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7th International Conference & Exposition on Petroleum Geophysics

Time-Domain High-Resolution Radon Transform

Published in GEOHORIZONS - 2008

Michel Schonewille, PGS (UK). Peter Aaron, PGS (US). Carl Notfors, PGS (Singapore). Ping Zhao* PGS (Australia)

Abstract


Multiple attenuation may be classified in two main methodologies; 1) Prediction of multiples from the data itself, and 2) utilizing moveout separation between multiples and primaries. A commonly used version of the prediction approach is the so called SRME technique, where surface related multiples are predicted from the data itself, and at least in principle, does not require any further information. The SRME approach, certainly in its 3D implementation is very computationally intensive, but in recent years with the advent of commodity priced Linux clusters, has become very popular. However, the SRME technique does not work well in shallow marine environments and does not handle interbed multiples, thus there is still a need for approaches based on separation. In this paper we present the method utilizing multiple-primary separation in a tutorial fashion and show its progression from its simplest form in FK space to the latest timedomain Radon high-resolution demultiple.

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