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dc.contributor.authorCastelltort Aiguabella, F. Xavier
dc.contributor.authorBalasch Solanes, J. Carles (Josep Carles)
dc.contributor.authorCirés Fortuny, Jordi
dc.contributor.authorColombo Piñol, Ferran
dc.date.accessioned2017-05-03T10:17:18Z
dc.date.available2017-05-03T10:17:18Z
dc.date.issued2016
dc.identifier.issn2173-6545
dc.identifier.urihttp://hdl.handle.net/10459.1/59569
dc.description.abstractThe monocline layout of the sedimentary pile of the Ebro Basin in its Eastern margin determines the generation and emptying of the adjacent erosive basins. It controls the drainage changes in the original sedimentary basin. A model of emptying erosive basins corresponding to a drainage architecture and sediment production is proposed. The emptying of erosive basins is achieved by two vectors: A) A drainage basin area growth due to anaclinal streams eroding into the resistant layers of the monocline stratigraphic succession. These streams empty and link small depressions generated at the expense of the lateral extension on the less resistant lithologic member. B) The drainage basin outlet point base level controls the drainage network entrenchment facilitated by the gradients created by Neogene extensional faults from the Valencia Trough. A model of the growth and entrenchment of erosive basins as well as the generated landforms and sediment production is described and analyzedca_ES
dc.language.isospaca_ES
dc.publisherSociedad Geológica de Españaca_ES
dc.relation.isformatofReproducció del document publicat a http://www.sociedadgeologica.es/archivos/geogacetas/geo60/geo60_13p51_54.pdfca_ES
dc.relation.ispartofGeogaceta, 2016, vol. 60, p. 51-54ca_ES
dc.rights(c) Sociedad Geológica de España, 2016ca_ES
dc.subjectDrainage networkca_ES
dc.subjectDrainage basinca_ES
dc.subjectRiver captureca_ES
dc.subjectEastern Ebro Basinca_ES
dc.subjectQuaternaryca_ES
dc.titleEvolución del drenaje en cuencas erosivas durante el Neógeno-Cuaternario. Margen oriental de la Cuenca del Ebroca_ES
dc.title.alternativeDrainage basins evolution during the Neogene-Quaternary. Ebro Basin eastern margin
dc.typearticleca_ES
dc.identifier.idgrec025316
dc.type.versionpublishedVersionca_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessca_ES


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