We present a review of the recent development in finite-difference time-domain modeling of
seismic wave propagation and earthquake motion. The finite-difference method is a robust …

The cross correlation of ambient signal allows seismologists to collect data even in the
absence of seismic events.“Seismic interferometry” shows that the cross correlation of …

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 …

T urning noise into useful data—every geophysicist's dream? And now it seems possible.
The field of seismic interferometry has at its foundation a shift in the way we think about the …

Seismic interferometry, also known as Green's function retrieval by crosscorrelation, has a
wide range of applications, ranging from surface-wave tomography using ambient noise, to …

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 …

In realistic materials, multiple scattering takes place and average field intensities or energy
densities follow diffusive processes. Multiple P to S energy conversions by the random …

Seismic interferometry is a technique for estimating the Green's function that accounts for
wave propagation between receivers by correlating the waves recorded at these receivers …

Seismic surface wave tomography is a tried and tested method to reveal the subsurface
structure of the Earth. However, the conventional 2-step scheme of inverting first for 2-D …

Seismic interferometry can be used to estimate interreceiver surface wave signals by cross-
correlation of signals recorded at each receiver. The quality of the estimated surface waves …