Irtash Fm
Type Locality and Naming
Along the Irtashsai, a left tributary of the Angren River, Prishchekent District. B.I. Pinhasov, 1985 (145, p.37). The stratotype is the Tashsai section on the Angren Plateau.
Synonym: Irtash Formation, Ирташская св.
Lithology and Thickness
Consists of hills (2-7m) of pale-pink nodular marls and concretionary limestones, representing ancient carbonate weathering crusts, interbedded with proluvial-deluvial red-brown debris siltstones, sandstones, and coarse-clastic rocks. Thickness up to 50 m.
Relationships and Distribution
Lower contact
In depressions, the carbonate crust lies between red-colored Oligocene-Miocene and brown-colored Upper Pliocene molasses. In the marginal parts of depressions and watersheds, it lies on the leveled Paleozoic. L.D. Anpleeva (Koloyarov et al., 1977) included the carbonate weathering crust thickness, developed on the Angren Plateau, in the Middle Miocene Arashan Fm
Upper contact
With erosion, it is overlain by the Gidzhal Fm and Pskent Fm
Regional extent
Angren Plateau, Chirchik River valley, Prishchekent Depression. F.P. Korsakov (166) includes the nodular limestones in the upper part of the red-colored Chulin Fm of the Prishchekent District.
GeoJSON
Fossils
Age
Depositional setting
Additional Information