Interpretação sísmica dos eventos magmáticos pós-aptianos no alto de Cabo Frio, sudeste do Brasil, gênese e relação com os lineamentos pré-sal
Autor(a) principal: | |
---|---|
Data de Publicação: | 2006 |
Tipo de documento: | Tese |
Idioma: | por |
Título da fonte: | Biblioteca Digital de Teses e Dissertações da UERJ |
Texto Completo: | http://www.bdtd.uerj.br/handle/1/7000 |
Resumo: | The continental shelf of the Cabo Frio Area, at the southern part of the Campos Basin, shows unique features in its tectono-sedimentary evolution when compared to other areas of the Campos and Santos basins. The presence of a regular pattern of antithetic faults in the basement and in the syn-rift and the post-rift sedimentary sections, along with important magmatic events in the Late Cretaceous and Early Tertiary sequences (whose climax took place in the earli er portion of the Middle Eocene) are some of these features. This work presents a historical perspective of the human perception of the magmatic events, from the ancient mythic and theologic theories to the current debate between plumers and non-plumers. These informations are needed to allow a better understanding of the conclusions of the present thesis. The present study was based on the analyses of seismic, satellite, magnetic, gravimetric and well data, as well as rock samples collected in dikes cropping out at the Arraial do Cabo Peninsula, the nearest onshore position at the boundary between the offshore Santos and Campos Basins. This thesis has confirmed the results of previous research that had identified two major magmatic pulses, one in the late Cretaceous and the other in the Early Tertiary (~83 and 50 My, respectively). There is also seismic evidence for volcanic edifices formed during the Albian, Maastrichtian and Paleocene times. The analyses of seismic reflection and well log data, in the working area, points to a set of diagnostic features that can lead to the identification of magmatic events and the distinction of intrusive from extrusive rocks, as well as their intercalations with epiclastic sedimentary sequences. Extrusive magmatic events can be recognized in seismic reflection data as chaotic seismofacies with well defined tops and poorly defined bases; these seismofacies are interpreted as a result of interbedding submarine lava flows and epiclastic and volcaniclastic sediments, along with slumps and shallow intrusions (sills). The presence of well shaped conic edifices also points to extrusive magmatism. Dikes and lava flows are recognized by strong positive reflections with abrupt lateral ends. Thicker dolerite sills may be recognized by re flection free zones with strong reflections in their tops and bases. The criteria proposed by this thesis may be used to identify and classify magmatic events in any context where they are associated with sedimentary sequences. The thesis also shows the seismic signatures of nonmagmatic events, which comprise a different range of geologic features that may induce the geophysicists and geologists to interpret them as magmatic events. Among these features, evaporites, turbiditic mounds, mud volcanoes originated by gas escape, slump seismofacies and carbonate deposits are the most important ones. Some alternative interpretations to explain the genesis of this magmatism are presented, which do not take into account the classic model of mantle plumes. The mapping of the main feeder dikes, in 2D and 3D reflection seismic sections, has revealed that they have a predominant SE-NW direction, coincident with the alignment of the Cruzeiro do Sul Deformation Zone, which includes the Jean Charcot submarine mounds and the volcanic mounds on and around the Cabo Frio High. This observation is coherent with the characteristics of the preexisting and reactivated strike-slip faults on land and the orientation of their transtensional component. Moreover, it is shown that the largest volumes of magmatic rocks, intercalated in the sedimentary section, are located at areas of intersections between fault zones trending SE-NW (strike -slip faults) and SW-NE (normal faults), as are the onshore alkaline bodies of the Poços de Caldas Cabo Frio alignment. |
