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UNCOVER THE OVERLOOKED GUMAI PLAY POTENTIAL
AT JABUNG BETARA COMPLEX, INDONESIA: A BEST CASE STUDY OF
GAS WHILE DRILLING (GWD) CLASSIFICATION IN FINDING THE NEW PAYS
Authors:
I Gusti Agung Aditya Surya Wibawa*, Beiruny Syam,
Hendra Niko Saputra, Mawar Indah Nursina, Abghia Dini Fanzuri
PetroChina International Companies in Indonesia
SEAPEX Exploration Conference
Fairmont Hotel, Singapore
2nd – 5th April 2019
PRESENTATION OUTLINE
1. EXPLORATION HISTORY & HIGHLIGHT
2. JABUNG BETARA COMPLEX GEOLOGICAL SETTINGS
3. JABUNG BETARA COMPLEX GWD OVERVIEW
4. GWD DATABASE AND CLASSIFICATION
5. GWD INTERPRETED DISTRIBUTION
6. SUMMARY & STUDY BREAKTHROUGH
EXPLORATION HISTORY
1992 1996-1998 2006 2013 2015 2023
EXPLORATION HIGHLIGHT
♦ High Gas While Drilling in Gumai Formation has founded in many development
wells during drilling activities.
♦ 77 potential wells were drilled on Betara Complex Structure (exploration +
development), but only 12 wells have wireline logs in intra GUF section (were
trying to acquire wireline in development wells but need more justification)
♦ The first testing program of Gumai Formation was conducted in NEB Basement-1
(exploration well) on 2013 by the result of 4.45 MMSCFD, 15 BCPD (CO2
content: 0%).
♦ Another good testing results in Gumai Formation has been proven on NEB-96,
NBE-1, Marmo-3 and Sabar-2 that act as our key wells.
♦ Based on Gas while drilling and testing data, further analysis is conducted to
predict reservoir distribution by generating structure maps and attributes anaylsis.
JABUNG BLOCK OVERVIEW : GEOLOGICAL SETTING
There are 77 potential wells that have been drilled in the Betara Complex area
but only 12 wells that have complete mudlog, wireline log and DST result data in Gumai Formation.
Basement configuration of South Sumatra Basin
(Ginger & Fielding, 2005)
MARMO-3
NBE-1
NEB-1
NEB-6
NEB BASE-1
NEB-96
NEB-5
SABAR UTARA-1
NEB-55
SABAR-2
The Betara Complex is a
combination of 5 major
fields in Jabung Block:
1. Northeast Betara
(NEB),
2. Sabar,
3. Marmo,
4. Northeast Betara
Extension (NBE),
5. North Betara (NB)
Field.
JABUNG BLOCK
Situation of South Sumatra
Basins and other basins to
the north and south. These
basins were formed and
developed in very similar
way in both timing and
tectono-stratigraphy
BETARA COMPLEX AREA
±500 sq km
GEOLOGICAL SETTINGS –
JABUNG BLOCK STRATIGRAPIC COLUMN
Syn-Orogenic
/Inversion
Post-Rift
Syn-Rift
Pre-Rift
Jabung Block Stratigraphy (Suta, 2003)
R
R
R
R SR
SR
SR SR
S
S
S
S
R
SR
S
: Reservoir
: Source Rock
: Seal
Legend
Fm. Target
GAS WHILE DRILLING OVERVIEW
1. More than 1000 feet of gross gas column existed in
the Gumai Formation interval in Betara Complex area.
2. Gas and Condensate is the predominate fluid type in
this area
A B
Average thickness: 700 ft – 1600 ft
Net to gross: 170 ft – 500 ft
Sand character: Lenses
GAS WHILE DRILLING DATABASE
: Good test result Ranking parameter:
Testing result, TG value, RT value, Cross over, & C5 availability)
GAS WHILE DRILLING DATABASE
: Poor test result
TESTING SUMMARY (GUF INTERVAL)
*) KEY WELLS: NEB-96, NEB BASE-1, SABAR-2, NBE-1 & MARMO-3
LOG FEATURE NEB BASE-1 (EXAMPLE KEY WELL)
Reservoir properties ‐ Lithology : Sandstone ‐ Rt : 27.3 ohm.m ‐ Xover : Narrow ‐ TG : 250 U (C1-C5)
‐ Porosity : 11.4 % ‐ Sw : 50.6 % ‐ Rate : 4.45 MMCFPD + 158 BCPD
#DST - 4
LOWEST POINT OF PROSPECTIVE GWD
♦ In NEB, Marmo and NBE Fields, a value of
200 and 300 units was applied as a cut-off
when determining potential reservoir zones.
