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