Affiliation:
1. The University of Texas at Austin, Bureau of Economic Geology, John A. and Katherine G. Jackson School of Geosciences, Austin, Texas, USA..
Abstract
Diffraction imaging aims to emphasize small subsurface objects, such as faults, fracture swarms, and channels. Similar to classical reflection imaging, velocity analysis is crucially important for accurate diffraction imaging. Path-summation migration provides an imaging method that produces an image of the subsurface without picking a velocity model. Previous methods of path-summation imaging involve a discrete summation of the images corresponding to all possible migration velocity distributions within a predefined integration range and thus involve a significant computational cost. We have developed a direct analytical formula for path-summation imaging based on the continuous integration of the images along the velocity dimension, which reduces the cost to that of only two fast Fourier transforms. The analytic approach also enabled automatic migration velocity extraction from diffractions using a double path-summation migration framework. Synthetic and field data examples confirm the efficiency of the proposed techniques.
Publisher
Society of Exploration Geophysicists
Subject
Geochemistry and Petrology,Geophysics
Reference44 articles.
1. Zero-offset Based Prediction of Common-offset Diffraction Traveltimes
2. Diffraction imaging by multifocusing
3. Azimuthally Anisotropic 3D Velocity Continuation
4. Burnett, W., S. Fomel, and R. Bansal, 2011, Diffraction velocity analysis by path-integral seismic imaging: 81st Annual International Meeting, SEG, Expanded Abstracts, 3898–3902.
5. Claerbout, J. F., 1986, Velocity extrapolation by cascaded 15 degree migration: Technical Report SEP-48: Stanford Exploration Project, 79–84.
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