Ameki Fm
Type Locality and Naming
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
Ameki Fm consists of grey-green sandy clays, sandy claystones and sandstones at its type locality in Eastern Nigeria. Two main lithological divisions have been recognized: a lower with fine to coarse grained sandstones with intercalations of calcareous shale and thin shelly limestone, limestone nodules; and an upper with coarse cross bedded sandstones, bands of fine grey-green sandstones and sandy clay (Whiteman, 1982). The maximum thickness estimate for the formation ranges from 1200-1500m (Nwajide, 2013).
Relationships and Distribution
Lower contact
Upper contact
Regional extent
GeoJSON
Fossils
Age
Depositional setting
Additional Information
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.