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TGS | EAST SHETLAND BASIN 3D 2013
New High Density Data
EASTSHETLAND
BASIN3D
WWW.TGS.COM
EAST SHETLAND BASIN
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631
037
632
509 S
050
089
037
037
509 S
509 S
509 S
152
631
043
509 S
509 S
043
679 S
040
509 BS
375 C
679 S
040
037 D
509 S
037 C
043 BS
277
509 S
277
037 F
037 F
037 B
050 B
043 BS
037 E
050 D
037 F
043 BS
043 CS
043 DS
3
2
211
210
33
29
30
34
NINIAN
BRENT GAS
LYELL
TERN
CLADHAN
BROOM
CHEVIOT
2/9
3/6
2/14
2/4b
2/3
3/13b
2/8
2/15b
2/10a
2/5
211/17
3/11a
3/2a
3/5
3/1b
3/9c
210/18
211/28b210/30b
2/13
3/8d
211/24c
211/16b
3/7d
3/7c
33/12d
3/4c
3/3b
3/12b
3/12a
210/25b
3/9a
33/9a
3/2b
3/15a
3/1a
3/10c
33/9c
2/19
210/19a
2/20
210/29b
3/14a
3/16
3/3F1
210/20e
210/24a
3/17
33/9d
210/23b
33/6f
211/19a
2/5F1
3/18
3/4b
3/8a
211/27a
210/20a
3/3a
210/19b
211/29F1
3/19a
34/7a
211/29b
211/18b
210/28a
33/9b
29/3aUP
211/21b
210/28b
3/11c
211/22aNW
34/10a
210/24c
3/15b
29/3aLW
2/18
3/14j
210/29c
211/22b
211/23d
30/1bUP
211/27d
211/26aF1
211/22aSE
211/26c
2/5F2
211/30b
211/11b
211/26a
211/21aF1
33/12a
211/21a
3/4aF3
3/20a
210/14
3/14f
211/23e
210/23a
210/15a
30/4d
3/1c
33/12h
211/16a
210/25aF1
3/7aF1
211/18c
211/26d
210/29a
3/2c
210/13
3/14h
2/15a
2/10b
33/9e
3/9e
211/18aF1
33/12b
30/4bUP
211/13b
211/27e
210/30a
33/6e
3/8aF4
29/6a
211/14
30/4a
3/8b
211/12b
30/1c
211/12a
211/24a
211/19aF3
210/24b
29/6dUP
30/7a
3/14i
3/14e
211/18aF4
3/8c
29/3b
211/24b
211/23a2F1
211/23a1
29/6bUP
29/6dLW
211/29a
3/20c
3/4aS
3/15c
211/19b
2/4a
3/10a
3/4aF1
29/3cUP
33/9g
29/6bLW
211/26b
29/9a
29/3cLW
3/9b
3/9d
211/212a5
3/14d
33/9bF1
211/13aF2
211/23a1F2
34/4b
3/11b
3/14b
3/4aF2
211/18aF5
3/14c
3/8f
30/4cUP
211/21a3F1
211/27c
33/12g
3/1aN
210/20d
211/21aS 211/21a4
STATFJORD (NORWAY)
ALWYN NORTH
PELICAN
HUTTON NORTH WEST
CORMORANT NORTH
HUTTON
DUNBAR
DUNLIN
THISTLE
COLUMBA E
JURA
HEATHER (LUNDIN)
STAFFA
COLUMBA B
FORVIE AREA
OSPREY
EIDER
MARTIN LINGE
STATFJORD (UK)
HUDSON
MURCHISON (UK)
STRATHSPEY
HEATHER(TARABAND)
GRANT
NUGGETS COMPLEX
DELTA
KERLOCH
OTTER
STATFJORD EAST
DON NORTH EAST
MERLIN
STATFJORD NORTH
KESTREL
DON SOUTH WEST
FIONN
COLUMBA D
CORMORANT - SOUTH
HEATHER SOUTH WEST
SKYE
ELLON
ISLAY
GULLFAKS SATELLITES
ORLANDO
SYGNA
DEVERON
DON WEST
VIGDIS
PLAYFAIR
WESTERN ISLES
PENGUIN CLUSTER
211/22 (Area 3)
003/03 (Area 8)
CAUSEWAY
MURCHISON (NORWAY)
CORMORANT EAST
SKINFAKS SOUTH
003/09 (Area 7)
003/12 (Area 2)
003/07 (Area 3)
WEST LYELL
CONRIE
003/08 (Area 12)
0029/03 (Area 1)
GULLTOPP
002/10 (Area 1)
MAGNUS SOUTH
003/10 (Area 1)
BALVENIE
BARNACLE
TORDIS
211/28a
3/10b
211/29c
211/27bF1
211/23a2
34/10b
2/4aF1
211/25b
210/24aF1
211/18aF2
211/18aF6
33/12aF2
211/23f
211/27f
211/23c
211/16c
210/25a
33/12c
30/1bLW
3/8aF3
33/12f
211/23a3
211/19aF2
3/7aN
3/7bF1
3/13a
211/23a1F3
210/20f
211/13aF1
211/23b
3/8e
30/4cLW
33/12e
211/21aF3
34/10d
3/14g
29/6cLW
211/19aF1
211/26aW
3/8aF2
3/8eF1
211/25a
211/18aF3
211/21a3F2
