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Cenozoic
Cretaceous
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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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Basal Formation
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Basal Fm base reconstruction

Basal Fm


Period: 
Triassic

Age Interval: 
Middle-Late Triassic (P2+3), S4


Province: 
North Tajik

Type Locality and Naming

Synonym: basal suite

Reference section:


Lithology and Thickness

Basal Fm consists of conglomerates, quartz gravelites, and sandstones with interlayers and lenses of claystones. The power is 2070 m.


Lithology Pattern: 
Aus Conglomerate


Relationships and Distribution

Lower contact

The deposits lie with a sharp angular unconformity on the Paleozoic rocks

Upper contact

overlain discordantly by the Upper Cretaceous.

Regional extent

In the southern part of the Turkestan region, J1+2 deposits are exposed along the rivers Kshut, Zauran, Rivat, Surhat.


GeoJSON

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Fossils


Age 

The Middle-Late Triassic age of the suite is determined by the spore-pollen complex.

Age Span: 

    Beginning stage: 
Ladinian

    Fraction up in beginning stage: 
0.5

    Beginning date (Ma): 
239.23

    Ending stage: 
Carnian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
227.30

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

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