Middle-Upper Proterozoic formations of the Keivsky area of the Kola Peninsula
Authors:
Abstract
The Keivsky area of about 10,000 km² is located in the central part of the Kola Peninsula between Efim Lake, the village of Kanevka, the northern foot of the Keiva Upland and the Ponoy River. Structurally, it corresponds to the Keiva synclinorium, stretching northwestward and joining the Voronyinsko‑Porosozersky in the northwest and the Imandra‑Varzugsky in the south ...
Область исследования:
(Archived) Without section
Funding:
None
References
- Bel'kov I. V. Kianite schists of the Keiv Formation. Izdatel'stvo AN SSSR, 1963.
- Lungershausen G. F. Problems of Planetary Geology. Gosgeoltekhizdat, 1963.
- Kharitonov L. Ya. Stratigraphy of the Proterozoic of Karelia, Kola Peninsula and adjacent countries of the Baltic Shield and its structural dissection. Tr. Mezhdunar. geologich. kongressa, XXI Session, Problem IX, 1960.
Similar articles
On the conditions of formation of the oxidation zone of the Osenneye molybdenum deposit
1965 S. V. Sendek
Some features of Late Upper Jurassic effusives of Priargunya and their metallogenic significance
1965 P. A. Strona, N. F. Kiseleva
Acidic Lower Cretaceous subvolcanic and volcanic formations of the North Argun Depression
1965 P. A. Strona, N. F. Kiseleva