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- W2007603648 abstract "Abstract Variations in the values from 14C, 3H, and δ 13C analyses can be used to differentiate young groundwater which was recharged in limestone from that recharged in sandstone areas. This is due to the fact that the process of isotopic maturation of groundwater occurs at different rates in different geologic environments." @default.
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- W2007603648 date "1982-10-01" @default.
- W2007603648 modified "2023-10-18" @default.
- W2007603648 title "Isotopical differentiation of groundwater of different hydrogeologic origin" @default.
- W2007603648 cites W652480899 @default.
- W2007603648 doi "https://doi.org/10.1016/0022-1694(82)90009-9" @default.
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