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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m21b.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP5W34M/3FA44LG
Repositóriosid.inpe.br/mtc-m21b/2013/11.26.16.45.32   (acesso restrito)
Última Atualização2014:02.11.12.44.01 (UTC) administrator
Repositório de Metadadossid.inpe.br/mtc-m21b/2013/11.26.16.45.33
Última Atualização dos Metadados2018:06.04.03.04.02 (UTC) administrator
DOI10.1016/j.tecto.2013.10.008
ISSN0040-1951
Rótuloscopus 2013-11
Chave de CitaçãoSantosPaFuPiViPá:2014:MaImSo
TítuloDeep structure of a stretched lithosphere: Magnetotelluric imaging of the southeastern Borborema province, NE Brazil
ProjetoINCT-ET (CNPq grant 573713/ 2008-1). CNPq (grants 150534/2012-4, 302347/2008-9 and 303813/2009-1) and FAPESP (grant 2012/21376-6)
Ano2014
MêsJan.
Data de Acesso10 maio 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho2388 KiB
2. Contextualização
Autor1 Santos, Andrea C. L.
2 Padilha, Antonio Lopes
3 Fuck, Reinhardt A.
4 Pires, Augusto C. B.
5 Vitorello, Ícaro
6 Pádua, Marcelo Banik de
Identificador de Curriculo1
2 8JMKD3MGP5W/3C9JGJG
3
4
5 8JMKD3MGP5W/3C9JHD6
6 8JMKD3MGP5W/3C9JHNR
Grupo1
2 DGE-CEA-INPE-MCTI-GOV-BR
3
4
5 DGE-CEA-INPE-MCTI-GOV-BR
6 DGE-CEA-INPE-MCTI-GOV-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais, INPE, C.P. 515, 12201-970 São José dos Campos, SP, Brazil; Instituto de Geociências, Universidade de Brasília, Campus Universitário Darcy Ribeiro, 70910-900 Brasília, DF, Brazil
2 Instituto Nacional de Pesquisas Espaciais (INPE)
3 Instituto de Geociências, Universidade de Brasília, Campus Universitário Darcy Ribeiro, 70910-900 Brasília, DF, Brazil
4 Instituto de Geociências, Universidade de Brasília, Campus Universitário Darcy Ribeiro, 70910-900 Brasília, DF, Brazil
5 Instituto Nacional de Pesquisas Espaciais (INPE)
6 Instituto Nacional de Pesquisas Espaciais (INPE)
Endereço de e-Mail do Autor1 andrealima@dge.inpe.br
2 antonio.padilha@inpe.br
3 reinhardt@unb.br
4 acbpires@unb.br
5 icaro@dge.inpe.br
6 banik@dge.inpe.br
Endereço de e-Mailmarcelo.pazos@inpe.br
RevistaTectonophysics
Volume610
Páginas39–50
Nota SecundáriaA1_ENGENHARIAS_III A1_GEOGRAFIA A2_GEOCIÊNCIAS A2_ENGENHARIAS_II
Histórico (UTC)2014-06-02 17:23:38 :: administrator :: 2013 -> 2014
2018-06-04 03:04:02 :: administrator -> marcelo.pazos@inpe.br :: 2014
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Tipo de Versãopublisher
Palavras-Chavemagnetotellurics
Borborema province
brasiliano orogeny
continental breakup
Pernambuco lineament
ResumoMagnetotelluric data were collected at 25 stations along a NNW-SSE linear profile deployed perpendicularly to the main structures in the southeastern portion of the Borborema province, northeast Brazil. The geotectonic scenario is characterized by a broad range of tectomagmatic events including periods of compressive tectonism associated with amalgamation of lithospheric blocks during the Brasiliano orogeny in the Late Neoproterozoic, superimposed by extensional events related to the continental break-up and plate drift that led to the formation of the southern Atlantic Ocean in the Early Cretaceous. Strike analysis and distortion decomposition show that most of the data are two-dimensional (2D) but sensitive to distant off-profile structures. Data fit an ENE regional geoelectric strike direction, consistent with the geological and tectonic setup. A joint 2D inversion of the TE and TM modes defined by this strike direction was undertaken and the obtained model exhibits signatures of the different tectonic events in the area. The model suggests that the SE Borborema province is electrically separated into two parts. The first, comprising the southern domain of the province (Sergipano belt and Pernambuco-Alagoas block), has a highly heterogeneous crust and an anomalously conductive upper mantle. The second, comprising the transversal domain of the province (Alto Moxotó terrain), displays crust and upper mantle predominantly homogeneous and resistive. A deep Neoproterozoic lithospheric shear zone (Pernambuco lineament) marks the limit between the two contrasting domains. Also, the region where the Jatobá basin is located in the southern domain presents a striking conductor at upper- to mid-crustal depths beneath the basin. These results correlate well with seismic refraction data that indicate thicker crust for the transversal domain than for the southern domain, with the thinnest crust coinciding with the location of the Jatobá basin. The data support the conclusion that the lithosphere of the southern domain of the Borborema province was significantly stretched in the Cretaceous during the opening of the South Atlantic Ocean, allowing refertilization of depleted upper mantle with incompatible elements from enriched deeper mantle material and reactivation of older crustal fabrics. The conductivity increase below the Jatobá basin is associated with ionic conduction in a currently reactivated fracture zone filled with high salinity fluid. Apparently, the Alto Moxotó terrain worked as a region of higher resistance to stretching, causing the crustal thinning and geoelectric effects to be concentrated to the south of the Pernambuco lineament.
ÁreaCEA
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4. Condições de acesso e uso
Idiomaen
Arquivo Alvo1-s2.0-S0040195113006124-main.pdf
Grupo de Usuáriosadministrator
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Grupo de Leitoresadministrator
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Visibilidadeshown
Política de Arquivamentodenypublisher denyfinaldraft24
Permissão de Leituradeny from all and allow from 150.163
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Repositório Espelhoiconet.com.br/banon/2006/11.26.21.31
Unidades Imediatamente Superiores8JMKD3MGPCW/3EU29DP
Lista de Itens Citandosid.inpe.br/mtc-m21/2012/07.13.14.54.32 2
sid.inpe.br/mtc-m21/2012/07.13.14.40.26 2
sid.inpe.br/bibdigital/2013/10.01.22.11 1
URL (dados não confiáveis)http://dx.doi.org/10.1016/j.tecto.2013.10.008
DivulgaçãoWEBSCI; PORTALCAPES; COMPENDEX; SCOPUS.
Acervo Hospedeirosid.inpe.br/mtc-m21b/2013/09.26.14.25.20
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel format isbn lineage mark nextedition notes number orcid parameterlist parentrepositories previousedition previouslowerunit progress rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype
7. Controle da descrição
e-Mail (login)marcelo.pazos@inpe.br
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