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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Main Author: Jnanaparama Aparajita, Made
Format: Theses
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/53257
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:53257
spelling id-itb.:532572021-03-03T08:48:21ZFULL-WAVEFORM INVERSION IN TIME DOMAIN BY ITERATIVE FREQUENCY INCREASED Jnanaparama Aparajita, Made Indonesia Theses full-waveform inversion time domain, local minimum, global minimum INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/53257 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 text
institution Institut Teknologi Bandung
building Institut Teknologi Bandung Library
continent Asia
country Indonesia
Indonesia
content_provider Institut Teknologi Bandung
collection Digital ITB
language Indonesia
description 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
format Theses
author Jnanaparama Aparajita, Made
spellingShingle Jnanaparama Aparajita, Made
FULL-WAVEFORM INVERSION IN TIME DOMAIN BY ITERATIVE FREQUENCY INCREASED
author_facet Jnanaparama Aparajita, Made
author_sort Jnanaparama Aparajita, Made
title FULL-WAVEFORM INVERSION IN TIME DOMAIN BY ITERATIVE FREQUENCY INCREASED
title_short FULL-WAVEFORM INVERSION IN TIME DOMAIN BY ITERATIVE FREQUENCY INCREASED
title_full FULL-WAVEFORM INVERSION IN TIME DOMAIN BY ITERATIVE FREQUENCY INCREASED
title_fullStr FULL-WAVEFORM INVERSION IN TIME DOMAIN BY ITERATIVE FREQUENCY INCREASED
title_full_unstemmed FULL-WAVEFORM INVERSION IN TIME DOMAIN BY ITERATIVE FREQUENCY INCREASED
title_sort full-waveform inversion in time domain by iterative frequency increased
url https://digilib.itb.ac.id/gdl/view/53257
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