Full text loading...
-
Elastic Reverse Time Migration with Non-Staggered Grid Finite Difference Modeling Approach
- Publisher: European Association of Geoscientists & Engineers
- Source: Conference Proceedings, 81st EAGE Conference and Exhibition 2019, Jun 2019, Volume 2019, p.1 - 5
Abstract
In this study, Elastic reverse time migration (ERTM) along with source normalized cross-correlation imaging condition is proposed to map subsurface geological features with clear physical meanings. RTM is a robust depth migration technique which can efficiently handle the lateral velocity variations, highly dipping reflectors, salt bodies and other complex structures all together. Irregular surface topography is properly honored during the modelling of seismic wave propagation which is not always a straightforward undertaking. The high order DRP/opt MacCormack scheme is used to solve partial differential velocity stress equations. Before back-propagating the receiver wavefield, proper pre-processing techniques are applied to remove surface waves and direct arrivals because only reflected signals are useful to image subsurface reflectors.The source and receiver wavefields are cross-correlated at each specific time step then all snapshots are stacked together to get final RTM results. The numerical experiments clearly demonstrate that our method can handle the surface topography and image subsurface geological features accurately.