A model of the tectonic development of Irtysh shear zone in terms of present day radioisotope data

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Authors:


Y.V.Ponomareva, orcid.org/0000-0003-1322-6773, Karaganda Technical University, Karaganda, the Republic of Kazakhstan, e-mail: This email address is being protected from spambots. You need JavaScript enabled to view it.

M.V.Ponomareva, orcid.org/0000-0001-8652-9607, Karaganda Technical University, Karaganda, the Republic of Kazakhstan, e-mail: mv_ponomareva18 @ mail.ru

A.V.Sadchikov, orcid.org/0000-0002-6022-2073, Karaganda Technical University, Karaganda, the Republic of Kazakhstan, e-mail: a.sadchikov @ kstu.kz

N.V.Zhelayeva, orcid.org/0000-0003-3572-3578, Karaganda Technical University, Karaganda, the Republic of Kazakhstan, e-mail: This email address is being protected from spambots. You need JavaScript enabled to view it.


повний текст / full article



Naukovyi Visnyk Natsionalnoho Hirnychoho Universytetu. 2021, (4): 005 - 009

https://doi.org/10.33271/nvngu/2021-4/005



Abstract:



Purpose.
To present the model of tectonic development of the Irtysh shear zone, based on recent uranium-lead dating for zircon.


Methodology. The authors analyzed the results of studies of foreign and domestic scientists, conducted field research, sample preparation, carried out iso-tope studies using SHRIMP-2 and LA-ICP-MS technology; determined small elements by the fusion method using ICP.


Findings.
Based on more than ten uranium-lead dating for zircon using the local method and the given geological and structural data, model of the Irtysh shear zone tectonic development has been proposed


Originality.
A tectonic model has been developed and the age and structural relationships of the Irtysh shear zone with the Kalba-Narym zone based on uranium-lead zircon dating have been established.


Practical value
. The article considers the structural and age relationships of the Irtysh crush zone which prove its formation along the deep Irtysh fault in the course of a long multi-stage tectogenesis.



Keywords:
crystalline schists, ophiolite complex, tectonic evolution, green shale, dike, collision, uranium-lead datings

References.


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