| 摘要 |
In the determination of acoustic velocity from a suite of seismograms, the signal power of windows from the seismograms is detected for different assumed values of velocity, vertical travel time, and dip. A function indicative of signal presence is plotted as a function of velocity for different vertical travel times to provide an indication of the acoustic velocity characteristic. A plot of signal power for different dip searches provides good results for seismograms from an area including dipping formations.
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