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Parkini Formation
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Parkini Fm base reconstruction

Parkini Fm


Period: 
Neogene

Age Interval: 
Late Mioceen


Province: 
Pakistan Balochistan Basin

Type Locality and Naming

Holotype section: Within Makran Flysch Province (MFP) of the Balochistan Basin


Lithology and Thickness

Sandy claystone. Predominantly mudstone. Thickness: 3,030-4,545 m.


Lithology Pattern: 
Claystone


Relationships and Distribution

Lower contact

Conformably underlain by Panjgur Fm

Upper contact

Conformably overlain by Talar Fm

Regional extent

Makran Flysch Province


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[66.05,25.58],[61.31,25.47],[62.82,27.53],[61.16,30.01],[65.39,29.61],[66.45,30.94],[69.53,32.65],[69.13,31.05],[66.94,30.46],[66.03,28.66],[66.05,25.58]]]]}}

Fossils


Age 

Late Miocene.

Age Span: 

    Beginning stage: 
Tortonian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
11.63

    Ending stage: 
Messinian

    Fraction up in the ending stage: 
0.3

    Ending date (Ma):  
6.68

Depositional setting

Panjgur Fm fan complex is covered by extensive and massive upper Miocene slope mudstones known as the Parkini Fm.


Depositional pattern:  


Additional Information


Compiler:  

Nusrat K. Siddiqui