1D AND 2D INVERSION OF GEOELECTRICAL DATA FOR GEOTHERMAL EXPLORATION
The geoelectric method is a method that uses the principle of electric current to investigate the subsurface structure of the earth. This method is done by injecting direct electric current into the earth's surface and then measuring the resulting potential difference, so that the apparent resi...
Saved in:
| Main Author: | |
|---|---|
| Format: | Final Project |
| Language: | Indonesia |
| Online Access: | https://digilib.itb.ac.id/gdl/view/65417 |
| Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
| Institution: | Institut Teknologi Bandung |
| Language: | Indonesia |
| id |
id-itb.:65417 |
|---|---|
| spelling |
id-itb.:654172022-06-22T15:46:17Z1D AND 2D INVERSION OF GEOELECTRICAL DATA FOR GEOTHERMAL EXPLORATION De Surya, Ramadhyan Indonesia Final Project Apparent Resistivity, Geothermal, Schlumberger. INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/65417 The geoelectric method is a method that uses the principle of electric current to investigate the subsurface structure of the earth. This method is done by injecting direct electric current into the earth's surface and then measuring the resulting potential difference, so that the apparent resistivity value is obtained for each measurement. This method can be used for shallow exploration which has a depth of about 300-1000 m, for example for geothermal exploration. This study aims to identify lithology which includes structure, rock type and thickness of rock layers as well as geothermal systems resulting from data modeling of the shclumberger method in geothermal area. Measurements were carried out in 18 geothermal areas. In each area of the geothermal location, measurements are made with measurement trajectories that vary from 2000 to 4000 meters. text |
| institution |
Institut Teknologi Bandung |
| building |
Institut Teknologi Bandung Library |
| continent |
Asia |
| country |
Indonesia Indonesia |
| content_provider |
Institut Teknologi Bandung |
| collection |
Digital ITB |
| language |
Indonesia |
| description |
The geoelectric method is a method that uses the principle of electric current to investigate the subsurface structure of the earth. This method is done by injecting direct electric current into the earth's surface and then measuring the resulting potential difference, so that the apparent resistivity value is obtained for each measurement. This method can be used for shallow exploration which has a depth of about 300-1000 m, for example for geothermal exploration. This study aims to identify lithology which includes structure, rock type and thickness of rock layers as well as geothermal systems resulting from data modeling of the shclumberger method in geothermal area. Measurements were carried out in 18 geothermal areas. In each area of the geothermal location, measurements are made with measurement trajectories that vary from 2000 to 4000 meters. |
| format |
Final Project |
| author |
De Surya, Ramadhyan |
| spellingShingle |
De Surya, Ramadhyan 1D AND 2D INVERSION OF GEOELECTRICAL DATA FOR GEOTHERMAL EXPLORATION |
| author_facet |
De Surya, Ramadhyan |
| author_sort |
De Surya, Ramadhyan |
| title |
1D AND 2D INVERSION OF GEOELECTRICAL DATA FOR GEOTHERMAL EXPLORATION |
| title_short |
1D AND 2D INVERSION OF GEOELECTRICAL DATA FOR GEOTHERMAL EXPLORATION |
| title_full |
1D AND 2D INVERSION OF GEOELECTRICAL DATA FOR GEOTHERMAL EXPLORATION |
| title_fullStr |
1D AND 2D INVERSION OF GEOELECTRICAL DATA FOR GEOTHERMAL EXPLORATION |
| title_full_unstemmed |
1D AND 2D INVERSION OF GEOELECTRICAL DATA FOR GEOTHERMAL EXPLORATION |
| title_sort |
1d and 2d inversion of geoelectrical data for geothermal exploration |
| url |
https://digilib.itb.ac.id/gdl/view/65417 |
| _version_ |
1822004847549874176 |