Extraction Method of Instantaneous Phase Gradient Attributes Based on Waveform of Marine Broadband Seismic Data
A technology of instantaneous phase and seismic data, applied in the field of petroleum exploration and development, can solve the problem of ignoring the corresponding relationship of phase discontinuity characteristics, and achieve the effects of stable phase characteristics, improved signal-to-noise ratio, and improved characterization ability.
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Embodiment 1
[0046] figure 1 and figure 2 It is the result of the method without broadband seismic data, that is, the effect analysis of wavelets with different polarities when broadband seismic data is not used. figure 1 is the instantaneous phase gradient attribute graph calculated by the positive polarity Riker wavelet with a main frequency of 35Hz, where figure 1 (a) is a zero-phase positive Ricker wavelet with a main peak and two obvious side lobes; figure 1(b) is the instantaneous phase obtained after the Hilbert transform of the wavelet, and the winding phenomenon of the phase from π to -π appears at the position of the side lobe of the corresponding wavelet, and two discontinuous change points appear; figure 1 (c) is the instantaneous phase gradient attribute after obtaining the first derivative of the instantaneous phase by retaining the phase winding phenomenon. Two false discontinuous interfaces appear at the corresponding wavelet side lobe positions, indicating the wavelet s...
Embodiment 2
[0052] Such as Figure 7 As shown, it is an example of calculating seismic signals fitted by different wavelets, and this embodiment is used to illustrate the advantages of calculating instantaneous phase gradient attributes based on broadband seismic data. Figure 7 (a) is the reflection coefficient of the formation, corresponding to three reflection coefficients at the positions of time 250ms, 350ms and 450ms respectively, and the reflection coefficient values are: -0.5, 0.2, -0.4; figure 1 (a), image 3 (a) and Figure 5 The positive polarity wavelet in (a) is convolved with the reflection coefficient to obtain the corresponding seismic trace data and calculate its corresponding instantaneous phase gradient attribute. Figure 7 (b) is the reflected seismic signal synthesized by the 35Hz positive polarity Rake wavelet, Figure 7 (c) is the instantaneous frequency attribute calculated by the conventional method. Because the conventional method performs unwrapping process...
Embodiment 3
[0054] Adopt the conventional method and the method of the present invention to survey and map the seismic section and the instantaneous attribute section somewhere, the result is as follows Figure 8 (a)~ Figure 8 (f) shown. in, Figure 8 (a) is the seismic section acquired by conventional horizontal streamers and processed conventionally; Figure 8 (b) is the instantaneous frequency attribute profile calculated by conventional methods on conventional data. It can be seen that the resolution is very low, and it is difficult to see the development characteristics of waterways; Figure 8 (c) is an instantaneous phase gradient attribute profile calculated based on conventional data using the method proposed by the present invention. Due to the interference of ghost waves in conventional seismic data, the position of the discontinuous interface does not have a good correspondence with the stratigraphic sequence interface , there are obvious multiple solutions in the calculati...
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