The document summarizes geological controls on waterflood performance in a field in South Oman. It describes the stratigraphy and facies variations within the field that impact reservoir connectivity. Specifically, the upper and middle members of the Gharif formation have better sand development but poorer lateral continuity compared to the lower Gharif member. Faults across the field also impact pressure communication between reservoir zones. Mapping of reservoir facies and pressure trends was important for planning infill well locations to optimize water injection goals.
Exploration history of Oil and Gas in GhanaElorm Obenechi
This is a document that Oil and Gas students will find useful. it talks in brief about Oil and Gas exploration in Ghana and current state (as at 2008).
It is a good read.
REI Drilling, Inc. - Water Transfer Boreholes for Mining ApplicationsMike Bohan
REI Drilling provides directional drilling services for all types of mining dewatering and/or water transfer for active mining or environmental mitigation purposes.
Give us a call: 330-540-4506
Exploration history of Oil and Gas in GhanaElorm Obenechi
This is a document that Oil and Gas students will find useful. it talks in brief about Oil and Gas exploration in Ghana and current state (as at 2008).
It is a good read.
REI Drilling, Inc. - Water Transfer Boreholes for Mining ApplicationsMike Bohan
REI Drilling provides directional drilling services for all types of mining dewatering and/or water transfer for active mining or environmental mitigation purposes.
Give us a call: 330-540-4506
“The History of WEHLU from Conventional to Unconventional”Gib Knight
For a snapshot of the history of the West Edmond Hunton Lime Unit take a look at the “The History of WEHLU from Conventional to Unconventional” by Galen Miller, Sr. Geologist with Gastar Exploration.
This 5 day training course provides participants with knowledge of critical well completion processes, completion equipment and operations associated with deepwater completions and available intelligent well and completion architecture used for both platform and subsea completions.
AAPG GTW 2017: Deep Water and Shelf ReservoirsDustin Dewett
Since the advent of 3D seismic interpretation, practical seismic interpretation workflows devote a significant amount of time to fault interpretation. Over twenty years ago, seismic similarity volumes first appeared as a method to more easily aid in the complicated process of fault interpretation. Today similarity attributes are used every day by most modern interpretation professionals. Traditionally, improvements to this family of seismic attributes concentrated on improvements to the quality of the seismic amplitude. From increased bandwidth to noise reduction, the improvements to seismic imaging have yielded significant advancements to geophysics and the ability to detect faults within the data. Simultaneously, focusing on post-stack filtering and signal enhancement techniques by many researchers produced interpreter driven uplift on the final seismic image. The most recent direction for fault enhancement within seismic data originates from work on filter banks and, more recently spectral decomposition. Accordingly, the effort to succinctly leverage these ideas into a single, open workflow could result in a significant advancement for all practitioners from academia to industry for years to come.
Although originally intended for stratigraphic purposes, Partyka et al. (1999) make specific note of using the spectral decomposition to identify structural features. Following Partyka et al., in 2008 Henderson et al. developed a method of extracting discontinuities from spectral magnitude data and isolating the discontinuities an RGB blend of three magnitudes. Building on the body of previous work, Dewett and Henza (2015) proposed a complex, highly customized approach to yield a focused multispectral similarity volume that communicates the structural fabric while simultaneously focusing the discontinuity response, which was intended as a method to bridge the gap between fault visualization, similarity enhancement, and fault sharpening techniques. The result was a fault enhancement method that aids both human-driven and computer-based fault interpretation techniques in a precise and accurate way.
Today, there are several options available to the seismic interpreter: interpretation directly on the raw data, filtering the data to enhance the fault response, similarity attributes, fault enhancement, and, multispectral fault enhancement techniques. At each level, the seismic interpreter can gain an increasingly superior fault image. However, there are a plethora of specific algorithms and techniques, each of which claims to be superior. So, confusion abounds, and individuals may develop their methods, ignoring all others. Nonetheless, what is becoming increasingly clear is that the direction of post-stack fault enhancement will continue down the multispectral path.
Classification and Regulatory Standards used in Novel Design Concepts for Dee...IQPC
Alastair Jones, Energy Upstream Sector Manager,
Lloyd’s Register Asia shares with us the classification and regulatory standards
to novel design concepts for deepwater
developments.
