Abstract
We present a new method called the pyramid transform for seismic trace interpolation. The pyramid transform is a resampling of data in the f-x-y domain that gives rise to frequency dependent spatial grids with a relationship that the sampling interval is inversely proportional to the frequency. Such transformation is reversible for wavefields. Using prediction filter, we demonstrate that seismic trace interpolation in the pyramid domain is more robust in the presence of noise and conflicting dips than interpolation in the conventional f-x-y domain.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
