Method, device and computer storage medium for eliminating elastic reverse time offset crosstalk interference
A technology of reverse time migration and crosstalk interference, which is applied in the fields of exploration geophysical data processing and parameter inversion, can solve the problems of high economic cost, inaccurate imaging results, and degraded imaging quality, so as to improve computing efficiency and reduce a large number of The effect of TRON snapshot storage space and cost reduction
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Embodiment 1
[0093] This example uses a pulse test and a theoretical model (two-layer model) to compare the imaging results of traditional and improved ERTM in practical applications. First, the migration impulse responses for a set of PP and PS are calculated. Upper layer speed V P =2000m / s, V S =1070m / s, density ρ=20.7g / cm 3 ;Lower velocity V P =3000m / s, V S =1600m / s, density ρ=2.29g / cm 3 . A single point scattering is placed at the position of the two-layer model (3800m, 3500m), the Rayleigh wave source with a center frequency of 12Hz is placed at (4000m, 0m), and the receiver position is offset by 400m relative to the source. Using the staggered grid finite difference method (Virieux J.P-SV wave propagation in heterogeneous media: Velocity-stressfinite-difference method. Geophysics, 1986, 51(4): 889–901.) to solve the velocity-stress elastic wave equation, simulated a A multi-component record of the receiver's position. For better quality, the events of the diffracted P and S w...
Embodiment 2
[0097] This example uses a pulse test and the right part of the theoretical model (BP 2004 model) to compare the imaging results of traditional and improved ERTM in practical applications. First, the migration impulse responses for a set of PP and PS are calculated. Upper layer speed V P =2000m / s, V S =1070m / s, density ρ=20.7g / cm 3 ;Lower velocity V P =3000m / s, V S =1600m / s, density ρ=2.29g / cm 3 . Experiments with the BP 2004 model used 400 surface explosives and 900 equidistant bottom bottom nodes (OBNs). Figure 5 The imaging results of PP and PS are shown, and the backscatter noise of traditional ERTM is removed by high-pass filter, which ensures that the comparison can be made under the same bandwidth. When using this smoothed migration velocity, strong velocity gradients at the top of the salt dome introduce erroneous images ( Figure 5 arrows in a and 5c). In contrast, the image obtained by the improved method is more consistent with the actual formation after r...
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