The V-Fields, Blocks 49/16, 49/21/, 48/20a, 48/25b, UK North Sea

2003 ◽  
Vol 20 (1) ◽  
pp. 861-870
Author(s):  
James Courtier ◽  
Hugh Riches
Keyword(s):  
North Sea ◽  
Early Permian ◽  
The North ◽  
Recoverable Reserves ◽  
Production Wells ◽  
Exploration Drilling ◽  
Structural Relief ◽  
The Uk ◽  
Gas Fields ◽  
North And South

AbstractThe Vulcan, Vanguard, North and South Valiant gas fields are collectively known as the V-Fields and lie on the eastern flank of the Sole Pit Basin in the southern sector of the UK North Sea. They are contained within blocks 49/16, 49/21, 48/20a and 48/25b and are operated by Conoco (UK) Ltd. The first field to be discovered was South Valiant, in 1970, and the initial phase of exploration drilling continued until 1983, with the discovery of the North Valiant, Vanguard and Vulcan fields. Prominent faults and dip closures define the limits of the fields and gas is contained within aeolian sands of Early Permian age. The gross average reservoir thickness is approximately 900 ft with porosities ranging from 3-23% and permeabilities varying from 0.1 mD to 2 Darcies in producing zones. The development of the V-Fields consisted of drilling centrally located production wells in each field, targeting higher quality reservoir zones in areas of maximum structural relief. Initial gas-in-place is estimated at 2.6 TCF with recoverable reserves of about 1.6 TCF. The fields were brought on-stream in October 1988 and currently produce, as of November 1999, up to 260MMSCFD of gas through the LOGGS complex to the Conoco terminal at Theedle-thorpe, Lincolnshire.

The V-Fields, Blocks 49/16, 49/21, 48/20a, 48/25b, UK North Sea

1991 ◽  
Vol 14 (1) ◽  
pp. 497-502 ◽  
Author(s):  
M. J. Pritchard
Keyword(s):  
North Sea ◽  
Early Permian ◽  
Eastern Flank ◽  
Southern Sector ◽  
Recoverable Reserves ◽  
Exploration Drilling ◽  
The Uk ◽  
Gas Fields

AbstractThe Vulcan, Vanguard, North Valiant and South Valiant gas fields (collectively known as the 4 V-Fields) lie on the eastern flank of the Sole Pit Basin in the southern sector of the UK North Sea. They are contained within Blocks 49/16, 49/21, 48/25b and are operated by Conoco (UK) Limited. The first field to be discovered was South Valiant, in 1970 and exploration drilling continued until 1983 with the discovery of North Valiant, Vanguard and Vulcan Fields. Prominent faults and dip closures define the limits of the fields, and gas is contained within reservoir sands of Early Permian age, which are of desert origin. The gross average reservoir thckness is about 890 feet and porosities vary from 3-23% with permeabilities in producing zones varying from 0.1 md to 1950 md. Initial gas in place is estimated at 2.6 TCF with recoverable reserves of about 1.7 TCF. The fields were brought on-stream in October 1988 and produce, on average 325 MMSCFD of gas through the LOGGS complex to the Conoco/Britoil terminal at Theddlethorpe. Lincolnshire.

The Maria Field, Block 16/29a, UK North Sea

2020 ◽  
Vol 52 (1) ◽  
pp. 875-885 ◽  
Author(s):  
I. N. Stephens ◽  
S. Small ◽  
P. H. Wood
Keyword(s):  
North Sea ◽  
Upper Jurassic ◽  
Reservoir Properties ◽  
The North ◽  
Recoverable Reserves ◽  
Fault Block ◽  
Production Wells ◽  
The North Sea ◽  
The Uk ◽  
Clay Formation

AbstractThe Maria oilfield is located on a fault-bounded terrace in Block 16/29a of the UK sector of the North Sea, at the intersection of the South Viking Graben and the eastern Witch Ground Graben. The field was discovered in December 1993 by the 16/29a-11Y well and was confirmed by two further appraisal wells. The reservoir consists of shoreface sandstones of the Jurassic Fulmar Formation. The Jurassic sandstones, ranging from 100 to 180 ft in thickness, have variable reservoir properties, with porosities ranging from 10 to 18% and permeabilities from 1 to 300 mD. Hydrocarbons are trapped in a truncated rotated fault block, striking NW–SE. The reservoir sequence is sealed by Kimmeridge Clay Formation and Heather Formation claystones. Geochemical analysis suggests that Middle Jurassic Pentland Formation and Upper Jurassic Kimmeridge Clay Formation mudstones have been the source of the Maria hydrocarbons. Estimated recoverable reserves are 10.6 MMbbl and 67 bcf (21.8 MMboe). Two further production wells were drilled in 2018 to access unexploited areas.

