Canales de alta y baja sinuosidad en la

High and low-sinuosity channels into the "Facies Tierra de Campos" (Central sector of Duero Basin)

dc.contributor.author	Mediavilla López, Rosa
dc.contributor.author	Santisteban, Juan Ignacio
dc.contributor.author	Dabrio, Cristino José
dc.date.accessioned	2016-04-08T09:50:42Z
dc.date.available	2016-04-08T09:50:42Z
dc.date.issued	1996
dc.identifier.uri	http://hdl.handle.net/10272/11817
dc.description.abstract	High 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 Astaracian	en_US
dc.language.iso	spa	en_US
dc.publisher	Sociedad Geológica de España	en_US
dc.rights	Atribución-NoComercial-SinDerivadas 3.0 España	*
dc.rights.uri	http://creativecommons.org/licenses/by-nc-nd/3.0/es/	*
dc.subject.other	SiIiciclastics	en_US
dc.subject.other	Fluvial	en_US
dc.subject.other	Sedimentology	en_US
dc.subject.other	Neogene	en_US
dc.subject.other	Duero Basin	en_US
dc.title	Canales de alta y baja sinuosidad en la "Facies Tierra de Campos" (Sector central de la Cuenca del Duero)	en_US
dc.title	High and low-sinuosity channels into the "Facies Tierra de Campos" (Central sector of Duero Basin)	eng
dc.type	info:eu-repo/semantics/article	en_US
dc.rights.accessRights	info:eu-repo/semantics/openAccess	en_US

Except where otherwise noted, this item's license is described as Atribución-NoComercial-SinDerivadas 3.0 España

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

High and low-sinuosity channels into the "Facies Tierra de Campos" (Central sector of Duero Basin)

dc.contributor.author	Mediavilla López, Rosa
dc.contributor.author	Santisteban, Juan Ignacio
dc.contributor.author	Dabrio, Cristino José
dc.date.accessioned	2016-04-08T09:50:42Z
dc.date.available	2016-04-08T09:50:42Z
dc.date.issued	1996
dc.identifier.uri	http://hdl.handle.net/10272/11817
dc.description.abstract	High 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 Astaracian	en_US
dc.language.iso	spa	en_US
dc.publisher	Sociedad Geológica de España	en_US
dc.rights	Atribución-NoComercial-SinDerivadas 3.0 España	*
dc.rights.uri	http://creativecommons.org/licenses/by-nc-nd/3.0/es/	*
dc.subject.other	SiIiciclastics	en_US
dc.subject.other	Fluvial	en_US
dc.subject.other	Sedimentology	en_US
dc.subject.other	Neogene	en_US
dc.subject.other	Duero Basin	en_US
dc.title	Canales de alta y baja sinuosidad en la "Facies Tierra de Campos" (Sector central de la Cuenca del Duero)	en_US
dc.title	High and low-sinuosity channels into the "Facies Tierra de Campos" (Central sector of Duero Basin)	eng
dc.type	info:eu-repo/semantics/article	en_US
dc.rights.accessRights	info:eu-repo/semantics/openAccess	en_US

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