STUDY of MICROGRAVITY ANOMALY PANTAI MUTIARA JAKARTA AREA FOR STRUCTURE IDENTIFICATION
<p align="justify">Pantai Mutiara is a reclamation area which used as a resident. This area is in Jakarta groundwater basin area which are controlled by normal fault with oriented to NorthWest-SouthEast and NorthEast-SouthWest. Study of gravity anomaly has done to identify the indica...
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id-itb.:109372017-10-09T10:31:14ZSTUDY of MICROGRAVITY ANOMALY PANTAI MUTIARA JAKARTA AREA FOR STRUCTURE IDENTIFICATION FIRMAN S. (NIM 123 00 014), MOKHAMAD Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/10937 <p align="justify">Pantai Mutiara is a reclamation area which used as a resident. This area is in Jakarta groundwater basin area which are controlled by normal fault with oriented to NorthWest-SouthEast and NorthEast-SouthWest. Study of gravity anomaly has done to identify the indication of geology structure in the area. With assisted by gradien analysis technique, that is secound order of vertical gradient (SVG) and first order of horizontal derivative (FHD), was identified existence of a normal fault at strike of NorthEast-SouthWest with NorthWest segment relative descend to SouthEast segment. Three dimension inverse modeling had been conducted to estimate the separation and dip of fault, and it found about 50 metres separation with 60 degrees dip of fault. text |
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<p align="justify">Pantai Mutiara is a reclamation area which used as a resident. This area is in Jakarta groundwater basin area which are controlled by normal fault with oriented to NorthWest-SouthEast and NorthEast-SouthWest. Study of gravity anomaly has done to identify the indication of geology structure in the area. With assisted by gradien analysis technique, that is secound order of vertical gradient (SVG) and first order of horizontal derivative (FHD), was identified existence of a normal fault at strike of NorthEast-SouthWest with NorthWest segment relative descend to SouthEast segment. Three dimension inverse modeling had been conducted to estimate the separation and dip of fault, and it found about 50 metres separation with 60 degrees dip of fault. |
| format |
Final Project |
| author |
FIRMAN S. (NIM 123 00 014), MOKHAMAD |
| spellingShingle |
FIRMAN S. (NIM 123 00 014), MOKHAMAD STUDY of MICROGRAVITY ANOMALY PANTAI MUTIARA JAKARTA AREA FOR STRUCTURE IDENTIFICATION |
| author_facet |
FIRMAN S. (NIM 123 00 014), MOKHAMAD |
| author_sort |
FIRMAN S. (NIM 123 00 014), MOKHAMAD |
| title |
STUDY of MICROGRAVITY ANOMALY PANTAI MUTIARA JAKARTA AREA FOR STRUCTURE IDENTIFICATION |
| title_short |
STUDY of MICROGRAVITY ANOMALY PANTAI MUTIARA JAKARTA AREA FOR STRUCTURE IDENTIFICATION |
| title_full |
STUDY of MICROGRAVITY ANOMALY PANTAI MUTIARA JAKARTA AREA FOR STRUCTURE IDENTIFICATION |
| title_fullStr |
STUDY of MICROGRAVITY ANOMALY PANTAI MUTIARA JAKARTA AREA FOR STRUCTURE IDENTIFICATION |
| title_full_unstemmed |
STUDY of MICROGRAVITY ANOMALY PANTAI MUTIARA JAKARTA AREA FOR STRUCTURE IDENTIFICATION |
| title_sort |
study of microgravity anomaly pantai mutiara jakarta area for structure identification |
| url |
https://digilib.itb.ac.id/gdl/view/10937 |
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1820666003863896064 |