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Cenozoic
Cretaceous
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Permian
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Nanzha Formation

Nanzha Fm


Period: 
Permian

Age Interval: 
P1 (26), Artinskian Stage (mid-Cisuralian Epoch; mid-Early Permian)


Province: 
Xinjiang

Type Locality and Naming

The type section is located at Xiaohaizi, Bachu County, Xinjiang.It was named by Xiong Jianfei in 1991.


Lithology and Thickness

Limestone. Composed of grey medium- and thick-bedded micrite, intercalated with calcareous shale. Thickness is about 80 m


Lithology Pattern: 
Clayey limestone


Relationships and Distribution

Lower contact

Disconformable contact is inferred with the underlying Xiaohaizi Fm of the Carboniferous System because of an indistinct difference in lithology between them and the lacking in the strata of the Kasimovian, Gzhelian and part of Moscovian Stages of the Late Carboniferous Epoch. However, Carboniferous Lexicon for Xiaohaizi Fm assigns it to the Kasimovian-Gzhelian (and into earliest Permian), which implies that these uppermost Carboniferous Stages are present.

Upper contact

Conformable contact with the siltstone layer at the base of the overlying Aqia Gr.

Regional extent


GeoJSON

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Fossils

Fusulinida fossils represented by the Eoparafusulina-Sphaeroschwagerina-Nankinella assemblage, and Conodonts represented by the Sweetognathus whitei-Neostreptognathodus pequopensis assemblage.


Age 

Chuanshanian Epoch. Conodonts imply Artinskian Stage (mid-Cisuralian Epoch; mid-Early Permian)

Age Span: 

    Beginning stage: 
Asselian

    Fraction up in beginning stage: 
0.5

    Beginning date (Ma): 
296.21

    Ending stage: 
Artinskian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
283.30

Depositional setting

It is interpreted as a shallow-sea platform facies.


Depositional pattern:  


Additional Information


Compiler:  

Shang Qinghua