“The History of WEHLU from Conventional to Unconventional”Gib Knight
For a snapshot of the history of the West Edmond Hunton Lime Unit take a look at the “The History of WEHLU from Conventional to Unconventional” by Galen Miller, Sr. Geologist with Gastar Exploration.
This 5 day training course provides participants with knowledge of critical well completion processes, completion equipment and operations associated with deepwater completions and available intelligent well and completion architecture used for both platform and subsea completions.
AAPG GTW 2017: Deep Water and Shelf ReservoirsDustin Dewett
Since the advent of 3D seismic interpretation, practical seismic interpretation workflows devote a significant amount of time to fault interpretation. Over twenty years ago, seismic similarity volumes first appeared as a method to more easily aid in the complicated process of fault interpretation. Today similarity attributes are used every day by most modern interpretation professionals. Traditionally, improvements to this family of seismic attributes concentrated on improvements to the quality of the seismic amplitude. From increased bandwidth to noise reduction, the improvements to seismic imaging have yielded significant advancements to geophysics and the ability to detect faults within the data. Simultaneously, focusing on post-stack filtering and signal enhancement techniques by many researchers produced interpreter driven uplift on the final seismic image. The most recent direction for fault enhancement within seismic data originates from work on filter banks and, more recently spectral decomposition. Accordingly, the effort to succinctly leverage these ideas into a single, open workflow could result in a significant advancement for all practitioners from academia to industry for years to come.
Although originally intended for stratigraphic purposes, Partyka et al. (1999) make specific note of using the spectral decomposition to identify structural features. Following Partyka et al., in 2008 Henderson et al. developed a method of extracting discontinuities from spectral magnitude data and isolating the discontinuities an RGB blend of three magnitudes. Building on the body of previous work, Dewett and Henza (2015) proposed a complex, highly customized approach to yield a focused multispectral similarity volume that communicates the structural fabric while simultaneously focusing the discontinuity response, which was intended as a method to bridge the gap between fault visualization, similarity enhancement, and fault sharpening techniques. The result was a fault enhancement method that aids both human-driven and computer-based fault interpretation techniques in a precise and accurate way.
Today, there are several options available to the seismic interpreter: interpretation directly on the raw data, filtering the data to enhance the fault response, similarity attributes, fault enhancement, and, multispectral fault enhancement techniques. At each level, the seismic interpreter can gain an increasingly superior fault image. However, there are a plethora of specific algorithms and techniques, each of which claims to be superior. So, confusion abounds, and individuals may develop their methods, ignoring all others. Nonetheless, what is becoming increasingly clear is that the direction of post-stack fault enhancement will continue down the multispectral path.
Classification and Regulatory Standards used in Novel Design Concepts for Dee...IQPC
Alastair Jones, Energy Upstream Sector Manager,
Lloyd’s Register Asia shares with us the classification and regulatory standards
to novel design concepts for deepwater
developments.
Management Presentation from October 9, 2012 Special Meeting of ShareholdersDan Keeney
This is the management presentation from the Special Meeting of Shareholders held in Houston, Texas on October 9, 2012. The final 10 slides provide additional technical detail.
Salt River Resoures Ltd - SRR presentation 18 July 2008Marius Welthagen
SRR is South Africa's Newest Mineral Oasis: Zn, Cu, Pb, Au, Ag VMS Deposit in the Northern Cape Province of South Africa. Technical Presentation by Dr Craig R. McClung
After emerging from the resources wilderness thanks to its world-class geology and industry-friendly government policies, South Australia is now a leader in Australian mining and hydrocarbon developments over the last decade.
In little more than a decade the State has gone from four operating mines to more than 20 and is rated Australia’s second most popular exploration destination.
With a comprehensive review of the Mining Act under way, the State’s attractiveness as a place for resources and energy investment is expected to be strengthened.
South Australia is now a leader in the exploration for next generation energy sources with companies such as Santos and BP leading the charge, while initiatives such as the Government’s Copper Strategy – designed to treble annual copper production to 1 mtpa – is set to establish the State as one of the world’s premier producers of the red metal.
