A fictitious domain method for lithosphere-asthenosphere interaction: Application to periodic slab folding in the upper mantle

Keyphrases

• Upper Mantle 100%
• South American Plate 100%
• Transition Zone 100%
• Asthenosphere 100%
• Mantle Viscosity 100%
• Fictitious Domain Method 100%
• Overriding Plate 100%
• Lithosphere-asthenosphere Interaction 100%
• Kinematics 50%
• Viscosity 50%
• Subduction 50%
• Coupling Method 50%
• Numerical Model 50%
• Subduction Zone 50%
• Numerical Techniques 50%
• Magmatism 50%
• Finite Element Method 50%
• Discretized 50%
• Andes 50%
• Maxwell 50%
• Field Plate 50%
• Subducting Plate 50%
• Stress Regime 50%
• Nazca Plate 50%
• Simplified Formulation 50%
• Analogue Modelling 50%
• Interface Method 50%
• Flat Subduction 50%
• Viscoelastic Body 50%
• Non-matching Interfaces 50%
• Staggered Coupling 50%
• Sedimentological Record 50%
• Plate Velocity 50%
• Impenetrable Barrier 50%
• Slab Dip 50%

Earth and Planetary Sciences

• Lithosphere 100%
• Upper Mantle 100%
• Asthenosphere 100%
• Cyclicity 75%
• Subduction Zone 25%
• Andes 25%
• Magmatism 25%
• Numerical Model 25%
• Analog Model 25%
• Nazca Plate 25%