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...
Gorde:
| Egile Nagusiak: | , |
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| Formatua: | Artigo |
| Hizkuntza: | Inglês |
| Argitaratua: |
Russian Academy of Sciences. Karelian Research Centre
2018-11-01
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| Saila: | Transactions of the Karelian Research Centre of the Russian Academy of Sciences |
| Gaiak: | |
| Sarrera elektronikoa: | http://journals.krc.karelia.ru/index.php/precambrian/article/view/846 |
| Etiketak: |
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