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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Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine
2014-08-01
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| Series: | Геофизический журнал |
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| Online Access: | https://journals.uran.ua/geofizicheskiy/article/view/116006 |
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| author | O.B. Gintov S. V. Mychak |
| author_facet | O.B. Gintov S. V. Mychak |
| author_sort | O.B. Gintov |
| collection | DOAJ |
| 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°. |
| format | Article |
| id | doaj-art-c9fab6b575db441fb10f51a0f1d48d0b |
| institution | Matheson Library |
| issn | 0203-3100 2524-1052 |
| language | English |
| publishDate | 2014-08-01 |
| publisher | Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine |
| record_format | Article |
| series | Геофизический журнал |
| spelling | doaj-art-c9fab6b575db441fb10f51a0f1d48d0b2025-06-27T10:13:47ZengSubbotin Institute of Geophysics of the National Academy of Sciences of UkraineГеофизический журнал0203-31002524-10522014-08-0136410.24028/gzh.0203-3100.v36i4.2014.116006Kinematics 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 plutonsO.B. Gintov0S. V. Mychak1S.I. Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine, KyivS.I. Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine, KyivStrain-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°.https://journals.uran.ua/geofizicheskiy/article/view/116006deformationstensionscracksrapakivianorthositesplutons |
| spellingShingle | O.B. Gintov S. V. Mychak 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 Геофизический журнал deformations tensions cracks rapakivi anorthosites 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 |
| url | https://journals.uran.ua/geofizicheskiy/article/view/116006 |
| work_keys_str_mv | AT obgintov kinematicsofformationoftheukrainianshieldduringtheperiod180173gaagoaccordingtotheresultsofstudiesofrockfracturingofthekorostenandkorsunnovomirgorodplutons AT svmychak kinematicsofformationoftheukrainianshieldduringtheperiod180173gaagoaccordingtotheresultsofstudiesofrockfracturingofthekorostenandkorsunnovomirgorodplutons |