Resumen de Evolución paleogeográfica de la Cuenca Ibérica en el Cretácico Superior.
Manuel Segura Redondo, José Francisco García-Hidalgo Pallarés, María Beatriz Carenas Fernández
In the Iberian Basin, during Upper Albian - Middle Campanian, several shallow carbonate platforms were developed. These platforms grade landwards, westwards to the Hesperian Massit to siliciclastic, littoral and coastal sediments. Two major depositional megasequences (2nd order) and 72 depositional sequences (3rd order) have been recognized. Detailed paleogeographical maps for the eleven basal depositional sequences are presented in this paper. Temporal ranging of these maps is about 2 My, from Upper Albian (702 My) to Lower Campanian (83 My).
