New palaeomagnetic data for Palaeoproterozoic AMCG complexes of the Ukrainian Shield
A palaeomagnetic study of rocks for two Palaeoproterozoic anorthosite-mangerite-charnockite-granite (AMCG) complexes in the Ukrainian Shield was done to put additional constraints on the interpretation of palaeogeography of Fennoscandia and Volgo-Sarmatia in the Palaeoproterozoic. With this study, 5...
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Subbotin Institute of Geophysics of the NAS of Ukraine
2023
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ftjeepe:oai:ojs.journals.uran.ua:article/286283 2023-10-01T03:55:53+02:00 New palaeomagnetic data for Palaeoproterozoic AMCG complexes of the Ukrainian Shield Нові палеомагнітні дані щодо палеопротерозойського AMЧГ комплекса Українського щита Bakhmutov, V.G. Mytrokhyn, O.V. Poliachenko, I.B. Cherkes, S.I. 2023-08-30 application/pdf https://journals.uran.ua/geofizicheskiy/article/view/286283 eng eng Subbotin Institute of Geophysics of the NAS of Ukraine https://journals.uran.ua/geofizicheskiy/article/view/286283/280415 https://journals.uran.ua/geofizicheskiy/article/view/286283 Авторське право (c) 2023 V.G. Bakhmutov, O.V. Mytrokhyn, I.B. Poliachenko, S.I. Cherkes https://creativecommons.org/licenses/by-nc-sa/4.0 Геофізичний журнал; Том 45 № 4 (2023): Geofizicheskiy Zhurnal; Vol. 45 No. 4 (2023): Геофизический журнал; Том 45 № 4 (2023): 2524-1052 0203-3100 Ukrainian shield Proterozoic palaeomagnetism AMCG complexes tectonic reconstruction Український щит протерозой палеомагнетизм АМЧГ комплекси тектонічна реконструкція info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2023 ftjeepe 2023-09-05T01:00:08Z A palaeomagnetic study of rocks for two Palaeoproterozoic anorthosite-mangerite-charnockite-granite (AMCG) complexes in the Ukrainian Shield was done to put additional constraints on the interpretation of palaeogeography of Fennoscandia and Volgo-Sarmatia in the Palaeoproterozoic. With this study, 5 sites of Korsun-Novomyrhorod and 3 sites of Korosten AMCG complexes in central and north-western parts of the shield, respectively, were chosen for palaeomagnetic sampling given the geological, modern geochronological and previous palaeomagnetic data. Primary remanent magnetization was isolated on samples of anorthosites,Gabbro, and monzonites within a narrow time interval of U-Pb geochronology dataset of 1.76—1.75Ga. The palaeomagnetic poles calculated for Korosten and Korsun-Novomyrhorod complexes are almost identical, which indicates that the Volyn and Ingul Domains developed within a single structure of the Ukrainian Shield since at least 1.75Ga. The new palaeomagnetic pole calculated for all 8 sites (Plat=22.7°N, Plon=167.4°E, A95=3.3°) agrees well with previous studies by Elming et al. [2001, 2010]. The selection of the most reliable palaeomagnetic poles for Fennoscandia and Volgo-Sarmatia of this time indicates that the present position of the Ukrainian Shield relative to Fennoscandia is not the same as for about 1.75Ga, when Fennoscandia occupied a subequatorial position within palaeolatitudes of 5—20°N, and Volgo-Sarmatia was located close to the equator and rotated relative to Fennoscandia counterclockwise by about 40° compared to its present position. Проведено палеомагнітне дослідження порід двох палеопротерозойських анортозит-мангерит-чарнокіт-гранітних (АМЧГ, або AMCG) комплексів Українського щита з метою визначення додаткових обмежень при інтерпретації палеогеографії Фенноскандії та Волго-Сарматії в палеопротерозої за палеомагнітними даними. З урахуванням геологічних, сучасних геохронологічних та отриманих раніше палеомагнітних даних вибрано та досліджено п’ять сайтів Корсунь-Новомиргородського та ... Article in Journal/Newspaper Fennoscandia Electrical Engineering and Power Engineering (EE&PE - E-Journal) |
institution |
Open Polar |
collection |
Electrical Engineering and Power Engineering (EE&PE - E-Journal) |
op_collection_id |
ftjeepe |
language |
English |
topic |
Ukrainian shield Proterozoic palaeomagnetism AMCG complexes tectonic reconstruction Український щит протерозой палеомагнетизм АМЧГ комплекси тектонічна реконструкція |
