The Longmen Shan fold-and-thrust belt is located between the highly elevated eastern Tibetan Plateau and the low-relief Sichuan Basin, defining the steepest margin around the Tibetan Plateau (Burchfiel et al., 1995;Clark & Royden, 2000;Clark et al., 2004;Kirby et al., 2002) (Figure 1). Unlike rivers draining the northern margin of the Tibetan Plateau, which flow north into Tarim Basin, the Yangtze River in the eastern margin flows into the southern Sichuan Basin and continues eastward into the East China Sea (Figures 1 and 2) (Zheng et al., 2013(Zheng et al., , 2021. During the Late Cenozoic, reorganization of the Yangtze drainage system may have led to large-scale erosion within the Sichuan Basin, with approximately 1-4 km of sediment being removed (Richardson et al., 2010). The Longmen Shan lacks evidence of a large foredeep flexure and syn-tectonic deposition during the Late Cenozoic, with a maximum Quaternary sedimentation thickness in the western Sichuan Basin of ∼600 m (Guo et al., 1996).