resarПриродные ресурсы Арктики и СубарктикиArctic and Subarctic Natural Resources2618-97122686-9683Академия наук Республики Саха (Якутия)10.31242/2618-9712-2020-25-4-1resar-199Research ArticleНауки о Земле. Общая и региональная геология, петрология и вулканологияEarth sciences. General and regional geology, petrology and volcanologyОсновные черты стратиграфии касимовско-гжельских и пермских отложений Сибирской платформы и ее складчатого обрамленияThe main features of the Kasimovian – Gzhelian and Permian stratigraphy in the Siberian platform and adjacent fold beltshttps://orcid.org/0000-0003-4115-5976КутыгинР. В.KutyginR. V.

КУТЫГИН Руслан Владимирович, кандидат геолого-минералогических наук, заведующий лабораторией

677000, Якутск, пр. Ленина, 39

WOS ResearcherID J-3318-2018, Scopus AuthorID 9277169500

KUTYGIN Ruslan Vladimirovich, candidate of geological  and mineralogical sciences, head of laboratory

39 Lenina pr., Yakutsk 677000

WOS ResearcherID J-3318-2018, Scopus AuthorID  9277169500

rkutygin@mail.ruБудниковИ. В.BudnikovI. V.

 БУДНИКОВ Игорь Васильевич, кандидат геолого-минералогических наук, директор департамента стратиграфии и региональной геологии

630091, Новосибирск, Красный проспект, 67

BUDNIKOV Igor Vasilyevich, candidate of geological and  mineralogical sciences, director of the Department of  Stratigraphy and Regional Geology

Krasniy pr. 67, Novosibirsk 630091

budnikov@sniiggims.ruСивчиковВ. Е.SivtchikovV. E.

СИВЧИКОВ Виктор Игоревич , до 2015 г. научный сотрудник

until 2015 was a Researcher

Krasniy pr. 67, Novosibirsk 630091

Институт геологии алмаза и благородных металлов СО РАНРоссияDiamond and Precious Metal Geology Institute, SB RASRussian FederationСибирский научно-исследовательский институт геологии, геофизики и минерального сырьяРоссияSiberian Research Institute of Geology, Geophysics and Mineral ResourcesRussian FederationСибирского научно-исследовательского института геологии, геофизики и минерального сырьяРоссияSiberian Research Institute of Geology, Geophysics and Mineral ResourcesRussian Federation202023092023254529Copyright © Кутыгин Р.В., Будников И.В., Сивчиков В.Е., 20232023Кутыгин Р.В., Будников И.В., Сивчиков В.Е.Kutygin R.V., Budnikov I.V., Sivtchikov V.E.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://resar.elpub.ru/jour/article/view/199

Рассмотрены основные проблемы стратиграфии касимовско-гжельских (верхнепенсильванских) и пермских отложений на территории Средней Сибири, в пределах которой выделяются пять структурно-фациальных областей: Тунгусская, Лено-Енисейская, Вилюйская, Таймырская и Верхоянская. Перечисленные области разделены на структурно-фациальные зоны или районы, характеризующиеся неповторимой последовательностью местных стратонов (свит, подсвит, толщ). Для корреляции верхнепенсильванских–пермских отложений внутри каждого из трех регионов (Сибирская платформа, Таймыр и Верхоянье) используются самостоятельные региональные стратиграфические шкалы, основанные на вертикальной последовательности палеонтологических комплексов и этапности осадконакопления. Верхнепенсильванско-пермские отложения Сибиркой платформы рассматриваются в составе семи последовательных региональных горизонтов (снизу вверх): катский (верхняя часть), клинтайгинский, бургуклинский, пеляткинский, дегалинский, гагарьеостровский и ивакинский. На Таймыре этому интервалу соответствуют турузовский, быррангский, соколинский, байкурский, ледянский и ивакинский, а в Верхоянье – кыгылтасский, хорокытский, эчийский, тумаринский, деленжинский, дулгалахский, хальпирский и некучанский (основание) региональные горизонты. Проведено сопоставление региональных стратиграфических шкал Сибирской платформы, Таймыра и Верхоянья с Международной хроностратиграфической шкалой. Для всех изученных структурно-фациальных областей приведены схемы корреляции, которые могут использоваться в качестве каркаса для новых (современных) региональных стратиграфических схем верхнего палеозоя Сибирской платформы и ее складчатого обрамления.

The main problems of the Kasimovian-Gzhelian (Upper Pennsylvanian) and Permian stratigraphy at the territory of Central Siberia are considered. Five structural-facies areas were identified: Tunguska, Lena-Yenisei, Vilyuy, Taimyr and Verkhoyanian (Verkhoyansk Region). Each of these areas is subdivided into structural-facies zones or districts characterized by a unique sequence of local strata (formations, subformations, units). To correlate the Upper Pennsylvanian – Permian deposits within each of the three regions – Siberian Platform, Taimyr, and Verkhoyanie, - independent regional stratigraphic scales are used, with their subdivisions based on the vertical sequence of paleontological complexes and stages of sedimentation. The Upper Pennsylvanian – Permian sediments of the Siberian Platform are considered as part of seven successive regional horizons (from bottom to top): Katian (the upper part), Klintaygian, Burguklian, Peliatkian, Degalian, Gagarieostrovian, and Ivakinian. In Taimyr, this interval corresponds to the Turuzavian, Byrrangian, Sokolinian, Bajkurian, Ledianian, Ivakinian regional horizons, and in Verkhoyanie – to the Kygyltassian, Khorokytian, Echian, Tumarian, Delenzhian, Dulgalakhian, Khalpirkian and Nekuchanian (the base part) regional horizons. The regional stratigraphic scales of the Siberian Platform, Taimyr, and Verkhoyanie are compared with the International Chronostratigraphic Scale. For all studied structural-facies areas, correlation schemes are presented that can be used as a framework for new (modern) Upper Paleozoic regional stratigraphic schemes of the Siberian Platform and its folded framing.

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