Geochemical specialization of terrigenous deposits of the Bashkirian meganticlinorium
- Авторы: Kovalev S.G.1, Snachev V.I.1, Romanovskaya M.A.2
-
Учреждения:
- Institute of Geology, Ufa Science Center
- Department of Geology
- Выпуск: Том 72, № 4 (2017)
- Страницы: 269-278
- Раздел: Article
- URL: https://bakhtiniada.ru/0145-8752/article/view/174472
- DOI: https://doi.org/10.3103/S0145875217040020
- ID: 174472
Цитировать
Аннотация
The materials on the geology and geochemical specialization of Riphean terrigenous rocks of the Bashkirian meganticlinorium, including carbonaceous shale and conglomerate, are reported. Conglomerate is characterized by a high concentration of Au and PGEs mostly related to intensely dislocated zones. It is concluded that potentially ore-bearing zones in terrigenous deposits of the Bashkirian meganticlinorium were formed as a result of multistage polygene processes controlled by the Riphean–Vendian geodynamic evolution of the region.
Об авторах
S. Kovalev
Institute of Geology, Ufa Science Center
Автор, ответственный за переписку.
Email: kovalev@ufaras.ru
Россия, Ufa, 450077
V. Snachev
Institute of Geology, Ufa Science Center
Email: kovalev@ufaras.ru
Россия, Ufa, 450077
M. Romanovskaya
Department of Geology
Email: kovalev@ufaras.ru
Россия, Moscow, 119991
Дополнительные файлы
