Caracterização petrográfica e geoquímica da parte leste do Granito Europa, Distrito Mineiro de Pitinga, AM
Autor(a) principal: | |
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Data de Publicação: | 2007 |
Outros Autores: | , , , , , |
Tipo de documento: | Artigo |
Idioma: | por |
Título da fonte: | Repositório Institucional da UFRGS |
Texto Completo: | http://hdl.handle.net/10183/22631 |
Resumo: | The important mineral deposits of the Pitinga Mine, in the Amazonian region are related to A-type granites intruded in the Iricoumé Group. The Europa granite is one of these A-type rocks, intruded in the Iricoumé Group, which is represented by subaerial vulcanoclastic rocks (crystal-rich ignimbrites, thin massive tuffs and siltic tufaceous arenites) and minor hipabissal rhyolites. The volcanic rocks were probably generated in a caldera environment. The Europa granite is an alkali-feldspar peralkaline granite (hipersolvus) without genetic relationship with to the volcanic rocks of the Iricoumé Group, but it could have been generated during the resurgence stages. The petrographic and geochemical data attest that fractional crystallization process was the principal mechanism during the crystallization, which led to the generation of two different granitic facies. The Nb soil anomalies overprinted on the more differentiated facies are related to the astrophillite weathering. |
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Prado, MaurícioFerron, José Maximino Tadeu MirasLima, Evandro Fernandes deBastos Neto, Artur CezarPereira, Vitor PauloMinuzzi, Orlando Renato RigonPierosan, Ronaldo2010-05-20T04:16:28Z20071518-2398http://hdl.handle.net/10183/22631000639970The important mineral deposits of the Pitinga Mine, in the Amazonian region are related to A-type granites intruded in the Iricoumé Group. The Europa granite is one of these A-type rocks, intruded in the Iricoumé Group, which is represented by subaerial vulcanoclastic rocks (crystal-rich ignimbrites, thin massive tuffs and siltic tufaceous arenites) and minor hipabissal rhyolites. The volcanic rocks were probably generated in a caldera environment. The Europa granite is an alkali-feldspar peralkaline granite (hipersolvus) without genetic relationship with to the volcanic rocks of the Iricoumé Group, but it could have been generated during the resurgence stages. The petrographic and geochemical data attest that fractional crystallization process was the principal mechanism during the crystallization, which led to the generation of two different granitic facies. The Nb soil anomalies overprinted on the more differentiated facies are related to the astrophillite weathering.application/pdfporPesquisas em Geociências. Vol. 34, n. 1 (jan./jun. 2007), p. 77-90PetrografiaGeoquímicaGranito EuropaMina PitingaPitinga (Presidente Figueiredo, AM)Europa granitePitinga mineNiobiumA-type graniteCaracterização petrográfica e geoquímica da parte leste do Granito Europa, Distrito Mineiro de Pitinga, AMinfo:eu-repo/semantics/articleinfo:eu-repo/semantics/otherinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/openAccessreponame:Repositório Institucional da UFRGSinstname:Universidade Federal do Rio Grande do Sul (UFRGS)instacron:UFRGSTEXT000639970.pdf.txt000639970.pdf.txtExtracted Texttext/plain45835http://www.lume.ufrgs.br/bitstream/10183/22631/2/000639970.pdf.txtede4a69cb9dbe748cfc7e124bc666174MD52ORIGINAL000639970.pdf000639970.pdfTexto completoapplication/pdf1786504http://www.lume.ufrgs.br/bitstream/10183/22631/1/000639970.pdf905f1fff7810bb650b188e437c210af2MD51THUMBNAIL000639970.pdf.jpg000639970.pdf.jpgGenerated Thumbnailimage/jpeg2180http://www.lume.ufrgs.br/bitstream/10183/22631/3/000639970.pdf.jpg3561f5fb95245520799b176e961038b7MD5310183/226312020-08-28 03:33:13.746oai:www.lume.ufrgs.br:10183/22631Repositório de PublicaçõesPUBhttps://lume.ufrgs.br/oai/requestopendoar:2020-08-28T06:33:13Repositório Institucional da UFRGS - Universidade Federal do Rio Grande do Sul (UFRGS)false |
dc.title.pt_BR.fl_str_mv |
