Akbulak-Carb-L Fm
Type Locality and Naming
Along the Akbulak River, left tributary of the Chatkal River, Chatkal ridge. I.M. Nigmadzhanov in 1986. Stratotype in the lower reaches of the Akbulak River.
Synonym: Akbulakskaya Svita, Акбулакская св.
Lithology and Thickness
Light gray, massive-thick-bedded limestones, strongly recrystallized, locally to marbles. The suite includes reef and biogenic mounds of the "Akbulak" type, tracing the northern lateral boundary of the suite thickness from 100-120 m in sections where organic buildups are absent, to 400-500 m, where they appear.
Relationships and Distribution
Lower contact
With angular unconformity and conglomerate-breccias at the base, it lies on the Chavatin Fm
Upper contact
The diachroneity of the upper boundary is established within the conodont zones crenulata and punctatus. And is conformably overlain by the Kulosyn Fm
Regional extent
Predominantly Chatkal Range, basin of left tributaries of the Chatkal River, Akbulak, Mazar-Sai, and Sargardon rivers. Laterally to the north, it transitions into the Koksuy Fm. Previously, the deposits of the A. suite were attributed to the Temirbastau Fm, Sargardon Fm, or combined Temirbastau Fm and Sargardon Fm.
GeoJSON
Fossils
Contains conodonts - Siphonodella duplicata (B. et M.), S. obsoleta Hass., Gnathodus punctatus (Coop.); brachiopods - Leptagonia analoga Phill., Camarotoechia cf. elegantula Row.
Age
Depositional setting
Additional Information