Juan Ignacio Baceta Caballero, Victoriano Pujalte Navarro, Aitor Payros Aguirre
Three examples of sillciclastic valley fills are recognized within the upper Maastrlchtian-lower Paleogene carbonate platform deposits of Alava. A genetic model, in the context of sequence stratigraphy, makes it evident the existence ofdiferent types ofmeaninful stratigraphic boundaries
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