Conceptual Model At Raft River Geothermal Area (1981)
Exploration Activity: Conceptual Model At Raft River Geothermal Area (1981)
|Exploration Activity Details|
|Location||Raft River Geothermal Area|
|Exploration Technique||Conceptual Model|
Use geoscience data to develop a conceptual model of the reservoir.
The geoscience data gathered in the drilling and testing of seven geothermal wells suggest that the thermal reservoir is: (a) produced from fractures found at the contact metamorphic zone, apparently the base of detached normal faulting from the Bridge and Horse Well Fault zones of the Jim Sage Mountains; (b) anisotropic, with the major axis of hydraulic conductivity coincident to the Bridge Fault Zone; (c) hydraulically connected to the shallow thermal fluid of the Crook and BLM wells based upon both geochemistry and pressure response; (d) controlled by a mixture of diluted meteoric water recharging from the northwest and a saline sodium chloride water entering from the southwest.
- Dolenc, M. R.; Hull, L. C.; Mizell, S. A.; Russell, B. F.; Skiba, P. A.; Strawn, J. A.; Tullis, J. A. (1 November 1981) Raft River geoscience case study
- Dolenc, M. R.; Hull, L. C.; Mizell, S. A.; Russell, B. F.; Skiba, P. A.; Strawn, J. A.; Tullis, J. A. (1 November 1981) Raft River geoscience case study- appendixes