2. 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
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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