In-Azaoua Fm
Type Locality and Naming
Section #1 of Claret & Tempère (1968) in Algeria (see figures with In-Azaoua Gr). Joulia (1959). Claret & Tempère (1968) make it a formation of the “Tamesna Lower Sandstones” Group (see “In-Azaoua Gr”). Group: Upper formation in the In-Azaoua Gr
References: Joulia, 1959; Claret & Tempère, 1968; Fabre et al., 1983; Abdoulaye et al., 2007
Synonym: Grès d'In Azaoua (not to confused with the Assaouas Fm of Jurassic);
Relationships and Distribution
Lower contact
Underlying unit is the Tindi Fm of the same In-Azaoua Gr
Upper contact
Overlain by either the “Terminal Complex” at top of the In-Azaoua Gr or the Graptolitic Shales Fm
Regional extent
GeoJSON
Fossils
These sandstones contain a few scattered tigillites [= tube-like trace-fossil, mainly found in Ordovician]
Age
Depositional setting
Marine
Additional Information