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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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Bukhara-Fergana Formation
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Bukhara-Fergana Fm base reconstruction

Bukhara-Fergana Fm


Period: 
Paleogene

Age Interval: 
late Paleocene, S2, S3


Province: 
North Tajik

Type Locality and Naming

Includes in Fergana Valley, Isfara River

To avoid confusion with the Bukhara Fm in the central-East Tajik region, "Fergana" is appended to the Bukhara name here.

Synonym: Bukhara Fm


Lithology and Thickness

In Alai-Fergana basin, it is limestones, evaporite beds and white sandstones with thin calcareous mudstone layers. 20-80 m.


Lithology Pattern: 
Sandy limestone


Relationships and Distribution

Lower contact

Upper contact

Alai beds Fm

Regional extent

Fergana Basin and Alai Valley Basin


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[68.81,39.88],[69.03,39.9],[69.45,39.98],[71.41,41.03],[71.78,41.31],[73.02,40.87],[71.84,39.88],[70.94,39.83],[70.1,39.66],[68.92,39.51],[68.44,39.58],[68.41,39.72],[68.54,39.89],[68.81,39.88]]]]}}

Fossils

Bivalves and gastropods.


Age 

Late Paleocene

Age Span: 

    Beginning stage: 
Selandian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
61.66

    Ending stage: 
Thanetian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
56.00

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.