Kansay Fm
Type Locality and Naming
At Kansay, N. Nuratau Ridge. R.R. Usmakov in 1993 (Korsakov et al., 1993).
Synonym: Kansay Suite, Кансайская св.
Lithology and Thickness
Lower part of the section, mica-quartz, quartz-mica-sericite-chlorite slates predominate, representing metamorphosed siltstone (aleurolites) and pelites in the stilpnomelane-chlorite-muscovite subfacies.
Middle and Upper parts of the section are composed of clay-mica slates, alternating with siltstone (aleurolites), sandstones, and layers (up to 1 m) of gravelites.
Total formation thickness is more than 1000 m.
Relationships and Distribution
Lower contact
The conditional Vendian-Lower Cambrian age is established (by R.R. Usmakov) based on stratigraphic position between the late Riphean deposits of the Suvliksay Fm
Upper contact
The overlying Zhivachisay Fm of the Middle-Upper Cambrian, characterized by organic remains.
Regional extent
Predominantly in the western part of the N. Nuratau Ridge. It is correlated with the Khodzhaakhmet Fm and Kurghantau Fm
GeoJSON
Fossils
Age
Depositional setting
Additional Information