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8122019 IPA12-G-095
httpslidepdfcomreaderfullipa12-g-095 18
IPA12-G-095
PROCEEDINGS INDONESIAN PETROLEUM ASSOCIATION
Thirty-Sixth Annual Convention amp Exhibition May 2012
SUCCESS STORY WITH LOW RESISTIVITY SAND IN AN EXPLORATION BLOCK
WESTERN EDGE OF CENTRAL SUMATRAN BASIN
Heri Setiawan
Panca Widiantoro
Hendarman
Made Primaryanta
ABSTRACT
The exploration area of focus for this study is
located at the western edge of the Central Sumatran
Basin Three exploration wells were drilled to 6500
ft (MD) The wells discovered oil in the Early
Miocene Lower Sihapas Formation estuarine
sandstone The gross reservoir interval was up to
140 ft thick exhibiting low resistivity typically
between 6 ndash 8 Ohm meters Each well tested up to
3000 BOPD of 44 API oil with zero water and
minimal gas The resistivity of the Lower Sihapas
oil-filled sands is lower than the resistivity of
underlying Upper Pematang water-filled sands
This paper will explain the exploration and
development strategy for these low-resistivitysands which can be applied to other similar areas
Keywords Success story low resistivity zone
exploration block Central Sumatran Basin
INTRODUCTION
This exploration block is located at the Western
Edge of the Central Sumatran Basin (Figure 1) The
Central Sumatran Basin is one of a series of rift
basins that occupy a back-arc position along the
leading edge of Sundaland It is the most prolific oil
producing basin in Indonesia
Three exploration wells drilled in the same structure
all discovered oil in the Lower Sihapas Formation
which is a prolific reservoir in the Central Sumatran
Basin The Lower Sihapas Formation comprises
siliciclastic sediments deposited in an estuarine
environment Tidal influence is confirmed from
conventional core sedimentologic structures such as
ripple current shale drapes cross lamination and
wavy lamination in Well-X
Mosesa Petroleum
The resistivity of the Lower Sihapas oil-filled sands
is lower than the resistivity of underlying Upper
Pematang water-filled sands Fluid type in the
sands is confirmed from cuttings MDT samples and
well-tests
This paper will discuss the causes of low and high
resistivities in sands formation pressures fluid
sampling petrophysical estimates and the
exploration and development strategy applicable to
this field and perhaps to similar fields
METHODOLOGY
We analysed data from mud-logs wireline logs
formation pressures fluid samples cores and production tests to understand the cause of low
resistivity in oil sands and high resistivity in water
sands This improved our choice of parameters for
petrophysical calculations and helped to define the
exploration and development strategy in this field
RESULTS
a Drilling Result Review
In May 2011 exploration wells Well-X and Well-Y
were drilled in the Z structure Oil in Zone A was
inferred from cuttings and sidewall cores (poor to
moderate oil shows) and from MDT samples
(100 oil with 440
API) See Figure 2 and Figure
3 Conventional core was cut in Zone A in Well-X
with 87 recovery
Slab core fluorescence photographs (Figure 4) show
that Zone A has poor-moderate oil shows Routine
core analysis revealed porosity in the range of 12-22
permeability in the range of 17-1700 md
Special core analysis (SCAL) was performed to
determine petrophysical parameters relative
permeability and capillary pressure
Water saturation derived from SCAL was in the
range of 20-30 Unusually resistivity in the
Back to Session
8122019 IPA12-G-095
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Zone A oil sand was lower than in the underlying
Zone B water sand (water proved from cuttings
sidewall cores and MDT sample with 100 water
saturation)
b Pressure Analysis
Formation pressure tests and fluid samples were
taken in both wells Figure 5 shows the pressure
gradients in Zone A and Zone B in Well X The
Zone A fluid gradient of 0328 psift is consistent
with an oil-bearing zone The Zone B fluid gradient
of 041 psift is consistent with a water-bearing
zone The fluid analyzer results in Figure 6 showed
agreement between the inferred fluid type during