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Thomaz Filho, AntônioThomaz Filho, AntônioFávera, Jorge Carlos Dellahttp://lattes.cnpq.br/4231307714993717Heilbron, Monica da Costa Pereira Lavallehttp://lattes.cnpq.br/3847685914783573Oliveira, Luiz Otávio Aguiarhttp://lattes.cnpq.br/4345913412613509Montovani, Marta Silvia Mariahttp://lattes.cnpq.br/1193370786873409http://lattes.cnpq.br/8134033324023464Oreiro, Sérgio Goulart2021-01-05T15:30:41Z2007-11-292006-12-15OREIRO, Sérgio Goulart. Interpretação sísmica dos eventos magmáticos pós-aptianos no alto de Cabo Frio, sudeste do Brasil, gênese e relação com os lineamentos pré-sal. 2006. 180 f. Tese (Doutorado em Análise de Bacias;Tectônia, Petrologia e Recursos Minerais) - Universidade do Estado do Rio de Janeiro, Rio de Janeiro, 2006.http://www.bdtd.uerj.br/handle/1/7000The continental shelf of the Cabo Frio Area, at the southern part of the Campos Basin, shows unique features in its tectono-sedimentary evolution when compared to other areas of the Campos and Santos basins. The presence of a regular pattern of antithetic faults in the basement and in the syn-rift and the post-rift sedimentary sections, along with important magmatic events in the Late Cretaceous and Early Tertiary sequences (whose climax took place in the earli er portion of the Middle Eocene) are some of these features. This work presents a historical perspective of the human perception of the magmatic events, from the ancient mythic and theologic theories to the current debate between plumers and non-plumers. These informations are needed to allow a better understanding of the conclusions of the present thesis. The present study was based on the analyses of seismic, satellite, magnetic, gravimetric and well data, as well as rock samples collected in dikes cropping out at the Arraial do Cabo Peninsula, the nearest onshore position at the boundary between the offshore Santos and Campos Basins. This thesis has confirmed the results of previous research that had identified two major magmatic pulses, one in the late Cretaceous and the other in the Early Tertiary (~83 and 50 My, respectively). There is also seismic evidence for volcanic edifices formed during the Albian, Maastrichtian and Paleocene times. The analyses of seismic reflection and well log data, in the working area, points to a set of diagnostic features that can lead to the identification of magmatic events and the distinction of intrusive from extrusive rocks, as well as their intercalations with epiclastic sedimentary sequences. Extrusive magmatic events can be recognized in seismic reflection data as chaotic seismofacies with well defined tops and poorly defined bases; these seismofacies are interpreted as a result of interbedding submarine lava flows and epiclastic and volcaniclastic sediments, along with slumps and shallow intrusions (sills). The presence of well shaped conic edifices also points to extrusive magmatism. Dikes and lava flows are recognized by strong positive reflections with abrupt lateral ends. Thicker dolerite sills may be recognized by re flection free zones with strong reflections in their tops and bases. The criteria proposed by this thesis may be used to identify and classify magmatic events in any context where they are associated with sedimentary sequences. The thesis also shows the seismic signatures of nonmagmatic events, which comprise a different range of geologic features that may induce the geophysicists and geologists to interpret them as magmatic events. Among these features, evaporites, turbiditic mounds, mud volcanoes originated by gas escape, slump seismofacies and carbonate deposits are the most important ones. Some alternative interpretations to explain the genesis of this magmatism are presented, which do not take into account the classic model of mantle plumes. The mapping of the main feeder dikes, in 2D and 3D reflection seismic sections, has revealed that they have a predominant SE-NW direction, coincident with the alignment of the Cruzeiro do Sul Deformation Zone, which includes the Jean Charcot submarine