Low-carbonaceous shales in the Riphean stratotype, plume events, and supercontinent breakup: Analysis of the relationship
- 作者: Maslov A.V.1,2, Kovalev S.G.2
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隶属关系:
- Zavaritskii Institute of Geology and Geochemistry, Ural Branch
- Institute of Geology, Ufa Science Center
- 期: 卷 473, 编号 2 (2017)
- 页面: 397-401
- 栏目: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/189593
- DOI: https://doi.org/10.1134/S1028334X17040134
- ID: 189593
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详细
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.
作者简介
A. Maslov
Zavaritskii Institute of Geology and Geochemistry, Ural Branch; Institute of Geology, Ufa Science Center
编辑信件的主要联系方式.
Email: amas2004@mail.ru
俄罗斯联邦, ul. Vonsovskogo 15, Yekaterinburg, 620016; ul. K. Marksa 16/2, Ufa, 450076
S. Kovalev
Institute of Geology, Ufa Science Center
Email: amas2004@mail.ru
俄罗斯联邦, ul. K. Marksa 16/2, Ufa, 450076
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