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In the case of randomly missing traces in regularly sampled data,
a prediction-error filter cannot be found.
This section explains an alternative way to find a filter
whose spectrum is the inverse of the given data's spectrum.
If there exist several linear events in a data set, the zeros which were
found by the prediction-error filter would locate along the dips
in the spectrum.
If we know the dips of the events, therefore, we can simulate
the prediction-error filter by putting zeros along the dips in the spectrum.
Suppose we have N plane waves and each dip is pj, j=1,...,N,
respectively.
For each frequency
, then, N zeros along the wavenumber
are determined as follows :
![\begin{displaymath}
k_j = p_j \omega\end{displaymath}](img4.gif)
and the corresponding zeros are
![\begin{displaymath}
z_j = \exp(-ik_j).\end{displaymath}](img5.gif)
From those zeros, the prediction-error filter for each
is determined
in the form of the Z transform like
![\begin{displaymath}
F(z) = (1-z/z_1) (1-z/z_2) \dots (1-z/z_N).\end{displaymath}](img6.gif)
Next: Interpolation
Up: THREE STEP INTERPOLATION
Previous: Dip picking
Stanford Exploration Project
11/18/1997