Self-organisation and fracture connectivity in rapidly heated continental crust

Keyphrases

• Source Area 100%
• Continental Crust 100%
• Fracture Network 100%
• Fracture Connectivity 100%
• Self-organization 100%
• Stiffness 50%
• Order of Magnitude 50%
• Partial Melt 50%
• Local Strain 50%
• Partial Melting 50%
• Top-bottom 50%
• Basaltic Magma 50%
• Single Structure 50%
• Strain Path 50%
• Physical Model 50%
• Prograde 50%
• Thermal Perturbation 50%
• Melt Transport 50%
• Simple Random 50%
• Interconnected Structure 50%
• Buoyancy-driven 50%
• Thermal Expansion 50%
• Thermal Energy 50%
• Crustal Deformation 50%
• Irreversible Processes 50%
• Vertical Fracture 50%
• Evolution Rule 50%
• Volume Expansion 50%
• Random Graph Models 50%
• Nonlinear Evolution 50%
• Regional Metamorphism 50%
• Isolated Fracture 50%
• Temperature Gradient 50%
• Volume Strain 50%
• High Permeability 50%
• Deviatoric Strain 50%
• Fracture Permeability 50%
• Fracture Spacing 50%
• Fracture Alignment 50%
• Heterogeneous Media 50%
• Single Pattern 50%

Engineering

• Continental Crust 100%
• Source Region 100%
• Self-Organization 100%
• Directionality 100%
• Fracture Network 100%
• Thermal Energy 50%
• Local Strain 50%
• Irreversible Process 50%
• Physical Model 50%
• Strain Path 50%
• Temperature Gradient 50%
• Deviatoric 50%
• Evolution Rule 50%
• Fracture Permeability 50%

Earth and Planetary Sciences

• Continental Crust 100%
• Self Organization 100%
• Fracture Network 100%
• Magma 50%
• Timescale 50%
• Partial Melting 50%
• Thermal Expansion 50%
• Heterogeneous Medium 50%
• Irreversible Process 50%
• Crustal Deformation 50%
• Regional Metamorphism 50%
• Thermal Energy 50%