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Geoelectric resistivity method is a geophysical method commonly used in the interpretation of the subsurface by injecting an electric current down the surface to obtain information about the distribution of the value of resistivity of the rock. This study aims to identify the structure of a quartz v...

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Main Author: (NIM : 90213024), FIRMAN
Format: Theses
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/27358
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:27358
spelling id-itb.:273582018-02-21T11:23:12Z#TITLE_ALTERNATIVE# (NIM : 90213024), FIRMAN Indonesia Theses INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/27358 Geoelectric resistivity method is a geophysical method commonly used in the interpretation of the subsurface by injecting an electric current down the surface to obtain information about the distribution of the value of resistivity of the rock. This study aims to identify the structure of a quartz vein (vein) which is thought to contain gold mineral at the location x. Measurements carried out as many as three tracks with electrodes spaced 5 meters, each 75 meters long, and the penetration depth of 15 meters from surface. Results obtained from the data processing is done with a software tool Res2dinv the form of a cross <br /> <br /> section 2D resistivity. From the data processing is seen that possible zonasilification as quartz vein (vein) and is thought to contain gold mineral found at an elevation of 602-610 meters . While the 3D model of the interpolated trajectory I and II shown that uric guess shaped Massive Vein. 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 Geoelectric resistivity method is a geophysical method commonly used in the interpretation of the subsurface by injecting an electric current down the surface to obtain information about the distribution of the value of resistivity of the rock. This study aims to identify the structure of a quartz vein (vein) which is thought to contain gold mineral at the location x. Measurements carried out as many as three tracks with electrodes spaced 5 meters, each 75 meters long, and the penetration depth of 15 meters from surface. Results obtained from the data processing is done with a software tool Res2dinv the form of a cross <br /> <br /> section 2D resistivity. From the data processing is seen that possible zonasilification as quartz vein (vein) and is thought to contain gold mineral found at an elevation of 602-610 meters . While the 3D model of the interpolated trajectory I and II shown that uric guess shaped Massive Vein.
format Theses
author (NIM : 90213024), FIRMAN
spellingShingle (NIM : 90213024), FIRMAN
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author_facet (NIM : 90213024), FIRMAN
author_sort (NIM : 90213024), FIRMAN
title #TITLE_ALTERNATIVE#
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url https://digilib.itb.ac.id/gdl/view/27358
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