Саноатда рақамли технологиялар 3-том 4-нөмір (2025) · 173-177-беттер
ORE-MAGMATIC SYSTEMS OF THE YAKHTAN ORE FIELD OF THE CHAKYLKALYAN-KARATEPA MOUNTAINS
Ochilov, Ilyos Saidovich, Akhmedov, Shovdullo Shukhratovich, Arabov, Sobid Zakirugli, Bobokulova, Zebo Bahodirkizi, Очилов, Ильес Саидович, Ахмедов, Шовдулло Шухратович, Арапов, Собид Закиругли, Бобокулова, Зебо Баходир кизи, Ochilov, Iles Saidovich, Axmedov, Shovdullo Shuxratovich, Arapov, Sobid Zokiro‘g‘li, Boboqulova, Zebo Bahodirqizi
Аңдатпа
The article analyzes the geological and petrochemical features of the Yakhton magmatic-metallogenic structure. It has been shown that the main magmatic components - granitoids, lamprophyres, and alkaline basaltoids - formed in connection with a single magma-forming focus. The rocks of the Yakhton complex specialize in tungsten and gold, forming typomorphic associations with minerals such as scheelite, pyrite, arsenopyrite. Gold-tungsten skarn and apogranitoid mineralization are developed simultaneously in the region. The “intrusive” and “telethermal” subtypes of the apocarbonate gold mineralization have also been identified. It reveals the metallogenic significance of the Yakhtan massif and its place in the mineralization of Southern Uzbekistan.
Yakhton magmatic-metallogenic structuregranitoidslamprophyresalkaline basaltoidsmagma generationgranodioritescheelitepyritearsenopyritetungsten mineralization
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