Changi Fm
Type Locality and Naming
Along the village of Changi, Parkent district, foothills of the Chatkal Range. V.V. Kurbatov in 1989; V.I. Troitsky, V.V. Kurbatov, 1998 (165, p.127). Stratotype along borehole 1 Kyzylkisaksay, village of Changi. Parastratotype at the Karankul pass.
Synonym: Changi Suite, Чангиская св.
Lithology and Thickness
Variegated breccias, conglomerates, gravelites, sandstones (on kaolinite cement), clays, siltstone (aleurolites), and one or two layers of bauxite-like rocks, characterizing deposits of a lake and alluvial plain. Thickness 6-145m.
Relationships and Distribution
Lower contact
The suite transgressively overlies the Paleozoic
Upper contact
It is also overlain by the Angren or Azatbash suite.
Regional extent
Exposed in discontinuous outcrops in the Chatkal-Kuramin Mountains (Changi, Karankul, Aksagat) and intersected by boreholes in the Parkent district, Angren coal mine, and Prishakhtinsky Chuly. Previously distinguished as the Mansuratin Fm
GeoJSON
Fossils
Organic remains not found.
Age
Depositional setting
Additional Information