Method for improving imaging effect of wave equation prestack depth migration
A pre-stack depth migration, wave equation technique, used in seismology, seismic signal processing, etc. for well logging
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Embodiment 1
[0067] Embodiment 1: Taking the 3600-shot seismic data obtained from the 3D seismic observation in the Daqing LMD area as an example, the method for improving the imaging effect of the wave equation pre-stack depth migration is described in more detail. The specific steps are:
[0068] (1) Use multiple streamers or multiple survey lines to record the seismic signals excited by the artificial source and reflected by the underground stratum, and record them on the magnetic tape. Specifically, in the LMD area of Daqing, the reflected seismic signals excited by the explosive source were obtained by means of multi-line acquisition, and recorded on the tape. The acquisition was 16 lines, bilateral observation, and the trace spacing was 40m; this time, the wave equation migration was used to directly generate the angular traces A total of 3,600 guns were used in the set method, covering 11.2 square kilometers. figure 1 It is a typical single-shot record after conventional noise su...
Embodiment 2
[0093] Embodiment 2: Using the 3600-shot seismic data obtained from the 3D seismic observation in the LMD area of Daqing, a process of improving the imaging effect of the pre-stack depth migration of the wave equation is performed again. The difference between Embodiment 2 and Embodiment 1 is that the first update algorithm is used for processing.
[0094] The processing process of the first update algorithm is: in step (3), the ρ corresponding to the event at different depths is directly picked up from the velocity error spectrum according to the position of the maximum energy cluster n , and layer the initial velocity model with the velocity error pick-up position. Define a unique correction factor r for each horizon i ; then solve the following system of linear equations:
[0095]
[0096] where n is the number of velocity stratification layers obtained when interpreting horizons based on events, and z i , v i with are the thickness of the i-th layer, the average...
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