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MSvE in p-tau domain. Real data.![]()
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Real data, p-tau domain, the nearest to p = 0 trace. An excellent example of incoherent multiples produced by a thin-layer slab of sediments superposed on a strong reflector - basalt with lateral variation of the sea floor.
- The first arrival and the expected - in accordance with the strategy of predictive deconvolution - moments of multiple arrivals are marked with impulses beneath. There is no visible self-repetition of waveforms, even rather short segments of the trace have a very low correlation coefficient. It is not hard to predict that none of strategies - which exploit the correlation of waveforms- can yield a satisfactory result.
Example of MSvE-run.
Besides a sea-surface two principle horizons generate multiples: a thin-layer slab of sediments
forming a sea-floor and basalt beneath.The fragment does not contain detectable primaries beneath basalt.
- A. Input trace;
- B. EET output: Envelope;
- C. Mask-filter I, responsible for removal of all of a free-surface related multiples;
- D. Relative output I;
- E. Mask-filter II, responsible for removal of intrabed reverberations sea-floor - basalt;
- F. Final output of MSvE
Another fragment from the same profile does.
Multiple Suppression via Envelopes.Real data.
- Left column: input CMP-gathers;
- Right column: output of MSvE.
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