Montes Santiago, M. J.Colombo Piñol, Ferrán2015-10-162015-10-161996http://hdl.handle.net/10272/11219In 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 outcropsspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Regional geologySequential analysisUpper EoceneJaca BasinPyreneesjournal articleopen access