HYDROGEOCHEMISTRY OF THE PERMAFROST ZONE IN THE CENTRAL PART OF THE YAKUTIAN DIAMOND-BEARING PROVINCE, RUSSIA

dc.contributor.author	Alexeev S.V.
dc.contributor.author	Alexeeva L.P.
dc.date.accessioned	2022-02-02T08:58:57Z
dc.date.available	2022-02-02T08:58:57Z
dc.date.issued	2003
dc.identifier	https://elibrary.ru/item.asp?id=13425972
dc.identifier.citation	Hydrogeology Journal, 2003, 11, 5, 574-581
dc.identifier.issn	1431-2174
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/34826
dc.description.abstract	The hydrogeochemical characteristics and zonation of the permafrost zone in the central part of the Yakutian diamond-bearing province formed mainly under the influence of cryogenic processes that occurred in the late Cenozoic. On the basis of field and experimental studies, conclusions were formulated that the perennial cryogenesis of the sedimentary cover in this region resulted in increasing the concentration of carbonate and sulfate compounds in groundwaters as well as increasing the concentration of easily soluble compounds (sodium, magnesium, and calcium chlorides).
dc.title	HYDROGEOCHEMISTRY OF THE PERMAFROST ZONE IN THE CENTRAL PART OF THE YAKUTIAN DIAMOND-BEARING PROVINCE, RUSSIA
dc.type	Статья

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