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Tectonic peculiarities of the Zhailma structure formation

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Category: Content №3 2022

Last Updated on 29 June 2022

Published on 30 November -0001

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Authors:

A.T.Roman, orcid.org/0000-0003-3489-9475, 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.

V.S.Portnov, orcid.org/0000-0002-4940-3156, 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.

N.S.Askarova, orcid.org/0000-0002-2103-6198, 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. 2022, (3): 011 - 016

https://doi.org/10.33271/nvngu/2022-3/011

Abstract:

Purpose. Studying the genesis and position of the Zhailma trough in the tectonic structures of Central Kazakhstan.

Methodology. Critical analysis of literature and stock materials, comparative analysis of geological, geophysical and morphological factors characteristic of continental rifts, features of the formation of volcanic graben synclines, analysis of the results of isotope dating of rocks.

Findings. The Zhailma graben-syncline is not an independent structure of the rift origin. The formation of Zhailma is associated with the general evolution of the Sarysu-Teniz segment of the Devonian volcano-plutonic belt. The formation of the Zhailma graben syncline is associated with subsidence after ejections of significant masses of felsic magmatic material.

Originality. The authors carried out a comparative analysis of the geological, geophysical and morphological data of the Zhailma structure with similar data characteristic of modern continental rifts. As a result of the analysis, it was established that the rift genesis of Zhailma remains controversial. This structure developed simultaneously with the Devonian volcanic-plutonic belt, and is genetically related to the processes of volcanism. The authors suggest that Zhailma is a volcanic graben-syncline.

Practical value. Over a long period of studying the structure, an opinion was formed about the futility of the Sarysu-Teniz segment of the Devonian volcano-plutonic belt for the identification of industrial deposits. An exception was the Zhailma trough, which is a unique Famennian-Carboniferous sedimentary structure in terms of ore saturation, containing significant reserves of iron-manganese, barite-polymetallic and barite proper ores. In this connection, the authors consider it practically important to study the existing graben-synclines in the area of the Devonian volcano-plutonic belt in order to identify industrial deposits of the Atasu type.

Keywords: Volcanic graben syncline, isotopic analysis, Devonian volcano-plutonic belt, Atasu ore region, continental rifts

References.

1. Shabalina, L.V. (2003). Model of the deep structure of the Central Kazakhstan paleorift system. Proceedings of the National Academy of Sciences of the Republic of Kazakhstan. Geology Series, (4), 16-23. Retrieved from https://kk.convdocs.org/docs/index-70374.html?page=2.

2. Shenger, A.M. (2009). Jelal. Rifts of the world. Moscow: Geokart.

3. Logachev, N.A. (2001). Main structural features and geo-dynamics of the Baikal rift zone. Physical mesomechanics, 2(1-2), 163-170.

4. Dolginov, E.A., & Bashkin, Yu.V. (2013). Patterns of continental rifting. Bulletin of the Moscow Society of Naturalists. Geological department, 88(4), 55-63.

5. Askarova, N.S., Roman, A.T., Kopobayeva, A.N., & Portnov, V.S. (2021). Feature space of the Atasu type deposits (Central Kazakhstan). Naukovyi Visnyk Natsionalnoho Hirnychoho Universytetu, (5), 5-10. https://doi.org/10.33271/nvngu/2021-5/005.

6. Lapteva, E.M., & Lapteva, N.I. (2008). Graphical representation of the geodynamics of rift structures based on remote data. Modern problems of remote sensing of the Earth from space, 356-362. Retrieved from http://d33.infospace.ru/d33_conf/2008_pdf/1/48.pdf.

7. Lyubetsky, V.N., Lyubetskaya, L.D., & Shabalina, L.V. (2009). Deep structure and stages of formation of commercial stratiform polymetallic ores in the Atasu and Rudno-Altai ore districts. Bulletin of the National Academy of Sciences of the Republic of Kazakhstan. Geological series, (5), 24-36. Retrieved from http://nblib.library.kz/elib/library.kz/journal/Lyubeckii023.pd.

8. Erlikh, E.N. (1966). Volcano-tectonic depressions, Geotectonics, (6), 48-63.

9. Erlikh, E.N. (1973). Modern structure and Quaternary volcanism of the western part of the Pacific Rim. Novosibirsk: Nauka.

10. Gorshkov, G.S. (1967). Volcanism of the Kuril Island Arc: monograph. Moscow.

11. Mazurov, A.K. (2002). Features of metallogeny and assessment of ore content of metallogenic complexes of rifts of Kazakhstan. Rifts of the lithosphere: Proceedings of the international scientific Conference, 244-248. Retrieved from www.elibrary.ru/item.asp?id=25329023.

12. Antonyuk, R.M., Ismailov, Kh.K., Klochkov, M.V., Kochergina,A.V., & Kuznetsov, K.V. (2012). Regularities of localization of deposits of the Atasu type in the rift structures of Central Kazakhstan of the Late DevonianEarly Carboniferous age. Geology and protection of mineral resources, 2(43), 11-21.

13. Kurchavov, A.M., Grankin, E.G., Malchenko, E.G., & Zhukovskii,V.I. (2000). Zoning, segmentation, and paleogeodynamics of the Devonian volcanic belt in Central Kazakhstan. Geotectonics, (4), 32-43.

14. Mazurov, A.K. (2002). Metallogeny of oceanic and continental paleorifts of Kazakhstan. Bulletin of the Tomsk Polytechnic University. Geology, prospecting and exploration of minerals, 305(6), 76-89.

15. Erlich, E. (2020). Geodynamics and magmatism of platforms. Litres. Retrieved from https://www.geokniga.org/bookfiles/geokniga-geodinamika-i-magmatizm-platform.pdf.

16. Seitmuratova, E.Yu., Borukaeva, M.R., & Lyapichev, G.F. (2000). Late Paleozoic volcanism of the active margin of the Kazakh paleocontinent. Geodynamics and minerageny of Kazakhstan, 104-118.

17. Seitmuratova, E.Yu., Arshamov, Ya.K., Baratov, R.T., & Dautbekov, D.O. (2017). Geological and metallogenic features of the volcano-plutonic belts of Kazakhstan. Proceedings of the National Academy of Sciences of the Republic of Kazakhstan, 3(416), 60-86.

18. Zhukovskiy, V.I., Malchenko, E.G., & Khamzin, B.S. (2008). Polymetallic and ferromanganese deposits of Central Kazakhstan (Atasu type). Ore provinces of Central Asia, (pp. 149-160). Almaty.

19. Kurchavov, A.M., & Khamzin, B.S. (2017). The main boundaries of ore formation in the orogenic structures of the Caledonides of Northern and Central Kazakhstan. Izvestiya NAS RK. Series geology and technical sciences, (3), 24-34. ISSN 2224-5278.

20. Kurchavov, A.M. (2004). Zoning of orogenic volcanism and problems of its geodynamic interpretation. Lithosphere, (3), 71-83.

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