In the energy space, uranium and nuclear energy is another area of keen interest, with the South Australian Government initiating a Royal Commission into Participation in the Nuclear Fuel Cycle in 2016.
The State has become synonymous with innovation, cutting-edge development and a remarkable rate of discovery. From uranium prospects, to geothermal energy and the buoyant hydrocarbons sector, South Australia is now a leader in the exploration for next generation energy sources.
With full support from the Department of State Development, the South Australian Resources and Energy Investment Conference will continue to showcase this burgeoning sector in 2017. From copper plays in the Gawler Craton, to iron ore and graphite developments on the Eyre Peninsula and the emergence of the State as a new hydrocarbon frontier, South Australia’s resources potential is at last being fully recognised.
The conference will feature the success stories and emerging players in the State from both minerals and oil and gas and will also tackle thorny industry issues such as infrastructure, corporate social responsibility and the future of the Woomera Prohibited Area.
Regional Geology of the Northern Carnarvon Basin.Omar ElGanzoury
An overview about one of the most substantial basins of the oil and gas industry in Australia that is looked at the following headings :
- Firstly , a brief introduction about the location, the area , the operators, the history of the drilled wells in addition to the the carbon-dioxide injection project.
- Following that , we will discuss the basin architecture with the sub basins evolution along with their tectono-staratigraphic framework and their hydrocarbon potentiality.
- Finally, we will give a detailed explanation for both the oil prone and gs prone petroleum systems within the basin.
1. Petroleum Development Oman
1
Geological Controls on Waterflood Performance,
an example from a field in South Oman
M.R.F. Shaikh, A.J.G. Faulkner, & Y. Al Busaidi
PDO
Paper Number: 1178244
2. Petroleum Development Oman
2
• Introduction
• Field Summary
– AB Field Stratigraphy
– Geology overview
• Facies and Pressure Trends in the AB Field
– AB South and Far South Areas
– AB Central and North Areas
• Water Injection within the Gharif
– History
– AB Northern Area and AB Southern Area
• Conclusions
• Acknowledgements
– Asset team and MOG and PDO
Geological Controls on Waterflood Performance,
an example from a field in South Oman
3. Petroleum Development Oman
3
AB Field Background and Development outline
• The AB field is located in South Oman
• Comprised of four isolated accumulations
• Multiple stacked reservoirs:
• Carboniferous-Permian Al Khlata
• Permian Gharif
• Mesozoic Kahmah Clastics.
• Initial development has targeted the Fluvial Gharif Fmn
• Gharif Formation consists of three members:
• transitional marine/terrestrial basal member
• two upper fluvial members.
• The AB FDP initiated an inverted 5-spot WI in August
1998 in the Northern Area of the field where all three
Gharif members were observed to be well developed.
• The 5-spot WI trial resulted in a full field inverted 9-spot
WI development over all four structures.
• On completion of all of the Gharif wells it is clear
that the subsurface development of the Gharif
Reservoir is not as homogeneous as modeled in the
FDP
• It has been observed that reservoir connectivity
within WI patterns is unable to sustain field
production forecasts
• By mapping regions of high and low quality reservoir
facies it has been possible to plan for future infill well
locations in order to ensure that the WI goals are met for
the AB Field.
0 1000 2000 3000 4000 5000m
1:45000
4. Petroleum Development Oman
4
AB Field - Stratigraphy
The main AB Field reservoirs are the basal sands of the Mesozoic Clastic (THMC-A1)
and the significantly older Haushi Sicilicastic of the Gharif and Al Khlata Formations.
The base of the Al Khlata is unconformable upon the Cambrian Ara.
