Home Multi-Country Search About Admin Login

Search by
Select Region(s) to search
Hold Ctrl (Windows/Linux) or Command (Mac) to select multiple
Yangak Formation

Yangak Fm


Period: 
Carboniferous

Age Interval: 
Middle Carboniferous (Bashkirian), F10


Province: 
Fergana

Type Locality and Naming

Along the village of Yangak, S. Fergana. A.D. Miklouho-Maclay, G.S. Porshnyakov, 1961 (296, p. 13). Stratotype in the basin of the Shuransay near the village of Yangak.

Synonym: Yangakskaya Suite, Янгакская св.


Lithology and Thickness

Limestones, interbedded with clay shales. Thickness 50-70m. In the Stratigraphic Lexicon (439) indicates thickness. up to 400-450m


Lithology Pattern: 
Clayey limestone


Relationships and Distribution

Lower contact

Conformably overlies the Vizebashkirian limestones

Upper contact

Conformably overlain by the Karatangin Fm

Regional extent

Southern Fergana, northern foothills of the Alai Range, interfluve of the Sokh-Shahimardan.


GeoJSON

null

Fossils

Limestones contain foraminifers Pseudostaffella antiqua (Dutk.), Eostaffella pseudostruvei Raus. et Reitl., E. parva Moell, characteristic of the early Bashkirian substage.


Age 

Assigned to the Bashkirian stage of the middle Carboniferous. In the Stratigraphic Lexicon (457) assigned to the upper Bashkirian substage. In the Stratigraphic Lexicon (439) indicates thickness. up to 400-450m and age within the upper part of the early Bashkirian substage and the upper Bashkirian substage of the middle Carboniferous. On the State Geological Map-500 of Uzbekistan (460) - Bashkirian stage of the middle Carboniferous.

Age Span: 

    Beginning stage: 
Bashkirian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
323.40

    Ending stage: 
Bashkirian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
315.15

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

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