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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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Akbulak-Quat Moraine Formation
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Akbulak-Quat Moraine Fm base reconstruction

Akbulak-Quat Moraine Fm


Period: 
Quaternary

Age Interval: 
Holocene, CK5


Province: 
Chatkal-Kuramin Region

Type Locality and Naming

Along the Akbulak River, basin of the Chatkal River, Pri-Tashkent region. Identified based on data from A.R. Blazheevich (Safarov et al., 1999).

Synonym: Akbulak Moraine, Акбулакская морена


Lithology and Thickness

Represented by morainic deposits of terminal, lateral, medial, and bottom moraines, as well as ice cores of modern glaciers. Chaotic accumulation of sharp-angled and angular fragments ranging in size from 15-30 cm to a meter and larger. Filling is varied to sandy-aleurolitic(silty). Thickness 40-50m, and up to 70m.


Lithology Pattern: 
Glacial till


Relationships and Distribution

Lower contact

Upper contact

Regional extent

Chatkal Range, Akbulak River.


GeoJSON

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Fossils


Age 

Quaternary (Holocene)

Age Span: 

    Beginning stage: 
Holocene

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
0.01

    Ending stage: 
Holocene

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
0.00

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)”