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Main source = Abduazimova, Z.M. (Ed.), 2001. Stratigraphic Dictionary of Uzbekistan. IMR (Institute of Mineral Resources), Tashkent, 580 pp. (In Russian) Translated to English by the GeoGPT group, Zhejiang Lab, Hangzhou, China--see About

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Kuhistan Formation
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Kuhistan Fm base reconstruction

Kuhistan Fm


Period: 
Cretaceous

Age Interval: 
upper Cenomanian - lower Turonian, Z1


Province: 
Zarafshan-N.Gissar

Type Locality and Naming

From the historical name of Central Tajikistan. M.R. Dzhalilov, Yu.N. Andreev, F.Kh. Hakimov et al., 1971 (191, pp.74-75). Stratotype in the area of the village of Ravat on the right bank of the Yagnob River.

Synonym: Kuhistan Suite, Хушикатская св.


Lithology and Thickness

Green and dark gray clays with interlayers of sandstones and shell limestones. Thickness 48-100m.


Lithology Pattern: 
Sandy_claystone


Relationships and Distribution

Lower contact

Conformably overlies the Sangrezin Fm

Upper contact

Conformably overlain by the Gezan Fm

Regional extent

Zarafshan Ridge (Mukhbel), North Central Gissar.


GeoJSON

{"type":"Feature","geometry":{"type":"Polygon","coordinates":[[[67.013,39.201],[67.112,39.276],[67.265,39.27],[67.417,39.25],[67.563,39.16],[67.292,39.048],[67.079,39.095],[67.013,39.201]]]}}

Fossils

Contains marine bivalve mollusks - Nucula gaurdakensis Bobk., Gyrostrea turkestanensis (Born.), Korobkovitrigoonia darwaseana Rom., Cyprimeria faba Sow.; foraminifers Brotzenella berthelini (Kell.), Hedbergella tschikrysovi (Arap.).


Age 

Belongs to the upper Cenomanian - lower Turonian. (56; 446; 452).

Age Span: 

    Beginning stage: 
Cenomanian

    Fraction up in beginning stage: 
0.7

    Beginning date (Ma): 
95.88

    Ending stage: 
Turonian

    Fraction up in the ending stage: 
0.3

    Ending date (Ma):  
92.55

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

I.M. Abdazimova – In: GeoGPT translation of: “Abduazimova, Z.M. (Ed.), 2001. Stratigraphic Dictionary of Uzbekistan. IMR (Institute of Mineral Resources), Tashkent, 580 pp. (In Russian)”