Hajirbulak Fm
Type Locality and Naming
Includes in Dushanbe-west Shirkent-Luchob, east Shirkent-Luchob. It was identified in 1941 by E. M. Golovin (Bensch, 1969).
Synonym: Hajirbulakskaya Suite, Хаджирбулакская свита
Reference section:
Lithology and Thickness
It consists of greenstone spilites, diabases, and their tuffs, containing lenses of limestones, siltstones, sandstones. The incomplete thickness is 200 m, and beyond the republic, the thickness of the suite reaches 1000 m.
Relationships and Distribution
Lower contact
The bottoms of the suite in the valley of the Luchob River are not exposed; in the southwestern spurs of the Gissar, it conformably lies on the Middle Visean
Upper contact
The Hajirbulak Fm (Хаджирбулакокая Свита) is overlain conformably by the Lower Bashkirian Suffin Fm (суффинской свитой).
Regional extent
It is developed in the Dushanbe region on a small area in the valley of the Luchob River.
GeoJSON
Fossils
Outside the territory of Tajikistan, in the Hajirbulak suite, F.R. Bensh (1969) found remains of Upper Namurian (Serpukhovian) Goniatites and foraminifera.
Age
Depositional setting
Additional Information