Paleoproterozoic late-orogenic and anorogenic alkaline granitic magmatism from northeast Brazil

Detalhes bibliográficos
Autor(a) principal: Plá Cid, J.
Data de Publicação: 2000
Outros Autores: Bitencourt, M. F., Nardi, L. V. S., Conceição, Herbet, Bonin, Bernard, Lafon, J. M.
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Institucional da UFBA
Texto Completo: http://www.repositorio.ufba.br/ri/handle/ri/5247
Resumo: p.47–75
id UFBA-2_a8b14fcfeedde44db75c0ef822bdbd46
oai_identifier_str oai:repositorio.ufba.br:ri/5247
network_acronym_str UFBA-2
network_name_str Repositório Institucional da UFBA
repository_id_str 1932
spelling Plá Cid, J.Bitencourt, M. F.Nardi, L. V. S.Conceição, HerbetBonin, BernardLafon, J. M.Plá Cid, J.Bitencourt, M. F.Nardi, L. V. S.Conceição, HerbetBonin, BernardLafon, J. M.2012-01-25T12:38:56Z2012-01-25T12:38:56Z20000301-9268http://www.repositorio.ufba.br/ri/handle/ri/5247v. 104.p.47–75During the Transamazonian cycle (2.090.2 Ga), two silica-saturated alkaline granite suites were intruded along the border of the Sa˜o Francisco craton, northeastern Brazil. The Couro de Onça intrusive suite (COIS) is late tectonic relative to major deformational events, and the Serra do Meio suite (SMS) postdates this event, being interpreted as anorogenic type, deformed during the Brasiliano cycle (0.65–0.52 Ga). The COIS encompasses alkali-feldspar granites, syenogranites, monzogranites, with dykes of similar composition and age (2.15795 Ma). They are metaluminous rocks of alkaline affinity, whose evolution was probably controlled by mineral fractionation processes involving mainly plagioclase, amphibole, and Fe–Ti oxide. The SMS, whose probable age is 2.01 Ga, is composed of metaluminous and peralkaline granites, with associated quartz syenites, with Ti-aegirine transformed during the Brasiliano deformation to riebeckite titanite aenigmatite. The temperatures of two stages of metamorphic transformation, overprinted during the Brasiliano event, are estimated at about 550 and 400–450°C. Both magmatic suites are derived from enriched mantle sources. The metaluminous and peralkaline trends observed in the SMS, characterized by high concentrations of HFS and RE elements controlled mainly by F-activity, reflect the evolution of different primary magmas produced by successive melting of the same mantle sources, in an anorogenic setting.Submitted by Ana Valéria de Jesus Moura (anavaleria_131@hotmail.com) on 2012-01-25T12:38:56Z No. of bitstreams: 1 S0301926800000814-main.pdf: 2921220 bytes, checksum: 0e8fcaccfe604dd99b8008aabeeed8f8 (MD5)Made available in DSpace on 2012-01-25T12:38:56Z (GMT). No. of bitstreams: 1 S0301926800000814-main.pdf: 2921220 bytes, checksum: 0e8fcaccfe604dd99b8008aabeeed8f8 (MD5) Previous issue date: 2000Alkaline granitesGeochemistryAnorogenicLate-orogenicPaleoproterozoic late-orogenic and anorogenic alkaline granitic magmatism from northeast BrazilPrecambrian Researchinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleengreponame:Repositório Institucional da UFBAinstname:Universidade Federal da Bahia (UFBA)instacron:UFBAinfo:eu-repo/semantics/openAccessORIGINALS0301926800000814-main.pdfS0301926800000814-main.pdfapplication/pdf2921220https://repositorio.ufba.br/bitstream/ri/5247/1/S0301926800000814-main.pdf0e8fcaccfe604dd99b8008aabeeed8f8MD51LICENSElicense.txtlicense.txttext/plain1762https://repositorio.ufba.br/bitstream/ri/5247/2/license.txt1b89a9a0548218172d7c829f87a0eab9MD52TEXTS0301926800000814-main.pdf.txtS0301926800000814-main.pdf.txtExtracted texttext/plain88653https://repositorio.ufba.br/bitstream/ri/5247/3/S0301926800000814-main.pdf.txteecadd2414fccf39eeeef66b83220e33MD53ri/52472022-07-05 14:03:37.218oai:repositorio.ufba.br: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Repositório InstitucionalPUBhttp://192.188.11.11:8080/oai/requestopendoar:19322022-07-05T17:03:37Repositório Institucional da UFBA - Universidade Federal da Bahia (UFBA)false
dc.title.pt_BR.fl_str_mv Paleoproterozoic late-orogenic and anorogenic alkaline granitic magmatism from northeast Brazil
dc.title.alternative.pt_BR.fl_str_mv Precambrian Research
title Paleoproterozoic late-orogenic and anorogenic alkaline granitic magmatism from northeast Brazil
spellingShingle Paleoproterozoic late-orogenic and anorogenic alkaline granitic magmatism from northeast Brazil
Plá Cid, J.
