Prediction method of plane distribution of thin sand body based on fractional 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 fractional Hilbert transform. The present invention will be described in detail below in conjunction with the embodiments.
[0043] Concrete steps of the present invention are as follows:
[0044] (1) Input the post-stack 3D seismic data volume w(i,j,n), i represents the serial number of the Inline survey line (the total survey line number is denoted as Nline), and j represents the Xline survey line serial number (the total survey line number is denoted as Nxline) , n represents the sampling point serial number of the single-trace seismic record (the total sampling point number 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 track record of the three-dimensional array w(i, j, n) Order Hilbert transform, get the result array w of the fractional order Hilbert transform of the three-dimen...
Embodiment 2
[0060] figure 1 It is the predicted section of sand bodies passing through Well W1 calculated by conventional methods (thin layer identification method based on Hilbert transform). The black thin layers in the figure represent sand bodies, and the curve next to Well W1 is the measured GR curve ( A low value of the GR curve indicates a sand body, and a high value of the GR curve indicates a mudstone formation). From figure 1 It can be seen that there are two defects in the conventional method: ①A set of black strata with good continuity appears on the top of the stratum (location: abscissa 470, ordinate 2098ms), and the GR value corresponding to this set of strata is a high value, that is, the set of strata The formation is not a sand body, and there are prediction artifacts; ② When the dip angle of the formation changes, at the position of the abscissa 510 in the figure, the black formation is intermittent, that is, the lateral continuity is poor, and the lateral resolution i...
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