Seismic interferometry (SI) is a technique used to estimate the Green's function (GF) between two receiver locations, as if there were a source at one of the receiver locations. However, in many applications, the requirements to recover the exact GF are not satisfied and SI yields a poor estimate of the GF. For these non-ideal cases, we improve the interferometric GFs, by applying singular value decomposition (SVD) to the cross-correlations before stacking. The SVD approach preserves energy that is stationary in the cross-correlations, which is the energy that contributes most to the GF recovery, and attenuates non-stationary energy, which leads to artefacts in the interferometric GF. We apply this method to construct virtual shot gathers (...
Under certain theoretical assumptions, the theory of seismic interferometry allows the construction ...
It is a well-established principle that cross-correlating seismic observations at different receiver...
Generating new seismic responses from existing recordings is generally referred to as seismic interf...
Seismic interferometry (SI) is a technique used to estimate the Green’s function (GF) between two re...
Seismic interferometry (SI) is a technique used to estimate the Green’s function (GF) between two re...
Seismic interferometry is a technique used to estimate the Green's function (GF) between two receive...
Seismic interferometry is a technique used to estimate the Green’s function (GF) between two receiv...
The conditions under which seismic interferometry (SI) leads to the exact Green's function (GF) are ...
The conditions under which seismic interferometry (SI) leads to the exact Green’s function (GF) are ...
In general, Green's functions obtained with seismic interferometry are only estimates of the true Gr...
Obtaining new seismic responses from existing recordings is generally referred to as seismic interfe...
Virtual Green's functions obtained by seismic interferometry (SI) can provide valuable reflectivity ...
Under certain theoretical assumptions, the theory of seismic interferometry allows the construction ...
It is a well-established principle that cross-correlating seismic observations at different receiver...
Generating new seismic responses from existing recordings is generally referred to as seismic interf...
Seismic interferometry (SI) is a technique used to estimate the Green’s function (GF) between two re...
Seismic interferometry (SI) is a technique used to estimate the Green’s function (GF) between two re...
Seismic interferometry is a technique used to estimate the Green's function (GF) between two receive...
Seismic interferometry is a technique used to estimate the Green’s function (GF) between two receiv...
The conditions under which seismic interferometry (SI) leads to the exact Green's function (GF) are ...
The conditions under which seismic interferometry (SI) leads to the exact Green’s function (GF) are ...
In general, Green's functions obtained with seismic interferometry are only estimates of the true Gr...
Obtaining new seismic responses from existing recordings is generally referred to as seismic interfe...
Virtual Green's functions obtained by seismic interferometry (SI) can provide valuable reflectivity ...
Under certain theoretical assumptions, the theory of seismic interferometry allows the construction ...
It is a well-established principle that cross-correlating seismic observations at different receiver...
Generating new seismic responses from existing recordings is generally referred to as seismic interf...