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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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Main Authors: Gintov, O.B., Mychak, S. V.
Format: Article
Language:rus
Published: Subbotin Institute of Geophysics of the NAS of Ukraine 2014
Subjects:
Online Access:https://journals.uran.ua/geofizicheskiy/article/view/116006
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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°. 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 rus https://journals.uran.ua/geofizicheskiy/article/view/116006/110143 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
institution Geofizicheskiy Zhurnal
collection OJS
language rus
topic deformations
tensions
cracks
rapakivi
anorthosites
plutons
rotation of flags
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
topic_facet deformations
tensions
cracks
rapakivi
anorthosites
plutons
rotation of flags
format Article
author Gintov, O.B.
Mychak, S. V.
author_facet Gintov, O.B.
Mychak, S. V.
author_sort Gintov, O.B.
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_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_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_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
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°.
publisher Subbotin Institute of Geophysics of the NAS of Ukraine
publishDate 2014
url https://journals.uran.ua/geofizicheskiy/article/view/116006
work_keys_str_mv AT gintovob kinematicsofformationoftheukrainianshieldduringtheperiod180173gaagoaccordingtotheresultsofstudiesofrockfracturingofthekorostenandkorsunnovomirgorodplutons
AT mychaksv kinematicsofformationoftheukrainianshieldduringtheperiod180173gaagoaccordingtotheresultsofstudiesofrockfracturingofthekorostenandkorsunnovomirgorodplutons
first_indexed 2024-04-21T19:40:28Z
last_indexed 2024-04-21T19:40:28Z
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