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Liankan Formation

Liankan Fm


Period: 
Paleogene

Age Interval: 
Middle Eocene, (2)


Province: 
Xinjiang

Type Locality and Naming

Turpan-Hami region. The naming section is located in the Huoyanshan area in the western part of the Turpan basin, at Nanshan Mountain, Lianmuqin Township, ~40 km west of Shanshan County. Named by Zhai Renjie, Zheng Jiajian and Tong Yongsheng in 1978.


Lithology and Thickness

Mainly alternating beds of grayish red and orange-red sandstone and muddy sandstone and brownish red, grayish purple and light blue sandy mudstone, with muddy conglomerate. From west to east the thickness decreases and may reach a maximum of >80 m.


Lithology Pattern: 
Clayey sandstone


Relationships and Distribution

Lower contact

It has a disconformable contact with underlying Paleocene Taizicun Fm.

Upper contact

It has a disconformable contact with the overlying Late Eocene-Oligocene Taoshuyuanzi Fm.

Regional extent

The formation is chiefly distributed at Shengjinkou,Lianmuqin, Nanliankan and Taizicun of Shanshan County, etc., in the western part of the Turpan basin.


GeoJSON

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Fossils

Now 6 genera and 7 species of fossil mammals have been found in the Liankan Formation, of which anthracotheres and deers of artiodactyls are more primitive than the Oligocene common types in other parts of Asia. The main species are Lophialetes expeditus, Teleolophus liankanensis, Bothriodon sp., Xinjiangmeryx parvus, etc.


Age 

Previously the age of the Liankan Formation is assigned to late Eocene (Zheng et al., 1999), and is now assigned to Middle Eocene (Wang et al., 2019; Integr. Strat. Timescale China).

Age Span: 

    Beginning stage: 
Lutetian

    Fraction up in beginning stage: 
0.5

    Beginning date (Ma): 
44.55

    Ending stage: 
Lutetian

    Fraction up in the ending stage: 
0.85

    Ending date (Ma):  
42.09

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

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