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.
Область исследования:
(Archived) Without section
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.
Similar articles
Regularities of changes in the chemical composition of groundwater in the areas of influence of potash production enterprises (on the example of Solikamsk mining-industrial district)
1985 V. G. Rumynin, N. G. Golovina, L. V. Proskurnina, E. A. Lomakin
Use of a package of subroutines for solving hydrogeochemical classification problems
1985 M. B. Shtokalenko
Changes in hydrogeological conditions during the exploitation of the Leningrad oil shale deposit
1985 N. S. Petrov