GENESIS OF DAWSONITE MINERALIZATION: THERMODYNAMIC ANALYSIS AND ALTERNATIVES

dc.contributor.author	Ryzhenko B.N.
dc.date.accessioned	2024-10-23T07:16:00Z
dc.date.available	2024-10-23T07:16:00Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13512139
dc.identifier.citation	Geochemistry International, 2006, 44, 8, 835-840
dc.identifier.issn	0016-7029
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46158
dc.description.abstract	Although the mineral dawsonite NaAlCO3(OH)2 is not well known to geologists, dawsonite mineralization is quite widely known and was documented, for example, in the Carpathians, Kuznetsk Basin, Donets Basin, Northern Caucasus, Caspian Sea area, Khibina, and Colorado. The Lower Carboniferous deposits of the Pripyat’ foredeep in Belarus (sandy–clayey rocks with carbonate beds of the Visean stage filling the El’sk depression) host the Zaozerskoe dawsonite deposit [1]. The sandstones, siltstones, and mudstones of the coal-bearing Balakhonskaya Group (Lower Permian–Upper Carboniferous) contain 2- to 35-m-thick tabular and lens-shaped bodies with average dawsonite contents of 10–15%.
dc.title	GENESIS OF DAWSONITE MINERALIZATION: THERMODYNAMIC ANALYSIS AND ALTERNATIVES
dc.type	Статья
dc.identifier.doi	10.1134/S0016702906080088

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