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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemarte3.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador6qtX3pFwXQZ3r59YCT/GUiif
Repositóriosid.inpe.br/iris@1905/2005/07.29.02.01.31   (acesso restrito)
Última Atualização2015:09.08.17.44.15 (UTC) marciana
Repositório de Metadadossid.inpe.br/iris@1905/2005/07.29.02.01.47
Última Atualização dos Metadados2018:06.06.04.14.26 (UTC) administrator
Chave SecundáriaINPE-5825-PRE/1971
ISSN0040-1951
1879-3266
Rótulo7202
Chave de CitaçãoPadilhaTrivVitoCost:1991:GeCoTe
TítuloGeophysical contraints on tectonic models of the Taubate Basin southeastern Brazil
Ano1991
Data Secundária19960104
MêsSet.
Data de Acesso08 maio 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho1530 KiB
2. Contextualização
Autor1 Padilha, Antonio Lopes
2 Trivedi, Nalin Babulal
3 Vitorello, Icaro
4 Costa, José Marques da
Grupo1 DGE-INPE-BR
RevistaTectonophysics
Volume196
Número1-2
Páginas157-172
Histórico (UTC)2014-09-29 15:13:34 :: administrator -> marciana :: 1991
2015-09-08 17:44:15 :: marciana -> administrator :: 1991
2018-06-06 04:14:26 :: administrator -> marciana :: 1991
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Palavras-ChaveGEOFISICA ESPACIAL
ResumoMagnetotelluric, gravity and geothermal flux data are analysed to constrain the tectonic evolution of the Taubate Basin, a SW-NE 20 km wide and 170 km long rift-like Tertiary basin in southeastern Brazil. The basin is characterized by half-grabens and contains up to 1000 m of sediments cut by normal faults. The magnetotelluric measurements show the presence of two layers: an upper highly conductive one (less than 10 omega m from 1-D inversions), associated with Tertiary sediments, and an extremely resistive (more than 10 000 omega m) lower layer, related to the crystalline basement. Gravity anomalies in the region are ascribed to both near-surface sources, sediments and granites, and a deep-seated source associated with crustal thinning towards the continental margin. Available geothermal flux values within the basin are anomalously high; however, they have probably been affected by convective transport because they were determined in water boreholes. These results suggest a stable thermal regime at present and, viewed together with the absence of magmatism and thermal subsidence, indicate that the mechanism related to the basin formation did not originate a deep-seated thermal anomaly in the region. The event can be seen as a shallow one, involving a small area in the upper part of the crust. The region can be characterized typically as a strike-slip mobile zone, with horizontal displacements between juxtaposed blocks. A transtensional model is suggested for the Taubate Basin to explain some of its principal geological features.
ÁreaCEA
ArranjoGeophysical contraints on...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
Arquivo Alvo1991_padilha.pdf
Grupo de Usuáriosadministrator
marciana
Grupo de Leitoresadministrator
marciana
Visibilidadeshown
Política de Arquivamentodenypublisher denyfinaldraft24
Permissão de Leituradeny from all and allow from 150.163
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3EU29DP
DivulgaçãoWEBSCI; PORTALCAPES.
Acervo Hospedeirosid.inpe.br/banon/2001/04.03.15.36
6. Notas
Campos Vaziosaffiliation alternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel doi e-mailaddress electronicmailaddress format isbn language lineage mark mirrorrepository nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project resumeid rightsholder schedulinginformation secondarymark session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url versiontype
7. Controle da descrição
e-Mail (login)marciana
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