GEOLOGI DAN PEMODELAN RESERVOIR FORMASI MUNDU PADA LAPANGAN M, CEKUNGAN JAWA TIMUR UTARA

M Field is a gas field located in the North East Java Basin and covers an area of ±70 km2. The objectives of this study are to determine M Field’s geological setting, to generate static reservoir model, and to estimate initial hydrocarbon in place. The study is focused on limestone reservoir in Mund...

Full description

Saved in:
Bibliographic Details
Main Author: Ika Kirana T, Dinda
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/56598
Tags: Add Tag
No Tags, Be the first to tag this record!
Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:56598
spelling id-itb.:565982021-06-23T12:38:00ZGEOLOGI DAN PEMODELAN RESERVOIR FORMASI MUNDU PADA LAPANGAN M, CEKUNGAN JAWA TIMUR UTARA Ika Kirana T, Dinda Indonesia Final Project M Field, Mundu Formation, North East Java Basin, reservoir modelling, hydrocarbon estimation INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/56598 M Field is a gas field located in the North East Java Basin and covers an area of ±70 km2. The objectives of this study are to determine M Field’s geological setting, to generate static reservoir model, and to estimate initial hydrocarbon in place. The study is focused on limestone reservoir in Mundu Formation. The dataset used in this study includes wireline log of 2 wells, 3D seismic data, mudlog data of 4 horizontal wells, and the report of sidewall core description data. The methods used in this study consist of four evaluation methods, which are: well data analysis by doing well-to-well correlation and petrophysical analysis; seismic data analysis by generating depth structure map and interpreting reservoir geometry; the integration of well data and seismic data; reservoir modelling by generating 3D structure model, generating petrophysical model, determining fluid contact, and estimating initial hydrocarbon in place. The results of these methods are the stratigraphy and structure of M Field which are derived from integration of well data and seismic data. Main structure of M Field is a west southwest – east shoutheast trending anticline associated with north – south trending normal faults suspected to be the manifestation of negative flower structure that possibly related to Sakala strike-slip fault system. The reservoir interval is limestone with varied thickness between 22–47 metres and deposited in the outer shelf of a non-rimmed carbonate shelf. The initial gas in place estimation of the reservoir is 399.2 BSCF. 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 M Field is a gas field located in the North East Java Basin and covers an area of ±70 km2. The objectives of this study are to determine M Field’s geological setting, to generate static reservoir model, and to estimate initial hydrocarbon in place. The study is focused on limestone reservoir in Mundu Formation. The dataset used in this study includes wireline log of 2 wells, 3D seismic data, mudlog data of 4 horizontal wells, and the report of sidewall core description data. The methods used in this study consist of four evaluation methods, which are: well data analysis by doing well-to-well correlation and petrophysical analysis; seismic data analysis by generating depth structure map and interpreting reservoir geometry; the integration of well data and seismic data; reservoir modelling by generating 3D structure model, generating petrophysical model, determining fluid contact, and estimating initial hydrocarbon in place. The results of these methods are the stratigraphy and structure of M Field which are derived from integration of well data and seismic data. Main structure of M Field is a west southwest – east shoutheast trending anticline associated with north – south trending normal faults suspected to be the manifestation of negative flower structure that possibly related to Sakala strike-slip fault system. The reservoir interval is limestone with varied thickness between 22–47 metres and deposited in the outer shelf of a non-rimmed carbonate shelf. The initial gas in place estimation of the reservoir is 399.2 BSCF.
format Final Project
author Ika Kirana T, Dinda
spellingShingle Ika Kirana T, Dinda
GEOLOGI DAN PEMODELAN RESERVOIR FORMASI MUNDU PADA LAPANGAN M, CEKUNGAN JAWA TIMUR UTARA
author_facet Ika Kirana T, Dinda
author_sort Ika Kirana T, Dinda
title GEOLOGI DAN PEMODELAN RESERVOIR FORMASI MUNDU PADA LAPANGAN M, CEKUNGAN JAWA TIMUR UTARA
title_short GEOLOGI DAN PEMODELAN RESERVOIR FORMASI MUNDU PADA LAPANGAN M, CEKUNGAN JAWA TIMUR UTARA
title_full GEOLOGI DAN PEMODELAN RESERVOIR FORMASI MUNDU PADA LAPANGAN M, CEKUNGAN JAWA TIMUR UTARA
title_fullStr GEOLOGI DAN PEMODELAN RESERVOIR FORMASI MUNDU PADA LAPANGAN M, CEKUNGAN JAWA TIMUR UTARA
title_full_unstemmed GEOLOGI DAN PEMODELAN RESERVOIR FORMASI MUNDU PADA LAPANGAN M, CEKUNGAN JAWA TIMUR UTARA
title_sort geologi dan pemodelan reservoir formasi mundu pada lapangan m, cekungan jawa timur utara
url https://digilib.itb.ac.id/gdl/view/56598
_version_ 1822930245232099328