ANALISIS DEFORMASI AKIBAT GEMPA LOMBOK JULIAGUSTUS 2018 DENGAN MENGGUNAKAN DATA INSAR
Lombok Island, in West Nusa Tenggara (NTB), is located on the active tectonic area, surrounding by the sources of earthquake which have potential to create shocks, such as Back Arc Thrust at the north region, megathrust at the south area, and sliding fault system at west and east region, therefor...
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| Format: | Final Project |
| Language: | Indonesia |
| Online Access: | https://digilib.itb.ac.id/gdl/view/48765 |
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| Institution: | Institut Teknologi Bandung |
| Language: | Indonesia |
| Summary: | Lombok Island, in West Nusa Tenggara (NTB), is located on the active tectonic area,
surrounding by the sources of earthquake which have potential to create shocks, such as Back
Arc Thrust at the north region, megathrust at the south area, and sliding fault system at west
and east region, therefore, Lombok Island has high earthquake potential. Some of the
earthquake are destructive, such as the earthquake incident on July 29, 2018 (6.4 Mw), August
5 (7 Mw), August 9 (6,2 Mw) and August 19 (6,9 Mw) in Lombok. This research is conducted
to give information regarding the size of sliding or movement of earth surface which caused by
some series of Lombok earthquake by using DInSAR (Differential Interferometry Synthetic
Aperture Radar) technology from 6 satellite imageries Sentinel-1 on July 2018 and August
2018 , also DEM SRTM 30meter. As the result of InSAR, indicate that generally, the change
of earth surface impacted by the series of Lombok earthquake is uplift at the north coast area
with cumulative result reached around 40 cm, but also has subsidence which detected at the
east and west coast area at around 3 cm. |
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