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Wenchang Formation

Wenchang Fm


Period: 
Paleogene

Age Interval: 
Early to Middle Eocene, (27c)


Province: 
South China Sea, Guangdong

Type Locality and Naming

Pearl River Mouth Basin (offshore). The naming section is located in WC19-1-2 well in the Wenchang depression of the Pearl River Estuary basin, Guangdong; the reference section is WC19-1-3 well. Named by the Western South Sea Branch, China National Offshore Oil Corp. in 1985. The stratotype section of the Wenchang Formation is represented by the 2986–3331 m interval of the well WC19-1-2, located between the Shenhu Fm and Enping Fm.


Lithology and Thickness

It is a sequence of lacustrine grayish black and brownish gray mudstone with light gray sandstone. Lower part consists of alternating beds of gray sandstone and grayish black, dark gray mudstone, with a few conglomerate beds. Upper part consists of light brownish red, grayish black and brownish gray mudstone with minor light gray sandstone and coal beds. The sandstone is poorly sorted and rounded, being mainly feldspar lithic sandstone feldspathic debris sandstone; mudstone is pure, without calcium, containing significant quantities of siderite grains. The total thickness is 0–912 m. At the seismic section this formation is equivalent to the reflector group between T8–T9.


Lithology Pattern: 
Sandy claystone


Relationships and Distribution

Lower contact

It has a disconformable contact with the underlying Paleocene Shenhu Fm and overlaps unconformably on the pre-Tertiary in some areas.

Upper contact

Its contact with the overlying Paleogene Enping Fm is unconformable.

Regional extent

This formation is distributed in a dissected graben basin, such as the Wenchang, Enping, Xinjiang Huizhou, Lufeng and Hanjiang depressions, and also present in the depression No. 27-2 of Fanyu, Baiyun and Kaiping depressions.


GeoJSON

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Fossils

This formation is rich in sporopollen, represented by the Quercoidites- Pentapollenites assemblage. In HJ15-1-1 well in the Hanjiang depression there occur small quantities of calcareous nannofossils such as Discoaster barbadiensis, D. kuepperi, Reticulofenestra umbilica and Tribrachiatus orthostylus.


Age 

Its age was previously considered to be Eocene (Zheng et al., 1999). Recent study assigns this formation to Early to Middle Eocene (National Commission on Stratigraphy of China, 2018).

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: 
0.5

    Ending date (Ma):  
44.55

Depositional setting

It is lacustrine deposits.


Depositional pattern:  

Additional Information


Compiler:  

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