In Hatapang, North Sumatra, Permo-Carboniferous metawacke of the Tapanuli Group is intruded by a Cretaceous-Tertiary granite. At the contact, quartz veins, aplite, and pegmatite dykes cut the surrounding rocks. Cassiterite (tin) and wolframite (tungsten) occur in the veins and greisen zones, along with minerals like pyrite, arsenopyrite, and muscovite. Thin section and chemical analyses were us…