PALEOPROTEROZOIC TECTONICS AND EVOLUTIONARY MODEL OF THE ONEGA SYNCLINORIUM

Consideration is being given to the Onega Paleoproterozoic structure (Onega synclinorium, OS) as a tectonotype of intraplate negative structures, which experience intermittent subsidence over a long period of time. The paper presents a model of the OS and discusses its tectonic evolution. The model...

Full description

Bibliographic Details

Published in:	Геодинамика и тектонофизика
Main Authors:	S. Yu. Kolodyazhny, N. B. Kuznetsov, A. V. Poleshchuk, D. S. Zykov, E. A. Shalaeva
Format:	Article
Language:	English
Published:	Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2023-08-01
Subjects:	onega paleoproterozoic structure intraplate tectonics geodynamics shear zone imbricate fan detachment seismic profiling
Online Access:	https://www.gt-crust.ru/jour/article/view/1717