Teragh Fm
Type Locality and Naming
Valsardieu, 1971. Group: Terada Gr
References: Joulia, 1959a; Lessard, 1961; Claret & Tempère, 1968; Abdoulaziz et al., 1968; Valsardieu, 1971; Termier, 1973; Fabre et al., 1983; Conrad et al., 1986; Coquel et al., 1995; Fabre, 2005.
Synonym: "Grès et conglomérats de Teragh"; Upper sandstone Member of the Farrazekat Fm of Joulia (1959).
Equivalent(s): In Ateï Fm sandstone of Algeria
Lithology and Thickness
Conglomerates, sandstones and argillites in blocks, varved argillites and sandstones, corresponding to old moraines, transgressive on a basement shaped by ice. More to the south, away from the Niger/Algeria border (section #2 of Claret & Tempère (1968); see Fig. 7-72), these sandstones get differentiated from the “In Ateï Fm sandstones” of Algeria by greater development of the coarse material, in particular at the base of the upper cycle where one observes cones of deltaic debris containing plants at different levels. It is located at the base of the Terada Gr and represents an advanced witness of the Permo-Carboniferous glaciations of Gondwana. Thickness is 150 m.
Relationships and Distribution
Lower contact
Underlying unit is the Farrazekat Fm.
Upper contact
Overlying units are Talak Fm / Aoulingen Fm or Tim Mersoï Fm
Regional extent
GeoJSON
Fossils
Valsardieu (1971, p. 75) and Conrad et al. (1986) describe abundant plant material (Rhacopteris, Lepidodendron, Ulodendron, Archaeosigillaria, Calamites)
Age
Depositional setting
Fluvio-deltaic/glacial to continental shelf deposits. Includes old moraines, transgressive on a basement shaped by ice
Additional Information