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NARROW
GeoRef Subject
-
all geography including DSDP/ODP Sites and Legs
-
Africa
-
East Africa
-
Mozambique (1)
-
-
North Africa
-
Libya (1)
-
-
West Africa
-
Cameroon (1)
-
-
-
Antarctica
-
Antarctic Peninsula (1)
-
South Shetland Islands (1)
-
-
Arctic Ocean
-
Norwegian Sea
-
Voring Plateau (1)
-
-
-
Arctic region
-
Greenland
-
East Greenland (3)
-
-
Svalbard (3)
-
-
Asia
-
Arabian Peninsula
-
Oman (2)
-
Saudi Arabia (1)
-
-
Far East
-
Philippine Islands (1)
-
-
Middle East
-
Cyprus (1)
-
-
-
Atlantic Ocean
-
North Atlantic
-
Faeroe-Shetland Basin (39)
-
Gulf of Mexico (1)
-
North Sea
-
East Shetland Basin (4)
-
Viking Graben (3)
-
-
Northeast Atlantic (22)
-
Reykjanes Ridge (1)
-
Rockall Plateau (1)
-
Rockall Trough (4)
-
-
-
Atlantic Ocean Islands
-
Faeroe Islands (15)
-
Shetland Islands
-
Unst (11)
-
-
-
Atlantic region (3)
-
Caledonides (7)
-
Central Graben (1)
-
Europe
-
Baltic region (1)
-
Pyrenees (1)
-
Southern Europe
-
Italy
-
Piemonte Italy
-
Lanzo Massif (1)
-
-
-
-
Western Europe
-
Ireland
-
Galway Ireland (1)
-
-
Scandinavia
-
Norway
-
Northern Norway (1)
-
-
-
United Kingdom
-
Great Britain
-
England
-
London Basin (1)
-
Somerset England (1)
-
-
Scotland
-
Argyllshire Scotland
-
Mull Island (1)
-
-
Great Glen Fault (3)
-
Hebrides
-
Inner Hebrides
-
Mull Island (1)
-
-
Outer Hebrides (1)
-
-
Highland region Scotland
-
Caithness Scotland (2)
-
-
Moine thrust zone (4)
-
Orkney Islands (3)
-
Scottish Highlands
-
Grampian Highlands (1)
-
-
Shetland Islands
-
Unst (11)
-
-
-
-
-
-
-
Midland Valley (1)
-
North America
-
Appalachians (1)
-
-
ODP Site 642 (1)
-
Orcadian Basin (4)
-
Scotia Sea Islands
-
South Shetland Islands (1)
-
-
South America
-
Andes (1)
-
Argentina (1)
-
Chile (1)
-
Patagonia (1)
-
-
Southern Ocean
-
Bransfield Strait (1)
-
-
Storegga Slide (1)
-
-
commodities
-
brines (1)
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heavy mineral deposits (1)
-
metal ores
-
chromite ores (3)
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platinum ores (1)
-
-
mineral deposits, genesis (1)
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mineral exploration (1)
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oil and gas fields (20)
-
petroleum
-
natural gas (10)
-
-
placers (1)
-
-
elements, isotopes
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carbon
-
C-13/C-12 (3)
-
C-14 (1)
-
-
isotope ratios (9)
-
isotopes
-
radioactive isotopes
-
C-14 (1)
-
Re-187/Os-188 (1)
-
-
stable isotopes
-
C-13/C-12 (3)
-
Nd-144/Nd-143 (2)
-
O-18/O-16 (3)
-
Os-188/Os-187 (1)
-
Re-187/Os-188 (1)
-
Sr-87/Sr-86 (1)
-
-
-
Lu/Hf (1)
-
metals
-
alkaline earth metals
-
magnesium (1)
-
strontium
-
Sr-87/Sr-86 (1)
-
-
-
gold (2)
-
platinum group
-
osmium
-
Os-188/Os-187 (1)
-
Re-187/Os-188 (1)
-
-
palladium (1)
-
platinum (2)
-
platinum ores (1)
-
-
rare earths
-
neodymium
-
Nd-144/Nd-143 (2)
-
-
-
rhenium
-
Re-187/Os-188 (1)
-
-
-
oxygen
-
O-18/O-16 (3)
-
-
phosphorus (1)
-
-
fossils
-
Chordata
-
Vertebrata
-
Pisces
-
Placodermi (1)
-
-
-
-
ichnofossils (2)
-
Invertebrata
-
Arthropoda
-
Mandibulata
-
Crustacea
-
Ostracoda (2)
-
-
-
Trilobitomorpha
-
Trilobita (1)
-
-
-
Mollusca
-
Cephalopoda
-
Ammonoidea (1)
-
-
-
Protista
-
Foraminifera (4)
-
Radiolaria (2)
-
-
-
microfossils (6)
-
palynomorphs
-
Dinoflagellata (4)
-
miospores
-
pollen (2)
-
-
-
Plantae
-
algae
-
Coccolithophoraceae (1)
-
diatoms (2)
-
nannofossils (1)
-
-
-
-
geochronology methods
-
Ar/Ar (3)
-
K/Ar (2)
-
Lu/Hf (1)
-
paleomagnetism (2)
-
Rb/Sr (1)
-
Re/Os (1)
-
Sm/Nd (1)
