Time-frequency analysis method
A technology of time-frequency analysis and time-spectrum, applied in the field of seismic signal spectrum analysis
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Embodiment 1
[0098] First, the synthetic seismic trace is constructed by the Morlet wavelet, such as figure 2 shown. It contains two combinations: three adjacent time and the same main frequency 20Hz wavelet; two same time position and main frequency are 20Hz and 40Hz respectively. The model design is mainly to test the accuracy of the method of the present invention, and at the same time to test the vertical time resolution and horizontal frequency resolution in the frequency spectrum.
[0099] Perform Gabor time-frequency processing, WVD time-frequency processing, exponential window smoothing pseudo-Spwvd time-frequency processing and the present invention's time-frequency processing respectively to the single channel model data, and the results obtained are respectively as follows Figure 3 to Figure 6 shown.
[0100] right Figure 3 to Figure 6 It can be seen that the spectral resolution is the lowest when Gabor is used, and the vertical and horizontal resolution is limited by the ...
Embodiment 2
[0102] Create a wedge-shaped thin-layer model, such as Figure 7 As shown, the wavelet is selected from Leike, and the main frequency is 15Hz. Input the model data, respectively do Gabor time-frequency processing, exponential window smoothing pseudo-Spwvd time-frequency processing and the time-frequency processing of the present invention. The frequency division results are as follows Figure 8 to Figure 10 As shown, they correspond to the 20Hz single-frequency profiles of the three methods.
[0103] Compare Figure 8 to Figure 10 It can be seen that the present invention has higher single-frequency thin-bed resolution capability in thin-interbed seismic frequency-division applications.
Embodiment 3
[0105] The study of fractured-vuggy carbonatite reservoirs is one of the key points of exploration in the Tarim area of China. Figure 11 It is a physical model based on fracture-cavity heterogeneity research, which is composed of caves of different scales, and shows strong amplitude on the seismic section.
[0106] Input the crack-cavity model signal, make Gabor time-frequency distribution, ST time-frequency distribution, CWT time-frequency distribution and the time-frequency distribution of the present invention respectively, choose 25Hz single-frequency profile to compare, the results obtained are respectively as follows Figure 12 to Figure 15 shown.
[0107] Compare Figure 12 to Figure 15 It can be seen that the frequency division accuracy of the present invention is better for caves of different scales, and the distinction between caves is obvious and easy to identify. layer prediction.
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