Detecting small-size objects is a primary challenge at archaeological sites due to the high degree of heterogeneity present in the near surface. Although high-resolution reflection seismic imaging often delivers the target resolution of the subsurface in different near-surface settings, the standard processing for obtaining an image of the subsurface is not suitable to map local diffractors. This happens because shallow seismic-reflection data are often dominated by strong surface waves that might cover weaker diffractions and because traditional common-midpoint moveout corrections are only optimal for reflection events. We propose an approach for imaging subsurface objects using masked diffractions. These masked diffractions are first reve...
Virtual-source surface wave responses can be retrieved using the crosscorrelation (CC) of wavefields...
Despite its unique properties the diffracted seismic wavefield is still rarely exploited in common p...
Diffraction imaging can help better understand small-scale geological structures. Due to their often...
At different places in the world, the local climate conditions have helped the preservation of archa...
Traditional least-squares full-waveform inversion (FWI) suffers from severe local minima problems in...
High-resolution reflection seismics is a powerful tool that can provide the required resolution for ...
One of the problems encountered in a variety of near-surface investigations is detecting and mapping...
Difficulties in detecting and characterising shallow objects close the surface with seismic shear wa...
One of the main objectives of seismic interpretation is the identification and positioning of struct...
Shallow buried heterogeneities act as diffractors to an incoming surface wave. Experimental and nume...
textSeismic waves can either be reflected or diffracted by subsurface objects depending on the objec...
This paper concerns the detection of shallow (of the order 1 m) buried objects using seismic excitat...
In mineral exploration, new methods to improve the delineation of ore deposits at depth are in deman...
We present a new approach to the problem of detecting point diffractors from active source surface ...
Virtual-source surface-wave responses can be retrieved using the crosscorrelation of wavefields obse...
Virtual-source surface wave responses can be retrieved using the crosscorrelation (CC) of wavefields...
Despite its unique properties the diffracted seismic wavefield is still rarely exploited in common p...
Diffraction imaging can help better understand small-scale geological structures. Due to their often...
At different places in the world, the local climate conditions have helped the preservation of archa...
Traditional least-squares full-waveform inversion (FWI) suffers from severe local minima problems in...
High-resolution reflection seismics is a powerful tool that can provide the required resolution for ...
One of the problems encountered in a variety of near-surface investigations is detecting and mapping...
Difficulties in detecting and characterising shallow objects close the surface with seismic shear wa...
One of the main objectives of seismic interpretation is the identification and positioning of struct...
Shallow buried heterogeneities act as diffractors to an incoming surface wave. Experimental and nume...
textSeismic waves can either be reflected or diffracted by subsurface objects depending on the objec...
This paper concerns the detection of shallow (of the order 1 m) buried objects using seismic excitat...
In mineral exploration, new methods to improve the delineation of ore deposits at depth are in deman...
We present a new approach to the problem of detecting point diffractors from active source surface ...
Virtual-source surface-wave responses can be retrieved using the crosscorrelation of wavefields obse...
Virtual-source surface wave responses can be retrieved using the crosscorrelation (CC) of wavefields...
Despite its unique properties the diffracted seismic wavefield is still rarely exploited in common p...
Diffraction imaging can help better understand small-scale geological structures. Due to their often...