mounds and the volcanic mounds on and around the Cabo Frio High. This observation is coherent with the characteristics of the preexisting and reactivated strike-slip faults on land and the orientation of their transtensional component. Moreover, it is shown that the largest volumes of magmatic rocks, intercalated in the sedimentary section, are located at areas of intersections between fault zones trending SE-NW (strike -slip faults) and SW-NE (normal faults), as are the onshore alkaline bodies of the Poços de Caldas Cabo Frio alignment.A plataforma continental da área de Cabo Frio, localizada no extremo SW da Bacia de Campos e extremo NW da Bacia de Santos, possui distintas feições em sua evolução tectono -sedimentar quando comparada com outras áreas das referidas bacias. Entre essas feições, destaca-se a presença de falhas antitéticas no embasamento e nas seções sedimentares sin-rifte e pós-rifte, além de eventos magmáticos marcantes no Neocretácio e Eoterciário, com clímax no Eoceno Médio. O presente trabalho mostra uma perspectiva histórica da percepção humana dos fenômenos magmáticos, desde as primeiras teorias míticas e teológicas da antiguidade, até o atual debate entre os que adotam ou não o modelo de plumas mantélicas. Tais informações são necessárias para um melhor entendimento das conclusões aqui apresentadas. A base de dados do presente estudo consiste de análises detalhadas de dados de sísmica, de satélite, de métodos potenciais (magnéticos e gravimétricos) e de poços. Amostras de diques básicos na península de Arraial do Cabo, situada na porção continental mais próxima do limite entre as Bacias de Santos e de Campos, foram coletadas para estudos geocronológicos. O estudo integrado de todos esses dados confirmou o resultado de pesquisas anteriores, as quais identificaram dois eventos magmáticos principais, um no Santoniano/Campaniano (~ 83 Ma) e outro no Eoceno Médio (~ 50 Ma). Há também evidências, em seções sísmicas, de edifícios vulcânicos formados durante o Albiano, o Maastrichtiano e o Paleoceno. As análises de dados de sísmica de relexão e de perfis de poços, na área de estudo, revelaram uma série de feições diagnósticas para eventos magmáticos, incluindo a distinção entre eventos intrusivos dos extrusivos, bem como de intercalações entre os mesmos e seqüências sedimentares epiclásticas. Eventos magmáticos extrusivos podem ser identificados, nas seções sísmicas, como sismofácies caóticas com topos bem definidos e bases mal definidas. Tais sismofácies são interpretadas como o resultado da intercalação de derrames submarinos de lavas com sedimentos epiclásticos e vulcanoclásticos, juntamente com feições de escorregamentos e soleiras rasas. A presença de cones bem delimitados também constitui evidência de magmatismo extrusivo. Diques e derrames de lava são reconhecidos por fortes reflexões positivas com terminações laterais abruptas. Diques mais espessos de diabásio originam zonas com fracas reflexões, delimitadas acima e abaixo por fortes reflexões. Os critérios apresentados nessa tese podem ser aplicados a quaisquer contextos em que haja eventos magmáticos intercalados com seqüências sedimentares. A assinatura sísmica de eventos não- magmáticos é também mostrada; tais eventos correspondem a diferentes feições geológicas que podem ser interpretados por geofísicos e geólogos como sendo de origem magmática. Entre tais eventos, os mais importantes são os evaporitos, os mounds turbidíticos, os vulcões de lama originados por escape de gás e depósitos carbonáticos. Serão apresentadas algumas interpretações para a gênese do magmatismo pós-Aptiano na área em epígrafe, interpretações essas que não levam em conta o modelo clássico de plumas mantélicas. O mapeamento dos principais diques alimentadores, em seções sísmicas 2D e 3D, revelou que tais diques têm uma orientação preferencial SE-NW, coincidente com o alinhamento da Zona de deformações Cruzeiro do Sul, a qual inclui os Montes Submarinos Jean Charcot e as construções vulcânicas no Alto de Cabo Frio e suas cercanias. Tal observação é coerente com as características das falhas de rejeito direcional, preexistentes e