Initial subsurface layering, if any.
Properties of existing rocks/sediments.
Sea-level change curve.
Sources of flow and sediment, sources of wave action, boundary conditions Externally imposed vertical tectonics as a function of horizontal position and time
Erosion and deposition through time.
Optionally, compaction, including porosity reduction.
Clastic erosion, transport, deposition
Compaction (load-based, vertical porous flow, full 3D porous flow)
Rudimentary carbonate growth
Separate equations for wave propagation
Shield's criterion and transport capacity criterion for clastic transport (similar to SEDSIM)
Sigle-phase flow in porous media for vertical and 3D compaction options.
This part will be filled out by CSDMS staff
See more publications of GPM