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dc.contributor.authorStevaux, J. C.
dc.contributor.authorSouza, I. A.
dc.date.accessioned2014-05-20T15:25:42Z
dc.date.available2014-05-20T15:25:42Z
dc.date.issued2004-01-01
dc.identifierhttp://dx.doi.org/10.1016/S1040-6182(03)00042-9
dc.identifier.citationQuaternary International. Oxford: Pergamon-Elsevier B.V., v. 114, p. 55-65, 2004.
dc.identifier.issn1040-6182
dc.identifier.urihttp://hdl.handle.net/11449/36057
dc.description.abstractFluvial environments and sedimentary facies involved in the floodplain (C2a type) construction of an anastomosed river system (Upper Parana River, Brazil) were studied. Sediment volume of floodplain deposits and sedimentation rate of each environment were obtained: channel (51.56%; 8.5 mm/yr), splay (33.85%; 1.27 mm/yr), pond (8.60%; 1.0 mm/yr), abandonment (3.64%; 3.87 mm/yr) and natural levee (3.41%; 2.34 mm/yr), reaching a total sedimentation rate average of 5.07 mm/yr. The causes of abandonment are also discussed. (C) 2003 Elsevier B.V. Ltd and INQUA. All rights reserved.en
dc.format.extent55-65
dc.language.isoeng
dc.publisherElsevier B.V.
dc.relation.ispartofQuaternary International
dc.sourceWeb of Science
dc.titleFloodplain construction in an anastomosed riveren
dc.typeArtigo
dcterms.licensehttp://www.elsevier.com/about/open-access/open-access-policies/article-posting-policy
dcterms.rightsHolderElsevier B.V.
dc.contributor.institutionUniversidade Estadual de Maringá (UEM)
dc.contributor.institutionUniversidade Estadual Paulista (Unesp)
dc.description.affiliationUniv Estadual Maringa, Dept Geog, BR-87020900 Maringa, Parana, Brazil
dc.description.affiliationUniv Estadual Paulista, Rio Claro, SP, Brazil
dc.description.affiliationUnespUniv Estadual Paulista, Rio Claro, SP, Brazil
dc.identifier.doi10.1016/S1040-6182(03)00042-9
dc.identifier.wosWOS:000187735200007
dc.rights.accessRightsAcesso restrito
dc.relation.ispartofjcr2.163
dc.relation.ispartofsjr1,123
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