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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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Kunshan Formation
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Kunshan Fm base reconstruction

Kunshan Fm


Period: 
Paleogene

Age Interval: 
Upper Eocene, K1, D1, C2, C2a, S5


Province: 
SW Tajik, North Tajik, Central W Tajik

Type Locality and Naming

Includes in Khation Region, Sughd Region, Darvaz district, Dushanbe - west Shirkent-Luchob, Dushanbe - east Shirkent-Luchob.

Synonym:


Lithology and Thickness

Greenish-grey (calcareous) mudstones with rare interbeds of limestones and shell beds, at the top reddish-brown mudstones. 0 to 175 m.


Lithology Pattern: 
Shallow-marine marl


Relationships and Distribution

Lower contact

Overlies the sandy claystone of the Tochar Fm.

Upper contact

Overlain by the Sanglak Fm.

Regional extent

Afghan-Tajik Basin.


GeoJSON

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Fossils


Age 

Middle-Late Eocene; arbitrarily assigned to Bartonian here.

Age Span: 

    Beginning stage: 
Bartonian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
41.03

    Ending stage: 
Bartonian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
37.71

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Bosboom, R., Mandic, O., Dupont‐Nivet, G., Proust, J. N., Ormukov, C., & Aminov, J. (2017). Late Eocene palaeogeography of the proto‐Paratethys Sea in Central Asia (NW China, southern Kyrgyzstan and SW Tajikistan). Geological Society, London, Special Publications, 427, 565–588. https://doi.org/10.1144/SP427.11.