Fig. 5From: Coupled onshore erosion and offshore sediment loading as causes of lower crust flow on the margins of South China SeaReconstructed tectonic subsidence for the central Baiyun Sag showing how the observed depth is substantially higher than that predicted based on syn-rift subsidence. Tectonic subsidence of the basement increases as the rate of sedimentation increases in the early Miocene. Modified from Clift et al. (2015)Back to article page