Kirchhoff’s Depth Migration over Heterogeneous Velocity Models with Ray Tracing Modeling Approach
Complex seismic signatures are generated due to the complexity of the subsurface which is difficult to interpret. In the present study, an attempt has been made to model the complex subsurface using the Ray tracing modeling technique. Add to this, for the imaging of these geological features, Kirchhoff’s prestack depth migration is applied over the synthetic common shot gather dataset. It is found that the Kirchhoff’s migration technique in addition with the Ray tracing modeling concept has the flexibility towards the imaging of various complex geology which gives satisfactory results with proper delineation of the reflectors at their respective true depth position. The entire work has been carried out under the MATLAB environment.
Digital Object Identifier (DOI): doi.org/10.5281/zenodo.1339798Procedia APA BibTeX Chicago EndNote Harvard JSON MLA RIS XML ISO 690 PDF Downloads 1139
 Alaei, B. 2012. Seismic Modeling of Complex Geological Structures, in: Masaki Kanao (Ed.), Seismic Waves-Research and Analysis, InTech, pp. 213-236.
 Berkhout A.J. 2012. Combining full wavefield migration and full waveform inversion, a glance into the future of seismic imaging, Geophysics 77, S43–S50.
 Carcione, J. M., G. C. Herman, and A. P. E. ten Kroode, 2002. Seismic modeling, Geophysics 67, 1304-1325.
 Clearbout, J. F., 1986, Fundamental of geophysical data processing, McGraw-Hill.
 Geoltrain, S., and Brac, J., 1993, Can we image complex structures with first-arrival traveltime migration, Geophysics, 58, 564-575.
 Gray, S. H., and May, W. E, 1994, Kirchhoff migration using eikonal equation traveltimes, Geophysics, 59, 810-817.
 Schneider, W. A., 1978, Integral formulation for migration in two and three dimensions, Geophysics, 43, 49-76.