Correlation weighted reverse time migration imaging method based on wave field separation
A technology of reverse time migration imaging and wave field separation, which is applied in the direction of measuring devices, instruments, scientific instruments, etc., can solve the problems of low universality and too large human-influenced factors on the imaging section, and achieve high-precision imaging Effect
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[0046] The invention proposes a correlation weighted reverse time migration imaging method based on wave field separation. The present invention uses the horizontal layered medium model to simulate the real underground medium situation in the field, and the horizontal layered medium velocity model is as follows figure 1 As shown, the velocity of the first layer is 2500m / s, the velocity of the second layer is 3000m / s, and the density model of the horizontal layered medium is as follows figure 2 As shown, the density of the first layer is 1800kg / m 3 , the density of the second layer is 2800kg / m 3 , the horizontal length of the model is 1500m, and the vertical length is 1500m.
specific Embodiment approach
[0048] (1) Based on the velocity model and density model of the above-mentioned horizontal layered medium, given the source wavelet f and the seismic record M, the shot point position is at the horizontal coordinate of 750m, a total of 301 traces are received, and the trace interval is 5m. They are all on the surface, the depth is 0m, the time sampling interval is 0.5ms, and the receiving record length is 1s. Using the first-order stress-velocity acoustic wave equation (as shown in Equation (1)) to perform finite-difference forward modeling, the source wave field S(x,z,t) at each moment can be obtained:
[0049]
[0050] In the formula, x and z are space coordinates respectively, and v x , v z They are the vibration velocity of the particle in the x and z directions, p is the stress, t is the time, ρ is the density, and v is the sound wave velocity.
[0051] (2) Taking the seismic record M as the disturbance, the finite-difference inverse time continuation is also carried...
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