Low-carbonaceous shales in the Riphean stratotype, plume events, and supercontinent breakup: Analysis of the relationship
- Авторы: Maslov A.1,2, Kovalev S.2
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Учреждения:
- Zavaritskii Institute of Geology and Geochemistry, Ural Branch
- Institute of Geology, Ufa Science Center
- Выпуск: Том 473, № 2 (2017)
- Страницы: 397-401
- Раздел: Geology
- URL: https://journals.rcsi.science/1028-334X/article/view/189593
- DOI: https://doi.org/10.1134/S1028334X17040134
- ID: 189593
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Аннотация
The relationship of events of igneous plume activity to the periods of low-carbonaceous clay shale deposition has been considered in the Riphean stratotype (western slope of the Southern Urals). The relation between plume events, warm climate periods, and active black shale deposition assumed in the Early Precambrian is poorly defined in the Late Precambrian.
Об авторах
A. Maslov
Zavaritskii Institute of Geology and Geochemistry, Ural Branch; Institute of Geology, Ufa Science Center
Автор, ответственный за переписку.
Email: amas2004@mail.ru
Россия, ul. Vonsovskogo 15, Yekaterinburg, 620016; ul. K. Marksa 16/2, Ufa, 450076
S. Kovalev
Institute of Geology, Ufa Science Center
Email: amas2004@mail.ru
Россия, ul. K. Marksa 16/2, Ufa, 450076