This study deals with petrology and radioactivity of Gabal Al-Aglab younger granite, central Eastern desert, Egypt. Geologically the area consists of ophiolotic Mélange and younger granite. The study reveals that the younger granite are post orogenic granites, characterized by high differential index, which in turn represents the latest stage of the successive younger granite intrusions. Microscopically, Gabal Al-Aglab younger granites is holocrystalline, medium to coarse grained, characterized by the predominance of perthite over plagioclase, quartz and biotite. Zircon, apatite, titanite, allanite, and opaque minerals are the accessory and secondary minerals. The pegmatites occur as lenticular and circular pockets at the periphery of the younger granites. Geochemically, the younger granites show mainly peraluminous to metaluminous character and originated from subalkaline magma in within plate tectonic setting (crustal thickness > 30 km) at water vapour pressure varying from 0.5 to 3 kb with crystallization temperature between 670º to 800º C. Field survey together with the complied total count aeroradiometric map reveal that the pegmatites of Gabal Al-Aglab younger granite is significantly highly radioactive compared to the surrounding rocks. The uranium content varies between 3 to 12 ppm with an average of 7.1 ppm and thorium from 11 to 35 ppm with an average of 20 ppm and an average ratio (Th/U) 2.8.The pegmatites show higher U contents relative to their hosted younger granites as identified by microscopic investigation, scanning electron microscopy and confirmed by XRD.

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Wadi Mayet El-Abd is located in the northern part of G. Gattar, north Eastern Desert of Egypt. Significant remarks have been recorded on the heterogeneous distributions of heavy minerals content along the stream course, where they are most common in both deeper sediments and downstream sites. Moreover, these sediments appear to be slightly favorable delivery pools for thorium but not for uranium which is probably due to either the marked enrichment in the thorium-bearing minerals or the selective leaching for uranium during the supergene processes. The greater eU/U and eTh/U ratios, besides the negative values of the calculated authigenic uranium and further the markedly reverse relationships between uranium and thorium as well as uranium and Th/U ratio reveal the disequilibrium state of uranium and confirm U leaching. The available data propose that, the study sediments are potential sink for radioactive accessory minerals as well as rare metal minerals that may control the geochemical enrichment of trace elements as; U, Th, Zr, Y, Nb, REE, Ba, Zn and V. The present work adopts the ESEM/EDX-BSE as an appropriate tool for the recognition of the accessory minerals. The minerals; betafite, ishikawaite, xenotime, fluorite and zircon have been identified as the most abundant uraniferous accessory minerals; whereas monazite dominates as thorium-bearing mineral. Moreover, thorite and uranothorite have occasionally been recognized. A particular attention has been given to the contents of the rare metals in general and radionuclides in paticular in the accessory minerals, despite of their frequency in the whole stream sediments. In conclusion, the study sediments are conceivably genetically related to common sources. Actually it reflects the mineral constituent of the different rocks composing the drained area. Hence it may represent an erosional remnant either of the bordering granites and Hammamat molasses terrenes of Wadi Mayet El-Abd or drained from the further reaches which represent by the nearby weathered sediments of Wadi Belih at downstream sites.