Method and device for constructing elastic migration seismic wave field
A technology of seismic wave field and construction method, applied in the field of exploration geophysics
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Embodiment 1
[0110] The invention provides a method for constructing an elastic migration seismic wave field, such as figure 1 As shown, the method specifically includes:
[0111] Step S11, according to the elastic wave velocity stress equation, obtain the finite difference coefficient of the extended compact interlaced grid;
[0112] Step S12, calculating the extended compact staggered grid finite difference operator matrix;
[0113] Step S13, constructing a source wave field forward extrapolation operator and a receiver wave field reverse time extrapolation operator;
[0114] Step S14, according to the forward extrapolation operator of the source wave field, the preset medium model and the source function, realize the forward extrapolation of the seismic wave field, and obtain the source wave field;
[0115] Step S15, according to the reverse time extrapolation operator of the detection wave field, the preset medium model and the preset multi-component seismic data, realize the reverse...
Embodiment 2
[0158] This embodiment describes the specific process of the elastic migration seismic wavefield construction method provided in Embodiment 1. The method flow of this embodiment is as follows figure 2 Shown:
[0159] Process 1. Extended compact staggered grid differential discretization of the elastic wave velocity-stress equation
[0160] In the elastic migration seismic wave field construction method provided in Embodiment 1, the elastic wave velocity stress equation used is:
[0161] ∂ v x ∂ t = 1 ρ ( ∂ ...
Embodiment 3
[0221] This embodiment provides a specific embodiment of applying the elastic migration seismic wave field construction method, which specifically uses the elastic migration seismic wave field construction method provided in Embodiment 1 to perform elastic reverse time migration imaging on a preset medium model.
[0222] The pre-set medium model P-wave velocity field such as image 3 shown. image 3 In , the horizontal coordinate is the spatial geographic location, the vertical coordinate is the depth position, and the color depth of different points in the coordinate system represents the longitudinal wave velocity at that point. image 3 The medium scale marks the different longitudinal wave velocities represented by different color depths, the shear wave velocity is 0.588 times the corresponding longitudinal wave velocity, and the density is constant ρ=1000kg / m 3 , the horizontal width is 17km, the vertical depth is 3.5km, the horizontal and vertical spatial sampling inter...
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