Synergetic tectonics. 3. The main tectonic regularity in the structure of continental margins
Tectonic evolution of continental outskirts (CO) is considered as a result of selfdevelopment in relation with periodical orthogonal change of the Earth's proper rotation axis position — tectonic (T) stages. Relation of Tstages with folding, their organizing role in the Wilson cycle and accordi...
Збережено в:
| Дата: | 2013 |
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| Автор: | |
| Формат: | Стаття |
| Мова: | Російська |
| Опубліковано: |
S. Subbotin Institute of Geophysics of the NAS of Ukraine
2013
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| Онлайн доступ: | https://journals.uran.ua/geofizicheskiy/article/view/111342 |
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| Назва журналу: | Geofizicheskiy Zhurnal |
Репозитарії
Geofizicheskiy Zhurnal| Резюме: | Tectonic evolution of continental outskirts (CO) is considered as a result of selfdevelopment in relation with periodical orthogonal change of the Earth's proper rotation axis position — tectonic (T) stages. Relation of Tstages with folding, their organizing role in the Wilson cycle and accordingly in KO structure is under investigation. A model of CO evolution is proposed, inherent types of crystalline crust, sedimentary basins, orogenies are under analysis. Important role of horizontal and vertical sets of Tstages in the studies and contemporary CO structure has been shown. Basic provisions of tectonics of the sets of tectonic stages are demonstrated on examples of tectonic development of south and west CO of East European plate. |
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