Method for stable estimation of anisotropic parameters for P-wave prestack imaging
A method is disclosed for determining interval anisotropic parameters. The method includes determining normal moveout (NMO) velocities and effective anelliptical parameters from seismic data traces. The NMO velocities are processed to obtain interval NMO velocities. The NMO velocities, effective anelliptical parameters and interval NMO velocities are inverted to obtain the interval anisotropic parameters. In one embodiment, the inversion includes damped least squares. In one embodiment, the inversion is preconditioned.
1. A method for determining interval anisotropic parameters, comprising:
determining normal moveout velocities and effective anelliptical parameters from seismic data traces; and
inverting the normal moveout velocities and the effective anisotropic parameters to obtain the interval anelliptical parameters, the inverting comprising damped least squares inversion.
2. The method of claim 1 further comprising preconditioning the inverting.
3. The method of claim 1 wherein the inverting comprises solving a system of linear equations by conjugate gradients.
4. The method of claim 1 wherein the determining normal moveout velocities and effective anelliptical parameters are performed by scanning a time migrated trace gather, the time migrated trace gather accounting for ray bending.
5. The method of claim 1 further comprising generating a prestack depth migrated image using the interval normal moveout velocities and interval anelliptical parameters.
6. A computer program stored in a computer readable medium, the program including logic operable to cause a programmable computer to perform steps, comprising:
determining normal moveout velocities and effective anelliptical parameters from seismic data traces;
inverting the normal moveout velocities and the effective anisotropic parameters to obtain interval anelliptical parameters, the inverting comprising damped least squares inversion.
7. The computer program of claim 6 further comprising preconditioning the inverting.
8. The computer program of claim 6 wherein the inverting comprises solving a system of linear equations by conjugate gradients.
9. The computer program of claim 6 wherein the determining normal moveout velocities and effective anelliptical parameters are performed by scanning a time migrated trace gather of the seismic data traces, the time migrated gather accounting for ray bending.
10. The computer program of claim 6 further comprising generating a prestack depth migrated image using the interval normal moveout velocities and interval anelliptical parameters.