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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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Tochar Formation
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Tochar Fm base reconstruction

Tochar 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

Lower part (0 to 40 m) is grey sandstones with mudstone and white gypsum at the top. Upper part (0 to 175 m) is red mudstones, siltstones and sandstones.


Lithology Pattern: 
Sandy claystone


Relationships and Distribution

Lower contact

Overlies the marl of the upper Beshkent Fm.

Upper contact

Overlain by the marl of the Kunshan Fm.

Regional extent

Afghan-Tajik Basin.


GeoJSON

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Fossils

Bivalves in upper part.


Age 

Middle-late Eocene; placed as upper Lutetian for graphic purposes.

Age Span: 

    Beginning stage: 
Lutetian

    Fraction up in beginning stage: 
0.5

    Beginning date (Ma): 
44.55

    Ending stage: 
Lutetian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
41.03

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.