Precambrian of the Ukrainian Shield and Plate Tectonics
By the example of the Ukrainian Shield Ingul megablock the reconstruction features of the plate tectonic development of the lithosphere in the Archean - Early Proterozoic have been shown. We analyze the geological model proposed by E. B. Glevassky in comparison with the tectonophysical data on the m...
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| Дата: | 2012 |
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| Формат: | Стаття |
| Мова: | rus |
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Subbotin Institute of Geophysics of the NAS of Ukraine
2012
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| Онлайн доступ: | https://journals.uran.ua/geofizicheskiy/article/view/116694 |
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| Назва журналу: | Geofizicheskiy Zhurnal |
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Geofizicheskiy Zhurnal| id |
journalsuranua-geofizicheskiy-article-116694 |
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journalsuranua-geofizicheskiy-article-1166942020-10-07T12:21:02Z Precambrian of the Ukrainian Shield and Plate Tectonics Gintov, O.B. By the example of the Ukrainian Shield Ingul megablock the reconstruction features of the plate tectonic development of the lithosphere in the Archean - Early Proterozoic have been shown. We analyze the geological model proposed by E. B. Glevassky in comparison with the tectonophysical data on the megablock. The proceedings of the independent studies are consistent with each other within the framework of the plate tectonic approach taking into account PT-conditions of the Early Precambrian. In contrast to the geological model providing the collision nature of the megablock granitoids, the tectonophysical model establishes that most granite massifs were formed in the process of microplates pushing apart. Subbotin Institute of Geophysics of the NAS of Ukraine 2012-12-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116694 10.24028/gzh.0203-3100.v34i6.2012.116694 Geofizicheskiy Zhurnal; Vol. 34 No. 6 (2012); 3-21 Геофизический журнал; Том 34 № 6 (2012); 3-21 Геофізичний журнал; Том 34 № 6 (2012); 3-21 2524-1052 0203-3100 rus https://journals.uran.ua/geofizicheskiy/article/view/116694/110756 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0 |
| institution |
Geofizicheskiy Zhurnal |
| collection |
OJS |
| language |
rus |
| format |
Article |
| author |
Gintov, O.B. |
| spellingShingle |
Gintov, O.B. Precambrian of the Ukrainian Shield and Plate Tectonics |
| author_facet |
Gintov, O.B. |
| author_sort |
Gintov, O.B. |
| title |
Precambrian of the Ukrainian Shield and Plate Tectonics |
| title_short |
Precambrian of the Ukrainian Shield and Plate Tectonics |
| title_full |
Precambrian of the Ukrainian Shield and Plate Tectonics |
| title_fullStr |
Precambrian of the Ukrainian Shield and Plate Tectonics |
| title_full_unstemmed |
Precambrian of the Ukrainian Shield and Plate Tectonics |
| title_sort |
precambrian of the ukrainian shield and plate tectonics |
| description |
By the example of the Ukrainian Shield Ingul megablock the reconstruction features of the plate tectonic development of the lithosphere in the Archean - Early Proterozoic have been shown. We analyze the geological model proposed by E. B. Glevassky in comparison with the tectonophysical data on the megablock. The proceedings of the independent studies are consistent with each other within the framework of the plate tectonic approach taking into account PT-conditions of the Early Precambrian. In contrast to the geological model providing the collision nature of the megablock granitoids, the tectonophysical model establishes that most granite massifs were formed in the process of microplates pushing apart. |
| publisher |
Subbotin Institute of Geophysics of the NAS of Ukraine |
| publishDate |
2012 |
| url |
https://journals.uran.ua/geofizicheskiy/article/view/116694 |
| work_keys_str_mv |
AT gintovob precambrianoftheukrainianshieldandplatetectonics |
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2024-04-21T19:41:11Z |
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2024-04-21T19:41:11Z |
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