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Breagh Field

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Series: Geological Society, London, Memoirs
Published: 30 October 2020
DOI: 10.1144/M52-2019-15
EISBN: 9781786205070
... ; Underhill 2003 ; Nesbit & Overshott 2010 ). This section will only focus on key events specific to the Breagh Field within the framework of the SNS. Development RWE Dea acquired a 70% interest from Sterling and the other non-operating partners and took operatorship in 2009. Sterling...
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Lithological log for Breagh Field well 42/13-4 showing the distribution of new records of Zoophycos. Bioturbation Index was recorded using the method of Taylor and Goldring (1993).
Published: 15 July 2020
Fig. 4. Lithological log for Breagh Field well 42/13-4 showing the distribution of new records of Zoophycos . Bioturbation Index was recorded using the method of Taylor and Goldring (1993) .
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Lithological log for Breagh Field well 42/13a-6 showing the distribution of new records of Zoophycos. Bioturbation Index was recorded using the method of Taylor and Goldring (1993). Key for lithologies is shown in Figure 4.
Published: 15 July 2020
Fig. 5. Lithological log for Breagh Field well 42/13a-6 showing the distribution of new records of Zoophycos . Bioturbation Index was recorded using the method of Taylor and Goldring (1993) . Key for lithologies is shown in Figure 4 .
Journal Article
Published: 26 February 2020
Petroleum Geoscience (2020) 26 (2): 204–231.
...Matthew G. Booth; John R. Underhill; Andy Gardiner; Duncan McLean Abstract Discovery of the Breagh gas field in the Southern North Sea (SNS) has demonstrated the potential that the Lower Carboniferous (Visean, 346.7–330.9 Ma) Farne Group reservoirs have to contribute to the UK's future energy mix...
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Onshore–offshore correlations based on palynology and limestone marker beds. The correlation has been anchored and flattened on the Oxford Limestone, which represents the youngest continuous marker in the Breagh Field. The correlation provides a basis for comparing and contrasting depositional sequences exposed on the Northumberland coast with electrical well logs and cores from the Breagh Field. The absence of Eelwell Limestone in the offshore sequences highlights the important role that incision by the Base Permian Unconformity (BPU) has in eroding and truncating the reservoir-bearing Visean sequence in Breagh, something that enhances prospectivity in the field. The inset map shows the location of the Breagh Field with the well correlation section. TVDSS, true vertical depth subsea.
Published: 26 February 2020
Fig. 14. Onshore–offshore correlations based on palynology and limestone marker beds. The correlation has been anchored and flattened on the Oxford Limestone, which represents the youngest continuous marker in the Breagh Field. The correlation provides a basis for comparing and contrasting
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Breagh closure analysis. Depth–structure map of the Base Permian Unconformity (BPU/top Rotliegend (base Zechstein)) composite surface. The outline of the Breagh Field, defined by the closing contour of the gas–water contact (GWC: 2337 m TVDSS) at the BPU level is shown in red. The largest possible closing contour (dashed grey) is mapped at 2440 m TVDSS giving an area 63% larger than the Breagh Field, indicating that the structure is underfilled.
Published: 16 April 2020
Fig. 19. Breagh closure analysis. Depth–structure map of the Base Permian Unconformity (BPU/top Rotliegend (base Zechstein)) composite surface. The outline of the Breagh Field, defined by the closing contour of the gas–water contact (GWC: 2337 m TVDSS) at the BPU level is shown in red
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Database map of the Breagh study area in Quadrants 41–43 showing the extent of the 3D seismic datasets (a subset of the PGS MegaSurvey 2015 and the INEOS Lochran 3D surveys), regional 2D lines, well control and the location of gas fields, including the Breagh Field. The orientation and locations of the well correlation and seismic sections A–A′ (Figs 5a and 6) and C–C′ (Figs 5b and 7), and seismic section E–E′ (Fig. 8) are indicated.