♦ For the Sabar Field, 150 units were used for
the cut-off for overlooked potential.
♦ The cut-off values obtained from lowest
depth of gas while drilling were compared
to DST results using 5 key wells in the study
area
NEB FIELD
SABAR FIELD
TOTA
L G
AS
(UN
IT)
WELLS
HC Potential Cut off line
40/64": 161 psi WHP, 990F WHT, 1.011 MMSCFD (SG: 0.82). CO2: 0.8%, H2S: 0 ppm.
36/64" : 1325 psi WHP, 1290F WHT, 247 BCPD (SG: 0.720, 650 API), 5.804 MMSCFD (SG gas: 0.820), no water, GOR: 23506 scf/stb.
TESTED WELLTESTED WELL
MARMO &
NBE FIELD
HC Potential Cut off line
TOTA
L G
AS
(UN
IT)
Gas converter:40 unit = 0.8% = 8,000 ppm190 unit = 3.8% = 38,000 ppm
WELLS
TESTED WELL
36/64": 1377 psi WHP, 1370F WHT, 549 BCPD (SG: 0.71, 680API). No water. 4.929 MMSCFD (SG gas: 0.830), GOR: 8986 scf/stb, CO2: 1.8%, H2S: 0 ppm.
SABAR-1 SABARUTARA -1
SABAR-3 SABAR-2
MUD WEIGHT INTERVAL FOR EACH FIELD
g
♦ Based on cross-plot above showed that our
current efficient mud weight range (Gumai
Formation - 12 1/4” drilling section) for each field
as followed:
1. NEB Field in range of 9 – 9.9 ppg.
2. Marmo, NB and NBE Field in range of 9.2
– 10 ppg
3. Sabar Field in range of 9.6 – 9.7 ppg
♦ The mud weight range is limited by proven zone
from 5 wells with flowed DST results.
GW
D (
un
its)
MUD WEIGHT (PPG)
GW
D (
un
its)
MUD WEIGHT (PPG)
0
500
1000
1500
2000
2500
3000
3500
4000
4500
8.8 9 9.2 9.4 9.6 9.8 10 10.2
Potential Zone
Proven Zone (by DST)0
500
1000
1500
2000
2500
3000
3500
4000
4500
8.8 9 9.2 9.4 9.6 9.8 10 10.2
Potential Zone
Proven Zone (by DST)
MW = 9 – 9.9 ppg
NEB FIELD
0
500
1000
1500
2000
2500
3000
3500
4000
4500
5000
9 9.2 9.4 9.6 9.8 10 10.2
Potential Zone
Proven Zone (by DST)
MARMO & NB,
NBE FIELD
0
500
1000
1500
2000
2500
3000
3500
4000
4500
8.8 9 9.2 9.4 9.6 9.8 10 10.2
Potential Zone
Proven Zone (by DST)
MW = 9.2 – 10 ppg
0
100
200
300
400
500
600
700
800
9.58 9.6 9.62 9.64 9.66 9.68 9.7 9.72
Potential Zone
Proven Zone (by DST)GW
D (
un
its)
MUD WEIGHT (PPG)
SABAR FIELD
0
500
1000
1500
2000
2500
3000
3500
4000
4500
8.8 9 9.2 9.4 9.6 9.8 10 10.2
Potential Zone
Proven Zone (by DST)
MW = 9.6 – 9.7 ppg
NEB-96 5.164 MMSCFD,
135 BCPD
SABAR-2 4.929 MMSCFD,
549 BCPD
NBE-1 5.9 MMSCFD,
254 BCPD
MARMO-3 1.01 MMSCFD
SEQUENCE CLASSIFICATION
NEB-6
Wavelet
IGUF A
IGUF B
IGUF C
IGUF D
GUF
IGUF A
IGUF B
IGUF C
IGUF D
BRF
UTAF
GUF is divided into 4 sequences based on flooding surface marker to observed its reservoir distribution
RESERVOIR DISTRIBUTION IN IGUF-A
A
B
Sabar-2
NEB-4
NEB BASE-1
NEB-6 Int GUF
Int GUF-A
Int GUF-B
