentina)es
dc.typeDocumento de conferenciaes
dcterms.abstractThe origin of alunite and natroalunite from a kaolin deposit (Equivocada Mine, Rio Negro Province) has been studied. Chemical analysis showed that alunite is K<sub>0.89</sub> and natroalunite Na<sub>0.97</sub>, in agreement with X ray diffraction data. The high contents of minor elements in alunite, especially Ba and Sr are compatible with a hydrothermal origin in contrast to natroalunite whose very low values suggest a secondary origin. Alunite has a δ<sup>34<sup/>S = +15.9‰ and a δ<sup>18</sup>O = +12.9‰, while in natroalunite these values are -5.8‰ and +19.0‰ respectively. δ<sup>34<sup/>S values suggest that alunite formed from a hypogenic process of hydrothermal origin whereas natroalunite is probably related to a supergen origin. The occurrence of alunite in veins crosscutting the other minerals, indicates that it was the last mineral to crystallize.en
dcterms.creator.authorMaiza, Pedroes
dcterms.creator.authorMarfil, Silvina Andreaes
dcterms.creator.authorCardellach, E.es
dcterms.creator.authorCorbella, M.es
dcterms.extent5 p.es
dcterms.isPartOf.issueVII MinMet (Buenos Aires, 2006)es
dcterms.isPartOf.seriesCongreso de Mineralogía y Metalogeniaes
dcterms.issued2006
dcterms.languageEspañoles
dcterms.licenseAttribution 4.0 International (BY 4.0)es
dcterms.subject.materiaIngeniería de los Materialeses

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