Crustal structure beneath the hi-climb seismic array in the central-western tibetan plateau from the improved h-κ-c method

Keyphrases

• Partial Melt 100%
• Two-region 100%
• Crustal Thickness 100%
• S-velocity 100%
• Seismic Array 100%
• Qiangtang Block 100%
• Hi-CLIMB 100%
• Western Tibetan Plateau 100%
• Crustal Structure 100%
• Ratio Values 50%
• Time of Arrival 50%
• Flow Model 50%
• Reduced Error 50%
• Tibet 50%
• Himalaya 50%
• Tibetan Plateau 50%
• Harmonic Correction 50%
• Azimuthal Variation 50%
• Receiver Function 50%
• Yarlung Zangbo Suture Zone 50%
• Lhasa Block 50%
• Crustal Flow 50%
• Mechanically Strong 50%
• Dipping Interface 50%
• Crustal Anisotropy 50%
• Northern Himalaya 50%

Earth and Planetary Sciences

• Tibetan Plateau 100%
• Crustal Structure 100%
• Stacking 66%
• Himalayas 66%
• Crustal Thickness 66%
• Harmonics 33%
• Arrival Time 33%
• Lower Crust 33%