Abstract
Abstract A profile of 11 samples from Lake Taupo have been analysed for 3He/4He ratios; helium, neon, and 3H concentrations. The results indicate no, significant input of Wairakei-type geothermal fluids to the lake over the past 20 years. This suggests that the thick sedimentary cover of Taupo pumice and ash has hydrologically isolated the waters of Lake Taupo from the source region of the A.D.
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