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
Peculiarities of fresh water formation in artesian basins of mountainous folded regions
1985 V. A. Kiryukhin
Peculiarities of gold water migration in the areas of peat-bog deposits development in the taiga landscape conditions
1985 M. N. Kochneva, V. N. Shemyakin
Formation of the chemical composition of groundwater in the foothill troughs of Algeria
1985 Lanur Aissa
Use of a package of subroutines for solving hydrogeochemical classification problems
1985 M. B. Shtokalenko