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Cenozoic
Cretaceous


Information provided by geoscience team at Ahmadu Bello University, Zaria, Nigeria --see About

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Lafia Formation
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Lafia Fm base reconstruction

Lafia Fm


Period: 
Cretaceous

Age Interval: 
Campanian-Maastrichtian


Province: 
Benue Trough Central

Type Locality and Naming

Outcrops and sections of the Lafia Formation occur in and around the town of Lafia, and along the bank of River Amba on the Lafia – Doma road.

Synonym: Upper Grits and Sandstones (Falconer, 1911) and Lafia Sandstone (Cratchley and Jones, 1965)

References: Reyment, 1965; Adeleye, 1975; Kogbe, 1976; Dessauvagie, 1975; Petters, 1978; Offodile, 1980; Whiteman, 1982; Benkhelil, 1989; Okosun, 1992; Guiraud, 1993; Akande et al., 1998; Zaborski et al., 1998; Jauro et al., 2007; Obaje, 2009; Nwajide, 2013


Lithology and Thickness

It is lithologically characterized by cross-bedded ferruginized sandstones, red, loose sands, flaggy mudstones, clays and claystones. The Lafia Formation is confined to the Kadarko sub-basin with a thickness of 500-1500m (Offodile, 1976) but only about 50m reported east of Lafia where wedging is apparent. The thickness of the formation range from 500 to 800 meters.


Lithology Pattern: 
Sandstone


Relationships and Distribution

Lower contact

Lies unconformably onto the Awgu Fm.

Upper contact

The post-folding Campano-Maastrichtian Lafia Formation ended the sedimentation in the Middle Benue Trough, after which widespread volcanic activities took over in the Tertiary. It is overlain by the Gombe Fm (Gombe Sandstone Fm) or its Paleocene equivalents in different parts of the Middle Benue Trough.

Regional extent

Benue Trough Central. The Lafia Formation is confined to the Kadarko sub-basin


GeoJSON

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Fossils

Freshwater mollusks and carbonized plant remains, Pollen and Spores


Age 

Late Cretaceous (Campanian-Maastrichtian; but a hiatus of uppermost Maastrichtian-lowermost Danian is indicated on the summary strat chart of Benue Trough)

Age Span: 

    Beginning stage: 
Campanian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
83.65

    Ending stage: 
Maastrichtian

    Fraction up in the ending stage: 
0.8

    Ending date (Ma):  
67.27

Depositional setting

The formation was deposited under continental condition (fluviatile)


Depositional pattern:  


Additional Information


Compiler:  

Enam O. Obiosio, Solomon Joshua Avong and Henry Nasir Suleiman (2024)- Stratigraphic Lexicon compiled from the following books:

Nigeria: Its Petroleum Geology, Resources and Potential, by Arthur Whiteman, 1982; (Volume 1) Published by Graham and Trotman Ltd.

A review of the Cretaceous System in Nigeria by P. M. Zaborski (1998) In Africa Geoscience Review, Vol.5, No.4, pp385-483

Geology and Mineral Resources of Nigeria by Nuhu George Obaje, Published by Springer-Verlag Berlin Heidelberg 2009; http://www.springer.com/series/772

Geology of Nigeria Sedimentary Basins, Nwajide C. S., 2013; Published by CSS Bookshops Limited, Lagos Nigeria.