Chemical deposits associated to metavolcanosedimentary sequences of the central portion of the São Francisco craton the state of Bahia, Brazil: a review

Detalhes bibliográficos
Autor(a) principal: Carvalho, Ilson Guimarães
Data de Publicação: 2000
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Institucional da UFBA
Texto Completo: http://www.repositorio.ufba.br/ri/handle/ri/2630
Resumo: p. 279-284
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spelling Carvalho, Ilson GuimarãesCarvalho, Ilson Guimarães2011-09-09T13:02:23Z2011-09-09T13:02:23Z2000-062177-4382http://www.repositorio.ufba.br/ri/handle/ri/2630v. 30, n. 2.p. 279-284Supracrustal suites of metavolcanosedimentary rocks (SC) occur in the central portion of the São Francisco Craton in the State of Bahia. They were primarily formed by calc- alkaline to perialkaline volcanic flows and tuffs, clastic and chemical sediments. The latter are referred to the banded iron (BIF), iron-manganese (BIMF) and manganese (BMP) formations, iron-poor magnesian-rich carbonate formation (IPMRCF), and minor metacherts. BIF and IPMRCF are present in all the reported SC. BIF is typified by the presence of the oxide, carbonate and silicate facies. Occurrences of the sulfide facies are reported for the Sobradinho-Salitre and the Boquira SC. The burial metamorphism and thermal effects pronounced by the Transamazonian migmatization and granitization are accountable for the generation of amphibolites, epidosites, steatite and talc schists, phyllites, sandstones, quartzites, itabirites, metamorphic limestones to include banded carbonates, marbles and calc-silicate rocks. It is suggested that the deposition was similarly processed throughout an extensive crustal segment and that it was part of the cratonic evolution occurred during the end of the Archean to the beginning of the Proterozoic.Submitted by Ana Valéria de Jesus Moura (anavaleria_131@hotmail.com) on 2011-09-09T13:02:23Z No. of bitstreams: 1 10639-35957-1-PB.pdf: 1184322 bytes, checksum: fcd1439f7b9e622d11027afabc60527b (MD5)Made available in DSpace on 2011-09-09T13:02:23Z (GMT). No. of bitstreams: 1 10639-35957-1-PB.pdf: 1184322 bytes, checksum: fcd1439f7b9e622d11027afabc60527b (MD5) Previous issue date: 2000-06São Francisco Craton. Paleoproterozoic. Metavolcanosedimentary sequences. BIF. Banded iron-manganese formations. MagnesiteChemical deposits associated to metavolcanosedimentary sequences of the central portion of the São Francisco craton the state of Bahia, Brazil: a reviewRevista Brasileira de Geociênciasinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleengreponame:Repositório Institucional da UFBAinstname:Universidade Federal da Bahia (UFBA)instacron:UFBAinfo:eu-repo/semantics/openAccessORIGINAL10639-35957-1-PB.pdf10639-35957-1-PB.pdfapplication/pdf1184322https://repositorio.ufba.br/bitstream/ri/2630/1/10639-35957-1-PB.pdffcd1439f7b9e622d11027afabc60527bMD51LICENSElicense.txtlicense.txttext/plain1918https://repositorio.ufba.br/bitstream/ri/2630/2/license.txt7e0f2f68e8dd9be31545fb0c2cd16dc0MD52TEXT10639-35957-1-PB.pdf.txt10639-35957-1-PB.pdf.txtExtracted texttext/plain27284https://repositorio.ufba.br/bitstream/ri/2630/3/10639-35957-1-PB.pdf.txtffa7fa9e702d30f19bbe6e13e26ccb90MD53ri/26302022-07-05 14:03:30.598oai:repositorio.ufba.br:ri/2630TGljZW5zZSBncmFudGVkIGJ5IEFuYSBWYWzDqXJpYSBkZSBKZXN1cyBNb3VyYSAoYW5hdmFsZXJpYV8xMzFAaG90bWFpbC5jb20pIG9uIDIwMTEtMDktMDlUMTM6MDI6MjNaIChHTVQpOgoKVGVybW8gZGUgTGljZW7Dp2EsIG7Do28gZXhjbHVzaXZvLCBwYXJhIG8gZGVww7NzaXRvIG5vIApyZXBvc2l0w7NyaW8gSW5zdGl0dWNpb25hbCBkYSBVRkJBCgogICAgUGVsbyBwcm9jZXNzbyBkZSBzdWJtaXNzw6NvIGRlIGRvY3VtZW50b3MsIG8gYXV0b3Igb3Ugc2V1CnJlcHJlc2VudGFudGUgbGVnYWwsIGFvIGFjZWl0YXIgZXNzZSB0ZXJtbyBkZSBsaWNlbsOnYSwgY29uY2VkZSBhbwpSZXBvc2l0w7NyaW8gSW5zdGl0dWNpb25hbCBkYSBVbml2ZXJzaWRhZGUgRmVkZXJhbCBkYSBCYWhpYSBvIGRpcmVpdG8KZGUgbWFudGVyIHVtYSBjw7NwaWEgZW0gc2V1IHJlcG9zaXTDs3JpbyBjb20gYSBmaW5hbGlkYWRlLCBwcmltZWlyYSwgCmRlIHByZXNlcnZhw6fDo28uIEVzc2UgdGVybW8sIG7Do28gZXhjbHVzaXZvLCBtYW50w6ptIG9zIGRpcmVpdG9zIGRlIAphdXRvci9jb3B5cmlnaHQsIG1hcyBlbnRlbmRlIG8gZG9jdW1lbnRvIGNvbW8gcGFydGUgZG8gYWNlcnZvIGludGVsZWN0dWFsCiBkZXNzYSBVbml2ZXJzaWRhZGUuIAoKICAgIFBhcmEgb3MgZG9jdW1lbnRvcyBwdWJsaWNhZG9zIGNvbSByZXBhc3NlIGRlIGRpcmVpdG9zIGRlIApkaXN0cmlidWnDp8OjbywgZXNzZSB0ZXJtbyBkZSBsaWNlbsOnYSBlbnRlbmRlIHF1ZTogCgogICAgTWFudGVuZG8gb3PCoCBkaXJlaXRvcyBhdXRvcmFpcywgcmVwYXNzYWRvcyBhIHRlcmNlaXJvcywgZW0gY2FzbyAKZGUgcHVibGljYcOnw7VlcywgbyByZXBvc2l0w7NyaW8gcG9kZSByZXN0cmluZ2lyIG8gYWNlc3NvIGFvIHRleHRvIAppbnRlZ3JhbCwgbWFzIGxpYmVyYSBhcyBpbmZvcm1hw6fDtWVzIHNvYnJlIG8gZG9jdW1lbnRvIChNZXRhZGFkb3MgZGVzY3JpdGl2b3MpLgogRGVzdGEgZm9ybWEsIGF0ZW5kZW5kbyBhb3MgYW5zZWlvcyBkZXNzYSB1bml2ZXJzaWRhZGUgCmVtIG1hbnRlciBzdWEgcHJvZHXDp8OjbyBjaWVudMOtwq1maWNhIGNvbSBhcyByZXN0cmnDp8O1ZXMgaW1wb3N0YXMgcGVsb3MgCmVkaXRvcmVzIGRlIHBlcmnDs2RpY29zLiAKCiAgICBQYXJhIGFzIHB1YmxpY2HDp8O1ZXMgZW0gaW5pY2lhdGl2YXMgcXVlIHNlZ3VlbSBhIHBvbMOtwq10aWNhIGRlIApBY2Vzc28gQWJlcnRvLCBvcyBkZXDDs3NpdG9zIGNvbXB1bHPDs3Jpb3MgbmVzc2UgcmVwb3NpdMOzcmlvIG1hbnTDqm0gCm9zIGRpcmVpdG9zIGF1dG9yYWlzLCBtYXMgbWFudMOqbSBvIGFjZXNzbyBpcnJlc3RyaXRvIGFvIG1ldGFkYWRvcyAKZSB0ZXh0byBjb21wbGV0by4gQXNzaW0sIGEgYWNlaXRhw6fDo28gZGVzc2UgdGVybW8gbsOjbyBuZWNlc3NpdGEgZGUgCmNvbnNlbnRpbWVudG8gcG9yIHBhcnRlIGRlIGF1dG9yZXMvZGV0ZW50b3JlcyBkb3MgZGlyZWl0b3MsIHBvciAKZXN0YXJlbSBlbSBpbmljaWF0aXZhcyBkZSBhY2Vzc28gYWJlcnRvLgoKICAgIEVtIGFtYm9zIG8gY2FzbywgZXNzZSB0ZXJtbyBkZSBsaWNlbsOnYSwgcG9kZSBzZXIgYWNlaXRvIHBlbG8gCmF1dG9yLCBkZXRlbnRvcmVzIGRlIGRpcmVpdG9zIGUvb3UgdGVyY2Vpcm9zIGFtcGFyYWRvcyBwZWxhIAp1bml2ZXJzaWRhZGUuIERldmlkbyBhb3MgZGlmZXJlbnRlcyBwcm9jZXNzb3MgcGVsbyBxdWFsIGEgc3VibWlzc8OjbyAKcG9kZSBvY29ycmVyLCBvIHJlcG9zaXTDs3JpbyBwZXJtaXRlIGEgYWNlaXRhw6fDo28gZGEgbGljZW7Dp2EgcG9yIAp0ZXJjZWlyb3MsIHNvbWVudGUgbm9zIGNhc29zIGRlIGRvY3VtZW50b3MgcHJvZHV6aWRvcyBwb3IgaW50ZWdyYW50ZXMgCmRhIFVGQkEgZSBzdWJtZXRpZG9zIHBvciBwZXNzb2FzIGFtcGFyYWRhcyBwb3IgZXN0YSBpbnN0aXR1acOnw6NvCg==Repositório InstitucionalPUBhttp://192.188.11.11:8080/oai/requestopendoar:19322022-07-05T17:03:30Repositório Institucional da UFBA - Universidade Federal da Bahia (UFBA)false
