Abstract:El Sela area is mainly covered by ophiolitic mélange (Sul Hamed), biotite granite, two-mica granite (El Sela), muscovite granites (Qash Amer), and cross cut by microgranite dolerite and bostonite dikes as well as quartz and japser veins. These granitic rocks are hydrothermally altered, especially around El Sela ENE-WSW shear zone, that causing hydrothermal alterations accompanied by radioactive mineralization. These rocks are mainly composed of alkali feldspar, quartz, muscovite, and biotite with zircon, fluor… Show more
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