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U/Pb (11)
-
U/Th/Pb (1)
-
-
geologic age
-
Cenozoic
-
Quaternary
-
Holocene
-
middle Holocene (1)
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-
Pleistocene
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upper Pleistocene (1)
-
-
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Tertiary
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Neogene
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Pliocene (2)
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-
Paleogene
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Eocene
-
lower Eocene
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Ypresian (1)
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-
middle Eocene
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Bartonian (1)
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Lutetian (1)
-
-
upper Eocene
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Priabonian (1)
-
-
-
Oligocene (2)
-
Paleocene
-
lower Paleocene
-
K-T boundary (1)
-
-
upper Paleocene (4)
-
-
-
Zambales Ophiolite (1)
-
-
-
Dalradian (4)
-
Mesozoic
-
Cretaceous
-
Lower Cretaceous
-
Albian (1)
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Berriasian (1)
-
-
Upper Cretaceous
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Campanian (1)
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Coniacian (1)
-
K-T boundary (1)
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Maestrichtian (2)
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Senonian (1)
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Turonian (1)
-
-
-
Jurassic
-
Lower Jurassic
-
Dunlin Group (1)
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middle Liassic (1)
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Pliensbachian (1)
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Toarcian (1)
-
upper Liassic (1)
-
-
Middle Jurassic
-
Bajocian
-
Brent Group (2)
-
Ness Formation (1)
-
-
-
Upper Jurassic
-
Kimmeridge Clay (4)
-
Kimmeridgian (1)
-
Volgian (1)
-
-
-
-
Paleozoic
-
Cambrian
-
Upper Cambrian (1)
-
-
Carboniferous
-
Upper Carboniferous (1)
-
-
Devonian
-
Middle Devonian
-
Givetian (1)
-
-
Old Red Sandstone (3)
-
-
lower Paleozoic (1)
-
Ordovician
-
Lower Ordovician (1)
-
-
Silurian (5)
-
upper Paleozoic (1)
-
-
Precambrian
-
Archean
-
Neoarchean (3)
-
-
Lewisian Complex (1)
-
Stillwater Complex (1)
-
upper Precambrian
-
Proterozoic
-
Lewisian (1)
-
Mesoproterozoic
-
Laxfordian (1)
-
-
Neoproterozoic
-
Tonian (2)
-
-
Paleoproterozoic (1)
-
-
-
-
-
igneous rocks
-
igneous rocks
-
plutonic rocks
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diabase (1)
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diorites
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tonalite (1)
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-
granites
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charnockite (1)
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ultramafics
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chromitite (3)
-
peridotites
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harzburgite (1)
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lherzolite (1)
-
-
-
-
volcanic rocks
-
andesites
-
boninite (1)
-
-
basalts
-
alkali basalts
-
alkali olivine basalt (1)
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-
flood basalts (1)
-
mid-ocean ridge basalts (1)
-
-
komatiite (1)
-
pyroclastics
-
hyaloclastite (1)
-
tuff (2)
-
-
-
-
ophiolite (12)
-
-
metamorphic rocks
-
metamorphic rocks
-
amphibolites (1)
-
cataclasites (1)
-
gneisses
