Nieto, Luis M.Ruiz Ortiz, Pedro AlejandroRey Arrans, Javier2014-11-182014-11-182002http://hdl.handle.net/10272/9342The break-up of the lower Liassic carbonate platform (Fm Gavilán) in the Jabalcuz area records a variety of sedimentary models of this event. Two fracture phases related to the genesis of the Fm GavUán-top unconformity have been recognized. These fracture phases and sea-level fluctuations were responsible for the differentiation of areas where, 1) condensed levels on relative submarine highs, 2) fault-related carbonate clastic wedges, and 3) paleokarst and related features on relatively more elevated and temporary emerged areas, were deposited. The presence of all this sedimentary models in a same laterally continuous outcrop, is really exceptional in the whole Betic External ZonesspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Carixian-DomerianCarbonate platformPelagic sedimentationUnconformityPalaeofaultjournal articleopen access