PSEUDO-ANALYTICAL METHOD FOR THE SOLUTION OF WAVE EQUATIONS
First Claim
1. A method of seismic exploration within a predetermined volume of the earth containing structural and stratigraphic features conducive to the generation, migration, accumulation, or presence of subsurface resources, comprising the steps of:
- a. accessing a digital representation of a seismic survey that images at least a portion of said predetermined volume of the earth;
b. selecting at least a portion of said seismic survey, thereby selecting a plurality of seismic traces;
c. obtaining a velocity model at least approximately representative of at least a portion of said imaged portion of said predetermined volume of the earth, said velocity model having at least one velocity therein;
d. using at least said a portion of said velocity model to determine an error compensating pseudo-differential operator;
e. using said error compensating pseudo-differential operator to construct a time-marching wave equation solution for use in a migration program;
f. migrating said plurality of seismic traces using said migration program, thereby producing a plurality of migrated seismic traces; and
,g. using at least a portion of said plurality of migrated seismic traces to explore for subsurface resources within the predetermined volume of the earth.
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Accused Products
Abstract
The instant invention is a method for numerically propagating waves or solving wave equations on a digital computer. This invention can be used to compute highly accurate solutions to the wave equation, in fact in some cases it computes the analytical solution, something previously considered impossible. The instant method can also propagate waves that are not described by differential equations, such as anisotropic scalar waves. The invention has the advantages that it is computationally efficient, accurate, and flexible. Of importance is the ability to propagate waves that simulate the P-wave arrivals in both isotropic and anisotropic media with a scalar as opposed to a vector equation.
89 Citations
19 Claims
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1. A method of seismic exploration within a predetermined volume of the earth containing structural and stratigraphic features conducive to the generation, migration, accumulation, or presence of subsurface resources, comprising the steps of:
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a. accessing a digital representation of a seismic survey that images at least a portion of said predetermined volume of the earth; b. selecting at least a portion of said seismic survey, thereby selecting a plurality of seismic traces; c. obtaining a velocity model at least approximately representative of at least a portion of said imaged portion of said predetermined volume of the earth, said velocity model having at least one velocity therein; d. using at least said a portion of said velocity model to determine an error compensating pseudo-differential operator; e. using said error compensating pseudo-differential operator to construct a time-marching wave equation solution for use in a migration program; f. migrating said plurality of seismic traces using said migration program, thereby producing a plurality of migrated seismic traces; and
,g. using at least a portion of said plurality of migrated seismic traces to explore for subsurface resources within the predetermined volume of the earth. - View Dependent Claims (2, 3, 4, 5, 6, 7)
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8. A method of seismic exploration within a predetermined volume of the earth containing structural and stratigraphic features conducive to the generation, migration, accumulation, or presence of subsurface resources, comprising the steps of:
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a. accessing a digital representation of a seismic survey that images at least a portion of said predetermined volume of the earth; b. selecting at least a portion of said seismic survey, thereby selecting a plurality of seismic traces; c. obtaining a velocity model at least approximately representative of at least a portion of said imaged portion of said predetermined volume of the earth, said velocity model having at least one velocity therein; d. using at least said a portion of said velocity model to determine an error compensating pseudo-differential operator; e. using said error compensating pseudo-differential operator to construct time-marching wave equation solution for use in an inversion program; f. inverting said plurality of seismic traces using said inversion program, thereby producing an earth parameter model; and
,g. using at least a portion of said earth parameter model to explore for subsurface resources within the predetermined volume of the earth. - View Dependent Claims (9, 10, 11, 12, 13, 14)
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15. A method of seismic exploration within a predetermined volume of the earth containing structural and stratigraphic features conducive to the generation, migration, accumulation, or presence of subsurface resources, comprising the steps of:
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a. obtaining a velocity model at least approximately representative of at least a portion of said predetermined volume of the earth, said velocity model having at least one velocity therein; b. using at least said a portion of said velocity model to determine an error compensating pseudo-differential operator; c. using said error compensating pseudo-differential operator to construct a time-marching wave equation solution for use in a seismic modeling program; d. using said seismic modeling program to create a plurality of synthetic seismic traces at least approximately representative of a portion of the predetermined volume of the earth; and
,e. using said plurality of synthetic seismic traces to explore for subsurface resources within the predetermined volume of the earth. - View Dependent Claims (16, 17, 18, 19)
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Specification