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What Is Phase in Seismic Data Processing?
Phase describes the timing relationship between different frequency components of the seismic wavelet. Phase tells us the shape of the seismic wavelet and how the wiggles line up in time. Amplitude tells us how strong the wavelet and Phase tells us when/where is the wavelet is strong.
Changing phase changes the shape of the trace without changing its frequency content.
Common Phase Types in Seismic
Zero-phase
•Main peak is centered exactly on the reflector.
•Symmetric wavelet.
•Preferred for interpretation.
Minimum-phase
•Physically realistic for earth wavelets.
•Wavelet energy starts early.
•Used in processing before deconvolution.
Mixed-phase
•A combination of phase types due to:
oPoor source signature
oInstrument response
oAbsorption
oProcessing distortions
Why Phase Matters?
Even if amplitude is correct, phase errors make seismic difficult to interpret.
Phase affects:
•Reflector alignment
•Wavelet shape
•Tuning effects
•AVO analysis
•Inversion accuracy
•Horizon picking accuracy
What Is Phase Comparison?
Phase comparison is the process of comparing the phase of two seismic datasets to check whether they are aligned or not.
Example comparisons:
•Migrated vs unmigrated
•Raw vs filtered
•Vintage 1 vs Vintage 2
•Stack vs angle stacks
•Seismic vs well synthetic
•Time-lapse (4D) seismic
Phase comparison determines:
•Do wavelets line up correctly?
•Is one dataset shifted or rotated relative to the other?
•Do they have the same seismic character?
How Does Phase Comparison Work?
Phase comparison is done using cross-correlation, phase spectra, or wavelet estimation.
Cross-Correlation (Most Common)
How it works:
1.Choose two traces you want to compare.
2.Calculate cross-correlation.
3.Find:
oTime shift (static mismatch)
oPhase rotation (wavelet mismatch)
If correlation peak = 0 time lag → phases are aligned. If correlation is low → phases differ significantly.
Phase Spectrum Comparison
Use FFT to compute:
•Amplitude spectrum
•Phase spectrum
Plot phase vs frequency for both datasets.
We look for:
•Constant phase shift → simple rotation
•Frequency-dependent shift → mixed phase distortion
Wavelet Extraction
Extract wavelets from both datasets:
•Compare their shapes
•Compare their peak location
•Compare symmetry
This tells you zero-phase vs minimum-phase differences.
Phase Rotation & Matching
If one dataset has different phase:
•Apply a phase rotation (e.g., +30°, –20°)
•Recompare
•Repeat until wavelets match
This is standard in:
•Time-lapse (4D)
•Merging vintages
•Matching seismic to well synthetic
Why Do We Do Phase Comparison?
•To ensure two volumes can be merged
•To check if processing changed the wavelet
•To match seismic to synthetics
•To prepare for impedance inversion
•To ensure consistency across angle stacks
•To detect 4D changes in reservoir monitoring
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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
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