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

Mediavilla López, Rosa María and Santisteban, Juan I. and Dabrio, Cristino J. (1996) Canales de alta y baja sinuosidad en la "Facies Tierra de Campos" (Sector central de la Cuenca del Duero). Geogaceta, 20 (2). pp. 289-292. ISSN 0213-683X

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Abstract

High and low-sinuosity channels are recognized in the siliciclastic 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 lowsinuosity
streams flowing aproximately at right angles. Their combined evolution in the study area along
time and space suggest an in crease of slope during the Astaracian.


Item Type:Article
Uncontrolled Keywords:Siliciclastics, Fluvial, Sedimentology, Neogene, Duero Basin
Subjects:Sciences > Geology > Stratigraphic geology
ID Code:10727
Deposited On:31 May 2010 08:46
Last Modified:23 Feb 2011 13:03

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