gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2026-17-1-0872ALUDIMgtcrust-2202Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSПАЛЕОГАЙОТЫ ДЖИДИНСКОЙ ОСТРОВОДУЖНОЙ СИСТЕМЫ ПАЛЕОАЗИАТСКОГО ОКЕАНА: ГЕОЛОГИЧЕСКОЕ СТРОЕНИЕ, СОСТАВ, ВОЗРАСТ, СРАВНИТЕЛЬНЫЙ АНАЛИЗ С ПОДОБНЫМИ СТРУКТУРАМИ ЦЕНТРАЛЬНО-АЗИАТСКОГО СКЛАДЧАТОГО ПОЯСА, ГЕОДИНАМИЧЕСКИЕ МОДЕЛИPALEOGUYOTS OF THE DZHIDA ISLAND-ARC SYSTEM OF THE PALEO-ASIAN OCEAN: STRUCTURE, COMPOSITION, AGE, COMPARATIVE ANALYSIS WITH SIMILAR STRUCTURES OF THE CENTRAL ASIAN FOLD BELT, GEODYNAMIC MODELShttps://orcid.org/0000-0002-2890-1105ГордиенкоИ. В.GordienkoI. V.

670047, Улан-Удэ, ул. Сахьяновой, 6а, Республика Бурятия 

6а Sakhyanova St, Ulan-Ude 670047, Republic of Buryatia

ivgord1936@yandex.ruГорноваМ. А.GornovaM. A.

664033, Иркутск, ул. Фаворского, 1а 

1а Favorsky St, Irkutsk 664033

https://orcid.org/0000-0002-6701-2570ЕлбаевА. Л.ElbaevА. L.

670047, Улан-Удэ, ул. Сахьяновой, 6а, Республика Бурятия

6а Sakhyanova St, Ulan-Ude 670047, Republic of Buryatia

https://orcid.org/0000-0001-5944-2047МедведевA. Я.MedvedevA. Ya.

664033, Иркутск, ул. Фаворского, 1а

1а Favorsky St, Irkutsk 664033

ЛанцеваВ. С.LantsevaV. S.

670047, Улан-Удэ, ул. Сахьяновой, 6а, Республика Бурятия

6а Sakhyanova St, Ulan-Ude 670047, Republic of Buryatia

Геологический институт им. Н.Л. Добрецова СО РАНРоссияDobretsov Geological Institute, Siberian Branch of the Russian Academy of SciencesRussian FederationИнститут геохимии им. А.П. Виноградова СО РАНРоссияVinogradov Institute of Geochemistry, Siberian Branch of the Russian Academy of SciencesRussian Federation202617022026171872872Copyright © Гордиенко И.В., Горнова М.А., Елбаев А.Л., Медведев A.Я., Ланцева В.С., 20262026Гордиенко И.В., Горнова М.А., Елбаев А.Л., Медведев A.Я., Ланцева В.С.Gordienko I.V., Gornova M.A., Elbaev А.L., Medvedev A.Y., Lantseva V.S.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/2202

В составе Джидинской палеоостроводужной системы выделены и охарактеризованы Джидотский и Ургольский крупные палеогайоты, а также ряд более мелких фрагментов древних океанических островов, включенных в аккреционно-коллизионную структуру северо-восточной части Центрально-Азиатского складчатого пояса. Палеогайоты и их фрагменты образуют отдельные блоки тектонического меланжа океанической литосферы в составе крупных аллохтонов. Образование построек палеогайотов происходило преимущественно в эдиакарии – начале раннего кембрия в пределах Палеоазиатского океана под действием горячих точек (мантийных плюмов). Океаническая кора вместе с палеогайотами субдуцировала под Джидинскую энсиматическую островную дугу. Формирование джидинских палеогайотов и островной дуги происходило в одном временном интервале с подобными образованиями Баянхонгорской, Озерной зон Центральной, Западной Монголии, Восточно-Тувинской и Горноалтайской зон Алтае-Саянской области.

The Dzhidot and Urgol large paleoguyots and a number of smaller fragments of oceanic islands close in composition to the paleoguyots within the accretionary-collisional structures of the north-eastern part of the Central Asian orogenic belt are distinguished and described. Paleoguyots and their fragments form separate blocks of the oceanic crust in tectonic mélange as a part of large allochthons. Formation of paleoguyots occurred predominantly in the Ediacaran – beginning of the Early Cambrian in the oceanic environment under the influence of hot spots (mantle plumes). The oceanic crust containing paleogayots was subducted beneath the Dzhida island arc. The formation of the Dzhida paleoguyots and island arc took place at the same time intervas as similar formations of the Bayankhongor and Ozernaya zones of Western, Central Mongolia, East Tuva and Gorny Altay zones the Altay-Sayan region of the Central Asian Fold Belt.

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