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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Siteplutao.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
IdentificadorJ8LNKAN8RW/39RQE84
Repositóriodpi.inpe.br/plutao/2011/06.11.03.31.59   (acesso restrito)
Última Atualização2011:07.25.16.29.20 (UTC) administrator
Repositório de Metadadosdpi.inpe.br/plutao/2011/06.11.03.32
Última Atualização dos Metadados2018:06.05.00.01.19 (UTC) administrator
Chave SecundáriaINPE--PRE/
DOI10.1016/j.palaeo.2010.12.026
ISSN0031-0182
Rótulolattes: 0307721738107549 1 RossettiBGVATB:2011:LaSeLe
Chave de CitaçãoRossettiBGVAMTB:2011:LaSeLe
TítuloLate Quaternary sedimentation in the Paraíba Basin, Northeastern Brazil: landform, sea level and tectonics in Eastern South America passive margin
ProjetoFAPESP[006/04687-7]
Ano2011
MêsFeb.
Data de Acesso19 maio 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho5434 KiB
2. Contextualização
Autor1 Rossetti, Dilce de Fátima
2 Bezerra, Francisco Hilário Rego
3 Góes, Ana Maria
4 Valeriano, Márcio de Morisson
5 Andrades Filho, Clódis de Oliveira
6 Mittani, Juan Carlos Ramirez
7 Tatumi, Sonia Hatsue
8 Brito-Neves, Beijamim Bley
Identificador de Curriculo1 8JMKD3MGP5W/3C9JGTQ
2
3
4 8JMKD3MGP5W/3C9JHPL
Grupo1 DSR-OBT-INPE-MCT-BR
2
3
4 DSR-OBT-INPE-MCT-BR
5 DSR-OBT-INPE-MCT-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Univ Fed Rio Grande Norte UFRN, Natal, RN, Brazil
3 Univ Sao Paulo USP, Sao Paulo, Brazil
4 Instituto Nacional de Pesquisas Espaciais (INPE)
5 Instituto Nacional de Pesquisas Espaciais (INPE)
6 Fac Tecnol Sao Paulo FATEC SP, Sao Paulo, Brazil
7 Fac Tecnol Sao Paulo FATEC SP, Sao Paulo, Brazil
8 Univ Sao Paulo USP, Sao Paulo, Brazil
Endereço de e-Mail do Autor1 rossetti@dsr.inpe.br
2
3
4 valerian@dsr.inpe.br
Endereço de e-Mailrossetti@dsr.inpe.br
RevistaPalaeogeography, Palaeoclimatology, Palaeoecology
Volume300
Número1-4
Páginas191-204
Nota SecundáriaA1_CIÊNCIAS_BIOLÓGICAS_I A2_ECOLOGIA_E_MEIO_AMBIENTE A1_FILOSOFIA_/_TEOLOGIA:subcomissão_FILOSOFIA A2_GEOCIÊNCIAS A1_GEOGRAFIA A1_INTERDISCIPLINAR A2_SAÚDE_COLETIVA
Histórico (UTC)2011-06-11 17:43:45 :: lattes -> marciana :: 2011
2011-11-07 10:34:04 :: marciana -> administrator :: 2011
2018-06-05 00:01:19 :: administrator -> marciana :: 2011
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-ChaveSedimentary facies
Stratigraphy
Luminescence dating
Neotectonics
Sea level
Landform
South American passive margin
COSEISMIC REACTIVATION
QUARTZ
EVOLUTION
HOLOCENE
MARINE
SINGLE
PALEOGEOGRAPHY
PROTOCOL
DEPOSITS
ISLAND
ResumoLate Quaternary deposits in the northeastern Brazil have been scarcely investigated, despite their relevance to the discussion of the post-rift evolution of the South American passive margin within the context of landform, sea level and tectonic deformation. Sedimentological, stratigraphic and morphological characterization of these deposits, referred as Post-Barreiras Sediments, led to their distinction from underlying Early/Middle Miocene strata. Based on optically stimulated luminescence (OSL) dating, two sedimentary units (PB1 and PB2) were recognized and related to the time intervals between 74.8 +/- 9.3 and 30.8 +/- 6.9 ka, and 8.8 +/- 0.9 and 1.8 +/- 0.2 ka, respectively. Unit PB1 consists of indurated sandstones and breccias either with massive bedding or complex types of soft sediment deformation structures generated by contemporaneous seismic activity. Unit PB2 is composed of massive sands or sands related to structures developed by dissipation of dunes. The present work, focusing on the Post-Barreiras Sediments, discusses landform, sea level and tectonics of the eastern South American passive margin during the latest Quaternary. Non-deposition and sub-aerial exposure related to the Tortonian worldwide low sea level combined with tectonic quiescence followed the Miocene transgression. Tectonic deformation in the latest Pleistocene created space to accommodate unit PB1 in downthrown faulted blocks and, perhaps, also synclines produced by strike-slip deformation. Although deposition of this unit was simultaneous with the progressive fall in sea level that followed the Last Interglacial Maximum, punctuated rises combined with land subsidence led to marine deposition close to the modern coastline. Renewed subsidence in the Holocene gave rise to accommodation of the Post-Barreiras Sediments. Most of unit PB2 was deposited during the Holocene Transgression, but it is not composed of marine sediments, which suggests either an insignificant rise in relative sea level or aeolian reworking of thin transgressive sands. The data presented here lead to a review of the evolution of the South American passive margin based on assumptions of uniform sedimentation and undeformed planation surfaces over a wide coastal area of the northeastern Brazil. (C) 2011 Elsevier B.V. All rights reserved.
ÁreaSRE
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4. Condições de acesso e uso
Idiomaen
Arquivo Alvosdarticle-7.pdf
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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
Unidades Imediatamente Superiores8JMKD3MGPCW/3ER446E
DivulgaçãoWEBSCI; PORTALCAPES; AGU; MGA; COMPENDEX.
Acervo Hospedeirodpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel format isbn lineage mark mirrorrepository nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress readergroup rightsholder schedulinginformation secondarydate session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url
7. Controle da descrição
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