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Attenuates periodic/ringing events
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Cepstrum(reverse order of Spec) Deconvolution is a wavelet-removal technique that works by transforming seismic data into the cepstrum where source periodicities (multiples, bubble pulses, reverberations) appear as isolated peaks. By applying a lifter (reverse order of fil) filter in the quefrency domain, these periodic components are removed, producing a cleaner, more reflectivity-like trace.
What is Cepstrum Deconvolution?
Cepstrum deconvolution is a method for removing the source wavelet from seismic data by converting the signal into the cepstrum domain — a special domain where reverberations, multiples, and periodic wavelet signatures appear as distinct peaks and can be isolated and removed.
It is especially good at:
•Removing short-period multiples
•Removing source bubble effects in marine data
•Removing ghosts
•Flattening reverberations
•Extracting the minimum-phase wavelet
Why Use Cepstrum Deconvolution?
Traditional deconvolution (spiking/predictive) struggles when:
•Wavelet is mixed-phase
•Reverberations are embedded inside the wavelet
•Multiples have regular periodicity
•Data have strong source bubble oscillations
Cepstrum deconvolution excels because:
•Convolution becomes addition in the cepstrum
•Periodic wavelet features show up as distinct spikes
•These can be suppressed using windows or filters
How Cepstrum Deconvolution Works?
A seismic trace is: x(t) = w(t) * r(t)
Step 1 — Fourier Transform: X(f) = W(f) . R(f)
Step 2 — Take Log Spectrum: ln X(f) = ln W(f) + ln R(f)
This is the key: Convolution becomes addition.
| Step 3 — Inverse FFT of log spectrum → Cepstrum |
C(Ƭ) = F-1 {ln X(f)}
•Ƭ is called "quefrency"
•Peaks at particular t correspond to periodicities (multiples, bubble oscillations)
Step 4 — Apply a “lifter” (cepstral filter)
•Suppress long-period or short-period components
•Remove wavelet periodicity
•Keep reflectivity terms
Step 5 - Transform back
Ẍ(f) = exp {FFT(Cfiltered)}
Inverse FFT gives the cepstrum-deconvolved trace.

What Cepstrum Deconvolution Removes?
Short-path multiples - Bubble pulse or peg-leg multiples appear as repeating periodic events that are strong in cepstrum.
Ghost effects - Source/receiver ghost period appears as a cepstrum peak.
Source wavelet periodicity - Any oscillatory wavelet component (Vibroseis sweep edges, bubble oscillation).
Reverberations / ringing - Room acoustics / poor weathering layers.
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If value is too small - we may be attenuating the primaries, if the value is too big , we may not attenuating the multiples. Optimum values are recommended. For marine bubbles, anything between 20-40ms is a good starting point.
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Cepstrum deconvolution separates convolution into addition by taking log of the spectrum and inverse transforming it (the “cepstrum”). This allows us to detect and remove periodic wavelet components.
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There are no action items available for this module so the user can ignore it.
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YouTube video lesson, click here to open [VIDEO IN PROCESS...]
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Yilmaz. O., 1987, Seismic data processing: Society of Exploration Geophysicist
* * * If you have any questions, please send an e-mail to: support@geomage.com * * *
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The input data connection for this module. Connect this item to the output of the preceding module in the processing workflow to feed seismic trace data into the cepstrum deconvolution algorithm.
The seismic gather to be deconvolved. This can be a pre-stack gather (e.g., a CMP, shot, or receiver gather) or a post-stack gather. Connect this to the Output gather of the previous module in the sequence. Each trace in the gather is processed independently through the cepstrum deconvolution algorithm to remove periodic wavelet components such as multiples, bubble pulses, and reverberations.
Defines the start of the cepstral window used to isolate the primary signal. In the cepstrum domain, this is the minimum quefrency boundary — the point where the primary energy is considered to begin. Quefrency values below this threshold contain the very low-frequency (smooth) component of the log spectrum and are excluded from the primary window.
Default value: -100 ms. The negative sign indicates this is the pre-zero time window that captures the maximum-phase component of the wavelet. Setting this value too small (close to zero or positive) risks distorting the wavelet by excluding important low-quefrency components. Setting it too large (very negative) may inadvertently include low-frequency noise in the primary window. For most datasets, the default value of -100 ms is a good starting point.
Defines the end of the cepstral primary window, and is the single most important parameter in cepstrum deconvolution. This value sets the quefrency boundary between the primary signal region and the periodic noise region. Any cepstral energy at quefrencies beyond this value — corresponding to short-period multiples, bubble pulses, reverberations, source/receiver ghosts, and ringing — will be attenuated by the lifter filter.
Default value: 400 ms. If this value is set too small, primary reflections may be attenuated along with the periodic noise, degrading the signal. If it is set too large, short-period multiples and reverberations will not be sufficiently removed. For marine data affected by bubble oscillations, values in the range of 20 to 40 ms are a recommended starting point. Use the cepstrum display to identify the quefrency of the dominant periodic event and set this value just below that peak.
Controls the amount of pre-whitening applied during the deconvolution step to stabilize the spectral division and prevent division by very small numbers (numerical instability). This is expressed as a fraction of the average spectral amplitude.
Default value: 0.01 (1%). A small noise value (e.g., 0.01) gives a stronger deconvolution effect but may amplify noise in frequency bands with low energy. A larger value (e.g., 0.1 or 10%) makes the output more stable but reduces the strength of the deconvolution. Increase this value if the output traces show unusual amplitude spikes or spectral ringing after processing.