References

gtcrust

Геодинамика и тектонофизика

Geodynamics & Tectonophysics

2078-502X

Institute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch

10.5800/GT-2024-15-2-0745

ORDEGX

gtcrust-1815

Research Article

ПАЛЕОГЕОДИНАМИКА

PALEOGEODYNAMICS

РАННЕНЕОПРОТЕРОЗОЙСКИЕ ГРАНИТОИДЫ РЯЗАНОВСКОГО МАССИВА ЕНИСЕЙСКОГО КРЯЖА – ИНДИКАТОРЫ ПРОЯВЛЕНИЯ ГРЕНВИЛЬСКОГО ОРОГЕНЕЗА НА ЗАПАДНОЙ ОКРАИНЕ СИБИРСКОГО КРАТОНА

EARLY NEOPROTEROZOIC GRANITOIDS IN THE RYAZANOVSKY MASSIF OF THE YENISEI RIDGE AS INDICATORS OF THE GRENVILLE OROGENY AT THE WESTERN MARGIN OF THE SIBERIAN CRATON

Ножкин

А. Д.

Nozhkin

A. D.

630090, Новосибирск, прт Академика Коптюга, 3

3 Academician Koptyug Ave, Novosibirsk 630090

Туркина

О. М.

Turkina

O. M.

Новосибирск, пр-т Академика Коптюга, 3

3 Academician Koptyug Ave, Novosibirsk 630090

Лиханов

И. И.

Likhanov

I. I.

3 Academician Koptyug Ave, Novosibirsk 630090

likh@igm.nsc.ru

Ронкин

Ю. Л.

Ronkin

Yu. L.

620016, Екатеринбург, ул. Академика Вонсовского, 15

15 Academician Vonsovsky St, Ekaterinburg 620016

Институт геологии и минералогии им. В.С. Соболева СО РАНРоссияSobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of SciencesRussian Federation

Институт геологии и геохимии им. А.Н. Заварицкого УрО РАНРоссияZavaritsky Institute of Geology and Geochemistry, Ural Branch of the Russian Academy of SciencesRussian Federation

2024

19042024

152745745

2024

Ножкин А.Д., Туркина О.М., Лиханов И.И., Ронкин Ю.Л.

Nozhkin A.D., Turkina O.M., Likhanov I.I., Ronkin Y.L.

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/1815

Реконструкция геологической истории Енисейского кряжа важна не только для понимания тектонической эволюции подвижных поясов на границах древних кратонов, но и для решения вопроса о вхождении Сибирского кратона в состав древнего суперконтинента Родиния. По результатам минералого-петрологических, геохимических и изотопно-геохронологических исследований получены новые данные по петрогеохимическому составу, особенностям петрогенезиса, U-Pb возрасту циркона, Sr и Nd изотопным параметрам пород Рязановского гранитоидного массива, расположенного вблизи Приенисейской зоны разломов Енисейского кряжа. Эти породы представлены высокожелезистыми разностями и сопоставимы с А-гранитами или высокодифференцированными I-гранитами. Их состав эволюционирует от нормальных до субщелочных гранитов и лейкогранитов, отличающихся повышенными концентрациями высокозарядных и радиоактивных элементов. Изотопные (Sr, Nd) характеристики пород свидетельствуют в пользу генерации из древнего корового субстрата, усредненный возраст которого соответствует палеопротерозою. Формирование этих гранитов на рубеже мезо- и неопротерозоя (1013±9.9 млн лет) отвечает времени раннего этапа орогенеза гренвильского возраста и формирования структуры суперконтинента Родиния. Геодинамическая история региона сопоставляется с синхронной последовательностью и схожим стилем тектонотермальных событий по периферии крупных докембрийских кратонов Лаврентии и Балтики, что подтверждает палеоконтинентальные реконструкции вхождения Сибирского кратона в состав Родинии.

Studies of the geological history of the Yenisei Ridge are important not only for understanding the tectonic evolution of mobile belts at the boundaries of ancient cratons but also for problem solving whether the Siberian craton was a part of the Rodinia supercontinent. The mineralogical-petrological, geochemical and isotope-geochronological studies yielded new data on the petrogeochemical composition, petrogenesis features, U-Pb age of zircon, and Sr and 147Sm-143Nd isotopic parameters for the rocks of the Ryazanovsky granitoid massif located near the Yenisei fault zone of the Yenisei Ridge. These rocks are represented by high-ferruginous peraluminous varieties and are comparable to A-granites or highly differentiated I-granites. Their composition evolves from normal to subalkaline granites and leucogranites, characterized by increased concentrations of highly charged and radioactive elements. Isotopic (Sr, Nd) characteristics of the rocks indicate generation from an ancient crustal substrate, the average age of which corresponds to the Paleoproterozoic. The formation of these granites at the Meso-Neoproterozoic boundary (1013±9.9 Ma) corresponds to the early stage of the Grenville orogeny and the formation time of the structure of the Rodinia supercontinent. This episode of regional crustal evolution is correlated with the synchronous successions and similar style of tectonothermal events on the periphery of large Precambrian cratons (Laurentia and Baltica), thus confirming the reliability of the proposed paleocontinental reconstructions of incorporation of the Siberian craton into the Rodinia.

гранитоидыпетрогеохимияU-Pb датированиеSr и Nd изотопный составгренвильский орогенезЕнисейский кряж

granitoidspetrogeochemistryU-Pb datingSr and Nd isotopic compositionGrenville orogenyYenisei Ridge

Работа выполнена за счет средств гранта Российского научного фонда (проект № 21-77-20018) с дополнительной поддержкой полевых работ в рамках госзаданий ИГМ СО РАН (122041400176-0; 122041400057-2).

This study was funded by the Russian Science Foundation (RSF), grant № 21-77-20018, with the fieldwork done as part of the state assignment for the Institute of Geology and Mineralogy SB RAS (122041400176-0; 122041400057-2).

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