Zitai Formation

The Zitai or Zhitai Formation[1][2] is a geological sequence of Middle Ordovician origin, that occurs along the southeastern edge of the Yangtze Platform in southern China. It is a purple-red limestone with a few interspersed yellow-green shale beds. It contains a fossil fauna dominated by trilobites and nautiloids.

Zitai Formation
Stratigraphic range: Floian-Dapingian
~478–468 Ma
TypeGeological formation
Lithology
PrimaryLimestone
Location
Coordinates30.3°N 117.4°E / 30.3; 117.4
Approximate paleocoordinates8.7°N 134.3°W / 8.7; -134.3
RegionAnhui, Hubei, Hunan
Country China
Zitai Formation (China)

References

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