Huiquanpu Formation

Huiquanpu Formation
Stratigraphic range: Cenomanian-Campanian
~99–71 Ma
TypeGeological formation
UnderliesMiddle Miocene basalt
OverliesArchean gneiss basement
ThicknessOver 200 m (660 ft)
Lithology
PrimaryMudstone
OtherConglomerate
Location
Coordinates40°18′N 114°12′E / 40.3°N 114.2°E / 40.3; 114.2
Approximate paleocoordinates40°24′N 104°24′E / 40.4°N 104.4°E / 40.4; 104.4
RegionHebei & Shanxi Provinces
Country China
Huiquanpu Formation is located in China
Huiquanpu Formation
Huiquanpu Formation (China)
Huiquanpu Formation is located in Shanxi
Huiquanpu Formation
Huiquanpu Formation (Shanxi)

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]

  1. ^ Xiao-chun, Wu; Jian-Ru, Shi; Li-Yang, Dong; Carr, Thomas D.; Jian, Yi; Shi-Chao, Xu (December 2019). "A new tyrannosauroid from the Upper Cretaceous of Shanxi, China". Cretaceous Research. 108: 104357. doi:10.1016/j.cretres.2019.104357.
  2. ^ Weishampel, David B; et al. (2004). "Dinosaur distribution (Late Cretaceous, Asia)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 593-600. ISBN 0-520-24209-2.