spellingShingle |
Ukrainian shield Proterozoic palaeomagnetism AMCG complexes tectonic reconstruction Український щит протерозой палеомагнетизм АМЧГ комплекси тектонічна реконструкція Bakhmutov, V.G. Mytrokhyn, O.V. Poliachenko, I.B. Cherkes, S.I. New palaeomagnetic data for Palaeoproterozoic AMCG complexes of the Ukrainian Shield |
topic_facet |
Ukrainian shield Proterozoic palaeomagnetism AMCG complexes tectonic reconstruction Український щит протерозой палеомагнетизм АМЧГ комплекси тектонічна реконструкція |
description |
A palaeomagnetic study of rocks for two Palaeoproterozoic anorthosite-mangerite-charnockite-granite (AMCG) complexes in the Ukrainian Shield was done to put additional constraints on the interpretation of palaeogeography of Fennoscandia and Volgo-Sarmatia in the Palaeoproterozoic. With this study, 5 sites of Korsun-Novomyrhorod and 3 sites of Korosten AMCG complexes in central and north-western parts of the shield, respectively, were chosen for palaeomagnetic sampling given the geological, modern geochronological and previous palaeomagnetic data. Primary remanent magnetization was isolated on samples of anorthosites,Gabbro, and monzonites within a narrow time interval of U-Pb geochronology dataset of 1.76—1.75Ga. The palaeomagnetic poles calculated for Korosten and Korsun-Novomyrhorod complexes are almost identical, which indicates that the Volyn and Ingul Domains developed within a single structure of the Ukrainian Shield since at least 1.75Ga. The new palaeomagnetic pole calculated for all 8 sites (Plat=22.7°N, Plon=167.4°E, A95=3.3°) agrees well with previous studies by Elming et al. [2001, 2010]. The selection of the most reliable palaeomagnetic poles for Fennoscandia and Volgo-Sarmatia of this time indicates that the present position of the Ukrainian Shield relative to Fennoscandia is not the same as for about 1.75Ga, when Fennoscandia occupied a subequatorial position within palaeolatitudes of 5—20°N, and Volgo-Sarmatia was located close to the equator and rotated relative to Fennoscandia counterclockwise by about 40° compared to its present position. Проведено палеомагнітне дослідження порід двох палеопротерозойських анортозит-мангерит-чарнокіт-гранітних (АМЧГ, або AMCG) комплексів Українського щита з метою визначення додаткових обмежень при інтерпретації палеогеографії Фенноскандії та Волго-Сарматії в палеопротерозої за палеомагнітними даними. З урахуванням геологічних, сучасних геохронологічних та отриманих раніше палеомагнітних даних вибрано та досліджено п’ять сайтів Корсунь-Новомиргородського та ... |
format |
Article in Journal/Newspaper |
author |
Bakhmutov, V.G. Mytrokhyn, O.V. Poliachenko, I.B. Cherkes, S.I. |
author_facet |
Bakhmutov, V.G. Mytrokhyn, O.V. Poliachenko, I.B. Cherkes, S.I. |
author_sort |
Bakhmutov, V.G. |
title |
New palaeomagnetic data for Palaeoproterozoic AMCG complexes of the Ukrainian Shield |
title_short |
New palaeomagnetic data for Palaeoproterozoic AMCG complexes of the Ukrainian Shield |
title_full |
New palaeomagnetic data for Palaeoproterozoic AMCG complexes of the Ukrainian Shield |
title_fullStr |
New palaeomagnetic data for Palaeoproterozoic AMCG complexes of the Ukrainian Shield |
title_full_unstemmed |
New palaeomagnetic data for Palaeoproterozoic AMCG complexes of the Ukrainian Shield |
title_sort |
new palaeomagnetic data for palaeoproterozoic amcg complexes of the ukrainian shield |
publisher |
Subbotin Institute of Geophysics of the NAS of Ukraine |
publishDate |
2023 |
url |
https://journals.uran.ua/geofizicheskiy/article/view/286283 |
genre |
Fennoscandia |
genre_facet |
Fennoscandia |
op_source |
Геофізичний журнал; Том 45 № 4 (2023): Geofizicheskiy Zhurnal; Vol. 45 No. 4 (2023): Геофизический журнал; Том 45 № 4 (2023): 2524-1052 0203-3100 |
op_relation |
https://journals.uran.ua/geofizicheskiy/article/view/286283/280415 https://journals.uran.ua/geofizicheskiy/article/view/286283 |
op_rights |
Авторське право (c) 2023 V.G. Bakhmutov, O.V. Mytrokhyn, I.B. Poliachenko, S.I. Cherkes https://creativecommons.org/licenses/by-nc-sa/4.0 |
_version_ |
1778524732741648384 |