Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Tatiana Myskova"'
Publikováno v:
Transactions of the Karelian Research Centre of the Russian Academy of Sciences, Vol 0, Iss 10 (2019)
Based on existing and newly obtained geological materials, complemeted by new petrogeochemical,geochronological and isotope-geochemical data, a new interpretation of the history of the geological development of the Khedozero-Bolshozerskaya structure
Externí odkaz:
https://doaj.org/article/c71b2ed8c4e244e2b2804c1ce7027e76
Publikováno v:
Transactions of the Karelian Research Centre of the Russian Academy of Sciences, Vol 0, Iss 10, Pp 34-62 (2016)
The geochemical and isotopic data were obtained for gneisses of the Kola Series, Baltic Shield. They are metamorphosed in granulite facies and interpreted according to the igneous nature of zircons and gneisses. The biotitic and garnet-biotitic gneis
Externí odkaz:
https://doaj.org/article/23d4a6f638bc4438a8a2c736c135c930
Publikováno v:
Proceedings of the Karelian Research Centre of the Russian Academy of Sciences. :103
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::44f8a8d47323691ec486a4c297582bb0
https://doi.org/10.17076/geo1688
https://doi.org/10.17076/geo1688
Autor:
Pavel Lvov, Tatiana Myskova
Publikováno v:
Transactions of the Karelian Research Centre of the Russian Academy of Sciences, Vol 0, Iss 10 (2019)
Based on existing and newly obtained geological materials, complemeted by new petrogeochemical,geochronological and isotope-geochemical data, a new interpretation of the history of the geological development of the Khedozero-Bolshozerskaya structure
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::63aa5c53afc394300b9bbcbfd756d5c5
https://doi.org/10.17076/geo996
https://doi.org/10.17076/geo996
Autor:
Raisa Milkevich, Tatiana Myskova
Publikováno v:
Transactions of the Karelian Research Centre of the Russian Academy of Sciences, Vol 0, Iss 10, Pp 34-62 (2016)
The geochemical and isotopic data were obtained for gneisses of the Kola Series, Baltic Shield. They are metamorphosed in granulite facies and interpreted according to the igneous nature of zircons and gneisses. The biotitic and garnet-biotitic gneis
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::76a960824cae4e69b185f4adf2594787
https://doi.org/10.17076/geo359
https://doi.org/10.17076/geo359