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Palembang northwest area very significant because there are located back arc basin formed by activity tectonic. Geology structure subsurface in this area are influence by sedimentation process an role as hydrocarbon sheal or line magma intrution with association mineral.<p>Total Bouguer Anomal...

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Main Author: SOTA (NIM 22306003); Pembimbing: Dr. Wawan Gunawan A. Kadir, IBRAHIM
Format: Theses
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/13537
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:13537
spelling id-itb.:135372012-02-16T11:34:49Z#TITLE_ALTERNATIVE# SOTA (NIM 22306003); Pembimbing: Dr. Wawan Gunawan A. Kadir, IBRAHIM Indonesia Theses INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/13537 Palembang northwest area very significant because there are located back arc basin formed by activity tectonic. Geology structure subsurface in this area are influence by sedimentation process an role as hydrocarbon sheal or line magma intrution with association mineral.<p>Total Bouguer Anomaly that obtained from gravity data, filtering with moving average that indirectly to get anomaly value residual. Second derivative vertical applying to anomaly residual determines fault kind and location of contact area between two mass densities. Modeling two dimensions (2D) and three dimensions (3D) that conducted to anomaly residual to shown contrast distribution densitas and existence struktur geology subsurface. <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 Palembang northwest area very significant because there are located back arc basin formed by activity tectonic. Geology structure subsurface in this area are influence by sedimentation process an role as hydrocarbon sheal or line magma intrution with association mineral.<p>Total Bouguer Anomaly that obtained from gravity data, filtering with moving average that indirectly to get anomaly value residual. Second derivative vertical applying to anomaly residual determines fault kind and location of contact area between two mass densities. Modeling two dimensions (2D) and three dimensions (3D) that conducted to anomaly residual to shown contrast distribution densitas and existence struktur geology subsurface. <br />
format Theses
author SOTA (NIM 22306003); Pembimbing: Dr. Wawan Gunawan A. Kadir, IBRAHIM
spellingShingle SOTA (NIM 22306003); Pembimbing: Dr. Wawan Gunawan A. Kadir, IBRAHIM
#TITLE_ALTERNATIVE#
author_facet SOTA (NIM 22306003); Pembimbing: Dr. Wawan Gunawan A. Kadir, IBRAHIM
author_sort SOTA (NIM 22306003); Pembimbing: Dr. Wawan Gunawan A. Kadir, IBRAHIM
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/13537
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