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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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Stamp Formation
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Stamp Fm base reconstruction

Stamp Fm


Period: 
Paleogene

Age Interval: 
Rupelian – Chattian (P? št), R1


Province: 
SE Tajik (SE Pamir)

Type Locality and Naming

Synonym: Stampskaya Suite, Штамская свита

Reference section:


Lithology and Thickness

It consists of red-colored plagio-porphyries, keratophyres, felsite-porphyries, trachybasalts, trachytes and their tuffs with layers of marbles and sandstones. The incomplete thickness is 800 m.


Lithology Pattern: 
Volcanic_ash


Relationships and Distribution

Lower contact

The contacts with the surrounding rocks are tectonic

Upper contact

Regional extent

It is widespread in the Rushan Ridge (Southern Pamir) in the upper reaches of the river Shkam.


GeoJSON

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Fossils

Organic remains have not been found.


Age 

The age is determined conditionally based on correlation with the volcanics of the Bartang Gr. Hence it is considered Upper part of Paleogene – Chattian - Rupelian

Age Span: 

    Beginning stage: 
Rupelian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
33.90

    Ending stage: 
Chattian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
23.04

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.