Tectonic and magmatic evolution of the ribeira belt in the highlands of the Rio de Janeiro state, Brazil, from neoproterozoic to lower paleozoic

Detalhes bibliográficos
Autor(a) principal: Tupinambá, Miguel
Data de Publicação: 2012
Outros Autores: Teixeira, Wilson, Heilbron, Monica
Tipo de documento: Artigo
Idioma: por
Título da fonte: Anuário do Instituto de Geociências (Online)
Texto Completo: https://revistas.ufrj.br/index.php/aigeo/article/view/6943
Resumo: The Highlands of the Rio de Janeiro (RSF) are composed of granitic gneiss, paragneiss and granite that are part of the Ribeira Belt. Their geological features were studied for over 50 years by authors who described orthogneisses and granites arranged in large overlapping tectonic sheaths. Tectonic domains and terranes were proposed for the Ribeira Belt, and the rocks of the RSF were included in the Oriental Terrane. The tectonic and magmatic evolution of the RSF begins in the Cryogenian with the installation of the magmatic arc of the Rio Negro Complex and sedimentation of the Italva, St. Fidélis and Bom Jesus do Itabapoana groups. During the Ediacaran collision of this arc with a passive margin the migmatitic leucogneisses of the Cordeiro Suíte were generated. At the collisional ending the calc-alkaline magmatic Serra dos Órgãos Suíte was produced. At the end of evolution, tectonic exhumation and tectonic collapse was coeval with the intrusion of Cambro-Ordovician granites of the Nova Friburgo Suíte.
id UFRJ-21_8334cbd2fbd23857729e2a242173d6a1
oai_identifier_str oai:www.revistas.ufrj.br:article/6943
network_acronym_str UFRJ-21
network_name_str Anuário do Instituto de Geociências (Online)
repository_id_str
spelling Tectonic and magmatic evolution of the ribeira belt in the highlands of the Rio de Janeiro state, Brazil, from neoproterozoic to lower paleozoicEvolução tectónica e magmática da faixa ribeira entre o neoproterozoico e o paleozoico inferior na região serrana do estado do Rio de Janeiro, BrasilThe Highlands of the Rio de Janeiro (RSF) are composed of granitic gneiss, paragneiss and granite that are part of the Ribeira Belt. Their geological features were studied for over 50 years by authors who described orthogneisses and granites arranged in large overlapping tectonic sheaths. Tectonic domains and terranes were proposed for the Ribeira Belt, and the rocks of the RSF were included in the Oriental Terrane. The tectonic and magmatic evolution of the RSF begins in the Cryogenian with the installation of the magmatic arc of the Rio Negro Complex and sedimentation of the Italva, St. Fidélis and Bom Jesus do Itabapoana groups. During the Ediacaran collision of this arc with a passive margin the migmatitic leucogneisses of the Cordeiro Suíte were generated. At the collisional ending the calc-alkaline magmatic Serra dos Órgãos Suíte was produced. At the end of evolution, tectonic exhumation and tectonic collapse was coeval with the intrusion of Cambro-Ordovician granites of the Nova Friburgo Suíte.A Região Serrana Fluminense (RSF) é constituída por gnaisses granitóides, paragnaisses e granitos que fazem parte da Faixa Ribeira. Seus aspectos geológicos são estudados há mais de 50 anos por autores que descreveram ortognaisses e granitos dispostos em grandes escamas tectônicas superpostas. Dominios e terrenos tectônicos foram propostos para a Faixa Ribeira, sendo as rochas da RSF incluidas no Terreno Oriental. A evolução tectônica e magmática da RSF se inicia no Cryogeniano com a instalação do arco magmático do Complexo Rio Negro e sedimentação das rochas dos grupos Italva, São Fidélis e Bom Jesus do Itabapoana. Durante a colisão Ediacarana deste arco com uma margem passiva teria ocorrido metamorfismo geração dos gnaisses migmáticos da Suíte Cordeiro. Seguiu-se à colisão o magmatismo calci-alcalino da Suíte Serra dos Órgãos. Ao final da evolução, a exumação tectônica do conjunto teria originado um colapso tectónico, com a consequente intrusão dos granitos pós-colisionais da Suíte Nova Friburgo durante o Cambro-Ordoviciano.Universidade Federal do Rio de Janeiro2012-12-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://revistas.ufrj.br/index.php/aigeo/article/view/694310.11137/2012_2_140_151Anuário do Instituto de Geociências; Vol 35, No 2 (2012); 140-151Anuário do Instituto de Geociências; Vol 35, No 2 (2012); 140-1511982-39080101-9759reponame:Anuário do Instituto de Geociências (Online)instname:Universidade Federal do Rio de Janeiro (UFRJ)instacron:UFRJporhttps://revistas.ufrj.br/index.php/aigeo/article/view/6943/5510Copyright (c) 2012 Anuário do Instituto de Geociênciashttp://creativecommons.org/licenses/by/4.0info:eu-repo/semantics/openAccessTupinambá, MiguelTeixeira, WilsonHeilbron, Monica2017-01-23T22:34:48Zoai:www.revistas.ufrj.br:article/6943Revistahttps://revistas.ufrj.br/index.php/aigeo/indexPUBhttps://revistas.ufrj.br/index.php/aigeo/oaianuario@igeo.ufrj.br||1982-39080101-9759opendoar:2017-01-23T22:34:48Anuário do Instituto de Geociências (Online) - Universidade Federal do Rio de Janeiro (UFRJ)false
