Earthquake attenuation estimating method based on changes of spectrum area
A technology of attenuation estimation and spectral area, which is applied in the field of seismic attenuation estimation based on spectral area changes, can solve the problems of seismic data containing noise and difficult Q value estimation results, etc.
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[0081] (1) Synthetic seismic data calculation example
[0082] First, we verify the effectiveness of the invention with noise-free and noisy synthetic seismic data. figure 1 It is noise-free synthetic seismic data, with a total of 100 seismic data, including two horizontal layers. The source wavelet is a zero-phase Ricker wavelet with a main frequency of 40 Hz. The time sampling interval is 1 millisecond. The Q value of the first layer is 200, and the Q values of the second layer are 100 (track 1 to track 40), 30 (track 41 to track 60), and 60 (track 61 to track 100). First, we use the constant phase wavelet in formula (1) to estimate the source wavelet according to formula (2), and the result is as follows figure 2 so. figure 2 (a) The time-domain waveforms of the actual source wavelet and the estimated constant-phase wavelet (that is, the estimated source wavelet) are given, figure 2 (b) The Fourier spectra of the actual source wavelet and the estimated constant-ph...
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