The structural geology of the of quarries of dimension stones in the mining district of Santo Antônio de Pádua, SE Brazil
Autor(a) principal: | |
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Data de Publicação: | 2008 |
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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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Anuário do Instituto de Geociências (Online) |
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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) |
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) |
repository.mail.fl_str_mv |
anuario@igeo.ufrj.br|| |
_version_ |
1797053539778822144 |