CV-3: Extensional Domain
Moeck-Beardsmore Play Types
Crustal extension and thinning cause the mantle to become elevated. This elevated mantle results in a higher geothermal gradient within the crust. Meteoric water circulates through deep faults or permeable formations in the crust and becomes heated.
According to Moeck and Beardsmore, extensional domain geothermal plays typically have the following properties:[2]
- Geologic Setting – Metamorphic Core Complexes, Back-arc Extension, Pull-apart Basins, Intracontinental Rifts
- Heat Source/Storage Properties of Reservoir – Thinned Crust+Elevated Heatflow, Recent Extensional Domains
- Dominant Heat Transport Mechanism – Fault Controlled, Hydrothermal Circulation
Examples
Want to add an example to this list? Select a Geothermal Resource Area to edit its "Moeck-Beardsmore Play Type" property using the "Edit with Form" option.
CSVGeothermal Resource Area | Geothermal Region | Control Structure | Host Rock Age | Host Rock Lithology | Mean Capacity | Mean Reservoir Temp |
---|---|---|---|---|---|---|
Alasehir Geothermal Area | Aegean-West Anatolian Extensional Region | 48 MW 48,000 kW 48,000,000 W 48,000,000,000 mW 0.048 GW 4.8e-5 TW | 434.15 K 161 °C 321.8 °F 781.47 °R | |||
Altheim Geothermal Area | Upper Austrian Molasse Basin | Jurassic | Limestone; Dolomites | 1 MW 1,000 kW 1,000,000 W 1,000,000,000 mW 0.001 GW 1.0e-6 TW | 373.15 K 100 °C 212 °F 671.67 °R | |
Bad Blumau Geothermal Area | Styrian Basin | Dolomite | 0.25 MW 250 kW 250,000 W 250,000,000 mW 2.5e-4 GW 2.5e-7 TW | 383.15 K 110 °C 230 °F 689.67 °R | ||
Beowawe Hot Springs Geothermal Area | Central Nevada Seismic Zone Geothermal Region | Pull-Apart in Strike-Slip Fault Zone | Ordovician | shale; quartzite | 17 MW 17,000 kW 17,000,000 W 17,000,000,000 mW 0.017 GW 1.7e-5 TW | 483.15 K 210 °C 410 °F 869.67 °R |
Blue Mountain Geothermal Area | Northwest Basin and Range Geothermal Region | Fault Intersection Intrusion Margins and Associated Fractures | Triassic | Metasedimentary | 49.5 MW 49,500 kW 49,500,000 W 49,500,000,000 mW 0.0495 GW 4.95e-5 TW | 470.15 K 197 °C 386.6 °F 846.27 °R |
Brady Hot Springs Geothermal Area | Northwest Basin and Range Geothermal Region | Accommodation Zone | Mesozoic | metamorphic rocks | 26.1 MW 26,100 kW 26,100,000 W 26,100,000,000 mW 0.0261 GW 2.61e-5 TW | 455.15 K 182 °C 359.6 °F 819.27 °R |
Bruchsal Geothermal Area | Upper Rhine Valley | Major Normal Fault | Triassic | Sandstone | 0.6 MW 600 kW 600,000 W 600,000,000 mW 6.0e-4 GW 6.0e-7 TW | 413.15 K 140 °C 284 °F 743.67 °R |
Coso Geothermal Area | Walker-Lane Transition Zone | Pull-Apart in Strike-Slip Fault Zone | Mesozoic | granitic | 300 MW 300,000 kW 300,000,000 W 300,000,000,000 mW 0.3 GW 3.0e-4 TW | 571.15 K 298 °C 568.4 °F 1,028.07 °R |
Desert Peak Geothermal Area | Northwest Basin and Range Geothermal Region | Stepover or Relay Ramp in Normal Fault Zones | Mesozoic | greenstone | 23 MW 23,000 kW 23,000,000 W 23,000,000,000 mW 0.023 GW 2.3e-5 TW | 481.15 K 208 °C 406.4 °F 866.07 °R |
Dixie Valley Geothermal Area | Central Nevada Seismic Zone Geothermal Region | Major Normal Fault Stepover or Relay Ramp in Normal Fault Zones | Jurassic | Basalt | 62 MW 62,000 kW 62,000,000 W 62,000,000,000 mW 0.062 GW 6.2e-5 TW | 504.15 K 231 °C 447.8 °F 907.47 °R |
Fernley Geothermal Area | Northwest Basin and Range Geothermal Region | 30 MW 30,000 kW 30,000,000 W 30,000,000,000 mW 0.03 GW 3.0e-5 TW | 422.15 K 149 °C 300.2 °F 759.87 °R | |||
