Kyzylatin Fm
Type Locality and Naming
Along the Kyzyltal and Kyzylata rivers, Pre-Tashkent Chul. G.A. Belenky, 1966 (96, pp.99-100). Stratotype in the headwaters of the Kelif River, on the right bank of the Kyzylata River, in the foothills of the Karzhantau range.
Synonym: Kyzylatinskaya Formation, Кызылатинская св.
Lithology and Thickness
Consists of two formations: variegated and pink. Lower formation - variegated, spotted, bluish-green, reddish-brown sandstones and siltstone (aleurolites); upper formation - pink sandstones and siltstone (aleurolites). Thickness 14-350m.
Relationships and Distribution
Lower contact
Lies unconformably on the Azatbash Fm or transgressively on the Paleozoic
Upper contact
It is overlain with erosion by the Akdachin Fm.
Regional extent
Pre-Tashkent Chul, foothills of the Chatkal and Karzhantau ranges, in the Tashkent depression, revealed by drilling. Along A., - to the Albian and is correlated with the Kyzylpilyal Fm of South Ferghana. Along O.A. Fedorenko et al. (478), corresponds to the Kekpenkaldyk Fm of the North Kyzylkum
GeoJSON
Fossils
Contains ostracods - Cypridea inornata Peck., Timiriasevia costata Gal., T. simakovi Mand., charophyte algae - Atopachara trivolvis Peck.
Age
Depositional setting
Additional Information