In the Original collision of your Asia and Indian plates, this granitic batholith was buried to depths of about 20 kilometres (12 mi) or even more, extremely metamorphosed, highly deformed, and partly remelted during the Eocene Interval to sort gneiss. Later on, the K2 Gneiss was then intruded by leucogranite dikes https://am67823226.pages10.com/the-best-side-of-5f-adbica-68346170