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Presentdayoredeposition in the geothermalsystems of kenya—i. the mwananyamalahotsprings, northeast of jombohill, coastprovince
(ELSELVIER, 1990)
The Mwananyamalageothermal field extends over an area of 4 km x 11 km in a region of faulted Permo—Triassic sandstones. The sandstones consist of deltaic arkoses, and fluvio-lacustrine shales, siltstones and sandstones. ...
Stableisotopestudies of some lowenthalpygeothermalsystems in Kenya
(ELSELVIER, 1990)
Oxygen and hydrogen isotope compositions of some lowenthalpygeothermalsystems in Kenya have been determined. Plots on View the MathML source versus δD diagrams show that the compositions do not deviate appreciably from ...
Fluid/mineralequilibriumcalculations for geothermalfluids and chemicalgeothermometry
(ELSELVIER, 1993)
Aquifer temperatures of 13 geothermal wells in Iceland whose measured reservoir temperatures range from 47 to 325°C have been estimated from the chemical composition of the discharged fluid by considering simultaneously ...
Geothermalenergy research in Kenya: a review
(ELSELVIER, 1996)
Geothermalenergy for electricity generation is likely to become increasingly important in Kenya in the future. There are numerous centres of thermal activity in Kenya, particularly within the Rift Valley, although aridity ...