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Synergetic tectonics. 3. The main tectonic regularity in the structure of continental margins

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...

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Main Author: Karpenko, I.V.
Format: Article
Language:rus
Published: Subbotin Institute of Geophysics of the NAS of Ukraine 2013
Online Access:https://journals.uran.ua/geofizicheskiy/article/view/111342
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spelling journalsuranua-geofizicheskiy-article-1113422020-10-07T10:46:54Z Synergetic tectonics. 3. The main tectonic regularity in the structure of continental margins Karpenko, I.V. 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. Subbotin Institute of Geophysics of the NAS of Ukraine 2013-03-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/111342 10.24028/gzh.0203-3100.v35i2.2013.111342 Geofizicheskiy Zhurnal; Vol. 35 No. 2 (2013); 65-77 Геофизический журнал; Том 35 № 2 (2013); 65-77 Геофізичний журнал; Том 35 № 2 (2013); 65-77 2524-1052 0203-3100 rus https://journals.uran.ua/geofizicheskiy/article/view/111342/106343 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
institution Geofizicheskiy Zhurnal
collection OJS
language rus
format Article
author Karpenko, I.V.
spellingShingle Karpenko, I.V.
Synergetic tectonics. 3. The main tectonic regularity in the structure of continental margins
author_facet Karpenko, I.V.
author_sort Karpenko, I.V.
title Synergetic tectonics. 3. The main tectonic regularity in the structure of continental margins
title_short Synergetic tectonics. 3. The main tectonic regularity in the structure of continental margins
title_full Synergetic tectonics. 3. The main tectonic regularity in the structure of continental margins
title_fullStr Synergetic tectonics. 3. The main tectonic regularity in the structure of continental margins
title_full_unstemmed Synergetic tectonics. 3. The main tectonic regularity in the structure of continental margins
title_sort synergetic tectonics. 3. the main tectonic regularity in the structure of continental margins
description 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.
publisher Subbotin Institute of Geophysics of the NAS of Ukraine
publishDate 2013
url https://journals.uran.ua/geofizicheskiy/article/view/111342
work_keys_str_mv AT karpenkoiv synergetictectonics3themaintectonicregularityinthestructureofcontinentalmargins
first_indexed 2024-04-21T19:40:16Z
last_indexed 2024-04-21T19:40:16Z
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