Method of processing seismic data for AVO or AVOA characterization
View Patent ↗The invention relates to a method of processing seismic data comprising a gather of seismic traces organised according to one or several acquisition parameters, each trace comprising a seismic signal defined by an amplitude as a function of time or depth, the method comprising the steps of: a) defining a base of elementary functions of the acquisition parameter(s), b) orthogonalising said elementary functions so as to define a base of orthogonal elementary functions c) for a given time or at a given depth, determining combination coefficients defining a combination of the orthogonal elementary functions, said combination being an estimator of a variation in the amplitude of the seismic signal as a function of the acquisition parameter(s).
1. A method of processing seismic data comprising a gather of seismic traces organized according to one or several acquisition parameters, each trace comprising a seismic signal corresponding to waves that have traveled through a subsoil and have been recorded by a seismic receiver, said signal being defined by an amplitude as a function of time or depth, the method comprising the steps of:
a) defining a base of elementary functions of the acqusition parameter(s),
b) orthogonalising said elementary functions so as to define a base of orthogonal elementary functions
c) for a given time or at a given depth, determining combination coefficients defining a combination of the orthogonal elementary functions, said combination being an estimator of a variation in the amplitude of the seismic signal as a function of the acquisition parameter(s), so as to deduce information about lithological properties of the subsoil based on said estimator.
2. The method according to claim 1 , in which said traces have been corrected previously in an RMO correction step.
3. The method according to claim 1 , in which the acquisition parameter(s) is (are) chosen from among the group of parameters comprising of the offset, azimuth angle, incidence angle, source-receiver coordinates.
4. The method according to claim 1 , wherein step c) is carried out for a plurality of sampling times or depths.
5. The method according to claim 1 , in which the elementary functions are polynomial or trigonometric functions.
6. The method according to claim 1 , wherein step b) further comprises the step of normalizing elementary functions so as to define a base of normalized elementary functions prior to orthogonilisation.
7. The method according to claim 1 , in which seismic data include a plurality of gathers of traces, wherein steps a), b) and c) are carried out independently for each gather of traces.
8. The method according to claim 7 , including the steps of determining variations of the coefficients as a function of the acquisition parameter(s) on a plurality of gathers of traces and filtering the coefficients.