García, A.Segura, M.García Hidalgo, J. F.Ruiz, G.Gil, J.Carenas, B.2015-11-202015-11-201996http://hdl.handle.net/10272/11380The Middle Cretaceous in the Iberian Ranges is a 2nd order cycle with an Upper Albian - Middle Turonian age. The cycle is bounded by two major unconformities and comprise 8 depositional sequences (3rd orderI The four basal sequences onlap older deposits; maximum marine facies are located in the fifth sequence (Picofrentes Marls) and the upper three sequences offlap rapidly northwestwards. Along this time there was a northwestward shifts in the basin and Tethyan transgressions (Upper Albian - Middle Cenomanian) change to Atlantic ones (uppermost Cenomanian - Middle Turonian)spaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Middle CretaceousDepositional sequencesCentral MountainsIberian RangesSpainDiscontinuidades estratigráficas y secuencias deposicionales del Cretácico medio (Albiense superior-Turoniense medio) en la Cordillera Ibérica central y el Sistema Central meridionalMiddle Cretaceous (Upper Albian-Middle Turonian) stratigraphic unconformities and Depositional Sequences of the central Iberian Ranges and southern Central Mountainsjournal articleopen access