Joint seismic-geodynamic-mineral physical modelling of African geodynamics: A reconciliation of deep-mantle convection with surface geophysical constraints

Keyphrases

• Geophysical Constraint 100%
• Deep Mantle 100%
• Physical Modeling 100%
• Mantle Convection 100%
• African Superplume 66%
• Cape Verde Islands 66%
• Cameroon 33%
• Mantle Flow 33%
• Canary Islands 33%
• Core-mantle Boundary 33%
• Seismic Tomography 33%
• Thermochemical Convection 33%
• 3D Image 33%
• Thermal Anomaly 33%
• Shear Wave Splitting 33%
• Azimuthal Anisotropy 33%
• Hoggar 33%
• Mantle Dynamics 33%
• Late Cenozoic 33%
• Thermal Contribution 33%
• Large Flow 33%
• Surface Gravity 33%
• Geodynamic Constraints 33%
• Density Heterogeneity 33%
• Mineral Physics 33%
• Asthenospheric Flow 33%
• Chemical Anomalies 33%
• Tomography 33%
• Asthenosphere 33%
• Dynamic Yield 33%
• Flow Prediction 33%
• Convection Model 33%
• African Plate 33%
• Mantle Structure 33%
• South African 33%
• Cenozoic Volcanism 33%

Earth and Planetary Sciences

• Mantle Convection 100%
• Cabo Verde 66%
• Mantle Dynamics 33%
• African Plate 33%
• Mantle Structure 33%
• Core-Mantle Boundary 33%
• Mineral Physics 33%
• Canary Island 33%
• Thermochemical 33%
• Tomography 33%
• Shear-Wave Splitting 33%
• Seismic Tomography 33%
• Surface Gravity 33%
• Asthenosphere 33%