Filling Materials in Brittle Structures as Indicator of Cenozoic Tectonic Events in Southeastern Brazil

Detalhes bibliográficos
Autor(a) principal: Calegari, Salomão Silva
Data de Publicação: 2020
Outros Autores: Aiolfi, Thaís Ruy, Neves, Mirna Aparecida, Soares, Caroline Cibele Vieira, Marques, Rodson de Abreu, Caxito, Fabrício de Andrade
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Anuário do Instituto de Geociências (Online)
Texto Completo: https://revistas.ufrj.br/index.php/aigeo/article/view/37227
Resumo: The filling materials in brittle structures can provide useful information about the Cenozoic evolution developed over proterozoic terrains. When these materials are affected by faults, they record deformation phases that can be determined chronologically and, in the occurrence of lateritic materials, it is possible to infer the paleoenvironmental conditions during the mineral formation. This work aimed to identify crystalline phases of brittle structure filling materials and to propose evolutionary interpretations for Cenozoic tectonic reactivation based on literature data. The study area is located in the Southern part of the Espírito Santo State, near the Brazilian Southeastern Continental Margin, where proterozoic geological structures have been reactivated since the mesozoic rift phase, up to the Holocene. The mineral assemblage found in the filling materials includes primary minerals such as quartz, muscovite, microcline, rutile, titanite, and bannisterite; and the weathering minerals such as kaolinite, illite, hematite, goethite, hydrobiotite, lithiophorite and, birnessite. The mineralogical association found in the filling materials denotes the action of fluid phases with mineral precipitation at the brittle discontinuities during the weathering processes that occurred during the Cenozoic, probably between the Miocene and the Pleistocene. The faults, which striations are marked on the filling materials, originated after (in the case of the manganese oxides) or during (in the case of the illite) the mineral formation, indicating that the maximum age of these faults is in the Miocene. The origin of the brittle structures that affected the filling materials studied here is linked to the uplifting of the Continental Brazilian Margin, when ancient geological structures were reactivated as normal faults due to the local action of an extensional regime.
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spelling Filling Materials in Brittle Structures as Indicator of Cenozoic Tectonic Events in Southeastern BrazilFilling Materials in Brittle Structures as Indicator of Cenozoic Tectonic Events in Southeastern BrazilBrittle Structures; Relative Dating; Cenozoic.Brittle Structures; Relative Dating; Cenozoic.The filling materials in brittle structures can provide useful information about the Cenozoic evolution developed over proterozoic terrains. When these materials are affected by faults, they record deformation phases that can be determined chronologically and, in the occurrence of lateritic materials, it is possible to infer the paleoenvironmental conditions during the mineral formation. This work aimed to identify crystalline phases of brittle structure filling materials and to propose evolutionary interpretations for Cenozoic tectonic reactivation based on literature data. The study area is located in the Southern part of the Espírito Santo State, near the Brazilian Southeastern Continental Margin, where proterozoic geological structures have been reactivated since the mesozoic rift phase, up to the Holocene. The mineral assemblage found in the filling materials includes primary minerals such as quartz, muscovite, microcline, rutile, titanite, and bannisterite; and the weathering minerals such as kaolinite, illite, hematite, goethite, hydrobiotite, lithiophorite and, birnessite. The mineralogical association found in the filling materials denotes the action of fluid phases with mineral precipitation at the brittle discontinuities during the weathering processes that occurred during the Cenozoic, probably between the Miocene and the Pleistocene. The faults, which striations are marked on the filling materials, originated after (in the case of the manganese oxides) or during (in the case of the illite) the