词条 | Ilek Formation | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
释义 |
| name = Ilek Formation | image = | caption = | type = Geological formation | age = Lower Cretaceous {{fossilrange|Berriasian|Albian|}} | period = Early Cretaceous | prilithology = Clay, siltstone | otherlithology = Marl, sandstone | namedfor = | namedby = L. A. Ragozin | year_ts = 1935 | region = Western Siberia | country = {{flag|Russia}} | coordinates = {{coord|55.9|N|88.0|E|display=inline,title}} | paleocoordinates = {{coord|54.2|N|84.6|E|display=inline}} | unitof = Kiya River Basin | subunits = | underlies = Kiya Formation | overlies = Tyazhin Formation | thickness = Up to {{Convert|746|m|ft|-1}} | extent = {{flag|Kemerovo Oblast}} | area = | map = {{Location map+ | Russia | relief = 1 | width = 300 | float = center | places = | lat_deg = 55.9 | lon_deg = 88.0 | mark = Green pog.svg | marksize = 10 }} | map_caption = }} The Ilek Formation is a Lower Cretaceous geologic formation in Western Siberia. Many different fossils have been recovered from the formation. It overlies the Late Jurassic Tyazhin Formation and underlies the Albian Kiya Formation.[1] The formation was described by L. A. Ragozin in 1935. It consists of sands with sandstone concretions, layers of silts, clays and marls. Age of the formation, according to a crude 1962 estimate, is Valanginian(?) - Hauterivian - Barremian. Its thickness varies greatly, reaching 746 m in Teguldet borehole.[3] Fauna
See also{{Portal|Earth sciences|Paleontology|Cretaceous|Prehistory of Asia}}
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