Artigo Acesso aberto Produção Nacional

Cryogenian U-Pb (SHRIMP I) zircon ages of anorthosites from the upper sequences of Niquelândia and Barro Alto Complexes, Central Brazil

2007; Sociedade Brasileira de Geologia; Volume: 37; Issue: S4 Linguagem: Inglês

10.25249/0375-7536.200737s47075

ISSN

2177-4382

Autores

Ciro Teixeira Correia, Vicente Antônio Vitório Girardi, Miguel Ângelo Stipp Basei, Allen P. Nutman,

Tópico(s)

Mineralogy and Gemology Studies

Resumo

The Niquelândia Complex comprises two main superposed sequences dipping westward: the lower (LS), at the eastern, and the upper (US), at the western part of the body. The Complex is either interpreted as a single body, or as two distinct unrelated layered massifs. New SHRIMP U-Pb determinations on igneous zircon grains of anorthosites from Niquelândia US and from the upper portion of the Barro Alto Complex indicate crystallization ages of 833 ± 21 Ma and 733 ± 25 Ma, respectively, thus supporting Cryogenian Neoproteroic ages for the igneous crystallization of the US unit of Niquelândia and for the Barro Alto anorthosites.

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