Akbulak-Carb Fm
Type Locality and Naming
Along the Akbulak stream, Dzhalair Ridge, northern slope of the Turkestan Range. Z.S. Rumyantseva, 1973 (387, p. 77). Stratotype along the Akbulak stream near the spring.
Synonym: Akbulak Formation, Акбулакская св.
Lithology and Thickness
Spotted detrital-oncolitic, algal–foraminiferal limestones containing siliceous concretions and nodules. At the base of the formation, bauxites are locally developed with thickness from a few centimeters to 8–10 m, or a unit 4.5 m thick of reddish-brown gravelstones, sandstones, and siltstones. Total thickness: 40–85 m.
Relationships and Distribution
Lower contact
It transgressively overlies the limestones of the Sulyuktin Fm
Upper contact
It is transgressively overlain by the limestones of the Ramazan Fm (165; 439).
Regional extent
Northern slope of the Turkestan Range, Dzhalair Ridge.
GeoJSON
Fossils
Contains foraminifera: Eostaffella jachakia Rum., E. angusta (Kir.), E. (Eostaffelina) protvae (Raus.), Millerella carbonica Grozd. and Leb., M. uralica Kir., Novella primitiva Raus., Pseudostaffella antiqua (Dutk.), P. cf. varsanofievae Raus., P. inconstans (Reitl.), Asteroarchaediscus ex gr. baschkiricus (Krest. and Theod.), and others.
Age
Depositional setting
Additional Information