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Hudukdaban Formation

Hudukdaban Fm


Period: 
Ordovician

Age Interval: 
Katian-Hirnantian, (10)


Province: 
Xinjiang

Type Locality and Naming

The type section is at Hudukdaban (44°30′N, 83°E) south of Jinghe County, Xinjiang. The Hudukdaban Fm was named by Xinjiang Party of Regional Geological Survey and Chinese Academy of Geological Sciences (1974), and was published by Hou Hongfeit et al. (1979). In 1977, Xinjiang Party of Regional Geological Survey and Chinese Academy of Geological Science measured the Guozigou section in Huocheng, and defined the upper horizon the Hudukdaban Fm and the lower horizon the Aktash Fm, a suggestion was followed by Hou et al. (1979) and Xiao (1979).

Synonym: (呼独克达坂组)


Lithology and Thickness

The formation is gray massive limestone and very thick lime-mud mound. In Huocheng, the Hudukdaban Fm is composed of a sequence about 798 m thick.


Lithology Pattern: 
Reef limestone


Relationships and Distribution

Lower contact

In Guozigou, Huocheng, this formation rests conformably on the micritic limestone of Koksaleixi Fm

Upper contact

It is unconformably overlain by the Nilkahe Fm of early Silurian.

Regional extent

The Hudukdaban Fm is exposed in Hudukdaban and Huocheng south of Jinghe.


GeoJSON

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Fossils

It yields tabular corals Agetolites asiaticus, Plasmorporella granulosa, Paratetradium xinertaiense, Rhabdotetradium cf. quadratum, Neoplasmoporella gracilis, Catenipora sp. and Eofletcheria tianshanensis.


Age 

Katian-Hirnantian. The strata of the Hudukdaban Fm had previously been referred to the limestone yielding Late Ordovician coral south of Jinghe.

Age Span: 

    Beginning stage: 
Katian

    Fraction up in beginning stage: 
0.7

    Beginning date (Ma): 
447.47

    Ending stage: 
Hirnantian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
443.07

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Jianpo Wang and Xiaofeng Wang