- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
NARROW
GeoRef Subject
-
all geography including DSDP/ODP Sites and Legs
-
Atlantic Ocean
-
North Atlantic
-
North Sea
-
Forties Field (3)
-
-
-
-
Central Graben (1)
-
Europe
-
Western Europe
-
Scandinavia
-
Denmark (1)
-
Norway (1)
-
-
United Kingdom (2)
-
-
-
-
commodities
-
oil and gas fields (4)
-
petroleum
-
natural gas (1)
-
-
-
fossils
-
microfossils (1)
-
palynomorphs
-
Dinoflagellata (1)
-
-
-
geologic age
-
Cenozoic
-
Tertiary
-
Paleogene
-
Eocene (2)
-
Paleocene (3)
-
-
-
-
Mesozoic
-
Jurassic (1)
-
-
-
metamorphic rocks
-
turbidite (1)
-
-
minerals
-
silicates
-
orthosilicates
-
nesosilicates
-
garnet group (1)
-
-
-
-
-
Primary terms
-
Atlantic Ocean
-
North Atlantic
-
North Sea
-
Forties Field (3)
-
-
-
-
Cenozoic
-
Tertiary
-
Paleogene
-
Eocene (2)
-
Paleocene (3)
-
-
-
-
continental shelf (1)
-
Europe
-
Western Europe
-
Scandinavia
-
Denmark (1)
-
Norway (1)
-
-
United Kingdom (2)
-
-
-
geophysical methods (3)
-
Mesozoic
-
Jurassic (1)
-
-
oil and gas fields (4)
-
palynomorphs
-
Dinoflagellata (1)
-
-
petroleum
-
natural gas (1)
-
-
sea-level changes (1)
-
sedimentary rocks
-
carbonate rocks
-
limestone (1)
-
-
clastic rocks
-
sandstone (3)
-
-
-
sedimentary structures
-
soft sediment deformation
-
sandstone dikes (1)
-
-
-
well-logging (1)
-
-
sedimentary rocks
-
sedimentary rocks
-
carbonate rocks
-
limestone (1)
-
-
clastic rocks
-
sandstone (3)
-
-
-
turbidite (1)
-
-
sedimentary structures
-
sedimentary structures
-
soft sediment deformation
-
sandstone dikes (1)
-
-
-
-
sediments
-
turbidite (1)
-
Brimmond Field
Abstract This paper updates the earlier account of the Forties Field detailed in Geological Society Memoir 14 ( Wills 1991 ), and gives a brief description of the Brimmond Field, a small Eocene accumulation overlying Forties (Fig. 1 ).
Constraining the origin of reservoirs formed by sandstone intrusions: Insights from heavy mineral studies of the Eocene in the Forties area, United Kingdom central North Sea
Development of the Brimmond Sand Fairway
Abstract The Eocene age Brimmond Sand Fairway is situated along the north-eastern flank of the Paleocene Forties Field (UKCNS blocks 21/10 and 22/6). Located along the western margin of this Brimmond Fairway are well imaged remobilized sands that form the reservoir interval for the Maule and Tonto Fields and, along with deep-water channels, the Brimmond Field. These Eocene Brimmond sandstones are encased in the Horda Shale which provides the sealing lithology. The interpretation of these remobilized and injected sands is driven from geometries derived from 3D seismic and historic logging of thin sandstones in the Eocene interval. Conical shape features with sills and steep dykes are mapped, with seismic evidence of injection along active faults and fractures. The developments of the Brimmond, Maule and Tonto Fields has been successful due to impressive seismic imaging with inversion and Direct Hydrocarbon Indicator (DHI) volumes allowing the identification of hydrocarbon bearing remobilized sandstones, along with 4D data imaging un-swept areas.
Paleogeographic reconstruction at T84 (mid-Eocene) time, showing the presen...
Plots of apatite:tourmaline index (ATi), garnet:zircon index (GZi), and rut...
(A) Regional location showing the Forties and Gannet field areas, with expa...
Abstract The Forties Field, discovered by BP in 1970, is the largest oilfield on the UK Continental Shelf. It is trapped in a simple four-way dip closure, with a Paleocene turbidite sandstone reservoir. The Forties Field originally contained between 4.2 and 5 billion bbl of oil, with 2.75 billion bbl produced to June 2017. Production has been supported by water injection and the influx of a regional aquifer. The original development contained equally spaced producers with peripheral injectors. As the field matured, production was concentrated in the crestal parts of the field with injectors tending to be moved upflank. With the development of seismic lithology prediction and fluid detection, together with 4D seismic technology, it became possible in the late 1990s to target bypassed oil in unexpected locations throughout the field. In 2003, BP sold the field to Apache who were able to rejuvenate production, adding over 170 MMbbl oil reserves, with an extended drilling campaign targeting bypassed pay identified using seismic technologies. Production at the Forties facility has been further enhanced by the development of four satellite oilfields, Bacchus (Jurassic reservoir), Brimmond, Maule and Tonto (Eocene reservoirs), together with Aviat (Pleistocene reservoir) produced for fuel gas supply.
