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Main source = Abduazimova, Z.M. (Ed.), 2001. Stratigraphic Dictionary of Uzbekistan. IMR (Institute of Mineral Resources), Tashkent, 580 pp. (In Russian) Translated to English by the GeoGPT group, Zhejiang Lab, Hangzhou, China--see About

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Beglyar Formation

Beglyar Fm


Period: 
Cretaceous

Age Interval: 
Middle-Upper Aptian, B1


Province: 
Bukhara-SW Gissar

Type Locality and Naming

Along the Belyar kol, Kugitangtau ridge, T.N. Bogdanova, 1986 (452, p.305). Stratotype on the western wing of the Kugitang anticline, 3 km to the northwest of the Kugitang settlement, 3 km to the southeast of the Belyar kol. The stratigraphic name is not used on the territory of Uzbekistan. Lower formation in Kamprek Gr

Synonym: Beglyar Suite, Беглярская св.


Lithology and Thickness

Massive, cross-bedded, coarse-grained sandstones with layers of conglomerates, siltstone (aleurolites), and clays, with limestone layers in the upper part. Thickness 35-75m


Lithology Pattern: 
Coarse-grained sandstone


Relationships and Distribution

Lower contact

It lies with erosion on the Kaligrek Fm

Upper contact

Schematic stratigraphic column indicates the upper contact as Kulkamysh Fm

Regional extent

Southwest Gissar. The upper part of the formation, probably, is analogous to the Kulkamysh Fm


GeoJSON

null

Fossils

Contains ammonites - Acanthohoplites ex gr. nolani Seun., A. bigoureti Seun., A. lorioli Sinz.; marine bivalve mollusks - Actostreon latissimum (Lam.), Liostrea leymerii Desh. and others.


Age 

It belongs to the Middle-Upper Aptian.

Age Span: 

    Beginning stage: 
Aptian

    Fraction up in beginning stage: 
0.6

    Beginning date (Ma): 
116.48

    Ending stage: 
Aptian

    Fraction up in the ending stage: 
0.7

    Ending date (Ma):  
115.66

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

I.M. Abdurazimova – In: GeoGPT translation of: “Abduazimova, Z.M. (Ed.), 2001. Stratigraphic Dictionary of Uzbekistan. IMR (Institute of Mineral Resources), Tashkent, 580 pp. (In Russian)”