Landscape-hydrogeochemical zonality of groundwater of the hypergenesis zone (on the example of the Prionezhye region)
Authors:
Abstract
In the relief of the modern surface of Prionezhye three terraces with absolute marks of hypsometric levels 30-60, 60-100 and 100 m and more are traced. The maximum heights do not exceed 300 m.
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References
- Perelman A.I. Geochemistry of landscape. 2nd ed. Moscow, Higher School, 1975.
- Perelman A.I. Geochemistry of elements in the zone of hypereogenesis. M., Nedra, 1972.
- Samarina V.S. Formation of Chemical Composition of Groundwater (on the Example of the Caspian Lowland). L., LSU Publishing House, 1963.
- Samarina V.S. Hydrogeochemistry. L., PH LSU, 1977.
- Sudarikov S.M. Hydrogeochemical prerequisites of ore-bearing capacity of the Eastern Prionezhye. - Proc. of universities. Geology and Exploration, 1978, No. 4.
- Slymo P.S. - The Biologist, 1964, 67.
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