1887

Abstract

Both Gabor deconvolution and inverse-Q filtering methods are based on the constant Q-model theory for attenuation of seismic waves. Gabor deconvolution methodologically differs from inverse-Q filter in that the compensation for attenuation and the inversion of the minimum phase wavelet component of the seismic trace are carried out simultaneously.

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/content/papers/10.3997/2214-4609.201405182
2005-06-13
2024-12-03
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/content/papers/10.3997/2214-4609.201405182
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