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orthogneiss (2)
-
-
marbles (1)
-
metaigneous rocks
-
metagabbro (1)
-
serpentinite (2)
-
-
metasedimentary rocks
-
metapelite (2)
-
-
metasomatic rocks
-
serpentinite (2)
-
-
mylonites
-
blastomylonite (1)
-
-
schists
-
greenschist (1)
-
-
-
ophiolite (12)
-
turbidite (6)
-
-
meteorites
-
meteorites (1)
-
-
minerals
-
alloys (1)
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antimonides (1)
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arsenides (2)
-
carbonates
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aragonite (1)
-
calcite (2)
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hydromagnesite (1)
-
-
minerals (1)
-
oxides
-
brucite (1)
-
chrome spinel (2)
-
chromite (2)
-
spinel group (1)
-
-
phosphates
-
apatite (2)
-
monazite (2)
-
-
platinum minerals (2)
-
silicates
-
framework silicates
-
feldspar group
-
alkali feldspar
-
anorthoclase (1)
-
K-feldspar (1)
-
sanidine (1)
-
-
-
silica minerals
-
opal
-
opal-A (1)
-
opal-CT (1)
-
-
quartz (2)
-
-
-
orthosilicates
-
nesosilicates
-
garnet group (2)
-
zircon group
-
zircon (9)
-
-
-
-
sheet silicates
-
chlorite group
-
chlorite (1)
-
-
clay minerals
-
smectite (1)
-
-
illite (1)
-
mica group
-
biotite (1)
-
muscovite (1)
-
-
serpentine group
-
antigorite (1)
-
serpentine (1)
-
-
-
-
sulfides
-
laurite (1)
-
pentlandite (1)
-
-
-
Primary terms
-
absolute age (18)
-
Africa
-
East Africa
-
Mozambique (1)
-
-
North Africa
-
Libya (1)
-
-
West Africa
-
Cameroon (1)
-
-
-
Antarctica
-
Antarctic Peninsula (1)
-
South Shetland Islands (1)
-
-
Arctic Ocean
-
Norwegian Sea
-
Voring Plateau (1)
-
-
-
Arctic region
-
Greenland
-
East Greenland (3)
-
-
Svalbard (3)
-
-
Asia
-
Arabian Peninsula
-
Oman (2)
-
Saudi Arabia (1)
-
-
Far East
-
Philippine Islands (1)
-
-
Middle East
-
Cyprus (1)
-
-
-
Atlantic Ocean
-
North Atlantic
-
Faeroe-Shetland Basin (39)
-
Gulf of Mexico (1)
-
North Sea
-
East Shetland Basin (4)
-
Viking Graben (3)
-
-
Northeast Atlantic (22)
-
Reykjanes Ridge (1)
-
Rockall Plateau (1)
-
Rockall Trough (4)
-
-
-
Atlantic Ocean Islands
-
Faeroe Islands (15)
-
Shetland Islands
-
Unst (11)
-
-
-
Atlantic region (3)
-
brines (1)
-
carbon
-
C-13/C-12 (3)
-
C-14 (1)
-
-
Cenozoic
-
Quaternary
-
Holocene
-
middle Holocene (1)
-
-
Pleistocene
-
upper Pleistocene (1)
-
-
-
Tertiary
-
Neogene
-
Pliocene (2)
-
-
Paleogene
-
Eocene
-
lower Eocene
-
Ypresian (1)
-
-
middle Eocene
-
Bartonian (1)
-
Lutetian (1)
-
-
upper Eocene
-
Priabonian (1)
-
-
-
Oligocene (2)
-
Paleocene
-
lower Paleocene
-
K-T boundary (1)
-
-
upper Paleocene (4)
-
-
-
Zambales Ophiolite (1)
-
-
-
Chordata
-
Vertebrata
-
Pisces
-
Placodermi (1)
-
-
-
-
clay mineralogy (2)
-
climate change (1)
-
continental shelf (12)
-
crust (8)
-
crystal chemistry (1)
-
crystal growth (1)
-
crystal structure (2)
-
data processing (6)
-
deformation (10)
-
diagenesis (9)
-
earthquakes (1)
-
economic geology (1)
-
Europe
-
Baltic region (1)
-
Pyrenees (1)
-
Southern Europe
-
Italy
-
Piemonte Italy
-
Lanzo Massif (1)
-
-
-
-
Western Europe
-
Ireland
-
Galway Ireland (1)
-
-
Scandinavia
-
Norway
-
Northern Norway (1)
-
-
-
United Kingdom
-
Great Britain
-
England
-
London Basin (1)
-
Somerset England (1)
-
-
Scotland
-
Argyllshire Scotland
-
Mull Island (1)
-
-
Great Glen Fault (3)
-
Hebrides
-
Inner Hebrides
-
Mull Island (1)
-
-
Outer Hebrides (1)
-
-
Highland region Scotland
-
Caithness Scotland (2)
-
-
Moine thrust zone (4)
-
Orkney Islands (3)
-
Scottish Highlands
-
Grampian Highlands (1)
-
-
Shetland Islands
-
Unst (11)
-
-
-
-
-
-
-
faults (21)
-
folds (7)
