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Neogene
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Cretaceous
Jurassic
Triassic
Permian
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Devonian
Silurian
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Mesoproterozoic
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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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Kichar Formation

Kichar Fm


Period: 
Silurian

Age Interval: 
Pridoli, N1


Province: 
Nuratau

Type Locality and Naming

By the village of Kichar, Shokhetau Mountains, N. Nuratau Range, R.R. Usmanov et al. in 1993 (Korsakov et al., 1993f.).

Synonym: Kichar Suite, Кичарская св.


Lithology and Thickness

Massive, less often layered organogenic limestones, locally dolomitized. Thickness more than 200 m.


Lithology Pattern: 
Reef limestone


Relationships and Distribution

Lower contact

Lower contact is tectonic.

Upper contact

Conformably overlies the Tulebay Fm [assumed that “underlies” was meant due to their relative ages]. Upper [assumed “Lower” was meant] contact is tectonic.

Regional extent

Northern Nuratau Range, Shokhetau Mountains. Stratotype in the area of the village of Kichar.


GeoJSON

null

Fossils

Tabulates - Favosites brusnitzini Peetz., F. ex gr. preplacenta Dubat., Pachyfavosites ex gr. exilis Sok and others


Age 

Pridoli age is established by tabulates

Age Span: 

    Beginning stage: 
Pridoli

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
422.73

    Ending stage: 
Pridoli

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
419.00

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

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