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
Wulagen Formation

Wulagen Fm


Period: 
Paleogene

Age Interval: 
Middle-Late Eocene, (3)


Province: 
Xinjiang

Type Locality and Naming

Kashi-Yarkand region (NW Tarim). The naming section is located on the south limb of the Wulagen (Ulagun) syncline in Wuqia County in the piedmont zone of the Tianshan Mountains, Xinjiang. Named by the Xinjiang Petroleum Administration in 1975.

Synonym: Ulagun Fm


Lithology and Thickness

In the piedmont zone of the Tianshan Mountains west of Kashi, the lithology is relatively uniform. Except in individual sections where red mudstone and gypsum beds are present, most sections consist dominantly of grayish green mudstone and calcareous sandstone with thin-bedded limestone. In the piedmont zone in the southeastern part of the southwest Tarim subbasin, the lithology is highly varied and turns into the alternating beds of red mudstone and conglomerate with grayish green bands in some sections. The thickness is ~20–120 m.


Lithology Pattern: 
Continental marl


Relationships and Distribution

Lower contact

The formation has a conformable contact with the underlying Eocene Kalataer Fm.

Upper contact

The formation has a conformable contact with the overlying Eocene Bashibulake Fm (Baxbulak Fm).

Regional extent

This formation is distributed from the national border eastward roughly to east of Hotan.


GeoJSON

null

Fossils

There occur the foraminifera Anomalina, Cibicides, Nonion, Rotalia, etc., the ostracods Cytherella, Loxoconcha, etc., the bivalves Sokolovia bohmi, Ostrea (Flemigostrea) kaschgarica and Liostrea kokanensis and the gastropods Turritella, Athleta, etc. The above-mentioned fossils are essentially the commonest genera and species in the Eocene Turkistan Formation in the Fergana and Tajik basins, former Soviet Union, of which the mollusk fossils are mostly the endemic species in Central Asia. Furthermore, some forms are also found in the mid-upper Eocene of France, Poland and Ukraine.


Age 

According to the characteristics of the mollusks and foraminifera, the age of the formation is probably mid-late Eocene.

Age Span: 

    Beginning stage: 
Lutetian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
48.07

    Ending stage: 
Lutetian

    Fraction up in the ending stage: 
0.75

    Ending date (Ma):  
42.79

Depositional setting

It is interpreted as neritic or lagoonal deposits.


Depositional pattern:  


Additional Information


Compiler:  

Tao Deng, Yuanqing Wang, Qian Li, et al.