-
foliation (1)
-
fractures (2)
-
geochemistry (5)
-
geochronology (2)
-
geomorphology (1)
-
geophysical methods (46)
-
heat flow (4)
-
heavy mineral deposits (1)
-
ichnofossils (2)
-
igneous rocks
-
plutonic rocks
-
diabase (1)
-
diorites
-
tonalite (1)
-
-
granites
-
charnockite (1)
-
-
ultramafics
-
chromitite (3)
-
peridotites
-
harzburgite (1)
-
lherzolite (1)
-
-
-
-
volcanic rocks
-
andesites
-
boninite (1)
-
-
basalts
-
alkali basalts
-
alkali olivine basalt (1)
-
-
flood basalts (1)
-
mid-ocean ridge basalts (1)
-
-
komatiite (1)
-
pyroclastics
-
hyaloclastite (1)
-
tuff (2)
-
-
-
-
inclusions
-
fluid inclusions (5)
-
-
intrusions (11)
-
Invertebrata
-
Arthropoda
-
Mandibulata
-
Crustacea
-
Ostracoda (2)
-
-
-
Trilobitomorpha
-
Trilobita (1)
-
-
-
Mollusca
-
Cephalopoda
-
Ammonoidea (1)
-
-
-
Protista
-
Foraminifera (4)
-
Radiolaria (2)
-
-
-
isostasy (1)
-
isotopes
-
radioactive isotopes
-
C-14 (1)
-
Re-187/Os-188 (1)
-
-
stable isotopes
-
C-13/C-12 (3)
-
Nd-144/Nd-143 (2)
-
O-18/O-16 (3)
-
Os-188/Os-187 (1)
-
Re-187/Os-188 (1)
-
Sr-87/Sr-86 (1)
-
-
-
lava (3)
-
magmas (2)
-
mantle (5)
-
maps (1)
-
Mesozoic
-
Cretaceous
-
Lower Cretaceous
-
Albian (1)
-
Berriasian (1)
-
-
Upper Cretaceous
-
Campanian (1)
-
Coniacian (1)
-
K-T boundary (1)
-
Maestrichtian (2)
-
Senonian (1)
-
Turonian (1)
-
-
-
Jurassic
-
Lower Jurassic
-
Dunlin Group (1)
-
middle Liassic (1)
-
Pliensbachian (1)
-
Toarcian (1)
-
upper Liassic (1)
-
-
Middle Jurassic
-
Bajocian
-
Brent Group (2)
-
Ness Formation (1)
-
-
-
Upper Jurassic
-
Kimmeridge Clay (4)
-
Kimmeridgian (1)
-
Volgian (1)
-
-
-
-
metal ores
-
chromite ores (3)
-
platinum ores (1)
-
-
metals
-
alkaline earth metals
-
magnesium (1)
-
strontium
-
Sr-87/Sr-86 (1)
-
-
-
gold (2)
-
platinum group
-
osmium
-
Os-188/Os-187 (1)
-
Re-187/Os-188 (1)
-
-
palladium (1)
-
platinum (2)
-
platinum ores (1)
-
-
rare earths
-
neodymium
-
Nd-144/Nd-143 (2)
-
-
-
rhenium
-
Re-187/Os-188 (1)
-
-
-
metamorphic rocks
-
amphibolites (1)
-
cataclasites (1)
-
gneisses
-
orthogneiss (2)
-
-
marbles (1)
-
metaigneous rocks
-
metagabbro (1)
-
serpentinite (2)
-
-
metasedimentary rocks
-
metapelite (2)
-
-
metasomatic rocks
-
serpentinite (2)
-
-
mylonites
-
blastomylonite (1)
-
-
schists
-
greenschist (1)
-
-
-
metamorphism (10)
-
metasomatism (3)
-
meteorites (1)
-
mineral deposits, genesis (1)
-
mineral exploration (1)
-
mineralogy (2)
-
minerals (1)
-
Mohorovicic discontinuity (3)
-
North America
-
Appalachians (1)
-
-
Ocean Drilling Program
-
Leg 104 (1)
-
-
ocean floors (6)
-
ocean waves (1)
-
oceanography (1)
-
oil and gas fields (20)
-
orogeny (3)
-
oxygen
-
O-18/O-16 (3)
-
-
paleoclimatology (3)
-
paleoecology (3)
-
paleogeography (7)
-
paleomagnetism (2)
-
Paleozoic
-
Cambrian
-
Upper Cambrian (1)
-
-
Carboniferous
-
Upper Carboniferous (1)
-
-
Devonian
-
Middle Devonian
-
Givetian (1)
-
-
Old Red Sandstone (3)
-
-
lower Paleozoic (1)
-
Ordovician
-
Lower Ordovician (1)
-
-
Silurian (5)
-
upper Paleozoic (1)
-
-
palynomorphs
-
Dinoflagellata (4)
-
miospores
-
pollen (2)
-
-
-
paragenesis (1)
-
petroleum
-
natural gas (10)
-
-
petrology (6)
-
phase equilibria (1)
-
phosphorus (1)
-
placers (1)
-
Plantae
-
algae
-
Coccolithophoraceae (1)
-
diatoms (2)
-
nannofossils (1)
-
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Early Neoproterozoic (Tonian) subduction-related magmatism and tectonothermal activity in Shetland and northern mainland Scotland: implications for the tectonic evolution of NE Laurentia and Rodinia reconstructions
U–Pb apatite geochronology shows multiple thermal overprints within the Neoarchean foreland basement of the Faroe–Shetland Terrane
