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Lei Conglomerate Formation
Click to display on map of the Ancient World at:
Lei Conglomerate Fm base reconstruction

Lei Conglomerate Fm


Period: 
Quaternary

Age Interval: 
Late Pleistocene


Province: 
Pakistan Indus Basin

Type Locality and Naming

Holotype section:


Lithology and Thickness

Conglomerate; Thickness: 150-900 m thick in Trans Indus-Potwar Province (TrI-PP). 900 m in Urak synclinorium in Quetta region, 150-455 m in Kirthar Province.


Lithology Pattern: 
Conglomerate


Relationships and Distribution

Lower contact

Unconformably underlain by Suan Fm (Suon Fm) or Dada Conglomerate Fm

Upper contact

Overlain by subrecent deposits

Regional extent

Wide distribution in Indus Basin and Quetta region. Same distribution as the underlying Soan Fm


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[70.24,33.83],[73.2,33.98],[73.25,29.19],[71.92,27.83],[69.94,27.51],[71.13,24.45],[68.07,23.68],[67.03,25.04],[66.21,28.1],[67.47,30.37],[69.52,30.42],[70.24,33.83]]]]}}

Fossils


Age 

Late Pleistocene.

Age Span: 

    Beginning stage: 
Calabrian

    Fraction up in beginning stage: 
0.8

    Beginning date (Ma): 
0.98

    Ending stage: 
Holocene

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
0.00

Depositional setting

Deposited in fluvial and lacustrine environments. Valley-fill which covered extensive regions of Northern Potwar.


Depositional pattern:  


Additional Information


Compiler:  

Nusrat K. Siddiqui