High-frequency surface-wave methods have been widely used for surveying near-surface
shear-wave velocities. A key step in high-frequency surface-wave methods is to acquire …

Passive surface wave methods are non-invasive, low-cost, and robust approaches to image
near-surface shear-wave velocity (Vs) structure using passive seismic sources. A clean and …

It has been widely recognized that the cross‐correlation function of ambient seismic noise
data recorded at two stations approximates to the part of Greens function between two …

We present the theory for wave-equation inversion of dispersion curves, where the misfit
function is the sum of the squared differences between the wavenumbers along the …

Rayleigh wave exploration is a powerful method for estimating near-surface shear-wave (S-
wave) velocities, providing valuable insights into the stiffness properties of subsurface …

Passive surface wave methods have gained much attention from geophysical and civil
engineering communities because of the limited application of traditional seismic surveys in …

Linear arrays are usually deployed for passive surface-wave investigations because of their
high efficiency and convenience. In populated urban areas, it is almost impossible to set up …

ABSTRACT Frequency–Bessel (F‐J) transform method can obtain higher‐mode Rayleigh
dispersion curves by multistation ambient noise data superposition. Because the dispersion …

Exploration of geothermal resources has become one of the major drivers for urbanization
and economic transformation in southeast China, and it calls for temporal and spatial …

Near‐surface seismic structure, particularly the shear wave velocity (Vs), can strongly affect
local site response, and should be accurately estimated for ground motion prediction during …