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Tyuyabuguz Formation

Tyuyabuguz Fm


Period: 
Quaternary

Age Interval: 
Upper Pliocene-Eopleistocene, CK12


Province: 
Chatkal-Kuramin Region

Type Locality and Naming

In the Tyuya-Buguz Reservoir, Tashkent Region. Ya.M. Khayfets et al., 1970.

Synonym:


Lithology and Thickness

The section is dominated by brownish and pale siltstone (aleurolites) and clays, with layers of sandstones, gravelites, and conglomerates. In the paleovalleys of the Chirchik and Angren rivers, conglomerates and gravel-sandy alluvium predominate. Thickness: up to 340m.


Lithology Pattern: 
Aus Conglomerate


Relationships and Distribution

Lower contact

It lies conformably on the Toytyubin Fm

Upper contact

It is unconformably overlain by Neopleistocene deposits

Regional extent

Along boreholes, in the Tyuya-Buguz Reservoir area, Tashkent Region, it caps the section of brown-colored molasses of the Upper Pliocene-Eopleistocene Upper TienShan Gr. It is correlated with the Kandyrkay Fm


GeoJSON

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Fossils

Upper Pliocene-Eopleistocene ostracods have been found - Lineocypris namanganica Schn., Schneiderella sp., Acutocypris sp., Candone compressaformis Hand., C. apscheronica Schn., Advenocypris aff. gracilis Schn., A. ex gr. decyrta Schn., Subulacypris sp., Herpetocypris sp., Darwinula sp., Lineocypris minuta Schn., Ilyocypris bradyi Sars., I. Gibba (Ramdohr.), Candona rostrata Brady. et Norman., Eucypris ex gr. longa Hand.


Age 

According to A., the age of the suite is Pliocene. But the fossil data indicates Upper Pliocene-Eopleistocene; hence considered the same for Lexicon.

Age Span: 

    Beginning stage: 
Piacenzian

    Fraction up in beginning stage: 
0.7

    Beginning date (Ma): 
2.89

    Ending stage: 
Gelasian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
1.80

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

B.I. Pinhasov, 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)”