Geophysical data on the structure of the southeastern part of the Wind Belt synclinorium
Authors:
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:
(Archived) Without section
Funding:
None
References
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