| Xiguayuan Formation | |
|---|---|
|  Stratigraphic range: Barremian  ~  | |
| Type | Geological formation | 
| Underlies | Quaternary sediments | 
| Overlies | Zhangjiakou Formation | 
| Thickness | Up to 2,500 m (8,200 ft) | 
| Lithology | |
| Primary | Conglomerate, sandstone, siltstone, mudstone | 
| Other | Volcanic and pyroclastic sediments | 
| Location | |
| Coordinates | 45°54′N117°18′E / 45.9°N 117.3°E | 
| Approximate paleocoordinates | 48°48′N117°24′E / 48.8°N 117.4°E | 
| Region | Hebei | 
| Country | China | 
The Xiguayuan Formation is an Early Cretaceous (Barremian) geologic formation in Hebei Province of China. Fossil ornithopod tracks have been reported from the formation. [1] It was deposited in a shallow lacustrine setting and is noted for its hyperpycnite facies. [2]
The formation has provided the following fossils:
{{citation}}:  CS1 maint: publisher location (link)