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Aral Formation
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Aral Fm base reconstruction

Aral Fm


Period: 
Neogene

Age Interval: 
Miocene


Province: 
Zaisan (Zaysan) Basin - Central

Type Locality and Naming

Synonym: Aralskaya, N1ar


Lithology and Thickness

Ca. 180 m of Calcareous monotonous grey compact clay with interbeds and lentils of marls. In the upper half of the section are inclusions of gypsum (crystals, small concretions).


Lithology Pattern: 
Gypsiferous claystone


Relationships and Distribution

Lower contact

Overlies the Ashutas Fm with a very gradual contact.

Upper contact

Unconformably overlain by the Pavlodar Fm. Contact is sharp.

Regional extent


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[82.65,48.87],[82.85,48.54],[82.61,48.18],[82.25,48.02],[83.07,47.29],[83.97,47.33],[84.52,48.24],[84.6,48.4],[84.1,48.36],[83.67,48.66],[83.49,48.97],[82.65,48.87]]]]}}

Fossils


Age 

Miocene (indicated as spanning the Lower, Middle and Upper Miocene)

Age Span: 

    Beginning stage: 
Aquitanian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
23.04

    Ending stage: 
Messinian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
5.34

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Information provided by Nariman Jamikeshev from Kazakh-language sources and from other publications.