Key Elements of the Petroleum Systems of the Rockall and Slyne-Erris Basins

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Key Elements of the Petroleum Systems of the Rockall and Slyne-Erris Basins Bandon Corrib Dooish Atlantic Ireland Conference, Dublin, 1 st - 2 nd November 2016

Rockall and Slyne-Erris Basins Only 11 exploration wells drilled to date Three proven hydrocarbon systems Dooish Discovery Upper Jurassic sourced gas-condensate in Middle Jurassic & Permian sst reservoirs Corrib Field Carboniferous sourced gas in Triassic sandstone reservoir Bandon Discovery Lower Jurassic sourced oil in Lower Jurassic sandstone reservoir Proven reservoirs Cretaceous, Middle Jurassic, Lower Jurassic, Triassic, Permian & Carboniferous Proven source rocks Lower Jurassic, Upper Jurassic & Carboniferous Rockall Basin Dooish Erris Basin Corrib Slyne Basin Bandon

North Atlantic Petroleum Systems Context Irish Atlantic shares geology with Newfoundland, UK, Faroe & Norwegian Atlantic margins Numerous rifted basins and more than one proven play Slyne-Erris and Rockall Basins are located in the centre of this trend Slyne-Erris and Rockall Basins contain one field and two discoveries, representing three hydrocarbon systems Dooish (gas-condensate) Corrib (gas) Bandon (oil) Jeanne-d Arc Basin: restricted marine Upper Jurassic (Kimmeridgian) Egret Formation source Flemish Pass Basin: Upper Jurassic (Kimmeridgian) Egret Formation source Porcupine Basin: restricted marine Upper Jurassic + lacustrine (algal) middle Jurassic sources Slyne Basin Bandon Discovery marine Lower Jurassic (Liassic) source Rockall Basin Dooish Discovery probable Upper Jurassic source Slyne Basin Corrib Field Carboniferous coal measures source UK Rockall Basin Benbecula Discovery unknown gas source Faroe-Shetland Basin: Upper Jurassic (Kimmeridgian-Volgian) Kimmeridge Clay Fm. marine source Plate Reconstruction at Barremian, 130 Ma (After Spencer & MacTiernan, 2001)

Rockall Basin: The Key Play Elements Location Map Dooish Irish Rockall Basin Stratigraphy RESERVOIR SOURCE SEAL EOCENE possible proven PALAEOCENE Sandstone reservoirs Shale (oil) & gas (coal) source rocks Shale regional top-seal Volcanics, particularly to the west Porcupine Basin Serica acreage Condensate discovery Gas discovery / field Oil discovery Map from PAD (2016) UPPER CRETACEOUS LOWER CRETACEOUS proven likely possible proven UPPER JURASSIC proven proven proven MIDDLE JURASSIC LOWER JURASSIC TRIASSIC PERMIAN proven possible possible possible proven proven CARBONIFEROUS proven proven CARBONIFEROUS proven proven

Rockall Basin: Dooish Discovery Kimmeridge Clay Formation Residual gas on CPI Westphalian C & older Coal Measures 12/2-2 West Dooish Dooish & West Dooish wells prove: Jurassic, Permian and Carboniferous reservoirs Late Jurassic (Volgian) Jurassic Kimmeridge Clay oilprone source rock Carboniferous Coal Measures gas-prone source rocks Effective Cretaceous top-seal Early Cretaceous Middle Jurassic (Bathonian-Bajocian) Permian 12/2-1z Dooish Discovery High GR Bathonian- Bajocian sands Clean sands Permian Westphalian C & older Coal Measures Dooish Discovery Structural trap below Base Cretaceous High N/G Middle Jurassic and Permian reservoir, average Ø 14% 214m 45 API gas condensate column Geochemical analysis suggested mixed terrestrial/marine source rock at peak maturity Core analysis suggests early oil charge flushed by later wet gas charge Upper Jurassic oil-prone source? - With possible Carboniferous component

