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Kiziletesikela Formation

Kiziletesikela Fm


Period: 
Ordovician

Age Interval: 
Katian, (4)


Province: 
Xinjiang

Type Locality and Naming

The type section is at Jiabosar on the north bank of the Ulungur River. The Kiziletesikela Formation was named by Xinjiang Party of Regional Geological Survey and Institute of Geology, Chinese Academy of Geological Science (1974), and was published by Hou Hongfei et al. (1979). Its name came from the Kiziletesikela Village in Fuyun County, northern Xinjiang. Following the naming of the Kiziletesikela Fm, Xinjiang Compiling Group for Regional Stratigraphic Scale (1981) included it in the Jiabosar Fm. Considering the different lithology of these two formations, Xiao Bing (1990) suggested that the previously defined Kiziletesikela Fm should be maintained.

Synonym: (克孜勒特斯科拉组), Kizeleteskela Fm (spelling),


Lithology and Thickness

It is composed of yellowish green thin-bedded argillaceous limestone. The formation recorded an incomplete thickness of 200 m.


Lithology Pattern: 
Clayey limestone


Relationships and Distribution

Lower contact

Upper contact

It is conformably overlain by the Jiabosar Fm

Regional extent

The Kiziletesikela Formation is seen only in Jiabosar.


GeoJSON

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Fossils

This formation yields corals Fuyunolites fuyunensis, Catenipora fuyunensis; trilobite Parisoceraurus dongjunggarensis; brachiopod Szhizophorella xinjiangensis.


Age 


Age Span: 

    Beginning stage: 
Katian

    Fraction up in beginning stage: 
0.4

    Beginning date (Ma): 
449.73

    Ending stage: 
Katian

    Fraction up in the ending stage: 
0.7

    Ending date (Ma):  
447.47

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Jianpo Wang and Xiaofeng Wang