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
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
On the nature and peculiarities of waves registered in the first arrivals during seismic exploration on the Baltic Shield
1974 S. A. Ankudinov
First experience of application of frequency electric sounding in the North Onega bauxite-bearing area
1974 G. P. Novitsky
Aeromagnetic survey data on the tectonics of the south-eastern margin of the Pechenga structure
1974 V. P. Zakharov
About the possibility of using industrial currents in geological mapping and searching for ore deposits
1974 V. S. Muzylev