This article examines the geological structure and metallogenic features of the Almalyk ore region, as well as the origin and interrelationships of lead-zinc and copper-porphyry deposits. Lead-zinc deposits were formed mainly as a result of contact-metasomatic and hydrothermal processes, while copper-porphyry deposits have a direct genetic connection with intrusive bodies. Geochemical data confirm that the deposits of the Almalyk ore region have a polygenetic nature and the main role in their formation is played by magmatic-hydrothermal systems.
| Mualliflar | Mustafaev, Bakhtishod Nuraliugli, Turapov, Mirali Kamalovich, Мустафаев, Бахтишод Нуралиугли, Турапов, Мирали Камалович, Mustafayev, Baxtishod Nuralio‘g‘li, Turapov, Mirali Kamalovich |
|---|---|
| Jurnal | Саноатда рақамли технологиялар |
| Nashr sanasi | 2026-01-17 |
| Jild | 4 |
| Son | 1 |
| Betlar | 25-30 |
| Til | O‘zbek |
| DOI | 10.70769/3030-3214.srt.4.1.2025.3 |
DOI: 10.70769/3030-3214.srt.4.1.2025.3 · Maqolaning asl sahifasi
Almalyk, lead-zinc deposits, copper porphyry, metallogeny, hydrothermal processes, magmatism, Алмалык, свинцово-цинковые месторождения, медный порфир, металлогения, гидротермальные процессы, магматизм, Olmaliq, qo‘rg‘oshin-rux konlari, mis porfiri, metallogeniya, gidrotermal jarayonlar, magmatizm
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