Provenance and Age of Volcanogenic–Terrigenous Rocks of the Bastakh Series (Ilin–Tass Anticlinorium, Northeast Russia)

The rocks of the Ilin–Tass anticlinorium overlie the folded structures of the Moma Range and extend from the headwaters of the Kolyma River in the northwesterly direction to the Indigirka River basin. The first data on U–Pb dating of detrital zircons from volcanogenic–terrigenous rocks of the Bastakh series are presented. It is found that the provenance area for the rocks of the Bastakh series was located along the entire periphery from the area of accumulation of volcanogenic–sedimentary formations. It is shown that the age of the three formations of the Bastakh series lower in the section, which was previously considered to be the Tithonian, covers the Neocomian and is accepted as the Tithonian–Barremian.

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Publication Details

Journal
Doklady Earth Sciences
Published
2025-01-01
DOI
https://doi.org/10.1134/s1028334x24604875
Primary Topic
Geological and Geochemical Analysis
Type
article
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article

Provenance and Age of Volcanogenic–Terrigenous Rocks of the Bastakh Series (Ilin–Tass Anticlinorium, Northeast Russia)

V. N. Danilov, E. A. Brusnitsyna, S. N. Sychev, В. Б. Хубанов et al.
Doklady Earth Sciences
Geological and Geochemical Analysis
article

Provenance and Age of Volcanogenic–Terrigenous Rocks of the Bastakh Series (Ilin–Tass Anticlinorium, Northeast Russia)

V. N. Danilov, E. A. Brusnitsyna, S. N. Sychev, В. Б. Хубанов, С. Д. Соколов, O. Yu. Lebedeva, A. V. Rogov
article en

Abstract

The rocks of the Ilin–Tass anticlinorium overlie the folded structures of the Moma Range and extend from the headwaters of the Kolyma River in the northwesterly direction to the Indigirka River basin. The first data on U–Pb dating of detrital zircons from volcanogenic–terrigenous rocks of the Bastakh series are presented. It is found that the provenance area for the rocks of the Bastakh series was located along the entire periphery from the area of accumulation of volcanogenic–sedimentary formations. It is shown that the age of the three formations of the Bastakh series lower in the section, which was previously considered to be the Tithonian, covers the Neocomian and is accepted as the Tithonian–Barremian.

Doklady Earth SciencesVol. 520(1)
St Petersburg University (RU), Geological Institute (RU), A.P. Karpinsky Russian Geological Research Institute (RU), Schmidt Institute of Physics of the Earth (RU), Yakut Scientific Research Institute of Agriculture (RU)
Openalex Percentile: Top 90%
Geological and Geochemical Analysis
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