Hydrogeological zonality as a spatial and temporal form of groundwater existence
Authors:
Abstract
Zonality is a planetary property of groundwater that determines the shape of its spatial and temporal arrangement in the Earth's interior. This definition requires clarification of the physics of our ideas about zonality.
Область исследования:
(Archived) Without section
References
- Belousov V.V. Fundamentals of geotectonics. M., Nedra, 1975.
- Garrels R., Mackesy F. Evolution of sedimentary rocks. M., Mir, 1974.
- Zverev V.P. Energetics of hydrogeochemical processes of modern sedimentogenesis. M., Nauka, 1983.
- Lvovich M.I. World Water Resources and Their Future. M., Mysl, 1974.
- Pavlov A.N. Structural Features of the Hydrosphere as a Basis for Understanding Hydro-geochemical Processes in the Earth Crust. - In: Problems of Theoretical and Regional Hydrogeochemistry, Moscow, Moscow State University Press, 1979, pp. 77-81.
- Pavlov A.N. Fundamentals of System Approach in Geology. L., LPI Publishing House, 1981.
- Pavlov A.N. Geological water cycle on the Earth. L., Nedra, 1977.
- Priklonsky V.A. Soil Science. Moscow, Gosgeolizdat, 1952. V. 2.
- Saukov A.A. Geochemistry. M., Nauka, 1966.
- Ushakov S.A., Krass M.S. Gravity Force and Questions of Mechanics of the Earth's Interior. M., Nedra, 1972.
- Sherbina V.V. Fundamentals of Geochemistry. M., Nedra, 1972.