Autor: |
Moacyr Moura Marinho, Johildo Figueiredo Salomão Barbosa, S L de Souza, Christopher Fanning, C M M Leite, J F Mascarenhas, J.J. Peucat |
Rok vydání: |
2002 |
Předmět: |
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Zdroj: |
Journal of South American Earth Sciences. 15:363-373 |
ISSN: |
0895-9811 |
DOI: |
10.1016/s0895-9811(02)00044-5 |
Popis: |
Felsic metavolcanics associated with supracrustal rocks provide U–Pb zircon and Sm–Nd TDM ages of approximately 3.3 Ga, which establish an Archean age of the Mundo Novo greenstone belt. A granodioritic gneiss from the Mairi complex, located on the eastern boundary of the Mundo Novo greenstone belt, exhibits a zircon evaporation minimum age of 3.04 Ga and a Nd model age of 3.2 Ga. These results constrain the occurrence of at least three major geological units in this area: the Archean Mundo Novo greenstone belt, the Archean Mairi gneisses, and the adjoining Paleoproterozoic ( |
Databáze: |
OpenAIRE |
Externí odkaz: |
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