#TITLE_ALTERNATIVE#
Seismic signal that record subsurface condition is non-stationer signal, it means data influence with wavelet and frequency that change depends on time. In the another side, atenuation influence caused by lithology makes the frequency of seismic signal decrease depends on time. To resolve this probl...
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| Format: | Final Project |
| Language: | Indonesia |
| Online Access: | https://digilib.itb.ac.id/gdl/view/7971 |
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| Institution: | Institut Teknologi Bandung |
| Language: | Indonesia |