RT Journal Article
T1 Modelos de abanicos aluviales en los materiales cantabrienses (Grupo Cea) del Manto del Esla, Cordillera Cantábrica
T1 Alluvial fan models in the Cantabrian successions (Cea Group) of the Esla Nappe, Cantabrian Mountains
A1 Llorens, T.
A1 Colmenero, Juan Ramón
A1 Suárez Ruiz, I.
AB The main aim of this paper is to describe two alluvial fan models that have been generated in the EslaNappe of the Cantabrian Zone during the lower Stephanian. These models have been named Duernaalluvial 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 werepromoted by alocyclic agents. The most important ot them is provenance of the sediments
YR 2006
FD 2006
LK http://hdl.handle.net/10272/8611
UL http://hdl.handle.net/10272/8611
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026