Explosive mechanism of formation of ore-bearing cataclasites on albitite-uranium deposits of the central part of Ukranian shield

On the basis of long-term investigations and literature analysis it is concluded that voluminous cataclasites are spatially and genetically associated with the alkaline sodium metasomatism process. The cataclasites were formed in the zones of long-living Meso-proterozoic breaks as a result of fluid-explosive phenomena occurring in the upward fluxes of plutonic alkaline uranium-bearing solutions. Peculiarities of deformations and spatial disposition of ore-bearing cataclasites is determined by multiple character of fluid-explosive phenomena exposed in tectonic zones upon alkaline metasomatism and ore deposition processes.

Авторы
Журнал
Номер выпуска
1
Язык
Русский
Страницы
85-88
Статус
Опубликовано
Том
396
Год
2004
Организации
  • 1 Inst. Geol. Rudn. Mestor. Petr., RAN, Moscow, Russian Federation
Ключевые слова
Deformation; Explosions; Geochronology; Ore deposit geology; Solutions; Structural geology; Tectonics; Fluid explosive phenomena; Uranium deposits
Дата создания
19.10.2018
Дата изменения
19.10.2018
Постоянная ссылка
https://repository.rudn.ru/ru/records/article/record/3584/
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