Huiquanpu Formation | |
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Stratigraphic range: Cenomanian-Campanian ~ | |
Type | Geological formation |
Underlies | Middle Miocene basalt |
Overlies | Archean gneiss basement |
Thickness | Over 200 m (660 ft) |
Lithology | |
Primary | Mudstone |
Other | Conglomerate |
Location | |
Coordinates | 40°18′N 114°12′E / 40.3°N 114.2°E |
Approximate paleocoordinates | 40°24′N 104°24′E / 40.4°N 104.4°E |
Region | Hebei & Shanxi Provinces |
Country | China |
The Huiquanpu Formation (simplified Chinese: 灰泉堡组; traditional Chinese: 灰泉堡組; pinyin: Huīquánpù Zǔ) is a geological formation in Shanxi and Hebei provinces, China, whose strata date back to the Late Cretaceous period. It predominantly consists of purple-red mudstone, with subordinate grey-white sandy conglomerates.[1]
Dinosaur remains are among the fossils that have been recovered from the formation.[2]