Published: 16 April 2020
Fig. 4. Database map of the Breagh study area in Quadrants 41–43 showing the extent of the 3D seismic datasets (a subset of the PGS MegaSurvey 2015 and the INEOS Lochran 3D surveys), regional 2D lines, well control and the location of gas fields, including the Breagh Field. The orientation
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Present-day depth (in metres) to the base Zechstein in the Southern North Sea. Modified after Peryt et al. (2010). The location of the Breagh Field is indicated in red. The map serves to show how gas expelled from active Carboniferous kitchen areas in the deeper parts of the basin (e.g. Silverpit Basin) during the Paleocene phase of gas expulsion would migrate updip towards the west. Breagh sits directly in the charge pathway of migrating gas and, being a local base Zechstein high, would have served to focus charge into the Breagh structure.
Published: 16 April 2020
Fig. 20. Present-day depth (in metres) to the base Zechstein in the Southern North Sea. Modified after Peryt et al. (2010) . The location of the Breagh Field is indicated in red. The map serves to show how gas expelled from active Carboniferous kitchen areas in the deeper parts of the basin
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Lithostratigraphic and biostratigraphic subdivision of Asbian–early Pendleian strata in Northumberland and the Breagh Field with schematic representation of principal limestone units and related miospore events in the studied sections. Studied sections are shaded to indicate intervals of continuous outcrop or core, or unshaded to indicate well sections without core. See the text for the explanation of the apparent discrepancy in the positions of the range tops of M. parthenopia and P. delicatus in Scremerston and Breagh (Clayton et al. 1978; Owens et al. 2004).
Published: 26 February 2020
Fig. 9. Lithostratigraphic and biostratigraphic subdivision of Asbian–early Pendleian strata in Northumberland and the Breagh Field with schematic representation of principal limestone units and related miospore events in the studied sections. Studied sections are shaded to indicate intervals
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Seismic section B–B′. SSW–NNE-orientated uninterpreted (above) and interpreted (below) seismic two-way travel time (TWTT) section across Quadrant 42. See Figure 4 for the location. The line passes from the Cleveland Basin onto the Dogger Shelf, transecting the Breagh Field and the Central Fracture Zone/North Dogger Fault Zone in the Mesozoic section. The section is orientated to intersect wells (gas fields) 41/22-1, 42/18-1 and 42/13-2, and wells (Breagh) 42/13-3 and 42/09-1, and is the equivalent transect to that shown in the correlation panel B–B′ (Fig. 5b). Seismic data are courtesy of ExxonMobil, INEOS, PGS and Total.
Published: 16 April 2020
Fig. 7. Seismic section B–B′. SSW–NNE-orientated uninterpreted (above) and interpreted (below) seismic two-way travel time (TWTT) section across Quadrant 42. See Figure 4 for the location. The line passes from the Cleveland Basin onto the Dogger Shelf, transecting the Breagh Field
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Seismic section C–C′. East–west-orientated (E–E′) (a) uninterpreted and (b) interpreted seismic two- way travel time travel (TWTT) section across the Lochran 3D survey, south of the Breagh Field. See Figure 4 for the location. Seismic data are courtesy of INEOS.
Published: 16 April 2020
Fig. 8. Seismic section C–C′. East–west-orientated (E–E′) ( a ) uninterpreted and ( b ) interpreted seismic two- way travel time travel (TWTT) section across the Lochran 3D survey, south of the Breagh Field. See Figure 4 for the location. Seismic data are courtesy of INEOS.
Journal Article
Published: 16 April 2020
Petroleum Geoscience (2020) 26 (2): 174–203.
...Fig. 19. Breagh closure analysis. Depth–structure map of the Base Permian Unconformity (BPU/top Rotliegend (base Zechstein)) composite surface. The outline of the Breagh Field, defined by the closing contour of the gas–water contact (GWC: 2337 m TVDSS) at the BPU level is shown in red...
