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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m16d.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP7W/3E9AHHU
Repositóriosid.inpe.br/mtc-m19/2013/06.08.22.44.50   (acesso restrito)
Última Atualização2013:07.17.16.27.28 (UTC) administrator
Repositório de Metadadossid.inpe.br/mtc-m19/2013/06.08.22.44.51
Última Atualização dos Metadados2021:07.28.22.49.00 (UTC) administrator
DOI10.1016/j.earscirev.2013.04.005
ISSN0012-8252
Rótuloscopus
Chave de CitaçãoRossettiBezeDomi:2013:LaOlTr
TítuloLate oligocene-miocene transgressions along the equatorial and eastern margins of Brazil
ProjetoFAPESP (2009/472131-5; 2012/06010-5); CNPq (573713/2008-1)
Ano2013
MêsAug.
Data de Acesso29 abr. 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho12296 KiB
2. Contextualização
Autor1 Rossetti, Dilce de Fátima
2 Bezerra, F. H. R.
3 Dominguez, J. M. L.
Identificador de Curriculo1 8JMKD3MGP5W/3C9JGTQ
Grupo1 DSR-OBT-INPE-MCTI-GOV-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais-INPE, Rua dos Astronautas 1758-CP 515, 12245-970 São José dos Campos, SP, Brazil
2 Universidade Federal do Rio Grande do Norte, UFRN, Departamento de Geologia, Campus Universitário, 59078-970, Natal, RN, Brazil
3 Universidade Federal da Bahia, UFBA, Instituto de Geociências-Rua Barão de Jeremoabo, s/n Campus Universitário de Ondina, CP: 40170-115, Salvador, BA, Brazil
Endereço de e-Mail do Autor1 rossetti@dsr.inpe.br
2 bezerrafh@geologia.ufrn.br
3 landim@ufba.br
Endereço de e-Mailmarcelo.pazos@inpe.br
RevistaEarth Science Reviews
Volume123
Páginas87-112
Nota SecundáriaA1 A1 C
Histórico (UTC)2021-07-28 22:49:00 :: administrator -> marcelo.pazos@inpe.br :: 2013
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-ChaveMiocene
Continental Brazilian margin
Tidal processes
Transgressions
Sea level
Tectonics
ResumoThe seaboard of Brazil is a highly favorable setting for studying episodes of worldwide sea-level rise because of its passive nature. Previous studies of the equatorial coast of Brazil have led to the recognition of extensive Oligo-Miocene and Miocene marine-influenced deposits, but these deposits have been overlooked in other coastal areas of Brazil. The aim of the present study is to show the origin and evolution of late Oligocene and Miocene marine-influenced strata exposed in more than 5000. km of coastal areas along the WNW-trending equatorial and NNE-trending eastern Brazilian continental margins. We review the most relevant data concerning the strata of these ages exposed along the equatorial and eastern margins of Brazil, and combine them with new data. Based on these occurrences, we analyze the history of sea-level fluctuations and show that marine-influenced strata are more widespread in these margins than originally thought. Our main results indicate that a marine influence is not only imprinted in the deposits exposed along the equatorial margin, but it is also widespread in several areas of the eastern margin. For a long geological time interval ranging from the end of the Cretaceous or Paleogene up to the late Oligocene, most of the Brazilian coast remained a non-depositional site exposed to subaerial erosion and lateritic soil development. The combination of sea-level rise and tectonic subsidence promoted sediment accumulation in the onshore portion of several basins. Two transgressive episodes occurred: one in the Oligo-Miocene and another in the early/middle Miocene. The latter gave rise to deposition of the Barreiras Formation. However, during the supposedly middle Miocene eustatic sea-level highstand in coastal Brazil, there was a renewed and extensive phase of non-deposition and subaerial erosion with lateritic soil formation, a process that lasted up to the Late Quaternary. This mismatching of the sedimentary record with other South American and continental areas is discussed herein. As in many other areas of South America and of the world, the regressive-transgressive events recorded along the Brazilian coast most likely responded to a combination of eustatic sea-level fluctuations and local factors such as tectonic activity, intraplate stresses and changes in dynamic topography during the post-rift history of the eastern South American Plate.
ÁreaSRE
Arranjourlib.net > DIDSR > Late oligocene-miocene transgressions...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
Idiomaen
Arquivo Alvo1-s2.0-S0012825213000792-main.pdf
Grupo de Usuáriosadministrator
marcelo.pazos@inpe.br
Grupo de Leitoresadministrator
marcelo.pazos@inpe.br
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/3ER446E
Lista de Itens Citandosid.inpe.br/mtc-m21/2012/07.13.14.44.37 2
URL (dados não confiáveis)http://dx.doi.org/10.1016/j.earscirev.2013.04.005
DivulgaçãoWEBSCI; PORTALCAPES; COMPENDEX; SCOPUS.
Acervo Hospedeirosid.inpe.br/mtc-m19@80/2009/08.21.17.02
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 typeofwork
7. Controle da descrição
e-Mail (login)marcelo.pazos@inpe.br
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