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— The formation conditions of the Bishuli thermomineral waters from the Crimean Plain were determined by a complex of isotopic methods. The absence of tritium (3H < 0.1 TU) and considerable radiocarbon age (τ = 28 ± 3 ka) are in line with the light isotopic composition of the mineral water (δ18O = –13.4‰ and δ2H = –96‰), which is strongly different from that of the recent precipitation, river water,...
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