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pro vyhledávání: '"Татьяна Юрьевна Товпенец"'
Publikováno v:
Transactions of the Karelian Research Centre of the Russian Academy of Sciences, Vol 0, Iss 11 (2018)
Shungite rocks of the Onega Paleoproterozoic structure are volcanogenic-sedimentary Precambrian carbon-bearing formations that vary in genesis, mineral composition, structureand carbon (shungite) content. Shungite rocks have industrially useful prope
Externí odkaz:
https://doaj.org/article/6c67fcf3b71e4acab52498c613359728