Germencik Geothermal Area | Aegean-West Anatolian Extensional Region | Fault Intersection | Marble | 73.4 MW 73,400 kW 73,400,000 W 73,400,000,000 mW 0.0734 GW 7.34e-5 TW | 491.15 K 218 °C 424.4 °F 884.07 °R | |
Gumuskoy Geothermal Area | Aegean-West Anatolian Extensional Region | Fault Intersection | Paleozic | Marble | 13.2 MW 13,200 kW 13,200,000 W 13,200,000,000 mW 0.0132 GW 1.32e-5 TW | 413.15 K 140 °C 284 °F 743.67 °R |
Hot Sulphur Springs Geothermal Area | Central Nevada Seismic Zone Geothermal Region | 18 MW 18,000 kW 18,000,000 W 18,000,000,000 mW 0.018 GW 1.8e-5 TW | 445.15 K 172 °C 341.6 °F 801.27 °R | |||
Humboldt House Geothermal Area | Northwest Basin and Range Geothermal Region | Fault Controlled | 0.3 MW 300 kW 300,000 W 300,000,000 mW 3.0e-4 GW 3.0e-7 TW | 466.15 K 193 °C 379.4 °F 839.07 °R | ||
Iwate Geothermal Area | Northeast Honshu Arc | Miocene; Pre-Tertiary | Dacitic welded tuff; Marine Sediments Tuffs; Shales; Chert; Slate; Granodiorite | 103.5 MW 103,500 kW 103,500,000 W 103,500,000,000 mW 0.104 GW 1.035e-4 TW | 578.15 K 305 °C 581 °F 1,040.67 °R | |
Kizildere Geothermal Area | Aegean-West Anatolian Extensional Region | Fault Intersection | Miocene | Limestone | 102 MW 102,000 kW 102,000,000 W 102,000,000,000 mW 0.102 GW 1.02e-4 TW | 459.15 K 186 °C 366.8 °F 826.47 °R |
Klamath Falls Geothermal Area | Cascades Geothermal Region | 1.8 MW 1,800 kW 1,800,000 W 1,800,000,000 mW 0.0018 GW 1.8e-6 TW | 386.15 K 113 °C 235.4 °F 695.07 °R | |||
Landau Geothermal Area | Upper Rhine Valley | Major Normal Fault | 3.6 MW 3,600 kW 3,600,000 W 3,600,000,000 mW 0.0036 GW 3.6e-6 TW | 413.15 K 140 °C 284 °F 743.67 °R | ||
Langjiu Geothermal Area | Tibet Geothermal Region | Fault Controlled | 1 MW 1,000 kW 1,000,000 W 1,000,000,000 mW 0.001 GW 1.0e-6 TW | 377.15 K 104 °C 219.2 °F 678.87 °R | ||
Lightning Dock Geothermal Area | Southern Basin and Range Geothermal Region | Fault Intersection | Paleozoic carbonate rocks and late Tertiary volcanic rocks | 4.4 MW 4,400 kW 4,400,000 W 4,400,000,000 mW 0.0044 GW 4.4e-6 TW | 443.15 K 170 °C 338 °F 797.67 °R | |
Mori Geothermal Area | Kuril-Kamchatka Arc | Caldera Rim Margins | Pre-Tertiary | Limestone | 50 MW 50,000 kW 50,000,000 W 50,000,000,000 mW 0.05 GW 5.0e-5 TW | 513.15 K 240 °C 464 °F 923.67 °R |
Nagqu Geothermal Area | Tibet geothermal region | 5.8 MW 5,800 kW 5,800,000 W 5,800,000,000 mW 0.0058 GW 5.8e-6 TW | 388.15 K 115 °C 239 °F 698.67 °R | |||
Neal Hot Springs Geothermal Area | Snake River Plain | Pull-Apart in Strike-Slip Fault Zone | Miocene | Basalt | 33 MW 33,000 kW 33,000,000 W 33,000,000,000 mW 0.033 GW 3.3e-5 TW | 429.15 K 156 °C 312.8 °F 772.47 °R |
Pamukoren Geothermal Area | Aegean-West Anatolian Extensional Region | 45 MW 45,000 kW 45,000,000 W 45,000,000,000 mW 0.045 GW 4.5e-5 TW | 448.15 K 175 °C 347 °F 806.67 °R | |||
Raft River Geothermal Area | Northern Basin and Range Geothermal Region | Fault Intersection | 1- Archean; 2-Proterozoic | 1- quartz monzonite; 2-schist; quartzite | 13 MW 13,000 kW 13,000,000 W 13,000,000,000 mW 0.013 GW 1.3e-5 TW | 468.15 K 195 °C 383 °F 842.67 °R |
Romania Geothermal Area | Europe | 0.5 MW 500 kW 500,000 W 500,000,000 mW 5.0e-4 GW 5.0e-7 TW | 358.15 K 85 °C 185 °F 644.67 °R | |||
