Method for separating and de-noising wave fields of longitudinal and transverse earthquake waves
A technology for seismic data and determination methods, applied in the direction of seismic signal processing, etc., can solve the problems of effective signal destruction, limited application space, and hindering the extraction of geological information.
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[0101] Take a physical model with 100 seismic records and 2048 sampling points as an example to illustrate the implementation steps:
[0102] Step 1: Read the seismic data with 100 traces and 2048 sampling points in each trace into a two-dimensional array F 1 middle.
[0103] Step 2: According to the superposition velocity of longitudinal waves and the time-distance law of P-P reflected waves, the original seismic data F 1 Perform normal time difference correction to get L 1 . The normal time difference is determined by:
[0104] Δt = t - t 0 = t 0 2 + x 2 v P 2 - t 0
[0105] Where: Δt is the normal time difference of the P-P reflected wave, x is the offset distance...
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