Jessu Fm
Type Locality and Naming
The type locality is the villages named after it. The lower sequence is the Dukul Fm followed by the Jessu Fm in the Middle Sequence and Sekuliye Fm at the top of the Sequence.
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 sandstone 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.
Jessu Formation generally ranges from 200 to 400 meters in thickness.
Relationships and Distribution
Lower contact
Lies conformably on the Dukui Fm
Upper contact
Lies conformably below the Sekuliye 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.