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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Datum:2013
1. Verfasser: Karpenko, I.V.
Format: Artikel
Sprache:Russisch
Veröffentlicht: S. Subbotin Institute of Geophysics of the NAS of Ukraine 2013
Online Zugang:https://journals.uran.ua/geofizicheskiy/article/view/111342
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Geofizicheskiy Zhurnal
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author Karpenko, I.V.
author_facet Karpenko, I.V.
author_sort Karpenko, I.V.
baseUrl_str
collection OJS
datestamp_date 2020-10-07T10:46:54Z
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.
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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. S. 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 ru https://journals.uran.ua/geofizicheskiy/article/view/111342/106343 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
spellingShingle Karpenko, I.V.
Synergetic tectonics. 3. The main tectonic regularity in the structure of continental margins
title 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_short 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
url https://journals.uran.ua/geofizicheskiy/article/view/111342
work_keys_str_mv AT karpenkoiv synergetictectonics3themaintectonicregularityinthestructureofcontinentalmargins