COMMENTS ON THE ARTICLE AUTHORED BY M.V. MINTS AND K.A. DOKUKINA – THE BELOMORIAN ECLOGITE PROVINCE (EASTERN FENNOSCANDIAN SHIELD, RUSSIA): MESO-NEOARCHEAN OR LATE PALEOPROTEROZOIC?

The comments are given on the article authored by M.V. Mints and K.A. Dokukina – The Belomorian Eclogite Province (Eastern Fennoscandian Shield, Russia): Meso-Neoarchean or Late Paleoproterozoic? (Geodynamics & Tectonophysics 2020, 11 (1), 151–200). The Belomorian (White Sea) province of the Fen...

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Published in:Applied Earth Science
Main Authors: S. G. Skublov, A. V. Berezin, L. I. Salimgaraeva, С. Г. Скублов, А. В. Березин, Л. И. Салимгараева
Other Authors: The publication was prepared under the research project of the Institute of Precambrian Geology and Geochronology RAS and supported by the Russian Foundation for Basic Research (Grant 20-35-90001)., Публикация подготовлена в рамках темы НИР ИГГД РАН при поддержке гранта РФФИ 20-35-90001.
Format: Article in Journal/Newspaper
Language:Russian
Published: Institute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch 2021
Subjects:
Online Access:https://www.gt-crust.ru/jour/article/view/1245
https://doi.org/10.5800/GT-2021-12-3-0544
id ftjgat:oai:oai.gtcrust.elpub.ru:article/1245
record_format openpolar
institution Open Polar
collection Geodynamics & Tectonophysics (E-Journal)
op_collection_id ftjgat
language Russian
topic Lu-Hf метод
Precambrian
White Sea mobile belt
petrochronology
isotope age
zircon
U-Pb method
Sm-Nd method
Lu-Hf method
докембрий
Беломорский подвижный пояс
петрохронология
изотопный возраст
циркон
U-Pb метод
Sm-Nd метод
spellingShingle Lu-Hf метод
Precambrian
White Sea mobile belt
petrochronology
isotope age
zircon
U-Pb method
Sm-Nd method
Lu-Hf method
докембрий
Беломорский подвижный пояс
петрохронология
изотопный возраст
циркон
U-Pb метод
Sm-Nd метод
S. G. Skublov
A. V. Berezin
L. I. Salimgaraeva
С. Г. Скублов
А. В. Березин
Л. И. Салимгараева
COMMENTS ON THE ARTICLE AUTHORED BY M.V. MINTS AND K.A. DOKUKINA – THE BELOMORIAN ECLOGITE PROVINCE (EASTERN FENNOSCANDIAN SHIELD, RUSSIA): MESO-NEOARCHEAN OR LATE PALEOPROTEROZOIC?
topic_facet Lu-Hf метод
Precambrian
White Sea mobile belt
petrochronology
isotope age
zircon
U-Pb method
Sm-Nd method
Lu-Hf method
докембрий
Беломорский подвижный пояс
петрохронология
изотопный возраст
циркон
U-Pb метод
Sm-Nd метод
description The comments are given on the article authored by M.V. Mints and K.A. Dokukina – The Belomorian Eclogite Province (Eastern Fennoscandian Shield, Russia): Meso-Neoarchean or Late Paleoproterozoic? (Geodynamics & Tectonophysics 2020, 11 (1), 151–200). The Belomorian (White Sea) province of the Fennoscandia Shield is a key site for studying the tectonics of the early periods because numerous Precambrian eclogites have been found there. It was not anticipated, but the problem of age determinations of the eclogite metamorphism of gabbroids in the White Sea mobile belt has turned out to be extremely relevant not only for this region, but also for the Precambrian geology in general. The reason is that a number of authors determine the age of eclogites as Archean (2.7–2.8 Ga), which makes the White Sea mobile belt the only example of the Archean eclogite metamorphism in the world and, therefore, the only dated evidence in support of the plate tectonic model of the evolution of the Earth’s crust at the earliest stage of its formation. The article consistently provides a critical analysis of the arguments put forward by the supporters of the Archean age of the eclogites of the White Sea mobile belt. Special emphasis is made on the isotope geochronological and geochemical features of the composition of zircons from eclogite samples, as well as on the phase and chemical compositions and distribution patterns of mineral inclusions. Considering the age of eclogite metamorphism that led to the formation of eclogites in the White Sea mobile belt, we propose our interpretation based on a set of independent isotope geochemical dating methods, including the local U- Pb method for heterogeneous zircons with magmatic cores and eclogite rims, the Lu-Hf and Sm-Nd methods for the minerals of eclogite paragenesis (garnet and omphacite). And this age interpretation is fundamentally different from the one described in the commented article: all the three methods independently determine the eclogite metamorphism as Paleoproterozoic and ...
