Abstract

AbstractBased on the finite element method and the interface point method of shortest path ray tracing, reverse‐time migration for anisotropic elastic waves is carried out. The migrated sections of synthetic data are clear and accurate. This demonstrates the reliability of the migration system. Furthermore, we migrate anisotropic wave field data with isotropic migration method to find out the effect of ignoring anisotropy. The results show that there are considerable errors on isotropically migrated sections where the positions of geological bodies are inconsistent with those in the real models.

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 call

Disclaimer: 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.