The equivalent offset method of prestack time migration

Author:

Bancroft John C.1,Geiger Hugh D.2,Margrave Gary F.1

Affiliation:

1. The CREWES Project, Dept. of Geology and Geophysics, The University of Calgary, 2500 University Drive N.W., Calgary, Alberta T2N 1N4, Canada. Emails:

2. Lithoprobe, Dept. of Geology and Geophysics, The University of Calgary, 2500 University Drive N.W., Calgary, Alberta T2N 1N4, Canada.

Abstract

A prestack time migration is presented that is simple, efficient, and provides detailed velocity information. It is based on Kirchhoff prestack time migration and can be applied to both 2-D and 3-D data. The method is divided into two steps: the first is a gathering process that forms common scatterpoint (CSP) gathers; the second is a focusing process that applies a simplified Kirchhoff migration on the CSP gathers, and consists of scaling, filtering, normal moveout (NMO) correction, and stacking. A key concept of the method is a reformulation of the double square‐root equation (of source‐scatterpoint‐receiver traveltimes) into a single square root. The single square root uses an equivalent offset that is the surface distance from the scatterpoint to a colocated source and receiver. Input samples are mapped into offset bins of a CSP gather, without time shifting, to an offset defined by the equivalent offset. The single square‐root reformulation gathers scattered energy to hyperbolic paths on the appropriate CSP gathers. A CSP gather is similar to a common midpoint (CMP) gather as both are focused by NMO and stacking. However, the CSP stack is a complete Kirchhoff prestack migrated section, whereas the CMP stack still requires poststack migration. In addition, the CSP gather has higher fold in the offset bins and a much larger offset range due to the gathering of all input traces within the migration aperture. The new method gains computational efficiency by delaying the Kirchhoff computations until after the CSP gather has been formed. The high fold and large offsets of the CSP gather enables precise focusing of the velocity semblance and accurate velocity analysis. Our algorithm is formulated in the space‐time domain, which enables prestack migration velocity analysis to be performed at selected locations and permits prestack migration of a 3-D volume into an arbitrarily located 2-D line.

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

Reference39 articles.

1. Bancroft, J. C., 1996, Natural anti‐aliasing in equivalent offset prestack migration: 66th Ann. Internat. Mtg., Soc. Expl. Geophys., Expanded Abstracts, 1465–1466b.

2. Bancroft, J. C., and Geiger, H. D., 1994, Equivalent offsets and CRP gathers for prestack migration: 64th. Ann. Internat. Mtg., Soc. Expl. Geophys., Expanded Abstracts, 672–675.

3. 1996, Velocity sensitivity for equivalent offset prestack migration: a contrast in robustness and fragility: Can. Soc. Expl. Geophys. National Convention, Expanded Abstracts, 149–150.

4. 1997, Prestack seismic migration: US Patent 5 596 547.

5. 1998, Prestack seismic migration: Canadian Patent 2 161 048.

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