5 SIMPLE TECHNIQUES FOR CP 47

During the initial collision of the Asia and Indian plates, this granitic batholith was buried to depths of about twenty kilometres (12 mi) or maybe more, remarkably metamorphosed, hugely deformed, and partially remelted through the Eocene Period to kind gneiss. Afterwards, the K2 Gneiss was then intruded by leucogranite dikes and finally exhumed