Converted-wave refraction statics is an algorithm that incorporates both compressional (P-) and shear (S-) wave refraction events to correct S-wave static errors in multi-component seismic data. Converted refraction (PPS) events are picked on an inline component shot record in the same way as first-breaks are picked on a normal vertical component record. These picks are then analysed using the reciprocal method to create a near-surface model from which S-wave receiver statics are derived. The derived PPS refraction statics have a similar short-wavelength character to the S-statics obtained via statistical analysis of converted-wave reflections. Based on standard P-wave practice, we believe that an optimal production approach will include co...
Dispersive Rayleigh waves, contained in conventional P-wave refraction records, can be used to deter...
Inconsistency between traveltime curves and theinterpreted model is inevitable in seismic refraction...
Statics correction can be computed by inverting the dispersion curves of surface waves. Here, we dir...
Converted-wave refraction statics is an algorithm that incorporates both P-wave and S-wave refractio...
P-wave reflection-statics solutions typically incorporate P-wave refraction data, derived from the f...
One of the most difficult steps in the PS processing sequence is estimation of the S-wave receiver s...
The estimation of good quality receiver statics solutions for converted wave data is often problemat...
A three-component 2D seismic line was acquired in the Blackfoot Field area in 1995 by the CREWES pro...
Ground roll and mud roll in seismic reflection data can be analysed to infer a near surface S-wave v...
Refraction statics corrections play an important role in many land surveys in producing correct subs...
In mineral exploration, increased interest towards deeper mineralizations makes seismic methods attr...
Refraction attributes can be readily computed from multi-fold seismic data using the standard algori...
International audienceThe joint study of pressure (P-) and shear (S-) wave velocities (Vp and Vs ), ...
Knott's calculations of reflected and refracted waves at rock-water, slate-granite, and granite...
The near-surface imaging and characterization of an onshore prospect field in the Niger Delta was su...
Dispersive Rayleigh waves, contained in conventional P-wave refraction records, can be used to deter...
Inconsistency between traveltime curves and theinterpreted model is inevitable in seismic refraction...
Statics correction can be computed by inverting the dispersion curves of surface waves. Here, we dir...
Converted-wave refraction statics is an algorithm that incorporates both P-wave and S-wave refractio...
P-wave reflection-statics solutions typically incorporate P-wave refraction data, derived from the f...
One of the most difficult steps in the PS processing sequence is estimation of the S-wave receiver s...
The estimation of good quality receiver statics solutions for converted wave data is often problemat...
A three-component 2D seismic line was acquired in the Blackfoot Field area in 1995 by the CREWES pro...
Ground roll and mud roll in seismic reflection data can be analysed to infer a near surface S-wave v...
Refraction statics corrections play an important role in many land surveys in producing correct subs...
In mineral exploration, increased interest towards deeper mineralizations makes seismic methods attr...
Refraction attributes can be readily computed from multi-fold seismic data using the standard algori...
International audienceThe joint study of pressure (P-) and shear (S-) wave velocities (Vp and Vs ), ...
Knott's calculations of reflected and refracted waves at rock-water, slate-granite, and granite...
The near-surface imaging and characterization of an onshore prospect field in the Niger Delta was su...
Dispersive Rayleigh waves, contained in conventional P-wave refraction records, can be used to deter...
Inconsistency between traveltime curves and theinterpreted model is inevitable in seismic refraction...
Statics correction can be computed by inverting the dispersion curves of surface waves. Here, we dir...