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
Middle Karamazar deposits Formation
Click to display on map of the Ancient World at:
Middle Karamazar deposits Fm base reconstruction

Middle Karamazar deposits Fm


Period: 
Cretaceous

Age Interval: 
Santonian (undifferentiated - K2), S1


Province: 
North Tajik

Type Locality and Naming

Synonym: Upper Cretaceous deposits

Reference section:


Lithology and Thickness

Aus Conglomerate. Pink or yellow sandstones and conglomerates with a thickness of 10-30 m.


Lithology Pattern: 
Aus Conglomerate


Relationships and Distribution

Lower contact

They lie in visible conformity on the marls, in other points (Adrasman, Qansay, etc.), these sandstones lie directly on the Paleozoic.

Upper contact

Regional extent

In the section near the village of Shaidan. In the Karamazar district, Upper Cretaceous deposits are encountered sporadically at individual points, poorly studied. Upper Cretaceous deposits are distinguished in the Karamazar, Turkestan, Zarafshan-Gissar, Karategin, Zaalay, Darvaz, Sarykol, and the Central Pamir regions.


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 them, remains of dinosaur bones, turtle shields, shark teeth, as well as shells of freshwater bivalves Sainshandia aralica Mart., Neotrigonioides gigantus Mart., and others have been found.


Age 

According to the conclusion of G. G. Martynson, for the Santonian stage of the Northeastern and Eastern Pararya. On this basis, the pink sandstones andConglomerates are considered Santonian. The question of the presence of the Coniacian stage in Karamazar remains open.

Age Span: 

    Beginning stage: 
Santonian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
85.70

    Ending stage: 
Santonian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
83.65

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

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