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
Upper Cambrian Formation
Click to display on map of the Ancient World at:
Upper Cambrian Fm base reconstruction

Upper Cambrian Fm


Period: 
Cambrian

Age Interval: 
Upper Cambrian, S2


Province: 
North Tajik

Type Locality and Naming

Synonym: Upper Division

Reference section:


Lithology and Thickness

Clay slates, claystones, limestones. It is represented by alternations of dark gray clay slates, claystones, limestones, and sandstones, which contain rare lenses of conglomerates. The thickness is 200 m. The number of slates increases up the section. At the bottom, coarse-grained sandstones and conglomerates usually predominate, containing (Yaskovich, 1968) in the pebbles remains of trilobites of the Mayan stage.


Lithology Pattern: 
Clayey limestone


Relationships and Distribution

Lower contact

On the rocks of the Mayan stage, the upper Cambrian lies with erosion, but without angular discordance.

Upper contact

It is overlain by terrigenous rocks of the Lower Ordovician in conformity.

Regional extent

It is widespread in the same locations as the middle division i.e., in Central Tajikistan (Zeravshan-Gissar and South Gissar districts) and in the Northern Pamir.


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[68.81,39.88],[69.03,39.9],[69.45,39.98],[71.41,41.03],[71.78,41.31],[73.02,40.87],[71.84,39.88],[70.94,39.83],[70.1,39.66],[68.92,39.51],[68.44,39.58],[68.41,39.72],[68.54,39.89],[68.81,39.88]]]]}}

Fossils

In the interlayers of limestones and carbonate cement of conglomerates, there are trilobites characteristic of the upper Cambrian: Homagnostus obesus Belt., H. asiaticum Hajr., Lisania sp., Onchonotellus oburdonicus Hajr., Prochuangia minuscula Hajr., Proceratopyge schaganica Hajr,, and others (Geol. USSR, vol. 23, 1972).


Age 

Upper Cambrian

Age Span: 

    Beginning stage: 
Paibian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
497.00

    Ending stage: 
Cambrian Stage 10

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
486.85

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

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