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Cenozoic
Cretaceous
Jurassic
Triassic
Permian
Carboniferous
Devonian
Silurian
Ordovician
Cambrian
Neoproterozoic


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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Gazdagan Formation
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Gazdagan Fm base reconstruction

Gazdagan Fm


Period: 
Cretaceous

Age Interval: 
Latest Cenomanian (K21), Ak-Ra1


Province: 
East Tajik (NE Pamir)

Type Locality and Naming

Includes in Akbaital-Rangkul region

Synonym: Gazdagansky horizon, газдаганинскому горизонту

Reference section:


Lithology and Thickness

Dark gray clays, 30 m thick with interlayers of limestones.


Lithology Pattern: 
Clayey limestone


Relationships and Distribution

Lower contact

Schematic stratigraphic column indicates the next formation as Shorbel Fm

Upper contact

Schematic stratigraphic column indicates the next formation as Turonian strata

Regional extent

In the Sarykolsky district of the Northern Pamir, the Upper Cretaceous forms the largest exposures and is most studied in the valley of the Kyzyljik river and along the northern rim of the Rangkul lake basin.


GeoJSON

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Fossils


Age 

Latest Cenomanian

Age Span: 

    Beginning stage: 
Cenomanian

    Fraction up in beginning stage: 
0.8

    Beginning date (Ma): 
95.22

    Ending stage: 
Cenomanian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
93.90

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

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