The Marchenko redatuming approach reconstructs wavefields at depth that contain not only primary reflections, but also multiply-scattered waves. While such fields in principle contain additional subsurface information, conventional imaging approaches cannot tap into the information encoded in internal multiples in a trivial manner. We discuss a new approach that uses the full information contained in Marchenko-redatumed fields, whose output are local reflection and transmission responses that fully enclose a target volume at depth, without contributions from over- or under-burden structures. To obtain the Target-Enclosing Extended Images (TEEIs) we solve a multi-dimensional deconvolution (MDD) problem that can be severely ill-posed, so we o...
Standard imaging techniques rely on the single scattering assumption. This requires that the recorde...
Complex overburdens can severely distort transmitted wavefields, posing serious challenges for seism...
Traditionally, the Marchenko equation forms a basis for 1D inverse scattering problems. A 3D extensi...
The Marchenko redatuming approach reconstructs wavefields at depth that contain not only primary ref...
Marchenko redatuming estimates the full response (including internal multiples) from a virtual sourc...
Seismic reflection data can be redatumed to a specified boundary in the subsurface by solving an inv...
<p>Seismic reflection data can be redatumed to a specified boundary in the subsurface by solving an ...
In this paper, we focus on the field data application of source-receiver Marchenko redatuming. Conve...
With the Marchenko method it is possible to retrieve Green's functions between virtual sources in th...
Imagine placing a receiver at any location in the earth and recording the response at that location ...
With the Marchenko method it is possible to retrieve Green's functions between virtual sources in th...
In Marchenko imaging, wavefields are retrieved at specified focal points in the subsurface through a...
Seismic imaging of subsurface structures situated deep beneath complex overburden structures, such a...
Imagine placing a receiver at any location in the earth and recording the response at that location ...
Seismic imaging of subsurface structures situated deep beneath complex overburden structures, such a...
Standard imaging techniques rely on the single scattering assumption. This requires that the recorde...
Complex overburdens can severely distort transmitted wavefields, posing serious challenges for seism...
Traditionally, the Marchenko equation forms a basis for 1D inverse scattering problems. A 3D extensi...
The Marchenko redatuming approach reconstructs wavefields at depth that contain not only primary ref...
Marchenko redatuming estimates the full response (including internal multiples) from a virtual sourc...
Seismic reflection data can be redatumed to a specified boundary in the subsurface by solving an inv...
<p>Seismic reflection data can be redatumed to a specified boundary in the subsurface by solving an ...
In this paper, we focus on the field data application of source-receiver Marchenko redatuming. Conve...
With the Marchenko method it is possible to retrieve Green's functions between virtual sources in th...
Imagine placing a receiver at any location in the earth and recording the response at that location ...
With the Marchenko method it is possible to retrieve Green's functions between virtual sources in th...
In Marchenko imaging, wavefields are retrieved at specified focal points in the subsurface through a...
Seismic imaging of subsurface structures situated deep beneath complex overburden structures, such a...
Imagine placing a receiver at any location in the earth and recording the response at that location ...
Seismic imaging of subsurface structures situated deep beneath complex overburden structures, such a...
Standard imaging techniques rely on the single scattering assumption. This requires that the recorde...
Complex overburdens can severely distort transmitted wavefields, posing serious challenges for seism...
Traditionally, the Marchenko equation forms a basis for 1D inverse scattering problems. A 3D extensi...