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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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Kamolin Formation
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Kamolin Fm base reconstruction

Kamolin Fm


Period: 
Neogene

Age Interval: 
Lower Miocene 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.

Upper unit of the Baldzhuan Gr.

Synonym: Kamoli Fm (spelling in Bosboom et al., 2017)


Lithology and Thickness

Compact massive and coarse laminated red sandstones with rare interbeds of mudstones, siltstones and conglomerates. 180 t 310 m.


Lithology Pattern: 
Sandstone


Relationships and Distribution

Lower contact

Overlies the Shurysay-TajikBasin Fm claystone of upper Oligocene.

Upper contact

Overlain by the Childara Fm claystone.

Regional extent

Afghan-Tajik Basin.


GeoJSON

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Fossils


Age 

Early Miocene

Age Span: 

    Beginning stage: 
Aquitanian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
23.04

    Ending stage: 
Burdigalian

    Fraction up in the ending stage: 
0.5

    Ending date (Ma):  
18.22

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.