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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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Sanglak Formation
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Sanglak Fm base reconstruction

Sanglak 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

Brownish-red mudstones with red-brownish-grey sandstones at the top, bivalve. 0 to 90 m.


Lithology Pattern: 
Claystone


Relationships and Distribution

Lower contact

Overlies the marl of the Kushan Fm.

Upper contact

Overlain by the stromatolitic base of the Hissarak Fm.

Regional extent

Afghan-Tajik Basin.


GeoJSON

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Fossils

Bivalves


Age 

Late Eocene; arbitrary placed as spanning the Priabonian here.

Age Span: 

    Beginning stage: 
Priabonian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
37.71

    Ending stage: 
Priabonian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
33.90

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.