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- W1544402110 abstract "Isotopic and thermodynamic reservoir characteristics of the Copahue-Caviahue geothermal field, Neuquen province. Argentina. The geothermal field of Copahue-Caviahue, situated in the neighboring of an active volcano, has been defined as a vapor dominated field, with stratified layers, connected by fractures, with good vertical permeability within the reservoir. 2 H and 18 O analyses done on vapor, water, associated gas analysis and the study of the gas vapor ratio, allowed to prove the existence of at least two productive layers, the shallower at ca. 800-1000m and the deeper at more than1400m (both bellow the well top level). Isotopic and geothermometric temperatures round 200oC and 250oC respectively, 13 C, N 2 , Ar and He analyses have let us to characterize the origin of geothermal gases as mainly magma derived." @default.
- W1544402110 created "2016-06-24" @default.
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- W1544402110 date "2002-09-01" @default.
- W1544402110 modified "2023-10-07" @default.
- W1544402110 title "Características isotópicas y termodinámicas de reservorio del campo geotérmico Copahue-Caviahue, provincia del Neuquén" @default.
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