Saukbulak Fm
Type Locality and Naming
Along the Saukbulak river, left tributary of the Akhangaran river, northern slope of the Kuramin ridge. I.M. Nigmadzhanov et al., 1992. Stratotype in the lower reaches of the Urgaz River, left bank, northeastern slope of Urgaz-Karatau.
Synonym: Saukbulak Suite, Саукбулакская св.
Lithology and Thickness
Gray limestones, often with a bluish tint, predominantly medium-bedded, clotted-nodular, clotted-algal, clotted-spheroidal, with rare mud and detritus. Distinguishing feature from overlying and underlying subdivisions - absence of siliceous inclusions and presence of oncoid-like algal formations. Thickness 120-160m.
Relationships and Distribution
Lower contact
Conformably overlies the Tutbulak Fm (lower reaches of the Urgaz and Saubulak rivers) or with stratigraphic unconformity on the Kulyat Fm dolomites (Almalyk River, Kalkanata Mountains).
Upper contact
Conformably overlain by the Sallyatash Fm (Tkachev et al., 1996). (165).
Regional extent
Kuraminsky Ridge, Kalkanata Mountains, Almalyk, Urgaz, Saubulak basins.
GeoJSON
Fossils
Contains foraminifera - Septabrunsiina krainica (Lip.), Endothyra latispiralis Lip., Spinoendothyra kosvensis (Lip.); brachiopods - Composita megala (Toln.), Rugosochonetes sp.; conodonts - Neopolygnathus Carina (Hass.), Eotaphrus bultyncki (Groes.), Clydagnathus cavusvormis R.A. et D.
Age
Depositional setting
Additional Information