Petrogenesis of the late-orogenic Bravo granite and surrounding high-grade country rocks in the Palaeoproterozoic orogen of Itabuna-Salvador-Curaçá block, Bahia, Brazil
| Autor(a) principal: | |
|---|---|
| Data de Publicação: | 2008 |
| Outros Autores: | , , , , , , , |
| Tipo de documento: | Artigo |
| Idioma: | eng |
| Título da fonte: | Repositório Institucional da UFBA |
| Texto Completo: | http://www.repositorio.ufba.br/ri/handle/ri/5156 |
Resumo: | p. 35–52 |
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Barbosa, Johildo Salomão FigueirêdoPeucat, Jean-JacquesMartin, HervéSilva, Fernando Alves daMoraes, Antonio Marcos deGomes, Luiz César CorrêaSabaté, PierreMarinho, Moacyr M.Fanning, C. MarkBarbosa, Johildo Salomão FigueirêdoPeucat, Jean-JacquesMartin, HervéSilva, Fernando Alves daMoraes, Antonio Marcos deGomes, Luiz César CorrêaSabaté, PierreMarinho, Moacyr M.Fanning, C. Mark2012-01-12T18:08:52Z2012-01-12T18:08:52Z20080301-9268http://www.repositorio.ufba.br/ri/handle/ri/5156v. 167p. 35–52In the São Francisco Craton, in Bahia state, Brazil, four Archaean crustal segments collided during the Palaeoproterozoic to form the important Itabuna-Salvador-Curaçá Orogen (ISCO). Granulites were formed in the central, deepest part of the ISCO while rocks in amphibolite to greenschist facies were formed at the borders. During the uplift of the orogen shear zones, faults and fractures provided channels for the intrusion of granites and syenites into the granulitic country rocks which reached higher crustal levels. This article reports a study of the Bravo granite with a zircon U–Pb SHRIMP age of 2060±6 Ma, and of its granulite host rocks formed from Archaean and Palaeoproterozoic protoliths in the Bravo and Tanquinho regions. The metamorphic peak occurred between 2064±6Ma and 2060±6Ma in the Bravo region. The Bravo granite is mostly metaluminous and alkaline due to high K2O contents (4.03–5.95%) which confer high-K to shoshonitic affinities. It is slightly younger than syenites of the orogen (Itiúba, 2084±9 Ma; São Felix, 2098±1 Ma) which are cut by late felsic veins chemically similar to the Bravo granite. The granulitic rocks form a peraluminous, medium-K calc-alkaline TTG suite. It is proposed that residual liquids represented by the vein rocks and the Bravo granite escaped from the syenitic cumulates, and migrated upwards through crustal discontinuities formed during the uplift of the ISCO.Submitted by Ana Valéria de Jesus Moura (anavaleria_131@hotmail.com) on 2012-01-12T18:08:52Z No. of bitstreams: 1 s2.0-S0301926808001332-main.pdf: 2186848 bytes, checksum: 9a8f7772d013c62f2cd3807def1e4d6f (MD5)Made available in DSpace on 2012-01-12T18:08:52Z (GMT). No. of bitstreams: 1 s2.0-S0301926808001332-main.pdf: 2186848 bytes, checksum: 9a8f7772d013c62f2cd3807def1e4d6f (MD5) Previous issue date: 2008BrazilGranulitePalaeoproterozoicSão Francisco CratonItabuna-Salvador-Curaçá orogenPetrogenesis of the late-orogenic Bravo granite and surrounding high-grade country rocks in the Palaeoproterozoic orogen of Itabuna-Salvador-Curaçá block, Bahia, BrazilPrecambrian Researchinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleengreponame:Repositório Institucional da UFBAinstname:Universidade Federal da Bahia (UFBA)instacron:UFBAinfo:eu-repo/semantics/openAccessLICENSElicense.txtlicense.txttext/plain1762https://repositorio.ufba.br/bitstream/ri/5156/2/license.txt1b89a9a0548218172d7c829f87a0eab9MD52ORIGINALs2.0-S0301926808001332-main.pdfs2.0-S0301926808001332-main.pdfapplication/pdf2186848https://repositorio.ufba.br/bitstream/ri/5156/1/s2.0-S0301926808001332-main.pdf9a8f7772d013c62f2cd3807def1e4d6fMD51TEXTs2.0-S0301926808001332-main.pdf.txts2.0-S0301926808001332-main.pdf.txtExtracted texttext/plain76636https://repositorio.ufba.br/bitstream/ri/5156/3/s2.0-S0301926808001332-main.pdf.txtfa6f2612b543c82f1fe1977874174c2fMD53ri/51562022-08-08 13:17:35.543oai:repositorio.ufba.br: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Repositório InstitucionalPUBhttp://192.188.11.11:8080/oai/requestopendoar:19322022-08-08T16:17:35Repositório Institucional da UFBA - Universidade Federal da Bahia (UFBA)false |
