Thin sand body plane distribution prediction method based on fractional order Hilbert transform
A technology of plane distribution and prediction method, which is applied in the field of oil and gas field exploration to achieve the effect of improving vertical resolution, avoiding prediction errors and improving accuracy
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Embodiment 1
[0042] The embodiment of the present invention provides a method for predicting the planar distribution of thin sand bodies based on the fractional Hilbert transform. The present invention will be described in detail below in conjunction with the embodiments.
[0043] The specific steps of the present invention are as follows:
[0044] (1) Enter the post-stack 3D seismic data volume w(i,j,n), i represents the number of the Inline survey line (the total number of survey lines is denoted as Nline), and j represents the number of the Xline survey line (the total number of survey lines is denoted as Nxline) , N represents the sampling point number of a single seismic record (the total number of sampling points is denoted as N);
[0045] (2) Let v=-1.0,-0.8,-0.6,-0.4,-0.2,0.2,0.4,0.6,0.8,1, score each seismic trace record of the three-dimensional array w(i,j,n) Order Hilbert transform, get the result array w of the fractional Hilbert transform of the three-dimensional array w(i,j,n) of e...
Embodiment 2
[0060] figure 1 It is the predicted section of sand body through Well W1 calculated by conventional method (thin layer recognition method based on Hilbert transform). The black thin layer in the figure represents the sand body, and the curve beside Well W1 is the measured GR curve ( The low value of the GR curve indicates the sand body, and the high value of the GR curve indicates the mudstone formation). From figure 1 Two defects of the conventional method can be seen: ① A set of black stratum with good continuity appears on the top of the stratum (location position: 470 track on the abscissa, 2098ms on the ordinate), and the corresponding GR value of this set of stratum is high, that is, the set The stratum is not a sand body, and there is a false prediction; ②When the stratum dip changes, the black stratum is intermittent at the position of 510 on the abscissa, that is, the lateral continuity is poor and the lateral resolution is low.
[0061] figure 2 It is the predicted se...
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