With the Marchenko method it is possible to retrieve Green's functions between virtual sources in the subsurface and receivers at the surface from reflection data at the surface and focusing functions. A macro model of the subsurface is needed to estimate the first arrival; the internal multiples are retrieved entirely from the reflection data. The retrieved Green's functions form the input for redatuming by multidimensional deconvolution (MDD). The redatumed reflection response is free of internal multiples related to the overburden. Alternatively, the redatumed response can be obtained by applying a second focusing function to the retrieved Green's functions. This process is called Marchenko redatuming by double focusing. It is more stabl...
In Marchenko imaging, wavefields are retrieved at specified focal points in the subsurface through a...
We have developed an adaptive double-focusing method that is specifically designed for the field-dat...
Traditionally, the Marchenko equation forms a basis for 1D inverse scattering problems. A 3D extensi...
With the Marchenko method it is possible to retrieve Green's functions between virtual sources in th...
Recent work on retrieving the Green’s function with the Marchenko equation shows how these functions...
Recently, a novel iterative scheme was proposed to retrieve Green's functions in an unknown medium f...
Recently, a novel iterative scheme was proposed to retrieve Green's functions in an unknown medium f...
Recent work on retrieving the Green’s function with the Marchenko equation shows how these functions...
Marchenko methods compute a focusing function for a receiver at the acquisition surface and a virtua...
Internal multiples can create severe artefacts in seismic imaging, especially when our zone of inter...
We have developed an adaptive double-focusing method that is specifically designed for the field-dat...
Recent work on retrieving the Green’s function with the Marchenko equation shows how these functions...
Recent work on retrieving the Green’s function with the Marchenko equation shows how these functions...
Marchenko redatuming is a novel scheme used to retrieve up- and downgoing Green's functions in an un...
In this paper, we focus on the field data application of source-receiver Marchenko redatuming. Conve...
In Marchenko imaging, wavefields are retrieved at specified focal points in the subsurface through a...
We have developed an adaptive double-focusing method that is specifically designed for the field-dat...
Traditionally, the Marchenko equation forms a basis for 1D inverse scattering problems. A 3D extensi...
With the Marchenko method it is possible to retrieve Green's functions between virtual sources in th...
Recent work on retrieving the Green’s function with the Marchenko equation shows how these functions...
Recently, a novel iterative scheme was proposed to retrieve Green's functions in an unknown medium f...
Recently, a novel iterative scheme was proposed to retrieve Green's functions in an unknown medium f...
Recent work on retrieving the Green’s function with the Marchenko equation shows how these functions...
Marchenko methods compute a focusing function for a receiver at the acquisition surface and a virtua...
Internal multiples can create severe artefacts in seismic imaging, especially when our zone of inter...
We have developed an adaptive double-focusing method that is specifically designed for the field-dat...
Recent work on retrieving the Green’s function with the Marchenko equation shows how these functions...
Recent work on retrieving the Green’s function with the Marchenko equation shows how these functions...
Marchenko redatuming is a novel scheme used to retrieve up- and downgoing Green's functions in an un...
In this paper, we focus on the field data application of source-receiver Marchenko redatuming. Conve...
In Marchenko imaging, wavefields are retrieved at specified focal points in the subsurface through a...
We have developed an adaptive double-focusing method that is specifically designed for the field-dat...
Traditionally, the Marchenko equation forms a basis for 1D inverse scattering problems. A 3D extensi...