Please use this identifier to cite or link to this item: http://www.repositorio.ufop.br/jspui/handle/123456789/4167
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dc.contributor.authorBabinski, Marly-
dc.contributor.authorSoares, Antônio Carlos Pedrosa-
dc.contributor.authorTrindade, Ricardo Ivan Ferreira da-
dc.contributor.authorMartins, Maximiliano de Souza-
dc.contributor.authorNoce, Carlos Maurício-
dc.date.accessioned2014-12-14T12:51:17Z-
dc.date.available2014-12-14T12:51:17Z-
dc.date.issued2012-
dc.identifier.citationBABINSKI, M. et al. Neoproterozoic glacial deposts from the Araçuaí orogen, Brazil : age, provenance and correlations with the São Francisco craton and West Congo belt. Gondwana Research, v. 21, p. 451-465, 2012. Disponível em: <http://www.sciencedirect.com/science/article/pii/S1342937X11001286>. Acesso em: 30 set. 2014.pt_BR
dc.identifier.issn1342-937X-
dc.identifier.urihttp://www.repositorio.ufop.br/handle/123456789/4167-
dc.description.abstractGlacigenic diamictite successions of the Macaúbas Group are widespread in the western domain of the Araçuaí orogen, east of the São Francisco craton (Brazil). Diamictites also occur on this craton and in the African counterpart of the Araçuaí orogen, theWest Congo belt. Detrital zircon grains fromthe matrix of diamictites and sandstones from the Macaúbas Group were dated by the U–Pb SHRIMP technique. The geochronological study sets the maximum depositional age of the glacial diamictites at 900 Ma, and indicates multiple sources for the Macaúbas basin with ages ranging from 900 to 2800Ma. Sm–Nd TDM model ages, determined on whole rock samples, range from 1.8 Ga to 2.5 Ga and get older up-section. Comparison of our data with those from the cratonic area suggest that these glacial deposits can be correlated to the Jequitaí and Carrancas diamictites in the São Francisco craton, and to the Lower Mixtite Formation of the West Congolian Group, exposed in Africa. The 900–1000 Ma source is most probably represented by the Zadinian–Mayumbian volcanic rocks and related granites from the West Congo belt. However, one of the most voluminous sources, with ages in the 1.1–1.3 Ga interval, has not been detected in the São Francisco-Congo craton. Possible sources for these grains could occur elsewhere in Africa, or possibly from within the Brasília Belt in western central Brazil.pt_BR
dc.language.isoen_USpt_BR
dc.subjectGeochronologypt_BR
dc.subjectNeoproterozoic glaciationspt_BR
dc.subjectMacaúbaspt_BR
dc.subjectAraçuaípt_BR
dc.titleNeoproterozoic glacial deposits from the Araçuaí orogen, Brazil : age, provenance and correlations with the São Francisco craton and West Congo belt.pt_BR
dc.typeArtigo publicado em periodicopt_BR
dc.rights.licenseO periódico Gondwana Research concede permissão para depósito deste artigo no Repositório Institucional da UFOP. Número da licença: 3484311276531.pt_BR
dc.identifier.doihttps://doi.org/10.1016/j.gr.2011.04.008-
Appears in Collections:DEGEO - Artigos publicados em periódicos

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