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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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Gurumdin Formation
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Gurumdin Fm base reconstruction

Gurumdin Fm


Period: 
Jurassic

Age Interval: 
Sinemurian (J1), M3a


Province: 
SE Tajik (SE Pamir)

Type Locality and Naming

Includes in SE Murghab district (Gurdumdin type section)

Synonym: Gurumdinskaya suite, гурумдинская свиты

Reference section:


Lithology and Thickness

It is composed of coarse-bedded, and at the top, light-colored massive limestones, partly reef-forming. (80-400 m)


Lithology Pattern: 
Reef limestone


Relationships and Distribution

Lower contact

Conformably underlying Darbazatazh Fm

Upper contact

Regional extent

It characterizes the Chor of the Southeastern Pamir.


GeoJSON

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Fossils

Organic remains are only characteristic of the Gurumdin Fm, containing Hettangian Sinemurian pelecypods Cardinia cf. elliptica Quenst., C. cf. hybrida Quenst., Pachyrisma aff. chamaeformis Schloth.


Age 

Sinemurian

Age Span: 

    Beginning stage: 
Sinemurian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
199.46

    Ending stage: 
Sinemurian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
192.90

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

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