
ESTUDO COMPARATIVO ENTRE OS COMPLEXOS DE BARRO ALTO E DO TOCANTINS, GOIÁS
1975; Sociedade Brasileira de Geologia; Volume: 5; Issue: 1 Linguagem: Inglês
10.25249/0375-7536.19751529
ISSN2177-4382
AutoresFIGUEIREDO ALMIR NEVES DE, MOTTA JORGE, MARQUES VALTER JOSÉ,
Tópico(s)Geochemistry and Geologic Mapping
ResumoThe two largest gabbro-peridotite-anorthositic Complexes presently recognized in Brazil, the Barro Alto and the Tocantins Complexes, outcrop in the central region of the Goiás State. They are believed to be Early Precambrian in age. The two complexes contain the same suite of rocks and have similar chemical, textural and mineralogical aspects. Stratiform and alpine features are present in both complexes.
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