IDENTIFICATION, CHARACTERIZATION AND VOLUMETRIC ESTIMATION OF DELTAIC RESERVOIR ON LOWER MAIN ZONE UTARI GAS FIELD, KUTAI BASIN, EAST KALIMANTAN
Kutai Basin is one of the largest hydrocarbon producing basin in Indonesia, with an estimated area of around 60.000 km2 and filled with Tertiary sedimentary deposit around 14 km thick. Utari field is one of the fields located on Kutai Basin, and is the biggest gas field in Indonesia. It is locate...
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Format: | Final Project |
Language: | Indonesia |
Subjects: | |
Online Access: | https://digilib.itb.ac.id/gdl/view/33639 |
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Institution: | Institut Teknologi Bandung |
Language: | Indonesia |
Summary: | Kutai Basin is one of the largest hydrocarbon producing basin in Indonesia, with an
estimated area of around 60.000 km2 and filled with Tertiary sedimentary deposit around 14
km thick. Utari field is one of the fields located on Kutai Basin, and is the biggest gas field in
Indonesia. It is located on the median axis of the Mahakam Delta. Utari Field has an anticline
axis trending NE-SW, which forms a structural and stratigraphic trap for this field petroleum
system. Generally, reservoirs on this field is found as deltaic deposit such as channels and
bars.
The aim of this study is to go beyond normal targets and identify reservoir on the
Lower Main Zone (N15-N14) which is located on the lower part of the deltaic petroleum
system as an advanced exploration effort on the Utari Field. This exploration is done by using
seismic data and exploration wells on the Central and North-West area. The result of
geometry identification using seismic amplitude shows that there are 2 types of sedimentary
bodies on this study area, which are distributary channels and mouth bars.
Based on analysis of exploration well data, it is known that there is a potential mature
source rock (Tmax ~440o & VR ~0,9%) consisting of a mixed type II kerogen and type III
kerogen. Furthermore, a depth map is made on the research area which is then correlated to
the depth of source rock maturity so that the potential kitchen of this reservoir are can be
estimated. Based on the analysis, it is found that the potential kitchen area of this reservoir is
located on the eastern area of Utari Field, so the reservoir can be charged from the syncline
on this area, with an estimated fluid in form of wet gas.
To estimate the volumetric of this reservoir, a reservoir characteristic analogue is
analyzed based from the reservoirs of an exploration well located on a bar facies. This
marginal levee analogue shows several characteristics ( ? =0.085 & Sw=0.86), which can be
used to assume the characteristics on the channel itself ( ? =0.12 & Sw=0.42). Finally, these
characteristics are used to calculate the volumetric estimation of the reservoir, with the
biggest reservoir containing approximately 12.98 BCF of initial gas in place. |
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