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Zhuoyoulegansu Formation

Zhuoyoulegansu Fm


Period: 
Paleogene

Age Interval: 
late Middle to early Late Eocene, (3)


Province: 
Xinjiang

Type Locality and Naming

Kashi-Yarkand region (NW Tarim). The naming section is located on a slope at the west side of a road ~ 1 km north of Wulukeqiate Township on the west bank of the Zhuoyoulegansu River in the west part of Wuqia County, Xinjiang. Named by Hao Yichun et al. in 1982; equivalent to the lower part of the Bashibulake Fm (Baxbulak Fm) established by the Xinjiang Petroleum Administration in 1975.


Lithology and Thickness

Lower part is brownish red mudstone with very fine to fine sandstone and thin- and medium-bedded gypsum; the base is white, massive gypsum. Upper part is brownish red, massive, fine sandstone and dark brownish red mudstone. The thickness is about 100–450 m.


Lithology Pattern: 
Sandy claystone


Relationships and Distribution

Lower contact

The formation has a conformable contact with the underlying middle Eocene Wulagen Fm (Ulagun Fm).

Upper contact

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

Regional extent

The distribution scope of this formation is the same as the Wulagen Fm.


GeoJSON

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Fossils

Hao Yichun et al. for the first time found fossil foraminifera and their main element are Nonion laevis, N. rolshauseni, Cibicides artemi, etc. These forms are all index species of the underlying Eocene Kalataer Fm (Karatal Fm) and Wulagen Fm; so it is advisable to assign the age of the formation to Eocene.


Age 


Age Span: 

    Beginning stage: 
Lutetian

    Fraction up in beginning stage: 
0.75

    Beginning date (Ma): 
42.79

    Ending stage: 
Bartonian

    Fraction up in the ending stage: 
0.2

    Ending date (Ma):  
40.37

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

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