nznistuНауки о Земле и недропользованиеEarth sciences and subsoil use2686-99932686-7931Federal State Budget Educational Institution of Higher Education "Irkutsk National Research Technical University"10.21285/2686-9993-2025-48-2-160-184OTFBNNnznistu-407Research ArticleГеофизикаGeophysicsПалеомагнитная корреляция траппов Тунгусской синеклизы Сибирской платформы с глобальным стратотипом пермо-триаса провинции Чжэцзян Южного КитаяPalaeomagnetic correlation of Tunguska syneclise traps of Siberian platform with Permian-Triassic global stratotype of Zhejiang Province, Southern Chinahttps://orcid.org/0000-0002-1196-8776КонстантиновК. М.KonstantinovK. M.

Константинов Константин Михайлович - доктор геолого-минералогических наук, руководитель департамента геофизики, институт «Сибирская школа геонаук».

Иркутск

Konstantin M. Konstantinov - Dr. Sci. (Geol. & Mineral.), Head of the Geophysics Department, Siberian School of Geosciences.

Irkutsk

konstantinovkm@ex.istu.eduhttps://orcid.org/0000-0001-5865-7521ТомшинМ. Д.TomshinM. D.

Томшин Михаил Дмитриевич - кандидат геолого-минералогических наук, старший научный сотрудник, заведующий лабораторией «Геологический музей».

Якутск

Mikhail D. Tomshin - Cand. Sci. (Geol. & Mineral.), Senior Researcher, Head of the Geological Museum Laboratory, Diamond and Precious Metal Geology Institute.

Yakutsk

tmd@diamond.ysn.ruhttps://orcid.org/0009-0009-5013-6241КонстантиновИ. К.KonstantinovI. K.

Константинов Иннокентий Константинович - инженер-исследователь, департамент рудной геологии, институт «Сибирская школа геонаук».

Иркутск

Innokenty K. Konstantinov - Research Engineer, Ore Geology Department, Siberian School of Geosciences.

Irkutsk

geologiaforever@mail.ruhttps://orcid.org/0009-0008-7764-8100ПоповА. Н.PopovA. N.

Попов Анатолий Николаевич - студент, институт «Сибирская школа геонаук».

Иркутск

Anatoly N. Popov - Student, Siberian School of Geosciences.

Irkutsk

anatoliy_popov_04@mail.ruhttps://orcid.org/0009-0002-6006-9416ПоздняковВ. Е.PozdniakovV. E.

Поздняков Вениамин Егорович - студент, Институт высоких технологий, лаборант-исследователь химико-аналитической лаборатории, институт «Сибирская школа геонаук».

Иркутск

Veniamin E. Pozdniakov - Student, Institute of High Technologies, Laboratory Research Assistant at the Chemical Analytical Laboratory, Siberian School of Geosciences.

Irkutsk

venya081004@gmail.comhttps://orcid.org/0009-0005-1961-5157ИШ.YiSh.

И Шэнь - студент, Школа географии.

Нанкин

Shen Yi - Student, School of Geography.

Nanjing

15962597891@163.comhttps://orcid.org/0009-0000-7524-2723ЧжоуЦ.ZhouZ.

Чжоу Цзытун - студент, Институт иностранных языков.

Нанкин

Zitong Zhou - Student, Institute of Foreign Languages.

Nanjing

2496383208@qq.comИркутский национальный исследовательский технический университетРоссияIrkutsk National Research Technical UniversityRussian FederationИнститут геологии алмаза и благородных металлов СО РАНРоссияDiamond and Precious Metal Geology Institute, Siberian Branch of the Russian Academy of SciencesRussian FederationНанкинский университетКитайNanjing UniversityChina202524072025482160184Copyright © Константинов К.М., Томшин М.Д., Константинов И.К., Попов А.Н., Поздняков В.Е., И Ш., Чжоу Ц., 20252025Константинов К.М., Томшин М.Д., Константинов И.К., Попов А.Н., Поздняков В.Е., И Ш., Чжоу Ц.Konstantinov K.M., Tomshin M.D., Konstantinov I.K., Popov A.N., Pozdniakov V.E., Yi S., Zhou Z.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.nznj.ru/jour/article/view/407

Целью проведения Международной китайско-российской геологической экспедиции в г. Нанкине и дельте реки Янцзы (Китай) в период с 26 октября по 9 ноября 2024 г., состоящей из студентов и преподавателей, являлось установление общих связей и закономерностей в геологическом строении и развитии Сибирской и Южно-Китайской платформ. Группа посетила ряд объектов, имеющих высокое научное значение для понимания формирования современного облика Восточной Азии, начиная с позднепермского-раннетриасового периода (около 250 млн лет). На основе палеомагнитных данных было выявлено, что на границе перми – триаса указанные литосферные блоки были удалены друг от друга на более чем 1500 км. В это время между ними существовал Монголо-Охотский океан, который закрылся в конце раннего мелового периода (около 125 млн лет). В то время на Сибирской платформе протекали активные тектоно-магматические процессы, связанные с формированием траппов Тунгусской синеклизы, а на Южно-Китайской платформе проходило спокойное осадконакопление терригенно-осадочных толщ в морских условиях. Именно эти геологические процессы стали основными объектами представленного в статье исследования. Методика состояла в сборе и анализе количественных данных, свидетельствующих о синхронности указанных событий во времени, которые найдут применение в решении широкого круга таких геологических задач, как межрегиональные корреляции стратиграфических разрезов, тектоно-магматических процессов, изучение катастрофических явлений и др. В качестве фактографической основы были использованы материалы по палеонтологическим, изотопным, палеомагнитным и другим исследованиям (собственные и опубликованные другими авторами). Благодаря проведенному исследованию было показано, что время внедрения базитов катангского вулканического комплекса Тунгусской синеклизы корреспондируется с пермо-триасовой границей разреза Мейшань D (округ Чансин, провинция Чжэцзян, Южный Китай).

The purpose of the International Chinese-Russian Geological Expedition of students and teachers in Nanjing and the Yangtze River Delta (China) from October 26 to November 9, 2024 was to establish common connections and patterns in the geological structure and development of the Siberian and South China platforms. The group visited a number of sites of high scientific importance in order to understand the formation patterns of the modern appearance of East Asia beginning from the Late Permian-Early Triassic period (about 250 million years ago). Based on palaeomagnetic data, it was revealed that at the Permian-Triassic boundary these lithospheric blocks were located more than 1,500 km apart separated by the Mongol-Okhotsk Ocean, which closed at the end of the Early Cretaceous period (about 125 million years ago). That was the time when Siberian platform featured active tectonic and magmatic processes related to the Tunguska syneclise trap formation while calm sedimentation of terrigenous-sedimentary strata in marine conditions took place on the South China platform. These geological processes have become the main objects of the research presented in the article. The methodology consisted of collecting and analyzing quantitative data indicating the synchronicity of specified events in time, which will find application in solving a wide range of geological problems including interregional correlations of stratigraphic sections, tectonic-magmatic processes, study of catastrophic phenomena, etc. Materials from paleontological, isotopic, paleomagnetic and other studies (authors’ and published by other researchers) were used as a factual basis. The conducted research has shown that the deposition time of the Katangsky volcanic complex basites of the Tunguska syneclise corresponds to the Permian-Triassic boundary of the Meishan section D (Changxing District, Zhejiang Province, South China).

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