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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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Kattamardzhana Formation
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Kattamardzhana Fm base reconstruction

Kattamardzhana Fm


Period: 
Triassic

Age Interval: 
Ladinian-Carnian, M3d


Province: 
SE Tajik (SE Pamir)

Type Locality and Naming

Includes in SE Murghab district (Gurdumdin type section Gurumd and Kattamardzhana rivers)

Synonym: Kattamardzhan, Kattamardzhanaisky, Каттамарджанаikкий

Reference section:


Lithology and Thickness

These are asymmetric stocks with relatively steep lateral contacts and gently sloping apical surfaces. The lateral contacts of most massifs are even.


Lithology Pattern: 
Volcanics


Relationships and Distribution

Lower contact

Schematic stratigraphic column indicates the lower contact as North Alay Gr (Ediacaran)

Upper contact

Regional extent

It is distributed in the Central, Southwestern, and Southeastern Pamir, but mainly in the axial part and on the northern slopes of the Rushan Ridge.


GeoJSON

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Fossils


Age 

Ladinian-Carnian

Age Span: 

    Beginning stage: 
Ladinian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
241.46

    Ending stage: 
Carnian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
227.30

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

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