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.
How to cite:
Verba V.V., Gaskelberg V.G. Structural-tectonic plan of the eastern part of the Keevskaya ian subzone of the Kareliids based on according to geological and geophysical data . // Journal of Mining Institute. 1974. Vol. 66. Iss. 2. p. 44-47.
