Dev-F3 Fm
Type Locality and Naming
“Devonian rocks consist of interbedded marine sandstone and mudstone. Sandstone members within the Devonian section are each given a code, F2 to F6 with F6 being the oldest and F2 the youngest. These sandstone members are principal oil and gas reservoirs in the Illizi Province.” (USGS-Klett, 2000). [NOTE: For clarity, the prefix “Devon” is added in this Lexicon to these units, and the interbeds of “unnamed” marine mudstone between the “F-sands” are considered as the upper portion of that “F” member; except for F2-sand which ends this succession.]]
Synonym: F3 member.
References: Dardour et al., 2004; Benvegnù, 2020
Lithology and Thickness
The F3 Fm. is divided into four cycles (I to IV) of alternating shale, siltstone and sandstone (Benvegnù, 2020). The lower part of the sequence is made up of neritic to coastal deltaic cycles (Dardour et al., 2004).
Relationships and Distribution
Lower contact
It conformably overlies the F4-5 Fm.
Upper contact
It is unconformably overlain by the F2 Fm.
Regional extent
GeoJSON
Fossils
Age
Depositional setting
Neritic to coastal deltaic environment - barrier island environment (Benvegnù, 2020).
Additional Information
T.R. Klett (2000): Province, Algeria, Tunisia, and Libya - The Tanezzuft-Oued Mya, Tanezzuft-Melrhir, and Tanezzuft-Ghadames. U.S. Geological Survey Bulletin, 2202-C.