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Thickness maps. Isopach maps depicting the major variations in stratigraphic thickness of: (a) the Zechstein Supergroup; (b) the Bacton Group; (c) the Lower Cretaceous–base Haisborough Group interval; and (d) the Chalk Group within the Breagh–Lochran area. Fault patterns at the top and base of the interval are indicated, along with the outline of the Breagh Field (in red). The Zechstein is thinned within the graben areas. A pronounced salt diapir occurs at the intersection between the two graben in the centre of the map. The Bacton Group is relatively consistent in thickness across the area. However, it is absent from the northern graben and severely thinned in the southern graben. The Lower Cretaceous is relatively thin across the area and the majority of the interval depicted by (a) is composed of Jurassic (mainly Lias Group) and Haisborough Group sections. The interval is appreciably thick within the centre of the Mesozoic graben, particularly in the south, indicating synsedimentary fault growth. The Chalk Group (b) is absent across much of the southern part of the study area and thickens NNE of the seabed subcrop. The orientation and locations of the well correlation and seismic sections A–A′ (Figs. 5a and 6) and B–B′ (Figs. 5b and 7), and seismic section C–C′ (Fig. 8) are indicated. The locations of the maps are indicated in Figure 4.
Published: 16 April 2020
at the top and base of the interval are indicated, along with the outline of the Breagh Field (in red). The Zechstein is thinned within the graben areas. A pronounced salt diapir occurs at the intersection between the two graben in the centre of the map. The Bacton Group is relatively consistent in thickness
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Structural analysis. (a) Depth–structure map Base Permian Unconformity (BPU/top Rotliegend (base Zechstein)) composite surface showing the main faults identified (white). (b) Map showing the main Permo-Carboniferous trends at base Zechstein level classed and coloured by the general strike orientation. Four main fault trends can be recognized, NNW–SSE, NW–SE, east–west and NE–SW, which can be divided into three broad fault domains of consistent structural style. The outline of the Breagh Field, defined by the closing contour of the gas–water contact (GWC: 2337 m TVDSS) at BPU level, is indicated in grey. The locations of seismic lines A–A′, B–B′ and C–C′ are also shown. The locations of the maps are indicated in Figure 4.
Published: 16 April 2020
strike orientation. Four main fault trends can be recognized, NNW–SSE, NW–SE, east–west and NE–SW, which can be divided into three broad fault domains of consistent structural style. The outline of the Breagh Field, defined by the closing contour of the gas–water contact (GWC: 2337 m TVDSS) at BPU level
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Regional map of the Southern North Sea (SNS) depicting the main fields (colour coded by reservoir age), hydrocarbon play fairways and structural elements of the Southern Permian Basin (SPB). See Figure 1 for the wider location. Modified after Underhill (2009) and Duguid and Underhill (2010). The Breagh Field is located on the NW margin of the basin in UKCS Quadrant 42. Depicted in red is the outline of the 3D seismic volume utilized in this study, and the extent of Figure 4 (stippled). Field abbreviations: Ali., Alison; Am., Amanda; Ba., Barque; Bai., Baird; Bess., Bessemer; Ca., Callisto; Clip., Clipper; Corv., Corvette; Deb., Deben; Gains., Gainsborough; Ga., Galahad; Gal., Galleon; Gan., Ganymede; Mo., Mordred; Ne., Newsham; Net., Nettleham; New., Newton-on-Trent; Ri., Rita; Sca., Scampton; Sta., Stainton; Thu., Thurne; Va., Vampire; Val., Valkyrie; Van., Vanguard; Vi., Viscount; Vi. A, Viking A; Vi. C, Viking C; Vic., Victoria; Vix., Vixen.
Published: 16 April 2020
(2010) . The Breagh Field is located on the NW margin of the basin in UKCS Quadrant 42. Depicted in red is the outline of the 3D seismic volume utilized in this study, and the extent of Figure 4 (stippled). Field abbreviations: Ali., Alison; Am., Amanda; Ba., Barque; Bai., Baird; Bess., Bessemer; Ca
Journal Article
Published: 15 July 2020
Proceedings of the Yorkshire Geological Society (2020) 63 (2): 135–145.
