Lower Cretaceous deposits are very widespread in the study area, and their sediments, due to their specific lithological-facial and paleontological features, are clearly and vividly distinguished in the section of the entire Mesozoic sedimentary complex. A comprehensive study of the material composition of Lower Cretaceous rocks, facies-paleogeographic conditions of accumulation of various lithological layers and the establishment of a close genetic relationship between facies types of rocks, as well as patterns of distribution of various minerals according to geological-paleogeographic patterns are important search criteria in geological exploration.
| Mualliflar | Джураев , Фазлиддин Очилхонович, Jurayev , Fazliddin Ochilxonovich, Juraev , Fazliddin Ochilkhanovich |
|---|---|
| Jurnal | Саноатда рақамли технологиялар |
| Nashr sanasi | 2025-07-08 |
| Jild | 3 |
| Son | 3 |
| Betlar | 129-135 |
| Til | O‘zbek |
| DOI | 10.70769/3030-3214.srt.3.3.2025.3 |
DOI: 10.70769/3030-3214.srt.3.3.2025.3 · Maqolaning asl sahifasi
Tashkurgan, Yakkasaray, Langar, Gilan, Kulkamysh, Maidanak, Shokhshor and Dukonkhona, sedimentary, terrigenous, hemogenic, stepped-terrace, paleozoic, archaic, alb and cenomanian, okuzbulak, almurod, karabil, Ташкурган, Яккасарай, Лангар, Гилан, Кулькамыш, Майданак, Шохшор и Дуконхона, осадочные, терригенные, гемогенные, ступенчато-терраса, палеозойские, архаичные, альбские и сеноманские, окузбулак, альмурод, карабиль, Toshqo‘rg‘on, Yakkasaroy, Langar, G‘ilon, Kulqamish, Maydanak, Shoxshor va Dukonxona, cho‘kindi, terrigen, xemogen, pog‘onali-terrasa, paleozoy, archasimon, alb va senoman, okuzbuloq, almurod, qarabil
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