Rockall Basin: Regional Seismic Line (1) Structural traps below Base Cretaceous including Dooish Discovery, 1s Muckish & Muckish East Prospects Re-mobilisation of sands across Erris Ridge and redeposition as turbidite fans during Aptian-Albian stratigraphic targets Upper Jurassic source kitchens in half-grabens below Base Cretaceous 5/22-1 12/2-1,1z 12/2-2 Rockall Basin N Erris Ridge 12/13-1A S Thick early Cretaceous and Triassic sandstones in 12/13-1A 1s Base Miocene 2s 2s Top Mid. Eocene 3s Top Maastrichtian Top Lr. Eocene Stratigraphic trapping potential Base Santonian Top Palaeocene 3s Nr. Top Turonian 4s 4s Base U. Cret. Base Cretaceous 5s Carboniferous source rocks within pre-rift Muckish East Prospect Muckish Prospect Dooish Discovery 5s

Rockall Basin: Regional Seismic Line (2) Structural traps below Base Cretaceous including Dooish Discovery, Muckish and Aghla More Prospects Turbidite fans of Aptian-Albian including the Derryveagh Prospect 2s 3s Top Palaeocene Top Maastrichtian SW Rockall Basin 12/2-2 12/2-1,1z 5/22-1 Rockall Basin Muckish Prospect NE 2s 3s 4s UK West of Shetlands and Atlantic West Africa stratigraphic trapping analogues Base Chalk Nr. Top Albian Mid Aptian 5s 6s Base Cret. Derryveagh Prospect (stratigraphic) Aghla More Prospect Dooish Discovery

Rockall Basin: Potential Carboniferous Source Geographic distribution of slicks, (satellite mapping) suggests more than one working hydrocarbon system Slick Mapping Study 2014 (CGG s Satellite Mapping Group) Note possible seepage slick close to prospect Note cluster of possible seepage slicks along offsetting fault Top Carboniferous 1743ft TVDSS 13/13-1 Well (Carboniferous top 250m) Gamma Ray Resistivity Sonic No thick Jurassic basins to SE of Erris Basin; therefore, slicks in this area probably have a Palaeozoic origin Dooish 12/2-1 and West Dooish 12/2-2 tagged the top of the Carboniferous Dooish 13/13-1 Coal Seam Sandstone 13/13-1 (nearby Donegal Basin) penetrated 800m of classic Carboniferous Coal Measures Dooish gas-condensate may have both a Carboniferous oil and gas component? Repeated seepage slicks: if Repeated seepage slicks: if these are genuine this implies a these are genuine this working Palaeozoic source implies kitchen a (no working known Palaeozoic Jurassic in source kitchen this area) (no known Jurassic in this area)

Slyne - Erris Basins: The Key Play Elements Location Map Irish Rockall Basin Sandstone reservoirs Shale (oil) & gas (coal) source rocks Shale or salt regional top-seal Corrib Bandon Porcupine Basin Serica acreage Condensate discovery Gas discovery / field Oil discovery Map from PAD (2016) Stratigraphy RESERVOIR SOURCE SEAL EOCENE PALAEOCENE Volcanics in North Slyne & Erris basins UPPER CRETACEOUS Thick chalk (where not eroded) LOWER CRETACEOUS Typically absent or highly condensed UPPER JURASSIC MIDDLE JURASSIC LOWER JURASSIC possible proven possible proven proven proven proven TRIASSIC proven Proven PERMIAN possible Proven CARBONIFEROUS possible proven

100m vertical scale Slyne Basin: Corrib Field Complex faulted roll-over anticline with Triassic Sherwood Sandstone reservoir and Mercia Halite top-seal Subsurface interpretation initially hampered by poor-quality seismic data 1 tcf dry gas in place, sourced from Carboniferous Coal Measures Thick, high-quality reservoir capable of strong delivery rates; e.g. 18/25-1 64mmscfg/d Corrib Field Top Sherwood Sandstone Reservoir Depth Map Corrib Field 2D Seismic Line Corrib 18/25-1 Well Mercia Halite top - seal Sherwood sandstone reservoir Permian Halite bottom seal 64 mmscfg/d, 80/64 choke 18/25-1 Carboniferous Coal Measures gas source 2D Seismic line and Top Sherwood Depth Map images from Corcoran & Mecklenburgh, 2005

