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...
Main Authors: | , , , , |
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Format: | Article |
Language: | English |
Published: |
Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust
2023-08-01
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Series: | Геодинамика и тектонофизика |
Subjects: | |
Online Access: | https://www.gt-crust.ru/jour/article/view/1717 |