The passira anorthositic complex and associated granites: an example of the anorogenic magmatism (calymmian/statherian) event in the Eastern Borborema Province, NE Brazil
Autor(a) principal: | |
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Data de Publicação: | 2011 |
Outros Autores: | , , , , , |
Tipo de documento: | Artigo |
Idioma: | por |
Título da fonte: | Repositório Institucional de Geociências - RIGEO |
Texto Completo: | https://rigeo.sgb.gov.br/handle/doc/1083 |
Resumo: | The Passira Anorthositic Complex (PAC) is situated in Pernambuco State, Northeastern Brazil, within the Rio Capibaribe Terrain of the Borborema Province. Host rocks are rhiacian migmatitic gneisses. The PAC is a massif-type complex of batholithic proportions composed mainly of metamorphosed anorthosite, gabbro, norite, diorite and ultramafic lenses mineralized in Fe-Ti oxide minerals. A dyke swarm formed by apatite-rich ferro-diorite enriched in Zr, Ba and LREE, occurs around the complex. A multicrystal U-Pb zircon age of 1.70+0.02 Ga was obtained for the anorthosite, which is interpreted as|the age of crystallization. The associated granites (now orthogneisses) include metaluminous alkaline; sub-alkaline garnet-bearing and peraluminous types having anorogenic geochemical characteristics. They have U-Pb ages between 1.58±0.09 Ga and 1.68±0.09 Ga, obtained in zircon and monazite monocrystals by laser ablation mass spectrometry. The PAC and associated granites behaved as a tectonic unit during the Brasiliano-age deformations. The association was formed in Rio Capibaribe Terrain during an extensional event occurred at the Statherian-Callymian transition |
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ACCIOLY, Ana Cláudia de AguiarMCREATH, IanGUIMARÃES, Ignez P.SANTOS, Edilton J.VANNUCCI, RicardoSANTOS, Almany C.SANTOS, Carlos Alberto2013-12-19T16:35:11Z2013-12-19T16:35:11Z2011ACCIOLY, Ana Cláudia Aguiar; MCREATH, Ian; GUIMARÃES, Ignez P.; SANTOS, Edilton J.; VANNUCCI, Ricardo; SANTOS, Almany C.; SANTOS, Carlos Alberto. The passira anorthositic complex and associated granites: an example of the anorogenic magmatism (calymmian/statherian) event in the Eastern Borborema Province, NE Brazil. In: CONGRESSO BRASILEIRO DE GEOQUIMICA, 13., 2011, Gramado, RS. Anais [...] Gramado, RS: SBGq 2011.https://rigeo.sgb.gov.br/handle/doc/1083The Passira Anorthositic Complex (PAC) is situated in Pernambuco State, Northeastern Brazil, within the Rio Capibaribe Terrain of the Borborema Province. Host rocks are rhiacian migmatitic gneisses. The PAC is a massif-type complex of batholithic proportions composed mainly of metamorphosed anorthosite, gabbro, norite, diorite and ultramafic lenses mineralized in Fe-Ti oxide minerals. A dyke swarm formed by apatite-rich ferro-diorite enriched in Zr, Ba and LREE, occurs around the complex. A multicrystal U-Pb zircon age of 1.70+0.02 Ga was obtained for the anorthosite, which is interpreted as|the age of crystallization. The associated granites (now orthogneisses) include metaluminous alkaline; sub-alkaline garnet-bearing and peraluminous types having anorogenic geochemical characteristics. They have U-Pb ages between 1.58±0.09 Ga and 1.68±0.09 Ga, obtained in zircon and monazite monocrystals by laser ablation mass spectrometry. The PAC and associated granites