Age Group Formation Member Unit Sub-unit
Depositional
Environment
THMC-A
THMC-A1
Khuff Upper PTKFU
Khuff Middle PTKFM
Khuff Lower PTKFL
HSGHU
HSGHU-1
HSGHM-2 HSGHM-2
HSGHM-1B
HSGHM-1A
HSGHL-3
HSGHL-3.1
HSGHL-3.2
HSGHL-2
HSGHL-2.1
HSGHL-1
HSGHL-1.1
Rahab HSAK1R Glacio-Lacustrine
HSAK-1
HSAK-5U
HSAK-5L
HSAK-9U
HSAK-9M
HSAK-9L
Cambrian Ara QA
HSAK P5
HSAK P9
Al Khlata Glacio-lacustrine/fluvial
Al Khlata
Permo-
Carboniferous
Haushi
Arid/ephemeral fluvial
Arid/ephemeral Deltaic
Fluvial-Deltaic
Shallow Marine
Translittoral -
Floodplane - lacustrine
HSAK P1
HSGHM-1
Middle Gharif
HSGHL-3
HSGHL-2
HSGHL-1
Lower Gharif
PTKFKhuffAkhdar
Permo-
Triassic
HSGHUUpper Gharif
GharifPermian
Undifferentiated
Mesozoic
Clastics
KahmahMesozoic THMC Fluvial - Deltaic- Paralic Tithonian
&
Base Jurassic
Unconformities
Hercynian,
Early Devonian
&
Angudan
Unconformities
5. Petroleum Development Oman
5
Gharif Variations
ABJ-30H1 ABJ-36H1 ABJ-76H1ABJ-10H1 ABJ-68H1ABJ-71H1ABJ-9H1ABJ-33H2ABJ-31H2ABJ-22H1 ABJ-26H1ABJ-66H1 ABJ-49H1
1000 2000 3000 4000 5000 6000 7000 8000 9000 10000
1000 2000 3000 4000 5000 6000 7000 8000 9000 10000
Distance, [m]
-2000-1600-1200
-800
-2000-1600-1200
-800
Z,[m]
1000 2000 3000 4000 5000 6000 7000 8000 9000 10000
1000 2000 3000 4000 5000 6000 7000 8000 9000 10000
Distance, [m]
-2000-1600-1200
-800
-2000-1600-1200
-800
Z,[m]
1000 2000 3000 4000 5000 6000 7000 8000 9000 10000
1000 2000 3000 4000 5000 6000 7000 8000 9000 10000
-2200
-2000
-1800
-1600
-1400
-1200
-1000
-800
-600
-2200
-2000
-1800
-1600
-1400
-1200
-1000
-800
-600
MCA
Khuff
PTKFR
PTKFC
PTKFL
Gharif
HSGHU
HSGHM-2
HSGHL-3
HSGHL-2
HSGHL-1
Al Khlata
HSAKR
HSAK-1
HSAK-5
HSAK-9
Zones
0 1000 2000 3000 4000 5000m
1:45000
A B
0 1000 2000 3000 4000 5000m
1:45000
AB-SOUTH Area
• UGh & MGh poor sand development.
• LGh very well developed in the East
of the Southern Area with good lateral
continuity
• Strong LGh pressure communication
in East of the Southern Area.
• LGh poorly developed in the West of
the Southern Area, though are
pressure depleted
AB-CENTRAL Area
• UGh & MGh poor sand
development
• LGh well developed in Northern
section of the Central Area, but
worsens to the South.
• Lateral Continuity better in the
North than the South This is also
reflected in the pressure data.
AB-NORTH Area
• UGh & MGh good sand
development
• LGh poor sand development
• Lateral continuity is evident in
all Gharif units.
• Pressure communication in the
MGh and LGh across the
Northern Area
A
B
6. Petroleum Development Oman
6
G & G issues
Low NG sandHigh NG sand
Main Stacked Channel
Fairway
Lower Gharif Channel Sands
present but isolated
Axial Flow direction
Kh is expected to be higher
parallel to the axial flow direction
Kh1 > Kh2
Kh1
Kh2
5 km
7. Petroleum Development Oman
7
G & G issues
Low NG sandHigh NG sand
Lower Gharif
Primary Target
Upper &
Middle Gharif
Secondary Target
Faulting
Faulting across the field is seen to juxtapose the Primary
Target Lower Gharif Reservoir against the Secondary Target
Middle and Upper Gharif Sands which Do not appear to have
as much lateral and vertical connectivity as observed in the
Lower Gharif.
Were sand is present either side of the faults there is
communication and fluid moves across faults
The vertical separation of faulted zones observed in wells is
up to 20 m.
