Extended offset data processing

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G06F 1900

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057610622

ABSTRACT:
Wide-angle reflections that have been overcorrected using a simple two-term hyperbolic moveout correction are adjusted by application of a bi-quadratic term. The biquadratic term is derived by scanning the overcorrected reflections for residual velocity. The residual velocity is used to calculate an adjustment as a linear function of the first power of the travel time to each receiver versus the fourth power of the corresponding receiver offset.

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Zisserman et al., "Identification Of Events From 3D Volumes Of Seismic Data", Image Processing--1994 International Conference, 1994, pp. 309-313, 1994.
Hubral, Peter and Krey, Theodor; "Interval Velocities from Seismic Reflection Time Measurements", pp. 13-18.
Tsvankin, Ilya and Thomsen, Leon; "Nonhyperbolic reflection moveout in anisotropic media", GEOPHYSICS, vol. 59, No. 8 (Aug. 1994), pp. 1290-1304.
Dix, C. Hewitt; "Seismic Prospecting for Oil", Harper & Brothers, New York, pp. 124-126.

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