Proterozoic Links Between The Borborema Province, Ne Brazil, And The Central African Fold Belt

dc.creatorVan Schmus W.R.
dc.creatorOliveira E.P.
dc.creatorDa Silva Filho A.F.
dc.creatorToteu S.F.
dc.creatorPenaye J.
dc.creatorGuimaraes I.P.
dc.date2008
dc.date2015-06-30T19:30:55Z
dc.date2015-11-26T14:45:07Z
dc.date2015-06-30T19:30:55Z
dc.date2015-11-26T14:45:07Z
dc.date.accessioned2018-03-28T21:54:16Z
dc.date.available2018-03-28T21:54:16Z
dc.identifier9781862392472
dc.identifierGeological Society Special Publication. , v. 294, n. , p. 69 - 99, 2008.
dc.identifier3058719
dc.identifier10.1144/SP294.5
dc.identifierhttp://www.scopus.com/inward/record.url?eid=2-s2.0-39549092822&partnerID=40&md5=1f3dd58871f0f460bd451d7ccbb9b420
dc.identifierhttp://www.repositorio.unicamp.br/handle/REPOSIP/106561
dc.identifierhttp://repositorio.unicamp.br/jspui/handle/REPOSIP/106561
dc.identifier2-s2.0-39549092822
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/1252380
dc.descriptionThe Congo (CC) and the São 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 Yaoundé domain occurs north of the CC. Crust north of the Sergipano domain comprises the Pernambuco-Alagoas (PEAL) domain. The NE-SW-striking Tcholliré-Banyo fault in Cameroon may extend southwestwards between the PEAL and Sergipano domains, defining northern limits of abundant SFC/ CC basement. The Adamawa-Yadé domain 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 Brasiliano 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 Ceará domains, which continue eastwards into western Nigeria and western Sahara. © The Geological Society of London 2008.
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dc.description99
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dc.languageen
dc.publisher
dc.relationGeological Society Special Publication
dc.rightsfechado
dc.sourceScopus
dc.titleProterozoic Links Between The Borborema Province, Ne Brazil, And The Central African Fold Belt
dc.typeActas de congresos


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