A reflection full waveform inversion method based on common imaging point gathers
A common imaging point gather and full waveform inversion technology, applied in seismology, instruments, measuring devices, etc., can solve problems such as difficult to ensure the accuracy of dynamic characteristics, achieve accurate two-way illumination compensation, and reduce calculation time , calculate the effect of stability
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Embodiment 1
[0069] In this embodiment, the two-dimensional inclusion model is used as the real model (such as Figure 4 shown), the model has a total of 401 × 201 grids, the grid spacing is 10 m × 10 m, and the minimum and maximum speed are 2000 m / s and 2500 m / s respectively. A total of 201 shots were performed, the shot points were evenly distributed at a depth of 10 meters underground, the distance between the shots was 20 meters, the first shot was at 0 meters in the horizontal position, and the detection points were evenly distributed on the surface at intervals of 10 meters, and the maximum offset distance of each shot was The initial model is a uniform background model of 2000 m / s. During the inversion process, the frequency domain data of 2-22 Hz is divided into 100 frequencies at intervals of 0.2 Hz, and the inversion results like Figure 5 shown. Referring to the real model, it can be found that the reflection full waveform inversion method based on the common imaging point gat...
Embodiment 2
[0082] In this embodiment, the two-dimensional Overthrust theoretical model is used as the real model (such as Image 6 shown), the model has a total of 801 × 187 grids, the grid spacing is 25 m × 25 m, and the minimum and maximum speed are 2300 m / s and 6500 m / s respectively. A total of 401 shots were played, the shot points were evenly distributed at a depth of 25 meters underground, the distance between the shots was 50 meters, the first shot was at 0 meters in the horizontal position, and the detection points were evenly distributed on the surface at 25 meters intervals. The maximum offset is limited to 4000 meters, the minimum offset is 0 meters, and the initial model is the real model Gaussian smoothing result (such as Figure 7 In the inversion process, the frequency domain data of 2-22 Hz is divided into 100 frequencies at intervals of 0.2 Hz, and the inversion results are as follows Figure 8 As shown, it can be seen that the present invention basically accurately rec...
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