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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]

Vertebrate paleofauna

See also

References

  1. ^ a b 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.
  3. ^ "Table 13.1," in Weishampel, et al. (2004). Page 268.
  4. ^ "Table 17.1," in Weishampel, et al. (2004). Page 364.
  5. ^ Shi-Chao Xu, Hai-Lu You, Jia-Wei Wang, Suo-Zhu Wang, Jian Yi and Lei Yia (2016). "A new hadrosauroid dinosaur from the Late Cretaceous of Tianzhen, Shanxi Province, China". Vertebrata PalAsiatica. in press.
  6. ^ "Table 17.1," in Weishampel, et al. (2004). Page 368.
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