The Vale de Abrutiga uranium phosphates mine, central Portugal

Detalhes bibliográficos
Autor(a) principal: Pinto, Marina M. S. Cabral
Data de Publicação: 2007
Outros Autores: Silva, Maria M. V. G.
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
Texto Completo: http://hdl.handle.net/10316/3931
https://doi.org/10.1016/j.chemer.2007.08.001
Resumo: A 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.
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spelling The Vale de Abrutiga uranium phosphates mine, central PortugalSecondary uranium phosphatesSaleeiteU-bearing mineralsWeatheringSorptionInclusionsPortugalA 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.http://www.sciencedirect.com/science/article/B7CW6-4PMJB1M-1/1/dd0e0fed43334af2b2db35db46c31f782007info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleaplication/PDFhttp://hdl.handle.net/10316/3931http://hdl.handle.net/10316/3931https://doi.org/10.1016/j.chemer.2007.08.001engChemie der Erde - Geochemistry. 67:3 (2007) 251-252Pinto, Marina M. S. CabralSilva, Maria M. V. G.info:eu-repo/semantics/openAccessreponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãoinstacron:RCAAP2020-11-06T16:48:52Zoai:estudogeral.uc.pt:10316/3931Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireopendoar:71602024-03-19T20:55:08.118701Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãofalse
dc.title.none.fl_str_mv The Vale de Abrutiga uranium phosphates mine, central Portugal
title The Vale de Abrutiga uranium phosphates mine, central Portugal
spellingShingle The Vale de Abrutiga uranium phosphates mine, central Portugal
Pinto, Marina M. S. Cabral
Secondary uranium phosphates
Saleeite
U-bearing minerals
Weathering
Sorption
Inclusions
Portugal
title_short The Vale de Abrutiga uranium phosphates mine, central Portugal
title_full The Vale de Abrutiga uranium phosphates mine, central Portugal
title_fullStr The Vale de Abrutiga uranium phosphates mine, central Portugal
title_full_unstemmed The Vale de Abrutiga uranium phosphates mine, central Portugal
title_sort The Vale de Abrutiga uranium phosphates mine, central Portugal
author Pinto, Marina M. S. Cabral
author_facet Pinto, Marina M. S. Cabral
Silva, Maria M. V. G.
author_role author
author2 Silva, Maria M. V. G.
author2_role author
dc.contributor.author.fl_str_mv Pinto, Marina M. S. Cabral
Silva, Maria M. V. G.
dc.subject.por.fl_str_mv Secondary uranium phosphates
Saleeite
U-bearing minerals
Weathering
Sorption
Inclusions
Portugal
topic Secondary uranium phosphates
Saleeite
U-bearing minerals
Weathering
Sorption
Inclusions
Portugal
description A 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.
publishDate 2007
dc.date.none.fl_str_mv 2007
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dc.identifier.uri.fl_str_mv http://hdl.handle.net/10316/3931
http://hdl.handle.net/10316/3931
https://doi.org/10.1016/j.chemer.2007.08.001
url http://hdl.handle.net/10316/3931
https://doi.org/10.1016/j.chemer.2007.08.001
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv Chemie der Erde - Geochemistry. 67:3 (2007) 251-252
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