Mostrar el registro sencillo del ítem

dc.contributor.authorCorrea, Iran Carlos Stallivierept_BR
dc.date.accessioned2010-05-20T04:16:24Zpt_BR
dc.date.issued2005pt_BR
dc.identifier.issn1518-2398pt_BR
dc.identifier.urihttp://hdl.handle.net/10183/22622pt_BR
dc.description.abstractFrom statistical parameters of the bottom morphology and of the application of the diagram proposed by Pejrup(1988) it was possible to characterize the dynamic and sedimentary processes that occur in the estuary of the Marajó bay. The sediments that recover the bottom of the studied area are formed by medium to very fine sands that grade to coarse to fine silt in direction to the continental shelf. The hydrodynamic of the area is dominated by the tidal and fluvial currents as well, partly due the action of winds which influence these currents. These factors associated with the estuarine circulation, are responsible for the transport, redistribution and deposition of the sediments in the study area.en
dc.format.mimetypeapplication/pdf
dc.language.isoporpt_BR
dc.relation.ispartofPesquisas em Geociências. Vol. 32, n.2 (2005), p.109-118pt_BR
dc.rightsOpen Accessen
dc.subjectMorphologyen
dc.subjectHidrodinâmicapt_BR
dc.subjectHydrodynamicen
dc.subjectMarajó, Baía de, Estuário (PA)pt_BR
dc.subjectTidal currentsen
dc.subjectEstuarine circulationen
dc.subjectMarajó bayen
dc.titleAplicação do diagrama de Pejrup na interpretação da sedimentação e da dinâmica do estuário da Baía de Marajó-PApt_BR
dc.typeArtigo de periódicopt_BR
dc.identifier.nrb000545481pt_BR
dc.type.originNacionalpt_BR


Ficheros en el ítem

Thumbnail
   

Este ítem está licenciado en la Creative Commons License

Mostrar el registro sencillo del ítem