Aplicação da estratigrafia de sequências para caracterização em multiescala de reservatórios no Grupo Guatá (Eopermiano da Bacia do Paraná) na Região São Gabriel-RS, Brasil

Detailed stratigraphic analysis of the Early Permian Rio Bonito and Palermo Formations of the intracratonic Paraná Basin in the region of São Gabriel County has been used for a study on reservoir characterization of paralic sandstones. Two main depositional systems were recognized, a fluvial-dominat...

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Autores: Küchle, Juliano, Holz, Michael
Formato: artículo
Estado:Versión publicada
Fecha de publicación:2002
País:Brasil
Recursos:Universidade Federal do Rio Grande do Sul (UFRGS)
Repositorio:Repositório Institucional da UFRGS
Idioma:portugués
OAI Identifier:oai:www.lume.ufrgs.br:10183/22578
Acesso em linha:http://hdl.handle.net/10183/22578
Access Level:acceso abierto
Palavra-chave:Formação Rio Bonito : Rio Grande do Sul
Estratigrafia de seqüências : Formação Rio Bonito
Reservoir characterization
Rio Bonito formation
Sequence stratigraphy
Multiscale models
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spelling 2010-05-20T04:16:13Z20021518-2398http://hdl.handle.net/10183/22578000373887Detailed stratigraphic analysis of the Early Permian Rio Bonito and Palermo Formations of the intracratonic Paraná Basin in the region of São Gabriel County has been used for a study on reservoir characterization of paralic sandstones. Two main depositional systems were recognized, a fluvial-dominated delta system at the base and a wavedominated barrier island system at the top, with an intervening succession characterized by a delta system with alternated wave and fluvial influence. The succession is divided in two third-order depositional sequences, enclosing thirteen fourthorder parasequences. This high-resolution stratigraphic framework was the base for a multiscale approach on reservoir characterization of the paralic sandstone bodies of the two sequences. Reservoir heterogeneities are discussed, starting from the scale of depositonal sequence (heterogeneity level 1), passing down to heterogeneity at the scale of systems tracts (heterogeneity level 2) and finalizing with an approach at parasequence scale (heterogeneity level 3). Main control on heterogeneity at the first level - depositional sequences - is base-level variation as generating mechanism for unconformities (sequence boundaries) and the sediment type and rate. At the second level -systems tracts - the reservoir heterogeneity is controlled by the lateral and vertical variations in thickness of particular systems within the different systems tracts and by the stratigraphic signatures of the bounding surfaces (sequence boundaries, transgressive surfaces and flooding surfaces), and at the third level the minor flooding surfaces control internal heterogeneity, reservoir continuity and connectivities between reservoirs. At this scale, five paralic reservoir bodies were recognized, with thickness range from 5 to 25 meters.application/pdfporPesquisas em Geociências. Porto Alegre, RS. Vol. 29, n. 2 (2002), p. 3-20Formação Rio Bonito : Rio Grande do SulEstratigrafia de seqüências : Formação Rio BonitoReservoir characterizationRio Bonito formationSequence stratigraphyMultiscale modelsAplicação da estratigrafia de sequências para caracterização em multiescala de reservatórios no Grupo Guatá (Eopermiano da Bacia do Paraná) na Região São Gabriel-RS, 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:UFRGSKüchle, JulianoHolz, MichaelTEXT000373887.pdf.txt000373887.pdf.txtExtracted Texttext/plain51407http://www.lume.ufrgs.br/bitstream/10183/22578/2/000373887.pdf.txt0ec8d72df2889b0e55ea96d480383973MD52ORIGINAL000373887.pdf000373887.pdfTexto completoapplication/pdf340447http://www.lume.ufrgs.br/bitstream/10183/22578/1/000373887.pdf8ca72f73bced50d253a65daee8e95493MD51THUMBNAIL000373887.pdf.jpg000373887.pdf.jpgGenerated Thumbnailimage/jpeg1758http://www.lume.ufrgs.br/bitstream/10183/22578/3/000373887.pdf.jpg4cb8b0ab28b987f36a56c5b3dd3e1745MD5310183/225782018-10-08 09:24:21.758oai:www.lume.ufrgs.br:10183/22578Repositório InstitucionalPUBhttps://lume.ufrgs.br/oai/requestlume@ufrgs.bropendoar:2018-10-08T12:24:21Repositório Institucional da UFRGS - Universidade Federal do Rio Grande do Sul (UFRGS)false
