Abstract
It was originally shown by Ziolkowski et al. (1982) that the far-field signature of an air gun array could be computed from near-field measurements. This is useful because of the practical difficulties in measuring the farfield radiation pattern of marine seismic source arrays, especially on the continental shelf due to the shallow depth of water; where as near-field measurements can always be made, thus providing a shot-by-shot estimate of the far-field signature as the survey proceeds.
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.
