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The influence of oxygen isotope exchange between CO2 and H2O in natural CO2-rich spring waters : implications for geothermometry

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Figure

Fig. 1. Natural processes affecting water d18O and d2H values (adapted from D'Amore and Panichi, 1987).
Fig. 2. a) Global compilation of COPah Tempe:available asisotopic composition in mineral spring waters, previously published by2-rich waters showing 18O depletion or enrichment without a change in d2H values relative to the GMWL
Fig. 3. a) Location map of Daylesford springs in Victoria, SE Australia. Springs emanate near major fault lines and Newer Volcanic eruption centres (adapted from2002 Cartwright et al.,)
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