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- W255684025 abstract "Approximately twenty-one percent of the geothermal waters in the United States are in the Basin and Range Province. Many of these waters have low to moderate temperatures (30 to 50/sup 0/). These waters may be a masked vestige of hot reservoirs at depth or may be direct discharge for deep circulating waters in systems with normal thermal characteristics. Moderate temperature waters flow from springs and wells in the basin sediments of the Safford Basin in southeastern Arizona. Integration of geologic, hydrologic, major-ion chemical, stable and radioisotope data from Safford indicates that the Safford thermal waters are produced by deep circulation into the basin, which has relatively normal thermal characteristics. These waters are forced to the surface by pressure derived from the high-standing mountain ranges at the basin margins. The absence of shifts in isotopic composition off the meteoric line indicates that temperatures in the reservoirs are too low to permit boiling (shift to the left) or water-mineral isotope exchange reactions (shift to the right). In the absence of shifts, the isotopic compositions of the thermal waters indicate the isotopic compositions in their source area and imply that the surrounding mountain ranges were the source area. Radiocarbon ages indicate that groundmore » water and the minerals in the aquifers are in equilibrium. The water-mineral equilibria relationships of waters sampled along the flow path also indicate a mountain source for the thermal waters and define the flow paths of waters from the mountain ranges deep into the basin sediments. Similar studies can be applied to geothermal systems throughout the Basin and Range, providing that variations in the stable isotope and major-ion chemistry of waters are discernable in the basin of interest.« less" @default.
- W255684025 created "2016-06-24" @default.
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- W255684025 date "1983-03-01" @default.
- W255684025 modified "2023-09-26" @default.
- W255684025 title "Isotopic and geochemical investigation of the thermal waters in the Safford Basin, Arizona. [Abstract only]" @default.
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