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Abstract The present study deals with the petro!,,>rapby, peh·ochemistry and the distribution of radioactive elements and minerals in the granitic rocks of Gabal El Zeit in the North Eastern Desert of Egypt. The area under examination is limited by Latitudes (270 25” ) and (280 00”) North and longitudes (330 25”) and (330 35”) East (Fig. !). This area is represented by an elongated NNW • SSE granitic mass (Main Gabal El Zeit) flanked by sedimentmy rocks of Paleozoic to Quaternary age (Salman etal,l988). |