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Abstract : <br /> <br /> <br /> <br /> <br /> Seismic data is generated by waves propagating through a subsurface. The image that is obtained in this process is a distorted image that does not correctly reflect the true geometry of the subsurface structure. The mig...

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Main Author: Triyoso (NIM 102 03 021), Kaswandhi
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/6350
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:6350
spelling id-itb.:63502017-09-27T11:45:09Z#TITLE_ALTERNATIVE# Triyoso (NIM 102 03 021), Kaswandhi Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/6350 Abstract : <br /> <br /> <br /> <br /> <br /> Seismic data is generated by waves propagating through a subsurface. The image that is obtained in this process is a distorted image that does not correctly reflect the true geometry of the subsurface structure. The migration process removes this wave propagation effect and as a result seismic events move to their correct subsurface position. Several migration methods are used to obtain the best result that is reflects the true geometry of the subsurface structure. This final project present a technique which is very popular used in migration of seismic data, known as Kirchhoff pre-stack depth migration (PSDM). The goal of pre-stack depth migration is building velocity model. Even in sparse seismic data, Kirchhoff pre-stack depth migration with good velocity model could image seismic data accurate enough with less time consuming. <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 Abstract : <br /> <br /> <br /> <br /> <br /> Seismic data is generated by waves propagating through a subsurface. The image that is obtained in this process is a distorted image that does not correctly reflect the true geometry of the subsurface structure. The migration process removes this wave propagation effect and as a result seismic events move to their correct subsurface position. Several migration methods are used to obtain the best result that is reflects the true geometry of the subsurface structure. This final project present a technique which is very popular used in migration of seismic data, known as Kirchhoff pre-stack depth migration (PSDM). The goal of pre-stack depth migration is building velocity model. Even in sparse seismic data, Kirchhoff pre-stack depth migration with good velocity model could image seismic data accurate enough with less time consuming. <br />
format Final Project
author Triyoso (NIM 102 03 021), Kaswandhi
spellingShingle Triyoso (NIM 102 03 021), Kaswandhi
#TITLE_ALTERNATIVE#
author_facet Triyoso (NIM 102 03 021), Kaswandhi
author_sort Triyoso (NIM 102 03 021), Kaswandhi
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/6350
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