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Huanglianggou Formation

Huanglianggou Fm


Period: 
Permian

Age Interval: 
P3 (5), late Permian (Lopingian Epoch?)


Province: 
Xinjiang

Type Locality and Naming

The type section is located at the Shengligou Valley to the north of Qitai County, Xinjiang. It was named by Yang Wenxiao et al., in 1964.


Lithology and Thickness

Clastics. Composed of interbeds of yellow-green and grey-green conglomerate and sandy siltstone, intercalated with thin-bedded sandstone and carbonaceous siltstone and marl. It is characterized by the occurrence of micro-conglomerate and is different from its underlying Pingdiquan Fm. Thickness is 203 m.


Lithology Pattern: 
Coarse-grained sandstone


Relationships and Distribution

Lower contact

Disconformable contact to the underlying Pingdiquan Fm.

Upper contact

Contact to the overlying Lower Triassic Series (Shangcangfanggou Gr) being conformable or disconformable

Regional extent

Distributed in western and central parts of the Jiangjunmiao mini-region, while extending from the Zhangpenggou area easterly to the areas of Liukeshu, Huanglianggou, Guxingliang and Shiqiantan the granularity of the clastics is getting finer from west to east, with a thickness of 390 m.


GeoJSON

null

Fossils

Plant fossils such as Calamites sp., Pecopteris cf. anthriscifolia, P. cf. imbricata, Annularia sp., Callipteris altaica, Noeggerathiopsis sp.


Age 

Assigned as late Permian (Lopingian Epoch?)

Age Span: 

    Beginning stage: 
Wuchiapingian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
259.55

    Ending stage: 
Changhsingian

    Fraction up in the ending stage: 
0.5

    Ending date (Ma):  
253.07

Depositional setting

It is interpreted as a lake facies. [NOTE – logic was not given.]


Depositional pattern:  


Additional Information


Compiler:  

Hou Jingpeng