EARLY PRECAMBRIAN CRUSTAL EVOLUTION OF THE BELOMORIAN AND TRANS-NORTH CHINA OROGENS AND SUPERCONTINENTS RECONSTRUCTION

Comparative analysis of the crustal evolution of the Early Precambrian Belomorian and Trans-North China orogens (Fig. 1) has shown [Slabunov et al., 2015] that: Both belts were formed by the superposition of two Precambrian orogenies. The earth crust of the Belomorian belt was produced during the Me...

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Published in:Geodynamics & Tectonophysics
Main Authors: A. I. Slabunov, Jinghui Guo, V. V. Balagansky, N. V. Lubnina, Lifei Zhang
Other Authors: joint RFBR-NNSFC project
Format: Article in Journal/Newspaper
Language:English
Published: Institute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch 2017
Subjects:
Daly
Fennoscandian
Lapland
Online Access:https://www.gt-crust.ru/jour/article/view/434
https://doi.org/10.5800/GT-2017-8-3-0293
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description Comparative analysis of the crustal evolution of the Early Precambrian Belomorian and Trans-North China orogens (Fig. 1) has shown [Slabunov et al., 2015] that: Both belts were formed by the superposition of two Precambrian orogenies. The earth crust of the Belomorian belt was produced during the Mesoarchaean to Neoarchaean Belomorian collisional orogeny [Slabunov, 2008; Slabunov et al., 2006] and then was reworked during the Palaeoproterozoic Lapland-Kola collisional orogeny [Daly at al., 2006; Balagansky et al., 2014]. The earth crust of the Trans-North China orogen was formed during a Neoarchean accretionary orogeny and then was reworked during a Paleoproterozoic collisional orogeny [Zhao et al., 2012; Guo et al., 2012, 2005]. The Lapland granulite belt is the core of the Lapland-Kola Palaeoproterozoic collisional orogen in the Fennoscandian shield and the Khondolite belt occupies the same tectonic position in a Palaeoproterozoic collisional orogen in the North China craton. Comparative analysis of the crustal evolution of the Early Precambrian Belomorian and Trans-North China orogens (Fig. 1) has shown [Slabunov et al., 2015] that: Both belts were formed by the superposition of two Precambrian orogenies. The earth crust of the Belomorian belt was produced during the Mesoarchaean to Neoarchaean Belomorian collisional orogeny [Slabunov, 2008; Slabunov et al., 2006] and then was reworked during the Palaeoproterozoic Lapland-Kola collisional orogeny [Daly at al., 2006; Balagansky et al., 2014]. The earth crust of the Trans-North China orogen was formed during a Neoarchean accretionary orogeny and then was reworked during a Paleoproterozoic collisional orogeny [Zhao et al., 2012; Guo et al., 2012, 2005]. The Lapland granulite belt is the core of the Lapland-Kola Palaeoproterozoic collisional orogen in the Fennoscandian shield and the Khondolite belt occupies the same tectonic position in a Palaeoproterozoic collisional orogen in the North China craton.
