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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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Babatag Formation
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Babatag Fm base reconstruction

Babatag Fm


Period: 
Cretaceous

Age Interval: 
Upper Turonian (K21), K1, D1, C1


Province: 
SW Tajik, Central W Tajik

Type Locality and Naming

Includes in Khation Region, Darvaz district, Hisar-Zarafshan ranges

Upper substage of the Aptian stage and Albian stage in the Turkestan, Zarafshan-Gissar, South Gissar, Karategin, Dushanbe, Qafirnigan, Vakhsh, Zaalai and Darvaz districts includes five horizons: 1 – Karakuz (Upper Aptian - Lower Albian); 2 - Derbent (Lower Albian); 3 - Babatag (Middle Albian); 4 – Akkapchigay (Upper Albian); 5 - Shirabad (Upper Albian). Corresponding to these are variegated sandstones, argillites and clays containing layers of limestone, less often gypsum and conglomerates. Their total thickness is 100-800 m.

Synonym: Babatag horizon, Babatag suite, upper Mingbatman suite, lower Jetimtausk suite


Lithology and Thickness

In the South Gissar, Dushanbe, and Kafirnigan districts, this horizon is represented by the Babatag suite (Andreev, 1969b), consisting of limestones and shell-coquinas interbedded with gray and variegated clays, marls, and sandstones. The thickness is 20-120 m. In the Zeravshan-Gissar, Karategin, Vakhsh, Zaalaik, and Darvaz districts, the Babatag horizon is represented by red-colored sandstones and siltstones of the upper part of the Mingbatman suite, and possibly variegated sandstones, siltstones, and clays with rare layers of shell-coquinas from the lower part of the Jetimtausk suite. The thickness of the horizon is 25-100 m. The upper part of the Mingbatman suite contains a sharply impoverished fauna complex similar to that of the Babatag suite.


Lithology Pattern: 
Sandy limestone


Relationships and Distribution

Lower contact

Overlies the Derbent Fm.

Upper contact

Underlies the Akkapchigay Fm.

Regional extent

Afghan-Tajik Basin.


GeoJSON

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Fossils

In the South Gissar, Dushanbe, and Kafirnigan districts, it contains a rich and diverse complex of marine and brackish water fauna, characteristic of the entire middle Albian - from the zone of Hoplites dentatus to the zone of Anahoplites rossicus (Andreev, 1969b).


Age 

Middle Albian

Age Span: 

    Beginning stage: 
Albian

    Fraction up in beginning stage: 
0.35

    Beginning date (Ma): 
108.76

    Ending stage: 
Albian

    Fraction up in the ending stage: 
0.6

    Ending date (Ma):  
105.58

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Chapman, J.B., et al. (9 co-authors), 2020. The Afghan-Tajik Basin: A composite record of sedimentary basin evolution in response to tectonics in the Pamir. Basin Research, 32(3), 525-545. https:/doi.org/10.1111/bre.12381.