Estructuras sedimentarias de deformación originadas por licuefacción en depósitos de tormentas (Mioceno de la Cuenca del Guadalquivir, provincia de Jaén)

Abstract

Soft-sediment deformation structures related with hummocky cross stratification appear in the Upper Miocene calcarenites of the Guadalquivir Basin. They are analysed and after consider their different possible genetic mechanisms, they are interpreted as originated by licuefaction processes triggered by the storm wave action