Describe processes represented by the model
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Subsidence and uplift
Eustatic oscillations
Water depth dependent in-situ carbonate production
Spatial variations in sediment production rate
Depth dependent sediment transport
Diffusional sediment transport
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Describe key physical parameters and equations
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See Burgess et al. (2001), Basin Research
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Describe length scale and resolution constraints
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10s to 100s km length scale
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Describe time scale and resolution constraints
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Internal time step years to decades
Model chron resolution 1000 years
Total run time 1-10 My
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Describe any numerical limitations and issues
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Diffusion and other sediment transport routines require short time steps
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