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Publikováno v:
Anais da Academia Brasileira de Ciências, Vol 73, Iss 3, Pp 445-460 (2001)
U-Pb SHRIMP and Sm-Nd isotopic ages were determined for felsic metavolcanic rocks from the Silvânia Sequence and Jurubatuba Granite in the central part of the Brasília Belt. Zircon grains from a metavolcanic sample yielded 2115 ± 23 Ma and from th
Externí odkaz:
https://doaj.org/article/2a093d54180749b998333c316f1f4e8f