Sola, Fernando2013-11-212013-11-212010http://hdl.handle.net/10272/7460A conglomeratic level intercalated in a turbiditic sequence in the Almanzora corridor (Betic Cordillera) has been mapped. This level is 3 to 15 m thick, with clasts bigger than 3 m diameter. It can be continued along 6 km, which makes it being a good key bed in the study area. The level origin has been interpreted as a collapse deposit from the southern margin of the basin, probably due to a seismic eventspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Key bedSeismiteGordo MegabedAlmanzora Corridorjournal articleopen access