This article briefly describes the hological structure of the Vaudil site located on the territory of the Fergana region, and the main emphasis is placed on the composition of the coal seams located on the site, what rocks are4 associated with them and how distributed they are.
| Mualliflar | Хамза КАНАТОВ, Азизбек ЮСУПОВ, Ойдин ШОДМОНОВ, Мехрож ЖЎРАЕВ, Абдулла АЛМАРДОНОВ |
|---|---|
| Jurnal | Ўзбекистон Миллий университети хабарлари |
| Nashr sanasi | 2024-03-30 |
| Jild | 3 |
| Son | 3.1 |
| Betlar | 246-250 |
| Til | Rus |
| DOI | 10.69617/nuuz.v3i3.1.1783 |
DOI: 10.69617/nuuz.v3i3.1.1783 · Maqolaning asl sahifasi
Geochemistry carbonate metamorphism terrigenous deposits limestone alleurolite slate marl dolomite structural floor pre-Mesozoic orumentum retinue suite of acglomerates sandstones tier, Геохимия карбонат метаморфизм терригенные отложения известняк аллевролит сланец мергел доломит структуный этаж домезазойский орундомент свита конгломератов, песчаников, ярус., : Geokimyo karbonat metamorfizm terrigen yotqiziqlar ohaktosh allevrolit slanes mergel dalamit strukturniy qavat mezazoydan oldingi vosita svita konglomerat qumtoshlar yarus.
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