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“X” field is located in area of South Sumatra basin. The target of this research is Talang Akar formation. The Talang Akar formation consist of sandstone, shale, and coal intercalation. Since the sandstone is relatively thin, it will be difucult to determine the sandstone dissemination by only...

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Main Author: FRIADI SINAGA (NIM12306014) pembimbing : Ign.Sonny Winardhi, Ph.D, JAN
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/16158
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:16158
spelling id-itb.:161582017-10-09T10:31:16Z#TITLE_ALTERNATIVE# FRIADI SINAGA (NIM12306014) pembimbing : Ign.Sonny Winardhi, Ph.D, JAN Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/16158 “X” field is located in area of South Sumatra basin. The target of this research is Talang Akar formation. The Talang Akar formation consist of sandstone, shale, and coal intercalation. Since the sandstone is relatively thin, it will be difucult to determine the sandstone dissemination by only using conventional seismic amplitude data. <br /> <br /> <br /> <br /> <br /> <br /> <br /> Based on sensitivity analysis, VpVs ratio parameter is considered to be sensitive in distinguishing sandstone and shale. So, seismic inversion have to be done in order to map the sandstone lithology at “X” field. The kind of inversion used here is simultaneous inversion. <br /> <br /> <br /> <br /> <br /> <br /> <br /> The simultaneous inversion which is done in angle gather domain, produce P- impedance, S-impedance, density and VpVs ratio volumes. The VpVs ratio volume is able to show the location of sandstone lithology 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 “X” field is located in area of South Sumatra basin. The target of this research is Talang Akar formation. The Talang Akar formation consist of sandstone, shale, and coal intercalation. Since the sandstone is relatively thin, it will be difucult to determine the sandstone dissemination by only using conventional seismic amplitude data. <br /> <br /> <br /> <br /> <br /> <br /> <br /> Based on sensitivity analysis, VpVs ratio parameter is considered to be sensitive in distinguishing sandstone and shale. So, seismic inversion have to be done in order to map the sandstone lithology at “X” field. The kind of inversion used here is simultaneous inversion. <br /> <br /> <br /> <br /> <br /> <br /> <br /> The simultaneous inversion which is done in angle gather domain, produce P- impedance, S-impedance, density and VpVs ratio volumes. The VpVs ratio volume is able to show the location of sandstone lithology
format Final Project
author FRIADI SINAGA (NIM12306014) pembimbing : Ign.Sonny Winardhi, Ph.D, JAN
spellingShingle FRIADI SINAGA (NIM12306014) pembimbing : Ign.Sonny Winardhi, Ph.D, JAN
#TITLE_ALTERNATIVE#
author_facet FRIADI SINAGA (NIM12306014) pembimbing : Ign.Sonny Winardhi, Ph.D, JAN
author_sort FRIADI SINAGA (NIM12306014) pembimbing : Ign.Sonny Winardhi, Ph.D, JAN
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/16158
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