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- W2066044497 abstract "Oxygen is a major component of rocks and of hydrous solutions, and interacting rock and water of initially arbitrary compositions always set up a potential for isotope exchange that in time leads to mutual isotope shifts. Regardless of kinetic factors exchanged rocks may be viewed as exhausted isotope shifting capacities that correspond to equivalent quantities of exchanged fluid. Since most of the actual isotope exchange in geothermal systems takes place in reaction zones with a relatively narrow temperature range, a zeroeth-order “mixed model” is considered, which consists of batches of water passing through a fixed rock reservoir. The model provides an estimate of the cumulative water throughput, or hydrological maturity, of geothermal systems in terms of the measurable isotope shifts of present-day throughput and the overall isotope shifting potential. The assumption of discrete batches of throughput partially simulates the inefficiency of natural water-rock interaction, while the continuous process (with vanishing batch size) sets a lower limit for the required fluid throughput. Hydrogen and strontium isotopes, respectively, could provide better sensitivity at very early and very late stages of evolution. Several examples of geothermal systems are discussed and placed into a tentative order of maturity." @default.
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- W2066044497 date "1985-06-01" @default.
- W2066044497 modified "2023-09-24" @default.
- W2066044497 title "Isotope shift data and the natural evolution of geothermal systems" @default.
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- W2066044497 doi "https://doi.org/10.1016/0009-2541(85)90155-x" @default.
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