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Keyword [receiver function]
Result: 21 - 40 | Page: 2 of 6
21. Crustal Seismic In The Northeast Of China
22. Application Of Receiver Function Method For Crust And Upper Mantle Structure Beneath Sichuan And Yunnan Region
23. The Structure Of The Crust And Upper Mantle In Eastern South China From Teleseismic Receiver Function
24. Numerical Modeling And Migration Of Receiver Function
25. The Study Of The Crustal And Upper Mantle Structure In Northeast China From Teleseismic Receiver Function
26. Shear Wave Velocity Structures In The Northeastern Tibetan Plateau By Joint Inversion Of Receiver Function And Rayleigh Waves
27. S Wave Velocity Structure Of The Crust Of The North China Basin And Its Adjacent Area Obtained With Linear Inversion Of The Receiver Function
28. The P-receiver Function And Velocity Structure Tomography Of Upper Crust In Jiangsu And Anhui Province
29. 1-D S-wave Velocity Of Northeast China Computed By Nonlinear Receiver Function Inverse
30. Crustal And Uppermost Mantle Velocity Structure Beneath The Mid-lower Yangtze Metallogenic Belt And Its Adjacent Regions From Joint Inversion Of Receiver Function And Surface Wave
31. Crustal And Upper Mantle 3-D Shear Wave Velocity Structures Beneath Xinjiang Tarim Basin And Its Adjacent Regions
32. Seismic Phase Characteristics Based Imaging Methods And Their Applications
33. Receiver Function And Surface Wave Tomography Studies Of Southwest China
34. Tomographic Study On The Crustal And Upper Mantle Structure Beneath The South-North Seismic Zone
35. Structure Of Crust-mantle Beneath Qiangtang Terrane And Interaction Model
36. Seismic Anisotropy In The Northeastern Margin Of Tibetan Plateau From Receiver Functions And Ambient Noise Surface-waves
37. A Geodynamic Study For The Deep Structure And Plateau Growth In Northeastern Tibet
38. Inversion Of Crustal 3-d Structure And Seismic Activity Of Yishu Fault Zone And Adjacent Areas
39. The Structure Of The Crust And Mantle Beneath Southeast Tibetan Plateau From Receiver Function And Surface Wave Dispersion
40. The Crustal Anisotropy And S Wave Velocity Structures Beneath The Southeastern Margin Of Tibetan Plateau
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