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Vein-type ore deposits were widely distributed over the Eastern Desert of Egypt and enclosing mineralization such as Sn-W mineralization at the Mueilha peraluminous granites (Abdalla et al. 2008), fluorite and beryl at Homr Akarem calc-alkaline granites (Hassan, and El Shatoury, 1976), Vein-type uranium mineralization are structurally controlled, for example Gabal El-Missikat, Gabal ElErediya at the central Eastern Desert (Bakhit, 1978; Abu Dief,1985; Hussein et al., 1986; Bakhit and Meleik, 1990; Hussein and Sayyah, 1991, Abu-Deif and El-Tahir, 2008) and Gabel El Sella peraluminous granites at the south Eastern Desert (Ibrahim et al., 2003).

Um Samra-Um Bakra Shear Zone, Central Eastern Desert, Egypt: Example of Vein -Type Base Metal Mineralization