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The groundwater chemistry of the aquifers around and within the Devonian rift basin of the Shira area is very different from that of the Permian Oslo Rift. The anionic chemical composition in the Russian Devonian Aquifers is often dominated by apparently evaporite-derived sulphate and chloride salinity. The composition of the more saline ground- and lake-waters is typically of sodium sulphate (-chloride) type.

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