1100m 1050m TWT(s) Slyne Basin: Bandon Discovery Bandon Discovery: complex faulted anticline with 38m oil column in high-quality Lower Jurassic reservoirs STOOIP 12mmbo proven within one fault compartment Proven Lower Jurassic oil source has de-risked the Jurassic play in the basin e.g. Boyne Prospect Triassic Sherwood Sandstone upside with Carboniferous gas source 27/4-1 log Interpretation W 27/4-1,1z 27/5-1 E 150m thick immature oil prone source rocks in Lower Jurassic Bandon Discovery: 38m oil column in high quality Lower Jurassic sandstones 0.5 1.0 1.5 Boyne Prospect Middle Jurassic Oil shows in high quality Middle Jurassic sandstones Triassic Sherwood Sandstone Permian halite Carboniferous Coal Measures Ro 0.7% + 2.0 Lower Jurassic Triassic Sherwood Sandstone 2.5 Mature gas prone Carboniferous source rocks 3D Seismic PreSTM (2008) Triassic Mature oil prone Lower Jurassic source rocks

100m vertical scale Slyne Basin: Source Rocks Extensive, thick Lower Jurassic Portree & Pabba Shale oil source in juxtaposition with reservoir sandstones Bandon Discovery has confirmed direct link between oil & source Deeper Carboniferous gas source can charge Triassic Sherwood Sst N Corrib 18/20-1 Corrib 18/25-1 38m oil column Mid Jurassic Unconformity (top Bajocian Limestone Marker) Bajocian Lst. Bandon 27/4-1 27/5-1 27/13-1 Triassic Sherwood sandstone Bajocian Lst. S correlation Lower Jurassic Suisnish Sandstone Westphalian C & older Coal Measures

Depth (mss) Slyne Basin: Jurassic Source Rocks, 27/4-1,1z Portree Shale Formation Source rocks geochemically matched to 27/4-1/1z oil samples Immature at well location but mature in basin centre Well 27/4-1,1z Source Potential S2 (kg/tonne) Organic Richness (TOC %wt) Active Total Organic Carbon Source Rock Quality HI (mgs2/gtoc) Depth (mtvdss) 200 300 400 500 600 700 800 900 1000 1100 1200 27/4-1,1z Vitrinite Reflectance (Ro%) Vitrinite Reflectence Ro (%) 0.1 1.0 10.0 0 Top 100 early mature oil window at Ro 0.5% 27/4-1 Ro (%) 27/4-1z Ro (%) seabed 273 mss Portree Shale Fm. Pabba Shale is faulted out 1300 27/4-1,1z 1400 1500 1600 1700 1800 1900 2000 Lower Jurassic oil source rocks not quite reached early oil window at well location, but certainly mature in basin centre

Carboniferous Coal Measures Depth (mss) Depth (mtvdss) Slyne Basin: Carboniferous Source Rocks, 27/5-1 Well 27/5-1 Thick coal measures (at least 270m) proven by 27/5-1 on the eastern flank of the Slyne Basin Immature for gas generation at well location, but mature in the basin centre Gamma Ray Resistivity Sonic Dolerite Sill 1614.5 mtvdss 27/5-1 Vitrinite Reflectence Reflectance Ro (%) (Ro%) 0.1 1.0 10.0 0 100 27/5-1 Ro (%) 200 seabed 273 mss 300 400 500 600 700 800 900 1000 1100 1200 1300 1400 1500 1600 1700 1800 1900 2000 27/5-1 Well TD 1883.5 mtvdss Coal Seam Sandstone Carboniferous coals within oil window at well location

Petroleum Systems of the Rockall and Slyne-Erris Basins: Conclusions Despite limited drilling in Slyne-Erris & Rockall Basins, there are: Bandon Proven reservoirs at multiple levels Corrib Cretaceous, Middle Jurassic, Lower Jurassic, Triassic, Permian, Carboniferous Proven source rocks Lower Jurassic, Upper Jurassic, Carboniferous Three hydrocarbon discoveries Dooish (gas-condensate), Corrib (gas) & Bandon (oil) Dooish Improvements in seismic data quality coupled with falling costs of seismic data acquisition and drilling offer real opportunities to unlock value