behaved as a tectonic unit during the Brasiliano-age deformations. The association was formed in Rio Capibaribe Terrain during an extensional event occurred at the Statherian-Callymian transitionGEOLOGIAGEOQUÍMICAMAGMATISMO ANOROGÊNICOGRANITÓIDES CALIMINIANOSPROVÍNCIA BORBOREMABRASILNORDESTEThe passira anorthositic complex and associated granites: an example of the anorogenic magmatism (calymmian/statherian) event in the Eastern Borborema Province, NE Brazilinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleGramado, RSporreponame:Repositório Institucional de Geociências - RIGEOinstname:Companhia de Pesquisa de Recursos Minerais (CPRM)instacron:CPRMinfo:eu-repo/semantics/openAccessTEXTEvento_CGQ02T01.pdf.txtEvento_CGQ02T01.pdf.txtExtracted texttext/plain9751http://rigeo.sgb.gov.br/jspui/bitstream/doc/1083/2/Evento_CGQ02T01.pdf.txt7751499a9fd73db305d2dbe55c44a150MD52THUMBNAILEvento_CGQ02T01.pdf.jpgEvento_CGQ02T01.pdf.jpgGenerated Thumbnailimage/jpeg1838http://rigeo.sgb.gov.br/jspui/bitstream/doc/1083/3/Evento_CGQ02T01.pdf.jpgb5d9efe7ac34fe68863ce2ac223d4a72MD53ORIGINALEvento_CGQ02T01.pdfEvento_CGQ02T01.pdfproducao cientificaapplication/pdf1300860http://rigeo.sgb.gov.br/jspui/bitstream/doc/1083/1/Evento_CGQ02T01.pdfce6fb8a10bb0e7d78776f0abf0b22780MD51doc/10832024-04-30 09:24:10.823oai:rigeo.sgb.gov.br:doc/1083Repositório InstitucionalONGhttps://rigeo.sgb.gov.br/oai/request https://rigeo.cprm.gov.br/oai/requestrigeo@sgb.gov.bropendoar:2024-04-30T12:24:10Repositório Institucional de Geociências - RIGEO - Companhia de Pesquisa de Recursos Minerais (CPRM)false |
dc.title.none.fl_str_mv |
The passira anorthositic complex and associated granites: an example of the anorogenic magmatism (calymmian/statherian) event in the Eastern Borborema Province, NE Brazil |
title |
The passira anorthositic complex and associated granites: an example of the anorogenic magmatism (calymmian/statherian) event in the Eastern Borborema Province, NE Brazil |
spellingShingle |
The passira anorthositic complex and associated granites: an example of the anorogenic magmatism (calymmian/statherian) event in the Eastern Borborema Province, NE Brazil ACCIOLY, Ana Cláudia de Aguiar GEOLOGIA GEOQUÍMICA MAGMATISMO ANOROGÊNICO GRANITÓIDES CALIMINIANOS PROVÍNCIA BORBOREMA BRASIL NORDESTE |
title_short |
The passira anorthositic complex and associated granites: an example of the anorogenic magmatism (calymmian/statherian) event in the Eastern Borborema Province, NE Brazil |
title_full |
The passira anorthositic complex and associated granites: an example of the anorogenic magmatism (calymmian/statherian) event in the Eastern Borborema Province, NE Brazil |
title_fullStr |
The passira anorthositic complex and associated granites: an example of the anorogenic magmatism (calymmian/statherian) event in the Eastern Borborema Province, NE Brazil |
title_full_unstemmed |
The passira anorthositic complex and associated granites: an example of the anorogenic magmatism (calymmian/statherian) event in the Eastern Borborema Province, NE Brazil |
title_sort |
The passira anorthositic complex and associated granites: an example of the anorogenic magmatism (calymmian/statherian) event in the Eastern Borborema Province, NE Brazil |
author |
ACCIOLY, Ana Cláudia de Aguiar |
author_facet |
