Home Multi-Country Search About Admin Login
Cenozoic
Cretaceous
Jurassic
Triassic
Permian
Carboniferous
Devonian
Silurian
Ordovician
Cambrian
Neoproterozoic
Mesoproterozoic

Search by
Select Region(s) to search
Hold Ctrl (Windows/Linux) or Command (Mac) to select multiple
Shuixiakou Formation

Shuixiakou Fm


Period: 
Permian

Age Interval: 
P (70), Capitanian Stage (late Guadalupian Epoch; late-Middle Permian)


Province: 
Shaanxi

Type Locality and Naming

The type section is located at Shuixiakou of the Yudoutan area 35 km to the southeast of the Zhenan County Town, Shaanxi Province. It was named by Chinese Academy of Geological Sciences in 1963.


Lithology and Thickness

Shale and Limestone. Its basal part is composed of black shale and sandy shale. Lower part is composed of dark-grey medium-bedded micritic siliceous limestone, intercalated with thin-bedded limestone and shale. Upper part is composed of black thin-bedded siliceous micrite, intercalated with yellow-green medium-bedded calcareous quartz-sandstone and sandy shale. Thickness is 397.5 m.


Lithology Pattern: 
Siliceous limestone


Relationships and Distribution

Lower contact

Conformable contact with the grey-white limestone at the top of the underlying Maokou Fm (Wulipo Fm).

Upper contact

Conformable contact with the dark-grey massive limestone and clayey limestone at the base of the overlying Xikou Fm

Regional extent

Distributed in the Xikou area-Yundoutan area of the Zhenan County, Shaanxi Province, meanwhile in the area of the Yunxi County of Hubei Province its thickness reaches as great as 613 m.


GeoJSON

null

Fossils

Yields Fusulinid fossils represented by Metadoliolina shanxiensis, M. lepida, Neoschwagerina douvillei, Yabeina shiraiwensis, Y. gubleri, etc.; Brachiopods such as Monticulifera zhenanensis, M. sipensis, Neoplicatifera huangi, Tyloplecta nankingensis; and Corals such as Tachylasma magnum, Allotropiophyllum sinensis.


Age 

The stratigraphic horizon of the formation is corresponding to that of the upper part of the Maokou Fm, belonging to the Lengwuan Stage of the Yangsingian Epoch = Capitanian Stage (late Guadalupian Epoch; late-Middle Permian)

Age Span: 

    Beginning stage: 
Wordian

    Fraction up in beginning stage: 
0.5

    Beginning date (Ma): 
266.78

    Ending stage: 
Capitanian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
259.55

Depositional setting

It is interpreted as shallow-sea deposits.


Depositional pattern:  


Additional Information


Compiler:  

Fei Shuying, Zhu Zili