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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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Penjikent Formation
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Penjikent Fm base reconstruction

Penjikent Fm


Period: 
Neogene

Age Interval: 
Pliocene (N2), S4


Province: 
North Tajik

Type Locality and Naming

Synonym: Penjikent depression Fm

Reference section:


Lithology and Thickness

According to D.A. Starshinin, are represented by brown, pale-brown, and gray conglomerates and sandstones. The size of the fragments increases from bottom to top in the section and from the center to the periphery of the depression. The incomplete thickness of the deposits reaches 1000 m.


Lithology Pattern: 
Aus Conglomerate


Relationships and Distribution

Lower contact

They lie conformably on the red-colored rocks of the Miocene

Upper contact

Unconformably overlain by the lower Quaternary formations

Regional extent

They are widespread in the southern part of the Turkestan region and in the Zeravshan-Gissar region. This is correlated with Bactrian Gr of Ferghana.


GeoJSON

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Fossils


Age 

The Pliocene age is assumed by comparison with the Bactrian series of Ferghana.

Age Span: 

    Beginning stage: 
Zanclean

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
5.34

    Ending stage: 
Piacenzian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
2.58

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

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