Through the First collision in the Asia and Indian plates, this granitic batholith was buried to depths of about twenty kilometres (12 mi) or maybe more, extremely metamorphosed, really deformed, and partly remelted during the Eocene Period of time to form gneiss. Later, the K2 Gneiss was then intruded by leucogranite https://troydulbs.blognody.com/34103890/top-guidelines-of-am678