#TITLE_ALTERNATIVE#
Topography and low velocity layer effect at area of seismic data acquisition that have lateral P-wave velocity variation cause the first break at any given trace has not yet resided in right position actually. Static correction need to be done until the position of source and receiver is one level d...
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| Format: | Final Project |
| Language: | Indonesia |
| Online Access: | https://digilib.itb.ac.id/gdl/view/12092 |
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| Institution: | Institut Teknologi Bandung |
| Language: | Indonesia |
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