Tutbulak Fm
Type Locality and Naming
In the city of Tutbulak, on the left bank of the Saubulak River in its lower course, on the northern slope of the Kuramin Range. I.M. Nigmadjanov et al., 1992. Stratotype in the area of the summit of Mount Tutbulak.
Synonym: Tutbulakskaya Suite, Тутбулакская св.
Lithology and Thickness
Gray to black, medium- to thick-bedded, organogenic-detrital, detrital-crinoidal, brachiopod-detrital limestones. In the lower and middle parts, siliceous inclusions of grayish-brown and black color in the form of nodules, lenses, and layers, the quantity of which in some places reaches 40% of the volume of the rock. Thickness 140-200m.
Relationships and Distribution
Lower contact
Lies with angular and stratigraphic unconformity on the Kulbatin Fm
Upper contact
It is conformably overlain by the Saukbulak Fm
Regional extent
Northern slope of the Kuramin Range, between the Kyzata and Urgaz rivers.
GeoJSON
Fossils
In the upper parts - accumulations (banks) of numerous paleochoristites. Contains brachiopods - Palaeochoristites desinuatus (Lis.), P. čatkalicus (Dik.), Camarotoechia cf. rowleyi Well.; foraminifers - Parathurammina cushmani Sul., Eotuberitina maljavkini (Reitl.), Endothyra latispiralis Lip., conodonts - Siphonodella duplicata (B. et M.), S. isosticha (Coop.), Neopolygnathus communis (B. et M.).
Age
Depositional setting
Additional Information