| dc.title.pt_BR.fl_str_mv |
Petrogenesis of the late-orogenic Bravo granite and surrounding high-grade country rocks in the Palaeoproterozoic orogen of Itabuna-Salvador-Curaçá block, Bahia, Brazil |
| dc.title.alternative.pt_BR.fl_str_mv |
Precambrian Research |
| title |
Petrogenesis of the late-orogenic Bravo granite and surrounding high-grade country rocks in the Palaeoproterozoic orogen of Itabuna-Salvador-Curaçá block, Bahia, Brazil |
| spellingShingle |
Petrogenesis of the late-orogenic Bravo granite and surrounding high-grade country rocks in the Palaeoproterozoic orogen of Itabuna-Salvador-Curaçá block, Bahia, Brazil Barbosa, Johildo Salomão Figueirêdo Granulite Palaeoproterozoic São Francisco Craton Itabuna-Salvador-Curaçá orogen |
| title_short |
Petrogenesis of the late-orogenic Bravo granite and surrounding high-grade country rocks in the Palaeoproterozoic orogen of Itabuna-Salvador-Curaçá block, Bahia, Brazil |
| title_full |
Petrogenesis of the late-orogenic Bravo granite and surrounding high-grade country rocks in the Palaeoproterozoic orogen of Itabuna-Salvador-Curaçá block, Bahia, Brazil |
| title_fullStr |
Petrogenesis of the late-orogenic Bravo granite and surrounding high-grade country rocks in the Palaeoproterozoic orogen of Itabuna-Salvador-Curaçá block, Bahia, Brazil |
| title_full_unstemmed |
Petrogenesis of the late-orogenic Bravo granite and surrounding high-grade country rocks in the Palaeoproterozoic orogen of Itabuna-Salvador-Curaçá block, Bahia, Brazil |
| title_sort |
Petrogenesis of the late-orogenic Bravo granite and surrounding high-grade country rocks in the Palaeoproterozoic orogen of Itabuna-Salvador-Curaçá block, Bahia, Brazil |
| author |
Barbosa, Johildo Salomão Figueirêdo |
| author_facet |
Barbosa, Johildo Salomão Figueirêdo Peucat, Jean-Jacques Martin, Hervé Silva, Fernando Alves da Moraes, Antonio Marcos de Gomes, Luiz César Corrêa Sabaté, Pierre Marinho, Moacyr M. Fanning, C. Mark |
| author_role |
author |
| author2 |
Peucat, Jean-Jacques Martin, Hervé Silva, Fernando Alves da Moraes, Antonio Marcos de Gomes, Luiz César Corrêa Sabaté, Pierre Marinho, Moacyr M. Fanning, C. Mark |
| author2_role |
author author author author author author author author |
| dc.contributor.author.fl_str_mv |
Barbosa, Johildo Salomão Figueirêdo Peucat, Jean-Jacques Martin, Hervé Silva, Fernando Alves da Moraes, Antonio Marcos de Gomes, Luiz César Corrêa Sabaté, Pierre Marinho, Moacyr M. Fanning, C. Mark Barbosa, Johildo Salomão Figueirêdo Peucat, Jean-Jacques Martin, Hervé Silva, Fernando Alves da Moraes, Antonio Marcos de Gomes, Luiz César Corrêa Sabaté, Pierre Marinho, Moacyr M. Fanning, C. Mark |
| dc.subject.por.fl_str_mv |
Granulite Palaeoproterozoic São Francisco Craton Itabuna-Salvador-Curaçá orogen |
| topic |
Granulite Palaeoproterozoic São Francisco Craton Itabuna-Salvador-Curaçá orogen |
| description |
p. 35–52 |
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2008 |
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2008 |
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2012-01-12T18:08:52Z |
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2012-01-12T18:08:52Z |
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0301-9268 |
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v. 167 |
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0301-9268 v. 167 |
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