5 km
8. Petroleum Development Oman
8
0 1000 2000 3000 4000 5000m
1:45000
Poor developed UGh & MGh with
no lateral continuity
Moderate developed LGh with
poor lateral continuity
Poor developed UGh & MGh with
poor lateral continuity
Very well developed LGh with
Exceptional lateral continuity
Poor developed UGh & MGh with
no lateral continuity
Moderate developed LGh with
reasonable lateral continuity
Poor developed UGh & MGh with
no lateral continuity
Moderate developed LGh with
poor lateral continuity
Poor developed UGh & MGh with
no lateral continuity
Moderate developed LGh with
reasonable lateral continuity
Moderate developed UGh & MGh
with poor lateral continuity
Well developed LGh with good
lateral continuity
Well developed UGh & MGh with
good lateral continuity
Moderate developed LGh with
reasonable lateral continuity
0 1000 2000 3000 4000 5000m
1:45000
AB North – Northern Flank Area
• MGh and LGh-3 has limited to no pressure
communication with AB North - Central Area
• LG-1 & 2 are not completed in the AB North
Flank Area
• Well data shows that the LGh-1 is pressure
depleted
Fault acting as baffle across MGh
Fault acting as potential baffle across LGh
AB North – Central Area
• MGh – In communication with nearby wells and
AB North - Northern Flank Area; but no
communication with AB North – Southern Flank
Area
• LGh – LGh-1 is in limited communication with
nearby wells
– LGh 2&3 are in communication with AB
North Southern Flank Area
– LGh 2&3 has limited communication
with AB North – Northern Flank Area
AB North – Southern Flank Area
• MGh - limited pressure communication with
AB North – Central Area
• LGh - LGh-1 limited pressure
communication with AB North – Central Area
• LGh – LGh 2&3 Well data shows pressure
communication with AB North – Central Area
AB Central – Northern Flank Area
• LGh – Wells are in communication in all LGh
sub-zones
• LGh - LGh-2 is the main reservoir, then
LGh1
AB South – Western Flank Area
• This area has no/very limited communication
with the rest of the South
Fault acting as baffle across LGh
Fault acting as baffle across MGh and LGh
AB Central– Eastern Flank Area
• Has substandard reservoir properties
• Acts as a barrier between northern and
southern areas in the Central Area
AB Central– Southern Flank Area
• LGh-1 & 3 are more productive than the
LGH-2
AB South– Eastern Flank Area
• Wells are in communication
• Some wells show waterflood response
• This area has lower pressure than South
Western area
Fault acting as baffle across LGh
AB Far South– Northern Flank Area
• Higher pressure (+4000KPa) than and not in
communication with the AB Far South
Southern Flank area
AB Far South– Southern Flank Area
• Wells are in communication with each other,
but not in communication with the AB Far
South Northern Flank area
North AB Area
Well developed UGh
& MGh reservoir
Central AB Area
Moderate developed
UGh and MGh
reservoir
Well developed LGh
reservoir
South AB Area
Poor developed
UGh and MGh
reservoir on flanks
Excellent developed
LGh reservoir in
center
Far South AB Area
Poor UGh, MGh &
LGh reservoirs
Facies and Pressure Trends
9. Petroleum Development Oman
9
RFT Pressure vs. Time (at Datum)
Combined Gharif Reservoirs prior to Injection
MDT Pressure Distribution of Gharif Reservoir
•The initial Reservoir Pressure Gharif 15450 kpa at datum -1240 m.
•The current Gharif Reservoir pressure in the range 4000-12000 kpa.
10. Petroleum Development Oman
10
UGh & MGh have better sand development
than the LGh but lateral continuity between
wells is evident in all three units.
