Enviar artigo por via de e-mail Low-carbonaceous shales in the Riphean stratotype, plume events, and supercontinent breakup: Analysis of the relationship
- Autores: Maslov A.1,2, Kovalev S.2
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Afiliações:
- Zavaritskii Institute of Geology and Geochemistry, Ural Branch
- Institute of Geology, Ufa Science Center
- Edição: Volume 473, Nº 2 (2017)
- Páginas: 397-401
- Seção: Geology
- URL: https://journals.rcsi.science/1028-334X/article/view/189593
- DOI: https://doi.org/10.1134/S1028334X17040134
- ID: 189593
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Resumo
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.
Sobre autores
A. Maslov
Zavaritskii Institute of Geology and Geochemistry, Ural Branch; Institute of Geology, Ufa Science Center
Autor responsável pela correspondência
Email: amas2004@mail.ru
Rússia, ul. Vonsovskogo 15, Yekaterinburg, 620016; ul. K. Marksa 16/2, Ufa, 450076
S. Kovalev
Institute of Geology, Ufa Science Center
Email: amas2004@mail.ru
Rússia, ul. K. Marksa 16/2, Ufa, 450076