sampling and actual fluid type confirmed when the
sample was opened at surface
c Low and High resistivity values
Low resistivity in hydrocarbon-filled sand can be
caused by dispersed shale andor laminated shale
Shale decreases resistivity because it contains
bound water
XRD data from conventional core in Well-X in
Table 1 shows that Zone A contains clay minerals
such as illite kaolinite and glauconite comprising
over 10 of the total minerals
High resistivity in water-filled sands can be caused by the presence of fresh formation water The
salinity of water samples from Zone B was low at
1000-2000 ppm The water may be meteoric water
flushed from outcrops on the south-western edge of
the Central Sumatran Basin
d Petrophysical analysis
The petrophysical analysis in Figure 7 had to
accommodate the presence of clay minerals in both
dispersed and laminated shale that caused low
resistivity
Petrophysical parameters
Petrophysical parameters were determined from log
and core analysis Water density and matrix density
came from cross plots of bulk density and core
porosity after NOB correction To calculate the total
porosity of shale The wet shale density log and the
neutron log response in shale was cross-plotted
The dry shale density was inferred from the
dominant clay determined from XRD data
Water saturation parameters a m and n came from
SCAL data a and m from a cross plot of core
porosity and formation water and n from a cross
plot of brine saturation and formation resistivity
Vshale
Vshale was calculated from the Gamma Ray log
with the Clavier (1971) method to account for the
mineral response Vshale results from the Clavier
method was compared to Vshale results from the
XRD data
Porosity
Porosity can be calculated from neutron density
and sonic logs with either the single porosity
method and combined porosity method We used
the combined method of neutron and density
porosity and calibrated the result to core porosity
Water Resistivity
Water resistivity came from the Picket plot of RT
and effective porosity as water was not found in
this zone Water is assumed to be bound water
trapped in shale
Water Saturation
As the shale volume is 3-40 and the lithology is
dispersed and laminated shale and sand theModified Simandoux equation was used to
accommodate the presence of clay minerals in both
Water saturation indicated from the Simandoux
modified method was high at 50-70 which for
sand with good porosity and permeability is
inconsistent with the test result of zero water cut
Water saturation from a capillary pressure
measurement from the conventional core from
Well-X is shown in Figure 7 Water saturation from
the capilary pressure show value 30-40 this value
is more reliable for this case
CONCLUSION
Oil was discovered in lower resistivity sand in the
Lower Sihapas Formation as proved by oil shows
in cuttings and sidewall cores MDT fluid samples
fluorescence in core photographs formation
pressure gradients and well tests The anomalously
low resistivity is suspected to be a result of clay
minerals in both dispersed and laminated shale as
seen in the XRD data
The higher resistivity in the underlying Upper
Pematang Formation water sand is suspected to be
due to fresh formation water from outcrop sourced
8122019 IPA12-G-095
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meteoric water at the south-western edge of the
Central Sumatran Basin
Petrophysical estimates were based on parameters
from log and core data The water saturation
estimate accommodates the presence of clay
minerals but is still not reliable
The data all supported oil in Zone A so the
development strategy was to perforate only zone A
and produce oil with a single completion
Subsequent production tests showed good AOFrsquos in
Well-X and Well-Y Zone A of 2500 bopd and
20763 bopd respectively as seen in (Figure 8)
Future exploration strategies include drilling look-
alike fault blocks and structural culminations as
well as re-evaluation of old wells using the new
techniques and observations
This paper is a case study that it is possible to find
hydrocarbons in low resistivity sands with the right
