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Álvaro, J.J. ; Vennin, E. ; Moreno-Eiris, Elena ; Perejón, Antonio ; Bechstádt, T. | Sociedad Geológica de España. | 2000In the Esla nappe, three major discontinuities have been recognized within the Lancara Formation. Discontinuity D1 is located at the top of the white bedded limestones. It is recognized as an erosive contact and marks a sharp change from a perit[...]texto impreso
Álvaro, J.J. ; Vennin, E. ; Moreno-Eiris, Elena ; Perejón, Antonio ; Bechstádt, T. | Sociedad Geológica de España. | 2000In the Esla nappe, three major discontinuities have been recognized within the Lancara Formation. Discontinuity D1 is located at the top of the white bedded limestones. It is recognized as an erosive contact and marks a sharp change from a perit[...]