author2 joint RFBR-NNSFC project
format Article in Journal/Newspaper
author A. I. Slabunov
Jinghui Guo
V. V. Balagansky
N. V. Lubnina
Lifei Zhang
spellingShingle A. I. Slabunov
Jinghui Guo
V. V. Balagansky
N. V. Lubnina
Lifei Zhang
EARLY PRECAMBRIAN CRUSTAL EVOLUTION OF THE BELOMORIAN AND TRANS-NORTH CHINA OROGENS AND SUPERCONTINENTS RECONSTRUCTION
author_facet A. I. Slabunov
Jinghui Guo
V. V. Balagansky
N. V. Lubnina
Lifei Zhang
author_sort A. I. Slabunov
title EARLY PRECAMBRIAN CRUSTAL EVOLUTION OF THE BELOMORIAN AND TRANS-NORTH CHINA OROGENS AND SUPERCONTINENTS RECONSTRUCTION
title_short EARLY PRECAMBRIAN CRUSTAL EVOLUTION OF THE BELOMORIAN AND TRANS-NORTH CHINA OROGENS AND SUPERCONTINENTS RECONSTRUCTION
title_full EARLY PRECAMBRIAN CRUSTAL EVOLUTION OF THE BELOMORIAN AND TRANS-NORTH CHINA OROGENS AND SUPERCONTINENTS RECONSTRUCTION
title_fullStr EARLY PRECAMBRIAN CRUSTAL EVOLUTION OF THE BELOMORIAN AND TRANS-NORTH CHINA OROGENS AND SUPERCONTINENTS RECONSTRUCTION
title_full_unstemmed EARLY PRECAMBRIAN CRUSTAL EVOLUTION OF THE BELOMORIAN AND TRANS-NORTH CHINA OROGENS AND SUPERCONTINENTS RECONSTRUCTION
title_sort early precambrian crustal evolution of the belomorian and trans-north china orogens and supercontinents reconstruction
publisher Institute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch
publishDate 2017
url https://www.gt-crust.ru/jour/article/view/434
https://doi.org/10.5800/GT-2017-8-3-0293
long_lat ENVELOPE(63.761,63.761,-67.513,-67.513)
geographic Daly
geographic_facet Daly
genre Fennoscandian
Lapland
genre_facet Fennoscandian
Lapland
op_source Geodynamics & Tectonophysics; Том 8, № 3 (2017); 569-572
Геодинамика и тектонофизика; Том 8, № 3 (2017); 569-572
2078-502X
op_relation https://www.gt-crust.ru/jour/article/view/434/317
Azimov P.Ya., Slabunov A.I., Stepanova A.V., Serebryakov N.S., Babarina I.I., 2017. The Paleoproterozoic high-pressure Granulites in the Belomorian province of the Fennoscandia: the petrological evidences for continent-continent collision. In: A.I. Slabunov, S.A. Svetov, Sh.K. Baltibaev (Eds.), Early Precambrian vs modern geodynamics. Extended abstracts and field trips guide. KarRC RAS, Petrozavodsk, p. 13–17.
Balagansky V., Shchipansky A., Slabunov A.I., Gorbunov I., Mudruk S., Sidorov M., Azimov P., Egorova S., Stepanova A., Voloshin A., 2015. Archean Kuru-Vaara eclogites in the northern Belomorian province, Fennoscandian shield: crustal architecture, timing and tectonic implications. International Geology Review 57 (11–12), 1543–1565. https:// doi.org/10.1080/00206814.2014.958578.
Daly J.S., Balagansky V.V., Timmerman M.J., Whitehouse M.J., 2006. The Lapland-Kola orogen: Palaeoproterozoic collision and accretion of the northern Fennoscandian lithosphere. In: D.G. Gee., R.A. Stephenson (Eds.), European lithosphere dynamics. Geological Society, London, Memoirs, vol. 32, p. 579–598. https://doi.org/10.1144/GSL. MEM.2006.032.01.35.
Guo J.H., Peng P., Chen Y., Jiao S.J., Windley B.F., 2012. UHT sapphirine granulite metamorphism at 1.93–1.92 Ga caused by gabbronorite intrusions: implications for tectonic evolution of the northern margin of the North China craton. Precambrian Research 222–223, 124–142. https://doi.org/10.1016/j.precamres.2011.07.020.
Guo J.H., Sun M., Zhai M.G. 2005. Sm-Nd and SHRIMP U-Pb zircon geochronology of high-pressure granulites in the Sanggan area, North China craton: timing of Paleoproterozoic continental collision. Journal of Asian Earth Sciences 24 (5), 629–642. https://doi.org/10.1016/j.jseaes.2004.01.017.
Lubnina N.V., Slabunov A.I., 2011. Reconstruction of the Kenorland supercontinent in the Neoarchean based on paleomagnetic and geological data. Moscow University Geology Bulletin 66 (4), 242–249. https://doi.org/10.3103/ S0145875211040077.
Slabunov А.I., 2008. Geology and Geodynamics of Archean Mobile Belts (Example from the Belomorian Province of the Fennoscandian Shield). KarRC RAS, Petrozavodsk, 298 p. (in Russian).
Slabunov А.I., Azimov P.Ya., Glebovitsky V.А., Zhang L., Kevlich V.I., 2016. Archean and Paleoproterozoic migmatization in the Belomorian province, Fennoscandian shield: petrology, geochronology and geodynamic setting. Doklady Earth Sciences 467 (1), 71–74. https://doi.org/10.1134/S1028334X16030077.
