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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m21d.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W34T/46M8NUH
Repositóriosid.inpe.br/mtc-m21d/2022/04.11.18.43   (acesso restrito)
Última Atualização2022:04.11.18.43.20 (UTC) simone
Repositório de Metadadossid.inpe.br/mtc-m21d/2022/04.11.18.43.20
Última Atualização dos Metadados2023:01.03.16.46.04 (UTC) administrator
DOI10.1016/j.geomorph.2022.108218
ISSN0169-555X
Chave de CitaçãoRossettiVaBeVaAlMo:2022:LaDoRe
TítuloA large-scale domal relief due to intraplate neotectonic compression in central Amazonia
Ano2022
MêsJune
Data de Acesso18 maio 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho25769 KiB
2. Contextualização
Autor1 Rossetti, Dilce de Fátima
2 Vasconcelos, David L.
3 Bezerra, Francisco Hilário R.
4 Valeriano, Márcio de Morisson
5 Alves, Fábio Corrêa
6 Molina, Eder C.
Identificador de Curriculo1 8JMKD3MGP5W/3C9JGTQ
2
3
4 8JMKD3MGP5W/3C9JHPL
Grupo1 DIOTG-CGCT-INPE-MCTI-GOV-BR
2
3
4 DIOTG-CGCT-INPE-MCTI-GOV-BR
5 DIOTG-CGCT-INPE-MCTI-GOV-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Universidade Federal de Campina Grande (UFCG)
3 Universidade Federal do Rio Grande do Norte (UFRN)
4 Instituto Nacional de Pesquisas Espaciais (INPE)
5 Instituto Nacional de Pesquisas Espaciais (INPE)
6 Universidade de São Paulo (USP)
Endereço de e-Mail do Autor1 dilce.rossetti@inpe.br
2 davidgeologia2006.1@hotmail.com
3 hilario.bezerra@ufrn.br
4 marcio.valeriano@inpe.br
5 alves.fabioc@gmail.com
6 eder.molina@iag.usp.br
RevistaGeomorphology
Volume407
Páginase108218
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)2022-04-11 18:43:20 :: simone -> administrator ::
2022-04-11 18:43:21 :: administrator -> simone :: 2022
2022-04-11 18:44:24 :: simone -> administrator :: 2022
2023-01-03 16:46:04 :: administrator -> simone :: 2022
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-ChaveDomal relief
Growth fold
Intracratonic South America
Neotectonic geomorphology
ResumoIn intracratonic South America, the origin of neotectonic activity and its impact on large Amazonian rivers have been of continuous research interest. Despite the low relief of the land surface, which has generally been attributed to tectonic stability, there is increasing evidence of Neogene fault reactivation within central Amazonia. Recent research has also reported surface folding during the Quaternary, but this record was based only on morphological analysis of remote sensing data. This investigation focuses on a megascale (~60,000 km2) domal relief from central Amazonia (the Juruá dome). It firstly aims to verify the domal relief relationship to folding. It then explores the origin of the stress field from which it has developed within the context of Andean uplift and the westward movement of the South American plate. The approach consisted of analyzing river adjustments based on morphological and morphometric information from remote sensing imagery, integrated with subsurface data Bouguer gravity and magnetic anomaly maps, well logs, and seismic reflection sections. The results revealed that the Juruá dome coincides with the location of a basin depocenter. Subsurface evidence exists for the growth of a broad anticline producing thicker sedimentary units away from the dome core. NE- and NW-striking normal and reverse faults with flower structure geometries are abundant and suggest deformation from strike-slip tectonics. Gravity and magnetic data revealed that the fold and many of its associated faults are deep-rooted into basement rocks. Within the analyzed stratigraphic interval, faults are mostly developed into pre-Cretaceous units, but often propagate to the surface, where they define the edges of the dome and partly deform its overall shape. The fold and its related faults have modified the course of several rivers within the domal relief area, including the Juruá River, which is entrenched along NE-striking faults that are configured to release stress along the fold axis. The geomorphological and structural data are collectively compatible with a long-term NW-trending maximum horizontal compressive stress-field that is driving basin inversion. This neotectonic activity can be linked to far-field stresses from the pushes from the Andean orogeny and the movement of the South American plate against the North Andean and Nazca plates.
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4. Condições de acesso e uso
Idiomaen
Arquivo Alvorossetti_2022_large.pdf
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Grupo de Leitoresadministrator
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5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/46KUATE
Lista de Itens Citandosid.inpe.br/bibdigital/2022/04.03.22.23 4
sid.inpe.br/mtc-m21/2012/07.13.14.44.37 2
sid.inpe.br/mtc-m21/2012/07.13.14.54.54 1
DivulgaçãoWEBSCI; PORTALCAPES; COMPENDEX; SCOPUS.
Acervo Hospedeirourlib.net/www/2021/06.04.03.40
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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