211/13c
211/27aF1
211/27b
211/23a2F2
29/6cUP
211/26aN
211/14F1
29/6eLW
29/6eUP
211/27cF1
29/6cCS
211/13aE
211/29aF2211/30aF1
211/19s
TGS has used its best efforts to produce this map free of errors, utilization of same shall be at the sole risk of the user.
TGS assumes no liability or responsibility for reliance placed thereon.
WK800_ESB_Flyer 20 MARCH 2013
ESB 3D
Projection: WGS 1984, UTM Zone 31N
Legend
ESB10 3D
ESB09 3D
ESBRE09 3D
0 0.9 1.8 2.7 3.6 4.50.45
Kilometers
0 6 12 183
km
ESB10, ESB09  ESB00RE09
TGS | EAST SHETLAND BASIN 3D 2013
Ramform Viking
EAST SHETLAND BASIN - LOCATION MAP
INTRODUCTION
The East Shetland Basin survey (ESB09/10) is a joint TGS/PGS venture
which provides:
ƒƒ 2,800 km2
of new multi-client 3D high density data
ƒƒ Significant upgrade on previous data in this area
ƒƒ Improved imaging and resolution to further explore this mature
area and unlock future potential
Additionally TGS has reprocessed ESB00, acquired in 2000, with the
latest processing technology. Hence ESB00-RE09 complements both
the ESB09 and ESB10 surveys.
GEOLOGY AND PROSPECTIVITY
The ESB surveys span several blocks within the East Shetland Basin,
a failed rift basin within the Northern North Sea. The surveys cover
established fields such as the Cormorants, Hutton and NW Hutton
which produce from the Jurassic Brent formations, the main oil
producing reservoir of the North Sea. High density 3D data, with its
associated improved sampling, means that faults and flanks are better
imaged, which is key in this area where tilted fault blocks are the
main play.
The ESB surveys will enable geoscientists to exploit more fully
existing Mesozoic discoveries and will also provide new insight into
the remaining exploration potential of the East Shetland Basin which
is understood to include:
ƒƒ Hanging-wall fault terraces to large tilted fault blocks for Brent,
Banks and Heron Groups reservoirs
ƒƒ Slumped blocks of likely Brent and Banks Group reservoirs on the
fault scarp of large tilted fault blocks
ƒƒ Near field satellites with challenging lateral fault seal risk
requiring enhanced 3D seismic imaging
ƒƒ Combined structural and stratigraphic traps for Late Jurassic
submarine fan systems
ƒƒ Intra-Kimmeridge Clay sandstone reservoir targets of limited areal
distribution
ƒƒ Late Jurassic shore-zone sands along the western basin margin,
offering excellent reservoir properties due to shallow depth of
burial. There has been some significant success recently with this
type of play and our new data adds resolution and definition to
bring out similar opportunities
ƒƒ Combined structural and stratigraphic traps of the Palaeocene –
Early Eocene, previously little targeted by drilling within this basin
except above the principal Jurassic structural highs
This area has the potential to be re-interpreted for missed plays with
this state of the art modern data set which provides a step change in
imaging quality.
