Neoproterozoic glacial deposits from the Aracuai orogen, Brazil: Age, provenance and correlations with the Sao Francisco craton and West Congo belt


Autoria(s): Babinski, Marly; Pedrosa-Soares, A. C.; Trindade, R. I. F.; Martins, M.; Noce, C. M.; Liu, D.
Contribuinte(s)

UNIVERSIDADE DE SÃO PAULO

Data(s)

07/11/2013

07/11/2013

2012

Resumo

Glacigenic diamictite successions of the Macaubas Group are widespread in the western domain of the Aracuai orogen, east of the Sao Francisco craton (Brazil). Diamictites also occur on this craton and in the African counterpart of the Aracuai orogen, the West Congo belt. Detrital zircon grains from the matrix of diamictites and sandstones from the Macaubas 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 Macaubas basin with ages ranging from 900 to 2800 Ma. Sm-Nd T-DM 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 Jequitai and Carrancas diamictites in the Sao 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 Sao Francisco-Congo craton. Possible sources for these grains could occur elsewhere in Africa, or possibly from within the Brasilia Belt in western central Brazil. (C) 2011 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.

Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)

FAPESP (Fundacao de Amparo a Pesquisa do Estado de Sao Paulo)

CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico)

Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)

FINEP (Financiadora de Estudos e Projetos)

Financiadora de Estudos e Projetos (FINEP)

Fundacao de Amparo a Pesquisa de Minas Gerais (FAPEMIG)

FAPEMIG (Fundacao de Amparo a Pesquisa de Minas Gerais)

Identificador

GONDWANA RESEARCH, AMSTERDAM, v. 21, n. 41335, Special Issue, supl. 1, Part 4, pp. 451-465, MAR, 2012

1342-937X

http://www.producao.usp.br/handle/BDPI/43210

10.1016/j.gr.2011.04.008

http://dx.doi.org/10.1016/j.gr.2011.04.008

Idioma(s)

eng

Publicador

ELSEVIER SCIENCE BV

AMSTERDAM

Relação

GONDWANA RESEARCH

Direitos

restrictedAccess

Copyright ELSEVIER SCIENCE BV

Palavras-Chave #U-PB SHRIMP GEOCHRONOLOGY #NEOPROTEROZOIC GLACIATIONS #MACAUBAS GROUP #BRAZIL #ARACUAI-WEST CONGO OROGEN #CENTRAL-EASTERN BRAZIL #U-PB GEOCHRONOLOGY #BEBEDOURO FORMATION #DETRITAL ZIRCON #CAP CARBONATE #MINAS-GERAIS #BAMBUI GROUP #SE-BRAZIL #EVOLUTION #AFRICA #GEOSCIENCES, MULTIDISCIPLINARY
Tipo

article

original article

publishedVersion