Geochemical specialization of terrigenous deposits of the Bashkirian meganticlinorium
- Авторлар: Kovalev S.G.1, Snachev V.I.1, Romanovskaya M.A.2
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Мекемелер:
- Institute of Geology, Ufa Science Center
- Department of Geology
- Шығарылым: Том 72, № 4 (2017)
- Беттер: 269-278
- Бөлім: Article
- URL: https://bakhtiniada.ru/0145-8752/article/view/174472
- DOI: https://doi.org/10.3103/S0145875217040020
- ID: 174472
Дәйексөз келтіру
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.
Авторлар туралы
S. Kovalev
Institute of Geology, Ufa Science Center
Хат алмасуға жауапты Автор.
Email: kovalev@ufaras.ru
Ресей, Ufa, 450077
V. Snachev
Institute of Geology, Ufa Science Center
Email: kovalev@ufaras.ru
Ресей, Ufa, 450077
M. Romanovskaya
Department of Geology
Email: kovalev@ufaras.ru
Ресей, Moscow, 119991
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