In seismic imaging the aim is to obtain an image of the subsurface using reflection data. The reflection data are generated using sound waves and the sources and receivers are placed at the surface. The target zone, for example an oil or gas reservoir, lies relatively deep in the subsurface below several layers. The area above the target zone is called the overburden. This overburden will have an imprint on the image. Wavefield redatuming is an approach that removes the imprint of the overburden on the image by creating so-called virtual sources and receivers above the target zone. The virtual sources are obtained by determining the impulse response, or Green's function, in the subsurface. The impulse response is obtained by deconvolving al...
Seismic interferometry is a method to retrieve Green’s functions for sources (or receivers) where th...
Abstract We apply a deconvolution approach to the problem of determining the input motion at the bas...
We apply a deconvolution approach to the problem of determining the input motion at the base of an i...
In seismic imaging the aim is to obtain an image of the subsurface using reflection data. The reflec...
Multidimensional deconvolution constitutes an essential operation in a variety of geophysical scenar...
Seismic reflection data can be redatumed to a specified boundary in the subsurface by solving an inv...
In this work, the inverse problem of exploration geophysics is solved through two techniques based o...
<p>Seismic reflection data can be redatumed to a specified boundary in the subsurface by solving an ...
Seismic imaging of subsurface structures situated deep beneath complex overburden structures, such a...
Seismic imaging of subsurface structures situated deep beneath complex overburden structures, such a...
The Marchenko redatuming approach reconstructs wavefields at depth that contain not only primary ref...
Reweighting strategies have been widely used to diminish the influence.of outliers in inverse proble...
The Marchenko redatuming approach reconstructs wavefields at depth that contain not only primary ref...
Assuming that transmission responses are known between the surface and a particular depth level in t...
Assuming that transmission responses are known between the surface and a particular depth level in t...
Seismic interferometry is a method to retrieve Green’s functions for sources (or receivers) where th...
Abstract We apply a deconvolution approach to the problem of determining the input motion at the bas...
We apply a deconvolution approach to the problem of determining the input motion at the base of an i...
In seismic imaging the aim is to obtain an image of the subsurface using reflection data. The reflec...
Multidimensional deconvolution constitutes an essential operation in a variety of geophysical scenar...
Seismic reflection data can be redatumed to a specified boundary in the subsurface by solving an inv...
In this work, the inverse problem of exploration geophysics is solved through two techniques based o...
<p>Seismic reflection data can be redatumed to a specified boundary in the subsurface by solving an ...
Seismic imaging of subsurface structures situated deep beneath complex overburden structures, such a...
Seismic imaging of subsurface structures situated deep beneath complex overburden structures, such a...
The Marchenko redatuming approach reconstructs wavefields at depth that contain not only primary ref...
Reweighting strategies have been widely used to diminish the influence.of outliers in inverse proble...
The Marchenko redatuming approach reconstructs wavefields at depth that contain not only primary ref...
Assuming that transmission responses are known between the surface and a particular depth level in t...
Assuming that transmission responses are known between the surface and a particular depth level in t...
Seismic interferometry is a method to retrieve Green’s functions for sources (or receivers) where th...
Abstract We apply a deconvolution approach to the problem of determining the input motion at the bas...
We apply a deconvolution approach to the problem of determining the input motion at the base of an i...