O método radiométrico RB-Sr aplicado em rochas sedimentares o exemplo da bacia do Paraná, Brasil

Detalhes bibliográficos
Autor(a) principal: Silva, Diogo Rodrigues Andrade da
Data de Publicação: 2006
Outros Autores: Mizusaki, Ana Maria Pimentel, Anjos, Sylvia Maria Couto dos, Conceição, Rommulo Vieira
Tipo de documento: Artigo
Idioma: por
Título da fonte: Repositório Institucional da UFRGS
Texto Completo: http://hdl.handle.net/10183/22628
Resumo: The Rb-Sr method has been successfully applied to argillaceous sedimentary rocks in order to supply parameters for the definition of their depositional ages. In many studied cases, despite the geologically significant results, there are doubts concerning the interpretation of the obtained data and their limitations. This happens because sedimentary rocks are considered to be the mixture of detrital fragments of diverse sources, and therefore is the possibility of contain an isotopic record of their source rocks. The Rb-Sr method, when applied to mudrocks, allows constraining absolute depositional ages, owing to the resetting of the isotopic Rb/Sr system during deposition. This process is called isotopic homogenization in the depositional environment. Some special care must be taken with respect to sampling, sample grain size, depositional setting, and mineralogical composition. Nevertheless, questions still remain when concerning this methodology, particularly on the real occurrence and extent of the isotopic homogenization in the sedimentary environments. In the present work, the Rb-Sr method has been applied to samples of sedimentary rocks collected from different units representing several depositional settings from the Paraná Basin. The parameters responsible by the isotopic homogenization of Sr have been evaluated. The obtained results allowed the improvement of the application of the Rb-Sr method to sedimentary rocks, and significant results concerning depositional ages were obtained.
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spelling Silva, Diogo Rodrigues Andrade daMizusaki, Ana Maria PimentelAnjos, Sylvia Maria Couto dosConceição, Rommulo Vieira2010-05-20T04:16:27Z20061518-2398http://hdl.handle.net/10183/22628000603253The Rb-Sr method has been successfully applied to argillaceous sedimentary rocks in order to supply parameters for the definition of their depositional ages. In many studied cases, despite the geologically significant results, there are doubts concerning the interpretation of the obtained data and their limitations. This happens because sedimentary rocks are considered to be the mixture of detrital fragments of diverse sources, and therefore is the possibility of contain an isotopic record of their source rocks. The Rb-Sr method, when applied to mudrocks, allows constraining absolute depositional ages, owing to the resetting of the isotopic Rb/Sr system during deposition. This process is called isotopic homogenization in the depositional environment. Some special care must be taken with respect to sampling, sample grain size, depositional setting, and mineralogical composition. Nevertheless, questions still remain when concerning this methodology, particularly on the real occurrence and extent of the isotopic homogenization in the sedimentary environments. In the present work, the Rb-Sr method has been applied to samples of sedimentary rocks collected from different units representing several depositional settings from the Paraná Basin. The parameters responsible by the isotopic homogenization of Sr have been evaluated. The obtained results allowed the improvement of the application of the Rb-Sr method to sedimentary rocks, and significant results concerning depositional ages were obtained.application/pdfporPesquisas em Geociências. Vol. 33, n. 1 (2006), p. 83-100Rochas sedimentares : Método radiométricoRb-Sr datingSedimentary rocksParaná BasinDepositional agesO método radiométrico RB-Sr aplicado em rochas sedimentares o exemplo da bacia do Paraná, Brasilinfo: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:UFRGSORIGINAL000603253.pdf000603253.pdfTexto