The structural geology of the of quarries of dimension stones in the mining district of Santo Antônio de Pádua, SE Brazil

Detalhes bibliográficos
Autor(a) principal: Dayan, Henrique
Data de Publicação: 2008
Outros Autores: Valença, Joel Gomes
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/6780
Resumo: The mining district of Santo Antonio de Pádua is responsible for the greatest concentration of mining activity (except for oil offshore exploration) in the state of Rio de Janeiro. Two different lithotypes of dimension stones are quarried along two particular fault zones that are part of major splay of faults which branch off Rio Paraíba do Sul Shear Zone. The quarried dimension stones are two homogeneous orthogneisses that were emplaced in a transcurrent transpressive regime. We present here a possible explanation for the genesis of those rocks.
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spelling The structural geology of the of quarries of dimension stones in the mining district of Santo Antônio de Pádua, SE BrazilGeologia estrutural das pedreiras de rochas ornamentais no distrito Mineiro de Santo Antônio de Pádua, SE do BrasilThe mining district of Santo Antonio de Pádua is responsible for the greatest concentration of mining activity (except for oil offshore exploration) in the state of Rio de Janeiro. Two different lithotypes of dimension stones are quarried along two particular fault zones that are part of major splay of faults which branch off Rio Paraíba do Sul Shear Zone. The quarried dimension stones are two homogeneous orthogneisses that were emplaced in a transcurrent transpressive regime. We present here a possible explanation for the genesis of those rocks.O distrito mineiro de Santo Antonio de Pádua apresenta a maior concentração de atividade mineira (excetuando a atividade petrolífera da Bacia de Campos) no Estado do Rio de Janeiro. Dois litotipos principais são lavrados, com finalidade de rocha ornamental, ao longo de duas zonas de falhas, às quais fazem parte de um feixe maior de falhas pertinentes à Zona de Cisalhamento do Rio Paraíba do Sul. Os dois litotipos são dois ortognaisses homogêneos, que tiveram suas colocações num regime transcorrente-transpressivo. Nós apresentamos aqui uma possível explicação para a gênese destas rochas.Universidade Federal do Rio de Janeiro2008-01-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://revistas.ufrj.br/index.php/aigeo/article/view/678010.11137/2008_1_83-87Anuário do Instituto de Geociências; Vol 31, No 1 (2008); 83-87Anuário do Instituto de Geociências; Vol 31, No 1 (2008); 83-871982-39080101-9759reponame:Anuário do Instituto de Geociências (Online)instname:Universidade Federal do Rio de Janeiro (UFRJ)instacron:UFRJenghttps://revistas.ufrj.br/index.php/aigeo/article/view/6780/5377Copyright (c) 2008 Anuário do Instituto de Geociênciashttp://creativecommons.org/licenses/by/4.0info:eu-repo/semantics/openAccessDayan, HenriqueValença, Joel Gomes2017-01-23T21:48:47Zoai:www.revistas.ufrj.br:article/6780Revistahttps://revistas.ufrj.br/index.php/aigeo/indexPUBhttps://revistas.ufrj.br/index.php/aigeo/oaianuario@igeo.ufrj.br||1982-39080101-9759opendoar:2017-01-23T21:48:47Anuário do Instituto de Geociências (Online) - Universidade Federal do Rio de Janeiro (UFRJ)false
dc.title.none.fl_str_mv The structural geology of the of quarries of dimension stones in the mining district of Santo Antônio de Pádua, SE Brazil
Geologia estrutural das pedreiras de rochas ornamentais no distrito Mineiro de Santo Antônio de Pádua, SE do Brasil
title The structural geology of the of quarries of dimension stones in the mining district of Santo Antônio de Pádua, SE Brazil
spellingShingle The structural geology of the of quarries of dimension stones in the mining district of Santo Antônio de Pádua, SE Brazil
Dayan, Henrique
title_short The structural geology of the of quarries of dimension stones in the mining district of Santo Antônio de Pádua, SE Brazil
title_full The structural geology of the of quarries of dimension stones in the mining district of Santo Antônio de Pádua, SE Brazil
title_fullStr The structural geology of the of quarries of dimension stones in the mining district of Santo Antônio de Pádua, SE Brazil
title_full_unstemmed The structural geology of the of quarries of dimension stones in the mining district of Santo Antônio de Pádua, SE Brazil
title_sort The structural geology of the of quarries of dimension stones in the mining district of Santo Antônio de Pádua, SE Brazil
author Dayan, Henrique
author_facet Dayan, Henrique
Valença, Joel Gomes
author_role author
author2 Valença, Joel Gomes
author2_role author
dc.contributor.author.fl_str_mv Dayan, Henrique
Valença, Joel Gomes
description The mining district of Santo Antonio de Pádua is responsible for the greatest concentration of mining activity (except for oil offshore exploration) in the state of Rio de Janeiro. Two different lithotypes of dimension stones are quarried along two particular fault zones that are part of major splay of faults which branch off Rio Paraíba do Sul Shear Zone. The quarried dimension stones are two homogeneous orthogneisses that were emplaced in a transcurrent transpressive regime. We present here a possible explanation for the genesis of those rocks.
publishDate 2008
dc.date.none.fl_str_mv 2008-01-01
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/6780
10.11137/2008_1_83-87
url https://revistas.ufrj.br/index.php/aigeo/article/view/6780
identifier_str_mv 10.11137/2008_1_83-87
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv https://revistas.ufrj.br/index.php/aigeo/article/view/6780/5377
dc.rights.driver.fl_str_mv Copyright (c) 2008 Anuário do Instituto de Geociências
http://creativecommons.org/licenses/by/4.0
info:eu-repo/semantics/openAccess
rights_invalid_str_mv Copyright (c) 2008 Anuário do Instituto de Geociências
http://creativecommons.org/licenses/by/4.0
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
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 31, No 1 (2008); 83-87
Anuário do Instituto de Geociências; Vol 31, No 1 (2008); 83-87
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)
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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)
repository.mail.fl_str_mv anuario@igeo.ufrj.br||
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