Now, sequence-stratigraphic, biostratigraphic and strontium-isotopic data have made it possible to update what is known of the stratigraphy and sedimentary evolution of the Kimmeridgian–Berriasian synrift successions recorded in four subbasins (Aguilón, Oliete, Morella, Galve) of the central Iberian Rift System (NE Spain). The studied successions are arranged in three unconformity-bounded synrift sequences. The last work includes the formal definition of a new lithostratigraphic unit: the Cedrillas Formation -this unit was previously included in the lower part of the Villar del Arzobispo Fm-.
Aurell, M., Badenas, B., Canudo, J.I., Castanera, D., García-Penas, A., Gasca, J.M., Martín-Closas, C., Moliner, L., Moreno-Azanza, M., Rosales, I., Santas, L., Sequero, C., Val, J. 2019. Kimmeridgian–Berriasian stratigraphy and sedimentary evolution of the central Iberian Rift System (NE Spain). Cretaceous Research, xx, xxx-xxx. DOI: 10.1016/j.cretres.2019.05.011
Outcrop of the upper part of the Aguilar del Alfambra Formation (lower Berriasian), near Cerezos section.