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 …

This paper presents an interdisciplinary review of the correlation properties of random
wavefields. We expose several important theoretical results of various fields, ranging from …

A correlation-type reciprocity theorem is used to show that the elastodynamic Green's
function of any inhomogeneous medium (random or deterministic) can be retrieved from the …

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 …

It has been demonstrated experimentally and theoretically that an estimate of the Green's
function between two seismic stations can be obtained from the time‐derivative of the long …

Since it has already been demonstrated that point‐to‐point seismic propagation Green
Functions can be extracted from seismic noise, it should be possible to image Earth structure …

A definition of a diffuse field applicable to open heterogeneous systems is proposed. The
identity between the Green's function of the structure and the diffuse field's correlations is …

Green's functions (GFs) of surface wave propagation between two receivers can be
estimated from the cross-correlation of ambient noise under the assumption of diffuse …

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 …