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GCTuning Effects' Impact on Seismic*
Gwang Lee1, Keumsuk Lee2, and Han Kim3
Search and Discovery Article #40474 (2009)
Posted November 30, 2009
*Adapted from the Geophysical Corner column, prepared by the authors, in AAPG Explorer, October, 2009. Editor of Geophysical Corner is Bob A. Hardage ([email protected]). Managing Editor of AAPG Explorer is Vern Stefanic; Larry Nation is Communications Director.
1Pukyong National University
2Korea National Oil Corp
3Korea Ocean Research and Development Institute
When reflection times are measured along the peaks, troughs or zero crossings of seismic
traces, tuning effects make it difficult to measure accurate arrival times of individual reflection events. The thinnest interval over which a correct measurement of the distance between two closely spaced reflectors can be made is called the tuning thickness. The edges of reservoir bodies are often thinner than tuning thickness, and therefore a special approach – such as spectral decomposition or inversion – is required to reliably determine reservoir boundaries.
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We examine the tuning effect for a low-impedance wedge (Figure 1) that mimics a gas-sand layer embedded in shale. The wedge is illuminated by zero-phase and minimum-phase Ormsby wavelets that have identical frequency spectra (Figure 2). Figure 3a shows the synthetic
The thickness estimate and amplitude tuning curves measured from the
When the wedge is thinner than the tuning thickness, the top and bottom reflections are pushed apart and cause arrival times to be slightly too early for the top of the wedge and slightly too late for the bottom. Thus the measured thickness is greater than the true thickness when the wedge thins to less than λ/5.
The threshold thickness above which the measured amplitude (Figure 3c) gives the correct reflectivity of the top of the wedge is about 5λ/8 (60 m). For wedge thicknesses less than 5λ/8, the amplitude tuning curve is characterized by two maxima at about λ/5 (19 m) and about λ/2 (45 m). These maxima occur when the central trough of the top reflection aligns first with the leading negative side lobe of the wavelet from the bottom interface and then with the trailing negative side lobe. As the wedge thins to less than λ/5, the amplitude decreases rapidly, reaching about -0.02, which is approximately only 10 percent of the correct reflectivity.
Figure 4a shows the synthetic
The thickness tuning curves from zero-amplitude picking (dashed blue line, Figure 4c) and from the trough/peak picking (green line) both give the correct thickness until the wedge thins to about 21 m (slightly less than λ/4). The measured amplitude of the leading trough along the top of the wedge gives the correct reflectivity of the sand/shale interface until the wedge thins to approximately λ/8, slightly larger than one-half of the Rayleigh resolution (Figure 4c). There are no amplitude maxima as exhibited by the zero-phase wavelet (Figure 3c), because the leading peak from the bottom reflection does not constructively interfere with the leading trough of the top reflection event. The amplitude again decreases rapidly below the threshold thickness, reaching about -0.02.
1) Tuning thicknesses for both zero-phase and minimum-phase data are slightly less than the Rayleigh resolution limit.
2) Event amplitudes can be better measured from minimum-phase data than from zero-phase data. 3) Amplitude detuning is probably not required for minimum-phase data for bed thicknesses greater than about one-half of the Rayleigh resolution limit.
Because event amplitudes in zero-phase data are significantly affected by tuning, amplitude interpretations based on zero-phase data should be calibrated or detuned for correct amplitude analysis.
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