reativadas nas áreas continentais próximas, e com a orientação do componente transtensional das mesmas. Além disso, comprova-se que os maiores volumes de rochas magmáticas, intercaladas na seção sedimentar, estão localizados nas áreas de interseção entre duas zonas de falhas com direção SE- NW (falhas de rejeito direcional) e SW-NE (falhas normais). O mesmo acontece com os corpos alcalinos do alinhamento Poços de Caldas-Cabo Frio.Submitted by Boris Flegr (boris@uerj.br) on 2021-01-05T15:30:41Z No. of bitstreams: 6 Pre textuais.pdf: 115257 bytes, checksum: 98c8e10d71272cbaf4309ca47116ecbd (MD5) Parte I a IV.pdf: 2851126 bytes, checksum: 8bbea06ededa0fc8f925c05c09641d7b (MD5) Parte V a VIII.pdf: 2101313 bytes, checksum: 181ae7e601a6f478dd333bc0911d1ff4 (MD5) Parte IX a X.pdf: 2939777 bytes, checksum: e433ec11fc378bda032084934ee0e050 (MD5) Parte XI.pdf: 1904184 bytes, checksum: 6e86314440bece2973b958d39914ab59 (MD5) Parte XII a XIV.pdf: 3162494 bytes, checksum: 0e6fcecf58658351d3a42164456d622d (MD5)Made available in DSpace on 2021-01-05T15:30:41Z (GMT). No. of bitstreams: 6 Pre textuais.pdf: 115257 bytes, checksum: 98c8e10d71272cbaf4309ca47116ecbd (MD5) Parte I a IV.pdf: 2851126 bytes, checksum: 8bbea06ededa0fc8f925c05c09641d7b (MD5) Parte V a VIII.pdf: 2101313 bytes, checksum: 181ae7e601a6f478dd333bc0911d1ff4 (MD5) Parte IX a X.pdf: 2939777 bytes, checksum: e433ec11fc378bda032084934ee0e050 (MD5) Parte XI.pdf: 1904184 bytes, checksum: 6e86314440bece2973b958d39914ab59 (MD5) Parte XII a XIV.pdf: 3162494 bytes, checksum: 0e6fcecf58658351d3a42164456d622d (MD5) Previous issue date: 2006-12-15application/pdfporUniversidade do Estado do Rio de JaneiroPrograma de Pós-Graduação em Análise de Bacias e Faixas MóveisUERJBRCentro de Tecnologia e Ciências::Faculdade de GeologiaMagmatismPlumesCabo Frio HighMagmatismoPlumas mantélicasAlto de Cabo FrioCNPQ::CIENCIAS EXATAS E DA TERRA::GEOCIENCIAS::GEOLOGIAInterpretação sísmica dos eventos magmáticos pós-aptianos no alto de Cabo Frio, sudeste do Brasil, gênese e relação com os lineamentos pré-salSeismic interpretation of post-aptian magmatic events in the Cabo Frio high, Southeast Brazil, its genesis and its relation with pre-salt alignmentsinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/doctoralThesisinfo:eu-repo/semantics/openAccessreponame:Biblioteca Digital de Teses e Dissertações da UERJinstname:Universidade do Estado do Rio de Janeiro (UERJ)instacron:UERJORIGINALPre textuais.pdfapplication/pdf115257http://www.bdtd.uerj.br/bitstream/1/7000/1/Pre+textuais.pdf98c8e10d71272cbaf4309ca47116ecbdMD51Parte I a IV.pdfapplication/pdf2851126http://www.bdtd.uerj.br/bitstream/1/7000/2/Parte+I+a+IV.pdf8bbea06ededa0fc8f925c05c09641d7bMD52Parte V a VIII.pdfapplication/pdf2101313http://www.bdtd.uerj.br/bitstream/1/7000/3/Parte+V+a+VIII.pdf181ae7e601a6f478dd333bc0911d1ff4MD53Parte IX a X.pdfapplication/pdf2939777http://www.bdtd.uerj.br/bitstream/1/7000/4/Parte+IX+a+X.pdfe433ec11fc378bda032084934ee0e050MD54Parte XI.pdfapplication/pdf1904184http://www.bdtd.uerj.br/bitstream/1/7000/5/Parte+XI.pdf6e86314440bece2973b958d39914ab59MD55Parte XII a XIV.pdfapplication/pdf3162494http://www.bdtd.uerj.br/bitstream/1/7000/6/Parte+XII+a+XIV.pdf0e6fcecf58658351d3a42164456d622dMD561/70002024-02-27 14:16:02.633oai:www.bdtd.uerj.br:1/7000Biblioteca Digital de Teses e Dissertaçõeshttp://www.bdtd.uerj.br/PUBhttps://www.bdtd.uerj.br:8443/oai/requestbdtd.suporte@uerj.bropendoar:29032024-02-27T17:16:02Biblioteca Digital de Teses e Dissertações da UERJ - Universidade do Estado do Rio de Janeiro (UERJ)false |
dc.title.por.fl_str_mv |
Interpretação sísmica dos eventos magmáticos pós-aptianos no alto de Cabo Frio, sudeste do Brasil, gênese e relação com os lineamentos pré-sal |
dc.title.alternative.eng.fl_str_mv |
Seismic interpretation of post-aptian magmatic events in the Cabo Frio high, Southeast Brazil, its genesis and its relation with pre-salt alignments |
title |
Interpretação sísmica dos eventos magmáticos pós-aptianos no alto de Cabo Frio, sudeste do Brasil, gênese e relação com os lineamentos pré-sal |
spellingShingle |