...Fig. 4. Lithological log for Breagh Field well 42/13-4 showing the distribution of new records of Zoophycos . Bioturbation Index was recorded using the method of Taylor and Goldring (1993) . ...
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Specimens of Zoophycos: 3a at outcrop in the Brigantian Upper Bath-House Wood Limestone Member, Alston Formation, Bucket Rocks foreshore, Berwick-upon-Tweed, Northumberland [NU 00523 53224]. 13 cm pen for scale; 3b at outcrop in loose blocks of Brigantian Alston Formation, High Cup Gill, Cumbria [NY 7335 2545]. Here the Zoophycos traces (arrowed) can be seen to permeate the limestone and occur on several horizons within the limestone bed. 36 cm hammer for scale; 3c: Vertical cored section through the Brigantian Eelwell Limestone equivalent, Yoredale Formation in southern North Sea Breagh Field well 42/13a-6 at 2323.64 m measured depth (uncorrected core depth). Abundant bioturbation with several ‘layers' of Zoophycos spreiten (arrowed) that could be parts of the same individual Zoophycos helix. Note that the lower ‘layer' of Zoophycos cross-cuts all other bioturbation structures in its path. Scale bar in 1 cm units.
Published: 15 July 2020
Breagh Field well 42/13a-6 at 2323.64 m measured depth (uncorrected core depth). Abundant bioturbation with several ‘layers' of Zoophycos spreiten (arrowed) that could be parts of the same individual Zoophycos helix. Note that the lower ‘layer' of Zoophycos cross-cuts all other bioturbation
Series: Geological Society, London, Special Publications
Published: 01 January 2019
DOI: 10.1144/SP471.5
EISBN: 9781786204103
... Abstract Following the play-opening successes of the Breagh and Pegasus gas fields, we evaluated the potential of the Visean and Namurian (Carboniferous) petroleum plays in the northern Dutch offshore. This evaluation incorporated seismic and well data from the Dutch, British and German North...
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Structure maps. (a) Base Permian Unconformity/top Rotliegend (base Zechstein) two-way travel time (TWT) structure map (ms); (b) depth–structure map (m) showing the gas–water contact (GWC) for the Breagh Field (2337 m TVDSS; red); (c) top Bacton Group depth–structure map, which reveals the major graben system in the supra-Zechstein overburden; and (d) average velocities (m s−1) at base Zechstein level. The depth map is the result of the depth conversion of the seismic dataset following seismic interpretation of key overlying seismic horizons, and calculation of velocity intervals determined from analysis of available well time–depth data. Importantly, the depth conversion incorporates: (i) the influence of the Mesozoic graben in the overburden; (ii) a variable subcrop of high-velocity sediments at the seafloor (i.e. Chalk); and (iii) the effect of late-stage regional tilting. See the text for the discussion. The orientation and locations of the well correlation and seismic sections A–A′ (Figs. 5a and 6) and B–B′ (Figs. 5b and 7), and seismic section C–C′ (Fig. 8) are indicated. The locations of the maps are indicated in Figure 4.
Published: 16 April 2020
Fig. 9. Structure maps. ( a ) Base Permian Unconformity/top Rotliegend (base Zechstein) two-way travel time (TWT) structure map (ms); ( b ) depth–structure map (m) showing the gas–water contact (GWC) for the Breagh Field (2337 m TVDSS; red); ( c ) top Bacton Group depth–structure map, which
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Breagh gas field well correlation panel. The line of section is as per the inset location map in Figure 14. Correlations are based on limestones and palynology data provided from adjacent mudstones. The wells are presented to scale and at true vertical depth. Note the structural trap formed at the Base Permian Unconformity (BPU) level with a high-quality Zechstein salt seal above and high net/gross river-dominated cycles beneath. TVDSS, true vertical depth subsea.
Published: 26 February 2020
Fig. 16. Breagh gas field well correlation panel. The line of section is as per the inset location map in Figure 14 . Correlations are based on limestones and palynology data provided from adjacent mudstones. The wells are presented to scale and at true vertical depth. Note the structural trap