CHALCOPHILE ELEMENTS (HG, CD, PB, AND AS) IN BOTTOM SEDIMENTS OF WATER BODIES OF THE WHITE SEA CATCHMENT AREA ON THE KOLA PENINSULA

dc.contributor.author	Dauvalter V.A.
dc.date.accessioned	2024-11-02T11:07:41Z
dc.date.available	2024-11-02T11:07:41Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13519505
dc.identifier.citation	Geochemistry International, 2006, 44, 2, 205-208
dc.identifier.issn	0016-7029
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46324
dc.description.abstract	The north of European Russia including the Murmansk Region contains unique mineral resources. Many mining, processing, and smelting enterprises, the largest in Russia, are situated in the Murmansk Region, recovering annually millions of tons of rocks and ores to the surface, ejecting and discharging thousands of tons of contaminants, including highly toxic metal and organic compounds, into the atmosphere and water areas and streams.
dc.title	CHALCOPHILE ELEMENTS (HG, CD, PB, AND AS) IN BOTTOM SEDIMENTS OF WATER BODIES OF THE WHITE SEA CATCHMENT AREA ON THE KOLA PENINSULA
dc.type	Статья
dc.identifier.doi	10.1134/S001670290602011X

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