Interpretação sísmica dos eventos magmáticos pós-aptianos no alto de Cabo Frio, sudeste do Brasil, gênese e relação com os lineamentos pré-sal Oreiro, Sérgio Goulart Magmatism Plumes Cabo Frio High Magmatismo Plumas mantélicas Alto de Cabo Frio CNPQ::CIENCIAS EXATAS E DA TERRA::GEOCIENCIAS::GEOLOGIA |
title_short |
Interpretação sísmica dos eventos magmáticos pós-aptianos no alto de Cabo Frio, sudeste do Brasil, gênese e relação com os lineamentos pré-sal |
title_full |
Interpretação sísmica dos eventos magmáticos pós-aptianos no alto de Cabo Frio, sudeste do Brasil, gênese e relação com os lineamentos pré-sal |
title_fullStr |
Interpretação sísmica dos eventos magmáticos pós-aptianos no alto de Cabo Frio, sudeste do Brasil, gênese e relação com os lineamentos pré-sal |
title_full_unstemmed |
Interpretação sísmica dos eventos magmáticos pós-aptianos no alto de Cabo Frio, sudeste do Brasil, gênese e relação com os lineamentos pré-sal |
title_sort |
Interpretação sísmica dos eventos magmáticos pós-aptianos no alto de Cabo Frio, sudeste do Brasil, gênese e relação com os lineamentos pré-sal |
author |
Oreiro, Sérgio Goulart |
author_facet |
Oreiro, Sérgio Goulart |
author_role |
author |
dc.contributor.advisor1.fl_str_mv |
Thomaz Filho, Antônio |
dc.contributor.advisor1Lattes.fl_str_mv |
Thomaz Filho, Antônio |
dc.contributor.referee1.fl_str_mv |
Fávera, Jorge Carlos Della |
dc.contributor.referee1Lattes.fl_str_mv |
http://lattes.cnpq.br/4231307714993717 |
dc.contributor.referee2.fl_str_mv |
Heilbron, Monica da Costa Pereira Lavalle |
dc.contributor.referee2Lattes.fl_str_mv |
http://lattes.cnpq.br/3847685914783573 |
dc.contributor.referee3.fl_str_mv |
Oliveira, Luiz Otávio Aguiar |
dc.contributor.referee3Lattes.fl_str_mv |
http://lattes.cnpq.br/4345913412613509 |
dc.contributor.referee4.fl_str_mv |
Montovani, Marta Silvia Maria |
dc.contributor.referee4Lattes.fl_str_mv |
http://lattes.cnpq.br/1193370786873409 |
dc.contributor.authorLattes.fl_str_mv |
http://lattes.cnpq.br/8134033324023464 |
dc.contributor.author.fl_str_mv |
Oreiro, Sérgio Goulart |
contributor_str_mv |
Thomaz Filho, Antônio Fávera, Jorge Carlos Della Heilbron, Monica da Costa Pereira Lavalle Oliveira, Luiz Otávio Aguiar Montovani, Marta Silvia Maria |
dc.subject.eng.fl_str_mv |
Magmatism Plumes Cabo Frio High |
topic |
Magmatism Plumes Cabo Frio High Magmatismo Plumas mantélicas Alto de Cabo Frio CNPQ::CIENCIAS EXATAS E DA TERRA::GEOCIENCIAS::GEOLOGIA |
dc.subject.por.fl_str_mv |
Magmatismo Plumas mantélicas Alto de Cabo Frio |
dc.subject.cnpq.fl_str_mv |
CNPQ::CIENCIAS EXATAS E DA TERRA::GEOCIENCIAS::GEOLOGIA |
description |
The continental shelf of the Cabo Frio Area, at the southern part of the Campos Basin, shows unique features in its tectono-sedimentary evolution when compared to other areas of the Campos and Santos basins. The presence of a regular pattern of antithetic faults in the basement and in the syn-rift and the post-rift sedimentary sections, along with important magmatic events in the Late Cretaceous and Early Tertiary sequences (whose climax took place in the earli er portion of the Middle Eocene) are some of these features. This work presents a historical perspective of the human perception of the magmatic events, from the ancient mythic and theologic theories to the current debate between plumers and non-plumers. These informations are needed to allow a better understanding of the conclusions of the present thesis. The present study was based on the analyses of seismic, satellite, magnetic, gravimetric and well data, as well as rock samples collected in dikes cropping out at the Arraial do Cabo Peninsula, the nearest onshore position at the boundary between the offshore Santos and Campos Basins. This thesis has confirmed the results of previous research that had identified two major magmatic pulses, one in the late Cretaceous and the other in the Early Tertiary (~83 and 50 My, respectively). There is also seismic evidence for volcanic edifices formed during the Albian, Maastrichtian and Paleocene times. The analyses of seismic reflection and well log data, in the working area, points to a set of diagnostic features that can lead to the identification