Slabunov A., Guo J., Balagansky V., Zhang L., Zhang D., Shchipansky A., Li X., Azimov P., 2015. Long-living Early Precambrian mobile belts formed by superposition of Archean and Paleoproterozoic orogenies (examples from the North China and Fennoscandian shields). In: International workshop on the geology of Northeast Asia and the geophysical character of Asian continental margin. Program and Abstracts. Beijing, China, p. 25–26.
Slabunov A.I., Lobach-Zhuchenko S.B., Bibikova E.V., Sorjonen-Ward P., Balagansky V.V., Volodichev O.I., Shchipansky A.A., Svetov S.A., Chekulaev V.P., Arestova N.A., Stepanov V.S., 2006. The Archaean nucleus of the Fennoscandian (Baltic) Shield. In: D.G. Gee., R.A. Stephenson (Eds.), European lithosphere dynamics. Geological Society, London, Memoirs, vol. 32, p. 627–644. https://doi.org/10.1144/GSL.MEM.2006.035.01.37.
Slabunov A.I., Lubnina N.V., 2016. Neoarchean Supercontinent Kenorland: geological and paleomagnetic data. In: 35th International Geological Congress, Cape Town, South Africa. Abstracts. American Geosciences Institute, Alexandria, p. 3751. Available from: http://www.americangeosciences.org/information/igc.
Zhao G., Cawood P.A., Li S., Wilde S.A., Sun M., Zhang J., He Y., Yin C., 2012. Amalgamation of the North China craton: Key issues and discussion. Precambrian Research 222–223, 55–76. https://doi.org/10.1016/j.precamres.2012.09.016.
https://www.gt-crust.ru/jour/article/view/434
doi:10.5800/GT-2017-8-3-0293
op_rights Authors who publish with this Online Publication agree to the following terms:Authors retain copyright and grant the Online Publication right of first publication with the work simultaneously licensed under a Creative Commons Attribution License that allows others to share the work with an acknowledgement of the work's authorship and initial publication in this Online Publication.Authors are able to enter into separate, additional contractual arrangements for the non-exclusive distribution of the Online Publication's published version of the work (e.g., post it to an institutional repository or publish it in a book), with an acknowledgement of its initial publication in this Online Publication.Authors are permitted and encouraged to post their work online (e.g., in institutional repositories or on their website) prior to and during the submission process, as it can lead to productive exchanges, as well as earlier and greater citation of published work (See The Effect of Open Access).
Авторы, публикующие статьи в данном сетевом издании, соглашаются на следующее:1. Авторы сохраняют за собой авторские права и предоставляют сетевому изданию право первой публикации работы, которая по истечении 6 месяцев после публикации автоматически лицензируется на условиях Creative Commons Attribution License , что позволяет другим распространять данную работу с обязательным сохранением ссылок на авторов оригинальной работы и оригинальную публикацию в этом издании.2. Авторы имеют право размещать свою работу в сети Интернет на ресурсах, не относящихся к другим издательствам (например, на персональном сайте), в форме и содержании, принятыми издателем для опубликования в сетевом издании, так как это может привести к продуктивному обсуждению и большему количеству ссылок на данную работу (См. The Effect of Open Access).
