gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2024-15-3-0759USGZLAgtcrust-1848Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICST-t ЭВОЛЮЦИЯ РАННЕПРОТЕРОЗОЙСКИХ ПОРОД СЕВЕРНОГО ПРИЛАДОЖЬЯ ПО ДАННЫМ ИЗУЧЕНИЯ U-Pb, Rb-Sr И Sm-Nd СИСТЕМ В МИНЕРАЛАХT-t Evolution of the Early Proterozoic Rocks in the Northern Ladoga Region from the Data on U-Pb, Rb-Sr and Sm-Nd Systems in MineralsБалтыбаевШ. К.BaltybaevSh. K.

199034, Санкт-Петербург, наб. Макарова, 2; 199034, Санкт-Петербург, наб. Университетская, 7/9

Shauket K. Baltybaev

2 Makarova Emb, Saint Petersburg, 199034; 7-9 Universitetskaya Emb, Saint Petersburg 199034

shauket@mail.ruСаватенковВ. М.SavatenkovV. M.

199034, Санкт-Петербург, наб. Макарова, 2

2 Makarova Emb, Saint Petersburg, 199034

ПетраковаМ. Е.PetrakovaM. E.

199034, Санкт-Петербург, наб. Макарова, 2

2 Makarova Emb, Saint Petersburg, 199034

Институт геологии и геохронологии докембрия РАН; Санкт-Петербургский государственный университетРоссияInstitute of Precambrian Geology and Geochronology, Russian Academy of Sciences; Saint Petersburg State UniversityRussian FederationИнститут геологии и геохронологии докембрия РАНРоссияInstitute of Precambrian Geology and Geochronology, Russian Academy of SciencesRussian Federation202418062024153759759Copyright © Балтыбаев Ш.К., Саватенков В.М., Петракова М.Е., 20242024Балтыбаев Ш.К., Саватенков В.М., Петракова М.Е.Baltybaev S.K., Savatenkov V.M., Petrakova M.E.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.gt-crust.ru/jour/article/view/1848

Приводятся результаты изучения изотопных систем в минералах и породах южной окраины эпиархейского Карельского кратона в зоне сочленения с породами Свекофеннского подвижного пояса. Оценки возраста минералов метаморфических пород с использованием U-Pb, Sm-Nd и Rb-Sr изотопных систем позволили построить T-t тренд от ~1.88 до 1.61 млрд лет назад, который отражает историю остывания широкого спектра метаморфических пород от пиковых значений около 650–700 °С 1.88–1.79 млрд лет назад (U-Pb возраст монацитов и наиболее древний кажущийся Sm-Nd возраст амфиболов) до 300–400 °C 1.61 млрд лет назад (модельный Rb-Sr возраст биотитов) в зонах низко- и среднетемпературного метаморфизма. Cпецифика выведения глубинных пород к современной эрозионной поверхности и полученный T-t тренд увязываются с развитием покровно-надвиговых структур при эксгумации свекофеннид. Предполагается также существенная роль дифференциальных вертикально-блоковых перемещений во время посторогенного коллапса растяжения и позднейшего рифтогенеза.

This paper presents the results of a study of isotopic systems in minerals and rocks in southern margin of the epi-Archean Karelian craton in the zone of its junction with the Svecofennian mobile belt. U-Pb, Sm-Nd and Rb-Sr mineral ages of metamorphic rocks allowed reconstructing a T-t trend during ~1.88–1.61 Ga, which reflects a wide-ranging cooling history of metamorphic rocks from the peak values of about 650–700 °C at 1.88–1.79 Ga (U-Pb age of monazites and apparent oldest Sm-Nd age of amphiboles) to 300–400 °C at 1.61 Ga (model Rb-Sr age of biotites) in zones of low- and medium-temperature metamorphism. The specificity of removal of deep-seated rocks to the present-day erosion surface and the reconstructed T-t trend comply with the development of thrust-nappe structures during the exhumation of the Svecofennids. It is also assumed that differential vertical block movements played a significant role during the post-orogenic extensional collapse and neorifting.

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The authors declare that there are no conflicts of interest present.