[en] Granites exposed in northwestern part of Chitrial uranium deposit form the basement for Srisailam sediments. The Srisailam sediments occur as outlier in Chitrial area. These granites are intruded by quartz/quartzo-feldspathic/aplitic/pegmatite veins and mafic dykes. The basement granites of study area constitute grey and pink equigranular and porphyritic variants. They contain quartz, orthoclase, microcline, perthite, Na-plagioclase along with accessory biotite, ilmenite, sphene, apatite zircon, allanite, monazite and traces of fluorite. Among the opaques, magnetite, pyrite and goethite are present