GEOLOGY AND MODELING OF RESERVOIR BATUGAMPING FOR TACIPI FORMATION, FTH FIELD, SENGKANG SULAWESI, SOUTH SULAWESI

FTH Field is located in Sengkang Basin, the eastern part of South Sulawesi Province, with 154,3 km2 of area bordered by Walanae fault in the west, separating it from the West Sengkang Basin. The purposes of this study are to identify geological setting and the characteristics of limestone reservoir...

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Main Author: MUBINA , M.FATHAN
Format: Final Project
Language:Indonesia
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Online Access:https://digilib.itb.ac.id/gdl/view/28884
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:28884
spelling id-itb.:288842018-08-02T15:36:09ZGEOLOGY AND MODELING OF RESERVOIR BATUGAMPING FOR TACIPI FORMATION, FTH FIELD, SENGKANG SULAWESI, SOUTH SULAWESI MUBINA , M.FATHAN Geologi, hidrologi & meteorologi Indonesia Final Project limestone, Tacipi Formation, depositional facies, modeling, gas reserve INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/28884 FTH Field is located in Sengkang Basin, the eastern part of South Sulawesi Province, with 154,3 km2 of area bordered by Walanae fault in the west, separating it from the West Sengkang Basin. The purposes of this study are to identify geological setting and the characteristics of limestone reservoir of Tacipi Formation, and calculate hydrocarbon in place reserve. The focus of the study is within the limestone reservoir interval of Tacipi Formation using well data and seismic data processed through seismic interpretation, depositional facies analysis, and petrophysical analysis. The processed data is then used in the modeling of facies and petrophysical properties. Based on well data, the stratigraphy of the study area, from the oldest to the youngest, consists of Camba Formation, Tacipi Formation, and Walanae Formation. The evolution of the basin is affected by the collision in the west of Sulawesi during Miosen until Pliocene, forming reverse faults in the west and east of FTH field. The limestone of Tacipi Formation is a gas-bearing reservoir deposited on isolated carbonate platform during Late Miocene, together with the subsidence of the basin during deposition. The reservoir is reef limestone which depositional facies is classified into reefal, reef debris, and lagoonal. Petrophysical analysis results in the average volume of shale as 21%, porosity as 24%, and water saturation as 54%. Volumetric gas reserve is calculated through the three areas penetrated by wells resulting in 276 BSCF of gas. The lead area is decided, located in the northern part of the study area with 456 BSCF of estimated reserve. 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
MUBINA , M.FATHAN
GEOLOGY AND MODELING OF RESERVOIR BATUGAMPING FOR TACIPI FORMATION, FTH FIELD, SENGKANG SULAWESI, SOUTH SULAWESI
description FTH Field is located in Sengkang Basin, the eastern part of South Sulawesi Province, with 154,3 km2 of area bordered by Walanae fault in the west, separating it from the West Sengkang Basin. The purposes of this study are to identify geological setting and the characteristics of limestone reservoir of Tacipi Formation, and calculate hydrocarbon in place reserve. The focus of the study is within the limestone reservoir interval of Tacipi Formation using well data and seismic data processed through seismic interpretation, depositional facies analysis, and petrophysical analysis. The processed data is then used in the modeling of facies and petrophysical properties. Based on well data, the stratigraphy of the study area, from the oldest to the youngest, consists of Camba Formation, Tacipi Formation, and Walanae Formation. The evolution of the basin is affected by the collision in the west of Sulawesi during Miosen until Pliocene, forming reverse faults in the west and east of FTH field. The limestone of Tacipi Formation is a gas-bearing reservoir deposited on isolated carbonate platform during Late Miocene, together with the subsidence of the basin during deposition. The reservoir is reef limestone which depositional facies is classified into reefal, reef debris, and lagoonal. Petrophysical analysis results in the average volume of shale as 21%, porosity as 24%, and water saturation as 54%. Volumetric gas reserve is calculated through the three areas penetrated by wells resulting in 276 BSCF of gas. The lead area is decided, located in the northern part of the study area with 456 BSCF of estimated reserve.
format Final Project
author MUBINA , M.FATHAN
author_facet MUBINA , M.FATHAN
author_sort MUBINA , M.FATHAN
title GEOLOGY AND MODELING OF RESERVOIR BATUGAMPING FOR TACIPI FORMATION, FTH FIELD, SENGKANG SULAWESI, SOUTH SULAWESI
title_short GEOLOGY AND MODELING OF RESERVOIR BATUGAMPING FOR TACIPI FORMATION, FTH FIELD, SENGKANG SULAWESI, SOUTH SULAWESI
title_full GEOLOGY AND MODELING OF RESERVOIR BATUGAMPING FOR TACIPI FORMATION, FTH FIELD, SENGKANG SULAWESI, SOUTH SULAWESI
title_fullStr GEOLOGY AND MODELING OF RESERVOIR BATUGAMPING FOR TACIPI FORMATION, FTH FIELD, SENGKANG SULAWESI, SOUTH SULAWESI
title_full_unstemmed GEOLOGY AND MODELING OF RESERVOIR BATUGAMPING FOR TACIPI FORMATION, FTH FIELD, SENGKANG SULAWESI, SOUTH SULAWESI
title_sort geology and modeling of reservoir batugamping for tacipi formation, fth field, sengkang sulawesi, south sulawesi
url https://digilib.itb.ac.id/gdl/view/28884
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