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The earth subsurface resistivity structure has been modelled by using ABIC minimization inversion method. Firstly, the subsurface resistivity values are deduced <br /> <br /> <br /> <br /> <br /> from electric and magnetic field collected using magnetotelluric...

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Main Author: PUTRADIPURA (NIM : 10211070); Pembimbing : Wahyu Srigutomo, Ph.D, EDDO
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/20054
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:20054
spelling id-itb.:200542017-09-27T11:45:18Z#TITLE_ALTERNATIVE# PUTRADIPURA (NIM : 10211070); Pembimbing : Wahyu Srigutomo, Ph.D, EDDO Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/20054 The earth subsurface resistivity structure has been modelled by using ABIC minimization inversion method. Firstly, the subsurface resistivity values are deduced <br /> <br /> <br /> <br /> <br /> from electric and magnetic field collected using magnetotelluric method on the desired measured point. Magnetotelluric method is a geophysical tool that utilizes natural electromagnetic field induction to image the earth subsurface based on its electrical conductivity value. After the data has been collected, inversion process then carried out and resulting in resistivity subsurface model in respect with earth depth. The ABIC (Akaike Bayesian Information Criterion) minimization inversion method in magnetotelluric case is a non-linear inversion method that is approached linearly with smoothness added constraint. However, determining the smoothness constraint parameter in this inversion method for every each iteration is based on the ABIC index that derived from Bayes' theorem and maximum entropy theorem. This inversion method works well for both synthetic and real data. 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 earth subsurface resistivity structure has been modelled by using ABIC minimization inversion method. Firstly, the subsurface resistivity values are deduced <br /> <br /> <br /> <br /> <br /> from electric and magnetic field collected using magnetotelluric method on the desired measured point. Magnetotelluric method is a geophysical tool that utilizes natural electromagnetic field induction to image the earth subsurface based on its electrical conductivity value. After the data has been collected, inversion process then carried out and resulting in resistivity subsurface model in respect with earth depth. The ABIC (Akaike Bayesian Information Criterion) minimization inversion method in magnetotelluric case is a non-linear inversion method that is approached linearly with smoothness added constraint. However, determining the smoothness constraint parameter in this inversion method for every each iteration is based on the ABIC index that derived from Bayes' theorem and maximum entropy theorem. This inversion method works well for both synthetic and real data.
format Final Project
author PUTRADIPURA (NIM : 10211070); Pembimbing : Wahyu Srigutomo, Ph.D, EDDO
spellingShingle PUTRADIPURA (NIM : 10211070); Pembimbing : Wahyu Srigutomo, Ph.D, EDDO
#TITLE_ALTERNATIVE#
author_facet PUTRADIPURA (NIM : 10211070); Pembimbing : Wahyu Srigutomo, Ph.D, EDDO
author_sort PUTRADIPURA (NIM : 10211070); Pembimbing : Wahyu Srigutomo, Ph.D, EDDO
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/20054
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