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Hongquan Formation

Hongquan Fm


Period: 
Permian

Age Interval: 
P3 (33, 34), Lopingian Epoch (late Permian)


Province: 
Gansu

Type Locality and Naming

The type section is located at the Daquan 10 km to the north of the Hexibao Railway Station on the Lanzhou-Xinjiang Railway in the territory of Gansu Province. It was named by Liang Jiande et al., in 1977, and was cited officially by the Compiling Group on the Regional Stratigraphic Chart of Gansu Province in 1980.


Lithology and Thickness

Conglomerate and Clastics. Composed of purplish-red conglomerate and pebble-bearing coarse-grained sandstone, intercalated with siltstone and clayey siltstone, with its middle part containing 5 m-thick grey-green clayey siltstone and clayey shale; with it top part being intercalated with several layers of siliceous marls. Its basal part consists of a purple conglomerate layer. Total thickness is 141 m.


Lithology Pattern: 
Conglomerate


Relationships and Distribution

Lower contact

Disconformable contact with the underlying Xiashihezi Fm (lower Shihezi) Fm or the Dahuanggou Fm

Upper contact

Conformable or disconformable contact with the overlying Daquan Fm

Regional extent

Distributed in the areas of Dahuanggou of Synan County, Daquan and Daqinggou of Jinchang City, and Wufuo Temple of Jingtai County.


GeoJSON

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Fossils

Plant fossils (phytolites) such as the Pecopteris lativenosa, P. tenuicostata, Compsopteris wongii, Zamiopteris glossopteroides, Taeniopteris sp., Noeggerathiopsis sp., as well as Ostracoda fossils


Age 

Assigned as late Permian.

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 river facies.


Depositional pattern:  


Additional Information


Compiler:  

Hou Jingpeng