The Gawain Field, Blocks 49/24, 49/29a, UK North Sea

2003 ◽  
Vol 20 (1) ◽  
pp. 713-722
Author(s):  
R. A. Osbon ◽  
O. C. Werngren ◽  
A. Kyei ◽  
D. Manley ◽  
J. Six
Keyword(s):  
North Sea ◽  
Early Permian ◽  
Water Contact ◽  
Field Development ◽  
Dune Sands ◽  
Southern North Sea ◽  
Recoverable Reserves ◽  
Structural Relief ◽  
Sandstone Formation

AbstractThe Gawain Field is located on the Inde shelf in the Southern North Sea, 85 km NE of the Norfolk coast. Gawain was discovered in 1970 by well 49/29-1 and a total of nine wells have been drilled on the structure. Gas is produced from the Leman Sandstone Formation of Early Permian age. The reservoir section is comprised predominantly of stacked aeolian dune sands possessing excellent poroperm characteristics. The structure is a complex NW-SE trending horst block with a common gas-water contact at 8904 ft TVDss. Low structural relief has presented a major challenge to field development, which has utilized extended reach wells to maximize drainage potential. Initial gas-in-place is estimated at 289 BCF with recoverable reserves in the order of 196 BCF. The field came on production in September 1995 via a sub-sea tie back to the Thames infrastructure and has an expected field life of 10 years

The Viking Complex Field, Blocks 49/12a, 49/16, 49/17, UK North Sea

1991 ◽  
Vol 14 (1) ◽  
pp. 509-515
Author(s):  
C. P. Morgan
Keyword(s):  
North Sea ◽  
Complex Field ◽  
Early Permian ◽  
Daily Production ◽  
Entire Field ◽  
Seasonal Demand ◽  
Southern North Sea ◽  
Recoverable Reserves ◽  
Gas Bearing ◽  
North And South

AbstractThe Viking complex consists of several separate gas accumulations within Blocks 49/12a, 49/16 and 49/17 of the southern North Sea. The entire field is located on the northeast flank of the Sole Pit Basin, approximately 140 km off the Lincolnshire coast. North Viking was discovered in March 1969; South Viking was discovered in December 1968. Conoco (UK) Ltd operates the Viking complex on behalf of BP. North and South Viking consist of two parallel elongated faulted anticlines trending NW-SE. The gas-producing structures are largely fault controlled. The reservoir comprises Rotliegendes Group sands of Early Permian age. The gas-bearing Rotliegendes consists of stacked aeolian and fluvial sands with a gross thickness range of 430-720 ft (131-222 m, thickest on South Viking). Porosities range from 7-25% and the average permeability range is 0.1 md to over 1000 md in the producing zones. The total Viking gas-in-place is almost 3.2 TCF, with recoverable reserves estimated at 2.83 TCF. North Viking came onstream in October 1972 and is developed by a five-platform complex. South Viking came onstream in August 1973 and is developed by a three-platform complex into which are linked five unmanned satellite platforms. The average daily production in March 1989 was 196 MMSCFD, peaking to 311 MMSCFD with seasonal demand. Gas is piped to the Conoco/BP terminal at Theddlethorpe in Lincolnshire.

