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The objectives of this study are to analyze sedimentation facies and Sand distribution based on core data and well log correlation. Sandstones in the study interval can be divided into several litofacies, which are Bioturbated-Fine Sandstone, Paralel lamination-Fine Sandstone, Crosslamination-Medium...

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Main Author: NAFIARISTO HAMDANI (NIM 12007050); Pembimbing: Dr. Ir. Djuhaeni, FIAR
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/13475
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:13475
spelling id-itb.:134752017-09-27T11:46:40Z#TITLE_ALTERNATIVE# NAFIARISTO HAMDANI (NIM 12007050); Pembimbing: Dr. Ir. Djuhaeni, FIAR Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/13475 The objectives of this study are to analyze sedimentation facies and Sand distribution based on core data and well log correlation. Sandstones in the study interval can be divided into several litofacies, which are Bioturbated-Fine Sandstone, Paralel lamination-Fine Sandstone, Crosslamination-Medium Sandstone, Paralel lamination-Coarse Sandstone and Crosslamination - Coarse Sandstone. Based on the litofacies analysis integrated with log data, the study's interval is then divided into three sedimentation facies, which are Meandering low sinousity system facies, Point bar meandering system facies, and Braided Channel facies. All three facies is deposited in fluvial-deltaic environment. 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 objectives of this study are to analyze sedimentation facies and Sand distribution based on core data and well log correlation. Sandstones in the study interval can be divided into several litofacies, which are Bioturbated-Fine Sandstone, Paralel lamination-Fine Sandstone, Crosslamination-Medium Sandstone, Paralel lamination-Coarse Sandstone and Crosslamination - Coarse Sandstone. Based on the litofacies analysis integrated with log data, the study's interval is then divided into three sedimentation facies, which are Meandering low sinousity system facies, Point bar meandering system facies, and Braided Channel facies. All three facies is deposited in fluvial-deltaic environment.
format Final Project
author NAFIARISTO HAMDANI (NIM 12007050); Pembimbing: Dr. Ir. Djuhaeni, FIAR
spellingShingle NAFIARISTO HAMDANI (NIM 12007050); Pembimbing: Dr. Ir. Djuhaeni, FIAR
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author_facet NAFIARISTO HAMDANI (NIM 12007050); Pembimbing: Dr. Ir. Djuhaeni, FIAR
author_sort NAFIARISTO HAMDANI (NIM 12007050); Pembimbing: Dr. Ir. Djuhaeni, FIAR
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/13475
_version_ 1820736197945720832

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