Hebeika Fm
Type Locality and Naming
Khartoum Basin, central Sudan. AAF-2 is considered type well for the Hebeika Formation, because it was not encountered in well AAF-1.
Reference: Awad (1994), A. Gibreel (2015)
[Fig. 1: Khartoum Basin is #8 on map (Fig.3 in Awad, 1994)]
[Fig. 2: Khartoum Basin stratigraphy and depositional sequences (pg. 17 in A. Gibreel, 2015)]
Lithology and Thickness
"The Hebeika Formation consists predominantly of interbedded tuffaceous claystone and sandstone; "weathered” volcanic basalt may also occur (Sun Oil, unpubl. rep ). Basal sandstones occur locally; these are primarily unlithified, coarse to very coarse, often argillaceous and the grains are subrounded and subangular." (Awad, 1994). It is ca. 390 m thick in well AAF-4, and 273 m in well AAF-2.
Relationships and Distribution
Lower contact
Upper contact
Regional extent
GeoJSON
Fossils
Age
Depositional setting
Additional Information
Gibreel, Ahmed (Section Head G&G Studies, Ministry of Petroleum and Gas, Republic of Sudan(, 2015. Hydrocarbon potential and resources in Sudan. [Slide presentation at UNCTAD, 17th Africa OILGASMINE, Khartoum, 23-26 Nov 2015]. https://unctad.org/system/files/non-official-document/17OILGASMINE%20Ahmed%20Gibreel%20Ahmed%20El-Amain%20S1.pdf