Modelos de abanicos aluviales en los materiales cantabrienses (Grupo Cea) del Manto del Esla, Cordillera Cantábrica

dc.contributor.author	Llorens, T.
dc.contributor.author	Colmenero, Juan Ramón
dc.contributor.author	Suárez Ruiz, I.
dc.date.accessioned	2014-07-22T08:15:53Z
dc.date.available	2014-07-22T08:15:53Z
dc.date.issued	2006
dc.description.abstract	The main aim of this paper is to describe two alluvial fan models that have been generated in the Esla Nappe of the Cantabrian Zone during the lower Stephanian. These models have been named Duerna alluvial fan and Peña Verde-Remolina system. The alluvial fans were generated by two different processes, mass-flow the first, and water-flow the last one. The differences between both depositional models were promoted by alocyclic agents. The most important ot them is provenance of the sediments	en_US
dc.identifier.uri	http://hdl.handle.net/10272/8611
dc.language.iso	spa	en_US
dc.rights	Atribución-NoComercial-SinDerivadas 3.0 España
dc.rights.accessRights	open access
dc.rights.uri	http://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.other	Alluvial fans	en_US
dc.subject.other	Cea Group	en_US
dc.subject.other	Esla Nappe	en_US
dc.subject.other	Cantabrian Zone	en_US
dc.title	Modelos de abanicos aluviales en los materiales cantabrienses (Grupo Cea) del Manto del Esla, Cordillera Cantábrica	en_US
dc.title	Alluvial fan models in the Cantabrian successions (Cea Group) of the Esla Nappe, Cantabrian Mountains	eng
dc.type	journal article	en_US
dspace.entity.type	Publication

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