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Metasomatic Rocks of Gold Deposits and Their Connection with Ore Process of Mountain Auminzatau (Central Kyzylkum)

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Abstract

The metasomatic rocks of gold-ore deposits of the Auminzatau Mountains (Central Kyzylkum), which are similar in mineral composition and their features of the formation, are distinguished. The corresponding stages of ore mineralization are associated with certain types of metasomatic rocks, which are their typomorphic signs. They reflect the features of the evolution of the stages of a unified mineral-forming system, which can be used as search criteria.

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Funding

This work was prepared within the framework of the projects carried out with JSC Navoi Mining and Metallurgical Company on a contract basis.

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Authors and Affiliations

  1. Institute of Geology and Geophysics named after H.M. Abdullayev State Committee of Geology of Uzbekistan, Tashkent, Uzbekistan

    R. M. Sadirov & A. B. Yusupov

  2. National University of Uzbekistan Mirzo Ulugbek, Tashkent, Uzbekistan

    Sh. V. Usmanova

  3. Moscow State University, 119991, Moscow, Russia

    A. V. Tevelev

  4. LLC NTPP Geopoisk, Chelyabinsk, Russia

    A. V. Tevelev

Authors
  1. R. M. Sadirov
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  2. A. B. Yusupov
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  3. Sh. V. Usmanova
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  4. A. V. Tevelev
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Corresponding authors

Correspondence to R. M. Sadirov, A. B. Yusupov, Sh. V. Usmanova or A. V. Tevelev.

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The authors of this work declare that they have no conflicts of interest.

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Translated by D. Voroshchuk

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Sadirov, R.M., Yusupov, A.B., Usmanova, S.V. et al. Metasomatic Rocks of Gold Deposits and Their Connection with Ore Process of Mountain Auminzatau (Central Kyzylkum). Moscow Univ. Geol. Bull. 78, 717–721 (2023). https://doi.org/10.3103/S0145875223060133

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  • DOI: https://doi.org/10.3103/S0145875223060133

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