Geology of the correas massif, south of sÃo paulo state

Detalhes bibliográficos
Autor(a) principal: da Mata, Suelen Portughesi [UNESP]
Data de Publicação: 2020
Outros Autores: Vieira, Otávio Augusto Ruiz Paccola [UNESP], Godoy, Antonio Misson [UNESP]
Tipo de documento: Artigo
Idioma: por
Título da fonte: Repositório Institucional da UNESP
Texto Completo: http://dx.doi.org/10.5016/geociencias.v39i2.14625
http://hdl.handle.net/11449/207001
Resumo: The Massif Correas is located in São Paulo state south region, in the Itaboa district, Ribeirão Branco municipality and is related to neoproterozoic granitogenic evolution of the Central Mantiqueira Province, inserted in the Ribeira Belt south-central portion and in the Apiaí Terrain northern part. It highlights in the geological literature due to its correlation with the occurrence of mineralized greisens in cassiterite and wolframite and that constitute the Bairro dos Correas polymetallic deposit. The body covers an area of a granite stock of approximately 5 km², elongated ellipsoidal in the ENE-WSW direction and intrusive in Água Clara Formation metavolcanicsedimentary rocks, belonging to the Açungui Supergroup and in Granitic Complex Três Córregos rocks. Granite rocks are represented by varieties of gray to pink, isotropic and porphytic rocks and distinct in three facies called porphyritic monozogranite biotite, biotite-muscovite sienogranite porphyrytic, mica-albita porphyry granite with topaz and pegmatitic phase.
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spelling Geology of the correas massif, south of sÃo paulo stateGeologia do maciço correas, sul do estado de são pauloCorreas GraniteGeophysicsPetrographyThe Massif Correas is located in São Paulo state south region, in the Itaboa district, Ribeirão Branco municipality and is related to neoproterozoic granitogenic evolution of the Central Mantiqueira Province, inserted in the Ribeira Belt south-central portion and in the Apiaí Terrain northern part. It highlights in the geological literature due to its correlation with the occurrence of mineralized greisens in cassiterite and wolframite and that constitute the Bairro dos Correas polymetallic deposit. The body covers an area of a granite stock of approximately 5 km², elongated ellipsoidal in the ENE-WSW direction and intrusive in Água Clara Formation metavolcanicsedimentary rocks, belonging to the Açungui Supergroup and in Granitic Complex Três Córregos rocks. Granite rocks are represented by varieties of gray to pink, isotropic and porphytic rocks and distinct in three facies called porphyritic monozogranite biotite, biotite-muscovite sienogranite porphyrytic, mica-albita porphyry granite with topaz and pegmatitic phase.Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)Graduação em Geologia IGCE UNESP Universidade Estadual PaulistaGeociências e Meio Ambiente IGCE UNESP Universidade Estadual PaulistaDepartamento de Petrologia e Metalogenia IGCE UNESP Universidade Estadual Paulista, Av. 24-A, 1515-Bela VistaGraduação em Geologia IGCE UNESP Universidade Estadual PaulistaGeociências e Meio Ambiente IGCE UNESP Universidade Estadual PaulistaDepartamento de Petrologia e Metalogenia IGCE UNESP Universidade Estadual Paulista, Av. 24-A, 1515-Bela VistaCNPq: 304614/2017-3Universidade Estadual Paulista (Unesp)da Mata, Suelen Portughesi [UNESP]Vieira, Otávio Augusto Ruiz Paccola [UNESP]Godoy, Antonio Misson [UNESP]2021-06-25T10:47:24Z2021-06-25T10:47:24Z2020-01-01info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/article297-316http://dx.doi.org/10.5016/geociencias.v39i2.14625Geociencias, v. 39, n. 2, p. 297-316, 2020.1980-900X0101-9082http://hdl.handle.net/11449/20700110.5016/geociencias.v39i2.146252-s2.0-85097883610Scopusreponame:Repositório Institucional da UNESPinstname:Universidade Estadual Paulista (UNESP)instacron:UNESPporGeocienciasinfo:eu-repo/semantics/openAccess2021-10-23T16:00:37Zoai:repositorio.unesp.br:11449/207001Repositório InstitucionalPUBhttp://repositorio.unesp.br/oai/requestopendoar:29462021-10-23T16:00:37Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)false
