ENVIRONMENTAL DEPOSITION ANALYSIS AND FORMATION EVALUATION INTERVAL FS 1A- SB A, AREA B, DIAR FIELD, CENTRAL SUMATRA BASIN, RIAU, INDONESIA

Diar field is the largest oil field in Riau, Central Sumatra Basin. This field consists of twelve areas, which observation is in Area B for interval FS 1A-SB A in Duri Formation. Objectives of this observation are to determine distribution of architectural facies, environmental deposition of Duri...

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Main Author: Olytia, Lika
Format: Final Project
Language:Indonesia
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Online Access:https://digilib.itb.ac.id/gdl/view/34313
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:34313
spelling id-itb.:343132019-02-07T10:19:21ZENVIRONMENTAL DEPOSITION ANALYSIS AND FORMATION EVALUATION INTERVAL FS 1A- SB A, AREA B, DIAR FIELD, CENTRAL SUMATRA BASIN, RIAU, INDONESIA Olytia, Lika Geologi ekonomi Indonesia Final Project Diar Field, Duri Formation, Central Sumatra Basin, facies association, estuarine channel, formation evaluation INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/34313 Diar field is the largest oil field in Riau, Central Sumatra Basin. This field consists of twelve areas, which observation is in Area B for interval FS 1A-SB A in Duri Formation. Objectives of this observation are to determine distribution of architectural facies, environmental deposition of Duri Formation, and subsurface mapping for reservoir petrophysical properties. The data that have been used for this observation are core, petrography report, biostratigraphy report, and electric log from 233 wells. Based on biostratigraphy report and core analysis, reservoir in FS 1A-SB A was deposited about 20 million years ago in Early Miocene. Core analysis shows that intervals are consists of six sandstone lithofacies are Sbcvf, Sbfvf, Smvf, Smf, Sbvf, Sbf and three claystone-siltstone lithofacies are Fblc, Fbc, and Fm. Distribution analysis of architectural facies is made with stratigraphic correlation that shows this area have Highstand System Tract (HST) and Transgressive System Tract (TST). Based on core analysis, electrofacies distribution, and ichnofossil analysis, the depositional environment is estuarine. The architectural facies are estuarine channel, tidal mud flat, and marine shale with sedimentation trend is NE-SW. Core, XRD, and petrography data analysis on FS 1A-SB A shows that major mineral existed and consisted on rock are from grain and clay group. Clay mineral type which dominates the observation interval is mixed layer illite/smectite. The result of petrophysical analysis from estuarine channel facies for A1 a and A1 b shows that average value for effective porosity is 0,35, average value for effective water saturation is 0,53, average value for permeability is 573 mD, and average value for Vclay is 0,142. For petrophysics result from estuarine channel facies for A2 shows that average value for effective porosity is 0,32, average value for effective water saturation is 0,57, average value for permeability is 409 mD, and average value for Vclay is 0,19. 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
topic Geologi ekonomi
spellingShingle Geologi ekonomi
Olytia, Lika
ENVIRONMENTAL DEPOSITION ANALYSIS AND FORMATION EVALUATION INTERVAL FS 1A- SB A, AREA B, DIAR FIELD, CENTRAL SUMATRA BASIN, RIAU, INDONESIA
description Diar field is the largest oil field in Riau, Central Sumatra Basin. This field consists of twelve areas, which observation is in Area B for interval FS 1A-SB A in Duri Formation. Objectives of this observation are to determine distribution of architectural facies, environmental deposition of Duri Formation, and subsurface mapping for reservoir petrophysical properties. The data that have been used for this observation are core, petrography report, biostratigraphy report, and electric log from 233 wells. Based on biostratigraphy report and core analysis, reservoir in FS 1A-SB A was deposited about 20 million years ago in Early Miocene. Core analysis shows that intervals are consists of six sandstone lithofacies are Sbcvf, Sbfvf, Smvf, Smf, Sbvf, Sbf and three claystone-siltstone lithofacies are Fblc, Fbc, and Fm. Distribution analysis of architectural facies is made with stratigraphic correlation that shows this area have Highstand System Tract (HST) and Transgressive System Tract (TST). Based on core analysis, electrofacies distribution, and ichnofossil analysis, the depositional environment is estuarine. The architectural facies are estuarine channel, tidal mud flat, and marine shale with sedimentation trend is NE-SW. Core, XRD, and petrography data analysis on FS 1A-SB A shows that major mineral existed and consisted on rock are from grain and clay group. Clay mineral type which dominates the observation interval is mixed layer illite/smectite. The result of petrophysical analysis from estuarine channel facies for A1 a and A1 b shows that average value for effective porosity is 0,35, average value for effective water saturation is 0,53, average value for permeability is 573 mD, and average value for Vclay is 0,142. For petrophysics result from estuarine channel facies for A2 shows that average value for effective porosity is 0,32, average value for effective water saturation is 0,57, average value for permeability is 409 mD, and average value for Vclay is 0,19.
format Final Project
author Olytia, Lika
author_facet Olytia, Lika
author_sort Olytia, Lika
title ENVIRONMENTAL DEPOSITION ANALYSIS AND FORMATION EVALUATION INTERVAL FS 1A- SB A, AREA B, DIAR FIELD, CENTRAL SUMATRA BASIN, RIAU, INDONESIA
title_short ENVIRONMENTAL DEPOSITION ANALYSIS AND FORMATION EVALUATION INTERVAL FS 1A- SB A, AREA B, DIAR FIELD, CENTRAL SUMATRA BASIN, RIAU, INDONESIA
title_full ENVIRONMENTAL DEPOSITION ANALYSIS AND FORMATION EVALUATION INTERVAL FS 1A- SB A, AREA B, DIAR FIELD, CENTRAL SUMATRA BASIN, RIAU, INDONESIA
title_fullStr ENVIRONMENTAL DEPOSITION ANALYSIS AND FORMATION EVALUATION INTERVAL FS 1A- SB A, AREA B, DIAR FIELD, CENTRAL SUMATRA BASIN, RIAU, INDONESIA
title_full_unstemmed ENVIRONMENTAL DEPOSITION ANALYSIS AND FORMATION EVALUATION INTERVAL FS 1A- SB A, AREA B, DIAR FIELD, CENTRAL SUMATRA BASIN, RIAU, INDONESIA
title_sort environmental deposition analysis and formation evaluation interval fs 1a- sb a, area b, diar field, central sumatra basin, riau, indonesia
url https://digilib.itb.ac.id/gdl/view/34313
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