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

Ewekoro Fm


Period: 
Paleogene

Age Interval: 
Paleocene


Province: 
Dahomey Basin

Type Locality and Naming

The type locality is in the West African Portland Cement Quarry about 40 miles north of Lagos (Whiteman, 1982). According to Nwajide (1982) the type locality is in Ewekoro, between Itori and Papa-Alanto and the type section is 145m thick from the GSN Borehole Nos. 1582 and 1583 drilled at Akinsinde and near Itori.

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

Ewekoro Formation is a thin shelly limestone, in places glauconitic, which becomes sandy near the base. Is a lateral equivalent of the Imo Shale Fm. The surface of the limestone is pot-holed, water-worn and scoured (Whiteman, 1982). According to Whiteman (1982) the formation is about 40ft thick at the type locality but according to Nwajide (1982) the type section is about 145m thick.


Lithology Pattern: 
Limestone


Relationships and Distribution

Lower contact

It grades down to the top of the Abeokuta Gr (Araromi Fm) (Whiteman, 1982)

Upper contact

Unconformably underlies the Akinbo Fm

Regional extent

The formation is traceable for 320km continuously from east Accra, eastwards through the whole of the Dahomey Basin (Enu and Adegoke, 1988).


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[4.6,6.2],[5.9,6.5],[4.6,7],[2.7,7.5],[1.2,6.1],[4.3,6.4],[4.6,6.2]]]]}}

Fossils

Echinoids, Gastropods, nautiloids, pelecypods, ostracods


Age 

early Paleocene (unconformity at base => left schematic gap of Lower Selandian)

Age Span: 

    Beginning stage: 
Danian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
66.04

    Ending stage: 
Selandian

    Fraction up in the ending stage: 
0.0

    Ending date (Ma):  
61.66

Depositional setting

Marine setting, under tropical littoral to neritic conditions (Whiteman, 1982).


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.