@article{10272/11219,
year = {1996},
url = {http://hdl.handle.net/10272/11219},
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},
publisher = {Sociedad Geológica de España},
title = {Análisis secuencial y correlación de los abanicos aluviales de Peña Oroel y la Sierra de Cancias. (Eoceno superior. Cuenca Surpirenaica Central)},
title = {Sequential analysis and stratigraphic relationship of Peña Oroel and Sierra de Cancias aluvial fans. (Upper
Eocene. South-Pyrenean Central Basin)},
author = {Montes Santiago, M. J. and Colombo Piñol, Ferrán},
}