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Huadian Formation

Huadian Fm


Period: 
Paleogene

Age Interval: 
Middle Eocene , (14b)


Province: 
Jilin

Type Locality and Naming

The naming section is located at Gonglangtou and Daboji ~15 km northeast of Huadian County, Jilin. Named by Nishita Shouichi in 1940.


Lithology and Thickness

This formation may be divided into three parts: Lower part, yellowish brown or gray sandstone and pebbly sandstone with carbonaceous shale; Middle part, yellowish brown sandstone with variegated sandstone and mudstone, with several beds of minable oil shale; Upper part, grayish white, grayish green and gray pebbly sandstone, sandstone, muddy sandstone and sandy mudstone, with oil shale and lignite beds. The outcrops are generally poor, mainly found in the wells; the thickness reaches 1600–1900 m.


Lithology Pattern: 
Coarse-grained sandstone


Relationships and Distribution

Lower contact

Unconformable contact with both the underlying Early Cretaceous Heiweizi Fm or Paleozoic granite and metamorphic series.

Upper contact

Unconformable contact with the overlying Tumenzi Fm.

Regional extent

This formation is mainly distributed at Gonglangtou, Zaiboji, Miaoling, Beitaizi, Xitaizi and Zhongxinjie, Huadian County.


GeoJSON

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Fossils

Fossils of the Huadian Formation are only found in its middle and upper parts. In addition to plants, gastropods and Threskiorothidae and Anatidae of birds, the fishes are mainly Amia, Catostomidae and Clupeiformes, and the mammals mainly include Eochenus sinensis, Tupaiodon huadianensis, Ernosonex jilinensis, Asiomomys changbaicus and Zelomys orientalis.


Age 

According to Wang Banyue et al. (1990), some elements in the Huadian fauna are comparable to the Eocene Bridgerian-Uintan species of North America; so its age is probably late-mid Eocene or late Eocene. According to Zhou Jiajian et al. (1985), the fishes are very similar to those of the early-mid Eocene Green River Formation of North America. Therefore, from the general aspects of the biotas, the age of the Huadian Formation is probably middle Eocene or early-mid Eocene.

Age Span: 

    Beginning stage: 
Ypresian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
56.00

    Ending stage: 
Lutetian

    Fraction up in the ending stage: 
0.75

    Ending date (Ma):  
42.79

Depositional setting

According to the fauna, flora and sediments, the ecological environment of Huadian then was of forest-swamp-lake facies. A number of animals living in tropical and subtropical jungles appeared; meanwhile, there were numerous fishes and hydrophilic birds.


Depositional pattern:  


Additional Information


Compiler:  

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