Abstract: The geothermal reservoirs at Roosevelt Hot Springs and Utah FORGE EGS share common host rocks comprising Oligocene-Miocene granitoids and Precambrian gneiss representing end-member conditions of convective and conductive heat flow that formed within a large-scale magmatic geothermal system. Native state convective heat transfer at Roosevelt Hot Springs of […]
Publication Title: The Interplay of Impermeable Crystalline Basement Rocks, Tectonic Fracturing and Magmatic Intrusion in the Development of Geothermal Resources at Utah FORGE and Roosevelt Hot Springs
Authors: Stuart SIMMONS, Clay JONES, Stefan KIRBY, Phil WANNAMAKER, Kris PANKOW, Joe MOORE
Key Words: Utah FORGE, Roosevelt Hot Springs, heat transfer, helium isotopes, magnetotelluric resistivity, geology
