EXPLOSIVE ORIGIN OF ORE-BEARING CATACLASITES IN THE ALBITITE-URANIUM DEPOSITS OF THE CENTRAL UKRAINIAN SHIELD

dc.contributor.author	Tarasov N.N.
dc.date.accessioned	2022-08-03T05:20:56Z
dc.date.available	2022-08-03T05:20:56Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13464583
dc.identifier.citation	Doklady Earth Sciences, 2004, 396, 4, 481-483
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38443
dc.description.abstract	Extensional cataclasites in the albitite-uranium deposits of the Ukrainian Shield are spatially and genetically related to sodium metasomatism. They formed within the long-lived Middle Proterozoic fault zones owing to fluid explosions in the ascending flows of deep-seated, alkaline U-bearing solutions. The deformations and spatial distribution of the orebearing cataclasites are defined by multiple fluid explosions in the tectonic zones during alkaline metasomatism and ore deposition.
dc.title	EXPLOSIVE ORIGIN OF ORE-BEARING CATACLASITES IN THE ALBITITE-URANIUM DEPOSITS OF THE CENTRAL UKRAINIAN SHIELD
dc.type	Статья

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