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Abstract

The seismic inversion is known to be ambiguous, i.e. there is an infinite set of reflectivity series that agree with a seismic trace that has a certain bandwidth. We have found that the multi‐channel inversion has a unique solution, under some assumptions. The reflectivity solution and the seismic wavelet can be recovered because reflected signals have different interference in adjacent traces.

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/content/papers/10.3997/2214-4609.20145123
2011-05-10
2024-04-25

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