data observations and techniques This is good
news for other fields with oil indications and low
resistivity
ACKNOWLEDGEMENTS
The authors acknowledge the Management of PT
Mosesa Petroleum who allowed us to publish the
data and the exploration team UNPAD and
engineering team for their unlimited support and
advance materials and discussion
8122019 IPA12-G-095
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TABLE 1- XRD ANALYSIS RESULT
8122019 IPA12-G-095
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Figure 1- Research Location
Figure 2 - Composite Log of Well-Y
Oil Show
Sample Points
Sample Points
Research
Location
DST Interval
flow rate test
800-2500 BOPD
8122019 IPA12-G-095
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Figure 3 - Oil sample from Zone A and Water Sample from Zone B
Figure 4 - Fluorescent core photograph Zone A with oil shows
Oil Sam le Water Sam le
8122019 IPA12-G-095
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8122019 IPA12-G-095
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Figure 7 - Petrophysics Analysis Using Simandoux Modified Method in Well-X Zone A
Figure 8 - IPR vs VLP Matched Zone A Well X and Well Y
Pwh (psi) Pwf (psi) Rate (bfpd)
300 2105 939
260 2065 1303
140 1937 2525
0 1837 3467
Well-X Well-Y
8122019 IPA12-G-095
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Zone A oil sand was lower than in the underlying
Zone B water sand (water proved from cuttings
sidewall cores and MDT sample with 100 water
saturation)
b Pressure Analysis
Formation pressure tests and fluid samples were
taken in both wells Figure 5 shows the pressure
gradients in Zone A and Zone B in Well X The
Zone A fluid gradient of 0328 psift is consistent
with an oil-bearing zone The Zone B fluid gradient
of 041 psift is consistent with a water-bearing
zone The fluid analyzer results in Figure 6 showed
agreement between the inferred fluid type during
sampling and actual fluid type confirmed when the
sample was opened at surface
c Low and High resistivity values
Low resistivity in hydrocarbon-filled sand can be
caused by dispersed shale andor laminated shale
Shale decreases resistivity because it contains
bound water
XRD data from conventional core in Well-X in
Table 1 shows that Zone A contains clay minerals
such as illite kaolinite and glauconite comprising
over 10 of the total minerals
High resistivity in water-filled sands can be caused by the presence of fresh formation water The
salinity of water samples from Zone B was low at
1000-2000 ppm The water may be meteoric water
flushed from outcrops on the south-western edge of
the Central Sumatran Basin
d Petrophysical analysis
The petrophysical analysis in Figure 7 had to
accommodate the presence of clay minerals in both
dispersed and laminated shale that caused low
resistivity
Petrophysical parameters
Petrophysical parameters were determined from log
and core analysis Water density and matrix density
came from cross plots of bulk density and core
porosity after NOB correction To calculate the total
porosity of shale The wet shale density log and the
neutron log response in shale was cross-plotted
The dry shale density was inferred from the
dominant clay determined from XRD data
Water saturation parameters a m and n came from
SCAL data a and m from a cross plot of core
porosity and formation water and n from a cross
plot of brine saturation and formation resistivity
Vshale
Vshale was calculated from the Gamma Ray log
with the Clavier (1971) method to account for the
mineral response Vshale results from the Clavier
method was compared to Vshale results from the
XRD data
Porosity
Porosity can be calculated from neutron density
and sonic logs with either the single porosity
method and combined porosity method We used
the combined method of neutron and density
porosity and calibrated the result to core porosity
Water Resistivity
Water resistivity came from the Picket plot of RT
and effective porosity as water was not found in
this zone Water is assumed to be bound water
trapped in shale
Water Saturation
As the shale volume is 3-40 and the lithology is
dispersed and laminated shale and sand theModified Simandoux equation was used to
