We use CFD method to invesigate turbidite sedimentation during a single turbidity current event.
We use numerical simulations to study turbidity current responses, including the hydraulic behaviour and associated deposition, to typical fold and diapir-like topography in deepwater fold and thrust belt.
We use numerical simulations to domenstrate how turbidity current responses to typical relay ramp topography in rifts.
We use numerical simulation to study reactions of turbidity current to typical half-graben scale normal faults in rift basins. We find the fault-related topography has a direct impact upon its flow behaviour and preferential area of deposition.