1887

Abstract

Conventional marine seismic data is affected by the interference from ghosts in both source and receiver sides. The natural diversity provided by propagation directions, depths variations and imperfect reflections at the sea surface means the notches are not as deep as they often appear after stack. Since the apparent time delay between the main signal and its ghost is angle dependent, a deterministic de-ghosting process in the tau-p domain can reduce the effect of ghosts and retrieve the original wavelet spectrum. The amplitude and phase discrepancies around the notch frequencies caused by the variations in depths and effective refection coefficients can be reduced by using a stochastic search for the optimum set of de-ghosting parameters. A deconvolution process stabilized by averaging over a large number of traces in common–slowness panels may be used to address the remaining spectral defects.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.20130093
2013-06-10
2024-04-19
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20130093
Loading
This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error