Numanha Shale Fm
Type Locality and Naming
The type locality is in the villages named after it.
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; Ojo and Akande, 2004; Jauro et al., 2007; Obaje, 2009; Nwajide, 2013
[Fig 1. Stratigraphic successions in the Benue Trough and the Nigerian sector of the Chad Basin]
Lithology and Thickness
Schematically shown as entirely clay/shale in Fig. 2 of Sarki Yandoka et al., 2014
The Dukul Fm, Jessu Fm and Sekuliye Fm, the Numanha Shale Fm, and the Lamja Fm are the Turonian – Santonian equivalents of the Gongila Fm and Pindiga Fm in the Gongola Arm. The Turonian – Santonian deposits in the Yola Arm are lithologically and paleo-environmentally similar to those in the Gongola Arm, except the Lamja Sandstone Fm.
Thickness ??.
Relationships and Distribution
Lower contact
Lies conformably on the Sekuliye Fm
Upper contact
Lies conformably beneath the Lamja Fm (Lamja Sandstone Fm)
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.