Dikzankou Fm
Type Locality and Naming
In the first Darvaz, Muxuy, Karakul, and Central Pamir regions, they are distinguished as an independent stratigraphic subdivision from the composition of the Dikzankouskaya suite (Karapetov, 1960; Sorokin, 1961).
Synonym: Dikzankouskaya suite
Reference section:
Lithology and Thickness
The sediments are represented by gray marly and dolomitic limestones with interlayers of sericite-quartz schists and quartz sandstones. The thickness is 120-700 m.
Relationships and Distribution
Lower contact
The boundaries with the underlying Viskharv Fm and overlying Dikzankou Fm are conformable.
Upper contact
It transgressively overlies on the Kalaykhumb Fm
Regional extent
They are exposed in Darvaz, Muxuy, Karakul, and Central Pamir regions.
GeoJSON
Fossils
These sediments are characterized by findings of Lower Silurian corals Palaeofavosites aff. forbesiformis Sok., P. luhai Sok., Catenipora gothlandica (Yabe), Favosites favosus (Goldf.); Ketophylloides atlassovi grandis Lavrus, and others.
Age
Depositional setting
Additional Information