ACCIOLY, Ana Cláudia de Aguiar MCREATH, Ian GUIMARÃES, Ignez P. SANTOS, Edilton J. VANNUCCI, Ricardo SANTOS, Almany C. SANTOS, Carlos Alberto |
author_role |
author |
author2 |
MCREATH, Ian GUIMARÃES, Ignez P. SANTOS, Edilton J. VANNUCCI, Ricardo SANTOS, Almany C. SANTOS, Carlos Alberto |
author2_role |
author author author author author author |
dc.contributor.author.fl_str_mv |
ACCIOLY, Ana Cláudia de Aguiar MCREATH, Ian GUIMARÃES, Ignez P. SANTOS, Edilton J. VANNUCCI, Ricardo SANTOS, Almany C. SANTOS, Carlos Alberto |
dc.subject.por.fl_str_mv |
GEOLOGIA GEOQUÍMICA MAGMATISMO ANOROGÊNICO GRANITÓIDES CALIMINIANOS PROVÍNCIA BORBOREMA BRASIL NORDESTE |
topic |
GEOLOGIA GEOQUÍMICA MAGMATISMO ANOROGÊNICO GRANITÓIDES CALIMINIANOS PROVÍNCIA BORBOREMA BRASIL NORDESTE |
description |
The Passira Anorthositic Complex (PAC) is situated in Pernambuco State, Northeastern Brazil, within the Rio Capibaribe Terrain of the Borborema Province. Host rocks are rhiacian migmatitic gneisses. The PAC is a massif-type complex of batholithic proportions composed mainly of metamorphosed anorthosite, gabbro, norite, diorite and ultramafic lenses mineralized in Fe-Ti oxide minerals. A dyke swarm formed by apatite-rich ferro-diorite enriched in Zr, Ba and LREE, occurs around the complex. A multicrystal U-Pb zircon age of 1.70+0.02 Ga was obtained for the anorthosite, which is interpreted as|the age of crystallization. The associated granites (now orthogneisses) include metaluminous alkaline; sub-alkaline garnet-bearing and peraluminous types having anorogenic geochemical characteristics. They have U-Pb ages between 1.58±0.09 Ga and 1.68±0.09 Ga, obtained in zircon and monazite monocrystals by laser ablation mass spectrometry. The PAC and associated granites behaved as a tectonic unit during the Brasiliano-age deformations. The association was formed in Rio Capibaribe Terrain during an extensional event occurred at the Statherian-Callymian transition |
publishDate |
2011 |
dc.date.issued.fl_str_mv |
2011 |
dc.date.accessioned.fl_str_mv |
2013-12-19T16:35:11Z |
dc.date.available.fl_str_mv |
2013-12-19T16:35:11Z |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article |
format |
article |
status_str |
publishedVersion |
dc.identifier.citation.fl_str_mv |
ACCIOLY, Ana Cláudia Aguiar; MCREATH, Ian; GUIMARÃES, Ignez P.; SANTOS, Edilton J.; VANNUCCI, Ricardo; SANTOS, Almany C.; SANTOS, Carlos Alberto. The passira anorthositic complex and associated granites: an example of the anorogenic magmatism (calymmian/statherian) event in the Eastern Borborema Province, NE Brazil. In: CONGRESSO BRASILEIRO DE GEOQUIMICA, 13., 2011, Gramado, RS. Anais [...] Gramado, RS: SBGq 2011. |
dc.identifier.uri.fl_str_mv |
https://rigeo.sgb.gov.br/handle/doc/1083 |
identifier_str_mv |
ACCIOLY, Ana Cláudia Aguiar; MCREATH, Ian; GUIMARÃES, Ignez P.; SANTOS, Edilton J.; VANNUCCI, Ricardo; SANTOS, Almany C.; SANTOS, Carlos Alberto. The passira anorthositic complex and associated granites: an example of the anorogenic magmatism (calymmian/statherian) event in the Eastern Borborema Province, NE Brazil. In: CONGRESSO BRASILEIRO DE GEOQUIMICA, 13., 2011, Gramado, RS. Anais [...] Gramado, RS: SBGq 2011. |
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https://rigeo.sgb.gov.br/handle/doc/1083 |
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