Seismic structure of the upper mantle in a central Pacific corridor

Keyphrases

• Upper Mantle 100%
• Transition Zone 100%
• Seismic Structure 100%
• Central Pacific 100%
• Plate Motions 50%
• Frequency Dependence 50%
• Oceanic Mantle 50%
• Lower Boundary 50%
• Velocity Gradient 50%
• High Velocity 50%
• Olivine 50%
• Body Waves 50%
• Shear Wave 50%
• Attenuation 50%
• Seismic Model 50%
• Velocity Structure 50%
• Hawaii 50%
• Anisotropy 50%
• Asthenosphere 50%
• Tonga 50%
• Crystal-melt Separation 50%
• Reflectivity 50%
• Water Content 50%
• Control Model 50%
• Travel Time 50%
• Surface Waves 50%
• Final Model 50%
• Jordan 50%
• Spherically Symmetric 50%
• Low-velocity Zone 50%
• Homologous Temperature 50%
• Depth Marking 50%
• Phase Delay 50%
• Polarization Anisotropy 50%
• Radial Shear 50%
• Reverberation 50%
• Steep Gradients 50%
• Low Velocity 50%
• Higher Modes 50%
• Layered Framework 50%
• Impedance Contrast 50%
• Crust Formation 50%
• Anisotropic Layer 50%
• Shear Anisotropy 50%
• Radial Anisotropy 50%
• Surface Wave Mode 50%
• Mantle Minerals 50%
• Shear Velocity 50%
• Mantle Discontinuities 50%
• Anisotropic Structure 50%
• High Gradient 50%
• Separation Zone 50%
• Gradient Zone 50%

Earth and Planetary Sciences

• Upper Mantle 100%
• Central Pacific 100%
• Surface Wave 66%
• Plate Motion 33%
• Olivine 33%
• Velocity Structure 33%
• Asthenosphere 33%
• Reflectance 33%
• Moisture Content 33%
• Hawaii 33%
• Travel Time 33%
• Low Velocity Zone 33%
• Mantle Discontinuity 33%
• Reverberation 33%
• Jordan 33%