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Metadados

1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m21b.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W34P/3NF25CP
Repositóriosid.inpe.br/mtc-m21b/2017/03.03.12.44   (acesso restrito)
Última Atualização2017:03.03.12.44.24 (UTC) administrator
Repositório de Metadadossid.inpe.br/mtc-m21b/2017/03.03.12.44.24
Última Atualização dos Metadados2018:06.04.02.27.20 (UTC) administrator
DOI10.1016/j.tecto.2017.01.022
ISSN0040-1951
Chave de CitaçãoPadilhaVitoPáduFuck:2017:ImAsWe
TítuloCryptic signatures of Neoproterozoic accretionary events in northeast Brazil imaged by magnetotellurics: Implications for the assembly of West Gondwana
Ano2017
MêsMar.
Data de Acesso08 maio 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho3208 KiB
2. Contextualização
Autor1 Padilha, Antonio Lopes
2 Vitorello, Icaro
3 Pádua, Marcelo Banik de
4 Fuck, Reinhardt A.
Identificador de Curriculo1 8JMKD3MGP5W/3C9JGJG
2 8JMKD3MGP5W/3C9JHD6
3 8JMKD3MGP5W/3C9JHNR
Grupo1 DIDGE-CGCEA-INPE-MCTIC-GOV-BR
2 GES-CEA-SESPG-INPE-MCTIC-GOV-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
3 Instituto Nacional de Pesquisas Espaciais (INPE)
4 Universidade de Brasília (UNB)
Endereço de e-Mail do Autor1 antonio.padilha@inpe.br
2
3 marcelo.banik@inpe.br
RevistaTectonophysics
Volume699
Páginas164-177
Nota SecundáriaA1_GEOGRAFIA A1_ENGENHARIAS_III A2_GEOCIÊNCIAS A2_ENGENHARIAS_II
Histórico (UTC)2017-03-03 12:44:24 :: simone -> administrator ::
2017-03-03 12:44:25 :: administrator -> simone :: 2016
2017-03-03 12:45:10 :: simone -> administrator :: 2016 -> 2017
2017-07-17 06:38:15 :: administrator -> simone :: 2017
2017-12-13 11:46:24 :: simone -> administrator :: 2017
2018-06-04 02:27:20 :: administrator -> simone :: 2017
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-ChaveComposition and structure of the continental crust
Magnetotellurics
South America
Subduction zone processes
ResumoThe Borborema Province, in northeast Brazil, is a complex orogenic system severely affected by deformational, metamorphic, and magmatic processes mostly during the Gondwana convergence in late Neoproterozoicearly Phanerozoic Brasiliano/Pan-African Orogeny. New magnetotelluric (MT) data collected along the northwestern part of the province and eastern part of the contiguous Parnaíba Basin are combined with previous MT data to assess the regional deep electrical resistivity structure. Dimensionality analysis shows that a 3D electrical structure predominates in the subsurface and thus 3D inversion was carried out. The final geoelectric model allows delineating the geometry and variation in physical properties of different lithospheric blocks bounded by major electrical discontinuities. These lithospheric blocks constitute a coalesced mosaic made up of four main terrane compartments: a resistive cratonic keel detected along the western part of the study area, currently hidden beneath the Parnaíba Basin (Parnaíba block); two complex domains in the center characterized by several resistive and conductive zones throughout the crust and upper mantle (Ceará Central and Rio Grande do Norte domains); and a conductive block in the east, with the geoelectric response being controlled by possible remains of late Neoproterozoic subduction activity to the south (Central sub-province). The interfaces between these blocks are interpreted as suture zones correlated to their Neoproterozoic collage, one curved conductor concealed by the sediments of the Parnaíba Basin and bordering the eastern margin of the basin, another huge conductor corresponding to the location of the Orós-Jaguaribe subdomain on the surface, and a third interface coinciding with the position of the Patos shear zone. The presence of these proposed sutures could be a conspicuous evidence of a Neoproterozoic accretion system in northeast Brazil and would support tectonic evolution models for the West Gondwana assembly involving oceanic closure and collision of continental blocks during the Brasiliano Orogeny.
ÁreaCEA
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Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreement
agreement.html 03/03/2017 09:44 1.0 KiB 
4. Condições de acesso e uso
Idiomaen
Arquivo Alvopadilha_crypt.pdf
Grupo de Usuáriossimone
Grupo de Leitoresadministrator
simone
Visibilidadeshown
Política de Arquivamentodenypublisher denyfinaldraft24
Permissão de Leituradeny from all and allow from 150.163
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Vinculação8JMKD3MGP5W34M/3G62S5E
Repositório Espelhosid.inpe.br/mtc-m21b/2013/09.26.14.25.22
Unidades Imediatamente Superiores8JMKD3MGPCW/3EU29DP
8JMKD3MGPCW/3F2PBEE
Lista de Itens Citandosid.inpe.br/bibdigital/2013/10.12.21.02 5
sid.inpe.br/mtc-m21/2012/07.13.14.40.26 2
sid.inpe.br/bibdigital/2013/10.01.22.11 1
DivulgaçãoWEBSCI; PORTALCAPES.
Acervo Hospedeirosid.inpe.br/mtc-m21b/2013/09.26.14.25.20
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress format isbn label lineage mark nextedition notes number orcid parameterlist parentrepositories previousedition previouslowerunit progress project rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarytype url
7. Controle da descrição
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