Grain-scale contact phase-field simulations of pressure solution creep indicate that microstructural geometry governs creep rates and that temperature and clay effects can be incorporated via catalyzing/inhibiting parameters without explicit clay modeling.
Griggs, Experimental flow of rocks under conditions favoring recrys- tallization, Bulletin of the Geological Society of America 51 (7) (1940) 1001–1022
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Contact phase-field modeling for chemo-mechanical degradation processes. Part II: Numerical applications with focus on pressure solution
Grain-scale contact phase-field simulations of pressure solution creep indicate that microstructural geometry governs creep rates and that temperature and clay effects can be incorporated via catalyzing/inhibiting parameters without explicit clay modeling.