Vibroseis deconvolution: a comparison of cross-correlation and frequency-domain sweep deconvolution |
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Authors: | KF Brittle LR Lines AK Dey |
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Institution: | University of Calgary, Department of Geology and Geophysics, Earth Science Building 240, 2500 University Drive N.W., Calgary, Alberta T2N 1N4, Canada |
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Abstract: | Ideally, traditional vibroseis processing produces a band-limited zero-phase Klauder wavelet through cross-correlation of the sweep with the recorded signal. An alternative wavelet processing method involves deconvolving the sweep from the recorded vibroseis trace. This deconvolution can be achieved through frequency-domain division. We compare and contrast the advantages and disadvantages of sweep deconvolution versus cross-correlation on synthetic and real data. |
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