of magmatic events and the distinction of intrusive from extrusive rocks, as well as their intercalations with epiclastic sedimentary sequences. Extrusive magmatic events can be recognized in seismic reflection data as chaotic seismofacies with well defined tops and poorly defined bases; these seismofacies are interpreted as a result of interbedding submarine lava flows and epiclastic and volcaniclastic sediments, along with slumps and shallow intrusions (sills). The presence of well shaped conic edifices also points to extrusive magmatism. Dikes and lava flows are recognized by strong positive reflections with abrupt lateral ends. Thicker dolerite sills may be recognized by re flection free zones with strong reflections in their tops and bases. The criteria proposed by this thesis may be used to identify and classify magmatic events in any context where they are associated with sedimentary sequences. The thesis also shows the seismic signatures of nonmagmatic events, which comprise a different range of geologic features that may induce the geophysicists and geologists to interpret them as magmatic events. Among these features, evaporites, turbiditic mounds, mud volcanoes originated by gas escape, slump seismofacies and carbonate deposits are the most important ones. Some alternative interpretations to explain the genesis of this magmatism are presented, which do not take into account the classic model of mantle plumes. The mapping of the main feeder dikes, in 2D and 3D reflection seismic sections, has revealed that they have a predominant SE-NW direction, coincident with the alignment of the Cruzeiro do Sul Deformation Zone, which includes the Jean Charcot submarine mounds and the volcanic mounds on and around the Cabo Frio High. This observation is coherent with the characteristics of the preexisting and reactivated strike-slip faults on land and the orientation of their transtensional component. Moreover, it is shown that the largest volumes of magmatic rocks, intercalated in the sedimentary section, are located at areas of intersections between fault zones trending SE-NW (strike -slip faults) and SW-NE (normal faults), as are the onshore alkaline bodies of the Poços de Caldas Cabo Frio alignment. |
publishDate |
2006 |
dc.date.issued.fl_str_mv |
2006-12-15 |
dc.date.available.fl_str_mv |
2007-11-29 |
dc.date.accessioned.fl_str_mv |
2021-01-05T15:30:41Z |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/doctoralThesis |
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dc.identifier.citation.fl_str_mv |
OREIRO, Sérgio Goulart. Interpretação sísmica dos eventos magmáticos pós-aptianos no alto de Cabo Frio, sudeste do Brasil, gênese e relação com os lineamentos pré-sal. 2006. 180 f. Tese (Doutorado em Análise de Bacias;Tectônia, Petrologia e Recursos Minerais) - Universidade do Estado do Rio de Janeiro, Rio de Janeiro, 2006. |
dc.identifier.uri.fl_str_mv |
http://www.bdtd.uerj.br/handle/1/7000 |
identifier_str_mv |
OREIRO, Sérgio Goulart. Interpretação sísmica dos eventos magmáticos pós-aptianos no alto de Cabo Frio, sudeste do Brasil, gênese e relação com os lineamentos pré-sal. 2006. 180 f. Tese (Doutorado em Análise de Bacias;Tectônia, Petrologia e Recursos Minerais) - Universidade do Estado do Rio de Janeiro, Rio de Janeiro, 2006. |
url |
http://www.bdtd.uerj.br/handle/1/7000 |
dc.language.iso.fl_str_mv |
por |
language |
por |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
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openAccess |
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dc.publisher.none.fl_str_mv |
Universidade do Estado do Rio de Janeiro |
dc.publisher.program.fl_str_mv |
Programa de Pós-Graduação em Análise de Bacias e Faixas Móveis |
dc.publisher.initials.fl_str_mv |
UERJ |
dc.publisher.country.fl_str_mv |
BR |
dc.publisher.department.fl_str_mv |
Centro de Tecnologia e Ciências::Faculdade de Geologia |
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Universidade do Estado do Rio de Janeiro |
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repository.mail.fl_str_mv |
bdtd.suporte@uerj.br |
_version_ |
1792352273871929344 |