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-2024-15-2-0749

MHGVEB

gtcrust-1819

Research Article

ПАЛЕОГЕОДИНАМИКА

PALEOGEODYNAMICS

МИНЕРАЛОГИЯ И ВОЗРАСТ КАРБОНАТИТОВ МАССИВА СРЕДНЯЯ ЗИМА (ВОСТОЧНЫЙ САЯН)

MINERALOGY AND ZIRCON AGE OF CARBONATITES OF THE SREDNYAYA ZIMA COMPLEX (EASTERN SAYAN)

Прокопьев

И. Р.

Prokopyev

I. R.

630090, Новосибирск, пр-т Академика Коптюга, 3

630090, Новосибирск, ул. Пирогова, 1

3 Academician Koptyug Ave, Novosibirsk 630090

1 Pirogov St, Novosibirsk 630090

prokop@igm.nsc.ru

Дорошкевич

А. Г.

Doroshkevich

A. G.

630090, Новосибирск, пр-т Академика Коптюга, 3

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

3 Academician Koptyug Ave, Novosibirsk 630090

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

Варченко

М. Д.

Varchenko

M. D.

630090, Новосибирск, пр-т Академика Коптюга, 3

630090, Новосибирск, ул. Пирогова, 1

3 Academician Koptyug Ave, Novosibirsk 630090

1 Pirogov St, Novosibirsk 630090

Семенова

Д. В.

Semenova

D. V.

630090, Новосибирск, пр-т Академика Коптюга, 3

3 Academician Koptyug Ave, Novosibirsk 630090

Избродин

И. А.

Izbrodin

I. A.

630090, Новосибирск, пр-т Академика Коптюга, 3

3 Academician Koptyug Ave, Novosibirsk 630090

Крук

М. Н.

Kruk

M. N.

630090, Новосибирск, пр-т Академика Коптюга, 3

3 Academician Koptyug Ave, Novosibirsk 630090

Институт геологии и минералогии им. В.С. Соболева СО РАН ; Новосибирский государственный университетРоссияSobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences ; Novosibirsk State UniversityRussian Federation

Институт геологии и минералогии им. В.С. Соболева СО РАН ; Геологический институт им. Н.Л. Добрецова СО РАНРоссияSobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences ;Dobretsov Geological Institute, Siberian Branch of the Russian Academy of SciencesRussian Federation

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

2024

19042024

152749749

2024

Прокопьев И.Р., Дорошкевич А.Г., Варченко М.Д., Семенова Д.В., Избродин И.А., Крук М.Н.

Prokopyev I.R., Doroshkevich A.G., Varchenko M.D., Semenova D.V., Izbrodin I.A., Kruk M.N.

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/1819

Щелочно-ультраосновной карбонатитовый массив Средняя Зима расположен в Восточном Саяне и входит в ареал проявления неопротерозойского редкометалльного щелочного карбонатитового магматизма вдоль южной и юго-восточной окраины Сибирского кратона. Минералогические исследования кальцитовых карбонатитов массива Средняя Зима показали присутствие первичных магматических минералов, таких как кальцит, биотит (аннит-флогопит), ильменит и фторапатит. Из акцессорных минералов диагностированы пирохлор, циркон, бурбанкит, магнетит, рутил, титанит, стронцианит и барит. Химический состав магматических минералов карбонатитов Средней Зимы схож с таковым близковозрастных карбонатитовых массивов Белая Зима и Арбарастах. Редкоэлементный и структурный анализ циркона карбонатитов продемонстрировал наличие двух зон – магматической и участков перекристаллизации. U-Pb датирование магматического циркона показало возрастной интервал его кристаллизации – 637±4 млн лет, что совпадает со временем формирования щелочных карбонатитовых редкометалльных массивов, расположенных вдоль южной окраины Сибирского кратона. Их образование связано с завершающей стадией распада суперконтинента Родиния.

The Srednyaya Zima alkaline-ultramafic carbonatite complex is located in the Eastern Sayan and is a part of the area of manifestation of Neoproterozoic rare-metal alkaline-carbonatite magmatism along the southern and southeastern margins of the Siberian craton. Mineralogical studies of calciocarbonatites of the Srednyaya Zima complex have shown the presence of primary magmatic mineral phases of calcite, biotite (annite-phlogopite), ilmenite, and fluorapatite. Pyrochlore, zircon, burbankite, magnetite, rutile, titanite, strontianite, and barite were identified of the accessory minerals. The chemical composition of the magmatic minerals of the Srednyaya Zima carbonatites is similar to the mineral composition of the closely aged carbonatite complexes Belaya Zima and Arbarastakh. The rare-element and structural analysis of zircon from carbonatites showed the presence of two zones – a magmatic core and areas of recrystallization. U-Pb dating of igneous zircon showed the age interval of its crystallization – 637±4 Ma, which coincides with the geochronology of the formation of alkali-ultramafic rare-metal complexes along the southern margin of the Siberian craton. The formation of Neoproterozoic alkaline-carbonatite complexes is associated with tectonic events of the breakup of the Rodinia supercontinent.

карбонатитынефелиновые сиенитынеопротерозойРодинияцирконU-PbLA ICP-MS

carbonatitesnepheline syenitesNeoproterozoicRodiniazirconU-PbLA ICP-MS

Минералогические и геохронологические исследования выполнены за счет средств гранта РНФ № 23-17-00098. Геология района изучена в рамках государственного задания по базовым проектам НИР ИГМ СО РАН (122041400241-5) и ГИН СО РАН (AAAA-A21-121011390002-2).

Mineralogical and geochronological researches were carried out by the grant of the RSF (№ 23-17-00098). The geology of the region was studied as a part of the state assignment within the basic research projects of IGM SB RAS (122041400241-5) and GIN SB RAS (AAAA-A21-121011390002-2).

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