Influence of Grain Boundary Structural Evolution on Pressure Solution Creep Rates

Keyphrases

• Structural Evolution 100%
• Compaction 100%
• Creep Rate 100%
• Pressure Solution Creep 100%
• Grain Boundary 100%
• Compaction Rate 100%
• Fault Rocks 66%
• Grain Contacts 66%
• Low Porosity 66%
• Grain Boundary Evolution 66%
• Porosity 33%
• Order of Magnitude 33%
• Mass Transport 33%
• Pressure Solution 33%
• Constitutive Equation 33%
• Sodium Chloride 33%
• Analytical Model 33%
• Thermodynamic Model 33%
• Creep 33%
• Reservoir Sandstone 33%
• Grain Boundary Diffusion 33%
• Deformation Mechanism 33%
• High Porosity 33%
• Granular Materials 33%
• Stress-induced 33%
• Natural Conditions 33%
• Microphysical Processes 33%
• Solution Rate 33%
• Intergranular Pressure Solution 33%
• Constriction 33%
• High Strain 33%
• Compaction Experiment 33%
• Compaction Behavior 33%
• Upper Crust 33%
• Rock Deformation 33%
• Single Grain 33%
• Sandstone Rock 33%
• Diffusion Path 33%
• Individual Grains 33%

Engineering

• Creep Rate 100%
• Porosity 100%
• Structural Boundary 100%
• Constitutive Equation 33%
• Thermodynamic Model 33%
• Creep 33%
• Deformation Mechanism 33%
• Induced Stress 33%
• Individual Grain 33%
• Rock Deformation 33%
• Diffusion Path 33%
• Analytical Model 33%
• Grain Boundary Diffusion 33%
• Single Grain 33%
• Mass Transport 33%

Earth and Planetary Sciences

• Pressure Solution 100%
• Porosity 100%
• Structural Evolution 100%
• Laboratory Experiment 25%
• Constitutive Equation 25%
• Halite 25%
• Deformation Mechanism 25%
• Upper Crust 25%
• Sandstone 25%
• Constriction 25%
• Granular Material 25%
• Mass Transport 25%