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- W2003809804 abstract "The hot springs of Zambia are associated with zones of major deep seated fault and fracture systems along which water of mainly meteoric origin circulates to great depths and is heated by normal geothermal gradients. The chemistry of the hot spring waters at the surface represents the effect of a predominantly hot water rock interaction process and a mixing with little juvenile water. Geochemistry also provides evidence in some waters of a mixing between deep, hot waters and shallow, cooler waters. Interpretations of geochemical data and estimates of underground temperatures for some springs indicate the existence of exploitable low enthalpy geothermal resources in most parts of the country." @default.
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- W2003809804 date "1988-01-01" @default.
- W2003809804 modified "2023-09-23" @default.
- W2003809804 title "Geothermal resources of Zambia" @default.
- W2003809804 doi "https://doi.org/10.1016/0375-6505(88)90079-x" @default.
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