Canales de alta y baja sinuosidad en la "Facies Tierra de Campos" (Sector central de la Cuenca del Duero)

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dc.contributor.authorMediavilla López, Rosa
dc.contributor.authorSantisteban, Juan Ignacio
dc.contributor.authorDabrio, Cristino José
dc.date.accessioned2016-04-08T09:50:42Z
dc.date.available2016-04-08T09:50:42Z
dc.date.issued1996
dc.description.abstractHigh and low-sinuosity channels are recognized in the silicidastic fluviatile sediments of the "Facies Tierra de Campos" in the central sector of Duero Basin. From paleodrainage directions and their lateral relations, we propose a model integrated by a high-sinuosity main-collector system and subsidiary low-sinuosity streams flowing aproximately at right angles. Their combined evolution in the study area along time and space suggest an increase of slope during the Astaracianen_US
dc.identifier.urihttp://hdl.handle.net/10272/11817
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherSiIiciclasticsen_US
dc.subject.otherFluvialen_US
dc.subject.otherSedimentologyen_US
dc.subject.otherNeogeneen_US
dc.subject.otherDuero Basinen_US
dc.titleCanales de alta y baja sinuosidad en la "Facies Tierra de Campos" (Sector central de la Cuenca del Duero)en_US
dc.titleHigh and low-sinuosity channels into the "Facies Tierra de Campos" (Central sector of Duero Basin)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 20-2, (1996)