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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m21b.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W34P/3PFBKML
Repositóriosid.inpe.br/mtc-m21b/2017/08.18.18.39   (acesso restrito)
Última Atualização2017:08.18.18.39.34 (UTC) simone
Repositório de Metadadossid.inpe.br/mtc-m21b/2017/08.18.18.39.34
Última Atualização dos Metadados2018:06.04.02.27.45 (UTC) administrator
DOI10.1016/j.geomorph.2017.07.026
ISSN0169-555X
Chave de CitaçãoRossettiVaGrCoTaYe:2017:ImLaHo
TítuloThe imprint of Late Holocene tectonic reactivation on a megafan landscape in the northern Amazonian wetlands
Ano2017
MêsOct.
Data de Acesso26 abr. 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho4234 KiB
2. Contextualização
Autor1 Rossetti, Dilce de Fátima
2 Valeriano, Márcio de Morisson
3 Gribel, R.
4 Cohen, M. C. L.
5 Tatumi, Sonia H.
6 Yeed, M.
Identificador de Curriculo1 8JMKD3MGP5W/3C9JGTQ
2 8JMKD3MGP5W/3C9JHPL
Grupo1 DIDSR-CGOBT-INPE-MCTIC-GOV-BR
2 DIDSR-CGOBT-INPE-MCTIC-GOV-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
3 Instituto Nacional de Pesquisas da Amazônia (INPA)
4 Universidade Federal do Pará (UFPA)
5 Universidade Federal de São Paulo (UNIFESP)
6 Universidade Federal de São Paulo (UNIFESP)
Endereço de e-Mail do Autor1 dilce.rossetti@inpe.br
2 marcio.valeriano@inpe.br
RevistaGeomorphology
Volume295
Páginas406-418
Nota SecundáriaA1_INTERDISCIPLINAR A1_GEOGRAFIA A1_GEOCIÊNCIAS A1_ENGENHARIAS_I A1_CIÊNCIAS_AGRÁRIAS_I A2_ENGENHARIAS_III A2_BIODIVERSIDADE B1_CIÊNCIAS_BIOLÓGICAS_I B1_ANTROPOLOGIA_/_ARQUEOLOGIA B2_ASTRONOMIA_/_FÍSICA
Histórico (UTC)2017-08-18 18:39:34 :: simone -> administrator ::
2017-08-18 18:39:35 :: administrator -> simone :: 2017
2017-08-18 18:40:19 :: simone -> administrator :: 2017
2018-01-09 11:46:57 :: administrator -> simone :: 2017
2018-01-09 17:40:06 :: simone -> administrator :: 2017
2018-06-04 02:27:45 :: 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-ChaveMegafan paleolandorm
Northern Amazonia
Neotectonics
Late Holocene
ResumoThe modern Amazonian ecosystem outcomes from the complex interplay of different factors performed over the geological history, with tectonics being long speculated as perhaps a fundamental one. Nevertheless, areas where tectonic activity can be fully characterized are still scarce in view of the large dimension of this region. In this work, we investigate the signature of neotectonics in one megafan paleolandform that typifies a large sector of the Negro-Branco basin in northern Amazonia. The approach joined regional morphostructural descriptions of the Viruá megafan surface and the acquisition of topographic, sedimentological, and chronological data focusing on the central sector of the megafan. The results revealed an abundance of rivers that form dendritic, subdendritic, and trellis patterns. These rivers also have numerous straight segments, orthogonal junctions, and orthogonal shifts in courses. Structural lineaments, defined by straight channels and also straight lake margins, are aligned along the NW-SE and NE-SW directions that are coincidental with the main regional structural pattern in Amazonia. This study also led to recognize two large areas of lower topography in the south-central part of the megafan that consist of rectangular depressions parallel to the morphostructural lineaments. A sedimentological survey indicated that cores extracted external to the largest depression have only distributary channel and overbank sand sheet megafan deposits. Optically stimulated luminescence (OSL) ages ranged from 17.5 ± 2.0 to 46.9 ± 3.4 ky and radiocarbon ages ranged from 5.95.7 to 20.119.6 cal ky BP. In contrast, cores extracted within the depression consisted of fluvial deposits younger than 2.11.9 cal ky BP that increased in thickness toward the central part of the depression. We propose that the studied megafan was affected by tectonic reactivation until at least a couple thousand years ago. Tectonics would have produced subsiding areas more prone to flooding than adjacent terrains, which constituted sites for renewed deposition of fluvial sediments reworked from the megafan surface following its abandonment. A comparison of our data with those from other Amazonian areas with similar records of late Holocene tectonics suggests a landscape imprinted by faulting, probably of strike-slip motion. This finding increases the record of neotectonic activity in the Amazonian wetlands and may be useful in studies aiming at discussing the origin and extension of late Holocene deformation in the South American intraplate. In addition, we present a megafan with an unusual development in a cratonic region under the combined effect of climate and tectonics.
ÁreaSRE
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4. Condições de acesso e uso
Idiomaen
Arquivo Alvorossetti_imprint.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
Unidades Imediatamente Superiores8JMKD3MGPCW/3ER446E
Lista de Itens Citandosid.inpe.br/mtc-m21/2012/07.13.14.54.54 1
sid.inpe.br/mtc-m21/2012/07.13.14.44.37 1
DivulgaçãoWEBSCI; PORTALCAPES; COMPENDEX; SCOPUS.
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 mirrorrepository nextedition notes number orcid parameterlist parentrepositories previousedition previouslowerunit progress project rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype url
7. Controle da descrição
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