Maximum-joint-entropy-based post-stack seismic wave impedance inversion method
A technology of wave impedance inversion and maximum correlation entropy, applied in the field of seismic exploration, can solve the problems of poor robustness and can not completely eliminate the interference of impulse noise, and achieve the effect of high precision and strong robustness
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Embodiment 1
[0058] In this embodiment, the classic marmousi model is used as a reference model to generate post-stack seismic records, and the proposed maximum correlation entropy algorithm is used for inversion.
[0059] Known marmousi velocity models such as figure 2 As shown in (a), the post-stack seismic records generated by the convolution method are as follows: figure 2 As shown in (b), the seismic wavelet is the Reker wavelet with a dominant frequency of 40 Hz, and the sampling interval of the synthesized seismic records is 2 ms.
[0060] In order to analyze the robustness of the maximum correlation entropy criterion to noisy records, first analyze the image 3 (a) In the case of 5db Gaussian noise, the comparison is as follows image 3 L shown in (b) 2 Norm inversion results and such as image 3 (c) The maximum correlation entropy inversion results shown. Next, to the synthesized post-stack record add such as Figure 4 5db Laplacian noise (non-Gaussian noise) shown in (a),...
Embodiment 2
[0063] In this example, seismic inversion is carried out using the actual data of a shale gas work area in the west. The post-stack seismic records are as follows: Figure 5 (a) shown. For shale gas, kerogen content (TOC) is a key indicator to predict the presence of oil and gas in shale. Analyzing the intersection diagram of this work area, density and wave impedance are closely related to TOC. Therefore, whether a good TOC can be obtained depends on the results of seismic wave impedance inversion.
[0064] In order to verify the effectiveness of the maximum correlation entropy method and its advantages and disadvantages compared with traditional algorithms, such as Figure 5 (b) to Figure 5 (e) shown in this part respectively with L 1 , L 2 , Huber norm and maximum correlation entropy methods are used to invert the actual data. The inversion results obtained by the four methods are the wave impedance curve at the well position and the real logging curve; no matter fro...
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