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- W1539934178 abstract "Enthalpy-chloride relations suggest that a deep reservoir exists at Zunil with a temperature near 300/sup 0/C. Water from that reservoir moves to shallower and cooler local reservoirs, where it mixes with diluted water and then attains a new water-rock chemical equilibrium. This mixed water, in turn, generally is further diluted before being discharged from thermal springs. The stable-isotopic composition of the thermal water indicates that recharge for the deep water at Zunil comes mainly from local sources. The presence of measurable tritium, which suggests that the deep water has been underground about 20 to 30 years, also indicates a local source for the recharge." @default.
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- W1539934178 date "1982-10-01" @default.
- W1539934178 modified "2023-09-23" @default.
- W1539934178 title "Oxygen and hydrogen isotopes in thermal waters at Zunil, Guatemala" @default.
- W1539934178 hasPublicationYear "1982" @default.
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