Sirte Shale Fm
Type Locality and Naming
The Sirte Shale is considered the main source rock in the Sirt Basin. It is the upper unit of the Rakb Gr is the Sirte Fm.
Synonym: Sirte Fm, Sirt Fm, Sirte Shale, Sirte Shales, Sirt Shale, or Sirt Shales. It is coeval to the Tagrifet Limestone elsewhere in the Sirte Basin.
References: Selley, 1997; Ahlbrandt, 2001; Abugares, 2007
Lithology and Thickness
Relationships and Distribution
Lower contact
It conformably overlies the Rachmat Fm.
Upper contact
It is conformably overlain by the Kalash Limestone Member of the Satal Fm.
Regional extent
GeoJSON
Fossils
Age
Depositional setting
Additional Information
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.