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...
Guardat en:
| Autors principals: | , |
|---|---|
| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Russian Academy of Sciences. Karelian Research Centre
2018-11-01
|
| Col·lecció: | Transactions of the Karelian Research Centre of the Russian Academy of Sciences |
| Matèries: | |
| Accés en línia: | http://journals.krc.karelia.ru/index.php/precambrian/article/view/846 |
| Etiquetes: |
Sense etiquetes, Sigues el primer a etiquetar aquest registre!
|