
handle: 10272/11219
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
Regional geology, Pyrenees, Jaca Basin, Sequential analysis, Upper Eocene
Regional geology, Pyrenees, Jaca Basin, Sequential analysis, Upper Eocene
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