“…The closure of the back-arc basin started at the beginning of the Late Cretaceous, while foreland subsidence, detrital supply, and facies changes related to the creation of the foreland basin system, are recorded from the Turonian to Campanian (Biddle et al, 1986;Fildani et al, 2003;Olivero et al, 2003;Fildani and Hessler, 2005;Romans et al, 2010Romans et al, , 2011.…”