Ruiz Ortiz, Pedro AlejandroMolina, José MiguelNieto, Luis M.2016-06-012016-06-011996http://hdl.handle.net/10272/12217Carbonate 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 depositionspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Carbonate turbiditesBase-of-slope apronBetic External ZonesUpper JurassicLower Cretaceousjournal articleopen access