Abstract
Path-integral imaging forms an image with no knowledge of the velocity model by summing over the migrated images obtained for a set of migration velocity models. Double path-integral imaging migration extracts the stationary velocities, i.e. those velocities at which common-image gathers align horizontally, as a byproduct. An application of the technique to a real data set demonstrates that quantitative information about the time migration velocity model can be determined by double path-integral migration velocity analysis. Migrated images using interpolations with different regularizations of the extracted velocities prove the high quality of the resulting time-migration velocity information. The so-obtained velocity model can then be used as a starting model for subsequent velocity analysis tools like migration tomography or other tomographic methods. © 2011 Nanjing Geophysical Research Institute.
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Costa, J. C., & Schleicher, J. (2011). Double path-integral migration velocity analysis: A real data example. Journal of Geophysics and Engineering, 8(2), 154–161. https://doi.org/10.1088/1742-2132/8/2/003
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