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Databases of surface wave dispersion     seismic tomography  upper mantle  lateral resolution  azimuthal anisotropy       font style='font-size:12px;'> 2015/9/10
Observations of seismic surface waves provide the most important constraint on the elastic properties of the Earths lithosphere and upper mantle. Two databases of fundamental mode surface wave disper...
Through inversion of fundamental mode group velocities of Love and Rayleigh waves, we study the crustal and subcrustal structure across the central Deccan Volcanic Province (DVP), which is one of the ...
Southern Peru is located in the northern Central Andes, which is the highest plateau along an active subduction zone. In this region, the Nazca slab changes from normal to flat subduction, with the as...
Modulation of short surface ripples by long surface or internal waves by a cascade mechanism is considered. At the first stage, the orbital velocity of the long wave (LW) adiabatically modulates an in...
Surface Wave Dispersion for some Eurasian Paths.I.Rayleigh Waves from Kamchatka and Japan to Finland.
Surface Wave Dispersion for some Eurasian Paths. II. Love Waves     Surface  Dispersion  Eurasian Paths       font style='font-size:12px;'> 2009/6/19
Surface Wave Dispersion for some Eurasian Paths. II. Love Waves.
A Procedure for Determination of the Surface Wave Group Velocity     Procedure  Determination  Surface Wave Group  Velocity       font style='font-size:12px;'> 2009/6/18
A Procedure for Determination of the Surface Wave Group Velocity.
Estimates of the Inaccuracy of Surface-Wave Magnitude due to Errors of Seismogram Evaluation.
Inversion of multi-mode surface-wave phase velocity for shallow engineering site investigation has received much attention in recent years. A sensitivity analysis and inversion of both synthetic and f...
Partial derivatives of surface wave phase velocity with respect to layer parameters, such as P-wave velocity and S-wave velocity, are the Jacobians of the linearlized least-squares scheme for the inve...
Shear wave velocity of the crust below central Mexico is estimated using surface wave dispersion measurements from regional earthquakes recorded on a dense, 500 km long linear seismic network. Vertica...

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