stripes
A 25 km diameter granite intrusion lies on the margin of the Nuba Mountains. It apparently comprises a single unit of peralkaline granite of perthite, sodic amphibole replaced by aegirine and accessory zircon. Rock analyses are available in Curtis and Lenz (1985)
BATYRMURZAEV, A.S., TROFIMOV, N.N., SHAKHPAZOV, I.M., AHMED, F., KHALIL, B.E., ZAKIEVA, F.S., GADZLIIEO, S.Z. and SLYMAEV, A.A. 1982. The absolute age of minerals in certain Sudanese provinces. In: Mobile belts and deposits. A collection of scientific papers, Academy of Sciences, Moscow. Patrice Lumumba University: 30-6. CURTIS, P. and LENZ, H. 1985. Geological and geochronological investigations of selected alkali igneous complexes in the Nuba Mountains, southern Kordofan, Sudan. Geologisches Jahrbuch, 69: 3-24.