Seismic interferometry, also referred to as Green's function retrieval by crosscorrelation, is a technique with many applications, such as for the reconstruction of surface seismic, VSP, to Ocean-Bottom data using active or passive data. Due to the impurity of the Green's function retrieved in the presence of one-sided illumination or intrinsic losses, multidimensional deconvolution emerged as an alternative. Multidivisional deconvolution addresses the limitations by deconvolving the point-spread function from the crosscorrelation result, which removes the source signature, surface related multiples and takes intrinsic losses into account. The similarity of the inverse problems of interferometry by multidimensional deconvolution applied to ...
Seismic reflection imaging is a popular method to image, characterize and monitor the Earth's subsur...
Crosswell reflection method is a high-resolution seismic imaging method that uses recordings between...
In seismic interferometry the response to a virtual source is created from responses to sequential t...
Seismic interferometry is a technique by which the Green’s function (or impulse response) between tw...
Seismic interferometry by crosscorrelation has found wide application over the last decade. With whi...
Our objective is to complement lithospheric seismic tomography with an interferometric method to ret...
We introduce seismic interferometry of passive data by multidimensional deconvolution (MDD) as an al...
Seismic interferometry (SI) allows retrieval of virtual-source responses at positions of receivers, ...
Seismic interferometry (SI) allows retrieval of virtual-source responses at positions of receivers, ...
Virtual Green's functions obtained by seismic interferometry (SI) can provide valuable reflectivity ...
Obtaining new seismic responses from existing recordings is generally referred to as seismic interfe...
Virtual-source surface wave responses can be retrieved using the crosscorrelation (CC) of wavefields...
A major assumption for retrieving the earth’s reflection response with seismic interferometry by cro...
Seismic interferometry by multi-dimensional deconvolution (MDD) has recently been proposed as an alt...
Retrieving virtual source surface waves from ambient seismic noise by cross correlation assumes, amo...
Seismic reflection imaging is a popular method to image, characterize and monitor the Earth's subsur...
Crosswell reflection method is a high-resolution seismic imaging method that uses recordings between...
In seismic interferometry the response to a virtual source is created from responses to sequential t...
Seismic interferometry is a technique by which the Green’s function (or impulse response) between tw...
Seismic interferometry by crosscorrelation has found wide application over the last decade. With whi...
Our objective is to complement lithospheric seismic tomography with an interferometric method to ret...
We introduce seismic interferometry of passive data by multidimensional deconvolution (MDD) as an al...
Seismic interferometry (SI) allows retrieval of virtual-source responses at positions of receivers, ...
Seismic interferometry (SI) allows retrieval of virtual-source responses at positions of receivers, ...
Virtual Green's functions obtained by seismic interferometry (SI) can provide valuable reflectivity ...
Obtaining new seismic responses from existing recordings is generally referred to as seismic interfe...
Virtual-source surface wave responses can be retrieved using the crosscorrelation (CC) of wavefields...
A major assumption for retrieving the earth’s reflection response with seismic interferometry by cro...
Seismic interferometry by multi-dimensional deconvolution (MDD) has recently been proposed as an alt...
Retrieving virtual source surface waves from ambient seismic noise by cross correlation assumes, amo...
Seismic reflection imaging is a popular method to image, characterize and monitor the Earth's subsur...
Crosswell reflection method is a high-resolution seismic imaging method that uses recordings between...
In seismic interferometry the response to a virtual source is created from responses to sequential t...