Near-surface wavefield perturbations can be very complex and completely mask the target reflections. Despite this complexity, conventional methods rely on parameterizations characterized by simple time and amplitude anomalies to compensate for these perturbations. Determining and compensating for time shifts is generally referred to as (residual) static corrections, whereas surface-consistent deconvolution techniques deal with amplitude anomalies. We present an approach that uses the full waveform to parameterize near-surface perturbations. Therefore, we refer to this method as waveform statics. Important differences from conventional static corrections are that this approach allows time shifts to vary with frequency and takes amplitude var...
We develop an automatic workflow for enhancing surface wave signals in ambient noise cross correlati...
Surface-consistent residual static correction is applied to land data on a routine basis. However, i...
One of the most difficult steps in the PS processing sequence is estimation of the S-wave receiver s...
Very high-frequency marine multichannel seismic reflection data generated by small-volume air- or wa...
• Statics correction can be computed by inverting the dispersion curves of surface waves (groundroll...
In mineral exploration, increased interest towards deeper mineralizations makes seismic methods attr...
Statics correction can be computed by inverting the dispersion curves of surface waves. Here, we dir...
When upcoming body waves travel through a heterogeneous near-surface region, the continuity of the w...
Shallow seismic reflection surveys can assist in determination of velocity and/or thickness variatio...
A seismic survey is conducted to acquire data which can be used to image the earth's discontuinities...
Seismic reflection methods are widely used for the detection of hydrocarbons in subsurface structure...
Seismic reflection methods are widely used for the detection of hydrocarbons in subsurface structure...
With a rapid increase in computational resources two dimensional full-waveform inversion is evolving...
Ground roll and mud roll in seismic reflection data can be analysed to infer a near surface S-wave v...
Correcting seismic data for the effects of the earth’s near-surface remains a significant problem in...
We develop an automatic workflow for enhancing surface wave signals in ambient noise cross correlati...
Surface-consistent residual static correction is applied to land data on a routine basis. However, i...
One of the most difficult steps in the PS processing sequence is estimation of the S-wave receiver s...
Very high-frequency marine multichannel seismic reflection data generated by small-volume air- or wa...
• Statics correction can be computed by inverting the dispersion curves of surface waves (groundroll...
In mineral exploration, increased interest towards deeper mineralizations makes seismic methods attr...
Statics correction can be computed by inverting the dispersion curves of surface waves. Here, we dir...
When upcoming body waves travel through a heterogeneous near-surface region, the continuity of the w...
Shallow seismic reflection surveys can assist in determination of velocity and/or thickness variatio...
A seismic survey is conducted to acquire data which can be used to image the earth's discontuinities...
Seismic reflection methods are widely used for the detection of hydrocarbons in subsurface structure...
Seismic reflection methods are widely used for the detection of hydrocarbons in subsurface structure...
With a rapid increase in computational resources two dimensional full-waveform inversion is evolving...
Ground roll and mud roll in seismic reflection data can be analysed to infer a near surface S-wave v...
Correcting seismic data for the effects of the earth’s near-surface remains a significant problem in...
We develop an automatic workflow for enhancing surface wave signals in ambient noise cross correlati...
Surface-consistent residual static correction is applied to land data on a routine basis. However, i...
One of the most difficult steps in the PS processing sequence is estimation of the S-wave receiver s...