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Nuoco Formation

Nuoco Fm


Period: 
Carboniferous

Age Interval: 
C1 (64), Tournaisian and Visean (Early Carboniferous)


Province: 
Xizang (Tibet)

Type Locality and Naming

The type section lies at Dongbei Hill on the north end of Nuo Co (a glacial lake) west of Lagu Village, Baxoi County, Tibet. It was named by Yin Jixiang in 1984.


Lithology and Thickness

Claystone, Sandstone and Clayey Limestone. Clastic rock (lower part) and carbonate rock (upper part) formations. The Lower Member is composed of gray silty slate, intercalated with fine-grained sandstone and slate interbedded with gray slate and fine-grained sandstone, 250 m thick. The Upper Member consists of gray medium to thick-bedded clayey limestone, purple porphyritic clayey limestone or nodular limestone, with small pyrite crystals and suture structures, 31 m thick.


Lithology Pattern: 
Sandy limestone


Relationships and Distribution

Lower contact

Conformable contact with the underlying Upper Devonian Songzong Group (Dev column 25)

Upper contact

Conformable contact with the overlying Lagu Fm

Regional extent

Distributed along Risongzong and Charidong of Bowo, and Yaze to Lagu of Baxoi.


GeoJSON

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Fossils

Lower Member yields Brachiopods Fusella cf. tornacensis, Marginatia sp. and Tylothyris pseudoposterrus; Bryozoan Fenestella cf. donaica; trilobites Cyrtosymbole sp., Ditomopyge sp. and Neoproetus sp.; Bivalves Phestia sp. and Dunbarella sp., crinoid stem Pentagonocyclicus sp., etc. Upper Member contains Ammonoid Beyrichoceratoides sp.,


Age 

Lower Member belongs to the Tournaisian, and the Upper Member the Visean.

Age Span: 

    Beginning stage: 
Tournaisian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
359.30

    Ending stage: 
Serpukhovian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
323.40

Depositional setting

It is interpreted as a


Depositional pattern:  


Additional Information


Compiler:  

Fan Yingnian