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![]() | Imaging with multiples using linearized full-wave inversion | ![]() |
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We construct a one-layered model (Figure 5 a) with ocean-bottom geometry. The only sharp interface in the migration velocity is the seabed. Figure 5 b shows the synthetic data. The labels
,
and
correspond to the first, second, and third order events as shown in figure 2 b and c. Note that we used equation 2 to generate the synthetic data. Hence, internal multiples are absent.
Figure 5 c shows the migration image
. The migration image is made up of signal
and crosstalk artifacts
. In the figure, the label
indicates spurious reflectors generated by migrating the primary signal (
) as if it were a multiple.
is the correct reflector in the image.
is an artifact generated by migrating the multiple signal (
or
) as if it were a primary reflection. In equation form, they are denoted as follows:
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Onelayerv2
Figure 5. (a) Original one layered model, (b) synthetic data, (c) migration image and (d) inversion image. |
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![]() | Imaging with multiples using linearized full-wave inversion | ![]() |
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