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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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Khan-Yuly Formation
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Khan-Yuly Fm base reconstruction

Khan-Yuly Fm


Period: 
Jurassic

Age Interval: 
Upper Callovian - Lower Oxfordian (J3), Sar2


Province: 
East Tajik (easternmost Pamir)

Type Locality and Naming

Includes in Sarykoln district (Istyk type section (Kokchagin area)

Synonym: Khan-Yuly Suite, Ханюлыйская свита

Reference section:


Lithology and Thickness

It is represented by gray and light-colored variable-bedded limestones, interbedded with claystones and marls. (80 m).


Lithology Pattern: 
Limestone


Relationships and Distribution

Lower contact

Schematic stratigraphic column indicates the lower contact as Kichikhan-Yuly Fm

Upper contact

Schematic stratigraphic column indicates the upper contact as Jerkapchal Fm

Regional extent

In the Kokchaginsky area, in the basin of the rivers Zhilgakochusu (Kokchagi), Khan-Yuly.


GeoJSON

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Fossils

It contains numerous remains of fauna, including the following pteriomorphs: Aequipecten subinaequicostatus Kas., A. fibrosus Sow., Exogyra ex gr. virgula Buv., Ceratomya calloviensis Kas.


Age 

Based on the remains of the fauna and its position in the section, the suite is considered Upper Callovian and partly, possibly, Lower Oxfordian.

Age Span: 

    Beginning stage: 
Callovian

    Fraction up in beginning stage: 
0.7

    Beginning date (Ma): 
162.66

    Ending stage: 
Oxfordian

    Fraction up in the ending stage: 
0.2

    Ending date (Ma):  
160.18

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

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