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- W2148027865 endingPage "99" @default.
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- W2148027865 abstract "The Congo (CC) and the Sao Francisco (SFC) cratons were joined at about 2.05 Ga; northern parts of Palaeoproterozoic basement subsequently underwent extension at about 1 Ga, forming intracratonic basins. Neoproterozoic metasedimentary rocks in these basins yield detrital zircons as young as 630 Ma. The Brasiliano and Pan-African (c. 620- 580 Ma) assembly of West Gondwana extensively altered this system. The Sergipano domain occurs north of the SFC, and the comparable Yaoundedomain occurs north of the CC. Crust north of the Sergipano domain com- prises the Pernambuco- Alagoas (PEAL) domain. The NE- SW-striking Tchollire ´ -Banyo fault in Cameroon may extend southwestwards between the PEAL and Sergipano domains, defining northern limits of abundant SFC/CC basement. The Adamawa -Yadedomain in Africa does not appear to extend into Brazil. The Transverse domain of Brazil is a collage of Palaeoproterozoic crustal blocks, the 1.0 Ga Cariris Velhos orogen (CVO), late Neoproterozoic basins, and Brasi- liano granites. The CVO extends ENE for more than 700 km in Brazil, but eastern continuation into Africa has not been identified. North of the Transverse domain contiguous c. 2.15 Ga gneisses comprise basement of Rio Grande do Norte and Cearadomains, which continue eastwards into western Nigeria and western Sahara." @default.
- W2148027865 created "2016-06-24" @default.
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- W2148027865 creator A5060683210 @default.
- W2148027865 creator A5085698958 @default.
- W2148027865 date "2008-01-01" @default.
- W2148027865 modified "2023-10-01" @default.
- W2148027865 title "Proterozoic links between the Borborema Province, NE Brazil, and the Central African Fold Belt" @default.
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- W2148027865 doi "https://doi.org/10.1144/sp294.5" @default.
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