Iron Ore Series of the Sarysu–Teniz Watershed (Central Kazakhstan): Age Substantiations and Formation Setting

This work presents the results of the study of the Late Precambrian volcanogenic-sedimentary iron ore Bozdak series of the Sarysu–Teniz watershed in the west of Central Kazakhstan. The first U–Th–Pb (SIMS) age estimates (718 ± 5 Ma) of accessory zircons from trachyrhyolites indicate that they have been formed at the very beginning of the Cryogenian period of the Neoproterozoic. Geochemical features of the effusive rocks show that the accumulation of ferruginous quartzites has been accompanied by contrasting basalt-trachyrhyolite volcanism in the rift setting.

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Publication Details

Journal
Doklady Earth Sciences
Published
2025-05-22
DOI
https://doi.org/10.1134/s1028334x25606431
Primary Topic
Geochemistry and Geologic Mapping
Type
article
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article

Iron Ore Series of the Sarysu–Teniz Watershed (Central Kazakhstan): Age Substantiations and Formation Setting

К. Е. Degtyarev, А. Н. Журавлев, Н. А. Каныгина, А. А. Тretyakov
Doklady Earth Sciences
Geochemistry and Geologic Mapping
article

Iron Ore Series of the Sarysu–Teniz Watershed (Central Kazakhstan): Age Substantiations and Formation Setting

К. Е. Degtyarev, А. Н. Журавлев, Н. А. Каныгина, А. А. Тretyakov
article en

Abstract

This work presents the results of the study of the Late Precambrian volcanogenic-sedimentary iron ore Bozdak series of the Sarysu–Teniz watershed in the west of Central Kazakhstan. The first U–Th–Pb (SIMS) age estimates (718 ± 5 Ma) of accessory zircons from trachyrhyolites indicate that they have been formed at the very beginning of the Cryogenian period of the Neoproterozoic. Geochemical features of the effusive rocks show that the accumulation of ferruginous quartzites has been accompanied by contrasting basalt-trachyrhyolite volcanism in the rift setting.

Doklady Earth SciencesVol. 522(2)
Geological Institute (RU)
Climate action
Openalex Percentile: Top 95%
Geochemistry and Geologic Mapping
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