op_rightsnorm CC-BY
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https://doi.org/10.1144/GSL
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spelling ftjgat:oai:oai.gtcrust.elpub.ru:article/434 2023-05-15T16:12:56+02:00 EARLY PRECAMBRIAN CRUSTAL EVOLUTION OF THE BELOMORIAN AND TRANS-NORTH CHINA OROGENS AND SUPERCONTINENTS RECONSTRUCTION A. I. Slabunov Jinghui Guo V. V. Balagansky N. V. Lubnina Lifei Zhang joint RFBR-NNSFC project 2017-10-14 application/pdf https://www.gt-crust.ru/jour/article/view/434 https://doi.org/10.5800/GT-2017-8-3-0293 eng eng Institute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch https://www.gt-crust.ru/jour/article/view/434/317 Azimov P.Ya., Slabunov A.I., Stepanova A.V., Serebryakov N.S., Babarina I.I., 2017. The Paleoproterozoic high-pressure Granulites in the Belomorian province of the Fennoscandia: the petrological evidences for continent-continent collision. In: A.I. Slabunov, S.A. Svetov, Sh.K. Baltibaev (Eds.), Early Precambrian vs modern geodynamics. Extended abstracts and field trips guide. KarRC RAS, Petrozavodsk, p. 13–17. Balagansky V., Shchipansky A., Slabunov A.I., Gorbunov I., Mudruk S., Sidorov M., Azimov P., Egorova S., Stepanova A., Voloshin A., 2015. Archean Kuru-Vaara eclogites in the northern Belomorian province, Fennoscandian shield: crustal architecture, timing and tectonic implications. International Geology Review 57 (11–12), 1543–1565. https:// doi.org/10.1080/00206814.2014.958578. Daly J.S., Balagansky V.V., Timmerman M.J., Whitehouse M.J., 2006. The Lapland-Kola orogen: Palaeoproterozoic collision and accretion of the northern Fennoscandian lithosphere. In: D.G. Gee., R.A. Stephenson (Eds.), European lithosphere dynamics. Geological Society, London, Memoirs, vol. 32, p. 579–598. https://doi.org/10.1144/GSL. MEM.2006.032.01.35. Guo J.H., Peng P., Chen Y., Jiao S.J., Windley B.F., 2012. UHT sapphirine granulite metamorphism at 1.93–1.92 Ga caused by gabbronorite intrusions: implications for tectonic evolution of the northern margin of the North China craton. Precambrian Research 222–223, 124–142. https://doi.org/10.1016/j.precamres.2011.07.020. Guo J.H., Sun M., Zhai M.G. 2005. Sm-Nd and SHRIMP U-Pb zircon geochronology of high-pressure granulites in the Sanggan area, North China craton: timing of Paleoproterozoic continental collision. Journal of Asian Earth Sciences 24 (5), 629–642. https://doi.org/10.1016/j.jseaes.2004.01.017. Lubnina N.V., Slabunov A.I., 2011. Reconstruction of the Kenorland supercontinent in the Neoarchean based on paleomagnetic and geological data. Moscow University Geology Bulletin 66 (4), 242–249. https://doi.org/10.3103/ S0145875211040077. Slabunov А.I., 2008. Geology and Geodynamics of Archean Mobile Belts (Example from the Belomorian Province of the Fennoscandian Shield). KarRC RAS, Petrozavodsk, 298 p. (in Russian). Slabunov А.I., Azimov P.Ya., Glebovitsky V.А., Zhang L., Kevlich V.I., 2016. Archean and Paleoproterozoic migmatization in the Belomorian province, Fennoscandian shield: petrology, geochronology and geodynamic setting. Doklady Earth Sciences 467 (1), 71–74. https://doi.org/10.1134/S1028334X16030077. Slabunov A., Guo J., Balagansky V., Zhang L., Zhang D., Shchipansky A., Li X., Azimov P., 2015. Long-living Early Precambrian mobile belts formed by superposition of Archean and Paleoproterozoic orogenies (examples from the North China and Fennoscandian shields). In: International workshop on the geology of Northeast Asia and the geophysical character of Asian continental margin. Program and Abstracts. Beijing, China, p. 25–26. Slabunov A.I., Lobach-Zhuchenko S.B., Bibikova E.V., Sorjonen-Ward P., Balagansky V.V., Volodichev O.I., Shchipansky A.A., Svetov S.A., Chekulaev V.P., Arestova N.A., Stepanov V.S., 2006. The Archaean nucleus of the Fennoscandian (Baltic) Shield. In: D.G. Gee., R.A. Stephenson (Eds.), European lithosphere dynamics. Geological Society, London, Memoirs, vol. 32, p. 627–644. https://doi.org/10.1144/GSL.MEM.2006.035.01.37. Slabunov A.I., Lubnina N.V., 2016. Neoarchean Supercontinent Kenorland: geological and paleomagnetic data. In: 35th International Geological Congress, Cape Town, South Africa. Abstracts. American Geosciences Institute, Alexandria, p. 3751. Available from: http://www.americangeosciences.org/information/igc. Zhao G., Cawood P.A., Li S., Wilde S.A., Sun M., Zhang J., He Y., Yin C., 2012. Amalgamation of the North China craton: Key issues and discussion. Precambrian Research 222–223, 55–76. https://doi.org/10.1016/j.precamres.2012.09.016. https://www.gt-crust.ru/jour/article/view/434 