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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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Myshikkol Formation
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Myshikkol Fm base reconstruction

Myshikkol Fm


Period: 
Carboniferous

Age Interval: 
Lower Bashkirian, CK9, CK9b


Province: 
Chatkal-Kuramin Region

Type Locality and Naming

Along the river Myshikkol, Altyntopkan Mountains, Kuramin Ridge. I.M. Bogomolny and others in 1967.

Synonym: Myshikkolskaya Suite, Мышиккольская св.


Lithology and Thickness

Limestones, interbedded with siliceous slates, siltstone (aleurolites), sandstones, tuff-sandstones, tuff-argillites, tuffs of andesite-dacite composition. Laterally, the composition of the suite and the character of interbedding are variable. Thickness from 70 to 400 m.


Lithology Pattern: 
Limestone


Relationships and Distribution

Lower contact

Conformably overlies the Tashgezek Fm

Upper contact

Unconformably overlain by the effusives of the Upper Paleozoic.

Regional extent

Kuramin Ridge, 3. Karamazar, rivers Myshikkol, Koshmulla, Yangikan, Beguly, Almabulak, Chashly


GeoJSON

{"type":"Feature","geometry":{"type":"Polygon","coordinates":[[[69.882,40.711],[70.015,40.741],[70.126,40.818],[70.23,40.772],[70.066,40.7],[69.889,40.711],[69.882,40.711]]]}}

Fossils

Contains conodonts - Declinognathodus noduliferus (El. et Gr.), Neognathodus symmetricus Lane; brachiopods - Productus cf. concinus Sow., Echinoconchus punctatus (Mart.).


Age 

Middle Carboniferous (Lower Bashkirian)

Age Span: 

    Beginning stage: 
Bashkirian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
323.40

    Ending stage: 
Bashkirian

    Fraction up in the ending stage: 
0.4

    Ending date (Ma):  
320.10

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

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