The Shingus pegmatite region is one of the largest in Pakistan. It is related to the Indo-Pakistan plate in the zone of subduction of Precambrian gneisses of the Nangaparbat complex, which overlie Cretaceous amphibole-pyroxene granulites of the Kokhistan island arc.
There are several pegmatite fields in the Shingus region: 1) Shingus-Bulochi
on both sides of the Indus gorge near villages of the same names, 16 km east of the junction of the Gilgit and Indus Rivers; 2) Haramosh
near a peak of the same name, 15 to 20 km north of Shingus; 3) Stak Nala
, 20 km east of Shingus village.
Ref: E. Ya. Kievlenko, Geology of gems, 2003, p. 110