Caracterização petrográfica e geoquímica da parte leste do Granito Europa, Distrito Mineiro de Pitinga, AM |
title |
Caracterização petrográfica e geoquímica da parte leste do Granito Europa, Distrito Mineiro de Pitinga, AM |
spellingShingle |
Caracterização petrográfica e geoquímica da parte leste do Granito Europa, Distrito Mineiro de Pitinga, AM Prado, Maurício Petrografia Geoquímica Granito Europa Mina Pitinga Pitinga (Presidente Figueiredo, AM) Europa granite Pitinga mine Niobium A-type granite |
title_short |
Caracterização petrográfica e geoquímica da parte leste do Granito Europa, Distrito Mineiro de Pitinga, AM |
title_full |
Caracterização petrográfica e geoquímica da parte leste do Granito Europa, Distrito Mineiro de Pitinga, AM |
title_fullStr |
Caracterização petrográfica e geoquímica da parte leste do Granito Europa, Distrito Mineiro de Pitinga, AM |
title_full_unstemmed |
Caracterização petrográfica e geoquímica da parte leste do Granito Europa, Distrito Mineiro de Pitinga, AM |
title_sort |
Caracterização petrográfica e geoquímica da parte leste do Granito Europa, Distrito Mineiro de Pitinga, AM |
author |
Prado, Maurício |
author_facet |
Prado, Maurício Ferron, José Maximino Tadeu Miras Lima, Evandro Fernandes de Bastos Neto, Artur Cezar Pereira, Vitor Paulo Minuzzi, Orlando Renato Rigon Pierosan, Ronaldo |
author_role |
author |
author2 |
Ferron, José Maximino Tadeu Miras Lima, Evandro Fernandes de Bastos Neto, Artur Cezar Pereira, Vitor Paulo Minuzzi, Orlando Renato Rigon Pierosan, Ronaldo |
author2_role |
author author author author author author |
dc.contributor.author.fl_str_mv |
Prado, Maurício Ferron, José Maximino Tadeu Miras Lima, Evandro Fernandes de Bastos Neto, Artur Cezar Pereira, Vitor Paulo Minuzzi, Orlando Renato Rigon Pierosan, Ronaldo |
dc.subject.por.fl_str_mv |
Petrografia Geoquímica Granito Europa Mina Pitinga Pitinga (Presidente Figueiredo, AM) |
topic |
Petrografia Geoquímica Granito Europa Mina Pitinga Pitinga (Presidente Figueiredo, AM) Europa granite Pitinga mine Niobium A-type granite |
dc.subject.eng.fl_str_mv |
Europa granite Pitinga mine Niobium A-type granite |
description |
The important mineral deposits of the Pitinga Mine, in the Amazonian region are related to A-type granites intruded in the Iricoumé Group. The Europa granite is one of these A-type rocks, intruded in the Iricoumé Group, which is represented by subaerial vulcanoclastic rocks (crystal-rich ignimbrites, thin massive tuffs and siltic tufaceous arenites) and minor hipabissal rhyolites. The volcanic rocks were probably generated in a caldera environment. The Europa granite is an alkali-feldspar peralkaline granite (hipersolvus) without genetic relationship with to the volcanic rocks of the Iricoumé Group, but it could have been generated during the resurgence stages. The petrographic and geochemical data attest that fractional crystallization process was the principal mechanism during the crystallization, which led to the generation of two different granitic facies. The Nb soil anomalies overprinted on the more differentiated facies are related to the astrophillite weathering. |
publishDate |
2007 |
dc.date.issued.fl_str_mv |
2007 |
dc.date.accessioned.fl_str_mv |
2010-05-20T04:16:28Z |
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info:eu-repo/semantics/article info:eu-repo/semantics/other |
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http://hdl.handle.net/10183/22631 |
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1518-2398 |
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000639970 |
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http://hdl.handle.net/10183/22631 |
dc.language.iso.fl_str_mv |
por |
language |
por |
dc.relation.ispartof.pt_BR.fl_str_mv |
Pesquisas em Geociências. Vol. 34, n. 1 (jan./jun. 2007), p. 77-90 |
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info:eu-repo/semantics/openAccess |
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openAccess |
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application/pdf |
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