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Bailuyuan Formation

Bailuyuan Fm


Period: 
Paleogene

Age Interval: 
Middle Eocene , (18)


Province: 
Shaanxi

Type Locality and Naming

The naming section is located near Maoxi Village on the south bank of the Bahe River in Lantian County, Shaanxi. Named by Liu Dongsheng, Ding Menglin and Gao Fuqing in 1960.


Lithology and Thickness

Predominantly a sequence of white massive sandstone with purplish red mudstone. With a maximum of up to 508 m.


Lithology Pattern: 
Clayey sandstone


Relationships and Distribution

Lower contact

The formation disconformably overlies the Middle Eocene Honghe Fm.

Upper contact

Unconformably underlies the Miocene Lengshuigou Fm (or the Koujiacun Fm, which may be below the Lengshuigou Fm – see that entry).

Regional extent

It has a large outcrop area. On the right bank of the Bahe River it is mainly distributed in the Zhijiagou gully and some large gullies east of the Zhijiagou gully such as Taiqizhai, Mapo, Shahegou, Xiaozhai, Chenjiazhai, Shilihe and Huazuigou, and on the left bank it is only exposed near Maodong Village and Maoxi Village.


GeoJSON

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Fossils

Fossils mainly include the plants Palibrinia korswinii, P. pinnatifida and P. latifolia, as well as sporopollen; the mammals include Lantianius xiehuensis, Sianodon bahoensis and Simplaletes xianensis.


Age 

The age of this formation was suggested to be the Middle Eocene => Oligocene is absent in this region? [older Chinese lexicon strat column had put as late Eocene through Oligocene]

Age Span: 

    Beginning stage: 
Bartonian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
41.03

    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.