dc.title.none.fl_str_mv Tectonic and magmatic evolution of the ribeira belt in the highlands of the Rio de Janeiro state, Brazil, from neoproterozoic to lower paleozoic
Evolução tectónica e magmática da faixa ribeira entre o neoproterozoico e o paleozoico inferior na região serrana do estado do Rio de Janeiro, Brasil
title Tectonic and magmatic evolution of the ribeira belt in the highlands of the Rio de Janeiro state, Brazil, from neoproterozoic to lower paleozoic
spellingShingle Tectonic and magmatic evolution of the ribeira belt in the highlands of the Rio de Janeiro state, Brazil, from neoproterozoic to lower paleozoic
Tupinambá, Miguel
title_short Tectonic and magmatic evolution of the ribeira belt in the highlands of the Rio de Janeiro state, Brazil, from neoproterozoic to lower paleozoic
title_full Tectonic and magmatic evolution of the ribeira belt in the highlands of the Rio de Janeiro state, Brazil, from neoproterozoic to lower paleozoic
title_fullStr Tectonic and magmatic evolution of the ribeira belt in the highlands of the Rio de Janeiro state, Brazil, from neoproterozoic to lower paleozoic
title_full_unstemmed Tectonic and magmatic evolution of the ribeira belt in the highlands of the Rio de Janeiro state, Brazil, from neoproterozoic to lower paleozoic
title_sort Tectonic and magmatic evolution of the ribeira belt in the highlands of the Rio de Janeiro state, Brazil, from neoproterozoic to lower paleozoic
author Tupinambá, Miguel
author_facet Tupinambá, Miguel
Teixeira, Wilson
Heilbron, Monica
author_role author
author2 Teixeira, Wilson
Heilbron, Monica
author2_role author
author
dc.contributor.author.fl_str_mv Tupinambá, Miguel
Teixeira, Wilson
Heilbron, Monica
description The Highlands of the Rio de Janeiro (RSF) are composed of granitic gneiss, paragneiss and granite that are part of the Ribeira Belt. Their geological features were studied for over 50 years by authors who described orthogneisses and granites arranged in large overlapping tectonic sheaths. Tectonic domains and terranes were proposed for the Ribeira Belt, and the rocks of the RSF were included in the Oriental Terrane. The tectonic and magmatic evolution of the RSF begins in the Cryogenian with the installation of the magmatic arc of the Rio Negro Complex and sedimentation of the Italva, St. Fidélis and Bom Jesus do Itabapoana groups. During the Ediacaran collision of this arc with a passive margin the migmatitic leucogneisses of the Cordeiro Suíte were generated. At the collisional ending the calc-alkaline magmatic Serra dos Órgãos Suíte was produced. At the end of evolution, tectonic exhumation and tectonic collapse was coeval with the intrusion of Cambro-Ordovician granites of the Nova Friburgo Suíte.
publishDate 2012
dc.date.none.fl_str_mv 2012-12-01
dc.type.none.fl_str_mv
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv https://revistas.ufrj.br/index.php/aigeo/article/view/6943
10.11137/2012_2_140_151
url https://revistas.ufrj.br/index.php/aigeo/article/view/6943
identifier_str_mv 10.11137/2012_2_140_151
dc.language.iso.fl_str_mv por
language por
dc.relation.none.fl_str_mv https://revistas.ufrj.br/index.php/aigeo/article/view/6943/5510
dc.rights.driver.fl_str_mv Copyright (c) 2012 Anuário do Instituto de Geociências
http://creativecommons.org/licenses/by/4.0
info:eu-repo/semantics/openAccess
rights_invalid_str_mv Copyright (c) 2012 Anuário do Instituto de Geociências
http://creativecommons.org/licenses/by/4.0
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Universidade Federal do Rio de Janeiro
publisher.none.fl_str_mv Universidade Federal do Rio de Janeiro
dc.source.none.fl_str_mv Anuário do Instituto de Geociências; Vol 35, No 2 (2012); 140-151
Anuário do Instituto de Geociências; Vol 35, No 2 (2012); 140-151
1982-3908
0101-9759
reponame:Anuário do Instituto de Geociências (Online)
instname:Universidade Federal do Rio de Janeiro (UFRJ)
instacron:UFRJ
instname_str Universidade Federal do Rio de Janeiro (UFRJ)
instacron_str UFRJ
institution UFRJ
reponame_str Anuário do Instituto de Geociências (Online)
collection Anuário do Instituto de Geociências (Online)
repository.name.fl_str_mv Anuário do Instituto de Geociências (Online) - Universidade Federal do Rio de Janeiro (UFRJ)
repository.mail.fl_str_mv anuario@igeo.ufrj.br||
_version_ 1797053545604710400

Registros relacionados