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Liujia Formation

Liujia Fm


Period: 
Paleogene

Age Interval: 
Paleocene–Eocene, (19b)


Province: 
Sichuan

Type Locality and Naming

Sichuan Basin - south. The naming section is located in the Hulinbao–Hongyanba area north of Liujiachang 60 km northwest of Yibin County, Sichuan. Named by the Airborne Regional Geological Survey Party, Sichuan Bureau of Geology, in 1980.


Lithology and Thickness

Lower and Middle parts are light brick-red, massive, medium-grained, lithic quartzose sandstone and light brick-red fine- to medium-grained, clayey-calcareous, lithic, arkosic sandstone with some brownish red mudstone lenses. Upper part is light brick-red, thick-bedded to massive, medium- to fine-grained, clayey, lithic arkosic sandstone or alternating beds of medium- to thin-bedded, fine-grained, arkosic sandstone and brownish red, calcareous mudstone; the base, massive sandstone with huge well-developed oblique bedding. Its thickness is 88 m.


Lithology Pattern: 
Clayey sandstone


Relationships and Distribution

Lower contact

The base part conformably overlies the Cretaceous Gaokanba Fm.

Upper contact

In the type section, the upper part unconformably underlies the Quaternary.

Regional extent

This formation is mainly distributed within an area of ~20 km2 around Liujiachang. It is absent in other areas. Westward to Xiliangsi, this formation is 40 m thick, with its upper part being missing.


GeoJSON

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Fossils

The formation contains the ostracods Eucypris, Paracypris and Candona and the charophytes Charites.


Age 


Age Span: 

    Beginning stage: 
Danian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
66.04

    Ending stage: 
Bartonian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
37.71

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

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