Please use this identifier to cite or link to this item: https://hdl.handle.net/10316/3931
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dc.contributor.authorPinto, Marina M. S. Cabral-
dc.contributor.authorSilva, Maria M. V. G.-
dc.date.accessioned2008-08-29T16:06:49Z-
dc.date.available2008-08-29T16:06:49Z-
dc.date.issued2007en_US
dc.identifier.citationChemie der Erde - Geochemistry. 67:3 (2007) 251-252en_US
dc.identifier.urihttps://hdl.handle.net/10316/3931-
dc.description.abstractA brief summary about the composition and origins of the U deposit is present. The mineralization is composed by secondary uranium phosphates (saleeite and meta-saleeite). The precipitation was probably the main responsible factor for U retention within the quartz veins leading to the uranium phosphate mineralization of Vale de Abrutiga.en_US
dc.description.urihttp://www.sciencedirect.com/science/article/B7CW6-4PMJB1M-1/1/dd0e0fed43334af2b2db35db46c31f78en_US
dc.format.mimetypeaplication/PDFen
dc.language.isoengeng
dc.rightsopenAccesseng
dc.subjectSecondary uranium phosphatesen_US
dc.subjectSaleeiteen_US
dc.subjectU-bearing mineralsen_US
dc.subjectWeatheringen_US
dc.subjectSorptionen_US
dc.subjectInclusionsen_US
dc.subjectPortugalen_US
dc.titleThe Vale de Abrutiga uranium phosphates mine, central Portugalen_US
dc.typearticleen_US
dc.identifier.doi10.1016/j.chemer.2007.08.001-
item.grantfulltextopen-
item.fulltextCom Texto completo-
item.openairetypearticle-
item.languageiso639-1en-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.cerifentitytypePublications-
Appears in Collections:FCTUC Ciências da Terra - Artigos em Revistas Internacionais
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