Abstract
Diffraction events containing in seismic data characterize small size geological objects. This information can supplement conventional reflection method. Typically diffracted energy is much weaker than reflection one. Therefore diffractions have to be extracted from the full wavefield before diffraction imaging. We present a method for reflection-diffraction events separation using the hybrid Radon transform.
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.
