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Beryl Embayment

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Journal Article
Published: 01 December 1991
Journal of the Geological Society (1991) 148 (6): 1037–1047.
...PHILIP C. RICHARDS Abstract Coastal plain and fan delta sediments accumulated throughout the Sinemurian to late Pliensbachian in the Beryl Embayment area, North Sea. These sediments represent a marginal, clastic fringe along the southern extension of the Boreal Ocean into the northern North Sea...
Journal Article
Published: 01 June 1991
Journal of the Geological Society (1991) 148 (3): 459–471.
...P. C. RICHARDS Abstract The Middle Jurassic Sleipner Formation is sub-divided into three units in the Beryl Embayment area of the North Sea. The lowermost two units, the 'Interbedded Unit' and 'Lower Coal Marker', overlie Lower Jurassic marine silts and were probably deposited in progressively...
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A) Map showing the location of the Beryl Embayment of the northern North Sea, and the location of wells 9/13a-S48 and 9/13a-S36 in the Beryl Field (Block 9/13a UKCS) (from Knutson and Munro 1991). B) Schematic block diagram showing the range of Triassic depositional environments and the possible distribution of facies types.
Published: 01 January 2002
Figure 1 A) Map showing the location of the Beryl Embayment of the northern North Sea, and the location of wells 9/13a-S48 and 9/13a-S36 in the Beryl Field (Block 9/13a UKCS) (from Knutson and Munro 1991 ). B) Schematic block diagram showing the range of Triassic depositional environments
Journal Article
Published: 01 January 2002
Journal of Sedimentary Research (2002) 72 (1): 18–29.
...Figure 1 A) Map showing the location of the Beryl Embayment of the northern North Sea, and the location of wells 9/13a-S48 and 9/13a-S36 in the Beryl Field (Block 9/13a UKCS) (from Knutson and Munro 1991 ). B) Schematic block diagram showing the range of Triassic depositional environments...
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Series: Geological Society, London, Memoirs
Published: 30 October 2020
DOI: 10.1144/M52-2018-91
EISBN: 9781786205070
... Abstract The Gryphon Field was discovered in 1987 in Quadrant 9 in the Beryl Embayment. Oil was encountered in a thick Balder Formation sandstone, and the reservoir was interpreted as lobes of a submarine fan system, such as many of the prolific early Tertiary fields in the North Sea. After...
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Journal Article
Published: 13 October 2020
Scottish Journal of Geology (2020) 56 (2): 175–195.
... wells contain ‘Boreal Bathonian' ammonites from the Arctic Realm. Arctocephalites from the Boreal Arcticus Zone (uppermost Bajocian) correlates basinal partly anoxic mudstones in the Beryl Embayment (9/13b) with both bioturbated siltstones in the southern Viking Graben (9/10b), and calcareous mudstones...
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Journal Article
Published: 01 April 1995
Journal of the Geological Society (1995) 152 (2): 251–258.
...W. I. DUNCAN; N. W. K. BUXTON Abstract The UKCS (United Kingdom Continental Shelf) well 9/16-3 drilled on the western flank of the Beryl Embayment encountered a Middle Devonian sequence interpreted as part of the lacustrine Orcadian Basin. An anhydrite layer found within the sequence provides...
Journal Article
Published: 01 August 1993
Journal of the Geological Society (1993) 150 (4): 796–798.
... Abstract P. Richards writes: Frostick et al. 1992 provide a very readable and concise account of the Triassic evolution of the Beryl Embayment area. The account is an analysis of a sedimentary succession often glossed over by previous workers, and they should be commended for attempting to explain...
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Higher-resolution palaeogeographical reconstructions of the East Shetland Platform during the Late Thanetian–Early Ypresian (Dornoch and Balder formations). BE, Beryl Embayment; CS, Crawford Spur. Source: adapted from Valore et al. (2024).
Published: 20 November 2024
Fig. 5. Higher-resolution palaeogeographical reconstructions of the East Shetland Platform during the Late Thanetian–Early Ypresian (Dornoch and Balder formations). BE, Beryl Embayment; CS, Crawford Spur. Source: adapted from Valore et al. (2024) .