Using ground-penetrating radar to investigate deposits from the Storegga slide tsunami and other sand sheets in the Shetland Islands, UK
Petroleum generation and migration through the Faroe–Shetland Basin – the role of igneous intrusions
The use of a multi-sensor core scanner workflow as the backbone of a digital core repository
Abstract A core repository is a physical record of a country's or commercial organization's subsurface wealth. Some of the largest core repositories hold thousands of kilometres of core material and it is a challenge to turn this physical archive into an accessible digital resource for all. Non-destructive multi-sensor core logger, hyperspectral and X-ray imaging techniques offer a unique chance to rescue valuable data trapped within core samples, improving the way that a core repository delivers data to academic or industrial end users. Here we present a case study of an archived petroleum core acquired in 1985 at the Osprey Field, UK Continental Shelf. Data from the UK National Data Repository are augmented by a multi-sensor core logger, hyperspectral and X-ray dataset that is uploaded into a cloud-based digital repository. The data were analysed using a multi-variant analysis to reclassify the original lithological interpretations, uncovering a greater proportion of clay and cemented horizons than was previously interpreted. A workflow is established to optimize the use of legacy cores and exploit the abundance of data trapped within the core repository using continuous multi-sensor core scanning and imaging data, which are stored within the virtual environment for visualization and access to all.
Radioactive heat production variations in the Faroe–Shetland Basin: key new heat production, geological and geochronological data for regional and local basin modelling
Strike-slip influenced stratigraphic and structural development of the Foula Sandstone Group, Shetland: implications for offshore Devonian basin development on the northern UK continental shelf
Interaction between volcanic and non-volcanic systems and its implication for prospectivity in the Faroe–Shetland Basin, NE Atlantic continental margin
Interpreter's Corner: Practical application of global siliciclastic rock-property trends to AVA interpretation in frontier basins
Putative arthropod trace fossils from the Orcadian Basin at Achanarras Quarry (Middle Devonian of Scotland)
The Clair Field, Blocks 206/7a, 206/8, 206/9a, 206/12a and 206/13a, UK Atlantic Margin
Abstract The Clair Field is a giant oilfield containing in the region of 6–7 Bbbl of stock tank oil initially in place, located approximately 75 km west of the Shetland Islands. As such, it represents the single biggest hydrocarbon accumulation on the UK Continental Shelf. Clair was discovered in 1977, but first production did not occur from Phase 1 until 2005, after a lengthy appraisal period. The major appraisal milestone occurred in 1991 after well 206/8-8 proved up fractured clastic red beds of the Devonian Lower Clair Group. This was followed up with an extended well test on 206/8-10Z, which demonstrated the longer-term performance of the reservoir. Further appraisal on Clair Ridge led to the sanction of the Clair Ridge, which came on stream in November 2018. Following the Greater Clair appraisal programme in 2013–15, development options are currently being worked for Clair South, which will develop the Lower Clair Group reservoirs together with overlying shallow-marine reservoirs of the Cretaceous and Jurassic.