There is evidence of pressure communication
in the MGh and LGh across the Northern Area
-1350
-1350
-13
50
-1350
-13
50
-1
35
0
-12
90
-132
0
-1
26
0
-1440
-13
80
-138
0
-12
60
-1320
-1
32
0
-1320
-1320
-1290
-129
0
-12
90
-1
29
0
-1200
-1260
-1
26
0
-1500
-1230
-12
30
-144
0
-1
38
0
-138
0
-1380
-1
41
0
-1410
-1410
-1470
1410
-144
0
-12
90
-1
29
0
-1
26
0
-1320
-1320
-1
41
0
-1440
0 250 500 750 1000 1250m
1:10000
HSGHU
HSGHM-2
HSGHL-3
HSGHL-3
HSGHL-2
HSGHL-1
HSAKR
20.00 150.00GR 0.10 50.00LLD
0.10 50.00LLS 0.45 -0.15CNL
1.95 2.95RHOB 0.3500 -0.3500P OR_Cutoff
-1.0000 1.0000S o_Cutoff
5000 20000RFT
OpenOpen
Open
Open
Open
PERFS
HSGHL-3
ABJ-14H1 [MD]
20.00 150.00GR 0.10 50.00LLD
0.10 50.00LLS 0.45 -0.15CNL
1.95 2.95RHOB -1.0000 1.0000S o_Cutoff
0.3500 -0.3500P OR_Cutoff
5000 20000RFT
OpenOpen
Open
Open
OpenOpen
PERFS
HSGHL-3
ABJ-10H1 [MD]
20.00 150.00GR 1.00 50.00LLD
0.45 -0.15CNL
1.95 2.95RHOB -1.0000 1.0000S o_Cutoff
0.3500 -0.3500P OR_Cutoff
5000 20000RFT
ClosedClosedClosedClosedOpenOpenOpen
PERFS
HSGHL-3
ABJ-30H1 [MD]
20.00 150.00GR 0.10 50.00LLD
0.10 50.00LLS 0.45 -0.15CNL
1.95 2.95RHOB -1.0000 1.0000S o_Cutoff
0.3500 -0.3500P OR_Cutoff
5000 20000RFT
Open
Open
Open
Open
OpenOpenOpen
PERFS
HSGHL-3
ABJ-22H1 [MD]
20.00 150.00GR 0.10 50.00LLD
0.10 50.00LLS 0.45 -0.15CNL
1.95 2.95RHOB -1.0000 1.0000S o_Cutoff
0.3000 -0.3000P OR_Cutoff
5000 20000RFT
OpenOpenOpen
PERFS
HSGHL-3
ABJ-40H3 [MD]
20.00 150.00GR 0.10 50.00LLD
0.10 50.00LLS 0.45 -0.15CNL
1.95 2.95RHOB -1.0000 1.0000S o_Cutoff
0.3000 -0.3000P OR_Cutoff
5000 20000RFT
Open
OpenOpenOpenOpen
PERFS
HSGHL-3
ABJ-44H2 [MD]
HSGHU
HSGHM-2
HSGHL-3
HSGHL-3
HSGHL-2
HSGHL-1
HSAKR
Section flattened on Base Gharif
A B
AB Field Northern Area - Geology
A
B
UGhLGh
MGh
11. Petroleum Development Oman
11
-1350
-1350
-13
50
-1350
-13
50
-1
35
0
-12
90
-132
0
-1
26
0
-1440
-13
80
-138
0
-12
60
-1320
-1
32
0
-1320
-1320
-1290
-129
0
-12
90
-1
29
0
-1200
-1260
-1
26
0
-1500
-1230
-12
30
-144
0
-1
38
0
-138
0
-1380
-1
41
0
-1410
-1410
-1470
1410
-144
0
-12
90
-1
29
0
-1
26
0
-1320
-1320
-1
41
0
-1440
0 250 500 750 1000 1250m
1:10000
AB Field Northern Area - Structure
ABJ-14H1 ABJ-10H1 ABJ-30H1 ABJ-22H1
ABJ-40H3
ABJ-44H2
600 800 1000 1200 1400 1600 1800 2000 2200 2400 2600 2800
600 800 1000 1200 1400 1600 1800 2000 2200 2400 2600 2800
-1450
-1400
-1350
-1300
-1250
-1200
-1450
-1400
-1350
-1300
-1250
-1200
Symbol legend
HSGHU
HSGHM-2
HSGHL-3
HSGHL-2
HSGHL-1
HSAKR
HSAK-1
HSAK-5
HSAK-9
ABJ-14H1
ABJ-10H1
ABJ-30H1
ABJ-22H1
ABJ-40H3
ABJ-44H2
0 200 400 600 800 1000m
1:10000
A
B
ABJ-14H1 ABJ-10H1 ABJ-30H1 ABJ-22H1
ABJ-40H3
ABJ-44H2
600 800 1000 1200 1400 1600 1800 2000 2200 2400 2600 2800
600 800 1000 1200 1400 1600 1800 2000 2200 2400 2600 2800
-1450
-1400
-1350
-1300
-1250
-1200
-1450
-1400
-1350
-1300
-1250
-1200
Symbol legend
HSGHU
HSGHM-2
HSGHL-3
HSGHL-2
HSGHL-1
HSAKR
HSAK-1
HSAK-5
HSAK-9
ABJ-14H1
ABJ-10H1
ABJ-30H1
ABJ-22H1
ABJ-40H3
ABJ-44H2
0 200 400 600 800 1000m
1:10000
Faults and Folding has resulted in localised
compartmentalisation of the Northern Area of
the AB Field.
