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Keyword [Phase velocity]
Result: 21 - 40 | Page: 2 of 3
21. Study On The Measurement Of Disperse Phase Velocity Of Multiphase Flow
22. Research On GPS/INS Integrated Navigation Based On The Time Differenced Carrier Phase Velocity Estimation Approach
23. The Study Of Rayleigh Surface Wave Tomography In And Around The Northeastern Margin Of The Tibetan Plateau
24. Rayleigh Wave Phase Velocity Extracted. Time - Frequency Analysis
25. Ambient Noise Tomography In Dabie-Sulu Region And Locating The Microearthquakes Near The Wenchuan Fault Scientific Drilling
26. Rayleigh Wave Phase Velocities And Azimuthal Anisotropy Beneath Ordos Block And Its Surrounding Areas
27. Seismic Anisotropy In The Northeastern Margin Of Tibetan Plateau From Receiver Functions And Ambient Noise Surface-waves
28. Three-dimensional S Wave Velocity Structure And Radial Anisotropy In The Crust Beneath The Northeastern Tibetan Plateau From Ambient Noise Tomography
29. Three-dimensional S Wave Velocity Structure And Radial Anisotropy Of The Tarim Basin And Its Surrounding Regions
30. Shear Wave Structure In The Northeastern Tibetan Plateau From Two-plane-wave Method
31. Study Of QP Wave Reverse Time Migration(RTM)in Tilt Transversely Isotropic (TTI)Media
32. An Extension Of The PSE Approach And Its Applications To Nonlinear Evolution Of Multiple-Frequency Perturbations In Shear Layers
33. Study Of Ray Tracing Method In The VTI Medium
34. Multichannel Method Of Transient Rayleigh Wave Detecting In Consideration Of Arrival Time Difference Phase Between Channels
35. Crustal And Upper Mantle Velocity Structure Of The Tien Shan
36. Tomography And Azimuth Anisotropy In The East Qinling-Dabie Using Ambient Seismic Noise
37. Study On Inversion Methods Of Near-surface Parameters Based On Surface-wave Information
38. Extraction Of Higher Mode Dispersion Curve From Ambient Noise Based On Frequency-bessel Transform Method And Inversion Of 3D Shear Velocity Model In The US Continent
39. Surface Wave Tomography In The Northeast Margin Of The Qinghai-Tibet Plateau
40. Three-component Seismic-wave Gradiometry And Imagination
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