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Tumen Gr

Tumen Gr


Period: 
Neoproterozoic

Age Interval: 
Qingbaikuan (Tonian), Qb (26-b)


Province: 
Shandong

Type Locality and Naming

North-central Shandong. The Tumen Gr was named by Wang Liangchen (1959), which was introduced by Beijing Geological College and Bureau of the Shandong Geology (1961). The type section is located in Fulaishan Hill of the Juxian County, Shandong Province.

Synonym: (土门群)


Lithology and Thickness

The Tumen Gr consists mainly of cyclic deposition of sandstone, shale and limestone with stromatolites, microplants and macrofossils of algae. The Tumen Gr consists of an upward succession of the Heishanguan Fm, Erqingshan Fm, Tongjiazhuang Fm, Fulaishan Fm and Shiwangzhuang Fm (see figure). It is over 600 m thick.

[Figure: The Stratigraphic column of the Tumen Gr (made by Zhang Chuanheng)]


Lithology Pattern: 
Sandy limestone


Relationships and Distribution

Lower contact

It is unconformable with underlying Taishan Complex or metamorphosed granite pluton.

Upper contact

It is disconformably overlain by the Changqing Gr

Regional extent

North-central Shandong. It is developed in Linyi, Anqiu, Juxian area, Shandong Province.


GeoJSON

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Fossils

Microplants: Trachysphaeridium incrassatum, T. simplex, Taeniatum crasum, Leiopsophosphaera solida.


Age 

Qingbaikuan (Tonian) on schematic stratigraphic column.

Age Span: 

    Beginning stage: 
Tonian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
1,000.00

    Ending stage: 
Tonian

    Fraction up in the ending stage: 
0.65

    Ending date (Ma):  
818.00

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.