stripes
This is a heavily faulted fragment of a ring structure which is covered by Nubian Sandstone on its northeastern side. The intrusion consists of peralkaline or biotite granite in the northeast and syenite in the southwest. The southern area is composed of felsite porphyries and the western part of basement rocks, hybrid biotite granite and trachyte dykes.
BARTH, H. and MEINHOLD, K.-D. 1979. Mineral prospecting in the Bayuda Desert. Part 1, Volume A. Investigation of mineral potential. Technical Report Sudanese-German Exploration Project. Hannover (Bundesanstalt fur Geowissenschaften und Rohstoffe). 336 pp. (unpublished) BARTH, H., BESANG, C., LENZ, H. and MEINHOLD, K.-D. 1983. Results of petrological investigations and Rb/Sr age determinations on the non-orogenic igneous ring-complexes in the Bayuda Desert, Sudan. Geologisches Jahrbuch, 51: 1-34.