mineral formation, indicating that the maximum age of these faults is in the Miocene. The origin of the brittle structures that affected the filling materials studied here is linked to the uplifting of the Continental Brazilian Margin, when ancient geological structures were reactivated as normal faults due to the local action of an extensional regime.The filling materials in brittle structures can provide useful information about the Cenozoic evolution developed over proterozoic terrains. When these materials are affected by faults, they record deformation phases that can be determined chronologically and, in the occurrence of lateritic materials, it is possible to infer the paleoenvironmental conditions during the mineral formation. This work aimed to identify crystalline phases of brittle structure filling materials and to propose evolutionary interpretations for Cenozoic tectonic reactivation based on literature data. The study area is located in the Southern part of the Espírito Santo State, near the Brazilian Southeastern Continental Margin, where proterozoic geological structures have been reactivated since the mesozoic rift phase, up to the Holocene. The mineral assemblage found in the filling materials includes primary minerals such as quartz, muscovite, microcline, rutile, titanite, and bannisterite; and the weathering minerals such as kaolinite, illite, hematite, goethite, hydrobiotite, lithiophorite and, birnessite. The mineralogical association found in the filling materials denotes the action of fluid phases with mineral precipitation at the brittle discontinuities during the weathering processes that occurred during the Cenozoic, probably between the Miocene and the Pleistocene. The faults, which striations are marked on the filling materials, originated after (in the case of the manganese oxides) or during (in the case of the illite) the mineral formation, indicating that the maximum age of these faults is in the Miocene. The origin of the brittle structures that affected the filling materials studied here is linked to the uplifting of the Continental Brazilian Margin, when ancient geological structures were reactivated asnormal faults due to the local action of an extensional regime.Universidade Federal do Rio de JaneiroCalegari, Salomão SilvaAiolfi, Thaís RuyNeves, Mirna AparecidaSoares, Caroline Cibele VieiraMarques, Rodson de AbreuCaxito, Fabrício de Andrade2020-08-21info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://revistas.ufrj.br/index.php/aigeo/article/view/3722710.11137/2020_2_237_254Anuário do Instituto de Geociências; Vol 43, No 2 (2020); 237_254Anuário do Instituto de Geociências; Vol 43, No 2 (2020); 237_2541982-39080101-9759reponame:Anuário do Instituto de Geociências (Online)instname:Universidade Federal do Rio de Janeiro (UFRJ)instacron:UFRJenghttps://revistas.ufrj.br/index.php/aigeo/article/view/37227/pdf/*ref*/Allaby, M. (ed.). 2008. 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Fault-related dilation, permeability enhancement, fluid flow and mineral precipitation patterns: numerical models. In: WIBBERLEY, C.A.J.; KURZ, W.; IMBER, J.; HOLDSWORTH, R.E. & COLLETTINI, C. (eds.). The Internal Structure of Fault Zones: implications for mechanical and fluid-flow properties. The Geological Society, London, 299, p. 239-255.Copyright (c) 2020 Anuário do Instituto de Geociênciashttp://creativecommons.org/licenses/by/4.0info:eu-repo/semantics/openAccess2020-09-21T10:59:44Zoai:www.revistas.ufrj.br:article/37227Revistahttps://revistas.ufrj.br/index.php/aigeo/indexPUBhttps://revistas.ufrj.br/index.php/aigeo/oaianuario@igeo.ufrj.br||1982-39080101-9759opendoar:2020-09-21T10:59:44Anuário do Instituto de Geociências (Online) - Universidade Federal do Rio de Janeiro (UFRJ)false
dc.title.none.fl_str_mv Filling Materials in Brittle Structures as Indicator of Cenozoic Tectonic Events in Southeastern Brazil
Filling Materials in Brittle Structures as Indicator of Cenozoic Tectonic Events in Southeastern Brazil
title Filling Materials in Brittle Structures as Indicator of Cenozoic Tectonic Events in Southeastern Brazil
spellingShingle Filling Materials in Brittle Structures as Indicator of Cenozoic Tectonic Events in Southeastern Brazil
Calegari, Salomão Silva
Brittle Structures; Relative Dating; Cenozoic.
