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Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/184196
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dc.contributor.authorVillanova de Benavent, Cristina-
dc.contributor.authorViti, Cecilia-
dc.contributor.authorProenza Fernández, Joaquín Antonio-
dc.contributor.authorGalí Medina, Salvador, 1949--
dc.contributor.authorNieto, Fernando-
dc.date.accessioned2022-03-17T13:57:15Z-
dc.date.available2022-03-17T13:57:15Z-
dc.date.issued2015-07-
dc.identifier.issn1885-7264-
dc.identifier.urihttp://hdl.handle.net/2445/184196-
dc.description.abstractNi-phyllosilicates, commonly grouped under the name of "garnierites", are significant nickel ores found in hydrous silicate-type Ni-laterite deposits worldwide. They usually occur as vein infillings in the lower parts of laterite profiles, and consist of fine-grained, often intimately mixed, nickelmagnesium phyllosilicates, including serpentine, talc, sepiolite, smectite and chlorite (e.g. Brindley & Maksimović, 1974).-
dc.format.extent2 p.-
dc.format.mimetypeapplication/pdf-
dc.language.isoeng-
dc.publisherSociedad Española de Mineralogía-
dc.relation.isformatofReproducció del document publicat a: http://www.semineral.es/websem/PdfServlet?mod=archivos&subMod=publicaciones&archivo=Macla20_149-150.pdf-
dc.relation.ispartofMACLA. Revista de la Sociedad Española de Mineralogía, 2015, vol. 20, p. 149-150-
dc.rights(c) Villanova de Benavent, Cristina et al., 2015-
dc.sourceArticles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada)-
dc.subject.classificationMineralogia-
dc.subject.classificationNíquel-
dc.subject.otherMineralogy-
dc.subject.otherNickel-
dc.titleNi-enrichment processes revealed by TEM imaging on garnierites-
dc.typeinfo:eu-repo/semantics/article-
dc.typeinfo:eu-repo/semantics/publishedVersion-
dc.identifier.idgrec722176-
dc.date.updated2022-03-17T13:57:15Z-
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess-
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