Flexural isostatic response of continental-scale deltas to climatically driven sea level changes
Simulating how flexural isostatic responses to climatically driven sea level changes shape continental-scale delta evolution on passive margins.
Xuesong Ding
Research Assistant Professor
Xuesong Ding uses numerical modelling to investigate the interplay between dynamic topography, tectonics, sea-level change, and sediment transport on basin evolution.