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Abstract

The number of grids in a velocity model defined for transversely isotropic media with vertical symmetry axis is the crucial parameter in modelling and processing of seismic data. We propose a method to reduce the number of grids both along the symmetry axis and within the symmetry plane direction. The method is based on the preserve-traveltime smoothing technique.

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/content/papers/10.3997/2214-4609.20142481
2013-05-13
2024-04-23

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