dc.title.pt_BR.fl_str_mv Aplicação da estratigrafia de sequências para caracterização em multiescala de reservatórios no Grupo Guatá (Eopermiano da Bacia do Paraná) na Região São Gabriel-RS, Brasil
title Aplicação da estratigrafia de sequências para caracterização em multiescala de reservatórios no Grupo Guatá (Eopermiano da Bacia do Paraná) na Região São Gabriel-RS, Brasil
spellingShingle Aplicação da estratigrafia de sequências para caracterização em multiescala de reservatórios no Grupo Guatá (Eopermiano da Bacia do Paraná) na Região São Gabriel-RS, Brasil
Küchle, Juliano
Formação Rio Bonito : Rio Grande do Sul
Estratigrafia de seqüências : Formação Rio Bonito
Reservoir characterization
Rio Bonito formation
Sequence stratigraphy
Multiscale models
title_short Aplicação da estratigrafia de sequências para caracterização em multiescala de reservatórios no Grupo Guatá (Eopermiano da Bacia do Paraná) na Região São Gabriel-RS, Brasil
title_full Aplicação da estratigrafia de sequências para caracterização em multiescala de reservatórios no Grupo Guatá (Eopermiano da Bacia do Paraná) na Região São Gabriel-RS, Brasil
title_fullStr Aplicação da estratigrafia de sequências para caracterização em multiescala de reservatórios no Grupo Guatá (Eopermiano da Bacia do Paraná) na Região São Gabriel-RS, Brasil
title_full_unstemmed Aplicação da estratigrafia de sequências para caracterização em multiescala de reservatórios no Grupo Guatá (Eopermiano da Bacia do Paraná) na Região São Gabriel-RS, Brasil
title_sort Aplicação da estratigrafia de sequências para caracterização em multiescala de reservatórios no Grupo Guatá (Eopermiano da Bacia do Paraná) na Região São Gabriel-RS, Brasil
dc.creator.none.fl_str_mv Küchle, Juliano
Holz, Michael
author Küchle, Juliano
author_facet Küchle, Juliano
Holz, Michael
author_role author
author2 Holz, Michael
author2_role author
dc.subject.por.fl_str_mv Formação Rio Bonito : Rio Grande do Sul
Estratigrafia de seqüências : Formação Rio Bonito
topic Formação Rio Bonito : Rio Grande do Sul
Estratigrafia de seqüências : Formação Rio Bonito
Reservoir characterization
Rio Bonito formation
Sequence stratigraphy
Multiscale models
dc.subject.eng.fl_str_mv Reservoir characterization
Rio Bonito formation
Sequence stratigraphy
Multiscale models
description Detailed stratigraphic analysis of the Early Permian Rio Bonito and Palermo Formations of the intracratonic Paraná Basin in the region of São Gabriel County has been used for a study on reservoir characterization of paralic sandstones. Two main depositional systems were recognized, a fluvial-dominated delta system at the base and a wavedominated barrier island system at the top, with an intervening succession characterized by a delta system with alternated wave and fluvial influence. The succession is divided in two third-order depositional sequences, enclosing thirteen fourthorder parasequences. This high-resolution stratigraphic framework was the base for a multiscale approach on reservoir characterization of the paralic sandstone bodies of the two sequences. Reservoir heterogeneities are discussed, starting from the scale of depositonal sequence (heterogeneity level 1), passing down to heterogeneity at the scale of systems tracts (heterogeneity level 2) and finalizing with an approach at parasequence scale (heterogeneity level 3). Main control on heterogeneity at the first level - depositional sequences - is base-level variation as generating mechanism for unconformities (sequence boundaries) and the sediment type and rate. At the second level -systems tracts - the reservoir heterogeneity is controlled by the lateral and vertical variations in thickness of particular systems within the different systems tracts and by the stratigraphic signatures of the bounding surfaces (sequence boundaries, transgressive surfaces and flooding surfaces), and at the third level the minor flooding surfaces control internal heterogeneity, reservoir continuity and connectivities between reservoirs. At this scale, five paralic reservoir bodies were recognized, with thickness range from 5 to 25 meters.
publishDate 2002
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dc.relation.ispartof.pt_BR.fl_str_mv Pesquisas em Geociências. Porto Alegre, RS. Vol. 29, n. 2 (2002), p. 3-20
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