With the emergence of portable broadband seismic instrumentation, availability of digital
networks with wide dynamic range, and development of new powerful analysis techniques …

The term seismic interferometry refers to the principle of generating new seismic responses
by crosscorrelating seismic observations at different receiver locations. The first version of …

We apply the cross-coherence method to the seismic interferometry of traffic noise, which
originates from roads and railways, to retrieve both body waves and surface-waves. Our …

Surface-wave dispersion analysis is widely used in geophysics to infer a shear wave
velocity model of the subsoil for a wide variety of applications. A shear-wave velocity model …

The coda of earthquake motions and microtremors are sometimes referred to as diffuse-
wave fields. They are generated by the multiple scattering due to the complexity of the Earth …

In the 1990s, the method of time-reversed acoustics was developed. This method exploits
the fact that the acoustic wave equation for a lossless medium is invariant for time reversal …

Cross correlation of the ambient seismic field is now routinely used to measure seismic
wave travel times; however, relatively little attention has been paid to other information that …

It has previously been shown that the Green's function between two receivers can be
retrieved by cross-correlating time series of noise recorded at the two receivers. This …

The recently developed frequency‐Bessel transformation (F‐J) method is effective to extract
multimode surface wave dispersion curves from ambient noise cross‐correlation functions …

To study the applicability of the passive seismic interferometry technique to near-surface
geological studies, seismic noise recordings from a small scale 2-D array of seismic stations …