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Flattening without picking

Jesse Lomask and Jon Claerbout

lomask@sep.Stanford.EDU, jon@sep.Stanford.EDU

ABSTRACT

We introduce an analytical method for integrating dip information to flatten uninterpreted seismic data. First, dips are calculated over the entire seismic volume. The dip is then integrated in the Fourier domain, returning for each sample a time shift to a flat datum. Then each sample is shifted in the seismic data to remove all structural folding deformation in a single non-interpretive step. Using the Fourier domain makes it a quick process but requires that the boundaries are periodic. This method does not yet properly handle faults because of their discontinuous nature, but is presently very effective at removing warping and folding.



 
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Stanford Exploration Project
11/11/2002