Removal of internal multiples with the common-focus-point (CFP) approach: Part 2 — Application strategies and data examples
Author(s) -
D. J. Verschuur,
A. J. Berkhout
Publication year - 2005
Publication title -
geophysics
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.178
H-Index - 172
eISSN - 1942-2156
pISSN - 0016-8033
DOI - 10.1190/1.1925754
Subject(s) - multiple , focus (optics) , boundary (topology) , computer science , algorithm , point (geometry) , field (mathematics) , surface (topology) , reflector (photography) , layer (electronics) , scattering , domain (mathematical analysis) , extension (predicate logic) , optics , mathematics , geometry , mathematical analysis , arithmetic , physics , light source , chemistry , organic chemistry , pure mathematics , programming language
In the past, the surface-multiple-removal method based on the feedback model has been successfully applied to many different field data sets. The extension of surface to internal multiples can be made by replacing shot records with common-focus-point (CFP) gathers, a CFP gather representing focused data with one source in the subsurface and all receivers at the surface (or vice versa for a receiver gather). The internal-multiple-removal algorithm can be formulated in terms of boundary-related and layer-related versions. In the boundary-related version, the internal multiples are removed for one downward-scattering reflector at a time. In the layer-related version, the internal multiples are removed for a sequence of downward-scattering reflectors at a time. An exact velocity model is not required, but proper muting is critical; muting becomes straightforward in the CFP domain. The strategy for applying the two versions of the multiple-removal algorithm is demonstrated on physical-model and field data. One can conclude that the layer-related version is the most appropriate in most situations because it requires less user action and does not need exact knowledge of the multiple-generating boundary
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