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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m12.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador6qtX3pFwXQZ3r59YD6/JAKjG
Repositóriosid.inpe.br/iris@1912/2005/12.28.13.33
Última Atualização2012:11.06.17.01.23 (UTC) administrator
Repositório de Metadadossid.inpe.br/iris@1912/2005/12.28.13.33.26
Última Atualização dos Metadados2018:06.05.00.40.35 (UTC) administrator
Chave SecundáriaINPE--PRE/
DOI10.1017/S0016756805000488
ISSN0016-7568
Chave de CitaçãoPazRoss:2005:ExCoFo
TítuloLinking lacustrine cycles with syn-sedimentary tectonic episodes: an example from the Codó Formation (late Aptian), northeastern Brazil
ProjetoCNPq (460252/01)
Ano2005
MêsMay
Data de Acesso11 maio 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho965 KiB
2. Contextualização
Autor1 Paz, J. D. S.
2 Rossetti, D. F.
Grupo1 DSR-INPE-MCT-BR
2 DSR-INPE-MCT-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais, Divisão de Geração de Imagens (INPE, DGI)
2 Instituto Nacional de Pesquisas Espaciais, Coordenação do Programa Amazônia (INPE, AMZ)
Endereço de e-Mail do Autor1
2 rossetti@dsr.inpe.br
RevistaGeological Magazine
Volume142
Número3
Páginas269–285
Histórico (UTC)2005-12-28 13:33:27 :: marciana -> banon ::
2006-05-04 19:31:28 :: banon -> administrator ::
2006-09-04 16:03:10 :: administrator -> rossetti ::
2007-05-15 12:23:54 :: rossetti -> administrator ::
2010-05-12 04:10:15 :: administrator -> marciana ::
2012-11-06 17:02:46 :: marciana -> administrator :: 2005
2018-06-05 00:40:35 :: administrator -> marciana :: 2005
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-Chavelake system
cyclic sedimentation
evaporites
syn-sedimentary tectonics
late Aptian
Brazil
ResumoThe Codó Formation exposed in the eastern Grajaú Basin, northeastern Brazil, consists mostly of black shales, limestones and evaporites arranged into several shallowing-upward cycles formed by progradation of lake deposits. Three ranks of cycles are distinguished. The lower-rank cycles correspond to millimetric interbeddings of: bituminous black shales with evaporites, calcimudstones or peloidal wackestonepackstone; grey/green shale with calcimudstone, peloidal wackestonepackstone or ostracodal wackestone/grainstone; and ostracodal wackestone/grainstone and/or calcimudstones with cryptomicrobial mats and ooidal/pisoidal packstones. The intermediate-rank cycles average 1.7 m in thickness and are formed by complete and incomplete cycles. Complete cycles show a transition from central to intermediate and then to marginal facies associations and include two types: C1 cycle with central lake deposits consisting of evaporites and black shales; and C2 cycle with central lake deposits formed by grey/green shale. Complete cycles were produced by the upward gradation from central to marginal environments of the lake or saline pansabkha system. Incomplete cycles are those where at least one facies association is lacking, having been formed by successions either with central and intermediate facies associations (I1) or intermediate and marginal facies associations (I2). The higher-rank cycles are, on average, 5.2 m thick and consist of four depositional units that display shallowing-upward successions formed by complete and incomplete intermediate-rank cycles that vary their distribution upward in the section, and are bounded by sharp surfaces. While the lower-rank cycles display characteristics that reveal their seasonal signature, detailed sedimentological characterization and understanding of stratal stacking patterns related to the intermediate- and higher-rank cycles support a genesis linked to syn-sedimentary tectonic activity. This is particularly suggested by the high facies variability, limited lateral extension, and frequent and random thickness changes of the intermediate-rank cycles. Additionally, the four higher-rank cycles recognized in the Codó Formation match with stratigraphic zones having different styles of soft-sediment deformation structures attributed to seismic activities. Therefore, the several episodes of lake shallowing recorded in the Codó Formation are linked to seismic pulses that alternated with sediment deposition. This process would have created significant changes in the lake water level and resulted in sharply bounded successions with upward gradation from deeper to relatively shallower facies associations.
ÁreaSRE
Arranjourlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSR > Linking lacustrine cycles...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
URL dos dadoshttp://urlib.net/ibi/6qtX3pFwXQZ3r59YD6/JAKjG
URL dos dados zipadoshttp://urlib.net/zip/6qtX3pFwXQZ3r59YD6/JAKjG
Idiomaen
Arquivo Alvo269.full.pdf
Grupo de Usuáriosadministrator
marciana
rossetti
Grupo de Leitoresadministrator
marciana
Visibilidadeshown
Política de Arquivamentodenypublisher12 allowfinaldraft
Permissão de Leituraallow from all
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3ER446E
URL (dados não confiáveis)http://dx.doi.org.ez61.periodicos.capes.gov.br/10.1017/S0016756805000488
DivulgaçãoWEBSCI
Acervo Hospedeirosid.inpe.br/banon/2001/04.06.10.52
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress format isbn label lineage mark mirrorrepository nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress resumeid rightsholder schedulinginformation secondarydate secondarymark session shorttitle sponsor subject tertiarymark tertiarytype typeofwork
7. Controle da descrição
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