2007Stratigraphy and Geological CorrelationRequires access

Early Precambrian crystalline complexes of the Central Asian microcontinent: Age, sources, tectonic position

И. К. Козаков, Е. Б. Сальникова, T. Wang, А. Н. Диденко, Yu. V. Plotkina, V. N. Podkovyrov

Open publisher page 95 citations

Abstract

In the Early Caledonian superterrane of Central Asia, an accretionary orogen of mosaic structure, pre-Riphean Baidaragin and Bumbuger complexes are exposed in the Baidarik block of the Dzabkhan microcontinent. Zircon dating on ion-ion SHRIMP II microprobe and Nd isotopic-geochemical systematics are used to establish protolith age for Neoarchean orthogneisses of the Baidaragin complex, age constraints for accumulation of Lower Proterozoic metasediments of the Bumbuger Complex and provenance of sedimentary material. The results of isotopic dating facilitate correlation of the Baidarik block crystalline complexes with basement formations of North Eurasian ancient cratons. Possible position and migration path of the Dzabkhan microcontinent during the Early Proterozoic transformation of supercontinents Columbia-Rodinia-Pangea are considered based on interpretation of paleomagnetic data.

About this research paper

What this paper is about

In the Early Caledonian superterrane of Central Asia, an accretionary orogen of mosaic structure, pre-Riphean Baidaragin and Bumbuger complexes are exposed in the Baidarik block of the Dzabkhan microcontinent. Zircon dating on ion-ion SHRIMP II microprobe and Nd isotopic-geochemical systematics are used to establish protolith age for Neoarchean orthogneisses of the Baidaragin complex, age constraints for accumulation of Lower Proterozoic metasediments of the Bumbuger Complex and provenance of sedimentary material. The results of isotopic dating facilitate correlation of the Baidarik block crystalline complexes with basement formations of North Eurasian ancient cratons. Possible position and migration path of the Dzabkhan microcontinent during the Early Proterozoic transformation of supercontinents Columbia-Rodinia-Pangea are considered based on interpretation of paleomagnetic data.

Why it matters

OpenAlex reports 95 citations for this work. Citation counts describe recorded attention and do not establish research quality.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

In the Early Caledonian superterrane of Central Asia, an accretionary orogen of mosaic structure, pre-Riphean Baidaragin and Bumbuger complexes are exposed in the Baidarik block of the Dzabkhan microcontinent. Zircon dating on ion-ion SHRIMP II microprobe and Nd isotopic-geochemical systematics are used to establish protolith age for Neoarchean orthogneisses of the Baidaragin complex, age constraints for accumulation of Lower Proterozoic metasediments of the Bumbuger Complex and provenance of sedimentary material. The results of isotopic dating facilitate correlation of the Baidarik block crystalline complexes with basement formations of North Eurasian ancient cratons. Possible position and migration path of the Dzabkhan microcontinent during the Early Proterozoic transformation of supercontinents Columbia-Rodinia-Pangea are considered based on interpretation of paleomagnetic data.

Key concepts: Rodinia, Geology, Proterozoic, Precambrian, Riphean, Protolith, Zircon, Provenance

Related papers

Back to paper searchBrowse research topicsOriginal source
Early Precambrian crystalline complexes of the Central Asian microcontinent: Age, sources, tectonic position — Research Paper | ScholarLens