To enhance monitoring of the subsurface, virtual sources and receivers inside the subsurface can be created from seismic reflection data at the surface of the Earth using the Marchenko method. The response between these virtual sources and receivers can be obtained through the use of homogeneous Green's function retrieval. A homogeneous Green's function is a superposition of a Green's function and its time reversal. The main aim of this paper is to obtain accurate homogeneous Green's functions from field data. Classical homogeneous Green's function retrieval requires an unrealistic enclosing recording surface; however, by using a recently proposed single-sided retrieval scheme, this requirement can be avoided. We first demonstrate the princ...
Forecasting induced seismicity responses for field data is difficult if no detailed model of the sub...
The Marchenko method can be used to retrieve Green’s functions (including multiple scattering) betwe...
The methodology of Green’s function retrieval by cross-correlation has led to many interesting appli...
To enhance monitoring of the subsurface, virtual sources and receivers inside the subsurface can be ...
In recent work we showed with heuristic arguments that the Green’s response to a virtual source in t...
We create virtual sources and receivers in a 3-D subsurface using the previously derived single-side...
summary Recently we introduced a new approach for retrieving the Green’s response to a virtual sourc...
In recent work we showed with heuristic arguments that the Green's response to a virtual source in t...
We aim to monitor and characterize signals in the subsurface by combining these passive signals with...
Monitoring seismic wavefields caused by induced seismicity in the subsurface is a difficult process....
In wave theory, a Green’s function is defined as the response of a medium to an impulsive point sour...
Recent research showed that the Marchenko equation can be used to construct the Green’s function for...
In recent years, progress has been made in the field of virtual seismology. Using the novel data-dri...
By solving the Marchenko equations, the Green’s function can be retrieved between a virtual receiver...
Seismic interferometry and Marchenko focusing are alternative techniques to retrieve the Green’s fun...
Forecasting induced seismicity responses for field data is difficult if no detailed model of the sub...
The Marchenko method can be used to retrieve Green’s functions (including multiple scattering) betwe...
The methodology of Green’s function retrieval by cross-correlation has led to many interesting appli...
To enhance monitoring of the subsurface, virtual sources and receivers inside the subsurface can be ...
In recent work we showed with heuristic arguments that the Green’s response to a virtual source in t...
We create virtual sources and receivers in a 3-D subsurface using the previously derived single-side...
summary Recently we introduced a new approach for retrieving the Green’s response to a virtual sourc...
In recent work we showed with heuristic arguments that the Green's response to a virtual source in t...
We aim to monitor and characterize signals in the subsurface by combining these passive signals with...
Monitoring seismic wavefields caused by induced seismicity in the subsurface is a difficult process....
In wave theory, a Green’s function is defined as the response of a medium to an impulsive point sour...
Recent research showed that the Marchenko equation can be used to construct the Green’s function for...
In recent years, progress has been made in the field of virtual seismology. Using the novel data-dri...
By solving the Marchenko equations, the Green’s function can be retrieved between a virtual receiver...
Seismic interferometry and Marchenko focusing are alternative techniques to retrieve the Green’s fun...
Forecasting induced seismicity responses for field data is difficult if no detailed model of the sub...
The Marchenko method can be used to retrieve Green’s functions (including multiple scattering) betwe...
The methodology of Green’s function retrieval by cross-correlation has led to many interesting appli...