Peculiarities of gold water migration in the areas of peat-bog deposits development in the taiga landscape conditions
Abstract
The taiga region, in which the features of water migration of gold and other ore elements were studied, is characterized by flat, weakly articulated relief, deep seasonal freezing of soil-cover deposits and wide development of upper bogs.
Область исследования:
(Archived) Without section
References
- Aleksandrova L.N. Organic matter of soils and processes of its transformation. L., Nauka, 1980.
- Borovitsky V.P. Study of trace elements of peat-moss cover of bogs in areas of permafrost development in the search for ore deposits. - In Vn.: Microelements in biosphere and their application in agriculture and medicine of Siberia and Far East. Tomsk, ed. Tomsk Polytechnic Institute, 1969.
- Determan Goel-chromatography. M., Mir, 1970.
- Kiryukhin V.K., Shchvets V.M. Processes of iodine water formation, M., Nedra, 1980.
- Plusnin A.M., Pogrebnyak Y.F. Peculiarities of formation of water streams of gold dispersion in cryogenic landscapes. In the book: Features of geochemical halos in the cryogenesis zone. Gas-salt halos. Yakutsk, Izd. of the Institute of Permafrost Science, 1979.
- Reznikov A.A., Mulikovskaya E.P., Sokolov N.Yu. Methods of Analysis of Natural Waters, M., Nedra, 1970.
- Fischer E.N., Fischer V.L., Miller A.D. Experimental studies of the character of interaction of natural organic acids with gold. - Soviet Geology, 1974, No. 7.
- Shchvets V.M. Organic substances of underground waters; M., Nedra, 1973.
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