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- W2065934493 abstract "Transient cooling of magmatic intrusion in a geothermal reservoir due to conduction and convection is studied. The effects of overlying cap rock and different horizontal and vertical permeability of the reservoir are considered. Results are compared to the data from Salton Sea Geothermal Field. It is also observed that multiple layers of convection cells exist when horizontal permeability is much larger than the vertical permeability. The sharp dropoff of surface heat flow observed at Salton Sea Geothermal Field is confirmed by numerical results. Based on these numerical results, it is possible to speculate that the age of the intrusive body is about 8000 to 12,000 years." @default.
- W2065934493 created "2016-06-24" @default.
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- W2065934493 date "1980-01-11" @default.
- W2065934493 modified "2023-09-27" @default.
- W2065934493 title "Effect of permeability on cooling of a magmatic intrusion in a geothermal reservoir" @default.
- W2065934493 doi "https://doi.org/10.2172/7080942" @default.
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