Brittle Structures; Relative Dating; Cenozoic.
title_short Filling Materials in Brittle Structures as Indicator of Cenozoic Tectonic Events in Southeastern Brazil
title_full Filling Materials in Brittle Structures as Indicator of Cenozoic Tectonic Events in Southeastern Brazil
title_fullStr Filling Materials in Brittle Structures as Indicator of Cenozoic Tectonic Events in Southeastern Brazil
title_full_unstemmed Filling Materials in Brittle Structures as Indicator of Cenozoic Tectonic Events in Southeastern Brazil
title_sort Filling Materials in Brittle Structures as Indicator of Cenozoic Tectonic Events in Southeastern Brazil
author Calegari, Salomão Silva
author_facet Calegari, Salomão Silva
Aiolfi, Thaís Ruy
Neves, Mirna Aparecida
Soares, Caroline Cibele Vieira
Marques, Rodson de Abreu
Caxito, Fabrício de Andrade
author_role author
author2 Aiolfi, Thaís Ruy
Neves, Mirna Aparecida
Soares, Caroline Cibele Vieira
Marques, Rodson de Abreu
Caxito, Fabrício de Andrade
author2_role author
author
author
author
author
dc.contributor.none.fl_str_mv

dc.contributor.author.fl_str_mv Calegari, Salomão Silva
Aiolfi, Thaís Ruy
Neves, Mirna Aparecida
Soares, Caroline Cibele Vieira
Marques, Rodson de Abreu
Caxito, Fabrício de Andrade
dc.subject.por.fl_str_mv Brittle Structures; Relative Dating; Cenozoic.
Brittle Structures; Relative Dating; Cenozoic.
topic Brittle Structures; Relative Dating; Cenozoic.
Brittle Structures; Relative Dating; Cenozoic.
description The filling materials in brittle structures can provide useful information about the Cenozoic evolution developed over proterozoic terrains. When these materials are affected by faults, they record deformation phases that can be determined chronologically and, in the occurrence of lateritic materials, it is possible to infer the paleoenvironmental conditions during the mineral formation. This work aimed to identify crystalline phases of brittle structure filling materials and to propose evolutionary interpretations for Cenozoic tectonic reactivation based on literature data. The study area is located in the Southern part of the Espírito Santo State, near the Brazilian Southeastern Continental Margin, where proterozoic geological structures have been reactivated since the mesozoic rift phase, up to the Holocene. The mineral assemblage found in the filling materials includes primary minerals such as quartz, muscovite, microcline, rutile, titanite, and bannisterite; and the weathering minerals such as kaolinite, illite, hematite, goethite, hydrobiotite, lithiophorite and, birnessite. The mineralogical association found in the filling materials denotes the action of fluid phases with mineral precipitation at the brittle discontinuities during the weathering processes that occurred during the Cenozoic, probably between the Miocene and the Pleistocene. The faults, which striations are marked on the filling materials, originated after (in the case of the manganese oxides) or during (in the case of the illite) the mineral formation, indicating that the maximum age of these faults is in the Miocene. The origin of the brittle structures that affected the filling materials studied here is linked to the uplifting of the Continental Brazilian Margin, when ancient geological structures were reactivated as normal faults due to the local action of an extensional regime.
publishDate 2020
dc.date.none.fl_str_mv 2020-08-21
dc.type.none.fl_str_mv

dc.type.driver.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv https://revistas.ufrj.br/index.php/aigeo/article/view/37227
10.11137/2020_2_237_254
url https://revistas.ufrj.br/index.php/aigeo/article/view/37227
identifier_str_mv 10.11137/2020_2_237_254
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv https://revistas.ufrj.br/index.php/aigeo/article/view/37227/pdf
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dc.publisher.none.fl_str_mv Universidade Federal do Rio de Janeiro
publisher.none.fl_str_mv Universidade Federal do Rio de Janeiro
dc.source.none.fl_str_mv Anuário do Instituto de Geociências; Vol 43, No 2 (2020); 237_254
Anuário do Instituto de Geociências; Vol 43, No 2 (2020); 237_254
1982-3908
0101-9759
reponame:Anuário do Instituto de Geociências (Online)
instname:Universidade Federal do Rio de Janeiro (UFRJ)
instacron:UFRJ
instname_str Universidade Federal do Rio de Janeiro (UFRJ)
instacron_str UFRJ
institution UFRJ
reponame_str Anuário do Instituto de Geociências (Online)
collection Anuário do Instituto de Geociências (Online)
repository.name.fl_str_mv Anuário do Instituto de Geociências (Online) - Universidade Federal do Rio de Janeiro (UFRJ)
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