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Test gabor deconvolution procedure
Seismic signal non-stationary signals, the wavelet is changing with time. Gabor deconvolution of seismic traces cut into several pieces Gabor in each sub-wave film is constant, it is possible to achieve a non-stationary signal to smooth signal conversion. Therefore, Gabor deconvolution is considered to be a high-resolution, true-amplitude reflection coefficient estimation method.