Compaction Phases and Pore Collapse in Lower Cretaceous Chalk: Insight from Biot’s Coefficient

Engineering

• Elastic Strain 100%
• Compaction Phase 100%
• Porosity 66%
• Plastic Component 66%
• Physical Parameter 33%
• Subsurface 33%
• Saturated Water 33%
• Equilibration 33%
• Micro Crack 33%
• Elastic Wave 33%
• Strain Hardening 33%
• Assuming 33%
• Contact Area 33%
• Constant Magnitude 33%
• Core Recovery 33%
• Microcracks 33%
• Scale Model 33%
• Effective Stress 33%
• Wave Velocity 33%
• Bulk Density 33%

Earth and Planetary Sciences

• Laboratory Experiment 100%
• Porosity 100%
• Lower Cretaceous 100%
• Bulk Density 50%
• Wave Velocity 50%
• Scale Model 50%
• Elastic Wave 50%
• North Sea 50%
• Calcite 50%
• Strain Hardening 50%
• Microcracks 50%

Keyphrases

• Phase Collapse 100%
• Elastoplastic Hardening 25%
• Elastic Hardening 25%
• Core Recovery 25%