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A simplified fault pattern frames the main structural highs and lows of the Scottish offshore, UK North Sea. BE Beryl Embayment; EP Erland Platform; F-MH Forties-Montrose High; HH Halibut Horst; ME Magnus Embayment; NP Northern Permian Basin; TS Tampen Spur; UB Unst Basin.
Published: 01 May 2000
Fig. 5. A simplified fault pattern frames the main structural highs and lows of the Scottish offshore, UK North Sea. BE Beryl Embayment; EP Erland Platform; F-MH Forties-Montrose High; HH Halibut Horst; ME Magnus Embayment; NP Northern Permian Basin; TS Tampen Spur; UB Unst Basin.
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Core from a Triassic playa lake setting in North Sea, Lewis Member, Beryl Embayment. Mud-draped foresets showing paired-drape bundles (white arrows) are similar to those seen in Figure 2B. Location of core is ∼400 km from nearest known marine deposits.
Published: 01 July 2012
Figure 5. Core from a Triassic playa lake setting in North Sea, Lewis Member, Beryl Embayment. Mud-draped foresets showing paired-drape bundles (white arrows) are similar to those seen in Figure 2B . Location of core is ∼400 km from nearest known marine deposits.
Image
 Location of Palaeocene depocentres in the North Sea Basin. OMFB, Outer Moray Firth Basin; CG, Central Graben; SVG, South Viking Graben; BE, Beryl Embayment; ESB, East Shetland Basin; HH, Halibut Horst; FP, Forties Platform; FGS, Fladen Ground Spur; FMH, Forties–Montrose High.
Published: 01 May 2004
Fig. 1.  Location of Palaeocene depocentres in the North Sea Basin. OMFB, Outer Moray Firth Basin; CG, Central Graben; SVG, South Viking Graben; BE, Beryl Embayment; ESB, East Shetland Basin; HH, Halibut Horst; FP, Forties Platform; FGS, Fladen Ground Spur; FMH, Forties–Montrose High.
Series: Geological Society, London, Petroleum Geology Conference Series
Published: 01 January 2018
DOI: 10.1144/PGC8.32
EISBN: 9781786203151
... seismic data and expansion of the near-field acreage position have been key to driving the growth in drilling opportunities. Apache and partners committed to underwrite the new broadband 3D seismic data across the entire Beryl Embayment in 2012 prior to the 27th UKCS licensing round ( Fig. 6...
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—Maps of relay ramps in the North Sea. Tick marks are shown on the downthrown sides of faults, and open circles represent oil or gas fields. (a) Map of the Beryl embayment (modified from Figure 1 of Swallow, 1986), which is a relay ramp between fault zones A and B. The approximate dip direction of the ramp is based on contours of the base of the Cretaceous, shown by GECO (1989). (b) Map of the Groningen gas field, which appears to be in a stage 3 relay ramp between fault zones A and B.
Published: 01 February 1994
Figure 16 —Maps of relay ramps in the North Sea. Tick marks are shown on the downthrown sides of faults, and open circles represent oil or gas fields. (a) Map of the Beryl embayment (modified from Figure 1 of Swallow, 1986 ), which is a relay ramp between fault zones A and B. The approximate
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Distribution of the Upper Jurassic synrift plays and their associated extensional fault systems. Deflation of the North Sea dome leads to the shallow-marine depositional systems backstepping to concentrate the fairways in the Witch Ground graben and South Halibut Basins of the Outer Moray Firth, southern parts of the Viking Graben (including the Beryl embayment), and in and on the margins of the Central Graben and Horda platform. The onset on major rifting subsequently leads to the development of basin-margin submarine fan aprons in the South Viking Graben and the erosion of footwall highs in the East Shetland Basin. Many of the tilted fault blocks of the Brent province develop shoreline clastic fringes to an island archipelago and deep-water turbidite reservoir sandstones on their dip-slopes and neighboring hanging-wall depocenters.
