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Patala Formation
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Patala Fm base reconstruction

Patala Fm


Period: 
Paleogene

Age Interval: 
Late Paleocene


Province: 
Pakistan Indus Basin

Type Locality and Naming

Makarwal Gr – upper formation. Holotype section: Patala Nallah, Western Salt Range. Author: L.M. Davies & E.S. Pinfold, 1937. Reference section: None.


Lithology and Thickness

Shallow-marine marl. In the type section it consists of shale and marl with subordinate limestone. The shale is dark greenish grey, selenite bearing, in places carbonaceous and calcareous, and contains marcasite nodules. The thin interbeds of limestone are white to light grey and nodular. Coal seams of economic value are present locally (Dandot area).

Thickness: 20-182 m. It is 27 m thick in the type section and 90 m at Khewra Gorge. The thickness varies between 30 m to 75 m in Surghar Range, 30 m to 80 m in Kohat area, 60 m to 182 m in Hazara area, and is 20 m thick in Kalachitta Range.


Lithology Pattern: 
Shallow-marine marl


Relationships and Distribution

Lower contact

Conformably underlain by Lockhart Limestone Fm

Upper contact

Conformably overlain by Nammal Fm (transitional contact) in Salt Range, by Panoba Shale Fm in Kohat area and by the Margala Hill Limestone Fm in the Hazara and Kalachitta areas.

Regional extent

The formation is widely exposed in the Kohat-Margala Province (Ko-MP) (including Hazara area), Salt Range, and has been encountered in subsurface in oil wells drilled in Potwar and the T-CP.


GeoJSON

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Fossils

The formation is richly fossiliferous. Larger forams include Actinosiphon tibetica, Assilina dandotica, Daviesina intermedia, Discocyclina ranikotenesis, Kathina nammalensis, etc. Smaller forams include Glandulina laevigata, Cincoriala cvouidea, Cycloloculina glabra, etc.


Age 

Late Paleocene, except in Hazara area where it extends into the Early Eocene.

Age Span: 

    Beginning stage: 
Thanetian

    Fraction up in beginning stage: 
0.5

    Beginning date (Ma): 
57.62

    Ending stage: 
Thanetian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
56.00

Depositional setting

The sediments were deposited under transitional marine environments; higher proportion of carbonate facies in Kalachitta area points to stable marine setting while presence of coal in Salt Range indicate swampy conditions.


Depositional pattern:  


Additional Information

EMW: Coal, Source rock for oil & gas.


Compiler:  

Nusrat K. Siddiqui