Geological features of rocks of the beshkul intrusion

Keldibekova, Zilola Asrorqizi, Mamarozikov, Usmonjon Dovronovich, Hamrayev, Ahmadali Xurromo'g'li, Келдибекова, Зилола Асроркизи, Мамарозиков, Усмонжон Довронович, Хамраев, Ахмадали Хурромугли, Keldibekova, Zilola Asrorkizi, Mamarozikov, Usmonjon Dovronovich, Hamrayev, Ahmadali Xurromugli

Саноатда рақамли технологиялар · 2026-yil

Annotatsiya

The article highlights the geological characteristics of the Beshkul small intrusion rocks located in the southern segment of the Kumbel-Ugam fault zone, based on field observations and macroscopic study of samples. The color, granularity, structure, texture, visible mineral composition, and secondary changes of 10 samples taken from the massif were described. It has been established that the main part of the massif consists of granite, granosienite, and granosienite-porphyres. They are broken by a rod of fine-grained syenite, with a diameter of about 40 m. The granocyenites are vertically intersected by lamprophyre dikes (dikes 0.5-2 m thick) that extend in a northwesterly direction. Inside the massif, in the cataclastic zone with a width of about 30 m near lamprophires, sulfide chlorite metasomatites are developed, with a thickness of 1-1.5 m, and 25-30 m northwest of them, a hematitized sulfide zone is developed, with a width of 2.5-3 m.

Maqola ma’lumotlari
MualliflarKeldibekova, Zilola Asrorqizi, Mamarozikov, Usmonjon Dovronovich, Hamrayev, Ahmadali Xurromo'g'li, Келдибекова, Зилола Асроркизи, Мамарозиков, Усмонжон Довронович, Хамраев, Ахмадали Хурромугли, Keldibekova, Zilola Asrorkizi, Mamarozikov, Usmonjon Dovronovich, Hamrayev, Ahmadali Xurromugli
JurnalСаноатда рақамли технологиялар
NashriyotҚарши муҳандислик-иқтисодиёт институти
ISSN3030-3214, 2023-2026
Nashr sanasi2026-10-07
Jild4
Son3-1
TilIngliz
Ilmiy sohaGeologiya-mineralogiya
DOI10.70769/3030-3214.srt.4.3-1.2026.15
Indeksga qo‘shilgan2026-10-09

DOI: 10.70769/3030-3214.srt.4.3-1.2026.15 · Maqolaning asl sahifasi

Kalit so‘zlar

Qumbel-Ugom yer yoriqlari zonasi, Beshqo‘l, kichik intruziya, granosienit, granosienit-porfir, sienit shtoki, lamprofir, dayka, kataklaz, xloritli metasomatit, gematitizatsiya, sulfidli ma’danlashuv, Кумбель-Угамская зона разломов, Бешкуль, малая интрузия, граносиенит, граносиенит-порфир, шток сиенитов, лампрофир, дайка, катаклаз, хлоритовый метасоматит, гематитизация, сульфидная минерализация, Kumbel-Ugam fault zone, Beshkul, small intrusion, granosyenite, granosyenite porphyry, syenite stock, lamprophyre, dyke, cataclasis, chlorite metasomatite, hematitization, sulphide mineralization

Ilmiy soha

Geologiya-mineralogiya

Iqtibos keltirish

APAKeldibekova, Zilola Asrorqizi, Mamarozikov, Usmonjon Dovronovich, Hamrayev, Ahmadali Xurromo'g'li, Келдибекова, Зилола Асроркизи, Мамарозиков, Усмонжон Довронович, Хамраев, Ахмадали Хурромугли, Keldibekova, Zilola Asrorkizi, Mamarozikov, Usmonjon Dovronovich, & Hamrayev, Ahmadali Xurromugli (2026). GEOLOGICAL FEATURES OF ROCKS OF THE BESHKUL INTRUSION. Саноатда рақамли технологиялар, 4(3-1). https://doi.org/10.70769/3030-3214.srt.4.3-1.2026.15
GOST (OAK)Keldibekova, Zilola Asrorqizi va b. GEOLOGICAL FEATURES OF ROCKS OF THE BESHKUL INTRUSION // Саноатда рақамли технологиялар. – 2026. – T. 4, № 3-1. – DOI: 10.70769/3030-3214.srt.4.3-1.2026.15.
MLAKeldibekova, Zilola Asrorqizi, Mamarozikov, Usmonjon Dovronovich, Hamrayev, Ahmadali Xurromo'g'li, Келдибекова, Зилола Асроркизи, Мамарозиков, Усмонжон Довронович, Хамраев, Ахмадали Хурромугли, Keldibekova, Zilola Asrorkizi, Mamarozikov, Usmonjon Dovronovich, and Hamrayev, Ahmadali Xurromugli. “GEOLOGICAL FEATURES OF ROCKS OF THE BESHKUL INTRUSION.” Саноатда рақамли технологиялар, 4(3-1), 2026. https://doi.org/10.70769/3030-3214.srt.4.3-1.2026.15
ChicagoKeldibekova, Zilola Asrorqizi, Mamarozikov, Usmonjon Dovronovich, Hamrayev, Ahmadali Xurromo'g'li, Келдибекова, Зилола Асроркизи, Мамарозиков, Усмонжон Довронович, Хамраев, Ахмадали Хурромугли, Keldibekova, Zilola Asrorkizi, Mamarozikov, Usmonjon Dovronovich, and Hamrayev, Ahmadali Xurromugli. “GEOLOGICAL FEATURES OF ROCKS OF THE BESHKUL INTRUSION.” Саноатда рақамли технологиялар, 4(3-1) (2026). https://doi.org/10.70769/3030-3214.srt.4.3-1.2026.15
HarvardKeldibekova, Zilola Asrorqizi, Mamarozikov, Usmonjon Dovronovich, Hamrayev, Ahmadali Xurromo'g'li, Келдибекова, Зилола Асроркизи, Мамарозиков, Усмонжон Довронович, Хамраев, Ахмадали Хурромугли, Keldibekova, Zilola Asrorkizi, Mamarozikov, Usmonjon Dovronovich, and Hamrayev, Ahmadali Xurromugli (2026) ‘GEOLOGICAL FEATURES OF ROCKS OF THE BESHKUL INTRUSION’, Саноатда рақамли технологиялар, 4(3-1). https://doi.org/10.70769/3030-3214.srt.4.3-1.2026.15
BibTeX
@article{keldibekovazilolaasrorqizi2026,
  title = {GEOLOGICAL FEATURES OF ROCKS OF THE BESHKUL INTRUSION},
  author = {Keldibekova, Zilola Asrorqizi and Mamarozikov, Usmonjon Dovronovich and Hamrayev, Ahmadali Xurromo'g'li and Келдибекова, Зилола Асроркизи and Мамарозиков, Усмонжон Довронович and Хамраев, Ахмадали Хурромугли and Keldibekova, Zilola Asrorkizi and Mamarozikov, Usmonjon Dovronovich and Hamrayev, Ahmadali Xurromugli},
  journal = {Саноатда рақамли технологиялар},
  year = {2026},
  volume = {4},
  number = {3-1},
  doi = {10.70769/3030-3214.srt.4.3-1.2026.15},
  url = {https://doi.org/10.70769/3030-3214.srt.4.3-1.2026.15}
}

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