There is evidence of pressure communication
in the MGh and LGh across the Northern Area
A
B
12. Petroleum Development Oman
12
AB Field Northern Area - Pressure
-1350
-1
350
-1350
-1350
-1
350
-138
0
-138
0
-1380
-1
380
-1
410
-1260
-1320
-1
320
-1320
-1290
-1290
-1290
-1200
-1260
-1260
-1500
-1230
-1230
-1440
-1
380
-1380
-1
410
-1410
-1470
-1410
-1440
-129
0
-1
290
-1
260
-1320
-1320
-1
410
-1440
0 250 500 750 1000 1250m
1:15000
AB North – Northern Flank Area
• MGh and LGh-3 has limited to no pressure
communication with AB North - Central Area
• LG-1 & 2 are not completed in the AB North Flank Area
• Well data shows that the LGh-1 is pressure depleted
AB North – Central Area
• MGh – In communication with nearby wells and
AB North - Northern Flank Area; but no
communication with AB North – Southern Flank
Area
• LGh – LGh-1 is in limited communication with
nearby wells
– LGh 2&3 are in communication with AB
North Southern Flank Area
– LGh 2&3 has limited communication
with AB North – Northern Flank Area
AB North – Southern Flank Area
• MGh - limited pressure communication with
AB North – Central Area
• LGh - LGh-1 limited pressure
communication with AB North – Central Area
• LGh – LGh 2&3 Well data shows pressure
communication with AB North – Central Area
Fault acting as baffle
across MGh
0
2000
4000
6000
8000
10000
12000
14000
16000
18000
Aug-87 May-90 Jan-93 Oct-95 Jul-98 Apr-01 Jan-04 Oct-06 Jul-09
Pressure,kPa
TIME
AB - North Area
Sub Zone LowerGH
Initial Reservoir Pressure @ -1240 TVD ss =~16000 kPa
Initial
Reservoir
Pressure
Fault acting as potential
baffle across LGh
13. Petroleum Development Oman
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LG3
LG2
LG1
LG3
LG2
LG1
AB-NA WF Pattern Northern Flank
AB-NB WF Pattern North Area West Flank
AB-NC WF Pattern North Central Area
AB-ND WF Pattern North Area East Flank
GH Prod 11
WI 5
WSW 2
CIW 2
AK 1
GH-UGH-U
GH-MGH-M
AB-NE WF Pattern North Area Southern Flank
AB Field Northern Area - Wells
A
B
C D
E
14. Petroleum Development Oman
14
AB North Area has 5 injectors:
• Main focus has been to increase reservoir pressure
and increase the net voidage in this area of the field
• General observation:
• Very limited injectivity into LG-1 in AB North Area:
only 2 out of five injectors (C & D)
• Structure and Facies are seen to play a major role
in subsurface flow in AB North
• LGh is not as well developed compared to UGh &
MGh in AB North Area
• Local faults are seen to inhibit subsurface flow in
specific zones
• AB-NA WI is seen to support offset wells to the
West & South in the MGh and LGh
• AB-NB WI is seen to support in the LGh only
due to poor connectivity in the shallower zones
• AB-NC WI is seen to support all offset wells in
the UGh & MGh
• AB-ND WI is supporting wells to the south-west
and north-east – possible fault interference
• AB-NE WI supports wells to the north in the
MGh.
