Theoretical Basin ModellingEmphasising the unified approach of mathematical analysis and computer modelling to study all these important processes, this book is especially concerned with models which can describe the evolution of porosity and pore pressure as well as the reaction of minerals coupled with the flow in deformable porous media. |
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0.5 Porosity Figure approximation asymptotic analysis asymptotic solutions Athy-type Audet & Fowler behaviour boundary conditions boundary layer burial chapter clay compaction and diagenesis compaction model Comparison constant Darcy's law dehydration model depth diagenesis process diagenetic dimensionless dissolution and precipitation dissolution-precipitation effective pressure equa equation becomes equilibrium Ət Əz fast compaction function geological governing equations heat conduction Helgeson hydrostatic illite interface K-feldspar dissolution kinetics Lasaga loading mechanism mineral model equations montmorillonite moving boundary non-linear diffusion nonlinear nucleation obtained overburden pressure overpressuring parameter permeability pore fluid pore pressure pore water porosity porosity evolution porosity profile quartz rate laws reaction rate scaled height sedimentary basins sedimentation rate slow compaction smectite smectite dissolution soil solubility Solution with Numeric STANFORD LIBRARIES surface thickness tion top region Turcotte URL line valid velocity viscous compaction volume fractions ρι Φι θα Φο Әр фо მი