VESSEL DETAILS - RAMFORM VIKING AND OCEAN EXPLORER
Ramform Viking is a fully equipped high capacity seismic acquisition
vessel, capable of towing up to 16 streamers. Ramform Viking was
built in 1998 by Langsten SB, Norway. She is 86 m long, has a beam
of 39 m with a gross tonnage of 9456 tonnes and accommodation for
60 people. As well as comprehensive acquisition capability, she is
fully equipped for on-board seismic QC and processing, including PGS
Cube Manager Seismic Processing Software and Holoseis
Hi-End Visualisation System. Ramform Viking is in full compliance
with SOLAS, Marpol 73/78 and other relevant maritime and industrial
standards, EP Forum and IAGC requirements. Further documentation
and certification available on request.
Ocean Explorer is a six streamer 3D seismic vessel equipped with up
to date acquisition and onboard processing systems.
She is 81 m long, has a beam of 18 m, weighs 4458 tonnes gross and
has accommodation for 60 people. She has full on-board processing
capability. Ocean Explorer is in full compliance with SOLAS, Marpol
73/78 and other relevant maritime and industrial standards, EP
Forum and IAGC requirements.
Further documentation and certification available on request.
ACQUISITION PARAMETERS
Source: 	2 x 3111 in3
Sodera G Gun Arrays at 6 m and 2000 psi
Source separation:	 25 m
Sub-array separation:	 8 m
Source length:	 14 m
Streamer type	 RDH (solid and fluid hybrid)
Streamer Viking:	16 x 4800 m (12 x 4800 m in September)
Streamer Ocean:	 6 x 4800 m
Streamer spacing:	 50 m
Streamer depth:	 8.5 m
Near trace offset 	 200 m
Record length	 6656 ms
WWW.TGS.COM © 2013 TGS-NOPEC GEOPHYSICAL COMPANY ASA. ALL RIGHTS RESERVED.
TGS | EAST SHETLAND BASIN 3D 2013
TGS
Tel: +44 (0) 1234 272122
Email: EURsales@tgs.com
For more information, contact:
Example Dip Line
PGS
Email: europeinfo@pgs.com

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TGS EUR- East Shetland Basin 3D

  • 1. WWW.TGS.COM TGS | EAST SHETLAND BASIN 3D 2013 New High Density Data EASTSHETLAND BASIN3D
  • 2. WWW.TGS.COM EAST SHETLAND BASIN !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !(!( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( !( 631 037 632 509 S 050 089 037 037 509 S 509 S 509 S 152 631 043 509 S 509 S 043 679 S 040 509 BS 375 C 679 S 040 037 D 509 S 037 C 043 BS 277 509 S 277 037 F 037 F 037 B 050 B 043 BS 037 E 050 D 037 F 043 BS 043 CS 043 DS 3 2 211 210 33 29 30 34 NINIAN BRENT GAS LYELL TERN CLADHAN BROOM CHEVIOT 2/9 3/6 2/14 2/4b 2/3 3/13b 2/8 2/15b 2/10a 2/5 211/17 3/11a 3/2a 3/5 3/1b 3/9c 210/18 211/28b210/30b 2/13 3/8d 211/24c 211/16b 3/7d 3/7c 33/12d 3/4c 3/3b 3/12b 3/12a 210/25b 3/9a 33/9a 3/2b 3/15a 3/1a 3/10c 33/9c 2/19 210/19a 2/20 210/29b 3/14a 3/16 3/3F1 210/20e 210/24a 3/17 33/9d 210/23b 33/6f 211/19a 2/5F1 3/18 3/4b 3/8a 211/27a 210/20a 3/3a 210/19b 211/29F1 3/19a 34/7a 211/29b 211/18b 210/28a 33/9b 29/3aUP 211/21b 210/28b 3/11c 211/22aNW 34/10a 210/24c 3/15b 29/3aLW 2/18 3/14j 210/29c 211/22b 211/23d 30/1bUP 211/27d 211/26aF1 211/22aSE 211/26c 2/5F2 211/30b 211/11b 211/26a 211/21aF1 33/12a 211/21a 3/4aF3 3/20a 210/14 3/14f 211/23e 210/23a 210/15a 30/4d 3/1c 33/12h 