Geophysical data on the structure of the southeastern part of the Wind Belt synclinorium
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Abstract
The Wind Belt structural zone is a series of higher-order structures and is a southeastern continuation of the East Karelian syncline zone. From the northeast, the Wind Belt zone is bounded by the Belomorsky block of gneisses and gneisso-granites, and to the southwest of it are distributed granitoids of the Vodlozersky block.
Область исследования:
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References
- Gafarov R. A. Structure of the Precambrian Basement of the North of the Russian Platform. PH AS USSR, 1963.
- Geologic Structure of the Basement of the Russian Plate. L., Nedra, 1967. Authors: V. N. Zander, Y. I. Tomashunas, A. N. Berkovsky.
- Porotova G. A. Results of geophysical works on the structural zone of the Vetrenyi belt and the direction of further investigations. In the book: Issues of Geology and Regularities of the Location of Mineral Resources in Karelia. Petrozavodsk, 1966.
- 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: Deep Structure of the Eastern Part of the Baltic Shield. L., Nauka, 1968.
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