accommodate the presence of clay minerals in both
Water saturation indicated from the Simandoux
modified method was high at 50-70 which for
sand with good porosity and permeability is
inconsistent with the test result of zero water cut
Water saturation from a capillary pressure
measurement from the conventional core from
Well-X is shown in Figure 7 Water saturation from
the capilary pressure show value 30-40 this value
is more reliable for this case
CONCLUSION
Oil was discovered in lower resistivity sand in the
Lower Sihapas Formation as proved by oil shows
in cuttings and sidewall cores MDT fluid samples
fluorescence in core photographs formation
pressure gradients and well tests The anomalously
low resistivity is suspected to be a result of clay
minerals in both dispersed and laminated shale as
seen in the XRD data
The higher resistivity in the underlying Upper
Pematang Formation water sand is suspected to be
due to fresh formation water from outcrop sourced
8122019 IPA12-G-095
httpslidepdfcomreaderfullipa12-g-095 38
meteoric water at the south-western edge of the
Central Sumatran Basin
Petrophysical estimates were based on parameters
from log and core data The water saturation
estimate accommodates the presence of clay
minerals but is still not reliable
The data all supported oil in Zone A so the
development strategy was to perforate only zone A
and produce oil with a single completion
Subsequent production tests showed good AOFrsquos in
Well-X and Well-Y Zone A of 2500 bopd and
20763 bopd respectively as seen in (Figure 8)
Future exploration strategies include drilling look-
alike fault blocks and structural culminations as
well as re-evaluation of old wells using the new
techniques and observations
This paper is a case study that it is possible to find
hydrocarbons in low resistivity sands with the right
data observations and techniques This is good
news for other fields with oil indications and low
resistivity
ACKNOWLEDGEMENTS
The authors acknowledge the Management of PT
Mosesa Petroleum who allowed us to publish the
data and the exploration team UNPAD and
engineering team for their unlimited support and
advance materials and discussion
8122019 IPA12-G-095
httpslidepdfcomreaderfullipa12-g-095 48
TABLE 1- XRD ANALYSIS RESULT
8122019 IPA12-G-095
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Figure 1- Research Location
Figure 2 - Composite Log of Well-Y
Oil Show
Sample Points
Sample Points
Research
Location
DST Interval
flow rate test
800-2500 BOPD
8122019 IPA12-G-095
httpslidepdfcomreaderfullipa12-g-095 68
Figure 3 - Oil sample from Zone A and Water Sample from Zone B
Figure 4 - Fluorescent core photograph Zone A with oil shows
Oil Sam le Water Sam le
8122019 IPA12-G-095
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8122019 IPA12-G-095
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Figure 7 - Petrophysics Analysis Using Simandoux Modified Method in Well-X Zone A
Figure 8 - IPR vs VLP Matched Zone A Well X and Well Y
Pwh (psi) Pwf (psi) Rate (bfpd)
300 2105 939
260 2065 1303
140 1937 2525
0 1837 3467
Well-X Well-Y
8122019 IPA12-G-095
httpslidepdfcomreaderfullipa12-g-095 38
meteoric water at the south-western edge of the
Central Sumatran Basin
Petrophysical estimates were based on parameters
from log and core data The water saturation
estimate accommodates the presence of clay
minerals but is still not reliable
The data all supported oil in Zone A so the
development strategy was to perforate only zone A
and produce oil with a single completion
Subsequent production tests showed good AOFrsquos in
Well-X and Well-Y Zone A of 2500 bopd and
20763 bopd respectively as seen in (Figure 8)
Future exploration strategies include drilling look-
alike fault blocks and structural culminations as
well as re-evaluation of old wells using the new
techniques and observations
This paper is a case study that it is possible to find
hydrocarbons in low resistivity sands with the right
data observations and techniques This is good
news for other fields with oil indications and low
resistivity
ACKNOWLEDGEMENTS
