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Abstract

Summary

The diffraction component of the wave field gives significant information about the position of faults and fractured areas. There are different approaches for wave field separation into reflected and scattered components. For directional gathers obtained by full-azimuth migration there are also different ways of data filtering. The methods that are used for production projects as well as new developments are discussed in this report.

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/content/papers/10.3997/2214-4609.201702295
2017-09-11
2024-04-24
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