211/16a 210/25aF1 3/7aF1 211/18c 211/26d 210/29a 3/2c 210/13 3/14h 2/15a 2/10b 33/9e 3/9e 211/18aF1 33/12b 30/4bUP 211/13b 211/27e 210/30a 33/6e 3/8aF4 29/6a 211/14 30/4a 3/8b 211/12b 30/1c 211/12a 211/24a 211/19aF3 210/24b 29/6dUP 30/7a 3/14i 3/14e 211/18aF4 3/8c 29/3b 211/24b 211/23a2F1 211/23a1 29/6bUP 29/6dLW 211/29a 3/20c 3/4aS 3/15c 211/19b 2/4a 3/10a 3/4aF1 29/3cUP 33/9g 29/6bLW 211/26b 29/9a 29/3cLW 3/9b 3/9d 211/212a5 3/14d 33/9bF1 211/13aF2 211/23a1F2 34/4b 3/11b 3/14b 3/4aF2 211/18aF5 3/14c 3/8f 30/4cUP 211/21a3F1 211/27c 33/12g 3/1aN 210/20d 211/21aS 211/21a4 STATFJORD (NORWAY) ALWYN NORTH PELICAN HUTTON NORTH WEST CORMORANT NORTH HUTTON DUNBAR DUNLIN THISTLE COLUMBA E JURA HEATHER (LUNDIN) STAFFA COLUMBA B FORVIE AREA OSPREY EIDER MARTIN LINGE STATFJORD (UK) HUDSON MURCHISON (UK) STRATHSPEY HEATHER(TARABAND) GRANT NUGGETS COMPLEX DELTA KERLOCH OTTER STATFJORD EAST DON NORTH EAST MERLIN STATFJORD NORTH KESTREL DON SOUTH WEST FIONN COLUMBA D CORMORANT - SOUTH HEATHER SOUTH WEST SKYE ELLON ISLAY GULLFAKS SATELLITES ORLANDO SYGNA DEVERON DON WEST VIGDIS PLAYFAIR WESTERN ISLES PENGUIN CLUSTER 211/22 (Area 3) 003/03 (Area 8) CAUSEWAY MURCHISON (NORWAY) CORMORANT EAST SKINFAKS SOUTH 003/09 (Area 7) 003/12 (Area 2) 003/07 (Area 3) WEST LYELL CONRIE 003/08 (Area 12) 0029/03 (Area 1) GULLTOPP 002/10 (Area 1) MAGNUS SOUTH 003/10 (Area 1) BALVENIE BARNACLE TORDIS 211/28a 3/10b 211/29c 211/27bF1 211/23a2 34/10b 2/4aF1 211/25b 210/24aF1 211/18aF2 211/18aF6 33/12aF2 211/23f 211/27f 211/23c 211/16c 210/25a 33/12c 30/1bLW 3/8aF3 33/12f 211/23a3 211/19aF2 3/7aN 3/7bF1 3/13a 211/23a1F3 210/20f 211/13aF1 211/23b 3/8e 30/4cLW 33/12e 211/21aF3 34/10d 3/14g 29/6cLW 211/19aF1 211/26aW 3/8aF2 3/8eF1 211/25a 211/18aF3 211/21a3F2 211/13c 211/27aF1 211/27b 211/23a2F2 29/6cUP 211/26aN 211/14F1 29/6eLW 29/6eUP 211/27cF1 29/6cCS 211/13aE 211/29aF2211/30aF1 211/19s TGS has used its best efforts to produce this map free of errors, utilization of same shall be at the sole risk of the user. TGS assumes no liability or responsibility for reliance placed thereon. WK800_ESB_Flyer 20 MARCH 2013 ESB 3D Projection: WGS 1984, UTM Zone 31N Legend ESB10 3D ESB09 3D ESBRE09 3D 0 0.9 1.8 2.7 3.6 4.50.45 Kilometers 0 6 12 183 km ESB10, ESB09 ESB00RE09 TGS | EAST SHETLAND BASIN 3D 2013 Ramform Viking EAST SHETLAND BASIN - LOCATION MAP INTRODUCTION The East Shetland Basin survey (ESB09/10) is a joint TGS/PGS venture which provides: ƒƒ 2,800 km2 of new multi-client 3D high density data ƒƒ Significant upgrade on previous data in this area ƒƒ Improved imaging and resolution to further explore this mature area and unlock future potential Additionally TGS has reprocessed ESB00, acquired in 2000, with the latest processing technology. Hence ESB00-RE09 complements both the ESB09 and ESB10 surveys. GEOLOGY AND PROSPECTIVITY The ESB surveys span several blocks within the East Shetland Basin, a failed rift basin within the Northern North Sea. The surveys cover established fields such as the Cormorants, Hutton and NW Hutton which produce from the Jurassic Brent formations, the main oil producing reservoir of the North Sea. High density 3D data, with