Email this article Low-carbonaceous shales in the Riphean stratotype, plume events, and supercontinent breakup: Analysis of the relationship
- Authors: Maslov A.V.1,2, Kovalev S.G.2
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Affiliations:
- Zavaritskii Institute of Geology and Geochemistry, Ural Branch
- Institute of Geology, Ufa Science Center
- Issue: Vol 473, No 2 (2017)
- Pages: 397-401
- Section: Geology
- URL: https://journals.rcsi.science/1028-334X/article/view/189593
- DOI: https://doi.org/10.1134/S1028334X17040134
- ID: 189593
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Abstract
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.
About the authors
A. V. Maslov
Zavaritskii Institute of Geology and Geochemistry, Ural Branch; Institute of Geology, Ufa Science Center
Author for correspondence.
Email: amas2004@mail.ru
Russian Federation, ul. Vonsovskogo 15, Yekaterinburg, 620016; ul. K. Marksa 16/2, Ufa, 450076
S. G. Kovalev
Institute of Geology, Ufa Science Center
Email: amas2004@mail.ru
Russian Federation, ul. K. Marksa 16/2, Ufa, 450076
