Structural and tectonic plan of the eastern part of the Keevian subzone of the Kareliids based on geological and geophysical data.
Abstract
Mica-bearing pegmatites discovered during geological survey works of the NWTSU, confined to the rocks of the Keivka series of the Lower Proterozoic, allow us to consider the Keivka 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 shales. Proc. Leningr. geol. dir., 1940, No. 5.
- Kharitonov L. Ya. Structure and Stratigraphy of the Karelides of the Eastern Part of the Baltic Shield. M., Nedra, 1966.
- Alkaline granites of the Kola Peninsula. Collection of articles. Moscow, PH of the AS USSR, 1958.
Similar articles
Prospects of ore bearing capacity of Burakovsko-Aganozersky massif of basic and ultrabasic rocks according to geophysical data
1974 V. K. Polikarpov, S. V. Shatilov
Geophysical data on the structure of the southeastern part of the Wind Belt synclinorium
1974 N. N. Bolgurtsev