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Sandy Channels of the Nájera Formation: Depositional Characteristics and control factors

dc.contributor.authorMolinero Huguet, J.
dc.contributor.authorColombo Piñol, Ferrán
dc.description.abstractThe studied sedimentological section is located in continental tertiary sediments of the western part of the Ebro Basin, and have been interpreted as being generated by braided streams in a general depositional subenvironment corresponding to the external zones of alluvial fans. In this context we found channel deposits with characteristics that are typical of meandering rivers, suggesting that some streams with a sinuous thalweg circulated within this braid plain. The significant agradational pattern shown by these deposits was conditioned by both the lithological characteristics of the bed and the extra sedimentary supply from a local relief which was formed in response to the activity of a blind thrusten_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherNajera Formationen_US
dc.subject.otherEbro Basinen_US
dc.subject.otherLa Riojaen_US
dc.titleCanales arenosos de la Formación Nájera: Características Deposicionales y factores de controlen_US
dc.titleSandy Channels of the Nájera Formation: Depositional Characteristics and control factorseng

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