Reverse Time Migration Method Based on Full-Wave Field vsp/rvsp Seismic Data
A technology of reverse time migration and seismic data, applied in the field of seismic data processing of oil and gas exploration, can solve the problems of resolution limitation, low main frequency of ground seismic data, narrow effective frequency band, etc., and achieve the effect of reasonable and accurate wave field calculation
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Embodiment 1
[0040] A method of reverse time migration based on full-wave wave field VSP / RVSP seismic data, which is realized through the following process:
[0041] (1) Observation system conversion of VSP / RVSP seismic data;
[0042] Before the reverse time migration, the data needs to be edited by the head; based on the reversible principle of the ray path, the offset replacement and the rearrangement of the gathers are carried out, and the common shot point gathers suitable for the reverse time migration are obtained.
[0043](2) The finite difference algorithm solves the wave equation;
[0044] 1) The wave equation in the time-space domain is numerically solved by using the finite difference method after difference. Among them, the full-wave wave equation with any order of difference accuracy is as follows:
[0045]
[0046] 2) Perform Fourier transform on the above formula to obtain the form of frequency-space domain:
[0047]
[0048] 3) Determine the time step for wave field...
Embodiment 2
[0062] In order to verify the application effect of the method described in Example 1, this embodiment is based on the VSP / RVSP seismic data of a certain exploration area, and the method described in Example 1 is used to process the data to verify the effect of the method. figure 1 The flowchart described in .
[0063] Compared with the surface seismic reverse time migration method, the reverse time migration method based on the full-wave wavefield VSP / RVSP seismic data has higher precision and migration imaging quality. In order to prove the application effect of this method, we use the simulated data of the thin interbed model to carry out the reverse time migration comparison experiment. In borehole earthquakes, shot points are buried near the surface. The geophones are placed underground and arranged in sequence at certain depth intervals. The recorded data mainly include downlink direct arrival waves, first arrival waves, interlayer multiple waves, diffracted waves and ...
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