The Edradour Field, Block 206/4a, UK Atlantic Margin
Abstract The Edradour Field, located in Licence P1453 on Block 206/4a of the Faroe–Shetland Basin, was put on production in August 2017. It lies c. 50 km NW of the Shetland Islands in a water depth of c. 300 m, and consists of one subsea well that produces gas condensate from the Albian Black Sail Member of the Commodore Formation. It is part of a joint development scheme along with the Glenlivet Field that sees the commingled multiphase production transported to the Shetland Gas Plant via tieback to the pre-existing Laggan–Tormore flowlines. The Edradour single well development has reserves of 21 MMboe from a gas initially-in-place of 142 bcf. It is operated by Total E&P UK Ltd under the P1453 licence with Ineos E&P (UK) Ltd and SSE E&P UK Ltd as partners.
Abstract The Glenlivet Field, located in Block 214/30a within the Faroe–Shetland Basin, was put on production in August 2017. It lies approximately 70 km NW of the Shetland Islands, in a water depth of c. 440 m. The development consists of two subsea wells that produce gas condensate from the Paleocene Vaila Formation, which comprises deep-water turbidite deposits with excellent petrophysical properties. It is part of a joint development scheme along with the Edradour Field that sees the commingled multiphase production transported to the Shetland Gas Plant via tie-back to the pre-existing Laggan–Tormore flowlines. Glenlivet is operated by Total E&P UK Ltd under the P1195 licence since September 2014 with Ineos E&P (UK) Ltd and SSE E&P UK Ltd as partners.
Abstract The Laggan and Tormore fields are found within the Flett sub-basin of the Faroe–Shetland Basin. Situated 120 km west of the Shetland Islands in 600 m water depth, they are part of the deepest subsea development in the UK to date with a 143 km subsea tie-back to onshore facilities. The reservoirs are found within the T35 biostratigraphic sequence of the Paleocene Vaila Formation and comprise sand-rich turbiditic channelized lobes with good reservoir properties, separated by metric to decimetric shale packages. Laggan is a gas-condensate field, whereas Tormore fluid is a richer gas with a saturated oil rim. Seismic reservoir characterization is a key to the field development where differentiation of fluid type proved challenging. Both fields came on stream in 2016 as part of the Greater Laggan area development scheme.
The Schiehallion and Loyal fields, Blocks 204/20, 204/25a, 204/25b, 205/16 and 205/21b, UK Atlantic Margin
Abstract The Schiehallion subsea development comprises two fields, Schiehallion and Loyal, which are located approximately 200 km to the west of the Shetland Islands in the UK Continental Shelf. The Schiehallion and Loyal fields were discovered in late 1993 and 1994, respectively, with a combined oil-in-place of more than 2.3 Bbbl. The fields are developed under waterflood and were on production from 1998 to 2013. After an extended shut-in, the fields were brought back on line in 2017, through new floating production facilities. Most of the production to date has been from the Paleocene Vaila Formation deep-water turbidite, in the T31 and T34 reservoir intervals. The ongoing Quad 204 redevelopment drilling programme commenced in April 2015, has drilled and completed 21 wells to date, and is expected to continue for several more years. The campaign includes new producer–injector pairs and stand-alone wells to support existing well stock, targeting stacked turbidite reservoir intervals, including the youngest T35–T34 interval, the main T31 interval and the previously under-developed T28–T25 fairway. In addition to an active drilling programme, a 4D seismic survey was acquired and processed in 2018, and its interpretation is key to unlocking further potential sources of value in this mature field.
Abstract The Solan Field is a Jurassic reservoired oil accumulation located in Block 205/26a in the East Solan Basin, West of Shetland. The field was discovered in 1991 by the 205/26a-4 well which encountered oil in the Kimmeridgian to Early Volgian age Solan Sandstone and appraised between 1992 and 2009 by four wells and four sidetracks. Premier Oil farmed into Licence P.164 in 2011 and became operator. The reservoir, which is up to 100 ft thick, is a basin-floor turbidite sequence and is informally subdivided into a thick and good quality Upper Solan sandstone unit and a thinner, poorer quality, Lower Solan sandstone unit, separated by the laterally extensive Middle Solan unit. Whilst the reservoir sandstones are relatively clean (texturally and compositionally mature) and laterally extensive, sub-seismic structural and stratigraphic complexity resulted in a challenging field development. The field development to date comprises four subsea wells (two oil producers and two water injectors) tied back to a small jacket and topsides with an innovative subsea oil storage tank. Oil export is via shuttle tanker. First oil was achieved in April 2016. The field oil in place volume is in the range of 55–85 MMbbl.