Assessing our untapped energy resources. Derek Reay Geological Survey of Northern Ireland
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1 Assessing our untapped energy resources Derek Reay Geological Survey of Northern Ireland
2 Talk Outline Northern Ireland energy market Oil and Gas Exploration Description Exploration risks Application of Tellus data to oil and gas exploration General Examples Geothermal energy resources
3 NI Energy Infrastructure
4 Elements of petroleum exploration play Elements Organic-rich source rock Permeable reservoir rock Impermeable caprock Efficient trap Processes Source maturation Trap formation Hydrocarbon migration Relative timing of processes is crucial!
5 Petroleum exploration play areas and current licences
6 Exploration in the Northwest Irish Carboniferous Basin Source Carboniferous shale Reservoir Carboniferous sandstone Caprock Carboniferous shale Traps 1. Anticlines 2. Flower structures 3. Basin-centred gas
7 Flower structure from Belhavel - Castle Archdale fault system
8 Northeast Permo-Triassic Basins Source: Carboniferous coal/shale Reservoirs: 1. Carboniferous sandstones 2. Early Permian sandstones 3. Triassic SSG sandstones Caprocks: 1. Carboniferous mudstones 2. Late Permian salt/mudstone 3. Triassic MMG salt/mudstone Traps: 1. Tilted fault blocks 2. Anticlines 3. Fan deposits
9 Structural traps in the Permo-Triassic Basins MMG Mercia Mudstone Group (Caprock) SSG Sherwood Sandstone Group (Reservoir) MMG SSG LPS CM LC LPS Lower Permian Sandstone (Reservoir) CM Coal Measures (Source) LC Lower Carboniferous mudstones (Source)
10 Exploration risks/ negative factors Southwest play area Low permeability tight reservoir Identification of traps Timing of migration and trap formation Northeast play area Poor imaging of sub-basalt structure Source rock distribution and maturity Timing of migration and trap formation Post-migration leakage
11 Applications of Tellus data to oil & gas exploration Tellus geophysical data is used to Map faults deduce structural history Refine mapped geological boundaries Identify igneous intrusions Can also be used for Depth to basement modelling Integration with other geophysical data (seismic, gravity) to produce more realistic exploration models
12 Total magnetic intensity Magnetic domains Major lineaments Intrusions Dyke swarms
13 Magnetic pseudogravity Structural domains
14 Magnetic pseudogravity Horizontal gradient Lineaments Boundaries
15 Electromagnetic (EM) data Rock units
16 Fermanagh Tellus electromagnetic data and geology
17 Fermanagh total magnetic intensity and geology
18 Larne Basin Total Magnetic intensity EM data RTP
19 Underground gas storage in salt beds Larne and Islandmagee Larne No. 2 salt salt 900- salt Geology Magnetics RTP Magnetics 1 st Vert. Deriv. Caverns need to avoid faults and basalt dykes m salt Tellus data will improve the structural mapping in the prospective areas
20 Geothermal energy resource potential Types of geothermal resource Shallow geothermal (<300m; <25 C ) Ground Source Heat Pumps/ Borehole Heat Exchangers Aquifer thermal energy storage Applications HEATING-COOLING SINGLE BUILDINGS Low enthalpy medium to deep geothermal Hydrothermal aquifers ( m; <140 C) DIRECT USE/CHP DISTRICT HEATING High enthalpy deep geothermal energy (>5000m; >180 C ) POWER GENERATION
21 Distribution of geothermal resources in Northern Ireland Shallow geothermal Ground source heat pump technology Aquifer thermal energy storage Almost everywhere in Northern Ireland Restricted to good aquifers This technology is supported by Government funding e.g. Reconnect
22 Distribution of geothermal resources in Northern Ireland Low enthalpy geothermal energy resources 1000m 2500m Measured and modelled temperatures at 1000m and 2500m depth (Kelly et al. 2005) Potential resources in Rathlin, Larne and Lough Neagh sedimentary basins
23 Radiogenic heat Calculated from Tellus radiometric data A = 0.337(0.74eUppm+.199eThppm+.26K%) μw/m³
24 Mourne Mountains radiogenic granites with geothermal energy potential 1. Shallow low enthalpy heat 2. Deep Hot Dry Rocks
25 Conclusions Tellus geophysical (and geochemical) data can help us to: refine 2D geological maps increase our understanding of geological structure and basin history produce 3D models of subsurface geology These are important tools in exploration for hydrocarbons and geothermal resources So far Next qualitative and regional interpretation quantitative modelling and detailed interpretation
26 Acknowledgements Thanks to Chris van Dam, Alex Donald, Mark Patton, Adrian Walker and Baz Chacksfield (BGS) for producing the Tellus images.
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