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Zhongning Formation
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Zhongning Fm base reconstruction

Zhongning Fm


Period: 
Devonian

Age Interval: 
D3 (20-east), Late Devonian


Province: 
Ningxia

Type Locality and Naming

The type section is located at Shixia Valley of Baima Village, Zhongning County of Ningxia Hui Autonomous Region. It was named by Pan Jiang and others in 1980.


Lithology and Thickness

Sandstone. The Formation is composed of purplish-red, grayish-green and white coarse- and fine-grained feldspar quartz sandstone and siltstone, occasionally intercalated with thin-bedded sandy limestone. The Formation is about 300 m thick.


Lithology Pattern: 
Sandstone


Relationships and Distribution

Lower contact

It has an unconformable basal contact to the underlying Shixiagou Fm.

Upper contact

It has a disconformable upper contact with the overlying Yanghugou Fm of Carboniferous.

Regional extent


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[106.52,38.23],[104.85,37.501],[105.64,36.636],[107.27,37.1],[107.64,37.87],[106.52,38.23]]]]}}

Fossils

It contains Fish fossils Remigolapis zhongningensis, R. major; and Plant fossils Lepidophloeum rhombicum, Sublepidodendron mirabile.


Age 

Late Devonian

Age Span: 

    Beginning stage: 
Frasnian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
378.90

    Ending stage: 
Famennian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
359.30

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

(Wang Shitao)