Two crustal low-velocity channels beneath SE Tibet revealed by joint inversion of Rayleigh wave dispersion and receiver functions

Keyphrases

• Low Velocity 100%
• Dispersion Law 100%
• Strike-slip Fault 100%
• Low-velocity Zone 100%
• Receiver Function 100%
• Joint Inversion 100%
• SE Tibet 100%
• Rayleigh Wave Dispersion 100%
• Extrusion 50%
• High-resolution 50%
• Dynamic Process 50%
• Large Earthquake 50%
• 3D Image 50%
• Resolution Limit 50%
• Tibet 50%
• Prominent Features 50%
• Duct Flow 50%
• Shearing Motion 50%
• Rigid Block 50%
• Continuous Deformation 50%
• Eastern Himalayan Syntaxis 50%
• Eastward Expansion 50%
• Geodynamic Model 50%
• Lithospheric Structure 50%
• Seismic Array 50%
• Cenozoic 50%
• Lithospheric Deformation 50%
• Crustal Materials 50%
• Lower Crustal Flow 50%
• Eastern Tibet 50%

Earth and Planetary Sciences

• Tibet 100%
• Wave Dispersion 100%
• Rayleigh Wave 100%
• Strike-Slip Fault 50%
• Low Velocity Zone 50%
• Himalayas 25%
• Geodynamics 25%
• Lithospheric Structure 25%