AB North Area – Pattern Summary
A
B
C D
E
18. Petroleum Development Oman
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AB South Area – Pattern Performance
0
2000
4000
6000
8000
10000
12000
14000
16000
18000
Jan-04 May-05 Oct-06 Feb-08 Jul-09 Nov-10 Apr-12
Pressure,kPa
Time
AB Field - Southern Area
RFT Pressure vs. Time
Lower Gharif Zone
Easten flank AB South Area Press @ -1240 TVD ss =14500 kPa
2011 new wellsWestern side wells
Eastern side wells
Initial Reservoir Pressure @ -1240m TVD ss =~16000 kPa
West side of South Area Press @ -1240 TVD ss =8500-9000 kPa
East side of South Area Press@ -1240 TVD ss =7500 kPa (4000 with no INJ)
2010 new wells
-1350
-1350
-1350
-1
350
-1380
-1380
-1290
-1410
-1320
-1
320
-1260
-1290
-1260
-1440
-1380
-1380
-1410
-1260
-1
320
-1320
-1320
-1320
-1290
-1
290
-1290
-1200
-1260
-1500
-1230
-1230
-1440
-1380
-1380
-1380
-1410
-1410
-1470
0 500 1000 1500 2000 2500m
1:15000
AB Central– Southern Flank Area
• LGh-1 & 3 are more productive than the
LGH-2
AB South– Eastern Flank Area
• Wells are in communication
• Some wells show waterflood response
• This area has lower pressure than South
Western area
Fault acting as baffle across
MGh and LGh
Fault acting as
baffle across LGh
AB South – Western Flank Area
• This area has no/very limited communication
with the rest of the South
19. Petroleum Development Oman
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AB Southern Area Wells
Three AB SA WF Patterns
AB-SA WF Pattern in the South East Central
AB-SB WF Pattern in the Southern South Flank
AB-SC WF Pattern in the South West Central
GH Prod 11
WI 4
CIW 2
AK/MZ 2
LG3
LG2
LG1
LG3
LG2
LG1
N
42
B
A
C
20. Petroleum Development Oman
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AB Southern Area Pattern Performance
0
10
20
30
40
50
60
70
80
90
100
1.00
10.00
100.00
1000.00
Jan-08 May-08 Sep-08 Jan-09 May-09 Sep-09 Jan-10 May-10 Sep-10 Jan-11 May-11 Sep-11
Watercut%
Oil/Liquidratem3/d
South Area
Production Performance
OilCD
LiquidCD
oildepletion
WaterCut
AB-SB WF
AB-SA-WF
AB-SC-WF
6 OP wells
High
Low
Oil gain
in South
AB Field
21. Petroleum Development Oman
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AB South Area Pattern Summary:
Three WI currently impacting flow in the AB
South area.
Well data show that 3 wells have
responded to WF out of 9 producers
currently producing from GH.
Well data show that the East of the AB
South area is responding better to the
West – better rock quality to the East
A Tracer Injection in AB-A & AB-C has been
recommended to identify pattern
connectivity, flow path, confirm WF response
An additional 3 -4 new wells locations have
been recommended of which two have been
drilled
AB South Area – Pattern Summary
N
42
B
A
C
22. Petroleum Development Oman
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AB Field Production History - Southern Area
0
10
20
30
40
50
60
70
80
90
100
1
10
100
1000
Jan-02 Jan-03 Jan-04 Jan-05 Jan-06 Jan-07 Jan-08 Jan-09 Jan-10 Jan-11
BS&W,%
Rate(m3/d)
Date
AB - GH South Production History
Start WI OilCD LiquidCD OilWellcount WaterCut
AB -SB
AB-SA
AB-SC
High
Low
23. Petroleum Development Oman
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• The Gharif reservoir in each accumulation within the AB Field
responds to Water injection in a unique way due to a combination of
Facies variations and Structural controls.
• Vigilant monitoring of production and pressure data has allowed an
improved understanding of to subsurface fluid dynamics to be
modeled
• Facies Controls on WF include reservoir quality, connectivity and
lateral continuity across the field
• Structural Control on WF include compartmentalization due to minor
salt related faulting and folding.
• The resultant pressure distribution illustrates both production and
injection history within the target reservoir and illustrates the location
of superior connected pay within the field
• The results of this work has allowed for improved production
forecasts to be made as well as allowed for a more simplified
strategic well placement decision making process
Conclusions