Coble creep is a deformation mechanism characterized by the diffusion of atoms along the grain boundaries of a material. Learn more about it here.
Mineral Dissolution and Precipitation Under Stress: Model Formulation and Application to Metamorphic Reactions - Malvoisin - 2021 - Geochemistry, Geophysics, Geosystems - Wiley Online Library
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10: Grain boundary slides with respect to each others because of the
The role of creep in geopressure development
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