dc.title.pt_BR.fl_str_mv Chemical deposits associated to metavolcanosedimentary sequences of the central portion of the São Francisco craton the state of Bahia, Brazil: a review
dc.title.alternative.pt_BR.fl_str_mv Revista Brasileira de Geociências
title Chemical deposits associated to metavolcanosedimentary sequences of the central portion of the São Francisco craton the state of Bahia, Brazil: a review
spellingShingle Chemical deposits associated to metavolcanosedimentary sequences of the central portion of the São Francisco craton the state of Bahia, Brazil: a review
Carvalho, Ilson Guimarães
São Francisco Craton. Paleoproterozoic. Metavolcanosedimentary sequences. BIF. Banded iron-manganese formations. Magnesite
title_short Chemical deposits associated to metavolcanosedimentary sequences of the central portion of the São Francisco craton the state of Bahia, Brazil: a review
title_full Chemical deposits associated to metavolcanosedimentary sequences of the central portion of the São Francisco craton the state of Bahia, Brazil: a review
title_fullStr Chemical deposits associated to metavolcanosedimentary sequences of the central portion of the São Francisco craton the state of Bahia, Brazil: a review
title_full_unstemmed Chemical deposits associated to metavolcanosedimentary sequences of the central portion of the São Francisco craton the state of Bahia, Brazil: a review
title_sort Chemical deposits associated to metavolcanosedimentary sequences of the central portion of the São Francisco craton the state of Bahia, Brazil: a review
author Carvalho, Ilson Guimarães
author_facet Carvalho, Ilson Guimarães
author_role author
dc.contributor.author.fl_str_mv Carvalho, Ilson Guimarães
Carvalho, Ilson Guimarães
dc.subject.por.fl_str_mv São Francisco Craton. Paleoproterozoic. Metavolcanosedimentary sequences. BIF. Banded iron-manganese formations. Magnesite
topic São Francisco Craton. Paleoproterozoic. Metavolcanosedimentary sequences. BIF. Banded iron-manganese formations. Magnesite
description p. 279-284
publishDate 2000
dc.date.issued.fl_str_mv 2000-06
dc.date.accessioned.fl_str_mv 2011-09-09T13:02:23Z
dc.date.available.fl_str_mv 2011-09-09T13:02:23Z
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dc.identifier.uri.fl_str_mv http://www.repositorio.ufba.br/ri/handle/ri/2630
dc.identifier.issn.none.fl_str_mv 2177-4382
dc.identifier.number.pt_BR.fl_str_mv v. 30, n. 2.
identifier_str_mv 2177-4382
v. 30, n. 2.
url http://www.repositorio.ufba.br/ri/handle/ri/2630
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