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Gwadar Formation
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Gwadar Fm base reconstruction

Gwadar Fm


Period: 
Quaternary

Age Interval: 
Middle Pleistocene


Province: 
Pakistan Balochistan Basin

Type Locality and Naming

Holotype section: Gwandar hammerhead section within Makran Flysch Province (MFP) of the Balochistan Basin


Lithology and Thickness

Sandy claystone. Combined Gwandar and overlying/coeval Ormara Fm are predominantly sandy clay, 60-900 m thick


Lithology Pattern: 
Sandy claystone


Relationships and Distribution

Lower contact

Conformably underlain by Chatti Fm, or unconformably underlain by Hinglaj Fm

Upper contact

Conformably overlain by Ormara Fm

Regional extent

v


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 

Early Pleistocene probably

Age Span: 

    Beginning stage: 
Gelasian

    Fraction up in beginning stage: 
0.7

    Beginning date (Ma): 
2.03

    Ending stage: 
Calabrian

    Fraction up in the ending stage: 
0.4

    Ending date (Ma):  
1.39

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Nusrat K. Siddiqui