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Cretaceous
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Devonian
Silurian
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Nanshimengou Formation

Nanshimengou Fm


Period: 
Silurian

Age Interval: 
Pridoli of Silurian (S1), (39, 40)


Province: 
Gansu

Type Locality and Naming

It was named by Fu Lipu et al in 1983. The type section is located at Nanshimengou, Zhouqu County, Gansu Province.

Synonym: (南石门沟组)


Lithology and Thickness

The formation, 69 m thick, consists of dark gray, gray green phyllite intercalated with limestone, thin-bedded limestone or limestone lenses.


Lithology Pattern: 
Shallow-marine marl


Relationships and Distribution

Lower contact

The formation rests conformably onto the underlying Hongshuigou Fm (Hongshuigoukou Fm)

Upper contact

The formation rests conformably below the overlying Xiaputonggou Fm of earliest Devonian

Regional extent

The lithology and the thickness of the formation vary considerably. In the east part of its exposed area, it is dominated by clastic rock in Zhouqu and is 37 m thick at the Xiaolianggou section. In west, it is mainly composed of carbonate rock with increased thickness, 177 m thick at Yanglugou, 117 m at Zuokuowu in Têwo County, and 110 m at Xiawunagou.


GeoJSON

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Fossils

It yields anthozoa Squameofavosites sokolovi, Emmonsiella saaminicus, Favosites fungites, Laceripora dictyosa, Denaphyllum sp., Charsakia sp. etc.; brachiopods Atrypoidea sp., Gannania sp., Retziella latiplicata; conodonts Ozarkodina crispa, Ligonodina elegans, trilobite Encrinurus sp.; cephalopods Xiaoxiangoceras sp., Heyuncunoceras sp., etc.


Age 


Age Span: 

    Beginning stage: 
Pridoli

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
422.73

    Ending stage: 
Pridoli

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
419.00

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Wang Chuanshang and Wang Xiaofeng