2007Chinese Journal of GeophysicsRequires access

DSR one-way wave equation prestack τ migration

Cheng Jiu

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Abstract

By transforming the classical double-square-root(DSR) one-way wave equation from the depth domain to the two-way vertical traveltime(τ) domain,we derive an one-way DSR wave propagator which can be applied to mathematically implement sinking survey.Its algorithm to recursively continue the source and receiver wavefields,which includes a wavenumber domain phase shift in a constant background medium followed by a phase correction in the space domain that accommodates lateral velocity variations,can tackle the effects of lateral velocity variations for imaging under complex overburdens.Combing with the zero-offset and zero-time imaging condition,we develop a DSR equation prestack migration method that implements wavefield continuation and imaging in the τ space.To address the problems that full volume 3-D DSR equation migration could meet with in production application,we present a feasible common-azimuth prestack τ migration approach based on the theory of crossline common-offset migration.Numerical tests show that DSR equation prestack τ migration provides a significant improvement over the traditional prestack time migration technology in laterally varying media.

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By transforming the classical double-square-root(DSR) one-way wave equation from the depth domain to the two-way vertical traveltime(τ) domain,we derive an one-way DSR wave propagator which can be applied to mathematically implement sinking survey.Its algorithm to recursively continue the source and receiver wavefields,which includes a wavenumber domain phase shift in a constant background medium followed by a phase correction in the space domain that accommodates lateral velocity variations,can tackle the effects of lateral velocity variations for imaging under complex overburdens.Combing with the zero-offset and zero-time imaging condition,we develop a DSR equation prestack migration method that implements wavefield continuation and imaging in the τ space.To address the problems that full volume 3-D DSR equation migration could meet with in production application,we present a feasible common-azimuth prestack τ migration approach based on the theory of crossline common-offset migration.Numerical tests show that DSR equation prestack τ migration provides a significant improvement over the traditional prestack time migration technology in laterally varying media.

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Available abstract

By transforming the classical double-square-root(DSR) one-way wave equation from the depth domain to the two-way vertical traveltime(τ) domain,we derive an one-way DSR wave propagator which can be applied to mathematically implement sinking survey.Its algorithm to recursively continue the source and receiver wavefields,which includes a wavenumber domain phase shift in a constant background medium followed by a phase correction in the space domain that accommodates lateral velocity variations,can tackle the effects of lateral velocity variations for imaging under complex overburdens.Combing with the zero-offset and zero-time imaging condition,we develop a DSR equation prestack migration method that implements wavefield continuation and imaging in the τ space.To address the problems that full volume 3-D DSR equation migration could meet with in production application,we present a feasible common-azimuth prestack τ migration approach based on the theory of crossline common-offset migration.Numerical tests show that DSR equation prestack τ migration provides a significant improvement over the traditional prestack time migration technology in laterally varying media.

Key concepts: Prestack, Wave equation, Offset (computer science), Seismic migration, Azimuth, Acoustic wave equation, Time domain, Algorithm

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