Qigu Formation | |
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Stratigraphic range: Oxfordian-Early Kimmeridgian, | |
Type | Geological formation |
Underlies | Kalaza Formation |
Overlies | Toutunhe Formation (Junggar) Qiketai Formation (equivalent unit in the Turpan Basin) |
Thickness | Over 520 m (1,710 ft) |
Lithology | |
Primary | Siltstone, sandstone |
Location | |
Coordinates | 43°36′N 87°18′E / 43.6°N 87.3°E |
Approximate paleocoordinates | 42°54′N 97°30′E / 42.9°N 97.5°E |
Region | Xinjiang |
Country | China |
Extent | Southern Junggar Basin (blue) Turpan Basin (disputed) (cyan) |
The Qigu Formation is a Late Jurassic (Oxfordian) geologic formation in the Southern Junggar Basin in China. Indeterminate Dinosaur remains are among the fossils that have been recovered from the formation, including theropod teeth and a fibula.[1] a stegosaur dorsal vertebra[2] and a Eusauropod tooth.[3] Xinjiangtitan was erroneously thought to be from this formation, but it is actually from the older Qiketai Formation, which is in a different basin.[4] The term "Qigu Formation" is also used to sediments of equivalent age in the Turpan Basin, but this might better be treated as a separate formation. It is laterally equivalent to the Shishugou Formation.