In the First collision from the Asia and Indian plates, this granitic batholith was buried to depths of about twenty kilometres (twelve mi) or even more, highly metamorphosed, remarkably deformed, and partially remelted during the Eocene Period to sort gneiss. Afterwards, the K2 Gneiss was then intruded by leucogranite dikes And https://spice-gold76394.thezenweb.com/spice-gold-fundamentals-explained-70946564