Biotite granites of the zarkainar intrusion: composition, ore content and conditions of formation (southern nuratau)

Xalbay ISHBAYEV, Anvar SHUKUROV, Sarvar QODIROV, Quatbay KOSBERGENOV

Ўзбекистон Миллий университети хабарлари · 2024-yil

Annotatsiya

The Zarkainar intrusion is composed of S-type granitoids (quartz-diorite, granodiorite, biotite granite, etc.), formed due to sedimentary- metamorphic rocks as a result of plate collision. Most of it is composed of biotite granites. As a result of the research, complex blocks of gabbro-diorites, diorites and quartz diorite bodies, granodiorites-adamellites, tonalites, double-mica granites and vein rocks were identified. The latter consists of syntrusive (granite-aplites, aplite-pegmatites, pegmatites, etc.) and dikes of diorite porphyrites and spessartites of the calc-alkaline series, belonging to the independent North Nurata dike complex. Spessartite dikes are enriched in REE (up to 950 g/t). The granitoids of the Zarkainar intrusion form a consistent (homodromous) series - monzodiorites, monzonites and normal biotite granites.

Maqola ma’lumotlari
MualliflarXalbay ISHBAYEV, Anvar SHUKUROV, Sarvar QODIROV, Quatbay KOSBERGENOV
JurnalЎзбекистон Миллий университети хабарлари
NashriyotЎзбекистон Миллий университети
ISSN2181-7324, 3093-8996
Nashr sanasi2024-03-30
Jild3
Son3.1
Betlar236-242
TilIngliz
DOI10.69617/nuuz.v3i3.1.1781
Indeksga qo‘shilgan2026-08-27

Kalit so‘zlar

REE (up to 950 g/t). The granitoids of the Zarkainar intrusion form a consistent (homodromous) series - monzodiorites, monzonites and normal biotite granites., Гранитоиды Заркайнарского интрузива образуют последовательный (гомодромный) ряд - монцодиоритов, монцонитов и нормальных биотитовых гранитов., Zarqaynar intruzivi granitoidlari monsodiorit, monsonit, normal granitlar ketma-ket (gomodrom) qatorini hosil qiladi.

Iqtibos keltirish

APAXalbay ISHBAYEV, Anvar SHUKUROV, Sarvar QODIROV, & Quatbay KOSBERGENOV (2024). BIOTITE GRANITES OF THE ZARKAINAR INTRUSION: COMPOSITION, ORE CONTENT AND CONDITIONS OF FORMATION (SOUTHERN NURATAU). Ўзбекистон Миллий университети хабарлари, 3(3.1), 236-242. https://doi.org/10.69617/nuuz.v3i3.1.1781
GOST (OAK)Xalbay ISHBAYEV va b. BIOTITE GRANITES OF THE ZARKAINAR INTRUSION: COMPOSITION, ORE CONTENT AND CONDITIONS OF FORMATION (SOUTHERN NURATAU) // Ўзбекистон Миллий университети хабарлари. – 2024. – T. 3, № 3.1. – P. 236-242. – DOI: 10.69617/nuuz.v3i3.1.1781.
MLAXalbay ISHBAYEV, Anvar SHUKUROV, Sarvar QODIROV, and Quatbay KOSBERGENOV. “BIOTITE GRANITES OF THE ZARKAINAR INTRUSION: COMPOSITION, ORE CONTENT AND CONDITIONS OF FORMATION (SOUTHERN NURATAU).” Ўзбекистон Миллий университети хабарлари, 3(3.1), 236-242, 2024. https://doi.org/10.69617/nuuz.v3i3.1.1781
ChicagoXalbay ISHBAYEV, Anvar SHUKUROV, Sarvar QODIROV, and Quatbay KOSBERGENOV. “BIOTITE GRANITES OF THE ZARKAINAR INTRUSION: COMPOSITION, ORE CONTENT AND CONDITIONS OF FORMATION (SOUTHERN NURATAU).” Ўзбекистон Миллий университети хабарлари, 3(3.1), 236-242 (2024). https://doi.org/10.69617/nuuz.v3i3.1.1781
HarvardXalbay ISHBAYEV, Anvar SHUKUROV, Sarvar QODIROV, and Quatbay KOSBERGENOV (2024) ‘BIOTITE GRANITES OF THE ZARKAINAR INTRUSION: COMPOSITION, ORE CONTENT AND CONDITIONS OF FORMATION (SOUTHERN NURATAU)’, Ўзбекистон Миллий университети хабарлари, 3(3.1), 236-242. https://doi.org/10.69617/nuuz.v3i3.1.1781
BibTeX
@article{xalbayishbayev2024,
  title = {BIOTITE GRANITES OF THE ZARKAINAR INTRUSION: COMPOSITION, ORE CONTENT AND CONDITIONS OF FORMATION (SOUTHERN NURATAU)},
  author = {Xalbay ISHBAYEV and Anvar SHUKUROV and Sarvar QODIROV and Quatbay KOSBERGENOV},
  journal = {Ўзбекистон Миллий университети хабарлари},
  year = {2024},
  volume = {3},
  number = {3.1},
  pages = {236-242},
  doi = {10.69617/nuuz.v3i3.1.1781},
  url = {https://doi.org/10.69617/nuuz.v3i3.1.1781}
}

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