Ground roll and mud roll in seismic reflection data can be analysed to infer a near surface S-wave velocity model from which converted-wave static correction can be computed. A workflow that exploits processing tools available in industrial processing codes has been implemented to extract dispersion curves and related uncertainties along a seismic line. The dispersion curves are then inverted with a laterally constrained inversion algorithm based on an initial model previously determined through a Monte Carlo inversion. The final S-wave velocity models are finally used for static computation. The application of the method to synthetic data supplied static correction values with error lower than 5%
The shear (S)-wave velocity of near-surface materials (such as soil, rocks, and pavement) and its ef...
Surfacewave methods consist of the extraction and inversion of the Rayleigh wave phase-velocity disp...
Surface wave methods consist of the extraction and inversion of the Rayleigh wave phase-velocity dis...
Ground roll and mud roll in seismic reflection data can be analysed to infer a near surface S-wave v...
• Statics correction can be computed by inverting the dispersion curves of surface waves (groundroll...
Ground roll of seismic data is mainly composed of surface waves. Surface wave analysis can be used t...
Seismic reflection data contain surface waves that can be processed and interpreted to supply shear-...
Near surface velocity models are needed for static corrections applied to seismic reflection data. S...
Surface wave analysis is usually applied as a 1D tool to estimate VS profiles. Here we evaluate the ...
Statics correction can be computed by inverting the dispersion curves of surface waves. Here, we dir...
In mineral exploration, increased interest towards deeper mineralizations makes seismic methods attr...
The task of this work is the evaluation of the possibility to identify lateral variation through Sur...
In some areas, the estimation of static corrections for land seismic data is a critical step of the ...
A new strategy for processing and inverting surface waves retrieved by seismic reflection ground rol...
Surface wave analysis performed on data acquired on purpose or extracted from seismic gathers acquir...
The shear (S)-wave velocity of near-surface materials (such as soil, rocks, and pavement) and its ef...
Surfacewave methods consist of the extraction and inversion of the Rayleigh wave phase-velocity disp...
Surface wave methods consist of the extraction and inversion of the Rayleigh wave phase-velocity dis...
Ground roll and mud roll in seismic reflection data can be analysed to infer a near surface S-wave v...
• Statics correction can be computed by inverting the dispersion curves of surface waves (groundroll...
Ground roll of seismic data is mainly composed of surface waves. Surface wave analysis can be used t...
Seismic reflection data contain surface waves that can be processed and interpreted to supply shear-...
Near surface velocity models are needed for static corrections applied to seismic reflection data. S...
Surface wave analysis is usually applied as a 1D tool to estimate VS profiles. Here we evaluate the ...
Statics correction can be computed by inverting the dispersion curves of surface waves. Here, we dir...
In mineral exploration, increased interest towards deeper mineralizations makes seismic methods attr...
The task of this work is the evaluation of the possibility to identify lateral variation through Sur...
In some areas, the estimation of static corrections for land seismic data is a critical step of the ...
A new strategy for processing and inverting surface waves retrieved by seismic reflection ground rol...
Surface wave analysis performed on data acquired on purpose or extracted from seismic gathers acquir...
The shear (S)-wave velocity of near-surface materials (such as soil, rocks, and pavement) and its ef...
Surfacewave methods consist of the extraction and inversion of the Rayleigh wave phase-velocity disp...
Surface wave methods consist of the extraction and inversion of the Rayleigh wave phase-velocity dis...