Home Multi-Country Search About Admin Login
Cenozoic
Cretaceous
Jurassic
Triassic
Permian
Carboniferous
Devonian
Silurian
Ordovician
Cambrian
Neoproterozoic
Mesoproterozoic

Search by
Select Region(s) to search
Hold Ctrl (Windows/Linux) or Command (Mac) to select multiple
Dahuanggou Formation

Dahuanggou Fm


Period: 
Permian

Age Interval: 
P2 (33), middle Permian


Province: 
Gansu

Type Locality and Naming

The type section is located at Dahuanggou 50 km to the southwest of Jiuquan City, Gansu Province. It was named by Sun Jianchu in 1936.


Lithology and Thickness

Clastics. Composed chiefly of grey-green, yellow-green sandstone, fine-grained sandstone, sandy siltstone, medium-grained and coarse-grained sandstone, intercalated with sandy siltstone and a small amount of black siliceous siltstone, with its top part consisting of grey-white and light-grey-green pebble-bearing coarse-grained sandstone. Thickness is 353 m.


Lithology Pattern: 
Fine-grained sandstone


Relationships and Distribution

Lower contact

Conformable contact with the underlying Shanxi Fm

Upper contact

Between it and the overlying Yaogou Fm there might exist a break.

Regional extent

Distributed in the North Qilian Mt. area extending from Yumen in the west and to the slope of Liupan Mt. in the east, comprising the Hexi Corridor. In the Daqing Trench of South Gansu the thickness of the formation reaches as great as 297 m, composed mainly of light-red sandstone, and conglomeratic layers, with its top part containing purplish-red pebble-bearing sandstones, part of which may probably belong to the Yaogou Fm, with its thickness reaching as great as 244 m at Hejia Mt. of Tongwei County


GeoJSON

null

Fossils

Plant fossils: phytolites such as Lepidodendron sp., Sphenophyllum cf. thonii, Annularia sp., Pecopteris cf. polymorpha, Alethopteris norinii, Taeniopteris cf. multinervis, etc.


Age 

Assigned as middle Permian (Guadalupian Epoch); but, because it is conformable on the Shanxi Fm which Shuzhong Shen et al. (2019; Permian integrated stratigraphy and timescale of China) re-assign to only early-Early Permian, then also includes late-Early Permian (used here)

Age Span: 

    Beginning stage: 
Sakmarian

    Fraction up in beginning stage: 
0.9

    Beginning date (Ma): 
290.81

    Ending stage: 
Roadian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
269.21

Depositional setting

It is interpreted as a river-lake facies deposit.


Depositional pattern:  


Additional Information


Compiler:  

Hou Jingpeng