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Xiliugou Formation

Xiliugou Fm


Period: 
Paleogene

Age Interval: 
Eocene, (6c)


Province: 
Gansu

Type Locality and Naming

Lanzhou-Xining region. The Regional Survey Party of the Gansu Bureau of Geology designated a sequence of mainly fluvial deposits in the first rock unit of the original Xianshuihe Fm in the Lanzhou basin as the Xiliugou Formation in 1984. The naming section is located in an area from Yehucheng to Fenghuang Village, Yongdeng County, central Lanzhou basin, Gansu.


Lithology and Thickness

Dark red, massive pebbly sandstone and grit with thin-bedded mudstone. The thickness is 59–593 m.


Lithology Pattern: 
Conglomerate


Relationships and Distribution

Lower contact

It has an unconformable contact with the underlying Cretaceous Hekou Gr. Regionally, next older unit is uppermost Cretaceous Minhe Fm.

Upper contact

It has a conformable contact with the overlying Paleogene Yehucheng Fm.

Regional extent

This formation is distributed in the Lanzhou basin and Longzhong basin.


GeoJSON

null

Fossils

It yields the ostracods Cypris and Eucypris and the charophytes Stephanochara and Harrisichara.


Age 

China Lexicon chart had shown as span of entire Eocene; but revised basal age of overlying Yehucheng Fm implies span is now earliest Eocene.

Age Span: 

    Beginning stage: 
Ypresian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
56.00

    Ending stage: 
Ypresian

    Fraction up in the ending stage: 
0.7

    Ending date (Ma):  
50.45

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

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