doi:10.5800/GT-2017-8-3-0293 Authors who publish with this Online Publication agree to the following terms:Authors retain copyright and grant the Online Publication right of first publication with the work simultaneously licensed under a Creative Commons Attribution License that allows others to share the work with an acknowledgement of the work's authorship and initial publication in this Online Publication.Authors are able to enter into separate, additional contractual arrangements for the non-exclusive distribution of the Online Publication's published version of the work (e.g., post it to an institutional repository or publish it in a book), with an acknowledgement of its initial publication in this Online Publication.Authors are permitted and encouraged to post their work online (e.g., in institutional repositories or on their website) prior to and during the submission process, as it can lead to productive exchanges, as well as earlier and greater citation of published work (See The Effect of Open Access). Авторы, публикующие статьи в данном сетевом издании, соглашаются на следующее:1. Авторы сохраняют за собой авторские права и предоставляют сетевому изданию право первой публикации работы, которая по истечении 6 месяцев после публикации автоматически лицензируется на условиях Creative Commons Attribution License , что позволяет другим распространять данную работу с обязательным сохранением ссылок на авторов оригинальной работы и оригинальную публикацию в этом издании.2. Авторы имеют право размещать свою работу в сети Интернет на ресурсах, не относящихся к другим издательствам (например, на персональном сайте), в форме и содержании, принятыми издателем для опубликования в сетевом издании, так как это может привести к продуктивному обсуждению и большему количеству ссылок на данную работу (См. The Effect of Open Access). CC-BY Geodynamics & Tectonophysics; Том 8, № 3 (2017); 569-572 Геодинамика и тектонофизика; Том 8, № 3 (2017); 569-572 2078-502X info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2017 ftjgat https://doi.org/10.5800/GT-2017-8-3-0293 https://doi.org/10.1080/00206814.2014.958578 https://doi.org/10.1144/GSL https://doi.org/10.1016/j.precamres.2011.07.020 https://doi.org/10.1016/j.jseaes.2004.01.017 https://doi.org/10.1134/S1028334X16030 2022-07-19T15:36:53Z Comparative analysis of the crustal evolution of the Early Precambrian Belomorian and Trans-North China orogens (Fig. 1) has shown [Slabunov et al., 2015] that: Both belts were formed by the superposition of two Precambrian orogenies. The earth crust of the Belomorian belt was produced during the Mesoarchaean to Neoarchaean Belomorian collisional orogeny [Slabunov, 2008; Slabunov et al., 2006] and then was reworked during the Palaeoproterozoic Lapland-Kola collisional orogeny [Daly at al., 2006; Balagansky et al., 2014]. The earth crust of the Trans-North China orogen was formed during a Neoarchean accretionary orogeny and then was reworked during a Paleoproterozoic collisional orogeny [Zhao et al., 2012; Guo et al., 2012, 2005]. The Lapland granulite belt is the core of the Lapland-Kola Palaeoproterozoic collisional orogen in the Fennoscandian shield and the Khondolite belt occupies the same tectonic position in a Palaeoproterozoic collisional orogen in the North China craton. Comparative analysis of the crustal evolution of the Early Precambrian Belomorian and Trans-North China orogens (Fig. 1) has shown [Slabunov et al., 2015] that: Both belts were formed by the superposition of two Precambrian orogenies. The earth crust of the Belomorian belt was produced during the Mesoarchaean to Neoarchaean Belomorian collisional orogeny [Slabunov, 2008; Slabunov et al., 2006] and then was reworked during the Palaeoproterozoic Lapland-Kola collisional orogeny [Daly at al., 2006; Balagansky et al., 2014]. The earth crust of the Trans-North China orogen was formed during a Neoarchean accretionary orogeny and then was reworked during a Paleoproterozoic collisional orogeny [Zhao et al., 2012; Guo et al., 2012, 2005]. The Lapland granulite belt is the core of the Lapland-Kola Palaeoproterozoic collisional orogen in the Fennoscandian shield and the Khondolite belt occupies the same tectonic position in a Palaeoproterozoic collisional orogen in the North China craton. Article in Journal/Newspaper Fennoscandian Lapland Geodynamics & Tectonophysics (E-Journal) Daly ENVELOPE(63.761,63.761,-67.513,-67.513) Geodynamics & Tectonophysics 8 3 569 572

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