Keltemashat Fm
Type Locality and Naming
Along the Kelytemashat River, Koykebiltay Mountain, western part of the Talas Alatau ridge, O.I. Sergun'kova, 1959 (382, p. 64). Stratotype on the southern slope of Koykebiltay Mountain, right bank of the upper reaches of the Kelytemashat River. Upper formation in Ugam Gr
Synonym: Keltemahashat Suite, Keltmashatskaya suite, Кельтемашатская св.
Lithology and Thickness
Limestones are layered, predominantly medium-layered, organogenic, organogenic-detrital, detrital-slime, locally oolitic, with the presence of siliceous nodules. Characteristic feature - the presence of numerous shell layers consisting of thin-walled brachiopod shells. Thickness 160-260m up to 300 m.
Relationships and Distribution
Lower contact
Lies conformably on the Mashat Fm
Upper contact
It is conformably overlain by the Koykebiltau Fm (Talas Alatau ridge), Nauvalin Fm (Ugam, Pskem ridge) or Dzhegirgen Fm (Karjantau, northern slope of the Chatkal ridge) suite (Tkachev et al., 1992ф.; 1996ф.; 439; 460).
Regional extent
Throughout the Chatkal region.
GeoJSON
Fossils
Contains brachiopods - Striatifera angusta Jan., S. striata Fisch.; foraminifera - Eostaffella protvae (Raus.), Eosigmoilina minima Br., Globivalvulina moderata Reitl.; conodonts - Gnathodus bilineatus bollandensis Hig., Lochriea cruciformis (Clarke)
Age
Depositional setting
Additional Information