The authors acknowledge the Management of PT
Mosesa Petroleum who allowed us to publish the
data and the exploration team UNPAD and
engineering team for their unlimited support and
advance materials and discussion
8122019 IPA12-G-095
httpslidepdfcomreaderfullipa12-g-095 48
TABLE 1- XRD ANALYSIS RESULT
8122019 IPA12-G-095
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Figure 1- Research Location
Figure 2 - Composite Log of Well-Y
Oil Show
Sample Points
Sample Points
Research
Location
DST Interval
flow rate test
800-2500 BOPD
8122019 IPA12-G-095
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Figure 3 - Oil sample from Zone A and Water Sample from Zone B
Figure 4 - Fluorescent core photograph Zone A with oil shows
Oil Sam le Water Sam le
8122019 IPA12-G-095
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8122019 IPA12-G-095
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Figure 7 - Petrophysics Analysis Using Simandoux Modified Method in Well-X Zone A
Figure 8 - IPR vs VLP Matched Zone A Well X and Well Y
Pwh (psi) Pwf (psi) Rate (bfpd)
300 2105 939
260 2065 1303
140 1937 2525
0 1837 3467
Well-X Well-Y
8122019 IPA12-G-095
httpslidepdfcomreaderfullipa12-g-095 48
TABLE 1- XRD ANALYSIS RESULT
8122019 IPA12-G-095
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Figure 1- Research Location
Figure 2 - Composite Log of Well-Y
Oil Show
Sample Points
Sample Points
Research
Location
DST Interval
flow rate test
800-2500 BOPD
8122019 IPA12-G-095
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Figure 3 - Oil sample from Zone A and Water Sample from Zone B
Figure 4 - Fluorescent core photograph Zone A with oil shows
Oil Sam le Water Sam le
8122019 IPA12-G-095
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8122019 IPA12-G-095
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Figure 7 - Petrophysics Analysis Using Simandoux Modified Method in Well-X Zone A
Figure 8 - IPR vs VLP Matched Zone A Well X and Well Y
Pwh (psi) Pwf (psi) Rate (bfpd)
300 2105 939
260 2065 1303
140 1937 2525
0 1837 3467
Well-X Well-Y
8122019 IPA12-G-095
httpslidepdfcomreaderfullipa12-g-095 58
Figure 1- Research Location
Figure 2 - Composite Log of Well-Y
Oil Show
Sample Points
Sample Points
Research
Location
DST Interval
flow rate test
800-2500 BOPD
8122019 IPA12-G-095
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Figure 3 - Oil sample from Zone A and Water Sample from Zone B
Figure 4 - Fluorescent core photograph Zone A with oil shows
Oil Sam le Water Sam le
8122019 IPA12-G-095
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8122019 IPA12-G-095
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Figure 7 - Petrophysics Analysis Using Simandoux Modified Method in Well-X Zone A
Figure 8 - IPR vs VLP Matched Zone A Well X and Well Y
Pwh (psi) Pwf (psi) Rate (bfpd)
300 2105 939
260 2065 1303
140 1937 2525
0 1837 3467
Well-X Well-Y
8122019 IPA12-G-095
httpslidepdfcomreaderfullipa12-g-095 68
Figure 3 - Oil sample from Zone A and Water Sample from Zone B
Figure 4 - Fluorescent core photograph Zone A with oil shows
Oil Sam le Water Sam le
8122019 IPA12-G-095
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8122019 IPA12-G-095
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Figure 7 - Petrophysics Analysis Using Simandoux Modified Method in Well-X Zone A
Figure 8 - IPR vs VLP Matched Zone A Well X and Well Y
Pwh (psi) Pwf (psi) Rate (bfpd)
300 2105 939
260 2065 1303
140 1937 2525
0 1837 3467
Well-X Well-Y
8122019 IPA12-G-095
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8122019 IPA12-G-095
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Figure 7 - Petrophysics Analysis Using Simandoux Modified Method in Well-X Zone A
Figure 8 - IPR vs VLP Matched Zone A Well X and Well Y
Pwh (psi) Pwf (psi) Rate (bfpd)
300 2105 939
260 2065 1303
140 1937 2525
0 1837 3467
Well-X Well-Y
8122019 IPA12-G-095
httpslidepdfcomreaderfullipa12-g-095 88
Figure 7 - Petrophysics Analysis Using Simandoux Modified Method in Well-X Zone A
Figure 8 - IPR vs VLP Matched Zone A Well X and Well Y
Pwh (psi) Pwf (psi) Rate (bfpd)
300 2105 939
260 2065 1303
140 1937 2525
0 1837 3467
Well-X Well-Y