completoapplication/pdf4023840http://www.lume.ufrgs.br/bitstream/10183/22628/1/000603253.pdf24b38f15a4c15d0d5b36a43e96f340dbMD51TEXT000603253.pdf.txt000603253.pdf.txtExtracted Texttext/plain64417http://www.lume.ufrgs.br/bitstream/10183/22628/2/000603253.pdf.txta088475108aa37cfbfacb7f5f2caa85dMD52THUMBNAIL000603253.pdf.jpg000603253.pdf.jpgGenerated Thumbnailimage/jpeg1820http://www.lume.ufrgs.br/bitstream/10183/22628/3/000603253.pdf.jpge2294618702e9407c006da23ed68b88fMD5310183/226282018-10-17 07:54:13.947oai:www.lume.ufrgs.br:10183/22628Repositório de PublicaçõesPUBhttps://lume.ufrgs.br/oai/requestopendoar:2018-10-17T10:54:13Repositório Institucional da UFRGS - Universidade Federal do Rio Grande do Sul (UFRGS)false
dc.title.pt_BR.fl_str_mv O método radiométrico RB-Sr aplicado em rochas sedimentares o exemplo da bacia do Paraná, Brasil
title O método radiométrico RB-Sr aplicado em rochas sedimentares o exemplo da bacia do Paraná, Brasil
spellingShingle O método radiométrico RB-Sr aplicado em rochas sedimentares o exemplo da bacia do Paraná, Brasil
Silva, Diogo Rodrigues Andrade da
Rochas sedimentares : Método radiométrico
Rb-Sr dating
Sedimentary rocks
Paraná Basin
Depositional ages
title_short O método radiométrico RB-Sr aplicado em rochas sedimentares o exemplo da bacia do Paraná, Brasil
title_full O método radiométrico RB-Sr aplicado em rochas sedimentares o exemplo da bacia do Paraná, Brasil
title_fullStr O método radiométrico RB-Sr aplicado em rochas sedimentares o exemplo da bacia do Paraná, Brasil
title_full_unstemmed O método radiométrico RB-Sr aplicado em rochas sedimentares o exemplo da bacia do Paraná, Brasil
title_sort O método radiométrico RB-Sr aplicado em rochas sedimentares o exemplo da bacia do Paraná, Brasil
author Silva, Diogo Rodrigues Andrade da
author_facet Silva, Diogo Rodrigues Andrade da
Mizusaki, Ana Maria Pimentel
Anjos, Sylvia Maria Couto dos
Conceição, Rommulo Vieira
author_role author
author2 Mizusaki, Ana Maria Pimentel
Anjos, Sylvia Maria Couto dos
Conceição, Rommulo Vieira
author2_role author
author
author
dc.contributor.author.fl_str_mv Silva, Diogo Rodrigues Andrade da
Mizusaki, Ana Maria Pimentel
Anjos, Sylvia Maria Couto dos
Conceição, Rommulo Vieira
dc.subject.por.fl_str_mv Rochas sedimentares : Método radiométrico
topic Rochas sedimentares : Método radiométrico
Rb-Sr dating
Sedimentary rocks
Paraná Basin
Depositional ages
dc.subject.eng.fl_str_mv Rb-Sr dating
Sedimentary rocks
Paraná Basin
Depositional ages
description The Rb-Sr method has been successfully applied to argillaceous sedimentary rocks in order to supply parameters for the definition of their depositional ages. In many studied cases, despite the geologically significant results, there are doubts concerning the interpretation of the obtained data and their limitations. This happens because sedimentary rocks are considered to be the mixture of detrital fragments of diverse sources, and therefore is the possibility of contain an isotopic record of their source rocks. The Rb-Sr method, when applied to mudrocks, allows constraining absolute depositional ages, owing to the resetting of the isotopic Rb/Sr system during deposition. This process is called isotopic homogenization in the depositional environment. Some special care must be taken with respect to sampling, sample grain size, depositional setting, and mineralogical composition. Nevertheless, questions still remain when concerning this methodology, particularly on the real occurrence and extent of the isotopic homogenization in the sedimentary environments. In the present work, the Rb-Sr method has been applied to samples of sedimentary rocks collected from different units representing several depositional settings from the Paraná Basin. The parameters responsible by the isotopic homogenization of Sr have been evaluated. The obtained results allowed the improvement of the application of the Rb-Sr method to sedimentary rocks, and significant results concerning depositional ages were obtained.
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dc.relation.ispartof.pt_BR.fl_str_mv Pesquisas em Geociências. Vol. 33, n. 1 (2006), p. 83-100
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