Add to ORKGIn recent years, progress has been made in the field of virtual seismology. Using the novel data-driven Marchenko method, virtual sources and receivers can be created in the subsurface using only reflection data at the surface of the Earth and a background velocity model of the subsurface. Extensive studies have been performed on the application of the Marchenko method to 2D reflection data. This includes both synthetic reflection data and field reflection data. These studies have shown the potential improvements of the method for applications such as hydrocarbon imaging and wavefield monitoring. In the case of wavefield monitoring, a network of virtual receivers can be created in the subsurface to monitor the wavefield response of a subsur...
Marchenko redatuming estimates the full response (including internal multiples) from a virtual sourc...
Seismic interferometry and Marchenko focusing are alternative techniques to retrieve the Green’s fun...
Imagine placing a receiver at any location in the earth and recording the response at that location ...
In recent years, progress has been made in the field of virtual seismology. Using the novel data-dri...
The Marchenko method can be used to retrieve Green’s functions (including multiple scattering) betwe...
Recent developments in exploration seismology have enabled the creation of virtual sources and/or vi...
We aim to monitor and characterize signals in the subsurface by combining these passive signals with...
Traditionally, the Marchenko equation forms a basis for 1D inverse scattering problems. A 3D extensi...
Monitoring seismic wavefields caused by induced seismicity in the subsurface is a difficult process....
To enhance monitoring of the subsurface, virtual sources and receivers inside the subsurface can be ...
Traditionally, the Marchenko equation forms a basis for 1-D inverse scattering problems. A 3-D exten...
Forecasting induced seismicity responses for field data is difficult if no detailed model of the sub...
We create virtual sources and receivers in a 3-D subsurface using the previously derived single-side...
By solving the Marchenko equations, the Green’s function can be retrieved between a virtual receiver...
Marchenko redatuming can retrieve the impulse response to a subsurface virtual source from the singl...
Marchenko redatuming estimates the full response (including internal multiples) from a virtual sourc...
Seismic interferometry and Marchenko focusing are alternative techniques to retrieve the Green’s fun...
Imagine placing a receiver at any location in the earth and recording the response at that location ...
In recent years, progress has been made in the field of virtual seismology. Using the novel data-dri...
The Marchenko method can be used to retrieve Green’s functions (including multiple scattering) betwe...
Recent developments in exploration seismology have enabled the creation of virtual sources and/or vi...
We aim to monitor and characterize signals in the subsurface by combining these passive signals with...
Traditionally, the Marchenko equation forms a basis for 1D inverse scattering problems. A 3D extensi...
Monitoring seismic wavefields caused by induced seismicity in the subsurface is a difficult process....
To enhance monitoring of the subsurface, virtual sources and receivers inside the subsurface can be ...
Traditionally, the Marchenko equation forms a basis for 1-D inverse scattering problems. A 3-D exten...
Forecasting induced seismicity responses for field data is difficult if no detailed model of the sub...
We create virtual sources and receivers in a 3-D subsurface using the previously derived single-side...
By solving the Marchenko equations, the Green’s function can be retrieved between a virtual receiver...
Marchenko redatuming can retrieve the impulse response to a subsurface virtual source from the singl...
Marchenko redatuming estimates the full response (including internal multiples) from a virtual sourc...
Seismic interferometry and Marchenko focusing are alternative techniques to retrieve the Green’s fun...
Imagine placing a receiver at any location in the earth and recording the response at that location ...