Home Multi-Country Search About Admin Login
Cenozoic
Cretaceous
Neoproterozoic


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

Search by
Select Region(s) to search
Hold Ctrl (Windows/Linux) or Command (Mac) to select multiple
Nsukka Formation
Click to display on map of the Ancient World at:
Nsukka Fm base reconstruction

Nsukka Fm


Period: 
Cretaceous, Paleogene

Age Interval: 
Late Maastrichtian – Danian


Province: 
Anambra Basin

Type Locality and Naming

Located near the territory around the Nsukka municipality and northwards (Nwajide, 2013).

References: Reyment, 1965; Adeleye, 1975; Dessauvagie, 1975; Kogbe, 1976; 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

The Nsukka Formation is considered as the top of the Coal Measures (Tatam, 1944; du Preez, 1947; Reyment and Barber, 1956) and estimated to be around 400m (Nwajide, 2013). The lithology is made up of an alternation of sandstones, shales, and coal beds.


Lithology Pattern: 
Clayey sandstone


Relationships and Distribution

Lower contact

conformably overlies the Ajali Fm.

Upper contact

Imo Fm conformably overlies the Nsukka Fm as one goes into the Niger Delta succession. Nsukka Fm seems to be the last sediment in the Anambra Basin.

Regional extent

Anambra Basin


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[8.5,4.7],[8.7,5],[7.9,5.7],[8.3,8.5],[7.5,8.3],[6.7,7.5],[7.3,6.6],[7.4,6],[7.8,5.9],[8.1,5],[8.5,4.7]]]]}}

Fossils

Ichnofossils (Skolithos, Ophiomorpha), Foraminifera (Afrobolivinaafra, Gabonitalata, Globorotalia pseudobulloides, Globorotaliapseudomenardi), Ostracods (Bythocyprissp., Buntonia sp., Veenia nigeriensis, Bairda ilaroensis, Parcypris nigeriensis, Cythreisdeltaensis, Buntoniaioruba), Dinoflagellates (Paleocystodinium golzowense, Impletosphaeridium sp., Deflandrea dubium)


Age 

Late Maastrichtian to Danian

Age Span: 

    Beginning stage: 
Maastrichtian

    Fraction up in beginning stage: 
0.7

    Beginning date (Ma): 
67.88

    Ending stage: 
Danian

    Fraction up in the ending stage: 
0.5

    Ending date (Ma):  
63.85

Depositional setting

Paralic conditions of the second post-Santonian transgressive cycle (Whiteman, 1982). Coal beds presence indicates periods of peat formation in swampy, deltaic conditions.


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.