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Cretaceous
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Denytangga Formation

Denytangga Fm


Period: 
Silurian

Age Interval: 
Llandovery of Silurian(S1), (37)


Province: 
Xizang (Tibet)

Type Locality and Naming

It was proposed by the Xizang Zizhiqu Party of Comprehensive Reconnaissance Survey in 1980. The type section is located at the ridge, west of the road about 12 km north of Yunzhug Township in Xianza County, Xizang Zizhiqu.

Synonym: (德乌卡下组)


Lithology and Thickness

Lower part, 40 m thick, consists of interbeds of black graptolite shale with black bioclastic limestone. Upper part, approximately 50 m in thickness, is composed of yellow mudstone intercalated with purplish brown calcareous shale.


Lithology Pattern: 
Pelagic marl


Relationships and Distribution

Lower contact

The formation conformably contacts onto the underlying Riajiaoobuduo Fm of the Upper Ordovician (not in Ordov lexicon entries); regionally, the next older unit is the Xialazi Fm of upper Ordovician.

Upper contact

The formation conformably contacts with the overlying Zhanongema Fm

Regional extent

It is extremely restricted in distribution, as its exposures observed merely at the type section locality.


GeoJSON

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Fossils

The lower part of the formation is rich in graptolite of Normalograptus persculptus zone and the Parakidograptus acuminatus zone. The upper part, yields abundant graptolite of the Orthograptus vesiculosus zone, Pristiograptus cyphus zone, P. gregarius zone, Oktavites communis zone and Spirograptus turriculatus zone; and conodont of the Pterospathodus celloni zone.


Age 

Graptolite of 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: 
Gorstian

    Fraction up in the ending stage: 
0.0

    Ending date (Ma):  
426.74

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Wang Chuanshang and Wang Xiaofeng