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Xiajiang Gr

Xiajiang Gr


Period: 
Neoproterozoic

Age Interval: 
Late Qingbaikouan (late Tonian); Qb (52, 56)


Province: 
Guizhou

Type Locality and Naming

Northeast Guizhou. The Xiajiang Gr was named by Wang Y.L. (Wang Yuelun) in 1936, and published in the Report of Minerals of eastern Guizhou Province (the former Geological Survey of China). The naming sections are located in Zaibian of Congjiang County and Furongba, of Yinjiang County, Guizhou Province.

Synonym: (下江群)


Lithology and Thickness

The Xiajiang Gr is subdivided into six formations in SE Guizhou, from bottom to top: (Guiyan Fm), Jialu Fm, Niaoye Fm, Fanzhao Fm, Zhangjiaba Fm, Qingshuijiang Fm, Pinglue Fm and Longli Fm. In NE Guizhou, the upper three formations are absent, and the lowest formation (below the Jialu) is indicated as a Furongba Fm. The group consists mainly of slightly metamorphosed sandstone and shale, tuffaceous sandstone and minor carbonate rocks. The thickness northwest of Fanjing Mountain is about 4500 m. The thickness in southeast Guizhou is over 10,000 m.

[Figure: The Stratigraphic column of the Xiajiang Gr. in Guizhou Province. A-Volcanic ash beds in the Jialu Fm and zircons from the ash bed.]


Lithology Pattern: 
Clayey sandstone


Relationships and Distribution

Lower contact

The group is unconformable with the underlying Fanjingshan Gr (Duyangtang Fm)

and Sipu Gr

Upper contact

The group is overlain by earliest Nanhuan (Liangjiche Fm in NE Guizhou; Chang'an Fm in SE Guizhou).

Regional extent

East Guizhou. The group is well developed in the east part of Guizhou, with the thickness and volcanic rocks increasing southwards, and fluvial sediments gradually increasing.


GeoJSON

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Fossils

Some microplants have been found in the Xiajiang Gr


Age 

Late Qingbaikouan (late Tonian) on schematic stratigraphic section.

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

It is interpreted as a suite of shallow-sea sediments from shelf to slope.


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.