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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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Beshkent Formation
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Beshkent Fm base reconstruction

Beshkent Fm


Period: 
Paleogene

Age Interval: 
Middle 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

Upper part (Gandzhin layers; 0 to 60 m) of greenish-grey calcareous mudstones with interbeds of marls, shell beds, limestones and sandstones. Lower part (Turkestan layers; 0 to 130 m) of greenish-grey mudstones with rare shell beds.


Lithology Pattern: 
Shallow-marine marl


Relationships and Distribution

Lower contact

Overlies the marl of the Jukar Fm.

Upper contact

Overlain by the sandstone of the lower Tochar Fm.

Regional extent

Afghan-Tajik Basin.


GeoJSON

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Fossils

Shell beds.


Age 

Middle Eocene; arbitrarily placed as lower Lutetian for graphic purposes

Age Span: 

    Beginning stage: 
Lutetian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
48.07

    Ending stage: 
Lutetian

    Fraction up in the ending stage: 
0.5

    Ending date (Ma):  
44.55

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.