Turbiditas calcáreas y otros fenómenos de resedimentación/ erosión en el Jurásico superior-Cretácico inferior de la unidad de Huelma (Jaén). Zonas Externas de las cordilleras Béticas

Abstract

Carbonate turbidites made up by conglomerates and calcarenites are interpreted as a base-of-slope apron. The slope was, probably, the transition between the trough of the Intermediate domain and the External Subbetic swell. This slope was a place of erosion and resedimentation during the Late Jurassic and Early Cretaceous, in relation with two main tectonic events which resulted in the erosion of the platform margin and turbidite deposition