The Flora Field, Blocks 31/26a, 31/26c, UK North Sea

2003 ◽  
Vol 20 (1) ◽  
pp. 549-555 ◽  
Author(s):  
R. D. Hayward ◽  
C. A. L. Martin ◽  
D. Harrison ◽  
G. Van Dort ◽  
S. Guthrie ◽  
...  
Keyword(s):  
North Sea ◽  
Upper Jurassic ◽  
Water Contact ◽  
Upper Carboniferous ◽  
The North ◽  
Recoverable Reserves ◽  
The North Sea ◽  
Oil Water ◽  
The Uk ◽  
Clay Formation

AbstractThe Flora Field straddles Blocks 31/26a and 31/26c of the UK sector of the North Sea on the southern margin of the Central Graben. The field is located on the Grensen Nose, a long-lived structural high, and was discovered by the Amerada Hess operated well 31/26a-12 in mid-1997.The Flora Field accumulation is reservoired within the Flora Sandstone, an Upper Carboniferous fluvial deposit, and a thin Upper Jurassic veneer, trapped within a tilted fault block. Oil is sourced principally from the Kimmeridge Clay Formation of the Central Graben and is sealed by overlying Lower Cretaceous marls and Upper Cretaceous Chalk Group.Reservoir quality is generally good with average net/gross of 85% and porosity of 21%, although permeability (Kh) exhibits a great deal of heterogeneity with a range of 0.1 to <10000mD (average 300 mD). The reservoir suffers both sub-horizontal (floodplain shales) and vertical (faults) compartmentalization, as well as fracturing and a tar mat at the oil-water contact modifying flow and sweep of the reservoir. Expected recoverable reserves currently stand at 13 MMBBL

25 years of UK North Sea exploration

1991 ◽  
Vol 14 (1) ◽  
pp. 1-7 ◽  
Author(s):  
J. M. Bowen
Keyword(s):  
United Kingdom ◽  
North Sea ◽  
Oil And Gas ◽  
The North ◽  
The United Kingdom ◽  
East Midlands ◽  
Daunting Task ◽  
Shallow Wells ◽  
The Uk ◽  
Gas Fields

Any attempt to summarize 25 years of exploration for petroleum in the UK sector of the North Sea must be a daunting task. The outcome, in terms of the oil and gas fields discovered, is the subject of this volume. This introduction will attempt to outline, very briefly, some of the ups and downs of the exploration history which has led the industry to where it stands today, 25 years on (Fig. 1).When the author was at university in the early 1950s the very idea the the United Kingdom would be likely to become a significant, let alone major world producer of petroleum would have been viewed as utterly ridiculousIt is true that oil and gas indications had been encountered in wells and mines in such disparate areas as sussex, the west Midlands and the Midland Valley of Scotland and as seepages in Dorset, Lancashire and West Lothian, but these had been thoroughly investigated without the discovery of any economically significant oil or gas fields. Indeed, the only economic production at that time came from BP's small east Midlands fields based on Eakring where the first discovery had been made in 1939The first Serious attempt to explore for oil in the United Kingdom was initiated in 1918 for strategic reasons, when 11 relatively shallow wells were drilled on anticlinal features in various parts of the country. of these only one, Hardstoft-1 in Derbyshire, discovered producible oil, but attempts to follow up the discovery were unsuccessful.Exploration then

The Maureen Field, Block 16/29a, UK North Sea

1991 ◽  
Vol 14 (1) ◽  
pp. 347-352 ◽  
Author(s):  
P. L. Cutts
Keyword(s):  
North Sea ◽  
Water Injection ◽  
Upper Jurassic ◽  
Reservoir Properties ◽  
Injection Wells ◽  
The North ◽  
Clay Shales ◽  
Gravity Flows ◽  
Production Wells ◽  
The Uk

AbstractThe Maureen Oilfield is located on a fault-bounded terrace in Block 16/29a of the UK Sector of the North Sea, at the intersection of the South Viking Graben and the eastern Witch Ground Graben. The field was discovered in late 1972 by the 16/29-1 well, and was confirmed by three further appraisal wells. The reservoir consists of submarine fan sandstones of the Palaeocene Maureen Formation, deposited by sediment gravity flows sourced from the East Shetland Platform. The Palaeocene sandstones, ranging from 140 to 400 ft in thickness, have good reservoir properties, with porosities ranging from 18-25% and permeabilities ranging from 30-3000 md. Hydrocarbons are trapped in a simple domal anticline, elongated NW-SE, which was formed at the Palaeocene level by Eocene/Oligocene-aged movement of underlying Permian salt. The reservoir sequence is sealed by Lista Formation claystones. Geochemical analysis suggests Upper Jurassic Kimmeridge Clay shales have been the source of Maureen hydrocarbons. Estimated recoverable reserves are 210 MMBBL. Twelve production wells have been drilled on the Maureen Field. A further seven water injection wells have been drilled to maintain reservoir pressure.

