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Qimugen Formation

Qimugen Fm


Period: 
Paleogene

Age Interval: 
Late Paleocene to early Early Eocene, (3)


Province: 
Xinjiang

Type Locality and Naming

Kashi-Yarkand region (NW Tarim). The naming section is located near Qimugen in the foothills of the Kunlun Mountains, Xinjiang. Named by the Xinjiang Petroleum Administration in 1975.


Lithology and Thickness

Littoral–neritic, grayish green mudstone, gray sandstone and marlstone with thin-bedded coquina, with a ~5 m thick bed of gray limestone at the base and a 5–10 m thick gray and reddish gray, massive limestone at the top, which are of uniform distribution and may serve as markers for the stratigraphic division and correlation. The thickness is ~100 m.


Lithology Pattern: 
Continental marl


Relationships and Distribution

Lower contact

It has a conformable contact with the underlying Paleocene Aertash Fm (Alatax Fm).

Upper contact

It has a conformable contact with the overlying Eocene Gaijitage Fm or Kalataer Fm (Karatal Fm).

Regional extent

This formation is widespread, extending from the national border eastward approximately to east of Hotan River, but it is absent in the Wulagen uplift in the foothills of the Tianshan Mountains.


GeoJSON

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Fossils

The formation contains abundant fossils of ostracods, Eocytheropteron kalickyi and Kinthe scelinis; and foraminifera, Globorotalia spp., Globigerina sp., Spiroplectammina sp., Nonionellina sp., etc.


Age 


Age Span: 

    Beginning stage: 
Danian

    Fraction up in beginning stage: 
0.95

    Beginning date (Ma): 
61.88

    Ending stage: 
Ypresian

    Fraction up in the ending stage: 
0.15

    Ending date (Ma):  
54.81

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

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