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Alluvial fan models in the Cantabrian successions (Cea Group) of the Esla Nappe, Cantabrian Mountains

dc.contributor.authorLlorens, T.
dc.contributor.authorColmenero, Juan Ramón
dc.contributor.authorSuárez Ruiz, I.
dc.description.abstractThe 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 sedimentsen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.subject.otherAlluvial fansen_US
dc.subject.otherCea Groupen_US
dc.subject.otherEsla Nappeen_US
dc.subject.otherCantabrian Zoneen_US
dc.titleModelos de abanicos aluviales en los materiales cantabrienses (Grupo Cea) del Manto del Esla, Cordillera Cantábricaen_US
dc.titleAlluvial fan models in the Cantabrian successions (Cea Group) of the Esla Nappe, Cantabrian Mountainseng

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