author2 The publication was prepared under the research project of the Institute of Precambrian Geology and Geochronology RAS and supported by the Russian Foundation for Basic Research (Grant 20-35-90001).
Публикация подготовлена в рамках темы НИР ИГГД РАН при поддержке гранта РФФИ 20-35-90001.
format Article in Journal/Newspaper
author S. G. Skublov
A. V. Berezin
L. I. Salimgaraeva
С. Г. Скублов
А. В. Березин
Л. И. Салимгараева
author_facet S. G. Skublov
A. V. Berezin
L. I. Salimgaraeva
С. Г. Скублов
А. В. Березин
Л. И. Салимгараева
author_sort S. G. Skublov
title COMMENTS ON THE ARTICLE AUTHORED BY M.V. MINTS AND K.A. DOKUKINA – THE BELOMORIAN ECLOGITE PROVINCE (EASTERN FENNOSCANDIAN SHIELD, RUSSIA): MESO-NEOARCHEAN OR LATE PALEOPROTEROZOIC?
title_short COMMENTS ON THE ARTICLE AUTHORED BY M.V. MINTS AND K.A. DOKUKINA – THE BELOMORIAN ECLOGITE PROVINCE (EASTERN FENNOSCANDIAN SHIELD, RUSSIA): MESO-NEOARCHEAN OR LATE PALEOPROTEROZOIC?
title_full COMMENTS ON THE ARTICLE AUTHORED BY M.V. MINTS AND K.A. DOKUKINA – THE BELOMORIAN ECLOGITE PROVINCE (EASTERN FENNOSCANDIAN SHIELD, RUSSIA): MESO-NEOARCHEAN OR LATE PALEOPROTEROZOIC?
title_fullStr COMMENTS ON THE ARTICLE AUTHORED BY M.V. MINTS AND K.A. DOKUKINA – THE BELOMORIAN ECLOGITE PROVINCE (EASTERN FENNOSCANDIAN SHIELD, RUSSIA): MESO-NEOARCHEAN OR LATE PALEOPROTEROZOIC?
title_full_unstemmed COMMENTS ON THE ARTICLE AUTHORED BY M.V. MINTS AND K.A. DOKUKINA – THE BELOMORIAN ECLOGITE PROVINCE (EASTERN FENNOSCANDIAN SHIELD, RUSSIA): MESO-NEOARCHEAN OR LATE PALEOPROTEROZOIC?
title_sort comments on the article authored by m.v. mints and k.a. dokukina – the belomorian eclogite province (eastern fennoscandian shield, russia): meso-neoarchean or late paleoproterozoic?