Rye Patch Geothermal Area | Northwest Basin and Range Geothermal Region | 12.5 MW 12,500 kW 12,500,000 W 12,500,000,000 mW 0.0125 GW 1.25e-5 TW | 486.15 K 213 °C 415.4 °F 875.07 °R | |||
Salavatli Geothermal Area | Aegean-West Anatolian Extensional Region | Major Normal Fault | 58 MW 58,000 kW 58,000,000 W 58,000,000,000 mW 0.058 GW 5.8e-5 TW | 444.15 K 171 °C 339.8 °F 799.47 °R | ||
Salt Wells Geothermal Area | Northwest Basin and Range Geothermal Region | 23.6 MW 23,600 kW 23,600,000 W 23,600,000,000 mW 0.0236 GW 2.36e-5 TW | 466.15 K 193 °C 379.4 °F 839.07 °R | |||
San Emidio Desert Geothermal Area | Northwest Basin and Range Geothermal Region | 14.22 MW 14,220 kW 14,220,000 W 14,220,000,000 mW 0.0142 GW 1.422e-5 TW | 426.15 K 153 °C 307.4 °F 767.07 °R | |||
Soda Lake Geothermal Area | Northwest Basin and Range Geothermal Region | Miocene | pumice tuff | 26.1 MW 26,100 kW 26,100,000 W 26,100,000,000 mW 0.0261 GW 2.61e-5 TW | 452.15 K 179 °C 354.2 °F 813.87 °R | |
Steamboat Springs Geothermal Area | Walker-Lane Transition Zone | Fault Intersection | 1- Cretaceous; 2- Pliocene-Pleistocene | 1- granodiorite; 2- basaltic andesite | 147 MW 147,000 kW 147,000,000 W 147,000,000,000 mW 0.147 GW 1.47e-4 TW | 483.15 K 210 °C 410 °F 869.67 °R |
Stillwater Geothermal Area | Northwest Basin and Range Geothermal Region | Accommodation Zone | Quaternary | sandstone | 47.2 MW 47,200 kW 47,200,000 W 47,200,000,000 mW 0.0472 GW 4.72e-5 TW | 447.15 K 174 °C 345.2 °F 804.87 °R |
Thermo Hot Springs Geothermal Area | Northern Basin and Range Geothermal Region | 10.3 MW 10,300 kW 10,300,000 W 10,300,000,000 mW 0.0103 GW 1.03e-5 TW | 462.15 K 189 °C 372.2 °F 831.87 °R | |||
Tuzla Geothermal Area | Aegean-West Anatolian Extensional Region | Fault Intersection | 8 MW 8,000 kW 8,000,000 W 8,000,000,000 mW 0.008 GW 8.0e-6 TW | 405.15 K 132 °C 269.6 °F 729.27 °R | ||
Wabuska Hot Springs Geothermal Area | Walker-Lane Transition Zone Geothermal Region | Quaternary | gravels; sands | 2.4 MW 2,400 kW 2,400,000 W 2,400,000,000 mW 0.0024 GW 2.4e-6 TW | 403.15 K 130 °C 266 °F 725.67 °R | |
Wairakei-Poihipi Geothermal Area | Taupo Volcanic Zone | Fault Intersection | Quaternary | Volcaniclastic | 352 MW 352,000 kW 352,000,000 W 352,000,000,000 mW 0.352 GW 3.52e-4 TW | 483.15 K 210 °C 410 °F 869.67 °R |
Wendel Geothermal Area | Walker-Lane Transition Zone Geothermal Region | Displacement Transfer Zone | Mesozoic | Granite, Granodiorite | 3.8 MW 3,800 kW 3,800,000 W 3,800,000,000 mW 0.0038 GW 3.8e-6 TW | 413.15 K 140 °C 284 °F 743.67 °R |
Wild Rose Geothermal Area | Walker-Lane Transition Zone Geothermal Region | Fault Controlled | 16 MW 16,000 kW 16,000,000 W 16,000,000,000 mW 0.016 GW 1.6e-5 TW | 412.15 K 139 °C 282.2 °F 741.87 °R | ||
Yangbajain Geothermal Area | Himalayan Mountain Range | Fault Intersection | 24 MW 24,000 kW 24,000,000 W 24,000,000,000 mW 0.024 GW 2.4e-5 TW | 478.15 K 205 °C 401 °F 860.67 °R |
References
- ↑ Inga S. Moeck,Graeme Beardsmore. 2014. A New 'Geothermal Play Type' Catalog: Streamlining Exploration Decision Making. In: Proceedings. Thirty-Ninth Workshop on Geothermal Reservoir Engineering; 2014/02/24; Stanford, California. Stanford, California: Stanford University; p. 8
- ↑ 2.0 2.1 Inga Moeck. 2013. Geothermal Plays in Geologic Settings. In: IGA Workshop on Developing Best Practice for Geothermal Exploration and Resource/Reserve Classification; 2013/11/14; Essen, Germany. IGA website: International Geothermal Association; p. 19