its associated improved sampling, means that faults and flanks are better imaged, which is key in this area where tilted fault blocks are the main play. The ESB surveys will enable geoscientists to exploit more fully existing Mesozoic discoveries and will also provide new insight into the remaining exploration potential of the East Shetland Basin which is understood to include: ƒƒ Hanging-wall fault terraces to large tilted fault blocks for Brent, Banks and Heron Groups reservoirs ƒƒ Slumped blocks of likely Brent and Banks Group reservoirs on the fault scarp of large tilted fault blocks ƒƒ Near field satellites with challenging lateral fault seal risk requiring enhanced 3D seismic imaging ƒƒ Combined structural and stratigraphic traps for Late Jurassic submarine fan systems ƒƒ Intra-Kimmeridge Clay sandstone reservoir targets of limited areal distribution ƒƒ Late Jurassic shore-zone sands along the western basin margin, offering excellent reservoir properties due to shallow depth of burial. There has been some significant success recently with this type of play and our new data adds resolution and definition to bring out similar opportunities ƒƒ Combined structural and stratigraphic traps of the Palaeocene – Early Eocene, previously little targeted by drilling within this basin except above the principal Jurassic structural highs This area has the potential to be re-interpreted for missed plays with this state of the art modern data set which provides a step change in imaging quality. VESSEL DETAILS - RAMFORM VIKING AND OCEAN EXPLORER Ramform Viking is a fully equipped high capacity seismic acquisition vessel, capable of towing up to 16 streamers. Ramform Viking was built in 1998 by Langsten SB, Norway. She is 86 m long, has a beam of 39 m with a gross tonnage of 9456 tonnes and accommodation for 60 people. As well as comprehensive acquisition capability, she is fully equipped for on-board seismic QC and processing, including PGS Cube Manager Seismic Processing Software and Holoseis Hi-End Visualisation System. Ramform Viking is in full compliance with SOLAS, Marpol 73/78 and other relevant maritime and industrial standards, EP Forum and IAGC requirements. Further documentation and certification available on request. Ocean Explorer is a six streamer 3D seismic vessel equipped with up to date acquisition and onboard processing systems. She is 81 m long, has a beam of 18 m, weighs 4458 tonnes gross and has accommodation for 60 people. She has full on-board processing capability. Ocean Explorer is in full compliance with SOLAS, Marpol 73/78 and other relevant maritime and industrial standards, EP Forum and IAGC requirements. Further documentation and certification available on request. ACQUISITION PARAMETERS Source: 2 x 3111 in3 Sodera G Gun Arrays at 6 m and 2000 psi Source separation: 25 m Sub-array separation: 8 m Source length: 14 m Streamer type RDH (solid and fluid hybrid) Streamer Viking: 16 x 4800 m (12 x 4800 m in September) Streamer Ocean: 6 x 4800 m Streamer spacing: 50 m Streamer depth: 8.5 m Near trace offset 200 m Record length 6656 ms
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