Alkaline granites
Geochemistry
Anorogenic
Late-orogenic
title_short Paleoproterozoic late-orogenic and anorogenic alkaline granitic magmatism from northeast Brazil
title_full Paleoproterozoic late-orogenic and anorogenic alkaline granitic magmatism from northeast Brazil
title_fullStr Paleoproterozoic late-orogenic and anorogenic alkaline granitic magmatism from northeast Brazil
title_full_unstemmed Paleoproterozoic late-orogenic and anorogenic alkaline granitic magmatism from northeast Brazil
title_sort Paleoproterozoic late-orogenic and anorogenic alkaline granitic magmatism from northeast Brazil
author Plá Cid, J.
author_facet Plá Cid, J.
Bitencourt, M. F.
Nardi, L. V. S.
Conceição, Herbet
Bonin, Bernard
Lafon, J. M.
author_role author
author2 Bitencourt, M. F.
Nardi, L. V. S.
Conceição, Herbet
Bonin, Bernard
Lafon, J. M.
author2_role author
author
author
author
author
dc.contributor.author.fl_str_mv Plá Cid, J.
Bitencourt, M. F.
Nardi, L. V. S.
Conceição, Herbet
Bonin, Bernard
Lafon, J. M.
Plá Cid, J.
Bitencourt, M. F.
Nardi, L. V. S.
Conceição, Herbet
Bonin, Bernard
Lafon, J. M.
dc.subject.por.fl_str_mv Alkaline granites
Geochemistry
Anorogenic
Late-orogenic
topic Alkaline granites
Geochemistry
Anorogenic
Late-orogenic
description p.47–75
publishDate 2000
dc.date.issued.fl_str_mv 2000
dc.date.accessioned.fl_str_mv 2012-01-25T12:38:56Z
dc.date.available.fl_str_mv 2012-01-25T12:38:56Z
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://www.repositorio.ufba.br/ri/handle/ri/5247
dc.identifier.issn.none.fl_str_mv 0301-9268
dc.identifier.number.pt_BR.fl_str_mv v. 104.
identifier_str_mv 0301-9268
v. 104.
url http://www.repositorio.ufba.br/ri/handle/ri/5247
dc.language.iso.fl_str_mv eng
language eng
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.source.none.fl_str_mv reponame:Repositório Institucional da UFBA
instname:Universidade Federal da Bahia (UFBA)
instacron:UFBA
instname_str Universidade Federal da Bahia (UFBA)
instacron_str UFBA
institution UFBA
reponame_str Repositório Institucional da UFBA
collection Repositório Institucional da UFBA
bitstream.url.fl_str_mv https://repositorio.ufba.br/bitstream/ri/5247/1/S0301926800000814-main.pdf
https://repositorio.ufba.br/bitstream/ri/5247/2/license.txt
https://repositorio.ufba.br/bitstream/ri/5247/3/S0301926800000814-main.pdf.txt
bitstream.checksum.fl_str_mv 0e8fcaccfe604dd99b8008aabeeed8f8
1b89a9a0548218172d7c829f87a0eab9
eecadd2414fccf39eeeef66b83220e33
bitstream.checksumAlgorithm.fl_str_mv MD5
MD5
MD5
repository.name.fl_str_mv Repositório Institucional da UFBA - Universidade Federal da Bahia (UFBA)
repository.mail.fl_str_mv
_version_ 1808459393313800192