Home Multi-Country Search About Admin Login
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

Search by
Select Region(s) to search
Hold Ctrl (Windows/Linux) or Command (Mac) to select multiple
Shurabsay Formation
Click to display on map of the Ancient World at:
Shurabsay Fm base reconstruction

Shurabsay Fm


Period: 
Permian

Age Interval: 
Lower Permian (P1 s̀r), S1


Province: 
North Tajik

Type Locality and Naming

It was identified by N.P. Vasilyevsky (1952).

Synonym: Shurabsay suite, Shurabsai suite, Шурабсайская свита

Reference section:


Lithology and Thickness

The Shurabsay suite is best preserved in the Chorukhdayron graben and the Tashkessen and Adrasman basins. In the Yashkeresk basin, mainly subvolcanic facies of the suite are present.

In general, the section of the suite is four-membered:

1- arkosic conglomerates, gravelites, and sand Bedrock, containing pebbles of almost all older rocks of the Karamazar, the thickness ranges from several tens to 600 meters (Takeliy formation) (такелийская толща);

2 - dark gray, almost black, and green pyroxene trachyandesites and trachybasalts, as well as their agglomerates, thickness 200-800 meters (Uchochak, Pyazlysay, Dolonysay, and Suchilgan formations) (учоча1кская, пиязлысайская, долонысайская и сучилrанская толщи);

3 - brown and brick-red crystal tuffs and tuff lavas of trachytes, containing fragments of underlying trachyandesites, thickness 200-500m (Aynabulak and Chokadambulak formations) (айнабулакская и чокадамбулакская толщи);

4 - creamy and pinkish-gray fluidal and spheroidal lavas and ignimbrites of trachyphonolites at the base with a horizon (sometimes) of sandstones, tuff sandstones, and clay slates, thickness 200-600 meters (Sarytaipan, Tereklysay, and Karankul formations) (сарытайпанская, тереклисайская, каранкульская толщи).

The thickness of the Shurabsay suite (шурабсайской свиты) is 900-2000 meters.


Lithology Pattern: 
Volcanic_ash


Relationships and Distribution

Lower contact

It lies with a gap on volcanics of the conditionally Upper Carboniferous Oyasa Fm and older suites

Upper contact

It is overlain with a minor gap by volcanics of the Ravash suite (равашекой свиты), which are attributed to the lower part of the Upper Permian.

Regional extent

It is widespread in the Karamazar district.


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[70.39,41.04],[70.63,40.85],[70.33,40.59],[70.08,40.42],[69.69,40.2],[69.03,39.96],[69.33,40.33],[69.28,40.48],[69.43,40.72],[69.64,40.6],[69.9,40.71],[70.08,40.74],[70.13,40.82],[70.3,40.89],[70.39,41.04]]]]}}

Fossils

In the Sarytaipanskaya and Tereklysayskaya formations (сарытайпанской и тереклисайской толщах), J.N. Kuznetsov in 1956 and B.I. Sigalov in 1962 collected remains of the flora Ullmania sp.; Cordaites angustifolius Neub., C. insignis Rades, C. (Noeggerathiopsis) theodori Tschet., Samaropsis eumarginata (Goepp. et Berg.) and others. According to T.A. Systel's conclusion, some of these forms are characteristic of the Lower Permian, while the rest are known both in the Upper Carboniferous and in the Upper Permian. Palynological studies in the Shurabsayskaya suite have established forms characteristic of the Kungurian: Cordaitina uralensis (Zub), Azonoletes ex gr. fabaginus (Sam.).


Age 

Based on these data, the Shurabskaya suite is attributed to the Lower Permian.

Age Span: 

    Beginning stage: 
Asselian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
298.89

    Ending stage: 
Kungurian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
274.37

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

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