RESERVOIR CHARACTERIZATION AND RESERVE CALCULATION AT SOKA FIELD, MUDA FORMATION, EAST NATUNA BASIN

Soka Field is a gas field located in eastern part of East Natuna Basin. This study conducted within SB1 – SB3 interval of Pliocene – Pleistocene age in Muda Formation. This study aims to understanding Soka Field’s geological configuration especially in study’s interval, identifying facies, facies as...

Full description

Saved in:
Bibliographic Details
Main Author: Verdinov Simanjuntak, Marchel
Format: Final Project
Language:Indonesia
Subjects:
Online Access:https://digilib.itb.ac.id/gdl/view/63765
Tags: Add Tag
No Tags, Be the first to tag this record!
Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:63765
spelling id-itb.:637652022-03-04T13:59:22ZRESERVOIR CHARACTERIZATION AND RESERVE CALCULATION AT SOKA FIELD, MUDA FORMATION, EAST NATUNA BASIN Verdinov Simanjuntak, Marchel Geologi, hidrologi & meteorologi Indonesia Final Project East Natuna Basin, Muda Formation, facies and association facies, sequence stratigraphy, petrophysics, hydrocarbon in-place estimation. INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/63765 Soka Field is a gas field located in eastern part of East Natuna Basin. This study conducted within SB1 – SB3 interval of Pliocene – Pleistocene age in Muda Formation. This study aims to understanding Soka Field’s geological configuration especially in study’s interval, identifying facies, facies association, and depositional environment of study’s interval, determining petrophysics property value in every parasequence of study’s interval, and estimating reservoir hydrocarbon in-place of Soka Field. Data used in this study came from four wells (MS-1, MS-2, MS-3, and MS-4) consists of wireline logs, well cutting descriptions, and three dimension that covers all wells. Seismic of study’s area shows several faults of normal faults with northeast – southwest relative direction. Facies and depositional environment yielded ten lithofacies consist of sandstone and claystone. Lithofacies analysis is then matched with electrofacies resulting SB1 – SB3 interval shows four facies association which are offshore transition, lower shoreface, middle shoreface, and upper shoreface deposited in shoreline environment. Sequence stratigraphy analysis shows study’s interval is dominated by coarsening upward parasequence, progradation and retrogradation parasequence set, lowstand system tract, transgressive system tract, and highstand system tract. Petrophysics analysis shows average property value of shale volumes, effective porosity, and water saturation of reservoir 1 is 0,264, 0,308, and 0,860 and reservoir 2 is 0,378, 0,267, and 0,658. Reservoir cut-off property values of shale volumes is at 0,355, effective porosity at 0,233, and water saturation at 0,900. Hydrocarbon in-place estimation results shows gas volumes of reservoir 1 is 70,93 BCF and reservoir 2 is 281,87 BCF with CO2 content in reservoir around 70-80 percent. 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, hidrologi & meteorologi
spellingShingle Geologi, hidrologi & meteorologi
Verdinov Simanjuntak, Marchel
RESERVOIR CHARACTERIZATION AND RESERVE CALCULATION AT SOKA FIELD, MUDA FORMATION, EAST NATUNA BASIN
description Soka Field is a gas field located in eastern part of East Natuna Basin. This study conducted within SB1 – SB3 interval of Pliocene – Pleistocene age in Muda Formation. This study aims to understanding Soka Field’s geological configuration especially in study’s interval, identifying facies, facies association, and depositional environment of study’s interval, determining petrophysics property value in every parasequence of study’s interval, and estimating reservoir hydrocarbon in-place of Soka Field. Data used in this study came from four wells (MS-1, MS-2, MS-3, and MS-4) consists of wireline logs, well cutting descriptions, and three dimension that covers all wells. Seismic of study’s area shows several faults of normal faults with northeast – southwest relative direction. Facies and depositional environment yielded ten lithofacies consist of sandstone and claystone. Lithofacies analysis is then matched with electrofacies resulting SB1 – SB3 interval shows four facies association which are offshore transition, lower shoreface, middle shoreface, and upper shoreface deposited in shoreline environment. Sequence stratigraphy analysis shows study’s interval is dominated by coarsening upward parasequence, progradation and retrogradation parasequence set, lowstand system tract, transgressive system tract, and highstand system tract. Petrophysics analysis shows average property value of shale volumes, effective porosity, and water saturation of reservoir 1 is 0,264, 0,308, and 0,860 and reservoir 2 is 0,378, 0,267, and 0,658. Reservoir cut-off property values of shale volumes is at 0,355, effective porosity at 0,233, and water saturation at 0,900. Hydrocarbon in-place estimation results shows gas volumes of reservoir 1 is 70,93 BCF and reservoir 2 is 281,87 BCF with CO2 content in reservoir around 70-80 percent.
format Final Project
author Verdinov Simanjuntak, Marchel
author_facet Verdinov Simanjuntak, Marchel
author_sort Verdinov Simanjuntak, Marchel
title RESERVOIR CHARACTERIZATION AND RESERVE CALCULATION AT SOKA FIELD, MUDA FORMATION, EAST NATUNA BASIN
title_short RESERVOIR CHARACTERIZATION AND RESERVE CALCULATION AT SOKA FIELD, MUDA FORMATION, EAST NATUNA BASIN
title_full RESERVOIR CHARACTERIZATION AND RESERVE CALCULATION AT SOKA FIELD, MUDA FORMATION, EAST NATUNA BASIN
title_fullStr RESERVOIR CHARACTERIZATION AND RESERVE CALCULATION AT SOKA FIELD, MUDA FORMATION, EAST NATUNA BASIN
title_full_unstemmed RESERVOIR CHARACTERIZATION AND RESERVE CALCULATION AT SOKA FIELD, MUDA FORMATION, EAST NATUNA BASIN
title_sort reservoir characterization and reserve calculation at soka field, muda formation, east natuna basin
url https://digilib.itb.ac.id/gdl/view/63765
_version_ 1822932243853606912