Lithology and Thickness
The top of the
Rakb Gr. is equivalent to the Sirt Shale (Sirte Shale, or Sirte Fm) (Ahlbrandt, 2001). The Sirte Shale attains an average thickness of about 270 ft, and is made up of dark grey to dark brown organic rich shale (Selley, 1997). The mid-section of the
Rakb Gr is equivalent to the Rechmat Fm, while the base of the group is equivalent to the Arguib Fm. The Rachmat Formation consists of shales interbedded with minor limestones, sandstones and dolomites. The shales are dominantly grey, fissile to slightly blocky, to slightly non-calcareous, and glauconitic and pyritic in many locations. The
Rachmat Fm has a maximum thickness of up to 600 m in the Agedabia Trough (Abugares, 2007). The Arguib Fm (The Aragub carbonate is regarded as a basin-ward equivalent of the Etel Formation) consists of thin-bedded carbonates, shale, anhydrite, siltstone and sandstone – with its thickness ranging from 660 m in the Hagfa Trough to over 700 m in the Hameimat Trough.
GeoJSON
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Compiler:
s:T. S. Ahlbrandt (2001): The Sirte Basin Province of Libya—Sirte-Zelten Total Petroleum System,
U.S. Geological Survey Bulletin 2202–FR.C. Selley (1997): The Sirte Basin of Libya. In: African Basins. Sedimentary Basins of the World, 3, edited by R.C. Selley (Series Editor: K.J. Hsu),
Elsevier Science B.V., Amsterdam, pp. 27-37.Abugares, Miloud M. (2007): Deposition, Diagenesis, and Reservoir Development of the Cretaceous Lidam Formation, SE Sirt Basin, Libya.
Durham e-Theses. http://etheses.dur.ac.uk/2599/Elkanouni, I. E. D. (2014). Sedimentology, Sequence stratigraphy and Spatial-temporal Patterns of the late Paleocene Succession, western Sirt Basin, Libya, Durham e Theses. http://etheses.dur.ac.uk/10538/
Abdalla, M, Abdelnabi, A., Zubi, H., Qaysi, S. (2026): Depositional architecture and reservoir quality evaluation of the Early Cretaceous El Abd Sandstone Member: An integrated sedimentologic and diagenetic approach, eastern Sirte Basin, Libya. Jour. Sedimentary Environments, 11:41. https://doi.org/10.1007/s43217-026-00311-7.