The Jasmine Field, Blocks 30/06 and 30/07a, UK North Sea

2020 ◽  
Vol 52 (1) ◽  
pp. 498-510 ◽  
Author(s):  
H. M. Lawrence ◽  
L. E. Armstrong ◽  
K. Ashton ◽  
A. D. Jones ◽  
I. E. Mearns
Keyword(s):  
North Sea ◽  
Near Field ◽  
Dynamic Modelling ◽  
Structural Complexity ◽  
Late Triassic ◽  
Field Development ◽  
Well Production ◽  
Production Wells ◽  
Exploration Drilling ◽  
The Uk

AbstractThe high-pressure–high-temperature Jasmine Field lies 270 km east of Aberdeen in the UK Central North Sea and forms part of Chrysaor’s J-Area. Hydrocarbons were discovered at Jasmine in 2006, in Middle–Late Triassic fluvial sandstones of the Joanne Sandstone Member of the Skagerrak Formation. Appraisal proved a greater than 2000 ft hydrocarbon column and, in 2010, the Jasmine Field development was sanctioned. Five development wells were pre-drilled between 2010 and 2013, and the field was brought on line in November 2013, after which one further appraisal and three additional production wells were drilled. Jasmine infrastructure comprises an accommodation platform and a wellhead platform tied back to a riser platform adjacent to the Judy processing and export facility.Rapid early pressure depletion, a highly layered fluvial reservoir, structural complexity and variable fluid types present significant challenges for both static and dynamic modelling. Following production start-up, acquisition of new post-production reservoir pressure and flow data, and incorporation of allocated well production data, have been used to address these modelling challenges, and to provide encouragement for future infill and near-field exploration drilling opportunities.

The geosolitonic concept of high output hydrocarbon deposits formation

2021 ◽  
pp. 13-22
Author(s):  
R. M. Bembel ◽  
S. R. Bembel ◽  
M. I. Zaboeva ◽  
E. E. Levitina
Keyword(s):  
Western Siberia ◽  
Oil And Gas ◽  
Chemical Elements ◽  
Seismic Exploration ◽  
Oil And Gas Fields ◽  
Recoverable Reserves ◽  
Production Wells ◽  
Cumulative Production ◽  
Gas Fields ◽  
Hydrocarbon Deposits

Based on the well-known results of studies of the ether-geosoliton concept of the growing Earth, the article presents the conclusions that made it possible to propose a model of thermonuclear synthesis of chemical elements that form renewable reserves of developed oil and gas fields. It was revealed that local zones of abnormally high production rates of production wells and, accordingly, large cumulative production at developed fields in Western Siberia are due to the restoration of recoverable reserves due to geosoliton degassing. Therefore, when interpreting the results of geological and geophysical studies, it is necessary to pay attention to the identified geosoliton degassing channels, since in the works of R. M. Bembel and others found that they contributed to the formation of a number of hydrocarbon deposits in Western Siberia. When interpreting the results of geological-geophysical and physicochemical studies of the fields being developed, it is recommended to study the data of the ring high-resolution seismic exploration technology in order to identify unique areas of renewable reserves, which can significantly increase the component yield of hydrocarbon deposits.

Conversaziones, 1971

1971 ◽  
Vol 26 (2) ◽  
pp. 125-133
Keyword(s):  
North Sea ◽  
Oil Fields ◽  
Scale Model ◽  
British Petroleum ◽  
The North ◽  
Company Limited ◽  
The North Sea ◽  
Seismic Sections ◽  
Petroleum Company ◽  
Gas Fields

CONVERSAZIONES were held this year on 6 May and 24 June. At the first conversazione twenty-four exhibits and a film were shown. Dr P. E. Kent, F.R.S., and Mr P. J. Walmsley of The British Petroleum Company Limited arranged an exhibit demonstrating the latest progress in the exploration for hydrocarbons in the North Sea. The established gas fields and the recently discovered oil fields were shown on maps together with sections which illustrated their structure. Seismic sections and geological interpretations were exhibited to show the type of information being obtained in the North Sea and the structural complexities which arise. A scale model of one of the semi-submersible drilling outfits used in North Sea exploration was on display together with a sample of British North Sea oil.

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