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Processing steps with alternative implementations
Seismic processing is
characterized by a sequence of processing steps, that is more or less fixed or
standardized; however, for each of these steps there are number of alternative
ways for their implementation. The choice of the most appropriate way depends on
geophysical considerations; therefore the processing geophysicist should have a
thorough understanding of the geophysical principles that underly these
processes. An overview of the processing steps with, for each step a number
of alternative implementations, is given below:
-
Editing
- spike removal
- noise burst removal
-
Statics
- field statics, elevation corrections
- first arrival picking and modeling of the near surface
- reflection signal picking and residual (short wavelength) statics
- stackpower optimization (e.g. simulated annealing)
- wave equation redatuming
-
Velocity analysis
- CVG, CVS, semblance, the eigenvalue method, coherency inversion
- moveout correction and stacking
- normal incidence times and normal incidence wavefront curvature
- velocity model building
- relationship of stacking velocity with dmo and time migration velocity
-
Signal-to-noise enhancement
- straight stack, weighted stack, diversity stack
- velocity stack and parabolic Radon transform
- median filter based methods
- Wiener filter, matched filter, output energy filter
- Karhunen Loeve transform
- f,x-domain prediction filtering
-
Deconvolution
- spectrum estimation
- wavelet estimation and designature
- dereverberation and deghosting
- deabsorption
- estimation of the earth response
- least-squares filters: spiking deconvolution and gapped deconvolution
- vibroseis processing
- data adaptive deconvolution
- deterministic deconvolution
- deconvolution methods:
- least-squares Wiener filters
- maximum-, minimum entropy or parsimonious deconvolution
- homomorphic deconvolution
- ARMA model deconvolution
-
Multiple elimination
- predictive deconvolution in (t,x)-domain or linear (tau,p)-domain
- differential moveout methods:
- (weighted) stack
- k,f-domain filtering
- parabolic Radon transform
- SRME = free surface related multiple elimination
- dereverberation with wave equation redatuming of sources and receivers
-
DMO
- dmo and velocity analysis
- dmo and pre-stack imaging (psi)
- 2D and 3D Kirchhoff implementation
-
Migration
- time migration - velocity analysis
- depth migration - velocity model building
- migration algorithms:
- finite difference
- Fourier domain; e.g. phase-shift, phase-shift plus interpolation
- Kirchhoff or summation or (weighted)diffraction stack migration
- reverse time migration (RTM)
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