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Suotoushan Formation

Suotoushan Fm


Period: 
Devonian

Age Interval: 
D13- D 21 (78; 55), Emsian to Eifelian (late Early Devonian to early Middle Devonian)


Province: 
Yunnan

Type Locality and Naming

The type section is located at a gully of Bianqinggou, Qingmen of County, Chaotong City (103o48’E-27 o 23’N), Yunnan Province. It was named by Xian Shiyuan and Zhou Xiyun in 1974 and published in 1978.


Lithology and Thickness

Sandstone. The formation is characterized by grayish-white and yellow medium- to thick-bedded well-sorted, pure quartz sandstone. Few siltstone and sandy mudstone are observed. Maximum thickness is up to 440 m.


Lithology Pattern: 
Sandstone


Relationships and Distribution

Lower contact

It rests conformably on the Qingmen Fm in the type section and is disconformable with underlying Pojiao Fm or Cambrian rocks in Qiaojia and Ninglang. At the Ningiang section, it rests on the Dacaozi Fm.

Upper contact

It is conformable contact with overlying Haikou Fm, the contact being placed at the change from sandstone below to limestone or dolostone above. In Ninglang section, it is overlain by Lanniqing Fm.

Regional extent

The Formation is widely distributed in northeastern Yunnan forming step cliffs in landscape.


GeoJSON

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Fossils

The formation yields plant Hostimella sp. and fish fossil fragments.


Age 

Emsian to Eifelian (late Early Devonian to early Middle 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: 
0.95

    Ending date (Ma):  
385.75

Depositional setting

It is interpreted as a backshore littoral environment.


Depositional pattern:  


Additional Information


Compiler:  

(Xian Shiyuan)