Lithochemical features of shungite rocks horizons, Onega structure
The studies of maksovite of Onega structure dome-deposits were carried out. It is developed on different stratigraphic levels of Zaonega Formation of the Palaeoproterozoic (2.0-1.9 Ga). Maksovite were separated for five groups by content of mineral component, namely, supersilites, normosilites, mios...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
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Karelian Research Centre of the Russian Academy of Sciences
2018-11-01
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| Series: | Transactions of the Karelian Research Centre of the Russian Academy of Sciences |
| Subjects: | |
| Online Access: | http://journals.krc.karelia.ru/index.php/precambrian/article/view/846 |
| Summary: | The studies of maksovite of Onega structure dome-deposits were carried out. It is developed on different stratigraphic levels of Zaonega Formation of the Palaeoproterozoic (2.0-1.9 Ga). Maksovite were separated for five groups by content of mineral component, namely, supersilites, normosilites, miosilites, gypersilites and siallites. The geochemical features of maksovites are revealed depend on their stratigraphic position and within dome structures. |
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| ISSN: | 1997-3217 2312-4504 |