Evidence for dilution of deep, confined ground water by vertical recharge of isotopically heavy Pleistocene water (Q61660472)

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Evidence for dilution of deep, confined ground water by vertical recharge of isotopically heavy Pleistocene water
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    Evidence for dilution of deep, confined ground water by vertical recharge of isotopically heavy Pleistocene water (English)
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    D. I. Siegel
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    1991
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    19
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    5
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    433
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