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

dc.contributor.authorTarasov N.N.
dc.date.accessioned2022-08-03T05:20:56Z
dc.date.available2022-08-03T05:20:56Z
dc.date.issued2004
dc.description.abstractExtensional 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.identifierhttps://www.elibrary.ru/item.asp?id=13464583
dc.identifier.citationDoklady Earth Sciences, 2004, 396, 4, 481-483
dc.identifier.issn1028-334X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/38443
dc.titleEXPLOSIVE ORIGIN OF ORE-BEARING CATACLASITES IN THE ALBITITE-URANIUM DEPOSITS OF THE CENTRAL UKRAINIAN SHIELD
dc.typeСтатья

Файлы

Коллекции