Abu Harba area is located in the North Eastern Desert (NED) which mainly covered by metavolcanics,
Dokhan volcanics, metagabbro-diorite complex and younger granites. The detailed structural analysis of
Abu Harba area indicate that shear stress trending NNE-SSW and NW-SE directions represent nearly the
the Gulf of Aqaba and the Gulf of Suez trends. The lineaments in the area are multidirectional orientation
with three main trends; ENE-WSW, NE-SW and E-W with less dominant trends represented by N-S,
NNW-SSE and NW-SE directions.
The mineralizations of secondary uranium (uranophane, kasolite and betafite) in Abu Harba area seem
to be lithologically and structurally controlled. The alkali feldspar granites in the area contain highly
amounts of silica and alkalis, accessory minerals and iron oxides. On the other hand, the NE-SW
lineaments in the study area allowed the hydrothermal solution that bear uranium minerals to infiltrate
upwardly parallel faults and joint sets at the peripheral western part of G. Abu Harba alkali feldspar
granites. As the faults are suitable places for the flow of hydrothermal solutions bearing mineralization.
So, the mineralizations appear to be structurally controlled.