1. Cообщение Кристиана Клайника от 21.12.2018 со ссылкой на:
  2. Nafi M., Awad M.Z., Abdel Rahman E.M., EL Amein A., El Dawi M., El Faki E.M., Salih K., El Badri O., Brugge N., Babikir A., El Hag A., Abou A., El Doma A., Abakar A. (2011). New Evidence of Upper Carboniferous-Permotriassic Strata In Northern Sudan // SAPG Jurnal, Firs t issue. - P. 29-43.
  3. Nafi M., EL Amein A., El Dawi M., Salih K., El Bahi O., Abou A. (2015). Wadi Halfa Oolitic Ironstone Formation, Wadi Halfa and Argein Areas, North Sudan // ICGS 2015: 17th International Conference Held in Osaka, Japan during October, 8-9, 2015.
  4. Geological map of the Sudan (1981) - 1:2 000 000.
"I discovered this new deeply eroded complex impact structure in NW Sudan. The structure lies in the Kufra basin (Mourdi sub basin), possible age is Triassic or younger, after it is formed in Permian-Triassic age Lakia sadstone sediments. The central peak is 5.5 Km diameter and clearly seen, the whole crater is 14 Km diameter (circular deformed boundary). Further investigations in this structure in progress!" (Krisztian Klajnik, 2018).

Спутниковая фотография кратера из Wikimapia.

Lakia crater central peak (К. Клайник).

Lakia structure geology (К. Клайник).

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