Bissekty Formation

Bissekty Formation
Stratigraphic range: Mid-Late Turonian
~92–90 Ma
TypeGeological formation
UnderliesAitym Formation
OverliesDzheirantui Formation
Thicknessup to 80 m (260 ft)
Lithology
PrimarySandstone
OtherConglomerate, mudstone, siltstone
Location
Coordinates42°06′N 62°42′E / 42.1°N 62.7°E / 42.1; 62.7
Approximate paleocoordinates36°48′N 57°00′E / 36.8°N 57.0°E / 36.8; 57.0
RegionNavoiy & Xorazm Regions
Country Uzbekistan
ExtentKyzylkum Desert
Bissekty Formation is located in Uzbekistan
Bissekty Formation
Bissekty Formation
Bissekty Formation (Uzbekistan)

The Bissekty Formation (sometimes referred to as Bissekt) is a geologic formation and Lagerstätte which crops out in the Kyzyl Kum desert of Uzbekistan, and dates to the Late Cretaceous Period. Laid down in the mid to late Turonian, it is dated to about 92 to 90 Ma (million years ago).[1]

  1. ^ Averianov, Alexander; Sues, Hans-Dieter (April 2012). "Skeletal remains of Tyrannosauroidea (Dinosauria: Theropoda) from the Bissekty Formation (Upper Cretaceous: Turonian) of Uzbekistan". Cretaceous Research. 34: 284–297. Bibcode:2012CrRes..34..284A. doi:10.1016/j.cretres.2011.11.009. ISSN 0195-6671.