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Banxi Gr

Banxi Gr


Period: 
Neoproterozoic

Age Interval: 
Late Qingbaikouan (late Tonian), Qb (53, 54, 55, 58, 59)


Province: 
Hunan, Guizhou

Type Locality and Naming

The name Banxi Gr derived from the Banxi System named by Wang Xiaoqing (H. C. Wang) and Liu Zuyi in 1936. The typical section is located in Banxi village; 60 km northwest of Yiyang County, Hunan Province (now belongs to Taojiang County). At present, the representative sections are situated in Madiyi (Yuanling County) and Yuxikou (Zhijiang County), Hunan Province.

[Figure: The type section of the Banxi Group in Hunan Province]

Synonym: (板溪群)


Lithology and Thickness

In the Linxiang to Shimen district, the Banxi Gr is imperfect and dominated by purplish red psepholite (=gritstone to conglomerate) and silty slate, which represents the coastal fluvial to delta deposit, with thickness of 300 to 700 m.

In the Yueyang-Huaihua district, the Banxi Group is perfect and composed of greenish gray, purplish red slightly metamorphosed conglomerate, sandstone, slate, tuffite, carbonate rock and carbonaceous slate, which constituted two large cycles. The older is represented by the Madiyi Fm and the younger is the Wuqiangxi Fm. The Madiyi Formation has its carbonate rock and carbonaceous slate, gradually increasing from north to south.

In the middle area, the Banxi Group includes the Gaojian Fm overlain by the Mobin Fm (formerly named as Jiabang Fm and Lalan Fm), which are dominantly composed of greenish gray to dark gray and minor purplish gray low-grade metamorphic sandstone, tuff and slate. The lower part is intercalated with carbonaceous slate, locally with seafloor intermediate volcanic eruptive rock, and the total thickness varies from 3290 to 4750 m.

In northeast Guizhou (Songtao, Tongren, Jiangkou), the lower part of the former Banxi Gr is now called the Hongzixi Fm and the upper part also called as the Qingshuijiang Fm, which corresponds to the Wuqiangxi Fm in Hunan Province.


Lithology Pattern: 
Clayey sandstone


Relationships and Distribution

Lower contact

The Banxi Gr unconformably overlies the underlying Lengjiaxi Gr (Dayangu Fm) in northwest Hunan and Fanjiangshan Gr (Duyangtang Fm) in northeast Guizhou.

Upper contact

The Banxi Gr unconformably the Jiangkou Fm in northwest Hunan and Liangjiehe Fm in northeast Guizhou.

Regional extent

Eastern Guizou-northwest Hunan. Based on the different lithologic characters, the distribution area of Banxi Gr is divided into the north area (including the north part and the south part) and the middle area. The north area is subdivided into the Linxiang-Shimen district (the north part) and the Yueyang to Huaihua district (the south part).


GeoJSON

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Fossils

Only minor microplants were found from the Banxi Gr.


Age 

SHRIMP U-Pb dates (814±12 Ma, 805±16 Ma) had been acquired from a tuff bed of this formation (Gao Linzhi et al., 2011). Late Qingbaikouan (late Tonian),

Age Span: 

    Beginning stage: 
Tonian

    Fraction up in beginning stage: 
0.4

    Beginning date (Ma): 
888.00

    Ending stage: 
Tonian

    Fraction up in the ending stage: 
0.8

    Ending date (Ma):  
776.00

Depositional setting

The Banxi Gr in this district represents the terrestrial to neritic continental slope deposit and the total thickness varies from 572 to 3803 m. It represents the typical continental slope deposit.


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.