Egarbelitau Fm
Type Locality and Naming
By the mountains of Egarbelitau, northern foothills of the N. Nuratau ridge. V.P. Vashchenko et al. in 1990 (Korsakov et al., 1993f). Stratotype to the west of the Kutarma quarry (Korsakov et al., 1993f).
Synonym: Egarbelitauskaya Suite, Егарбелитауская св.
Lithology and Thickness
Thick-bedded, aphinitic, grey limestones, rarely conglomeratic limestones. Thickness more than 300 m.
Relationships and Distribution
Lower contact
With unclear relationships, it overlies the Asmansay Fm
Upper contact
It is conformably overlain by the Kutarmay Fm (Usmanov et al., 1999f.).
Regional extent
Northern foothills of the N. Nuratau ridge, fragmentarily, in tectonic blocks in Egarbelitau, Bozaigyr, Balyklitau. The most complete undisturbed section of the suite was studied by R.R. Usmanov et al. (1999f) at the eastern end of the southern branch of Balyklitau (thalweg of the Kly River).
GeoJSON
Fossils
Contains foraminifers Archaesphaera minima Sul., Parathurammina sp., Bisphaera cf. irregularis Bir., Cribrosphaeroides sp.; tabulates - Favosites ex gr. nikiforovae Chekh., Crassialveolites ex gr. multiperforatus Sub., Caliopora sp.; brachiopods - Stringocephalus burtini Deff.; stromatoporoids - Amphipora ex gr. alveolata Ermak., A. ex gr. vesiculosa Ermak.; conodonts - Pandorinellinae sp. - of Middle Devonian age.
Age
Depositional setting
Additional Information