| 词条 | Shendi Formation |
| 释义 |
| name = Shendi Formation | image = | caption = | type = Geological formation | age = {{Fossilrange|Campanian|Maastrichtian}} | period = Maastrichtian | prilithology = Sandstone, siltstone, mudstone | otherlithology = | namedfor = | namedby = | region = Northern State | country = {{flag|Sudan}} | coordinates = | unitof = | subunits = | underlies = | overlies = | thickness = | extent = | area = | map = | map_caption = }} The Shendi Formation is a Late Cretaceous geologic formation. Indeterminate Theropod remains have been recovered from it.[1] As well as those of the dyrosaurid Hyposaurus. It consists of a lower unit of fine grained meandering channel sediments, separated by an erosive contact with overlying meandering to braided river channel sandstones.[2] See also{{Portal|Geology|Paleontology|Dinosaurs|Cretaceous|Prehistory of Africa}}
References1. ^Weishampel, et al. (2004). "Dinosaur distribution" Pp. 517-607. in Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 pp. {{ISBN|0-520-24209-2}}. " Pp. 517-607. {{Africa-geologic-formation-stub}}2. ^{{Cite journal|last=Salih|first=Khalaf Allah O.|last2=Evans|first2=David C.|last3=Bussert|first3=Robert|last4=Klein|first4=Nicole|last5=Nafi|first5=Mutwakil|last6=Müller|first6=Johannes|date=2015-12-30|title=First record ofHyposaurus(Dyrosauridae, Crocodyliformes) from the Upper Cretaceous Shendi Formation of Sudan|journal=Journal of Vertebrate Paleontology|language=en|volume=36|issue=1|pages=e1115408|doi=10.1080/02724634.2016.1115408|issn=0272-4634}} 7 : Geologic formations of Sudan|Cretaceous System of Africa|Campanian Stage|Maastrichtian Stage|Sandstone formations|Siltstone formations|Mudstone formations |
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