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Dianbei Formation

Dianbei Fm


Period: 
Silurian

Age Interval: 
lower to middle Aeronian of Llandovery (S1), (60, 61)


Province: 
Jiangxi, Hubei

Type Locality and Naming

It is named by the Jiangxi Party of Regional Geological Survey in 1963. The type section is at Dianbei of Chuantan, north of the Wuning County seat in Jiangxi Province. It was first quoted by the Jiangxi Bureau of Geology and Mineral Resources in 1984.

Synonym: (殿背组)


Lithology and Thickness

It is 735 m in thickness, consisted by grey green, yellow green sandy shale, siltstone and mudstone intercalated with sandstone; there is a thin bed of quartz sandstone with ripple marks at the base of the formation.


Lithology Pattern: 
Sandy claystone


Relationships and Distribution

Lower contact

The formation conformably contacts with the underlying Lishuwo Fm of the uppermost Ordovician-Early Ordovician.

Upper contact

The formation conformably contacts with the overlying Qingshui Fm

Regional extent

It is exposed in northwest Jiangxi to southeast Hubei.


GeoJSON

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Fossils

It yields rare fossils. The bivalve Modiolopsis, Modiomorpha and trilobite Latiproetus are the only finds in the formation.


Age 


Age Span: 

    Beginning stage: 
Aeronian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
440.49

    Ending stage: 
Aeronian

    Fraction up in the ending stage: 
0.75

    Ending date (Ma):  
439.07

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Wang Chuanshang and Wang Xiaofeng