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Qiangshari Formation

Qiangshari Fm


Period: 
Silurian

Age Interval: 
Telychian of Llandovery (S1), (35)


Province: 
Xizang (Tibet)

Type Locality and Naming

It was named by Lin Baoyu in 1989. The type section is located at the southwest slope, approximately 1 km southeast of Kede Village, Pazhuo District, Dingri County, Xizang Zizhiqu. Xia Daixiang et al. (1997) regarded this formation as synonym with Shiqipo Fm. We retain this formation herein tentatively for further investigation.

Synonym: (强莎日组)


Lithology and Thickness

Lower part, 5 m in thickness, consists of gray thick-bedded argillaceous banded limestone. Upper part, about 2 m thick, is composed of grayish violet thin-layered shale intercalated with brown thin-bedded limestone. The thickness varies considerably and may reach up to 22.5 m.


Lithology Pattern: 
Clayey limestone


Relationships and Distribution

Lower contact

The formation rests conformably in between the underlying Zhagaqu Fm

Upper contact

The formation rests conformably in between the overlying Kede Fm

Regional extent

It is distributed at Dingjie to southern Dingri County.


GeoJSON

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Fossils

In the lower part, it yields rich conodont Pterospathodus amorphognathoides, P.pennatus procerus, Kockelella ranuliformis; cephalopod Xizhangoceras diviense, Michelinoceras? inflatum;and graptolite Monograptus priodon, etc. In the upper part, it bears graptolites Monograptus priodon, M. acus, Oktavites spiralis, Pristiograptus hisingeri; cephalopods Kionioceras himalayaense, Euthyocycloceras sp., etc.


Age 


Age Span: 

    Beginning stage: 
Telychian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
438.59

    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