dc.title.none.fl_str_mv Geology of the correas massif, south of sÃo paulo state
Geologia do maciço correas, sul do estado de são paulo
title Geology of the correas massif, south of sÃo paulo state
spellingShingle Geology of the correas massif, south of sÃo paulo state
da Mata, Suelen Portughesi [UNESP]
Correas Granite
Geophysics
Petrography
title_short Geology of the correas massif, south of sÃo paulo state
title_full Geology of the correas massif, south of sÃo paulo state
title_fullStr Geology of the correas massif, south of sÃo paulo state
title_full_unstemmed Geology of the correas massif, south of sÃo paulo state
title_sort Geology of the correas massif, south of sÃo paulo state
author da Mata, Suelen Portughesi [UNESP]
author_facet da Mata, Suelen Portughesi [UNESP]
Vieira, Otávio Augusto Ruiz Paccola [UNESP]
Godoy, Antonio Misson [UNESP]
author_role author
author2 Vieira, Otávio Augusto Ruiz Paccola [UNESP]
Godoy, Antonio Misson [UNESP]
author2_role author
author
dc.contributor.none.fl_str_mv Universidade Estadual Paulista (Unesp)
dc.contributor.author.fl_str_mv da Mata, Suelen Portughesi [UNESP]
Vieira, Otávio Augusto Ruiz Paccola [UNESP]
Godoy, Antonio Misson [UNESP]
dc.subject.por.fl_str_mv Correas Granite
Geophysics
Petrography
topic Correas Granite
Geophysics
Petrography
description The Massif Correas is located in São Paulo state south region, in the Itaboa district, Ribeirão Branco municipality and is related to neoproterozoic granitogenic evolution of the Central Mantiqueira Province, inserted in the Ribeira Belt south-central portion and in the Apiaí Terrain northern part. It highlights in the geological literature due to its correlation with the occurrence of mineralized greisens in cassiterite and wolframite and that constitute the Bairro dos Correas polymetallic deposit. The body covers an area of a granite stock of approximately 5 km², elongated ellipsoidal in the ENE-WSW direction and intrusive in Água Clara Formation metavolcanicsedimentary rocks, belonging to the Açungui Supergroup and in Granitic Complex Três Córregos rocks. Granite rocks are represented by varieties of gray to pink, isotropic and porphytic rocks and distinct in three facies called porphyritic monozogranite biotite, biotite-muscovite sienogranite porphyrytic, mica-albita porphyry granite with topaz and pegmatitic phase.
publishDate 2020
dc.date.none.fl_str_mv 2020-01-01
2021-06-25T10:47:24Z
2021-06-25T10:47:24Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv http://dx.doi.org/10.5016/geociencias.v39i2.14625
Geociencias, v. 39, n. 2, p. 297-316, 2020.
1980-900X
0101-9082
http://hdl.handle.net/11449/207001
10.5016/geociencias.v39i2.14625
2-s2.0-85097883610
url http://dx.doi.org/10.5016/geociencias.v39i2.14625
http://hdl.handle.net/11449/207001
identifier_str_mv Geociencias, v. 39, n. 2, p. 297-316, 2020.
1980-900X
0101-9082
10.5016/geociencias.v39i2.14625
2-s2.0-85097883610
dc.language.iso.fl_str_mv por
language por
dc.relation.none.fl_str_mv Geociencias
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv 297-316
dc.source.none.fl_str_mv Scopus
reponame:Repositório Institucional da UNESP
instname:Universidade Estadual Paulista (UNESP)
instacron:UNESP
instname_str Universidade Estadual Paulista (UNESP)
instacron_str UNESP
institution UNESP
reponame_str Repositório Institucional da UNESP
collection Repositório Institucional da UNESP
repository.name.fl_str_mv Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)
repository.mail.fl_str_mv
_version_ 1803046052660510720

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