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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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Shurysay-TajikBasin Formation
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Shurysay-TajikBasin Fm base reconstruction

Shurysay-TajikBasin Fm


Period: 
Paleogene

Age Interval: 
Upper Oligocene, 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.

There is also a same-named Shurysay Fm in the Alai-Fergana Basin of late Oligocene age and of a similar facies of "brownish-red mudstones intercalated by siltstones, evaporite beds and sandstones", which is called the Shurysay-Fergana Fm in this lexicon to avoid confusion.

Synonym: Shurysay Fm


Lithology and Thickness

Reddish-brown mudstones, sandstones and siltstones with gypsum, rare interbeds of limestone. 0 to 190 m.


Lithology Pattern: 
Sandy claystone


Relationships and Distribution

Lower contact

Overlies Hissarak Fm sandstone.

Upper contact

Overlain by the Kamolin Fm of the Baldzhuan Gr.

Regional extent

Afghan-Tajik Basin.


GeoJSON

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Fossils


Age 

Upper Oligocene

Age Span: 

    Beginning stage: 
Chattian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
27.29

    Ending stage: 
Chattian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
23.04

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.