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Kumyshkan Formation

Kumyshkan Fm


Period: 
Quaternary

Age Interval: 
Eopleistocene-Neopleistocene (lower link), CK10


Province: 
Chatkal-Kuramin Region

Type Locality and Naming

By the village of Kumyshkan, Parkent district, Tashkent region. T.M. Kremlyakova, M.V. Mikulin, M.P. Safarov (Safarovidr., 1999f.).

Synonym: Kumyshkanskaya Suite, Кумышканская св.


Lithology and Thickness

Reddish-brown paleosols with distinct illuvial layers (shohi) and separating loesses (silt loams). Thickness up to 30m


Lithology Pattern: 
Soil


Relationships and Distribution

Lower contact

Lies on siltstone (aleurolites) ("stone loesses") of the upper Pliocene without visible unconformity

Upper contact

It is conformably overlain by deposits of the Zarkent Fm.

Regional extent

Interfluve of the Chirchik and Angren rivers, foothill landscape zone.


GeoJSON

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Fossils


Age 

In the K. suite, 4 pedocomplexes are distinguished, the oldest of which corresponds to the level of the Jaramillo paleomagnetic episode.

Age Span: 

    Beginning stage: 
Calabrian

    Fraction up in beginning stage: 
0.2

    Beginning date (Ma): 
1.59

    Ending stage: 
Calabrian

    Fraction up in the ending stage: 
0.6

    Ending date (Ma):  
1.18

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

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