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Main source = Abduazimova, Z.M. (Ed.), 2001. Stratigraphic Dictionary of Uzbekistan. IMR (Institute of Mineral Resources), Tashkent, 580 pp. (In Russian) Translated to English by the GeoGPT group, Zhejiang Lab, Hangzhou, China--see About

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Kansay Formation
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Kansay Fm base reconstruction

Kansay Fm


Period: 
Cambrian

Age Interval: 
Vendian-Lower Cambrian (?), N4


Province: 
Nuratau

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.


Lithology Pattern: 
Sandy_claystone


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

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Fossils


Age 

On the State Geol Map-500 of Uzbekistan (460), the Kansay Fm is conditionally referred to the Vendian-Lower Cambrian.

Age Span: 

    Beginning stage: 
Ediacaran

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
635.00

    Ending stage: 
Guzhangian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
497.00

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

R.R. Usmakov – In: GeoGPT translation of: “Abduazimova, Z.M. (Ed.), 2001. Stratigraphic Dictionary of Uzbekistan. IMR (Institute of Mineral Resources), Tashkent, 580 pp. (In Russian)”