Non-hyperbolic velocity scanning and dynamic correction method
A speed scanning, non-hyperbolic technology, applied in the field of geophysical exploration, can solve problems such as difficult to obtain
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Embodiment 1
[0038] With the method of velocity scanning and dynamic correction of the present invention, model A is a horizontal layered velocity model in an actual area, with 7 layers in total: the thickness of the first layer is 600m, and the seismic wave velocity is 2800m / s; the thickness of the second layer is 450m, and the seismic wave The velocity is 3200m / s; the thickness of the third layer is 850m, and the seismic wave velocity is 3500m / s; the thickness of the fourth layer is 400m, and the seismic wave velocity is 4000m / s; the thickness of the fifth layer is 400m, and the seismic wave velocity is 4100m / s; the thickness of the sixth layer is 650m , the seismic wave velocity is 4450m / s; the thickness of the seventh layer is 500m, and the seismic wave velocity is 4300m / s. The obtained Δτ(x) time difference curves of the 2nd, 4th, and 7th floors ( image 3 , Figure 4 ), the more layers of the model, the greater the time difference Δτ, and the larger the offset x, the greater the tim...
Embodiment 2
[0040] Using the method of velocity scanning and dynamic correction of the present invention, Δτ is calculated for the layer velocity model of model B. Model B is a horizontal layer velocity model with 7 layers in total. Model B and model A only change the velocity of the fifth layer. , the thickness of the fifth layer is 400m, and the seismic wave velocity is 6000m / s. The relationship diagram between the obtained time difference curve Δτ(x) and x / h of the seventh floor ( Figure 5 ), when the ratio of offset to formation depth (x / h) is 1.5, the Δτ time difference of the seventh layer of model B reaches 20ms, and the hyperbolic method cannot be used for velocity scanning and dynamic correction. The Δτ of the seventh layer of model B The time difference is up to 8ms, and it is basically feasible to use the hyperbolic method for speed scanning and dynamic correction. For areas where there are high-speed formations, such as carbonate rock areas, the method of the invention is us...
Embodiment 3
[0042] Using the method of the present invention to obtain the stacking velocity error caused by the large offset distance, the hyperbolic equation velocity scan is used to obtain the stacking velocity in a certain area. According to the actual model A and the maximum offset distance, for the fourth layer, the processing method used The maximum offset distance is 4500m, and its Δτ time difference reaches 7ms. The maximum velocity error ΔVm calculated by the method of the present invention is 24m / s. For the 7th floor, the maximum offset distance adopted during processing is 6200m, and the Δτ time difference reaches 8ms. The calculated maximum velocity error ΔVm is 29m / s, and the stacked velocity error ΔVe caused by the large offset is estimated, and ΔVe is half of ΔVm; through the application of this method, high-precision formation velocity information in this area can be obtained.
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