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Wangshan Formation
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Wangshan Fm base reconstruction

Wangshan Fm


Period: 
Neoproterozoic

Age Interval: 
middle Sinian (middle Ediacaran), Z (27)


Province: 
Anhui

Type Locality and Naming

North Anhui. The Wangshan Fm was jointly named by the Jiangsu and Anhui Parties of Regional Geological Survey in 1976, which is first quoted in the Guidebook of 1: 200 000 Scale Geological Map of Xuzhou Sheet 1(978). The Wangshan Formation is located at Wangshan Hills between Xieji and Langan villages, Suxian County, Anhui Province. The type section includes two parts, the middle and lower parts are exposed in the Shijia section, the upper part is represented by the Jinshanzhai section in Suxian County, Anhui Province.

Synonym: (望山组)


Lithology and Thickness

The Wangshan Fm consists of three parts. Lower part is gray and light gray thin bedded dolomitic limestone, interbedded with calcareous shale, showing rib-like form after weathering. Middle part is gray and light gray medium- to thick-bedded dolomitic limestone with argillaceous banded limestone, locally with horizontal lamination bedding and polygonal structure. Upper part is gray and light gray thin- to medium-bedded limestone with chert nodules and banded and stromatolite reefs. The argillaceous component decreases upward as the dolomitic and siliceous components increase. The Wangshan Formation is 473-566 m thick.


Lithology Pattern: 
Dolomitic limestone


Relationships and Distribution

Lower contact

In the bottom of the formation, medium- to thick-bedded banded argillaceous limestone is continuous and conformable with the underlying Shijia Fm. The Wangshan Fm is also conformable on the underlying Weiji Fm

Upper contact

It is conformably overlain by the Gouhou Formation.

Regional extent

North Anhui. The Wangshan Formation is distributed around Wangshan and Jinshanzai, and a few parts are exposed in southwest slope of Heifengling Hills, Suxian County, Anhui Province.


GeoJSON

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Fossils

Microplants: Favososphaeridium sp., Trachysphaeridium sp., Eomycetopsis sp., Myxococcoides sp.; stromatolites: Katauia placertula, Anabaria radialis, Linella cf. minuta, Jurusania f., Xuejiella Formosa, Baicalia f., Inzeria f., Minjiaria f.


Age 

Uppermost (9 of 10) in a succession of eight formations spanning early through middle Sinian (early through middle Ediacaran) formations according to assigned "Z" code and schematic stratigraphic column.

Age Span: 

    Beginning stage: 
Ediacaran

    Fraction up in beginning stage: 
0.63

    Beginning date (Ma): 
574.39

    Ending stage: 
Ediacaran

    Fraction up in the ending stage: 
0.7

    Ending date (Ma):  
567.66

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Extracts from The Neoproterozoic Erathem (chapter in Stratigraphic Lexicon of China, draft of 2022) by Gao Linzhi, Ding Xiaozhong, Zhang Chuanheng, Zhang Heng.