Akterek Fm
Type Locality and Naming
Along the Akterek River, V. Karachatyr, S. Fergana F.R. Bensh, 1959 (382, p. 74). Stratotype on the left bank of the Dzhingilsai River (Kyrgyzstan).
Synonym: Akterek Suite, Актерекская св., Akterekian suite
Lithology and Thickness
Along F.R. Bensh (110), it is divided into two subsuites. Lower - sandstones, silty claystones, with conglomerates at the base. Thickness 700-720m. Upper - poorly sorted sandstones of various grain sizes, interbedded with siltstone (aleurolites) with lenses and layers of gravelites and conglomerates, less frequently limestones. Thickness 1200-1400m.
Relationships and Distribution
Lower contact
It lies with erosion on different horizons of the Kalmakbulak Fm and Karatangin Fm
Upper contact
It is conformably overlain by the Dzhilginsay Fm
Regional extent
South Fergana, E. Karachatyr, mainly in Kyrgyzstan, locally in Uzbekistan, Marhamat syncline area.
GeoJSON
Fossils
In the lower subsuite - In silty claystones, lenses and layers of clayey and algal-foraminiferal limestones with late Moscovian foraminifera of the Fusulina kamensis-Neostaffella umbilicata (Putrja et Leont.) zone, Ozawainella kurakhovensis Man., O. ex gr. mosquensis Raus., O. pseudoangulata Putrja, Taitzehoella librovitchi (Dutk.), Moellerites aff. paracolaniae (Saf.), Fusulinella tokmovensis Raus. et Dalm., F. praebocki Raus., F. bocki Moell., F, aff. pseudobocki Lee et Chen, F. ex gr. mosquensis Saf., Hemifusulina cf. consobrina Raus., Beedeina pseudoelegans (Chern.), Kamaina cf. kamensis (Saf.), K. ex gr. aspera (Chern.).
Age
Depositional setting
Additional Information