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Main source = Baratov, R.B., et al. (1976). Subdivisions of stratified and intrusive rocks of Tajikistan. Publishing House "Donish", Dushanbe, 269 pp. plus tables. Provided by Dr. Jovid Aminov, Nazarbayev University, Astana, Kazakhstan Translated to English by the GeoGPT group, Zhejiang Lab, Hangzhou, China--see About

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Agadzhan Formation
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Agadzhan Fm base reconstruction

Agadzhan Fm


Period: 
Triassic

Age Interval: 
Olenekian-Anisian (T1-2), E-Psh3


Province: 
East Tajik (East Pamir)

Type Locality and Naming

Includes in East Pshart (Agadjan river basin)

Synonym: Agadzhan layer, Agadjan layer, Agadjan Fm

Reference section:


Lithology and Thickness

It is composed of dark gray clay slates with beds and layers of dark cherts and greenstone-altered fissured basic volcanogenic rocks. (100-500 m)


Lithology Pattern: 
Volcanic_ash


Relationships and Distribution

Lower contact

The layer lies with an unclear contact on the faunistically characterized sediments of the Kuberkandinsky horizons, Shiberdzhilgin Fm

Upper contact

It is overlain by the faunistically characterized Middle-Upper Triassic Gumbekol Fm in conformity.

Regional extent

It is developed in the watershed part of the eastern half of the Pshart Range, on the periphery of the exits of the Middle-Upper Triassic Gumbekol Fm (гумбезкольской толщи).


GeoJSON

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Fossils

No organic remains have been found in either the Nychkedyilgin or Agadzhan Fms.


Age 

They are conditionally referred to the Lower-Middle Triassic, by their position in the section, above the Upper Permian and below the Middle-Upper Triassic sediments.

Age Span: 

    Beginning stage: 
Olenekian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
249.88

    Ending stage: 
Anisian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
241.46

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Extracted from Baratov, R. B. (1976). Subdivisions of stratified and intrusive rocks of Tajikistan. Donish, Dushanbe, 276.