Method for migration of seismic reflection waves

Communications – electrical: acoustic wave systems and devices – Seismic prospecting – Land-reflection type

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367 63, G01V 128

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044647379

ABSTRACT:
In seismic exploration a seismic source transmits seismic energy into the earth and seismic detectors record the seismic waves returning to the earth's surface from reflecting subsurface interfaces. The downgoing transmitted seismic energy and the upcoming reflected seismic waves are transformed into the frequency domain, downward continued, and summed to produce a migrated seismic depth section.

REFERENCES:
Schultz et al., "Depth Migration Before Stack", Geophysics, vol. 45, No. 3, Mar. 1980, pp. 376-393.
Judson et al., "Depth Migration After Stack", Geophysics, vol. 45, No. 3, Mar. 1980, pp. 361, 373-375.
Amalendu Roy, "Convergence in Downward Continuation for Some Simple Geometries", Geophysics, vol. 32, No. 5, Oct. 1967, pp. 853-871.
Rohde et al., "Migration of Time Contour Mays Using Downward Continuation", Technical Papers, Fiftieth Annual International Meeting and Exposition, Society of Exploration Geophysicists, 1980, pp. 337-373.

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