Neoproterozoic volcanosedimentary and plutonic complexes of Northern Ulutau (Central Kazakhstan)

The article presents the results of studying and substantiating the age of Late Precambrian volcanogenic sedimentary and plutonic complexes of the northern part of the Ulutau terrane (Northern Ulutau) in the west of Central Kazakhstan. The age estimates obtained (SHRIMP II, ID-TIMS, LA-ICP-MS) indicate the formation of acidic effusions and granitoids in the second half of the Tonian Neoproterozoic period ~835‒747 million years ago. Geochronological and isotope-geochemical data allow us to consider these formations as analogues of stratified and plutonic complexes of Southern Ulutau, formed in various parts of the lateral series of structures of the late precambrian active continental margin.

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Publication Details

Journal
Геотектоника
Published
2024-11-03
DOI
https://doi.org/10.31857/s0016853x24030013
Citations
1
Primary Topic
Geological and Geochemical Analysis
Type
article
Field-Weighted Citation Impact
0.53
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article

Neoproterozoic volcanosedimentary and plutonic complexes of Northern Ulutau (Central Kazakhstan)

К. Е. Degtyarev, А. Н. Журавлев, S. Yu. Skuzovatov, B. V. Fedorov et al.
1 citations
Геотектоника
Geological and Geochemical Analysis
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article

Neoproterozoic volcanosedimentary and plutonic complexes of Northern Ulutau (Central Kazakhstan)

К. Е. Degtyarev, А. Н. Журавлев, S. Yu. Skuzovatov, B. V. Fedorov, Yu. V. Plotkina, Н. А. Каныгина, А. А. Тretyakov, A. B. Kotov, Е. Б. Сальникова
article en
1 citations

Abstract

The article presents the results of studying and substantiating the age of Late Precambrian volcanogenic sedimentary and plutonic complexes of the northern part of the Ulutau terrane (Northern Ulutau) in the west of Central Kazakhstan. The age estimates obtained (SHRIMP II, ID-TIMS, LA-ICP-MS) indicate the formation of acidic effusions and granitoids in the second half of the Tonian Neoproterozoic period ~835‒747 million years ago. Geochronological and isotope-geochemical data allow us to consider these formations as analogues of stratified and plutonic complexes of Southern Ulutau, formed in various parts of the lateral series of structures of the late precambrian active continental margin.

Геотектоника(3)
Russian State Geological Prospecting University (RU), Vinogradov Institute of Geochemistry (RU), Geological Institute (RU), Institute of Precambrian Geology and Geochronology (RU)
Life below water
Openalex Percentile: Top 33%
Geological and Geochemical Analysis
0.53
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