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Isotopic composition of waters from the Danakil depression (Ethiopia)
Authors:R Gonfiantini  S Borsi  G Ferrara  C Panichi
Institution:Laboratorio di Geologia Nucleare dell ''Università, Pisa ,Italy;Laboratorio per le Ricerche Radiometriche applicate alla Geocronologia e alla Paleoecologia, CNR, Pisa ,Italy;Istituto Internazionale per le Ricerche Geotermiche, CNR, Pisa ,Italy
Abstract:During two expeditions in the Danakil depression (Ethiopia), water samples were collected from: (a) hot springs in Dallol, Salt Plain, in the north of the depression; (b) cold and hot springs around Lake Giulietti; and c) Lake Giulietti.The isotopic results indicate: the water from Dallol hot springs is enriched in18O by isotopic exchange with the rocks as has been observed in many other geothermal areas of the world; b) the isotopic composition of the Lake Giulietti water changes with depth, probably as a consequence of a seasonal stratification; c) the springs in the Lake Giulietti region contain waters which result from the mixing of local meteoric water with a brine, or with lake waters.
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