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The principle of maximum entropy with a χ² constraint is developed as a stacking technique for seismic data. The formalism is applied to the stacking of single correlated Vibroseis traces. The computational results can differ significantly from those of a mean stack. They also illustrate the effectiveness of the method in the reduction of noisy amplitudes compared to those that are less noisy.
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Inguva et al. (1981) studied this question.
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