Ise 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; Zaborski et al., 1998; Jauro et al., 2007; Obaje, 2009; Nwajide, 2013
Lithology and Thickness
Ise Fm: It is a pre-drift succession of conglomerates, sands, and mudrocks overlying the Basement Complex and continues upwards with medium to coarse, loose sand interbedded with kaolinitic clays (Nwajide, 2013). It is about 1,862m thick in the Ise-2 well (Omatsola and Adegoke, 1981).
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.