Plots of apatite:tourmaline index (ATi), rutile:zircon index (RuZi), and th...
Relative abundances of garnet types A, B, and C (as shown in Figure 7 ) in...
Garnet compositions in sandstones from the Maule, Brimmond, and Forties fie...
Reserve growth in oil fields of the North Sea
Characterizing the Paleocene turbidites of the North Sea: the Mey Sandstone Member, Lista Formation, UK Central Graben
Appendix A: Sources of additional data on each field
Appendix A contains a tabulation by field of approximately 900 published references and other publicly accessible sources covering around 500 UK fields, both developed and undeveloped, onshore and offshore. Where possible, hyperlinks to the source document are provided. Fields in production are current to the July 2020 OGA listing of consented fields. References listed include all relevant Geological Society (GS) publications including the Petroleum Geology Conference series 1–8 (only 4–8 published by GS), and PESGB DEVEX presentations up to and including DEVEX 2019, with content from multiple additional sources. Papers published by the Society of Petroleum Engineers are not routinely listed below but can be readily searched online via www.onepetro.org .
Abstract Observation of basin-scale networks of sandstone intrusions are described from subsurface studies and outcrop locations. Regional scale studies are prevalent in the volume and two new regionally significant subsurface sand injection complexes are described. Higher resolution studies, both outcrop and subsurface, show the small-scale complexity but high level of connectedness of sandstone intrusions. Discordance with bedding at all scales is diagnostic of sandstone intrusions. The propensity of hydraulic fractures to develop and fill with fluidized sand in a broad range of host rocks is demonstrated by examples from metamorphic and magmatic basement, and lignite. Terminology used to describe sandstone intrusions and other elements of sand injection complexes is diverse.
The habitat of bypassed pay in the Forties Field
Abstract The Forties Field, the largest oilfield in the UK North Sea, has been a prolific producer since its initial development. With an initial plateau rate of 500 000 bopd the field had produced some 2500 mmbo and the field rate had declined to 41 000 bopd by 2003 when the operatorship changed from BP to Apache. From 2004 to 2012, over 100 bypassed pay targets were drilled with a success rate of 75%, establishing a late life plateau of 50 000–60 000 bopd. The Forties reservoir is provided by Paleocene turbidites of the Forties Sandstone Member of the Sele Formation, deposited in a channelized proximal area of the Forties Fan. In this paper, the reservoir architecture is described, and bypassed pay examples are discussed in the context of the reservoir architecture and the production history. Bypassed pay is shown to occur in both the high net to gross channel axes and the heterogeneous wing deposits. Oil is trapped by subseismic channel architecture and subtle faulting. The occurrence of bypassed pay at a particular location is also shown to be dependent on the continually evolving pattern of injection and production within the field.
The tectonic and stratigraphic framework of the United Kingdom’s oil and gas fields
Abstract Onshore exploration success during the first half of the 20th century led to petroleum production from many, relatively small oil and gas accumulations in areas like the East Midlands, North Yorkshire and Midland Valley of Scotland. Despite this, the notion that exploration of the United Kingdom’s continental shelf (UKCS) might lead to the country having self-sufficiency in oil and gas production would have been viewed as extremely fanciful as recently as the late 1950s. Yet as we pass into the new century, only thirty-five years on from the drilling of the first offshore well, that is exactly the position Britain finds itself in. By 2001, around three million barrels of oil equivalent were being produced each day from 239 fields. The producing fields have a wide geographical distribution, occur in a number of discrete sedimentary basins and contain a wide spectrum of reservoirs that were originally deposited in diverse sedimentary and stratigraphic units ranging from Devonian to Eocene in age. Although carbonates are represented, the main producing horizons have primarily proved to be siliciclastic in nature and were deposited in environments ranging from aeolian and fluviatile continental red beds, coastal plain, nearshore beach and shelfal settings all the way through to deep-marine, submarine fan sediments. This chapter attempts to place each of the main producing fields into their proper stratigraphic, tectonic and sedimentological context in order to demonstrate how a wide variety of factors have successfully combined to produce each of the prospective petroleum play fairways and hence, make the UKCS such a prolific and important petroleum province.