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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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Khanbandytau Formation

Khanbandytau Fm


Period: 
Devonian

Age Interval: 
Middle Devonian, N3


Province: 
Nuratau

Type Locality and Naming

In the Khanbandytau Mountains, northern foothills of the N. Nuratau Range. P.N. Podkopaev et al. in 1961 (457, pp. 128-129).

Synonym: Khanbandytau Suite, Ханбандитауская св., Khanbandytay Fm, Khanbanditau Fm


Lithology and Thickness

Light organogenic massive and thin-bedded limestones. Thickness is 525m.


Lithology Pattern: 
Reef limestone


Relationships and Distribution

Lower contact

Lies conformably on the Uchkulach Fm

Upper contact

It is also conformably overlain by the Pistalitau Fm

Regional extent


GeoJSON

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Fossils

Contains brachiopods - Stringocephalus burtini Defr., Atrypa zonata Schnur., A. flabellata Roem., Spinatrypa bifidaeformis Rzon., Uncinulus parallelepipidus Bronn., Uncites Gryphus Schloth., Bornhardtina uncitoides Schulz; tabulates - Thamnopora sp., Caliapora taltiensis Yanet., C. battersbyi M.E. et H., Heliolites sp.; stromatoporoids - Amphipora ramosiensis Bog., Actinostroma">Actinostroma clathratum Nich., A. cystosum Bog., A. septatum Lec., Parallelopora adleriYavor., Stachyodes verticillata Mc'Coy, Stromatopora hupschii Barg.; conodonts - Polygnathus latifosatus Wirht., P. cristatus Hinde., P. angusticostatus Wit.


Age 

Age is Middle Devonian, Zheleznikov horizon. (165; 441; 460).

Age Span: 

    Beginning stage: 
Eifelian

    Fraction up in beginning stage: 
0.75

    Beginning date (Ma): 
387.55

    Ending stage: 
Givetian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
378.90

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

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