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Dushanzi Formation

Dushanzi Fm


Period: 
Neogene

Age Interval: 
Pliocene, N2, (1b)


Province: 
Xinjiang

Type Locality and Naming

Junggar Basin S. The type section is located at Dushanzi ~20 km SE of Usu County, Xinjiang. It was named by Compilation Team of the Regional Stratigraphic Table of Xinjiang in 1981.


Lithology and Thickness

Primarily yellowish brown and brownish yellow sandy mudstone alternating or interbedded with pebbly sandstone and conglomerate, containing calcareous concretions. The lithology is relatively uniform and the rocks show a dark greenish brown aspect. The outcrops in the Manas River valley are thickest, being up to >1500 m. From there toward the east and west the formation thins and is of restricted distribution on the northern margin of the basin and exposed sporadically, being generally <50 m.


Lithology Pattern: 
Sandy claystone


Relationships and Distribution

Lower contact

It has a conformable contact with the underlying Miocene Taxihe Fm.

Upper contact

It has a disconformably contact with the overlying early Pleistocene Xiyu Fm.

Regional extent

Southern margin of the basin, mainly distributed at the Toutun, Changji, Hutubi, Manas and Huoergesi rivers and Duoshanzi in Manas and Usu counties.


GeoJSON

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Fossils

Ilyocypris-Cyprideis-Candona; Perissodactyla: Hipparion, Chilotherium


Age 


Age Span: 

    Beginning stage: 
Zanclean

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
5.34

    Ending stage: 
Piacenzian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
2.58

Depositional setting

It is interpreted as a fluviolacustrine environment.


Depositional pattern:  

Additional Information


Compiler:  

Tao Deng, Sukuan Hou, J.Z. Qigao, Q. Li, Q.Q. Shi, B.Y. Sun, S.Q. Wang, F.X. Wu