Abstract

The work describes the genetic types and conditions for the localization of mineralization - individual deposits and ore occurrences. Also, the indicated mineralized zones, the conditions of occurrence of the mineralization, the geological-structural position and the peculiarities of the host complexes. Descriptions of promising tungsten, tin ore, polymetallic, mercury and other ore zones, which serve as a reserve in expanding the resource base in the Republic, are given. Tungsten, tin ore, and mercury mineralizations are characterized in somewhat more detail, since the latter in the region under study is often spatially associated with gold and forms mercury-antimony-polymetallic mineralization.

Highlights

  • At present, Western Uzbekistan is considered one of the most promising for gold, silver, tungsten, tin, mercury, antimony, lead-zinc, uranium and other minerals in the Central Asian ore province

  • The object of the study is the territory of the part of the Southern Tien Shan, which is located in Western Uzbekistan with deposits and ore occurrences of gold and rare-metal mineralization (Fig. 1)

  • We will dwell in more detail on the characteristics of the manifestations of tungsten mineralization, since the latter in the region under study is often spatially associated with gold ore and especially for forecasting with mercury and mercuryantimony-polymetallic mineralization

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Summary

Introduction

Western Uzbekistan is considered one of the most promising for gold, silver, tungsten, tin, mercury, antimony, lead-zinc, uranium and other minerals in the Central Asian ore province. The USA Journals Volume 02 Issue 12-2020 scientific institutions (Institute of Geology and Geophysics of the Academy of Sciences of Uzbekistan, Institute of Mineral Resources, etc.), numerous deposits and ore occurrences have been explored: pegmatite-rare-metal (Ketmenchi, Zirabulak, Kutchi ); pegmatitequartz-feldspar (Mulla-Burkhan, Kyz-Kurgan, etc.); greisen-rare metal (Sulu-Kyz, Tadyknaya, Kurai, Kara-mosque, Berkut); skarn-rare metal (Ingichka, Lyangar, Koitash, Yakhton, Karatyube, Sarutau, Sautbay, Daray-tut, Uchmulla, Maizak, Yarmakchi, Guljan, Tym, Mulla-Burkhan, Buzgulgryada, Chuyun); skarntin-polymetallic (Kyz-Kurgan); skarn-leadantimony (Kaltasai); hydrothermal-gold-oremetasomatic (Muruntau, Kokpatas, Tillatag, Dilan, Korakutan, Granitnaya, Yangi Davon, Pistal, Azhibugut, etc.); hydrothermal tin ore (Kochkarly, Lapas, Karnab, Kermene, Changalli, Devonasai, Kalta, Temirkan, Dzhilansay, Gaulinskoe, Karakuduk, Sukaiti, Chaidaroz, Tutak, Altyn-Kazgan); hydrothermal-copper metal (Miskan, Atkamarsay); hydrothermal-mercury

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