Structural-tectonic plan of the eastern part of the Keevskaya ian subzone of the Kareliids based on according to geological and geophysical data .
Abstract
The mica-bearing pegmatites identified during geological survey work of the NWTSU, confined to the rocks of the Keev series of the Lower Proterozoic, make it possible to consider the Keev subzone of the Karelides as promising for muscovite.
Область исследования:
(Archived) Without section
Funding:
None
References
- Sokolov P. V. Geology of the Keiv Plateau and the Keiv Formation of crystalline schists. Tr. Leningr. geol. upr. , 1940, No. 5 (in Russian)
- Kharitonov L. Ya. Structure and Stratigraphy of the Karelides of the Eastern Part of the Baltic Shield. M., Nedra, 1966 (in Russian)
- Shchelochnye granity Kol'skogo poluostrova Alkaline granites of the Kola Peninsula. Sb. statei Collection of articles. M., Izd-vo AN SSSR , 1958 (in Russian)
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