Fracture prediction analysis method based on structural evolution stratum strain
A crack prediction and analysis method technology, applied in geophysical measurement, seismology, measurement devices, etc., can solve the problems of collecting footprints, large resource consumption, interference noise, etc., and achieve the effect of eliminating the influence of outliers
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Embodiment 1
[0043] A fracture prediction analysis method based on tectonic evolution stratum strain, comprising the following steps:
[0044] A. Level calibration of the work area;
[0045] B. Pick up and track the target layer of seismic data and all layers above the target layer;
[0046] C. Calculate the gradient difference between the target horizon and all horizons above it;
[0047] D. Calculate the maximum positive curvature and maximum negative curvature of the gradient difference and eliminate singular values;
[0048] E. Judging the fracture development area and relative development degree according to the curvature value;
[0049] F. Superimpose the predicted areas to obtain the fracture development of the target layer.
[0050] Both the maximum positive curvature and the maximum negative curvature are a kind of curvature, which are defined as:
[0051] First let the surface be defined as:
[0052] Z(x,y)=Ax 2 +By 2 +Cxy+Dx+Ey+F
[0053] in
[0054]
[0055]
[005...
Embodiment 2
[0064] Based on the principles of the foregoing embodiments, this embodiment discloses a specific implementation manner.
[0065] A. Familiar with the data, understand the geological situation of the work area, use the logging data to make synthetic records for horizon calibration, or use VSP data for horizon calibration.
[0066] B. If figure 1 , figure 2 As shown, the target horizon of picking and tracking seismic data: For the 3D seismic horizon of thinning interpretation, it is necessary to perform horizon interpolation and check the interpolation results one by one. The survey lines with poor interpolation effects need to be manually analyzed according to the actual situation of the seismic event. Adjust and modify the interpolation results;
[0067] Pick and track all the horizons of the reflection interface in the geological period that can be compared and tracked above the target horizon: for the 3D seismic horizons that are interpreted thinly, first perform horizo...
Embodiment 3
[0077] Embodiment 2 can only realize the crack prediction of a single target layer. Based on Embodiment 2, the crack prediction of multiple target layers can be realized. The specific method is: first implement the method steps of Embodiment 2 to realize the crack prediction of a single target layer, and in the cycle step From B to F, it is enough to realize the fracture prediction of the remaining target layers.
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