Int GUF-C
Int GUF-D
BRF GUF
UTAF
NEB-4 A B SABAR-2 NEB BASE-1 NEB-6
+-
DST #4 4.45 MMCFPD +
158 BCPD (CO2: 0%)
RESERVOIR DISTRIBUTION IN IGUF-A
A
B
Sabar-2
NEB-4
NEB BASE-1
NEB-6
NEB-4 A B SABAR-2 NEB BASE-1 NEB-6
COSINE PHASE in purpose of looking at its
continuity
DST #4 4.45 MMCFPD +
158 BCPD (CO2: 0%)
Int GUF
Int GUF-A
Int GUF-B
Int GUF-C
Int GUF-D
BRF GUF
UTAF
RESERVOIR DISTRIBUTION IN IGUF-C
Int GUF
Int GUF-A
Int GUF-B
Int GUF-C
Int GUF-D
BRF GUF
UTAF
NEB-4 A B SABAR-2 NEB BASE-1 NEB-6
+-
A
B
Sabar-2
NEB-4
NEB BASE-1 NEB-6
DST #7 4.9 MMCFPD +
549 BCPD (CO2: 1.8%)
RESERVOIR DISTRIBUTION IN IGUF-C
NEB-4 A B SABAR-2 NEB BASE-1 NEB-6
COSINE PHASE in purpose of looking at its
continuity
DST #7 4.9 MMCFPD +
549 BCPD (CO2: 1.8%)
A
B
Sabar-2
NEB-4
NEB BASE-1 NEB-6
Int GUF
Int GUF-A
Int GUF-B
Int GUF-C
Int GUF-D
BRF GUF
UTAF
RESERVOIR DISTRIBUTION IN IGUF-D
NBE-1 A B MARMO-3 NEB-96
+-
DST#2 1.01 MMSCFD
(CO2: 0.8%)
DST#3 5.804 MMSCFD +
247 BCPD
DST#5 5.164 MMSCFD + 135
BCPD (CO2: 47%)
A
B
MARMO-3
NBE-1
NEB-96
Int GUF
Int GUF-A
Int GUF-B
Int GUF-C
Int GUF-D
BRF GUF
UTAF
RESERVOIR DISTRIBUTION IN IGUF-D
NBE-1 A B MARMO-3 NEB-96
Int GUF
Int GUF-A
Int GUF-B
Int GUF-C
Int GUF-D
BRF GUF
UTAF
COSINE PHASE in purpose of looking at its
continuity
DST#2 1.01 MMSCFD
(CO2: 0.8%)
DST#3 5.804 MMSCFD +
247 BCPD
DST#5 5.164 MMSCFD + 135
BCPD (CO2: 47%)
A
B
MARMO-3
NBE-1
NEB-96
ATTRIBUTE ANALYSIS IN IGUF-A
NEB Base-14.45 MMCFPD + 158 BCPD
TG : 250 U ; CO2 : 0%
NB-5TG : 209 U
NEB-96TG : 279 U
NB-40TG : 237 U
NEB-7TG : 440 U
NEB-13TG : 994 U
NEB-6TG : 1164 U
NEB-11TG : 1247 U
DEPTH STRUCTURE MAPCI : 25 ft
NEB-96TG : 279 U
NB-40TG : 237 U
NEB-13TG : 994 U
AVERAGE POSITIVE AMPLITUDE MAPCI : 25 ft
GT : 229.5’
GT : 293’
NEB-6TG : 1164 U
GT : 152’
*GT : Gross Thickness
NB-5TG : 209 U
NEB-11
TG : 1247 U
NEB-7
TG : 440 U
NEB Base-14.45 MMCFPD + 158 BCPD
TG : 250 U ; CO2 : 0%
The graph shows that thick reservoir correlate with high value of attribute in IGUF A
R2= 0.6688
ATTRIBUTE ANALYSIS IN IGUF-B
NEB-12TG : 260 U
NEB-35TG : 346 U
NEB-42
TG : 101 U
NEB BASE-1TG : 32 U
NEB-96TG : 354 U
NB-5
TG : 740 U
NEB-43
TG : 852 U
NEB-94TG : 1805 U
NB-4
TG : 4500 U
DEPTH STRUCTURE MAPCI : 25 ft
NEB-6
TG : 375 U
NEB-35
TG : 346 U
NEB-42TG : 101 U
NEB BASE-1
TG : 32 U
NEB-96
TG : 354 U
NB-5TG : 740 U
NEB-43TG : 852 U
NEB-94
TG : 1805 U
ENVELOPE MAPCI : 25 ft
GT : 168.5’
GT : 63.2’
GT : 105.5’
*GT : Gross Thickness
NB-4
TG : 4500 U
NEB-12
TG : 260 U
NEB-6TG : 375 U
The graph shows that thick reservoir correlate with high value of attribute in IGUF B
