Cenozoic

Cretaceous

Neoproterozoic

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

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Nsugbe Formation

Nsugbe Fm

Period:

Paleogene

Age Interval:

Eocene

Province:
Niger Delta - Outcrop

Type Locality and Naming

The Ameki Gr was given early attention by the Geological Survey of Nigeria but then affirmed by Nwajide (1979, 1980) and eventually nominating three component members that are laterally equivalent. It is an upward succession of the Ameki Fm, the Nanka Fm, and the Nsugbe Fm. The Nsugbe Fm was separated from the Nanka Fm and considered its lateral equivalent because it has a lithological succession that is different from the Nanka Fm, its textural characteristics set it apart, it has a degree of induration unknown to the Nanka Fm, and covers a substantial area of over 1000km² (Nwajide, 2013). Its type locality is around Nsugbe, a town some 10km north of northeast Onitsha (Nwajide, 2013).

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; Jauro et al., 2007; Zaborski et al., 1998; Obaje,2009; Nwajide, 2013

[Fig 1. Stratigraphic successions in the Benue Trough and the Nigerian sector of the Chad Basin]

Lithology and Thickness

Nsugbe Fm consists of two upward coarsening cycles. The lower cycle consists of flat-bedded, occasionally wave ripple-laminated, and burrowed, clayey, medium-grained sandstone. The cycle is capped off by an oligomictic, sharp-based, thick conglomerate composed of well-rounded quartz pebbles set in a matrix of coarse and poorly sorted ferruginous sandstone (Nwajide, 2013).

Lithology Pattern:

Clayey sandstone

Relationships and Distribution

Lower contact

Overlies the Nanka Fm.

Upper contact

Overlain unconformably by the Ogwashi-Asaba Fm

Regional extent

Niger Delta outcrop to Anambra Basin

GeoJSON

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Fossils

Whale remains (Pappocetus lugardi), Nautiloid (Deltoidnautilus nwajidei), gastropods (Siphonochelus nigeriensis, Turritella sp.)

Age

Late Eocene. Put here as Priabonian as constrained by assigned age span to the underlying Nanka Fm.

Age Span:

Beginning stage:

Priabonian

Fraction up in beginning stage:

0.0

Beginning date (Ma):

37.71

Ending stage:

Priabonian

Fraction up in the ending stage:

1.0

Ending date (Ma):

33.90

Depositional setting

The Nanka Fm has a Continental/coastal plain deposit to a shoreface setting and the Nsugbe Fm is characterized by a beach depositional setting (Nwajide, 2013)

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.