PENGUKURAN RESISTIVITAS PADA DAERAH DUGAAN SUMBER PENYEBAB ANOMALI GEOMAGNETIK DI PULAU LOMBOK NTB
<p>possibilities of the source of geomagnetic anomaly in Lombok Island, i.e. a specific local structure composed by a quite large magnetic body or a local fault in this region that could be associated with a source of seismic hazard (especially earthquakes). An interesting profile could be est...
| Main Authors: | , , , , |
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| Format: | Article |
| Language: | English |
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Universitas Udayana
2009-06-01
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| Series: | Majalah Ilmiah Teknologi Elektro |
| Online Access: | http://ojs.unud.ac.id/index.php/JTE/article/view/1572 |
| _version_ | 1828541303706615808 |
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| author | Bulkis Kanata Teti Zubaidah Widya Utama Dwa Desa Warnana Cipta Ramadani |
| author_facet | Bulkis Kanata Teti Zubaidah Widya Utama Dwa Desa Warnana Cipta Ramadani |
| author_sort | Bulkis Kanata |
| collection | DOAJ |
| description | <p>possibilities of the source of geomagnetic anomaly in Lombok Island, i.e. a specific local structure composed by a quite large magnetic body or a local fault in this region that could be associated with a source of seismic hazard (especially earthquakes). An interesting profile could be estimated lie around the minimum geomagnetic anomaly (8<sup>0</sup>45’36”S, 116<sup>0</sup>1’48”E) to the maximum one (8<sup>0</sup>43’48”S, 116<sup>0</sup> 5’24” E). Understanding the corresponding structure on that profile is very important - related to the possibility of the source of geomagnetic anomaly in Lombok Island - in order to get further information about potentially local fault in this region as a source of earthquakes hazard.</p> <p>Geoelectric method with vertical electrical sounding (VES) configuration have been applied in this profile, on three VES points (i.e. one point between the minimum and the maximum geomagnetic anomaly (X<sub>1</sub>: 8<sup>0</sup>46’42.9”S, 116<sup>0</sup>04’07.7”E), and two other points outside (X<sub>2</sub>: 8<sup>0</sup>46’03.3”S, 115<sup>0</sup>58’39.9”E; which is on negative anomaly area) and (X<sub>3</sub>: 8<sup>0</sup>42’11.6”S, 116<sup>0</sup>08’27.2”E; which is on positive anomaly area).</p> <p>The potency of X<sub>1</sub> as a critical zone has been shown, with the existence of resistivity contrast in this area, which its resistivity value between X<sub>2</sub> (very high resistivity; r >25,000 Wm) and X<sub>3</sub> (very low resistivity; ; r >1 W m). This results lead to the potentially local fault in this region as a source of earthquakes hazard.</p> |
| first_indexed | 2024-12-12T01:37:48Z |
| format | Article |
| id | doaj.art-8107a96731674c5abf90bab83d33b3aa |
| institution | Directory Open Access Journal |
| issn | 1693-2951 2503-2372 |
| language | English |
| last_indexed | 2024-12-12T01:37:48Z |
| publishDate | 2009-06-01 |
| publisher | Universitas Udayana |
| record_format | Article |
| series | Majalah Ilmiah Teknologi Elektro |
| spelling | doaj.art-8107a96731674c5abf90bab83d33b3aa2022-12-22T00:42:48ZengUniversitas UdayanaMajalah Ilmiah Teknologi Elektro1693-29512503-23722009-06-01811545PENGUKURAN RESISTIVITAS PADA DAERAH DUGAAN SUMBER PENYEBAB ANOMALI GEOMAGNETIK DI PULAU LOMBOK NTBBulkis KanataTeti ZubaidahWidya UtamaDwa Desa WarnanaCipta Ramadani<p>possibilities of the source of geomagnetic anomaly in Lombok Island, i.e. a specific local structure composed by a quite large magnetic body or a local fault in this region that could be associated with a source of seismic hazard (especially earthquakes). An interesting profile could be estimated lie around the minimum geomagnetic anomaly (8<sup>0</sup>45’36”S, 116<sup>0</sup>1’48”E) to the maximum one (8<sup>0</sup>43’48”S, 116<sup>0</sup> 5’24” E). Understanding the corresponding structure on that profile is very important - related to the possibility of the source of geomagnetic anomaly in Lombok Island - in order to get further information about potentially local fault in this region as a source of earthquakes hazard.</p> <p>Geoelectric method with vertical electrical sounding (VES) configuration have been applied in this profile, on three VES points (i.e. one point between the minimum and the maximum geomagnetic anomaly (X<sub>1</sub>: 8<sup>0</sup>46’42.9”S, 116<sup>0</sup>04’07.7”E), and two other points outside (X<sub>2</sub>: 8<sup>0</sup>46’03.3”S, 115<sup>0</sup>58’39.9”E; which is on negative anomaly area) and (X<sub>3</sub>: 8<sup>0</sup>42’11.6”S, 116<sup>0</sup>08’27.2”E; which is on positive anomaly area).</p> <p>The potency of X<sub>1</sub> as a critical zone has been shown, with the existence of resistivity contrast in this area, which its resistivity value between X<sub>2</sub> (very high resistivity; r >25,000 Wm) and X<sub>3</sub> (very low resistivity; ; r >1 W m). This results lead to the potentially local fault in this region as a source of earthquakes hazard.</p>http://ojs.unud.ac.id/index.php/JTE/article/view/1572 |
| spellingShingle | Bulkis Kanata Teti Zubaidah Widya Utama Dwa Desa Warnana Cipta Ramadani PENGUKURAN RESISTIVITAS PADA DAERAH DUGAAN SUMBER PENYEBAB ANOMALI GEOMAGNETIK DI PULAU LOMBOK NTB Majalah Ilmiah Teknologi Elektro |
| title | PENGUKURAN RESISTIVITAS PADA DAERAH DUGAAN SUMBER PENYEBAB ANOMALI GEOMAGNETIK DI PULAU LOMBOK NTB |
| title_full | PENGUKURAN RESISTIVITAS PADA DAERAH DUGAAN SUMBER PENYEBAB ANOMALI GEOMAGNETIK DI PULAU LOMBOK NTB |
| title_fullStr | PENGUKURAN RESISTIVITAS PADA DAERAH DUGAAN SUMBER PENYEBAB ANOMALI GEOMAGNETIK DI PULAU LOMBOK NTB |
| title_full_unstemmed | PENGUKURAN RESISTIVITAS PADA DAERAH DUGAAN SUMBER PENYEBAB ANOMALI GEOMAGNETIK DI PULAU LOMBOK NTB |
| title_short | PENGUKURAN RESISTIVITAS PADA DAERAH DUGAAN SUMBER PENYEBAB ANOMALI GEOMAGNETIK DI PULAU LOMBOK NTB |
| title_sort | pengukuran resistivitas pada daerah dugaan sumber penyebab anomali geomagnetik di pulau lombok ntb |
| url | http://ojs.unud.ac.id/index.php/JTE/article/view/1572 |
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