FULL-WAVEFORM INVERSION IN TIME DOMAIN BY ITERATIVE FREQUENCY INCREASED
With seismic imaging techniques using numerical solutions of seismic acoustic wave equations, full-waveform inversion in the time domain can be a tool for estimating high-resolution models from complex geological conditions. However, full-waveform inversion in the time domain has several drawback...
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| 主要作者: | |
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| 格式: | Theses |
| 語言: | Indonesia |
| 在線閱讀: | https://digilib.itb.ac.id/gdl/view/53257 |
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| 機構: | Institut Teknologi Bandung |
| 語言: | Indonesia |
| 總結: | With seismic imaging techniques using numerical solutions of seismic acoustic
wave equations, full-waveform inversion in the time domain can be a tool for
estimating high-resolution models from complex geological conditions. However,
full-waveform inversion in the time domain has several drawbacks, namely if you
determine the initials of the model that is far from the global minimum (the true
model) will give a stacked result at the local minimum and to overcome this
problem is to use the method of increasing the frequency iteratively. With this
method, at least it will keep away the results from a local minimum and close to a
global minimum. The result of using the iterative frequency increment method on
the full-waveform inversion time domain produces an image that resembles the
original synthetic model and produces an updated velocity value that is not too
different from the actual velocity value of the synthetic model |
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