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Abstract

Summary

We have shown an overview of the practical deghosted processes and it requiring resources over the last 10 years. The key to a successful seismic deghosting process is to find an appropriate deghosting operator for both source and receiver ghosts. Depending on the different survey configurations, streamer types, and geologic settings, a solution can be derived in different domains. It can be both FK, Tau-P, Xt-domains, or time domain. These domains are suitable for any streamer configuration and the search for the deghosting operator performed in floating windows. Since ghost operator depends on dips, then in Xt-domain a result has conflicting dips. This problem can be solved by estimation parameters in local windows with constant dips sections. In the Tau-P domain, data from different receivers are mixed, and for a streamer with variable depth, it complicates. Therefore, a special algorithm working in local Dip-Xt domains helps for a streamer with significant variations in depth. To obtain a stable solution for the entire seismic section, the estimation of ghost delay and reflection coefficient should be performed in a sliding window. The most robust method is a T-X/F-X Bootstrap performed in sliding windows that can be applied in any domain.

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/content/papers/10.3997/2214-4609.202150034
2021-03-22
2024-04-28
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References

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