MODELLING 2D RESISTIVITY TO DETERMINE THE DISTRIBUTION AREA OF EPITHERMAL GOLD DEPOSIT IN ‘MILA’ FIELD

For gold deposit exploration, geophysical method has a significant role in identifying the prospective zones. Geophysical methods can be used to map formation’s subsurface structures and its distribution area to locate the mineralization zones that are associated with gold deposits. Gold deposits ar...

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Main Author: Fawwaz, Faris
Format: Final Project
Language:Indonesia
Subjects:
Online Access:https://digilib.itb.ac.id/gdl/view/37026
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:37026
spelling id-itb.:370262019-03-18T13:27:15ZMODELLING 2D RESISTIVITY TO DETERMINE THE DISTRIBUTION AREA OF EPITHERMAL GOLD DEPOSIT IN ‘MILA’ FIELD Fawwaz, Faris Pertambangan dan operasi berkaitan Indonesia Final Project resistivity method, epithermal gold deposit, Pani, gold, inversion INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/37026 For gold deposit exploration, geophysical method has a significant role in identifying the prospective zones. Geophysical methods can be used to map formation’s subsurface structures and its distribution area to locate the mineralization zones that are associated with gold deposits. Gold deposits are indicated by the silicification zones related to the process of alterations. These zones tend to have higher resistivity compared to the surrounding area. One of the geophysical methods that can be used to map the gold mineralization zones is resistivity method. This method measures the potential difference by injecting electrical current into the ground through a pair of electrodes. From this measurement, variation of electrical potential difference will indicate resistivity variation that carries information regarding the structures and materials in which the current flows through. This principle assumes that earth’s material has resistive properties similar to resistors where the materials have different ability to conduct electrical current. This research takes place in MILA field located in Pani, north arm of the Sulawesi (Celebes) Island, using the Zonge series instrument with dipole-dipole electrode configurations. The survey was conducted on 9 East-West line with distance between line is 100 m and electrode distance is 50 m. After the acquisition, 2D modelling and 3D imaging of subsurface resistivity modelling is carried out. Then, the interpretation of the resulting 2D model and 3D image are performed. The final result of this research is the area of gold deposit’s distribution zones that is located in two separate zone, first on the middle area of research locations spread to the south and narrowing to the northwest and second to the northeast of the study areas. 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
topic Pertambangan dan operasi berkaitan
spellingShingle Pertambangan dan operasi berkaitan
Fawwaz, Faris
MODELLING 2D RESISTIVITY TO DETERMINE THE DISTRIBUTION AREA OF EPITHERMAL GOLD DEPOSIT IN ‘MILA’ FIELD
description For gold deposit exploration, geophysical method has a significant role in identifying the prospective zones. Geophysical methods can be used to map formation’s subsurface structures and its distribution area to locate the mineralization zones that are associated with gold deposits. Gold deposits are indicated by the silicification zones related to the process of alterations. These zones tend to have higher resistivity compared to the surrounding area. One of the geophysical methods that can be used to map the gold mineralization zones is resistivity method. This method measures the potential difference by injecting electrical current into the ground through a pair of electrodes. From this measurement, variation of electrical potential difference will indicate resistivity variation that carries information regarding the structures and materials in which the current flows through. This principle assumes that earth’s material has resistive properties similar to resistors where the materials have different ability to conduct electrical current. This research takes place in MILA field located in Pani, north arm of the Sulawesi (Celebes) Island, using the Zonge series instrument with dipole-dipole electrode configurations. The survey was conducted on 9 East-West line with distance between line is 100 m and electrode distance is 50 m. After the acquisition, 2D modelling and 3D imaging of subsurface resistivity modelling is carried out. Then, the interpretation of the resulting 2D model and 3D image are performed. The final result of this research is the area of gold deposit’s distribution zones that is located in two separate zone, first on the middle area of research locations spread to the south and narrowing to the northwest and second to the northeast of the study areas.
format Final Project
author Fawwaz, Faris
author_facet Fawwaz, Faris
author_sort Fawwaz, Faris
title MODELLING 2D RESISTIVITY TO DETERMINE THE DISTRIBUTION AREA OF EPITHERMAL GOLD DEPOSIT IN ‘MILA’ FIELD
title_short MODELLING 2D RESISTIVITY TO DETERMINE THE DISTRIBUTION AREA OF EPITHERMAL GOLD DEPOSIT IN ‘MILA’ FIELD
title_full MODELLING 2D RESISTIVITY TO DETERMINE THE DISTRIBUTION AREA OF EPITHERMAL GOLD DEPOSIT IN ‘MILA’ FIELD
title_fullStr MODELLING 2D RESISTIVITY TO DETERMINE THE DISTRIBUTION AREA OF EPITHERMAL GOLD DEPOSIT IN ‘MILA’ FIELD
title_full_unstemmed MODELLING 2D RESISTIVITY TO DETERMINE THE DISTRIBUTION AREA OF EPITHERMAL GOLD DEPOSIT IN ‘MILA’ FIELD
title_sort modelling 2d resistivity to determine the distribution area of epithermal gold deposit in ‘mila’ field
url https://digilib.itb.ac.id/gdl/view/37026
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