The retrieval of the Green's functions between receiver pairs by multi-dimensional deconvolution can be extended to extract the impulse response between source pairs through source-receiver reciprocity. However in general, the procedure requires the separation of the outgoing and incoming wavefields at the sources, which reduces to the separation of the direct waves and the reflected waves in the absence of free-surface and inter-layer multiples. We show that in theory, for non-transient noise sources where the separation may not be obvious in the data domain, the separation can be achieved by time-windowing in an intermediate crosscorrelation step, which can be readily included in the MDD scheme. We illustrate the method with a synthe...
Acoustic signals recorded simultaneously in a reverberant environment can be described as sums of di...
Standard imaging techniques rely on the single scattering assumption. This requires that the recorde...
Seismic interferometry is an effective tool to retrieve surface waves between two receiver stations ...
The retrieval of the Green's functions between receiver pairs by multi-dimensional deconvolution can...
A major assumption for retrieving the earth’s reflection response with seismic interferometry by cro...
Virtual-source surface wave responses can be retrieved using the crosscorrelation (CC) of wavefields...
The methodology of surface?wave retrieval from ambient seismic noise by crosscorrelation relies on t...
Seismic interferometry (SI) is usually implemented by crosscorrelation (CC) to retrieve the impulse ...
Multidimensional deconvolution constitutes an essential operation in a variety of geophysical scenar...
International audienceRetrieving virtual source surface waves from ambient seismic noise by cross co...
With the Marchenko method it is possible to retrieve Green's functions between virtual sources in th...
Virtual-source surface-wave responses can be retrieved using the crosscorrelation of wavefields obse...
It has recently been shown that the response to a virtual source in the subsurface can be derived fr...
In physical acoustic laboratories, wave propagation experiments often suffer from unwanted reflectio...
It has recently been shown that the response to a virtual source in the subsurface can be derived fr...
Acoustic signals recorded simultaneously in a reverberant environment can be described as sums of di...
Standard imaging techniques rely on the single scattering assumption. This requires that the recorde...
Seismic interferometry is an effective tool to retrieve surface waves between two receiver stations ...
The retrieval of the Green's functions between receiver pairs by multi-dimensional deconvolution can...
A major assumption for retrieving the earth’s reflection response with seismic interferometry by cro...
Virtual-source surface wave responses can be retrieved using the crosscorrelation (CC) of wavefields...
The methodology of surface?wave retrieval from ambient seismic noise by crosscorrelation relies on t...
Seismic interferometry (SI) is usually implemented by crosscorrelation (CC) to retrieve the impulse ...
Multidimensional deconvolution constitutes an essential operation in a variety of geophysical scenar...
International audienceRetrieving virtual source surface waves from ambient seismic noise by cross co...
With the Marchenko method it is possible to retrieve Green's functions between virtual sources in th...
Virtual-source surface-wave responses can be retrieved using the crosscorrelation of wavefields obse...
It has recently been shown that the response to a virtual source in the subsurface can be derived fr...
In physical acoustic laboratories, wave propagation experiments often suffer from unwanted reflectio...
It has recently been shown that the response to a virtual source in the subsurface can be derived fr...
Acoustic signals recorded simultaneously in a reverberant environment can be described as sums of di...
Standard imaging techniques rely on the single scattering assumption. This requires that the recorde...
Seismic interferometry is an effective tool to retrieve surface waves between two receiver stations ...