Análisis secuencial y correlación de los abanicos aluviales de Peña Oroel y la Sierra de Cancias. (Eoceno superior. Cuenca Surpirenaica Central)

Abstract

In the Cuarga Syndfne (jaca Basin), the Sierra de Cancias conglomerates, has been placed traditionally In a lower stratigraphic position than Peña Oroel conglomerates. However; a detai/led geological mapi, based in the systematic line-drawing of the photogeological layer beds, show a similar depositional architecture and a good correlationship between both outcrops