| Issue |
E3S Web Conf.
Volume 497, 2024
5th International Conference on Energetics, Civil and Agricultural Engineering (ICECAE 2024)
|
|
|---|---|---|
| Article Number | 03048 | |
| Number of page(s) | 10 | |
| Section | Agricultural Engineering | |
| DOI | https://doi.org/10.1051/e3sconf/202449703048 | |
| Published online | 07 March 2024 | |
Localization conditions of apometaterrigenous non-carbon the Sarykul deposit of the Karatyubinsky ore district in Uzbekistan
1 Tashkent State Technical University, Tashkent, 100095, Uzbekistan .
2 National University of Uzbekistan, Tashkent, 100174, Uzbekistan .
3 Tashkent Institute of Chemical Technology, Tashkent, 100011, Uzbekistan .
* Corresponding author: aydos_770@mail.ru
This article explores the occurrence of apometaterrigenous non-carbon tungsten mineralization at the Sarykul deposit in the Karatyubinsk Mountains. Initially considered unpromising, this newly discovered tungsten mineralization was found during gold mining operations. The prospecting activities targeting calcification zones in metaterrigenous rocks revealed their tungsten-bearing nature. This discovery has reshaped the understanding of tungsten mineralization genesis, lithological and structural conditions, and the overall minerogenic potential of the Karatyubinsky ore field.Apometaterrigenous tungsten mineralization originates from coarse flysch rocks transformed into shale rocks in the contact zone with a tungsten-specialized granitoid intrusive. The mineralization is associated with multicomponent metasomatites formed on aluminosilicate metaterrigenous rocks. Significant correlations exist between tungsten and elements such as Pb, Ag, Au, Be, Cu, Mo, V, and Mn. Scheelite mineralization forms autonomously, followed by the combination of different stages within mineralized zones. The regional trog structure, characterized by the formation of an olistostromic stratum due to high granulometric dispersion, is also linked to the apometaterrigenous mineralization.
© The Authors, published by EDP Sciences, 2024
This is an Open Access article distributed under the terms of the Creative Commons Attribution License 4.0, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
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