Published: 01 March 2022
Moray Firth, southern parts of the Viking Graben (including the Beryl embayment), and in and on the margins of the Central Graben and Horda platform. The onset on major rifting subsequently leads to the development of basin-margin submarine fan aprons in the South Viking Graben and the erosion
Journal Article
Published: 01 December 1990
Journal of the Geological Society (1990) 147 (6): 1085–1090.
... of the Norwegian oil and gas fields. 1987 London Graham and Trotman 253 264 Richards, P. C. 1989. Lower and Middle Jurassic sedimentology of the Beryle Embayment, and implications for the evolution of the northern North Sea. PhD thesis, University of Strathclyde. Richards P. C. Brown S...
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Location of the study area in the northern North Sea rift basin. (a) Regional setting; area of (b) illustrated. NOR = Norway; BE = Beryl Embayment-Brae area; MF = Moray Firth rift arm; NSD = location of North Sea Dome. Connecting dashed lines show axes of Late Jurassic trilete rift system. (b) Principal hydrocarbon fields and major normal faults in the northern North Sea basin; area of (c) illustrated. Hydrocarbon fields: SN = Snorre; ST = Statfjord; V = Visund; G = Gullfaks; B = Brent; S = Strathspey; A = Alwyn North. (c) Map of the study area as defined by the coverage of 3-D seismic data (Table 1). Trace of the Strathspey-Brent-Statfjord and Inner Snorre faults are shown at the truncation of the top prerift reflector in the hanging wall. Wells discussed in the text (Table 2) and the seismic lines shown in Figures 3 and 7 are annotated.
Published: 01 June 2002
Figure 1 Location of the study area in the northern North Sea rift basin. (a) Regional setting; area of (b) illustrated. NOR = Norway; BE = Beryl Embayment-Brae area; MF = Moray Firth rift arm; NSD = location of North Sea Dome. Connecting dashed lines show axes of Late Jurassic trilete rift
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Location of study area. (a) Structure map of the top of the Balder Fm in depth within the orange outline (c. 54.7 Ma) and key wells used for well-to-seismic ties (e.g. UK 204/22-2, Fig. 3c), with key sub-basins and structural elements (white lines). Background is present-day bathymetry from GEBCO. (b) Complete seismic and well dataset used in this study. The purple polygon shows the extent of data within the TGS J-Cube (a 3D-interpolated seismic volume created from 2D lines and additional vintage 3D data). AB, Annika Basin; BE, Beryl Embayment; CH, Corona High; CS, Crawford Spur; EB, Erlend Basin; EFH, East Faroe High; FB, Flett Basin; FH, Flett High; FSB, Faroe–Shetland basin; JB, Judd Basin; NNSB, Northern North Sea Basin. Source: (a) sub-basins and structural elements based on Stoker et al. (2012), Mudge (2015), Zastrozhnov et al. (2020) and our own mapping; (b) TGS J-Cube described by Whiteside et al. (2013) and TGS (2017).
Published: 20 November 2024
bathymetry from GEBCO. ( b ) Complete seismic and well dataset used in this study. The purple polygon shows the extent of data within the TGS J-Cube (a 3D-interpolated seismic volume created from 2D lines and additional vintage 3D data). AB, Annika Basin; BE, Beryl Embayment; CH, Corona High; CS, Crawford
Series: Geological Society, London, Memoirs
Published: 01 January 2003
DOI: 10.1144/GSL.MEM.2003.020.01.13
EISBN: 9781862393950
... operated partnership and participating interests in Blocks 9/13a, b and c are summarized in Table 1 . Pre-discovery History Fig. 2. Colour draped Base Cretaceous relief map of the Beryl Embayment (red, shallow; blue, deep). Illuminated from the northwest. Our understanding of the fields...
Series: Geological Society, London, Petroleum Geology Conference Series
Published: 01 January 2005
DOI: 10.1144/0060389
EISBN: 9781862394124
..., affording high confidence in the EnTec Seismic Inversion datasets. Structure The Nevis South Field is located in the Beryl Embayment, a prolific hydrocarbon province on the western margin of the South Viking Graben. The overall structural setting of the Beryl Embayment is one of a ramp-relay system...
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