Hofra Fm
Type Locality and Naming
Synonym: Equivalent to the Amal Fm in the eastern part of the basin.
References: Barr and Weeger, 1972; Ahlbrandt, 2001.
Lithology and Thickness
Relationships and Distribution
Lower contact
It unconformably overlies the Precambrian Basement Complex.
Upper contact
It is unconformably overlain by the Nubian Sandstone Fm. The Sirt Basin was a permanent high from the Middle Paleozoic until the Early Mesozoic (from SEPM overview).
Regional extent
GeoJSON
Fossils
Age
Depositional setting
Additional Information
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/