R2= 0.7206
ATTRIBUTE ANALYSIS IN IGUF-C
NEB-12TG : 260 U
NEB-35TG : 346 U
NEB-42TG : 101 U
NEB BASE-1TG : 32 U
NEB-96TG : 354 U
NB-5TG : 740 U
NEB-43TG : 852 U
NEB-94TG : 1805 U
NB-4TG : 4500 U
DEPTH STRUCTURE MAPCI : 25 ft
NEB-6TG : 375 U
NEB BASE-1TG : 32 U
NEB-6TG : 425 U
NEB-40TG : 233 U
NEB-1
TG : 533U
NEB-87TG : 131 U
ENVELOPE MAPCI : 25 ft
GT : 55’
GT : 105.3’
NEB-5TG : 188 U
*GT : Gross Thickness
GT : 84.1’
NB-7TG : 1619 U
SABAR-2
4.93 MMCFPD + 549 BCPDTG : 300 U ; CO2 : 1.8%
NEB-15TG : 1197 U
NEB-7TG : 1805 U
NEB-31
TG : 227 U
SABAR UTARA-1
No recovery
The graph shows that thick reservoir correlate with high value of attribute in IGUF C
R2= 0.667
ATTRIBUTE ANALYSIS IN IGUF-D
DEPTH STRUCTURE MAPCI : 25 ft
NEB-6TG : 425 U
NEB-14
TG : 498
NEB-5TG : 2806 U
NORTH BETARA-6TG : 1386 U
NEB-31TG : 2571 U
NEB-66TG : 3108 U
NBE-15.804 ; 247TG : 898 U
MARMO-31.01 ;
TG : 1977 U ; CO2: 0.8%
NEB-11TG : 1119 U
MARMO-2
0.01TG : 1386 U
NEB BASE-20.01 BOPD ;
TG : 20 UNEB-55
0.27 MMCFPD ; TG : 286 U
NEB-965.16 ; 135
TG : 3477 U
ENVELOPE MAPCI : 25 ft
NEB BASE-2TG : 20 U
NEB-55
TG : 286 U
NEB-31TG : 2571 U
NEB-965.16 ; 135
TG : 3477 U
NEB-11TG : 1119 U
NEB-66TG : 3108 U
GT : 148’
GT : 161’
MARMO-31.01 ;
TG : 1977 U ; CO2: 0.8%
NORTH BETARA-6TG : 1386 U
NEB-5TG : 2806 U
NEB-14
TG : 498
NEB-6TG : 425 U
*GT : Gross Thickness
1B
1A
The graph shows that thick reservoir correlate with small value of attribute in IGUF D.
R2= 0.614
SUMMARY & STUDY BREAKTHROUGH
Summary:
♦ The pattern of gas while drilling values in the Betara Complex area generally follow the
distribution of the sediments. The thicker the sediment the larger the gas while drilling values.
♦ In interpreting potential reservoir zones, GWD analysis has shown to be a useful tool, but
needs to be integrated with seismic attributes and reservoir characterization.
♦ Data quality control on the cut-off value must be periodically checked to observe the
developing pattern of GWD value for future developments.
Study Breakthrough:
♦ GWD classification has implemented as one of our quick look interpretation tools to control
drilling targets and propose field data acquisition such as SWC, pressure test, fluid analysis
and fluid sample interval.
♦ Study of GWD analysis acted as one of our preliminary justification in reviving our old wells
that have good potential indication in Gumai Formation (example: 2016 - conduct re-entry
well program by cased hole logging).
Thank you
SEAPEX Exploration Conference
Fairmont Hotel, Singapore
2nd – 5th April 2019