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Wudang Formation

Wudang Fm


Period: 
Devonian

Age Interval: 
D1, (52) Early Devonian


Province: 
Guizhou

Type Locality and Naming

The type section is located at Dapingshan of Mairangzhai, Wudang region of Guiyang City, Guizhou. It was firstly reported by Pan Jiang et al. in 1975.


Lithology and Thickness

Siltstone. This formation is a set of variegated clastic rocks, consisting of purplish-red, flesh-red and light-gray siltstone, silty mudstone and quartz sandstone, intercalated with ferruginous quartz sandstone and pebble sandstone in the base. It is 80-120 m thick.


Lithology Pattern: 
Siltstone


Relationships and Distribution

Lower contact

The formation has a disconformable basal contact to the underlying purplish-red thin-bedded ferruginous clayey siltstone of Gaozhaitian Gr of Lower Silurian.

Upper contact

The formation is overlain by light-gray to grayish-white quartz sandstone of Mazongling Fm.

Regional extent

Limited distribution to near Guiyang.


GeoJSON

null

Fossils

The formation yields abundant fish fossils Kueichowlepis sinensis, Sinopetalichthys kueiyangensis, Neoduyunaspis minuta.


Age 

Early Devonian

Age Span: 

    Beginning stage: 
Eifelian

    Fraction up in beginning stage: 
0.25

    Beginning date (Ma): 
392.05

    Ending stage: 
Eifelian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
385.30

Depositional setting

It is interpreted as a littoral (foreshore) facies.


Depositional pattern:  


Additional Information

The Wudang Fm is correlative with the lower part of the Mangshan Gr.


Compiler:  

(Xian Siyuan)