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1. Identity statement
Reference TypeJournal Article
Sitemtc-m21b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP5W34M/3GD3GDR
Repositorysid.inpe.br/mtc-m21b/2014/05.30.02.20.47   (restricted access)
Last Update2014:07.16.17.24.44 (UTC) administrator
Metadata Repositorysid.inpe.br/mtc-m21b/2014/05.30.02.20.48
Metadata Last Update2018:06.04.03.04.12 (UTC) administrator
DOI10.1016/j.catena.2013.11.021
ISSN0341-8162
Labelscopus 2014-05 RossettiCoBeHaPaCaFr:2014:LaQuFl
Citation KeyRossettiCoBeHaPaCaFr:2014:LaQuFl
TitleLate Quaternary fluvial terrace evolution in the main southern Amazonian tributary
ProjectCNPq (471483/06-0; 550331/2010-7).
Year2014
Access Date2024, May 18
Type of Workjournal article
Secondary TypePRE PI
Number of Files1
Size8773 KiB
2. Context
Author1 Rossetti, Dilce de Fátima
2 Cohen, M. C. L.
3 Bertani, Thiago de Castilho
4 Hayakawa, E. H.
5 Paz, J. D. S.
6 Castro, Darcilea F.
7 Friaes, Y.
Resume Identifier1 8JMKD3MGP5W/3C9JGTQ
Group1 DSR-OBT-INPE-MCTI-GOV-BR
2
3 SER-SRE-SPG-INPE-MCTI-GOV-BR
Affiliation1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Universidade Federal do Pará, Centro de Geociências, Belém, 66075-900 PA, Brazil
3 Instituto Nacional de Pesquisas Espaciais (INPE)
4 Universidade Federal de Alfenas, Instituto de Ciências da Natureza (ICN), Rua Gabriel Monteiro da Silva, 700-Prédio V Centro-Alfenas/MG, Brazil
5 Universidade Federal do Mato Grosso, Instituto de Ciências Exatas e da Terra, Av Fernando Correia, s/n, Cuiabá, 78060-900 MT, Brazil
6 Instituto Nacional de Pesquisas Espaciais (INPE)
7 Universidade Federal do Pará, Centro de Geociências, Belém, 66075-900 PA, Brazil
Author e-Mail Address1 rossetti@dsr.inpe.br
2 mcohen80@hotmail.com
3 thiagob@dsr.inpe.br
4 ericson_geo@yahoo.com.br
5 jackdspaz@yahoo.com.br
6 darcicastro@yahoo.com.br
7 yurifriaes@hotmail.com
e-Mail Addressmarcelo.pazos@inpe.br
JournalCatena
Volume116
Pages19-37
Secondary MarkA1_ENGENHARIAS_I A1_GEOGRAFIA A2_GEOCIÊNCIAS A2_CIÊNCIAS_AGRÁRIAS_I A2_ENGENHARIAS_III A2_SOCIOLOGIA B2_QUÍMICA B2_CIÊNCIAS_BIOLÓGICAS_I B3_ASTRONOMIA_/_FÍSICA C_ZOOTECNIA_/_RECURSOS_PESQUEIROS
History (UTC)2018-06-04 03:04:12 :: administrator -> marcelo.pazos@inpe.br :: 2014
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
Keywordsaggradation
deposition
fluvial landform
lowland environment
Quaternary
regional climate
river system
subsidence
tectonic evolution
tributary
Amazonia
South America
AbstractLate Quaternary sedimentary deposits from Amazonian lowlands are important geological archives for understanding the origin, evolution and controls of the largest fluvial drainage basin on Earth. Climate has been most often claimed as the main factor affecting river evolution in this region. An increasing volume of publications have also highlighted tectonics as a relevant control. This work investigates the late Quaternary evolution of the Madeira River, the biggest southern tributary of the Amazonas Basin and a major waterway in South America, with the goal of discussing the factor with highest potential of influence on its development in space and time. The approach consisted of carrying out a detailed morphological, sedimentological and chronological characterization of terrace deposits. Three terraces were recognized, which record sandy/pebbly channel, muddy channel/oxbow lake, point bar, floodplain, as well as crevasse channel, crevasse splay and levee deposits. The topographically highest terrace T1 formed in the time interval before 43,500 and 31,696-32,913. cal. yrs BP, the intermediate terrace T2 between 25,338-26,056 and 14,129-14,967. cal. yrs BP, and the lowest terrace T3 between 12,881-13,245 and 3158-3367. cal. yrs BP. These terraces are the testimony of successive downcutting and sediment aggradation. Episodes of terrace erosion and deposition cannot be fully accommodated within the framework of fluctuating river base level tied to Late Pleistocene-Holocene global or regional climate fluctuations. Changes in tectonic subsidence rates might have played an important role in the equilibrium state of this particular fluvial system. © 2013 Elsevier B.V.
AreaSRE
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Arrangement 2urlib.net > BDMCI > Fonds > Produção pgr ATUAIS > SER > Late Quaternary fluvial...
doc Directory Contentaccess
source Directory Contentthere are no files
agreement Directory Contentthere are no files
4. Conditions of access and use
Languageen
Target File1-s2.0-S0341816213003019-main.pdf
User Groupadministrator
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Reader Groupadministrator
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Visibilityshown
Archiving Policydenypublisher denyfinaldraft24
Read Permissiondeny from all and allow from 150.163
Update Permissionnot transferred
5. Allied materials
Mirror Repositoryiconet.com.br/banon/2006/11.26.21.31
Next Higher Units8JMKD3MGPCW/3ER446E
8JMKD3MGPCW/3F3NU5S
Citing Item Listsid.inpe.br/bibdigital/2013/10.18.22.34 5
sid.inpe.br/mtc-m21/2012/07.13.14.44.37 2
sid.inpe.br/bibdigital/2013/09.13.21.11 1
URL (untrusted data)http://dx.doi.org/10.1016/j.catena.2013.11.021
DisseminationWEBSCI; PORTALCAPES; SCOPUS.
Host Collectionsid.inpe.br/mtc-m21b/2013/09.26.14.25.20
6. Notes
Empty Fieldsalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel format isbn lineage mark month nextedition notes number orcid parameterlist parentrepositories previousedition previouslowerunit progress rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype
7. Description control
e-Mail (login)marcelo.pazos@inpe.br
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