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1. Identificação
Tipo de ReferênciaArtigo em Evento (Conference Proceedings)
Sitemtc-m21b.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W34P/3KQ6FT8
Repositóriosid.inpe.br/mtc-m21b/2015/12.17.15.55
Repositório de Metadadossid.inpe.br/mtc-m21b/2015/12.17.15.55.15
Última Atualização dos Metadados2018:06.04.02.55.58 (UTC) administrator
Chave SecundáriaINPE--PRE/
Chave de CitaçãoPadilhaVitoPádu:2015:ThMaIm
TítuloThree-dimensional magnetotelluric imaging of crustal structure beneath the Central Domain of the Borborema Province, NE Brazil
Ano2015
Data de Acesso17 maio 2024
Tipo SecundárioPRE CI
2. Contextualização
Autor1 Padilha, Antonio Lopes
2 Vitorello, Ícaro
3 Pádua, Marcelo Banik
Identificador de Curriculo1 8JMKD3MGP5W/3C9JGJG
2 8JMKD3MGP5W/3C9JHD6
Grupo1 DGE-CEA-INPE-MCTI-GOV-BR
2
3 DGE-CEA-INPE-MCTI-GOV-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 University of Arizona
3 Instituto Nacional de Pesquisas Espaciais (INPE)
Endereço de e-Mail do Autor1 antonio.padilha@inpe.br
2
3 marcelo.banik@inpe.br
Nome do EventoIUGG General Assembly, 26
Localização do EventoPrague, Czech Republic
Data22 June - 02 July
Histórico (UTC)2015-12-17 15:55:15 :: simone -> administrator ::
2018-06-04 02:55:58 :: administrator -> simone :: 2015
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
ResumoThe Borborema province, in northeast Brazil, consists of a complex set of crustal blocks of different ages, origin and evolution, with final amalgamation during the late Neoproterozoic Brasiliano orogeny. Its Central Domain is characterized by elongate NE-SW terranes largely affected by the Brasiliano metamorphic overprinting and by a suite of early Neoproterozoic metavolcanic rocks reflecting a distinct tectonic event (Cariris Velhos). Magnetotelluric (MT) data were collected at 64 stations along four profiles across this central region of the province to assess its deep electrical resistivity structure. Dimensionality analysis shows that the subsurface is electrically dominated by 3D structure, and 3D inversions of the full impedance tensor and vertical magnetic transfer function (tipper) were carried out. The dominant features in the final model are north-dipping crustal conductors, which can be correlated between the different MT profiles and cross contrasting terranes at the surface of the province. Considering the geometry and distribution of the conductors, they are interpreted as reflecting remnants of a pre-Neoproterozoic north-directed subduction zone with enhanced conductivity associated with graphitized biogenic material in metasedimentary rocks originally deposited in a restricted oceanic environment and subsequently metamorphosed and introduced into the deep crust by the subduction of the oceanic lithosphere. As the extent of crustal remobilization by the Brasiliano event seems to be restricted to the brittle upper crust, it is proposed that the Neoproterozoic geodynamic evolution in this domain of the Borborema Province occurred in an intracontinental setting.
ÁreaCEA
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4. Condições de acesso e uso
Grupo de Usuáriossimone
Visibilidadeshown
Permissão de Leituraallow from all
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Repositório Espelhosid.inpe.br/mtc-m21b/2013/09.26.14.25.22
Unidades Imediatamente Superiores8JMKD3MGPCW/3EU29DP
Acervo Hospedeirosid.inpe.br/mtc-m21b/2013/09.26.14.25.20
6. Notas
Campos Vaziosarchivingpolicy archivist booktitle callnumber copyholder copyright creatorhistory descriptionlevel dissemination doi e-mailaddress edition editor format isbn issn keywords label language lineage mark nextedition notes numberoffiles numberofvolumes orcid organization pages parameterlist parentrepositories previousedition previouslowerunit progress project publisher publisheraddress readergroup rightsholder schedulinginformation secondarydate secondarymark serieseditor session shorttitle size sponsor subject targetfile tertiarymark tertiarytype type url versiontype volume
7. Controle da descrição
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