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Cenozoic
Cretaceous
Jurassic
Triassic
Permian
Carboniferous
Devonian
Silurian
Ordovician
Cambrian
Neoproterozoic


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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Dulyangtash Formation
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Dulyangtash Fm base reconstruction

Dulyangtash Fm


Period: 
Jurassic

Age Interval: 
upper Callovian (J3), M3a


Province: 
SE Tajik (SE Pamir)

Type Locality and Naming

It is distinguished in the Southeast Pamir in the SE Murghab district (Gurumdin type section) of the Jurassic

Synonym: Dulyangtashskaya suite

Reference section:


Lithology and Thickness

Greenish-yellow marls. The total power of the sediments is 115 m.


Lithology Pattern: 
Shallow-marine marl


Relationships and Distribution

Lower contact

Schematic stratigraphic column indicates the lower contact as Kokchukur Fm

Upper contact

Schematic stratigraphic column indicates the upper contact as Teshyktash Fm (volc) / Kurtekin Fm (Paleogene)

Regional extent

It is widespread in the Southeast Pamir.


GeoJSON

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Fossils

No organic remains have been found in them.


Age 

upper Callovian

Age Span: 

    Beginning stage: 
Callovian

    Fraction up in beginning stage: 
0.8

    Beginning date (Ma): 
162.28

    Ending stage: 
Callovian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
161.53

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

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