Seismic velocity structure and depth-dependence of anisotropy in the Red Sea and Arabian shield from surface wave analysis

Keyphrases

• Anisotropic Model 20%
• Anisotropy 100%
• Arabia 20%
• Arabian Peninsula 20%
• Arabian Shield 100%
• Azimuthal Anisotropy 20%
• Body Waves 20%
• Continental Rift 20%
• Crustal Velocity 20%
• Density-driven Flow 20%
• Depth Dependence 100%
• Depth Extent 20%
• Forward Model 20%
• Frequency Dependence 20%
• Function Constraints 20%
• Fundamental Mode 20%
• Great Depth 20%
• Linearized Inversion 20%
• Lithosphere-asthenosphere Boundary 40%
• Lithospheric Mantle 20%
• Love Wave 20%
• Low Shear 20%
• Low Velocity 20%
• Low-velocity Zone 20%
• Mantle Lithosphere 20%
• Oceanic Ridge 20%
• Partial Melt 20%
• Phase Delay 20%
• Phase Velocity 20%
• Rayleigh Wave 20%
• Receiver Function 20%
• Red Sea 100%
• Red Sea Coast 20%
• Rifting 20%
• Saudi Arabian 20%
• Seismic Network 20%
• Seismic Velocity Structure 100%
• Shear Velocity 60%
• Shear Wave Splitting 20%
• Shear-wave Velocity Structure 20%
• Structure Dependence 100%
• Surface Wave Analysis 100%
• Surface Waves 40%
• Upper Mantle 40%
• Velocity Contrast 20%
• Wave Observation 20%

Earth and Planetary Sciences

• Asthenosphere 40%
• Cross Correlation 20%
• Lithosphere 100%
• Love Wave 20%
• Low Velocity Zone 20%
• Phase Velocity 20%
• Rayleigh Wave 20%
• Red Sea 100%
• Rifting 20%
• Shear-Wave Splitting 20%
• Surface Wave 100%
• Upper Mantle 40%
• Velocity Structure 100%
• Wave Velocity 20%