United Kingdom Oil and Gas Fields: 50th Anniversary Commemorative Volume

Geological Society Memoir 52 records the extraordinary journey of more than 50 years that has led to the development of some 458 oil and gas fields on the UK Continental Shelf (UKCS). It contains papers on almost 150 onshore and offshore fields in all of the UK's main petroliferous basins. These papers range from look-backs on some of the first-developed gas fields in the Southern North Sea, to papers on fields that have only just been brought into production or may still remain undeveloped, and includes two candidate CO2 sequestration projects.
These papers are intended to provide a consistent summary of the exploration, appraisal, development and production history of each field, leading to the current subsurface understanding which is described in greater detail. As such, the Memoir will be an enduring reference source for those exploring for, developing, producing hydrocarbons and sequestering CO2 on the UKCS in the coming decades. It encapsulates the petroleum industry's deep subsurface knowledge accrued over more than 50 years of exploration and production.
The Penguins Cluster, Blocks 211/13a and 211/14, UK North Sea Available to Purchase
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Published:October 30, 2020
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CitationD. Thorpe, M. Porter, T. McKie, L. J. Ritchie, 2020. "The Penguins Cluster, Blocks 211/13a and 211/14, UK North Sea", United Kingdom Oil and Gas Fields: 50th Anniversary Commemorative Volume, G. Goffey, J. G. Gluyas
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Abstract
The Penguins Cluster of fields are owned jointly (50:50) by Shell UK Ltd (Shell) and Esso Exploration and Production UK Ltd (Esso), with Shell as the operator. The cluster was discovered in 1974 and is composed of a combination of oil and gas condensate accumulations located 50–65 km north of the Brent Field, at the northern end of the North Viking Graben. Two main producing reservoirs are present: the Penguins West Field (Penguin A) consists of an Upper Jurassic Magnus Sandstone Member reservoir, while the Penguins East Field (Penguin C, D and E) consists of a Middle Jurassic Brent Group reservoir, underlain by currently undeveloped Statfjord and Triassic (Cormorant) reservoirs. The Magnus reservoir is composed of turbidite sands with an average porosity of 15% and permeabilities of 0.10–300 mD. The Brent reservoirs are composed of deltaic shoreface deposits with an average porosity of 14% and permeabilities of 0.01–1000 mD.
The fields were brought on stream in 2003 as a subsea development via what at the time was the world's longest comingled tieback to the Brent Charlie facility. A total of nine producing wells have been drilled from four subsea manifolds, producing c. 78 MMboe to date through depletion drive.
- Atlantic Ocean
- Bajocian
- Brent Group
- condensates
- development
- Dunlin Group
- Europe
- history
- Jurassic
- kerogen
- Kimmeridge Clay
- landform evolution
- lithostratigraphy
- Lower Jurassic
- Mesozoic
- Middle Jurassic
- Norian
- North Atlantic
- North Sea
- oil and gas fields
- permeability
- petroleum
- petroleum accumulation
- petroleum exploration
- plate tectonics
- reservoir properties
- Rhaetian
- rifting
- source rocks
- Statfjord Formation
- Triassic
- United Kingdom
- Upper Jurassic
- Upper Triassic
- Viking Graben
- Western Europe
- Magnus Sandstone Member
- Cormorant Formation
- Penguins West Field
- Penguins East Field
- Penguis Cluster Fields