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Geophysical methods can not be separated from how to interpret the image of the subsurface. One of the geophysical methods used to determine the subsurface resistivity distribution is CSAMT (Control Source Audio-Frequency Magneto- telluric). CSAMT is an electromagnetic method that using a grounded e...

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Main Author: WANA ( NIM 10205011) pembimbing Dr. Eng. Enjang Jaenal Mustopa, CANDRA
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/15216
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:15216
spelling id-itb.:152162017-09-27T11:45:15Z#TITLE_ALTERNATIVE# WANA ( NIM 10205011) pembimbing Dr. Eng. Enjang Jaenal Mustopa, CANDRA Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/15216 Geophysical methods can not be separated from how to interpret the image of the subsurface. One of the geophysical methods used to determine the subsurface resistivity distribution is CSAMT (Control Source Audio-Frequency Magneto- telluric). CSAMT is an electromagnetic method that using a grounded electric dipole source. In interpreting the subsurface resistivity distribution is necessary to build the scheme forward modeling and inversion. 1d forward modeling scheme using a horizontally layered earth model and the inversion of 1d using Occam optimization. <br /> 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 Geophysical methods can not be separated from how to interpret the image of the subsurface. One of the geophysical methods used to determine the subsurface resistivity distribution is CSAMT (Control Source Audio-Frequency Magneto- telluric). CSAMT is an electromagnetic method that using a grounded electric dipole source. In interpreting the subsurface resistivity distribution is necessary to build the scheme forward modeling and inversion. 1d forward modeling scheme using a horizontally layered earth model and the inversion of 1d using Occam optimization. <br />
format Final Project
author WANA ( NIM 10205011) pembimbing Dr. Eng. Enjang Jaenal Mustopa, CANDRA
spellingShingle WANA ( NIM 10205011) pembimbing Dr. Eng. Enjang Jaenal Mustopa, CANDRA
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author_facet WANA ( NIM 10205011) pembimbing Dr. Eng. Enjang Jaenal Mustopa, CANDRA
author_sort WANA ( NIM 10205011) pembimbing Dr. Eng. Enjang Jaenal Mustopa, CANDRA
title #TITLE_ALTERNATIVE#
title_short #TITLE_ALTERNATIVE#
title_full #TITLE_ALTERNATIVE#
title_fullStr #TITLE_ALTERNATIVE#
title_full_unstemmed #TITLE_ALTERNATIVE#
title_sort #title_alternative#
url https://digilib.itb.ac.id/gdl/view/15216
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