1982
DOI: 10.2172/5057050
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Hydro-geochemical studies of uranium mill tailing piles at Riverton, Wyoming and Maybell, Colorado. Annual report for FY 1981

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“…Present-day shallow groundwater ␦ 18 O values are Ϫ15 to Ϫ17‰ at Riverton, Wyoming, and Ϫ16.3‰ at Douglas, Wyoming (Narasimhan et al 1982;Lander 1991). However, the probable direction of any change in ␦ 18 O of formation water with depth can be constrained by examination of modern soil carbonates.…”
Section: Time Of Formationmentioning
confidence: 98%
“…Present-day shallow groundwater ␦ 18 O values are Ϫ15 to Ϫ17‰ at Riverton, Wyoming, and Ϫ16.3‰ at Douglas, Wyoming (Narasimhan et al 1982;Lander 1991). However, the probable direction of any change in ␦ 18 O of formation water with depth can be constrained by examination of modern soil carbonates.…”
Section: Time Of Formationmentioning
confidence: 98%