Resumen de El límite meridional de la transgresión cenomaniense superior en la Cordillera Ibérica (Murcia, Albacete y Valencia)

Rocío Giménez Fernández, María del Carmen Arias Fernández, Lorenzo Vilas Minondo

• During Late Cenomanian, an Atlantic transgression occurs as a result of the Iberian Plate tilting. Its southern limit is recognized in the Murcia-Albacete-Valencia area, with continental sediments, which are dividing the Iberian and Betic basins during that age.