--> ABSTRACT: Extended Stolt F-K Migration, by Craig Beasley, Walt Lynn, Ken Larner, and Hung V. Nguyen; #91035 (2010)
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Extended Previous HitStoltNext Hit F-K Previous HitMigrationNext Hit

Craig Beasley, Walt Lynn, Ken Larner, Hung V. Nguyen

Despite our understanding that depth Previous HitmigrationNext Hit is a more powerful imaging tool than time Previous HitmigrationNext Hit, time Previous HitmigrationNext Hit still constitutes the majority of Previous HitmigrationNext Hit done today. In selecting a time-Previous HitmigrationNext Hit algorithm, three primary criteria are of concern: accuracy in imaging steep dips, accuracy in the presence of vertical velocity variation, and computational effort. The ideal algorithm would be efficient and unlimited in its ability to image steep dips in arbitrary vertical velocity structures. It would also accommodate gentle lateral velocity variations deemed acceptable for time-Previous HitmigrationNext Hit methods.

A particularly attractive algorithm to consider is Previous HitStolt'sNext Hit f-k method: it is computationally efficient and has unlimited dip accuracy for constant-velocity media. Although Previous HitStolt'sNext Hit method can handle moderate vertical variations, errors become unacceptable for steep dips in the presence of large vertical velocity variation. An extension to Previous HitStoltNext Hit Previous HitmigrationNext Hit removes its restrictions on vertical velocity variation, yielding accuracy comparable to phase-shift Previous HitmigrationNext Hit at only a fraction of the computational time.

This extended Previous HitStoltNext Hit method is based on partitioning the velocity field in a manner analogous to that in cascaded finite-difference Previous HitmigrationNext Hit and performing a number of stages of Previous HitStoltNext Hit migrations. In each stage, the Previous HitmigrationNext Hit velocity field is closer to a constant--the ideal situation for Previous HitStoltNext Hit Previous HitmigrationNext Hit--than when the Previous HitmigrationNext Hit is done conventionally (i.e., in just one stage). Empirical results and error analyses show that four stages of extended Previous HitStoltNext Hit Previous HitmigrationTop are sufficient to migrate steeply dipping events accurately in nearly any vertically varying velocity field. In fact, for a wide range of velocity fields and dips, as few as two stages will produce phase-shift quality images. The method can be used for two-dimensional, two-pass three-dimensional, and single-pass three-dimensio al migrations.

AAPG Search and Discovery Article #91035©1988 AAPG-SEPM-SEG Pacific Sections and SPWLA Annual Convention, Santa Barbara, California, 17-19 April 1988.