Seismic interferometry involves the crosscorrelation of responses at different receivers to
obtain the Green's function between these receivers. For the simple situation of an impulsive …

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 …

Seismic interferometry is an exciting new field in geophysics utilizing multiple scattering
events to provide unprecedented views of the Earth's subsurface. This is the first book to …

A number of seismic methods exist to image the lithosphere below a collection of receivers,
using distant earthquakes. In the current practice, especially mode‐conversions in …

We analyze teleseismic P waves from four Mw≥ 6.5 earthquakes recorded by a petroleum
industry survey in Long Beach, California. The survey used a 2‐D array with up to 5200 …

In recent years, there has been an increase in the deployment of relatively dense arrays of
seismic stations. The availability of spatially densely sampled global and regional seismic …

Method for using seismic data from earthquakes to address the low frequency lacuna
problem in traditional hydrocarbon exploration methods. Seismometers with frequency …

We present fast and efficient plane-wave migration methods for densely sampled seismic
data in both the source and receiver domains. The methods are based on slant stacking …

Abstract<? A3B2 twb=. 3w?> In this study, we apply Gaussian-beam (GB) migration of
scattered teleseismic P waves to image the crust and upper mantle beneath Tibet using data …

Teleseismic receiver functions (RFs) are frequently used to determine depths of seismic
discontinuities in the crust and upper mantle. We developed an efficient reverse-time …