Owelli Sandstone Fm
Type Locality and Naming
Synonym: Owelli Fm
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
Owelli Fm: consists of massive, hard ferruginous sandstones. They are prominently cross-bedded in places and are generally medium to coarse-grained and contain pebble bands. Occasionally thin silty or argillaceous bands are present (Whiteman, 1982). The Owelli Sandstone is in general about 1,500ft thick (Simpson, 1954). There are also interbeds of marine, dark grey, micaceous, pyritic, calcareous, and occasionally glauconitic shales (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.