publisher Institute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch
publishDate 2021
url https://www.gt-crust.ru/jour/article/view/1245
https://doi.org/10.5800/GT-2021-12-3-0544
geographic White Sea
geographic_facet White Sea
genre Fennoscandia
Fennoscandian
White Sea
genre_facet Fennoscandia
Fennoscandian
White Sea
op_source Geodynamics & Tectonophysics; Том 12, № 3 (2021); 652-661
Геодинамика и тектонофизика; Том 12, № 3 (2021); 652-661
2078-502X
op_relation https://www.gt-crust.ru/jour/article/view/1245/573
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spelling ftjgat:oai:oai.gtcrust.elpub.ru:article/1245 2023-05-15T16:12:19+02:00 COMMENTS ON THE ARTICLE AUTHORED BY M.V. MINTS AND K.A. DOKUKINA – THE BELOMORIAN ECLOGITE PROVINCE (EASTERN FENNOSCANDIAN SHIELD, RUSSIA): MESO-NEOARCHEAN OR LATE PALEOPROTEROZOIC? КОММЕНТАРИИ К СТАТЬЕ М.В. МИНЦА И К.А. ДОКУКИНОЙ «СУБДУКЦИОННЫЕ ЭКЛОГИТЫ БЕЛОМОРСКОЙ ЭКЛОГИТОВОЙ ПРОВИНЦИИ (ВОСТОК ФЕННОСКАНДИНАВСКОГО ЩИТА, РОССИЯ): МЕЗОАРХЕЙ, НЕОАРХЕЙ ИЛИ ПОЗДНИЙ ПАЛЕОПРОТЕРОЗОЙ?» S. G. Skublov A. V. Berezin L. I. Salimgaraeva С. Г. Скублов А. В. Березин Л. И. Салимгараева The publication was prepared under the research project of the Institute of Precambrian Geology and Geochronology RAS and supported by the Russian Foundation for Basic Research (Grant 20-35-90001). Публикация подготовлена в рамках темы НИР ИГГД РАН при поддержке гранта РФФИ 20-35-90001. 2021-09-17 application/pdf https://www.gt-crust.ru/jour/article/view/1245 https://doi.org/10.5800/GT-2021-12-3-0544 rus rus Institute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch https://www.gt-crust.ru/jour/article/view/1245/573 Balagansky V., Shchipansky A., Slabunov A., 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. Bau M., Dulski P., 1999. Comparing Yttrium and Rare Earths in Hydrothermal Fluids from the Mid-Atlantic Ridge: Implications for Y and REE Behaviour during Near-Vent Mixing and for the Y/Ho Ratio of Proterozoic Seawater. 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Scientific Reports 7 (1), 1–13. https://doi.org/10.1038/srep43022. 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 12, № 3 (2021); 652-661 Геодинамика и тектонофизика; Том 12, № 3 (2021); 652-661 2078-502X Lu-Hf метод Precambrian White Sea mobile belt petrochronology isotope age zircon U-Pb method Sm-Nd method Lu-Hf method докембрий Беломорский подвижный пояс петрохронология изотопный возраст циркон U-Pb метод Sm-Nd метод info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2021 ftjgat https://doi.org/10.5800/GT-2021-12-3-0544 https://doi.org/10.1080/00206814.2014.958578 https://doi.org/10.1016/S0009-2541(98)00142-9 https://doi.org/10.1007/s00410-002-0364-7 https://doi.org/10.1134/S0869591114030035 https://doi.org/10.1134/S102 2022-07-19T15:37:05Z The comments are given on the article authored by M.V. Mints and K.A. Dokukina – The Belomorian Eclogite Province (Eastern Fennoscandian Shield, Russia): Meso-Neoarchean or Late Paleoproterozoic? (Geodynamics & Tectonophysics 2020, 11 (1), 151–200). The Belomorian (White Sea) province of the Fennoscandia Shield is a key site for studying the tectonics of the early periods because numerous Precambrian eclogites have been found there. It was not anticipated, but the problem of age determinations of the eclogite metamorphism of gabbroids in the White Sea mobile belt has turned out to be extremely relevant not only for this region, but also for the Precambrian geology in general. The reason is that a number of authors determine the age of eclogites as Archean (2.7–2.8 Ga), which makes the White Sea mobile belt the only example of the Archean eclogite metamorphism in the world and, therefore, the only dated evidence in support of the plate tectonic model of the evolution of the Earth’s crust at the earliest stage of its formation. The article consistently provides a critical analysis of the arguments put forward by the supporters of the Archean age of the eclogites of the White Sea mobile belt. Special emphasis is made on the isotope geochronological and geochemical features of the composition of zircons from eclogite samples, as well as on the phase and chemical compositions and distribution patterns of mineral inclusions. Considering the age of eclogite metamorphism that led to the formation of eclogites in the White Sea mobile belt, we propose our interpretation based on a set of independent isotope geochemical dating methods, including the local U- Pb method for heterogeneous zircons with magmatic cores and eclogite rims, the Lu-Hf and Sm-Nd methods for the minerals of eclogite paragenesis (garnet and omphacite). And this age interpretation is fundamentally different from the one described in the commented article: all the three methods independently determine the eclogite metamorphism as Paleoproterozoic and ... Article in Journal/Newspaper Fennoscandia Fennoscandian White Sea Geodynamics & Tectonophysics (E-Journal) White Sea Applied Earth Science 1 14