By PHILLIP BORDING and LARRY LINES

Editor's note: Bording is a consultant in Hazel Green, Ala., and Lines is with the University of Calgary, Canada.

The Geophysical Corner is a regular column in the EXPLORER, produced cooperatively by the AAPG Geophysical Integration and SEG Interpretation committees, and edited by R. Randy Ray. This month's column is titled "Seismic Modeling and Imaging - Making Waves."

Seismic Modeling Makes Waves

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Figure 2

Figure 3a

Figure 3b

Figure 2

This cartoon shows the seismic experiment, and the concept of the "exploding reflector" used in the reverse-time migration experiment. The upper left part of the figure shows the seismic reflection experiment for a coincident seismic source (flag) and receiver (triangle). Seismic energy travels from the source, down to the reflector and returning back to the receiver. In the upper right we see the "exploding reflector" model that is almost always equivalent to this seismic reflection experiment. In this model, we consider seismic waves to travel a one-way path from the reflector to the surface receiver (or half the reflected distance) at a velocity that is half the velocity of the medium. Reverse-time migration images the seismic data by reversing the path of the exploding reflector model. Recorded seismic energy is propagated backward in time to its point of origin.