Systematic analysis of certain deposits and ore occurrences in the Middle and South Tien Shan, in the result determine plenty of difference mineralogical regions and reporting units, concentration level of ore fields, reporting and formation conditions, production genetic, geological-industrial and so on. The types of number geological structures show that there are a mutual difference between the areas. In the process of analysis, it was found that the gross (total) ore content of the South Tien Shan much more than miner genic province significantly exceeds the potential of the Middle Tien Shan.
| Mualliflar | Элшод ҚУТЛИЭВ, Фарҳод ЧЎЛЛИЕВ, Эркин ҲАҚҚУЛОВ, Эркин ҲАҚҚУЛОВ |
|---|---|
| Jurnal | Ўзбекистон Миллий университети хабарлари |
| Nashr sanasi | 2024-03-30 |
| Jild | 3 |
| Son | 3.1 |
| Betlar | 260-263 |
| Til | Rus |
| DOI | 10.69617/nuuz.v3i3.1.1787 |
DOI: 10.69617/nuuz.v3i3.1.1787 · Maqolaning asl sahifasi
Turkestan-Alai, trachybasalts, basaltic andesite, subduction, Cambrian-Early Devonian, structural-tectonic., : Туркестано-Алайской, трахибазальтов, андезибазальтов, субдукция, кембрий-раннедевон, структурно-тектонические., Turkiston-Oloy, traxibazaltlar, bazalt andezitlari, subduktsiya, kembriy-erta devon, struktur-tektonik.
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