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Badu Formation

Badu Fm


Period: 
Carboniferous

Age Interval: 
C1 (31), late Early Carboniferous


Province: 
Gansu

Type Locality and Naming

The type section is located at Badu Village, 42 km north of Minshan (now Zhuoni County), Gansu Province. It was named by Ye Lianjun and Guan Sicong in 1944.


Lithology and Thickness

Siltstone and Sandy limestone. Dominated by clastic rocks, consisting of dark-gray clayey siltstone, sandy limestone and calcareous conglomerate intercalated with sandstone, as represented by the Baoshekou section on right bank of the Zhaohe River 50 km northeast of Lintan. Thickness over 525 m. Locally with pyroclastic rock around the Demuqiang gulf in Xiahe of the western area.


Lithology Pattern: 
Siltstone


Relationships and Distribution

Lower contact

Unconformable over the Wangjiadian Fm (Dev column 21), the top of which being cut off by fault. Regionally (Dev column 36; middle Qinling), the next older unit can also be the Jiehejie Fm ?

Upper contact

Regionally, the next younger unit is the Xiajialing Fm.

Regional extent

Distributed along Wangatan of Xiahe and Yeliguan of Lintan, Gansu.


GeoJSON

null

Fossils

Brachiopods Gigantoproductus sp., Striatifera sp., etc., Corals Lithostrotion sp., Aulina sp., Kueichouphyllum sp., Dibunophyllum sp., etc. and Fusulinid Eostaffella sp., etc.


Age 

late Early Carboniferous

Age Span: 

    Beginning stage: 
Visean

    Fraction up in beginning stage: 
0.25

    Beginning date (Ma): 
342.63

    Ending stage: 
Serpukhovian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
323.40

Depositional setting

It is interpreted as littoral-neritic sediments.


Depositional pattern:  


Additional Information


Compiler:  

Zhang Yan