Remacha Grau, EduardRaïmat, C.Oms, O.Cardona, D.Mutti, E.2015-09-032015-09-031996http://hdl.handle.net/10272/11092The turbidite equivalent of the Figols Allogroup can be recognized at the base ofthe Hecho Croup. Three deposition a! sequences -Figols 1,2 and 3- are recorded and are organized in third order stages of growth. All the sequences have similar features in the first stage. Lower boundaries are tectonically induced. A sudden zonal basinward shifting occurs and depositional systems (lobes) are developed. Second and third stages are well developed in Figols 2 and 3. The second stages record a strong and progressive landward shifting in both systems and the third stages are the basinat expression of the foreland carbonate rampsspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/TurbiditesHecho GroupEocenePyreneesjournal articleopen access