Kinematics of formation of the Ukrainian Shield during the period 1,80-1,73 Ga ago according to the results of studies of rock fracturing of the Korosten and Korsun-Novomirgorod plutons
Strain-deformed state of the earth’s crust of northwestern and central parts of the Ukrainian Shield while jointing the terrains of Fennoscandia and Sarmatia and forming of the Korosten and the Korsun-Novomirgorod plutons of gabbro-anorthosites and rapakivi has been considered here. It is shown that...
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| Date: | 2014 |
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| Main Authors: | , |
| Format: | Article |
| Language: | Russian |
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S. Subbotin Institute of Geophysics of the NAS of Ukraine
2014
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| Online Access: | https://journals.uran.ua/geofizicheskiy/article/view/116006 |
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| Journal Title: | Geofizicheskiy Zhurnal |
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Geofizicheskiy Zhurnal| _version_ | 1856543195319500800 |
|---|---|
| author | Gintov, O.B. Mychak, S. V. |
| author_facet | Gintov, O.B. Mychak, S. V. |
| author_sort | Gintov, O.B. |
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| collection | OJS |
| datestamp_date | 2020-10-07T11:57:02Z |
| description | Strain-deformed state of the earth’s crust of northwestern and central parts of the Ukrainian Shield while jointing the terrains of Fennoscandia and Sarmatia and forming of the Korosten and the Korsun-Novomirgorod plutons of gabbro-anorthosites and rapakivi has been considered here. It is shown that the difference determined by fracturing in the orientation of the axes of the main normal stresses in the formation of the Korosten and Korsun-Novomirgorod plutons in the interval of 1,75-1,8 Ga was according to the fracture formation of the first pluton ahead of the second one at ~10 Ma and Sarmatia turn counterclockwise to 54°. |
| first_indexed | 2025-07-17T11:06:14Z |
| format | Article |
| id | journalsuranua-geofizicheskiy-article-116006 |
| institution | Geofizicheskiy Zhurnal |
| language | Russian |
| last_indexed | 2025-07-17T11:06:14Z |
| publishDate | 2014 |
| publisher | S. Subbotin Institute of Geophysics of the NAS of Ukraine |
| record_format | ojs |
| spelling | journalsuranua-geofizicheskiy-article-1160062020-10-07T11:57:02Z Kinematics of formation of the Ukrainian Shield during the period 1,80-1,73 Ga ago according to the results of studies of rock fracturing of the Korosten and Korsun-Novomirgorod plutons Gintov, O.B. Mychak, S. V. deformations tensions cracks rapakivi anorthosites plutons rotation of flags Strain-deformed state of the earth’s crust of northwestern and central parts of the Ukrainian Shield while jointing the terrains of Fennoscandia and Sarmatia and forming of the Korosten and the Korsun-Novomirgorod plutons of gabbro-anorthosites and rapakivi has been considered here. It is shown that the difference determined by fracturing in the orientation of the axes of the main normal stresses in the formation of the Korosten and Korsun-Novomirgorod plutons in the interval of 1,75-1,8 Ga was according to the fracture formation of the first pluton ahead of the second one at ~10 Ma and Sarmatia turn counterclockwise to 54°. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2014-08-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116006 10.24028/gzh.0203-3100.v36i4.2014.116006 Geofizicheskiy Zhurnal; Vol. 36 No. 4 (2014); 24-36 Геофизический журнал; Том 36 № 4 (2014); 24-36 Геофізичний журнал; Том 36 № 4 (2014); 24-36 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/116006/110143 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0 |
| spellingShingle | deformations tensions cracks rapakivi anorthosites plutons rotation of flags Gintov, O.B. Mychak, S. V. Kinematics of formation of the Ukrainian Shield during the period 1,80-1,73 Ga ago according to the results of studies of rock fracturing of the Korosten and Korsun-Novomirgorod plutons |
| title | Kinematics of formation of the Ukrainian Shield during the period 1,80-1,73 Ga ago according to the results of studies of rock fracturing of the Korosten and Korsun-Novomirgorod plutons |
| title_full | Kinematics of formation of the Ukrainian Shield during the period 1,80-1,73 Ga ago according to the results of studies of rock fracturing of the Korosten and Korsun-Novomirgorod plutons |
| title_fullStr | Kinematics of formation of the Ukrainian Shield during the period 1,80-1,73 Ga ago according to the results of studies of rock fracturing of the Korosten and Korsun-Novomirgorod plutons |
| title_full_unstemmed | Kinematics of formation of the Ukrainian Shield during the period 1,80-1,73 Ga ago according to the results of studies of rock fracturing of the Korosten and Korsun-Novomirgorod plutons |
| title_short | Kinematics of formation of the Ukrainian Shield during the period 1,80-1,73 Ga ago according to the results of studies of rock fracturing of the Korosten and Korsun-Novomirgorod plutons |
| title_sort | kinematics of formation of the ukrainian shield during the period 1,80-1,73 ga ago according to the results of studies of rock fracturing of the korosten and korsun-novomirgorod plutons |
| topic | deformations tensions cracks rapakivi anorthosites plutons rotation of flags |
| topic_facet | deformations tensions cracks rapakivi anorthosites plutons rotation of flags |
| url | https://journals.uran.ua/geofizicheskiy/article/view/116006 |
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