Geophysical data on the structure of the southeastern part of the Vetreny Poyas synclinorium
Authors:
Abstract
The Vetreny Poyas structural zone is a series of higher-order structures and regionally is a southeastern continuation of the East Karelian synclinorium zone. To the northeast, the Vetreny Poyas zone is bounded by the Belomorian block of gneisses and gneiss-granites, and to the southwest of it granitoids of the Vodlozero block are developed.
Область исследования:
(Archived) Without section
Funding:
None
References
- Gafarov R. A. Structure of the Precambrian Basement of the North of the Russian Platform. Izd-vo AN SSSR, 1963 (in Russian)
- Geologic Structure of the Basement of the Russian Plate. L., Nedra, 1967. Authors: V. N. Zander, Yu. I. Tomashunas, A. N. Berkovsky (in Russian)
- Porotova G. A. Results of geophysical work on the Vetreny Poyas structural zone and the direction of further investigations. In the book: Issues of Geology and Regularities of the Location of Mineral Resources in Karelia. Petrozavodsk, 1966 (in Russian)
- Tsirulnikova M. Ya., Sokol R. S. Features of the tectonic structure of the eastern part of the Baltic Shield according to geophysical data. In the book: Geology and Deep Structure of the Eastern Part of the Baltic Shield. L., Nauka, 1968 (in Russian)
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