Fig. 4From: Coupled onshore erosion and offshore sediment loading as causes of lower crust flow on the margins of South China Sea a Geological cross-section through the Woodlark Basin based on seismic profile from Taylor et al. (1995). b Forward model of the basin predicted from faulting seen in Profile A together with the flexural cantilever model. c Estimates of lower crustal extension compared with total and upper crustal valuesBack to article page