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Cenozoic
Cretaceous
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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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Modun Formation
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Modun Fm base reconstruction

Modun Fm


Period: 
Cretaceous

Age Interval: 
Upper Turonian (K21), K1, D1, C2, C2a, S3, S4, 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: Modun horizon, Moudun horizon, Moudun Fm


Lithology and Thickness

In the Kafirnigan district, the lower Coniacian stage, Modun horizon, consists of greenish-gray clays with a thickness of 35-100 m, containing frequent interbeds of organic limestones and shell limestones with oysters.


Lithology Pattern: 
Claystone


Relationships and Distribution

Lower contact

Overlies the Disgiryak Fm.

Upper contact

Underlies the Modun Fm.

Regional extent

Afghan-Tajik Basin.


GeoJSON

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Fossils

In the Kafirnigan district, the, Modun horizon contains remains of oysters Liostrea rouvillei (Coq.), Exogyra turkestanensis Born., and others


Age 

Lower Coniacian

Age Span: 

    Beginning stage: 
Coniacian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
89.39

    Ending stage: 
Coniacian

    Fraction up in the ending stage: 
0.5

    Ending date (Ma):  
87.55

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Extracted from Baratov, R. B. (1976). Subdivisions of stratified and intrusive rocks of Tajikistan. Donish, Dushanbe, 276.