Rima Gr
Type Locality and Naming
Synonym: Taloka Fm Lower Sandstones and Mudstones (Jones, 1948), Dukamaje Fm (Clay-Shale Group (Raeburn and Tattam, 1930).
Reference section: Reyment,1965; Adeleye,1975; Kogbe,1976; Dessauvagie, 1975; Petters, 1978; Offodile, 1980; Whiteman, 1982; Benkhelil,1989; Okosun, 1992; Guiraud, 1993; Akandeet al., 1998; Zaborskiet al., 1998; Jauroet al., 2007 ; Obaje,2009; Nwajide, 2013
[Fig. 1. Stratigraphic successions in the Nigerian sector of the lullummeden Basin (Sokoto Basin)]
Lithology and Thickness
Wurno Fm consists of thin friable fine-grained sandstones intercalated with soft mudstone and shale (Ogilbee and Anderson, 1965). The formation locally contains carbonaceous matter and iron sulfide and characterized by load casts, bioturbation and flaser bedding (Nwajide, 2013).
Dukamaje Fm consists of dark fossiliferous shale with white spheroidal nodules and some thin limestone bands (Ogilbee and Anderson, 1965). Kogbe (1970 and 1976) stated that the Dukamaje Fm contains 98ft of Limestone and locally gypsiferous. It is estimated to be about 88ft at the Balle Borehole - GSN 3053 (Whiteman, 1982) and about 12m thick on the hill southwest of Dukamaje (Nwajide, 2013). It
Taloka Fm consists of white, fine grained, friable sandstones with intercalated mudstones and carbonaceous mudstones. It was given an estimated thickness of 393ft by Kogbe (1972).
Relationships and Distribution
Lower 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.