Ermaying Formation
The Ermaying Formation is a sedimentary succession of Anisian (Middle Triassic) age. It is found in the Shaanxi Province of China.[1] It is composed of an up to 600 m thick sequence of mudstone and sandstone.[2] It is famous for its fossils of tetrapods.[2]
| Ermaying Formation | |
|---|---|
| Stratigraphic range: Anisian ~ | |
| Type | Geological formation | 
| Sub-units | Two Members | 
| Underlies | Tongchuan & Xingshikou Formations | 
| Overlies | Liujiagou Formation | 
| Thickness | Up to 600 metres (2,000 ft) | 
| Lithology | |
| Primary | Mudstone, sandstone | 
| Other | Tuff | 
| Location | |
| Coordinates | 37°26′15″N 110°39′06″E | 
| Approximate paleocoordinates | 38.2°N 90.5°E | 
| Region | Shaanxi, Shanxi, Inner Mongolia | 
| Country |  China | 
|   Ermaying Formation (China)   Ermaying Formation (Shanxi) | |
Fossil content
    
Notable fossils include the genera Fenhosuchus, Eumetabolodon, Halazhaisuchus, Guchengosuchus, Neoprocolophon, Ordosiodon, Wangisuchus and Shansisuchus.
References
    
    
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