Zarkuin Fm
Type Locality and Naming
Includes in Dushanbe-west Shirkent-Luchob, east Shirkent-Luchob. It was delineated in 1962 by L.I. Gay and V.P. Loziev. Later, it was studied by F.R. Bensh (1969) and D.A. Starshinin.
Synonym: Zarkuinskaya formation, zаркуинская свита, Zarquin Fm, заркуинской свите.
Reference section:
Lithology and Thickness
It is composed of lavas, tuffs, tuff-breccias of andesite-dacite composition, interbedded with organogenic limestones. The incomplete thickness of the formation is 1200 m.
Relationships and Distribution
Lower contact
Unconformably underlain by Chinar Fm
Upper contact
overlying rocks are unknown.
Regional extent
They are spread in the Dushanbe region in the valley of the river Qafirnigan.
GeoJSON
Fossils
The limestones contain foraminifera of the upper substage of the Bashkirian stage and the lower substage of the Moscow stage, such as Ozawainella mosquensis Raus., Eostaffella parastruvei var. chusovensis Kir., Pseudostaffella compressa Raus., Profusulinella ovata Raus., Pr. prisca (Depr.), and others.
Age
Depositional setting
Additional Information