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Permian
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Kulgan Formation

Kulgan Fm


Period: 
Permian

Age Interval: 
P2 (25), middle Permian


Province: 
Xinjiang

Type Locality and Naming

The type section is located at the dried Xiaotikanlik Spring Trench, Sawapuqi region, Wensu County, Xinjiang. It was named by the Stratigraphic Party under the Xinjiang Geological Bureau in 1975. The name of the formation was issued publicly by the Compiling Group for the Regional Stratigraphic Chart of the Xinjiang Uygur Autonomous Region in 1981.


Lithology and Thickness

Siltstone to Sandstone. Composed of grey, silver-grey, grey-green and purple sandy siltstone, siltstone, fine-grained sandstone and coarse-grained sandstone, intercalated occasionally with albite-porphyry. Thickness is 145 m.


Lithology Pattern: 
Siltstone


Relationships and Distribution

Lower contact

Disconformable contact with the volcanic rocks of the underlying Xiaotikanlik Fm

Upper contact

Regionally overlain by Biyoulebaoguzi Gr

Regional extent

Distributed in the Sawapuqo and Kalasu areas of the South Tianshan Mt. region.


GeoJSON

null

Fossils

Plant fossils (phytolites) as represented by Sphenophyllum neofimbriatum, Annularia stellata, Pecopteris orientalis, Cordaites schenkii, Paracalamites stenocostatus, P. decoratus, as well as bivalve fossils.


Age 

Assigned as middle Permian

Age Span: 

    Beginning stage: 
Kungurian

    Fraction up in beginning stage: 
0.5

    Beginning date (Ma): 
278.84

    Ending stage: 
Wordian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
264.34

Depositional setting

It is interpreted as continental deposits.


Depositional pattern:  


Additional Information


Compiler:  

Hou Jingpeng, Zhu Zili