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Renheqiao Formation

Renheqiao Fm


Period: 
Silurian

Age Interval: 
the Llandovery of Silurian (S1), (38)


Province: 
Yunnan

Type Locality and Naming

The name was proposed by Sun Yunzhu and Situ Suiqin in 1947. The type section is located at west of Renheqiao, 7 km northwest of the Shidian County seat, Yunnan Province.

Synonym: (仁和桥组); Jenhochiao Fm


Lithology and Thickness

The formation consists of gray, grayish black carbonaceous silty shale with marl lenses partings. It is over 252 m in thickness.


Lithology Pattern: 
Claystone


Relationships and Distribution

Lower contact

The formation rests conformably onto the underlying Wanyaoshu Fm of Upper Ordovician.

Upper contact

The formation rests conformably below the overlying Lichaiba Fm

Regional extent

It is steady in lithology and is widely exposed in western Yunnan Province in the exposed thickness ranging from 49-457 m.


GeoJSON

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Fossils

It yields rich graptolites, in ascending order namely being: the Glyptograptus persculptus zone, the Parakidograptus-Diplograptus modestus zone, the Orthograptus vesiculosus zone, the Pristiograptus cyphus-Pristiograptus leei zone, the Demirastrites triangulates-Pristiograptus gregarias zone, the Demerastrites convolutes zone, the Monograptus sedgwickii zone, the Spirograptus turriculatus zone, the Monograptus crispus zone, the Monoclimacis griestoniensis zone and the Oktavites spiralis zone.


Age 

Graptolite of Glyptograptus (=Normalograptus) persculptus zone implies extends into Hirnantian of uppermost Ordovician

Age Span: 

    Beginning stage: 
Hirnantian

    Fraction up in beginning stage: 
0.5

    Beginning date (Ma): 
444.14

    Ending stage: 
Sheinwoodian

    Fraction up in the ending stage: 
0.0

    Ending date (Ma):  
432.93

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Wang Chuanshang and Wang Xiaofeng