EGU26-7954, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-7954
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Tuesday, 05 May, 15:10–15:20 (CEST)
 
Room D1
Reverse Time Migration Using Modified Nearly Analytical Discretization for Large-Scale High-Resolution Imaging
Toktam Zand
Toktam Zand
  • Institute of Geophysics of the Polish Academy of Sciences, Seismic Research, Poland (tzand@igf.edu.pl)

The advanced imaging technique reverse time migration (RTM) requires solving the partial differential wave equation, for which an analytical solution is infeasible and numerical methods are necessary. A significant challenge in numerical methods arises from inaccuracies in derivatives approximation, making the wave's velocity frequency-dependent and causing numerical dispersion. It is an unphysical artifact that degrades modeling and imaging, particularly at higher frequencies and over time. Avoiding numerical dispersion at high frequencies requires finer spatial grids, which substantially increase computational costs to achieve high-resolution imaging results.
The modified nearly analytical discretization (MNAD) method reduces numerical dispersion by incorporating additional analytical relations through solving both the wavefield and its spatial gradient fields numerically, employing them in higher-order derivative approximations, and improving spatial derivative estimation via energy conservation optimization. 
MNAD is introduced for RTM in large-scale studies, where leveraging compact stencils and coarser spatial and temporal grids enables high-resolution imaging with substantially lower computational and memory costs compared to conventional finite difference (FD) methods. Furthermore, adjoint-state imaging is enhanced with a novel data boundary condition interpolation using MNAD gradient fields, mitigating aliasing effects in recovered images from data recorded at half the Nyquist rate. The proposed approach provides a powerful opportunity for imaging, reducing the required number of sources/receivers and alleviating acquisition costs.
Synthetic experiments validate the method's performance in modeling and imaging on coarser grids than FD methods and in maintaining stability over longer times. Further, the MNAD-based RTM application to ocean bottom seismometer (OBS) data in a large-scale study confirms its capability to achieve high-resolution images with reduced computational costs. Finally, imaging with data sampled at half the Nyquist rate highlights the potential of the proposed approach for minimizing acquisition costs without sacrificing resolution and suffering from aliasing.
These findings affirm MNAD as a robust and efficient alternative to FD methods for large-scale, high-resolution imaging, offering significant advantages in computation, storage, and acquisition efficiency.

 
 

How to cite: Zand, T.: Reverse Time Migration Using Modified Nearly Analytical Discretization for Large-Scale High-Resolution Imaging, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-7954, https://doi.org/10.5194/egusphere-egu26-7954, 2026.